&EPA
United States
Environmental Protection
Agency
Office of Research and
Development
Washington DC 20460
EPA/600/R-01/010
December 1999
Innovative Technology
Verification Report
Sediment Sampling
Technology
Aquatic Research Instruments
Russian Peat Borer
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EPA/600/R-01/010
December 1999
Innovative Technology
Verification Report
Aquatic Research Instruments
Russian Peat Borer
Prepared by
Tetra Tech EM Inc.
Chicago, Illinois
Contract No. 68-C5-0037
Dr. Stephen Billets
Environmental Sciences Division
National Exposure Research Laboratory
Office of Research and Development
U.S. Environmental Protection Agency
Las Vegas, Nevada 89193-3478
ET1/
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Notice
This document was prepared for the U.S. Environmental Protection Agency (EPA) Superfund
Innovative Technology Evaluation Program under Contract No. 68-C5-0037. The document has
been subjected to the EPA's peer and administrative reviews and has been approved for publication.
Mention of corporation names, trade names, or commercial products does not constitute endorsement
or recommendation of specific products for use.
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UNITED STATES ENVIRONMENTAL PROTECTION AGENCY
Office of Research and Development
Washington, DC 20460
ENVIRONMENTAL TECHNOLOGY VERIFICATION PROGRAM
VERIFICATION STATEMENT
^A
ii i^.^T
TECHNOLOGY TYPE: SEDIMENT SAMPLER
APPLICATION: CORE SAMPLING OF SEDIMENT
TECHNOLOGY NAME: AQUATIC RESEARCH INSTRUMENTS RUSSIAN PEAT BORER
COMPANY: AQUATIC RESEARCH INSTRUMENTS
ADORES S: 1 HAYDEN CREEK ROAD
LEMHI, IDAHO 83466
WEB SITE: http://www.aquaticresearch.com
TELEPHONE: (208) 756-8433
VERIFICATION PROGRAM DESCRIPTION
The U.S. Environmental Protection Agency (EPA) created the Superfund Innovative Technology Evaluation (SITE) and
Environmental Technology Verification (ETV) Programs to facilitate deployment of innovative technologies through
performance verification and information dissemination. The goal of these programs is to further environmental protection
by substantially accelerating the acceptance and use of unproved and cost-effective technologies. These programs assist and
inform those involved in design, distribution, permitting, and purchase of environmental technologies. This document
summarizes results of a demonstration of the Russian Peat Borer designed and fabricated by Aquatic Research Instruments.
PROGRAM OPERATION
Under the SITE and ETV Programs, with the full participation of the technology developers, the EPA evaluates and
documents the performance of innovative technologies by developing demonstration plans, conducting field tests, collecting
and analyzing demonstration data, and preparing reports. The technologies are evaluated under rigorous quality assurance
(QA) protocols to produce well-documented data of known quality. The EPA National Exposure Research Laboratory,
wiu'ch demonstrates field sampling, monitoring, and measurement technologies, selected Tetra Tech EM Inc. as the
verification organization to assist in field testing two sediment sampling technologies. This demonstration was funded by
the SITE Program.
DEMONSTRATION DESCRIPTION
In April and May 1999, the EPA conducted a field demonstration of the Russian Peat Borer along with one other sediment
sampler. This verification statement focuses on the Russian Peat Borer: a similar statement has been prepared for the other
sampler. The performance and cost of the Russian Peat Borer were compared to those of two conventional samplers (the
Hand Corer and Vibrocorer), which were used as reference samplers. To verify a wide range of performance attributes, the
Russian Peat Borer demonstration had both primary and secondary objectives. Primary objectives for this demonstration
included evaluating the sampler's ability to (1) consistently collect a given volume of sediment, (2) consistently collect
sediment in a given depth interval, (3) collect samples with consistent characteristics from a homogenous layer of sediment,
(4) collect a representative sample from a clean sediment layer below a contaminated sediment layer, and (5) be adequately
decontaminated. Additional primary objectives were to measure sampling time and estimate sampling costs. Secondary
objectives included (1) documenting the skills and training required for sampler operation, (2) evaluating the sampler's
ability to collect samples under a variety of site conditions, (3) assessing the sampler's ability to collect an undisturbed
sample, (4) evaluating sampler durability, and (5) documenting the availability of the sampler and its spare parts. To ensure
data usability, data quality indicators for precision, accuracy, representativeness, completeness, and comparability were also
assessed based on project-specific QA objectives.
EPA-VS-SCM-36 The accompanying notice is an integral part of this verification statement. December 1999
iii
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The Russian Peat Borer was demonstrated at sites in EPA Regions 1 and 5. At the Region 1 site, the sampler was
demonstrated in a lake and wetland. At the Region 5 site, the sampler was demonstrated in a river mouth and freshwater
bay. Collectively, the two sites provided multiple sampling areas with the different water depths, sediment types, sediment
contaminant characteristics, and sediment thicknesses necessary to properly evaluate the sampler. Based on the
predemonstration investigation results, demonstration objectives, and site support facilities available, (1) the Hand Corer
was used as the reference sampler in the lake, wetland, and freshwater bay and (2) the Vibrocorer was used as the reference
sampler in the river mouth. A complete description of the demonstration and a summary of its results are available in the
"Innovative Technology VerificationReport: Sediment Sampling Technology—Aquatic Researchlnstruments RussianPeat
Borer" (EPA/600/R-01/010).
TECHNOLOGY DESCRIPTION
The RussianPeat Borer is a manually driven, chambered-type, side-filling core sampler designed to collect discrete, relatively
uncompressed sediment samples. Sampler components include a stainless-steel core tube, aluminum extension rods, a
stainless-steel turning handle, and a Delrin® core head and bottom point that support a stainless-steel cover plate. The cover
plate and bottom point are sharpened to minimize sediment disturbance during sampler deployment. The core tube is hinged
to the cover plate by two pivot pins at the top and bottom of the plate. Support equipment for the sampler may include a
slide-hammer mechanism to aid sampler deployment and retrieval in consolidated sediment. To collect a sediment sample,
the RussianPeat Borer is manually inserted into sediment, and the core tube is turned 180 degrees clockwise. This procedure
allows the core tube to rotate and its sharp edge to longitudinally cut through the sediment, collecting a semicylindrical
sediment core. While the core tube is manually turned, the stainless-steel cover plate provides support so that the collected
material is retained in the core tube.
VERIFICATION OF PERFORMANCE
Key demonstration findings are summarized below for the primary objectives.
Consistently Collecting a Given Volume of Sediment. In the shallow depth interval (0 to 4 inches below sediment surface
[bss]), to collect a specified number of samples, the Russian Peat Borer required 33 percent more attempts than expected
(65 actual versus 49 expected), whereas the reference samplers required 14 percent more attempts than expected (49 actual
versus 43 expected). In the moderate depth interval (4 to 32 inches bss), the Russian Peat Borer required 21 percent more
attempts than expected (46 actual versus 38 expected), but the reference samplers required 156 percent more attempts than
expected (64 actual versus 25 expected).
For the shallow depth interval, mean sample recoveries ranging from 71 to 84 percent were achieved by the Russian Peat
Borer, whereas mean sample recoveries for the reference samplers ranged from 85 to 100 percent. The variation in sample
recoveries as measured by their relative standard deviations (RSD) ranged from 26 to 42 percent for the Russian Peat Borer,
whereas the reference samplers' RSDs ranged from 0 to 33 percent. For the moderate depth interval, mean sample recoveries
ranging from 75 to 101 percent were achieved by the Russian Peat Borer, whereas the reference samplers' mean sample
recoveries ranged from 21 to 82 percent. The RSDs for the Russian Peat Borer ranged from 6 to 31 percent, whereas the
reference samplers' RSDs ranged from 3 to 161 percent. (Note: sample recoveries exceeding 100 percent resulted from the
volumetric measurement error associated with the presence of void spaces when the sediment was transferred to a graduated
container.)
Consistently Collecting Sedimentin a Given Depth Interval. The RussianPeatBorer collected samples in all depth intervals
and demonstration areas, which contained various sediment types. The reference samplers were unable to collect samples
in the deep depth interval (4 to 11 feet bss). For the shallow depth interval, the Russian Peat Borer's actual core lengths
equaled the target core length in 98 percent of the total sampling attempts. The reference samplers' actual core lengths
equaled the target core length in 94 percent of the total sampling attempts. However, the results for the samplers were
significantly different for the moderate depth interval: 93 percent for the Russian Peat Borer compared to 13 percent for the
reference samplers.
Collecting Samples with Consistent Characteristics from a Homogenous Layer of Sediment: Based on particle size
distribution results, both the Russian Peat Borer and reference samplers collected samples with consistent physical
characteristics from two homogenous layers of sediment (a sandy silt layer and a clayey silt layer).
Collecting a Representative Samplefrom a Clean Sediment Layer Below a Contaminated Sediment Layer. The Russian
Peat Borer collected samples from a clean sediment layer below a contaminated sediment layer that were at least as
representative as the samples collected from the clean layer by the reference sampler (the Hand Corer); contaminant
concentrations in the samples collected by both samplers were not statistically different at a significance level of 0.05.
EPA-VS-SCM-36 The accompanying notice is an integral part of this verification statement. December 1999
iv
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Sampler Decontamination. Both the Russian Peat Borer and reference samplers demonstrated the ability to be adequately
decontaminated after sampling in areas contaminated with either polychlorinated biphenyls or arsenic.
Sampling Time. Compared to the reference samplers, the Russian Peat Borer not only was able to collect samples in all
depth intervals and demonstration areas but also reduced sampling time by 16 to 77 percent, depending on the area.
Sampling Costs. Of the sampling costs estimated for two of the four areas sampled, in one area the sampling costs for the
Russian Peat Borer were 90 percent less than those for the reference sampler (the Vibrocorer), and in the other area the
sampling costs for the Russian Peat Borer were 22 percent more than those for the reference sampler (the Hand Corer).
Key demonstration findings are summarized below for the secondary objectives.
Skill and Training Requirements. The Russian Peat Borer, like the Hand Corer, is easy to operate and requires minimal
skills and training. However, operation of the Vibrocorer is relatively complicated and requires moderate skills and training.
The Russian Peat Borer was operated by one person, whereas the Hand Corer was operated by one or two persons and the
Vibrocorer was operated by two persons. When more than two extension rods were required, the Hand Corer was operated
using a tripod-mounted winch. The Vibrocorer operation required a motor-operated winch, whereas the Russian Peat Borer
was operated without a winch throughout the demonstration.
Sampling Under a Variety of Site Conditions'. The Russian Peat Borer collected samples in all depth intervals and
demonstration areas, which contained various sediment types. The reference samplers were unable to collect samples in the
deep depth interval (4 to 11 feet bss). Neither the Russian Peat Borer nor the Hand Corer requires a power supply. In
contrast, the Vibrocorer requires a three-phase, 230- or 440-volt, 50- to 60-hertz power supply, which is a sampler limitation
if the power supply fails.
Collecting an Undisturbed Sample. The Russian Peat Borer collected representative core samples of consolidated sediment
in discrete depth intervals. Visual observations indicated that these samples were relatively uncompressed. In addition, the
RussianPeat Borer collected sediment samples containing live biota. The reference samplers collected relatively compressed
core samples of both consolidated and unconsolidated sediments from the sediment surface downward. In moderate and
deep depth intervals, samples collected by the reference samplers may be of questionable representativeness because of core
shortening and core compression. In the samples collected by the Russian Peat Borer, sediment stratification was preserved
for consolidated sediment but not for unconsolidated sediment. Sediment stratification was preserved for both consolidated
and unconsolidated sediments in the samples collected by the reference samplers.
Sampler Durability and Availability. Based on their materials of construction and engineering designs, both the Russian
Peat Borer and reference samplers are considered to be sturdy. The Russian Peat Borer and its support equipment are not
expected to be available in local retail stores. Similarly, the primary components of the Hand Corer and Vibrocorer are not
expected to be available in local retail stores; extension rods for the Hand Corer may be locally available.
Based on the demonstration results, the Russian Peat Borer can be operated by one person with minimal skills and training
and does not require support equipment such as a winch and power source even when collecting sediment samples at depths
up to 11 feet bss. The sampler can collect representative and relatively uncompressed samples of consolidated sediment in
discrete depth intervals. The sampler preserves sediment stratification in consolidated sediment samples, but sediment
stratification may not be preserved in unconsolidated sediment samples. The Russian Peat Borer is a superior alternative
to conventional sediment samplers, particularly for sampling consolidated sediment. As with any sampler selection, the user
must determine the appropriate sampler for a given application based on project-specific data quality objectives.
Gary J. Foley, Ph.D.
Director
National Exposure Research Laboratory
Office of Research and Development
NOTICE: EPA verifications are based on an evaluation of technology performance under specific, predetermined criteria and
appropriate quality assurance procedures. The EPA makes no expressed or implied warranties as to the performance of the technology
and does not certify that a technology will always operate as verified. The end user is solely responsible for complying with any and
all applicable federal, state, and local requirements.
EPA-VS-SCM-36 The accompanying notice is an integral part of this verification statement. December 1999
V
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Foreword
The U.S. Environmental Protection Agency (EPA) is charged by Congress with protecting the
nation's natural resources. Under the mandate of national environmental laws, the agency strives
to formulate and implement actions leading to a compatible balance between human activities and
the ability of natural systems to support and nurture life. To meet this mandate, the EPA Office of
Research and Development provides data and scientific support that can be used to solve
environmental problems, build the scientific knowledge base needed to manage ecological resources
wisely, understand how pollutants affect public health, and prevent or reduce environmental risks.
The National Exposure Research Laboratory (NERL) is the agency's center for investigation of
technical and management approaches for identifying and quantifying risks to human health and the
environment. Goals of the laboratory's research program are to (1) develop and evaluate methods
and technologies for characterizing and monitoring air, soil, and water; (2) support regulatory and
policy decisions; and (3) provide the scientific support needed to ensure effective implementation
of environmental regulations and strategies.
The EPA Superfund Innovative Technology Evaluation (SITE) Program evaluates technologies
designed for characterization and remediation of contaminated Superfund and Resource
Conservation and Recovery Act sites. The SITE Program was created to provide reliable cost and
performance data in order to speed acceptance and use of innovative remediation, characterization,
and monitoring technologies by the regulatory and user community.
Effective measurement and monitoring technologies are needed to assess the degree of
contamination at a site, provide data that can be used to determine the risk to public health or the
environment, supply the necessary cost and performance data to select the most appropriate
technology, and monitor the success or failure of a remediation process. One component of the EPA
SITE Program, the Monitoring and Measurement Technology (MMT) Program, demonstrates and
evaluates innovative technologies to meet these needs.
Candidate technologies can originate within the federal government or the private sector. Through
the SITE Program, developers are given the opportunity to conduct a rigorous demonstration of their
technologies under actual field conditions. By completing the demonstration and distributing the
results, the agency establishes a baseline for acceptance and use of these technologies. The MMT
Program is administered by the Environmental Sciences Division of NERL in Las Vegas, Nevada.
Gary J. Foley, Ph.D.
Director
National Exposure Research Laboratory
Office of Research and Development
VI
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Abstract
The Russian Peat Borer designed and fabricated by Aquatic Research Instruments was demonstrated
under the U.S. Environmental Protection Agency (EPA) Superfund Innovative Technology
Evaluation Program in April and May 1999 at sites in EPA Regions 1 and 5, respectively. In
addition to assessing ease of sampler operation, key objectives of the demonstration included
evaluating the sampler's ability to (1) consistently collect a given volume of sediment,
(2) consistently collect sediment in a given depth interval, (3) collect samples with consistent
characteristics from a homogenous layer of sediment, and (4) collect samples under a variety of site
conditions. This report describes the demonstration results for the Russian Peat Borer and two
conventional samplers (the Hand Corer and Vibrocorer) used as reference samplers. During the
demonstration, the Russian Peat Borer was the only sampler that collected samples in the deep depth
interval (4 to 11 feet below sediment surface). It collected representative and relatively
uncompressed core samples of consolidated sediment in discrete depth intervals. The reference
samplers collected relatively compressed samples of both consolidated and unconsolidated sediments
from the sediment surface downward; sample representativeness may be questionable because of
core shortening and core compression. Sediment stratification was preserved only for consolidated
sediment samples collected by the Russian Peat Borer but for both unconsolidated and consolidated
sediment samples collected by the reference samplers. Sampling time was less for the Russian Peat
Borer than for the reference samplers. Sampling costs for the Russian Peat Borer were 90 percent
less than those for the Vibrocorer and 22 percent more than those for the Hand Corer.
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Contents
Chapter Page
Notice ii
Verification Statement iii
Foreword vi
Abstract vii
Figures xiii
Tables xv
Abbreviations, Acronyms, and Symbols xvii
Acknowledgments xix
1 Introduction 1
1.1 Description of the SITE Program 1
1.2 Scope of the Demonstration 4
2 Description of the Innovative Sediment Sampler 5
2.1 Sampler Description 5
2.2 General Operating Procedures 7
2.3 Advantages and Limitations 8
2.4 Developer Contact Information 8
3 Demonstration Site Descriptions 9
3.1 EPA Region 5 Site (Site 1) 9
3.1.1 Site l,Areal 9
3.1.2 Site 1, Area 2 10
3.2 EPA Region 1 Site (Site 2) 11
3.2.1 Site 2, Area 1 11
3.2.2 Site 2, Area 2 11
4 Demonstration Approach 12
4.1 Demonstration Objectives 12
Vlll
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Contents (Continued)
Chapter Page
4.2 Demonstration Design 13
4.3 Field Sampling and Measurement Procedures 16
4.4 Laboratory Sample Preparation and Analysis Methods 22
5 Description of the Reference Sediment Samplers 25
5.1 Hand Corer 25
5.1.1 Technology Description 25
5.1.2 General Operating Procedures 26
5.1.3 Advantages and Limitations 27
5.2 Vibrocorer 27
5.2.1 Technology Description 27
5.2.2 General Operating Procedures 28
5.2.3 Advantages and Limitations 29
6 Performance of the Russian Peat Borer 30
6.1 Primary Objectives 30
6.1.1 Ability to Consistently Collect a Specified Volume of Sediment .... 31
6.1.1.1 Number of Sampling Attempts Required 31
6.1.1.2 Volume of Sediment Collected 33
6.1.2 Ability to Consistently Collect Sediment in a Specified Depth
Interval 37
6.1.3 Ability to Collect Multiple Samples with Consistent Physical or
Chemical Characteristics, or Both, from a Homogenous Layer of
Sediment 39
6.1.4 Ability to Collect a Representative Sample from a Clean Sediment
Layer Below a Contaminated Sediment Layer 40
6.1.5 Ability to be Adequately Decontaminated 44
6.1.6 Time Requirements for Sample Collection Activities 44
6.2 Secondary Objectives 45
6.2.1 Skill and Training Requirements for Proper Sampler Operation 45
6.2.2 Ability to Collect Samples Under a Variety of Site Conditions 46
6.2.3 Ability to Collect an Undisturbed Sample 47
6.2.4 Durability Based on Materials of Construction and Engineering
Design 47
6.2.5 Availability of Sampler and Spare Parts 48
6.3 Data Quality 48
6.3.1 Field Measurement Activities 48
6.3.2 Laboratory Analysis Activities 49
7 Performance of the Reference Samplers 52
7.1 Primary Objectives 52
7.1.1 Ability to Consistently Collect a Specified Volume of Sediment .... 53
7.1.1.1 Number of Sampling Attempts Required 53
7.1.1.2 Volume of Sediment Collected 55
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Contents (Continued)
Chapter Page
7.1.2 Ability to Consistently Collect Sediment in a Specified Depth
Interval 57
7.1.3 Ability to Collect Multiple Samples with Consistent Physical or
Chemical Characteristics, or Both, from a Homogenous Layer of
Sediment 59
7.1.4 Ability to be Adequately Decontaminated 62
7.1.5 Time Requirements for Sample Collection Activities 62
7.2 Secondary Objectives 64
7.2.1 Skill and Training Requirements for Proper Sampler Operation 64
7.2.2 Ability to Collect Samples Under a Variety of Site Conditions 65
7.2.3 Ability to Collect an Undisturbed Sample 66
7.2.4 Durability Based on Materials of Construction and Engineering
Design 66
7.2.5 Availability of Sampler and Spare Parts 66
7.3 Data Quality 67
7.3.1 Field Measurement Activities 67
7.3.2 Laboratory Analysis Activities 68
8 Economic Analysis 69
8.1 Issues and Assumptions 69
8.1.1 Sampler Costs 69
8.1.2 Labor Costs 69
8.1.3 IDW Disposal Costs 70
8.1.4 Support Equipment Costs 70
8.1.5 Costs Not Included 70
8.2 Russian Peat Borer Costs 71
8.2.1 Sampler Cost 72
8.2.2 Labor Cost 72
8.2.3 IDW Disposal Cost 73
8.2.4 Support Equipment Cost 73
8.2.5 Summary of Russian Peat Borer Costs 73
8.3 Hand Corer Costs 73
8.3.1 Sampler Cost 74
8.3.2 Labor Cost 74
8.3.3 IDW Disposal Cost 74
8.3.4 Support Equipment Costs 74
8.3.5 Summary of Hand Corer Costs 74
8.4 Vibrocorer Costs 75
8.4.1 Sampler Cost 75
8.4.2 Labor Cost 75
8.4.3 IDW Disposal Cost 75
8.4.4 Support Equipment Cost 75
8.4.5 Summary of Vibrocorer Costs 75
8.5 Comparison of Economic Analysis Results 75
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Contents (Continued)
Chapter
Pas
9 Summary of Demonstration Results 77
9.1 Primary Objectives 77
9.2 Secondary Objectives 82
10 References 83
Appendix A Developer's Claims for the ARI Russian Peat Borer 85
Appendix B Performance and Cost of the Ekman Grab 89
B.I Description of the Ekman Grab 89
B.I.I Sampler Description 89
B.I.2 General Operating Procedures 90
B.I.3 Advantages and Limitations 91
B.2 Description of the Demonstration Sites 91
B.3 Demonstration Approach 91
B.3.1 Demonstration Objectives 91
B.3.2 Demonstration Design 92
B.3.3 Field Sampling and Measurement Procedures 93
B.4 Performance of the Ekman Grab 95
B.4.1 Primary Objectives 95
B.4.1.1 Ability to Consistently Collect a Specified Volume of
Sediment 96
B.4.1.2 Ability to Consistently Collect Sediment in a Specified
Depth Interval 98
B.4.1.3 Ability to Collect Multiple Samples with Consistent
Physical or Chemical Characteristics, or Both, from a
Homogenous Layer of Sediment 99
B.4.1.4 Ability to be Adequately Decontaminated 100
B.4.1.5 Time Requirements for Sample Collection Activities 100
B.4.1.6 Costs Associated with Sample Collection Activities 102
B.4.2 Secondary Objectives 104
B.4.2.1 Skill and Training Requirements for Proper Sampler
Operation 104
B.4.2.2 Ability to Collect Samples Under a Variety of Site
Conditions 105
B.4.2.3 Ability to Collect an Undisturbed Sample 105
B.4.2.4 Durability Based on Materials of Construction and
Engineering Design 106
B.4.2.5 Availability of Sampler and Spare Parts 106
B.4.3 Data Quality 106
B.4.3.1 Field Measurement Activities 106
B.4.3.2 Laboratory Analysis Activities 107
B.5 References 107
XI
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Contents (Continued)
Chapter Pas
Appendix C Statistical Methods 109
C.I Wilk-Shapiro Test 109
C.2 Wilcoxon Signed Rank Test 110
C.3 References 113
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Figures
Figure Page
2-1. Russian Peat Borer 6
4-1. Site 1 sampling locations 17
4-2. Site 2 sampling locations 18
5-1. Hand Corer 26
5-2. Vibrocorer 28
6-1. Percent sample recoveries for Russian Peat Borer at Site 1 34
6-2. Percent sample recoveries for Russian Peat Borer at Site 2 35
6-3. Russian Peat Borer sample particle size distribution results for
S1A2 (freshwater bay) 40
6-4. Russian Peat Borer sample arsenic and particle size distribution results for
S2A1 (lake) 41
6-5. Comparison of Russian Peat Borer and reference sampler sample arsenic
concentration results for S2A1 (lake) 43
7-1. Percent sample recoveries for Vibrocorer and Hand Corer at Site 1 55
7-2. Percent sample recoveries for Hand Corer at Site 2 56
7-3. Hand Corer sample particle size distribution results for S1A2 (freshwater bay) 60
7-4. Hand Corer sample arsenic and particle size distribution results for S2A1 (lake) 61
B-l. Ekman Grab 90
B-2. Sampling locations for Ekman Grab demonstration 94
B-3. Percent sample recoveries for Ekman Grab in S1A1 (river mouth),
S1A2 (freshwater bay), and S2A1 (lake) 99
B-4. Ekman Grab sample analytical results for S1A1 (river mouth) and S2A1 (lake) .... 101
C-l. Wilk-Shapiro test plot for core length measurements in S1A2 (freshwater bay) 110
C-2. Wilk-Shapiro test plot for core length measurements in S2A2 (wetland) Ill
C-3. Statistix® output for Hand Corer sample data for S2A2 (wetland) 112
Xlll
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Figures (Continued)
Figure Page
C-4. Statistix® output for Hand Corer and Russian Peat Borer sample data for
S2A1 (lake) 113
xiv
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Tables
Table Page
2-1. Russian Peat Borer Model Specifications 7
3-1. Demonstration Area Characteristics 10
4-1. Innovative Sediment Sampler Demonstration Design 14
4-2. Rationale for Sampling Approach 19
4-3. Sample Matrix 21
4-4. Laboratory Sample Preparation and Analysis Methods 23
4-5. Laboratory Quality Control Checks 24
6-1. Comparison of Expected and Actual Number of Sampling Attempts for
Russian Peat Borer at Site 1 32
6-2. Comparison of Expected and Actual Number of Sampling Attempts for
Russian Peat Borer at Site 2 33
6-3. Percent Sample Recovery Summary Statistics for Russian Peat Borer 36
6-4. Comparison of Target and Actual Core Length Data for Russian Peat Borer 38
6-5. Particle Size Distribution Summary Statistics for Russian Peat Borer 42
6-6. Time Required to Complete Sampling Activities for Russian Peat Borer 44
6-7. Summary of Quality Control Checks and Acceptance Criteria for Field and
Laboratory Parameters 50
7-1. Comparison of Expected and Actual Number of Sampling Attempts for
Reference Samplers at Site 1 53
7-2. Comparison of Expected and Actual Number of Sampling Attempts for
Reference Sampler at Site 2 54
7-3. Percent Sample Recovery Summary Statistics for Reference Samplers 57
7-4. Comparison of Target and Actual Core Length Data for Reference Samplers 58
7-5. Particle Size Distribution Summary Statistics for Hand Corer 62
7-6. Time Required to Complete Sampling Activities for Reference Samplers 63
xv
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Tables (Continued)
Table Page
8-1. Comparison of Investigation-Derived Waste Quantities Generated by
Russian Peat Borer and Reference Samplers 70
8-2. Russian Peat Borer Cost Summary 72
8-3. Hand Corer Cost Summary for S2A1 (Lake) 73
8-4. Vibrocorer Cost Summary for S1A1 (River Mouth) 74
8-5. Comparison of Costs for Russian Peat Borer and Reference Samplers 76
9-1. Summary of Results for Primary Objectives 78
9-2. Summary of Results for Secondary Objectives 80
B-l. Ekman Grab Demonstration Design 92
B-2. Rationale for Sampling Approach 95
B-3. Ekman Grab Sample Matrix 96
B-4. Comparison of Expected and Actual Number of Sampling Attempts for
Ekman Grab at Site 1 97
B-5. Comparison of Expected and Actual Number of Sampling Attempts for
Ekman Grab in S2A1 (Lake) 97
B-6. Percent Sample Recovery Summary Statistics for Ekman Grab 98
B-7. Comparison of Target and Actual Sediment Thickness Data for Ekman Grab 100
B-8. Particle Size Distribution Summary Statistics for Ekman Grab 102
B-9. Time Required to Complete Sampling Activities for Ekman Grab 103
B-10. Ekman Grab Cost Summary 104
C-l. Data Sets for Example Wilk-Shapiro Test Calculations 110
C-2. Hand Corer Sample Data for 4- to 12-Inch Below Sediment Surface
Depth Interval in S2A2 (Wetland) Ill
C-3. Hand Corer and Russian Peat Borer Sample Data for 10- to 30-Inch
Below Sediment Surface Depth Interval in S2A1 (Lake) 112
xvi
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Abbreviations, Acronyms, and Symbols
> Greater than
<, Less than or equal to
± Plus or minus
< Less than
ARI Aquatic Research Instruments
ASTM American Society for Testing and Materials
BS/BSD Blank spike/blank spike duplicate
bss Below sediment surface
CFR Code of Federal Regulations
cm Centimeter
DER Data evaluation report
EPA U.S. Environmental Protection Agency
ETV Environmental Technology Verification
FLAA Flame atomic absorption
ft Foot
ft/s Foot per second
GLNPO Great Lakes National Program Office
ICP Inductively coupled argon plasma
IDW Investigation-derived waste
ITVR Innovative technology verification report
L Liter
Ib Pound
m Meter
mg/kg Milligram per kilogram
mg/L Milligram per liter
mL Milliliter
MMT Monitoring and Measurement Technology
MS/MSD Matrix spike/matrix spike duplicate
NA Not applicable
NERL National Exposure Research Laboratory
ORD Office of Research and Development
OSWER Office of Solid Waste and Emergency Response
PCB Polychlorinated biphenyl
PE Performance evaluation
PSD Particle size distribution
PSR Percent sample recovery
QA Quality assurance
QA/QC Quality assurance/quality control
QC Quality control
XVII
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Abbreviations, Acronyms, and Symbols (Continued)
RPD Relative percent deviation
RSD Relative standard deviation
S1A1 Site 1, Area 1
S1A2 Site 1, Area 2
S2A1 Site 2, Area 1
S2A2 Site 2, Area 2
SITE Superfund Innovative Technology Evaluation
SOP Standard operating procedure
Statistix® Statistix® for Windows, Version 2.0
TCLP Toxicity characteristic leaching procedure
Tetra Tech Tetra Tech EM Inc.
TSA Technical system audit
XVlll
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Acknowledgments
This report was prepared for the U.S. Environmental Protection Agency (EPA) Superfund Innovative
Technology Evaluation (SITE) Program under the direction and coordination of Dr. Stephen Billets
and Dr. Brian Schumacher of the EPA National Exposure Research Laboratory—Environmental
Sciences Division in Las Vegas, Nevada. The SITE Program thanks Mr. Joseph LeMay and
Mr. Andy Beliveau of EPA Region 1, Mr. Robert Paulson of the Wisconsin Department of Natural
Resources, and Mr. Marc Tuchman and Mr. Scott Cieniawski of the EPA Great Lakes National
Program Office for their support in conducting field activities for this project. Mr. Jonathan Kuhns
of Hawk Consulting and Dr. Larry Jackson of Environmental Quality Management served as the peer
reviewers of this report.
This report was prepared for the EPA by Dr. Kirankumar Topudurti, Mr. Eric Monschein, and
Mr. Andrew Bajorat of Tetra Tech EM Inc. Special acknowledgment is given to Ms. Jeanne
Kowalski, Mr. Jon Mann, Mr. Stanley Labunski, Ms. Sandy Anagnostopoulos, Ms. Amy Stephen,
Mr. Gary Sampson, and Mr. Bob Overman for their assistance during the preparation of this report.
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Chapter 1
Introduction
The U.S. Environmental Protection Agency (EPA) Office
of Research and Development's (ORD) National
Exposure Research Laboratory (NERL) has conducted a
demonstration of an innovative sediment sampler known
as the Russian Peat Borer, a core sampler designed and
fabricated by Aquatic Research Instruments (ARI) of
Lemhi, Idaho. The demonstration was conducted under
the EPA Superfund Innovative Technology Evaluation
(SITE) Program at two sites during the last week of April
and first week of May 1999. The purpose of this
demonstration was to obtain reliable performance and
cost data on the Russian Peat Borer in order to (1) achieve
a better understanding of the sampler's capabilities
relative to conventional sediment samplers and
(2) provide an opportunity for the sampler to enter the
marketplace and compete with conventional samplers
without long delays.
This innovative technology verification report (ITVR)
presents the performance results of the demonstration and
associated costs for the Russian Peat Borer. Specifically,
this report describes the SITE Program and the scope of
the demonstration (Chapter 1), innovative sediment
sampler that was demonstrated (Chapter 2), two
demonstration sites (Chapter 3), demonstration approach
(Chapter 4), conventional sediment samplers used as
reference samplers during the demonstration (Chapter 5),
performance of the innovative sampler (Chapter 6),
performance of the reference samplers (Chapter 7),
economic analysis for the innovative and reference
samplers (Chapter 8), demonstration results in summary
form (Chapter 9), and references used to prepare the
ITVR (Chapter 10). ARI claims for, updates on, and
information on previous deployments of the innovative
sampler are provided in Appendix A. Appendix B
presents performance results for the Ekman Grab, a
conventional grab sampler that was included in the
demonstration because grab samplers are commonly used
to collect surficial sediment in order to assess the
horizontal distribution of sediment characteristics.
Appendix C describes the statistical methods used, as
appropriate, to address the primary objectives for the
demonstration.
1.1 Description of the SITE Program
Performance verification of innovative environmental
technologies is an integral part of the regulatory and
research mission of the EPA. The SITE Program was
established by the EPA Office of Solid Waste and
Emergency Response (OSWER) and ORD under the
Superfund Amendments and Reauthorization Act of 1986.
The primary purpose of the SITE Program is to promote
acceptance and use of innovative sampling, monitoring,
measurement, and treatment technologies.
The overall goal of the SITE Program is to conduct
research and performance verification studies of
innovative technologies that may be used to achieve long-
term protection of human health and the environment. The
various components of the SITE Program are designed to
encourage development, demonstration, acceptance, and
use of innovative sampling, monitoring, measurement, and
treatment technologies. The program is designed to meet
four primary objectives: (1) identify and remove obstacles
to development and commercial use of innovative
technologies, (2) support a development program that
identifies and nurtures emerging technologies,
(3) demonstrate promising innovative technologies to
establish reliable performance and cost information for site
characterization and cleanup decision-making, and
(4) develop procedures and policies that encourage use of
innovative technologies at Superfund sites as well as at
other waste sites and commercial facilities.
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The intent of a SITE demonstration is to obtain
representative, high-quality performance and cost data on
one or more innovative technologies so that potential
users can assess a given technology's suitability for a
specific application. The SITE Program includes the
following elements:
• Monitoring and Measurement Technology (MMT)
Program—Evaluates technologies that sample,
detect, monitor, and measure hazardous and toxic
substances. These technologies are expected to
provide better, faster, and more cost-effective
methods for producing real-time data during site
characterization and remediation studies than do
conventional technologies.
• Remediation Technology Program—Conducts
demonstrations of innovative treatment technologies
to provide reliable performance, cost, and
applicability data for site cleanups.
• Technology Transfer Program—Provides and
disseminates technical information in the form of
updates, brochures, and other publications that
promote the SITE Program and technologies. It also
offers technical assistance, training, and workshops
to support the technologies.
The innovative sediment sampler demonstration was
conducted as part of the MMT Program, which provides
developers of innovative hazardous waste sampling,
monitoring, and measurement technologies with an
opportunity to demonstrate their technologies'
performance under actual field conditions. These
technologies may be used to sample, detect, monitor, or
measure hazardous and toxic substances in soil, sediment,
waste material, or groundwater. The technologies include
chemical sensors for in situ (in place) measurements,
groundwater samplers, soil and sediment samplers, soil
gas samplers, laboratory and field-portable analytical
equipment, and other systems that support field sampling
or data acquisition and analysis.
The MMT Program promotes acceptance of technologies
that can be used to accurately assess the degree of
contamination at a site, provide data to evaluate potential
effects on human health and the environment, apply data
to assist in selecting the most appropriate cleanup action,
and monitor the effectiveness of a remediation process.
The program places a high priority on innovative
technologies that provide more cost-effective, faster, and
safer methods for producing real-time or near-real-time data
than do conventional technologies. These innovative
technologies are demonstrated under field conditions, and
the results are compiled, evaluated, published, and
disseminated by ORD. The primary objectives of the
MMT Program are as follows:
• Test field sampling and analytical technologies that
enhance sampling, monitoring, and site
characterization capabilities
• Identify performance attributes of innovative
technologies to address field sampling, monitoring, and
characterization problems in a more cost-effective and
efficient manner
• Prepare protocols, guidelines, methods, and other
technical publications that enhance acceptance of these
technologies for routine use
The MMT Program is administered by the Environmental
Sciences Division of NERL in Las Vegas, Nevada. The
NERL is the EPA's center for investigation of technical
and management approaches for identifying and
quantifying risks to human health and the environment.
The NERL's mission components include (1) developing
and evaluating methods and technologies for sampling,
monitoring, and characterizing water, air, soil, and
sediment; (2) supporting regulatory and policy decisions;
and (3) providing the technical support needed to ensure
effective implementation of environmental regulations and
strategies. By demonstrating selected innovative sediment
samplers, the MMT Program is supporting development
and evaluation of methods and technologies for sampling
and characterizing sediment.
The MMT Program's technology performance verification
process is designed to conduct demonstrations that will
generate high-quality data that potential users can employ
to verify technology performance and cost. Four key steps
are inherent in the process: (1) needs identification and
technology selection, (2) demonstration planning and
implementation, (3) report preparation, and (4) information
distribution.
The first step of the technology performance verification
process begins with identifying technology needs of the
EPA and regulated community. The EPA regional offices,
the U.S. Department of Energy, the U.S. Department of
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Defense, industry, and state environmental regulatory
agencies are asked to identify technology needs for
sampling, monitoring, and measurement of environmental
media. Once a need is identified, a search is conducted to
identify suitable technologies that will address the need.
The technology search and identification process consists
of examining industry and trade publications, attending
related conferences, exploring leads from technology
developers and industry experts, and reviewing responses
to Commerce Business Daily announcements. Selection
of technologies for field testing includes evaluation of the
candidate technologies based on several criteria. A
suitable technology for field testing
• Is designed for use in the field
• Is applicable to a variety of environmentally
contaminated sites
• Has potential for solving problems that current
methods cannot satisfactorily address
• Has estimated costs that are competitive with those of
current methods
• Is likely to achieve better results than current
methods in areas such as data quality and turnaround
time
• Uses techniques that are easier and safer than current
methods
• Is commercially available
Once candidate technologies are identified, their
developers are asked to participate in a developer
conference. This conference gives the developers an
opportunity to describe their technologies' performance
and to learn about the MMT Program.
The second step of the technology performance
verification process is to plan and implement a
demonstration that will generate high-quality data that
potential users can employ to verify technology
performance and cost. Demonstration planning activities
include a predemonstration sampling and analysis
investigation that assesses existing conditions at the
proposed demonstration site or sites. The objectives of
the predemonstration investigation are to (1) confirm
available information on applicable physical, chemical,
and biological characteristics of contaminated media at the
sites to justify selection of site areas for the technology
demonstration; (2) provide the technology developers with
an opportunity to evaluate the areas and identify logistical
requirements; (3) determine the overall logistical
requirements for conducting the demonstration; and
(4) provide the analytical laboratories with an opportunity
to identify any matrix-specific analytical problems
associated with contaminated media and propose
appropriate solutions. Information generated through the
predemonstration investigation is used to develop the
demonstration design and sampling and analysis
procedures.
Demonstration planning activities also include preparation
of a demonstration plan that describes the procedures to be
used to verify the performance and cost of each innovative
technology. The demonstration plan incorporates
information generated during the predemonstration
investigation as well as input from technology developers
and demonstration site representatives. The demonstration
plan also incorporates the quality assurance and quality
control (QA/QC) elements needed to produce data of
sufficient quality to document the performance and cost of
each technology.
During the technology performance verification process,
each innovative technology is evaluated independently and,
when possible, against a reference technology. The
performance of a developer or innovative technology is not
compared to that of another developer or innovative
technology. Rather, demonstration data are used to
evaluate the performance, cost, advantages, limitations, and
field applicability of each technology.
As part of the third step of the technology performance
verification process, the EPA publishes a verification
statement and a detailed evaluation of each technology in
an ITVR. To ensure its quality, the ITVR is published
only after comments from the technology developer and
external peer reviewers are satisfactorily addressed. All
demonstration data used to evaluate each innovative
technology are summarized in a data evaluation report
(DER) that constitutes a record of the demonstration. The
DER is not published by the EPA, but an unpublished copy
may be obtained by contacting the EPA project manager,
Dr. Stephen Billets.
The fourth step of the technology performance verification
process is to distribute demonstration information. The
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EPA distributes ITVRs free of charge through direct
mailings, at conferences, and on the Internet to benefit
technology developers and potential technology users.
ITVRs are available on the Internet through the
Hazardous Waste Clean-Up Information web site
supported by the EPA OSWER Technology Innovation
Office (http://www.clu-in.org). Additional information
on the SITE Program is provided at the ORD web site
(http://www.epa.gov/ORD/SITE).
1.2 Scope of the Demonstration
Environmental sediment sampling is conducted to
characterize sediment at a particular location. Sediment
characterization may involve biological analyses (for
biological availability and benthic biota), chemical
analyses (for organic and inorganic contaminants), and
physical analyses (for color, texture, and particle size
distribution [PSD]). Sediment samplers are typically
designed to collect discrete samples of sufficient quantity
and quality at a predetermined depth relatively easily and
in a reasonable amount of time. Although the samplers
now being used meet most sediment sampling
requirements, innovative samplers may be faster and
easier to operate, less expensive, and more accurate and
precise.
The MMT Program members involved in the Russian
Peat Borer demonstration included the EPA NERL, the
EPA National Risk Management Research Laboratory,
EPA Region 1, the Wisconsin Department of Natural
Resources, the EPA Great Lakes National Program Office
(GLNPO), and ARI.
The performance of the Russian Peat Borer was
demonstrated and compared to that of conventional
sediment samplers in order to provide evidence that the
Russian Peat Borer worked as intended and to facilitate
its use. The conventional sediment samplers, which are
referred to as reference samplers herein, are described in
Chapter 5. For the demonstration, either a Hand Corer or
a Vibrocorer was used as a reference sampler, depending
on site conditions and sampler availability.
In addition to the Russian Peat Borer, ARI was given the
opportunity to substitute one alternate innovative sampler
if ARI believed that the alternate sampler was better
suited for the conditions and objectives being addressed
in a particular sampling area. However, ARI elected not to
demonstrate an alternate innovative sampler.
A conventional grab sampler was also included in the
demonstration because grab samplers are commonly used
to collect surficial sediment in order to assess the horizontal
distribution of sediment characteristics. The Ekman Grab,
a commonly used grab sampler, was chosen for the
demonstration. Performance and cost data collected for the
Ekman Grab are not be compared to those for the Russian
Peat Borer but rather are presented in Appendix B as
supplemental information.
The demonstration had both primary and secondary
objectives. The primary objectives were critical to the
technology evaluation and required use of quantitative
results to draw conclusions regarding technology
performance. The secondary objectives pertained to
information that was useful but did not necessarily require
use of quantitative results to draw conclusions regarding
technology performance. Based on available historical data
forthe demonstration sites, the primary objectives required
use of chemical and physical characterization of sediment
but not biological characterization. The primary and
secondary objectives are presented in Chapter 4.
To meet the demonstration objectives, individual areas at
two sites were selected for conducting the demonstration.
The first site is referred to as Site 1; it included two areas
and lies in EPA Region 5. The second site is referred to as
Site 2; it included two areas and lies in EPA Region 1.
These sites and areas are described in Chapter 3.
In preparation for the demonstration, a predemonstration
sampling and analysis investigation was completed at the
two sites in February 1999. The purpose of this
investigation was to assess whether the sites were
appropriate for evaluating the Russian Peat Borer based on
the demonstration objectives. The demonstration was
conducted during the last week of April and first week of
May 1999. The procedures used to verify the performance
and cost of the Russian Peat Borer are summarized in a
demonstration plan completed in April 1999 (EPA 1999).
The demonstration plan also incorporates the QA/QC
elements needed to generate data of sufficient quality to
document innovative and reference sampler performance
and cost. The plan is available on the Internet through the
ORD web site (http://www.epa.gov/ORD/SITE).
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Chapter 2
Description of the Innovative Sediment Sampler
Core samplers are commonly used to collect sediment
profiles in order to assess the vertical distribution of
sediment characteristics. Based on the method of sample
collection, core samplers may be broadly classified into
two categories: (1) end-filling core samplers and (2) side-
filling core samplers (Faegri and Iversen 1989). An end-
filling sampler typically consists of one or more core tubes
or a box that collects sediment from the bottom end of the
sampler as it is pushed through the sediment. An end-
filling sampler generally collects sediment from the
sediment surface down to a particular depth. Once the
core sample is extruded through the end of the sampler, a
discrete depth interval of the core sample may be
subsampled. Examples of end-filling samplers include the
Hand Corer, Split Core Sampler, Dual Tube Liner
Sampler, and Vibrocorer. Additional details on end-filling
samplers are provided by Environment Canada (1994),
Blomqvist (1991), Faegri and Iversen (1989), Aaby and
Digerfeldt (1986), and Downing (1984).
A side-filling core sampler is operated by first driving the
sampler to a particular depth. The core tube is then rotated
clockwise to fill the tube by cutting out a segment of
sediment. A large cover plate attached to the core tube
holds the sampler stationary while the tube rotates
clockwise to collect the sediment. Resistance offered by
the sediment keeps the cover plate stationary, allowing the
core tube to rotate. Examples of side-filling samplers
include the Russian sampler and the Hiller sampler (Faegri
and Iversen 1989). The Russian sampler was described
first by Belokopytov and Beresnevich (1955) and later by
Jowsey (1966). Additional details on the Hiller sampler
are provided by Faegri and Iversen (1989) and Aaby and
Digerfeldt (1986).
This chapter describes the Russian Peat Borer designed
and fabricated by ARI. ARI developed the Russian Peat
Borer during the early 1990s, improving on similar
Russian samplers that have been used since the 1950s.
Sections 2.1 through 2.4 describe the Russian Peat Borer,
discuss its general operating procedures, outline its
advantages and limitations, and provide developer contact
information. Similar information for the reference
samplers used during the demonstration is provided in
Chapters.
2.1 Sampler Description
Components of the Russian Peat Borer include (1) a
stainless-steel, chambered-type core tube; (2) 40-inch-
long, 1-inch-diameter, aluminum extension rods; (3) a
stainless-steel turning handle; and (4) a Delrin® core head
and bottom point that support a stainless-steel cover plate
(see Figure 2-1). The cover plate is curved and sharpened
to minimize disturbance when the sampler is inserted into
sediment. The core tube is hinged to the cover plate by
two stainless-steel pivot pins at the top and bottom of the
plate. Support equipment for operation of the sampler
may include a slide-hammer mechanism and 10-foot-long,
1.3-inch-diameter, magnesium-zirconium extension rods.
The Russian Peat Borer is readily available in three
models whose specifications are presented in Table 2-1.
ARI will also manufacture Russian Peat Borers of
different design specifications upon request.
Site-specific sampling requirements should be considered
during selection of the most appropriate Russian Peat
Borer model for a given application. For example,
Model A (with its 2-inch-inside diameter, 20-inch-long
core tube) encounters the least resistance during sampler
deployment and retrieval through the sediment because of
its short length and small turning radius. As a result, this
model may be selected to collect samples in deep depth
intervals, where the degree of sediment compaction is
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Turning handle
Sharp edge
Rivet
Empty core
tube
Blunt edge
Beginning position
Sediment
Extension
rod
• Rivet
Rotation (clockwise)
ling position
Core head
Pivot pin
Sediment
Core tube
Closed position
Sediment
Rotation (counterclockwise)
Extruding position
Sharp edge
Jilfo
Sediment
Ending position
Sharp edge
Bottom point
Cross-sectional top views
Cross-sectional side view
Figure 2-1. Russian Peat Borer.
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Table 2-1. Russian Peat Borer Model Specifications
Core Tube
Model3
A
B
C
Length (inches)
20
40
25
Inside Diameter (inches)
2
2
3
Volume (ml)
500
1,050
1,450
Per Inch" (ml)
26
26
58
Weight0 (Ib)
5.5
15
14
Notes:
Ib = Pound
ml = Milliliter
a The model designations are specific to this report and are not used in the developer's product catalog.
b The design volume is the maximum volume of sediment that the sampler can collect per unit length of core tube (1 inch); for a given target depth
interval, the design volume corresponds to 100 percent sample recovery.
0 The weight shown does not include extension rods; each 40-inch-long, 1-inch-diameter, aluminum extension rod weighs about 2 Ib.
expected to be high. Model B (with its 2-inch-inside
diameter, 40-inch-long core tube) may be selected to
collect sediment in both shallow and moderate depth
intervals because of its greater length and ability to
collect sediment in both intervals in one attempt.
Model C (with its 3-inch-inside diameter, 25-inch-long
core tube) may be selected to collect sediment in
situations requiring larger sample volume because of its
larger core tube diameter.
The Russian Peat Borer is manually inserted into
sediment in the beginning position, and the core tube is
turned 180 degrees clockwise until the sharp edge of the
tube contacts the cover plate. This procedure allows the
core tube to rotate and the sharp edge to longitudinally
cut through the sediment, collecting a semicylindrical
sediment core. Resistance offered by the sedimentholds
the cover plate stationary, allowing the core tube to
rotate. The cover plate also provides support so that the
collected material is retained in the core tube.
The Russian Peat Borer is innovative because the core
head and bottom point are made of Delrin®, a self-
lubricating, thermoplastic polymer that has a high
modulus of elasticity as well as strength, stiffness, and
resistance to abrasion and the degrading effects of
moisture. Earlier sediment samplers with a similar
design typically were made entirely of stainless steel
and therefore were heavy; the use of Delrin® has made
the sampler lighter. In addition, ARI limited the
thickness of the stainless-steel cover plate and the core tube
to 2 millimeters in order to minimize the resistance created
by the sediment during sampler deployment and core tube
rotation. ARI also designed the aluminum extension rods to
be light in weight and to float in water. Finally, according
to ARI, the optional, 10-foot-long, 1.3-inch-diameter,
magnesium-zirconium rods available for sampler
deployment to depths greater than 50 feet below sediment
surface (bss) are durable, light in weight, and easily coupled
and uncoupled.
2.2 General Operating Procedures
The Russian Peat Borer can be operated by one person from
a platform, from a boat, or while wading in shallow water.
Figure 2-1 presents a five-stage depiction of the Russian Peat
Borer operating procedures. The sampler is operated by
manually inserting the bottom point of the sampler into the
sediment with the blunt edge of the core tube turned against
the cover plate to prevent sediment from entering the tube
during penetration. A slide-hammer mechanism can be used
to drive the sampler through highly consolidated sediment or
peat that is hard to penetrate. The sampling technician
should practice sampler deployment to determine whether a
slide-hammer is needed.
Once the sampler is driven into the sediment to the desired
depth, the turning handle is manually turned 180 degrees
clockwise, allowing the sharpened edge of the core tube to
longitudinally cut through the sediment, collecting a
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semicylindrical sediment core. The sampler reaches the
closed position once the sharp edge of the core tube is in
contact with the cover plate. Once it is in the closed
position, the sampler can be manually retrieved. As the
sampler is retrieved within the sediment, a constant,
clockwise pressure on the sampler is required to ensure
that the core tube remains in the closed position. As the
sampler is dislodged from the sediment, the sampler is
retrieved in such a way that the cover plate is above the
core tube. As a result, gravity pulls down on the cover
plate, further ensuring that the core tube remains in the
closed position. The sampler is turned progressively
more horizontal as it nears the water surface, reaching
about a 45-degree angle as it is removed from the water.
The sampler is positioned horizontally immediately
thereafter. The sampler is then rotated and placed on the
sampling platform in such a way that the core tube is
above the cover plate. The core tube is then manually
turned counterclockwise, rotating the tube and exposing
the semicylindrical core sample on the cover plate.
To allow consecutive, complete reconstruction of along
sediment profile, two Russian Peat Borers can be
alternately deployed side-by-side to alternating depths.
This procedure allows continuous core samples to be
collected sequentially, with one sampler remaining in
the sediment as a sample is collected using the other
sampler. This procedure is designed to minimize
disturbance of the sediment while ensuring that a
complete, continuous sediment core is collected.
2.3 Advantages and Limitations
An advantage of the Russian Peat Borer is that it is easy
to operate, requiring minimal skills and training.
Although ARI currently does not have a training video
or written standard operating procedure (SOP), sampler
assembly and collection procedures can be learned in the
field with a few practice attempts. The sampler can be
operated by one person because of its lightness (see
Table 2-1). Sampler operation is simple because it has
only one moving part (the core tube rotates
180 degrees). Moreover, the sampler does not require
disassembly to extrude the sample and reassembly after
each sampling attempt. The sampler requires no support
equipment other than two sawhorses for supporting the
sampler during sample extrusion, a slide-hammer
mechanism, and a safe sampling platform.
The Russian Peat Borer also has the unique ability to collect
discrete, relatively uncompressed core samples from shallow
to deep depth intervals without disturbing the sediment
stratification. In addition, when only deep core samples are
required, the amount of investigation-derived waste (IDW)
generated is minimized because the Russian Peat Borer is a
discrete sampler.
A limitation of the Russian Peat Borer is that the sampler
requires extension rods for deployment in deep water
applications. In addition, the sampler is not equipped with
disposable core liners. During sampler deployment, the
cover plate is exposed to different layers of sediment
contamination. Contaminants may adhere to the exposed
surface of the cover plate while the sampler passes through
different layers of sediment, increasing the risk of cross-
contamination between sampling depth intervals. However,
the sampling technician has the option to discard the portion
of the sediment core near the cover plate if necessary based
on project-specific requirements.
Another limitation of the Russian Peat Borer is that during
sampling, partially decomposed plant matter or small stones
may become caught between the core tube and the cover
plate, causing the core tube to remain in the open position
during sampler retrieval and resulting in sediment washout.
Furthermore, collection of a sediment sample using the
sampler requires that the sediment offer enough resistance
(support) to keep the cover plate stationary and allow
rotation of the core tube.
2.4 Developer Contact Information
Additional information about the Russian Peat Borer can be
obtained from the following source:
Mr. Will Young
Aquatic Research Instruments
1 Hayden Creek Road
Lemhi, ID 83466
Telephone: (208) 756-8433
Fax: (208) 756-8435
E-mail: hydrobio@aol.com
Internet: www.aquaticresearch.com
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Chapter 3
Demonstration Site Descriptions
This chapter discusses the two sites selected for
conducting the Russian Peat Borer demonstration. The
first site is referred to as Site 1 and includes two areas
along a river in EPA Region 5. The second site is referred
to as Site 2 and includes two areas along a river in EPA
Region 1. After a review of the information available on
these and other candidate sites, Sites 1 and 2 were selected
based on the following criteria:
• Site Diversity—Each site consisted of multiple
sampling areas with the different water depths, flow
regimes, sediment types, sediment contaminant
characteristics, and sediment thicknesses necessary to
evaluate the Russian Peat Borer.
Access and Cooperation—Site representatives were
interested in supporting the demonstration by
providing historical data and site access.
In February 1999, a predemonstration sampling and
analysis investigation was conducted to assess existing site
conditions and to confirm information provided by EPA
Regions 1 and 5. The predemonstration investigation
results summarized in Table 3-1 were used to develop the
demonstration design for the innovative and reference
samplers. The following sections provide brief
descriptions of the two demonstration sites.
3.1 EPA Region 5 Site (Site 1)
Site 1 consists of sections of a river in EPA Region 5.
Two areas along the river were selected as demonstration
areas. These areas and the sampling platforms used are
briefly described below and shown in Figure 4-1.
3.1.1 Site 1, Area 1
Site 1, Area 1 (S1A1) lies at the river mouth, which is
about 0.5 mile wide. The area generally represents an
open-water condition. During the demonstration, the
average water velocity in this area was less than or equal
to 0.07 foot per second (ft/s). The water depth in the
vicinity of S1A1 ranged from about 5 to 6 feet. Sampling
in S1A1 was conducted using the EPA GLNPO's
Mudpuppy, a 32-foot-long, 8-foot-wide, twin-motor, flat-
bottom boat specifically designed for sediment sampling
in rivers and harbors. The boat is equipped with a
vibrocoring unit supported by an A-frame and winch that
allows collection of sediment cores up to 15 feet long.
Additional features that make the Mudpuppy a suitable
platform for conducting vibrocoring or other sediment
sampling include the following:
A sampling platform at the bow of the boat with a hole
in the middle wide enough to accommodate the
vibrocoring unit
Adequate deck space for subsampling and processing
15-foot-long core samples
A differentially corrected global positioning system
with submeter accuracy that allows precise and
accurate determination of sampling locations
Four anchor lines for maintaining the boat's position
over sampling locations
An electrical power source for support equipment
Table 3-1. Demonstration Area Characteristics
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Demonstration Area
S1A1 (river mouth)
S1A2 (freshwater bay)
S2A1 (lake)
S2A2 (wetland)
Average Water
Velocity3 (ft/s)
<0.07
<0.05
<0.05
< 0.05 to 0.7
Water Depth3
(ft)
5 to 6
2
18
O.Sto 1.5
Predemonstration Investigation Results
Target Sampling
Depth Interval
(inches bss)
Oto4
4 to 12
Oto6
12 to 36
Oto4
10 to 30
4 to 12
Contaminant
PCBs
PCBs
PCBs
None"
Arsenic
Arsenic
Arsenic
Physical Characteristics
Unconsolidated sediment containing primarily
sand with some silt and little clay
Consolidated sediment containing primarily sand
and silt with some clay
Unconsolidated sediment containing primarily
sand and silt with some clay
Consolidated sediment containing primarily silt
with some sand and clay
Unconsolidated sediment containing primarily silt
with some sand and clay
Consolidated sediment containing primarily sand
with some silt and little clay
Consolidated sediment containing primarily sand
with some silt and little clay
Notes:
< = Less than or equal to
< = Less than
bss = Below sediment surface
ft = Foot
ft/s = Foot per second
PCB = Polychlorinated biphenyl
Average water velocity and water depth represent data collected during the actual demonstration.
No measurable PCB contamination was present in this depth interval.
Predemonstration investigation sample analytical results
for S1A1 indicated that polychlorinated biphenyl (PCB)
contamination in the 0- to 4-inch bss depth interval was
minimal. However, the 4- to 12-inch bss depth interval in
this area had the highest levels of PCB contamination of
any depth interval sampled during the predemonstration
investigation. Based on the PSD data, sediment in the 0-
to 4-inch bss depth interval was predominantly sand with
some silt and little clay. PSD in the 4- to 12-inch bss
depth interval was predominantly sand and silt with some
clay. Sediment in the 0- to 4-inch bss depth interval was
Unconsolidated and became increasingly consolidated
below this depth interval. During the demonstration, a
clay hardpan was encountered at about 5 feet bss in the
sampling area. Based on the PCB and PSD data from the
predemonstration investigation, the sediment in the 0- to
4-inch bss depth interval in S1A1 appeared to be
chemically and physically homogenous. However, the
sediment in the 4- to 12-inch bss depth interval in this area
did not appear to be as chemically or physically
homogenous as was the case in Site 1, Area 2 (S1A2).
3.1.2 Site 1, Area 2
S1A2 is about 11 miles upstream of S1A1. The river is
about 2,000 feet wide in S1A2. A small, protected bay is
present along the river channel's bank at this location.
This bay has a very slow-moving current and, because of
its configuration, backflow conditions. During the
demonstration, the average water velocity in the area of
the bay was less than 0.05 ft/s. The water depth in the bay
was about 2 feet. Sampling in S1A2 was conducted within
the bay using an 18-foot-long, 4-foot-wide, flat-bottom Jon
boat. The boat was equipped with a single engine, a set of
oars, and a single anchor line for positioning the boat over
sampling locations. The Mudpuppy could not be used to
conduct sampling in S1A2 because the water in this area
was too shallow (the Mudpuppy requires a minimum water
depth of about 3 feet).
Predemonstration investigation sample analytical results
for S1A2 indicated that PCB contamination in the 0- to
6-inch bss depth interval was minimal but greater than that
10
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in the 0- to 4-inch bss depth interval in S1A1.
Furthermore, the 12- to 36-inch bss depth interval in S1A2
had no measurable PCB contamination. Sediment in the
0- to 6-inch bss depth interval was predominantly sand and
silt with some clay. Sediment in the 12- to 36-inch bss
depth interval was predominantly silt with some sand and
clay. Sediment in the top few inches was unconsolidated
and became consolidated with increasing depth. Based on
the PSD data from the predemonstration investigation,
sediment in the 12- to 36-inch bss depth interval in S1A2
appeared to be the most physically homogenous at Site 1.
3.2 EPA Region 1 Site (Site 2)
Site 2 consists of sections of a river in EPA Region 1. The
river, which has a moderate flow, runs through a low-lying
wetland area and empties into a lake. Two areas along the
river were selected as demonstration areas. These areas
and the sampling platforms used are briefly described
below and are shown in Figure 4-2.
3.2.1 Site 2, Area 1
Site 2, Area 1 (S2A1) is a lake located about 5 miles
downstream of Site 2, Area 2 (S2A2). During the
demonstration, the average water velocity in the area was
less than 0.05 ft/s, and the water depth was about 18 feet.
Sampling in S2A1 was conducted using a 30-foot-long,
8-foot-wide pontoon boat. The pontoon boat was
equipped with a single engine and eight anchor lines for
positioning the boat over sampling locations. In addition,
a 6-inch-diameter hole was provided in the middle of the
boat to allow use of a core sampler with a tripod-mounted
winch. The front and sides of the boat would not
accommodate a tripod-mounted winch.
Predemonstration investigation sample analytical results
for S2A1 indicated that the 0- to 4-inch bss depth interval
in this area had more consistent and higher levels of
arsenic contamination and more consistent PSD than was
the case in S2A2. Arsenic contamination in the 0- to
4-inch bss depth interval in S2A1 was an order of
magnitude greater than that in the 10- to 30-inch bss depth
interval. Sediment in the 0- to 4-inch bss depth interval
was predominantly silt with some sand and clay. Sediment
in the 0- to 4-inch bss depth interval was unconsolidated
and became increasingly consolidated below this depth
interval. Sediment in the 10- to 30-inch bss depth interval
was predominantly sand with some silt and little clay.
Based on the arsenic and PSD data from the
predemonstration investigation, the sediment in the 10- to
30-inch bss depth interval in S2A1 appeared to be the most
chemically and physically homogenous sediment at Site 2.
3.2.2 Site 2, Area 2
S2A2 is a low-lying wetland along the river. This
area is about 5 miles upstream of S2A1. The river channel
is about 10 feet wide in S2A2. Water flow in this area is
low to moderate, reflecting seasonal variations. During
the demonstration, the average water velocity in the area
ranged from less than 0.05 to 0.7 ft/s, and water depths in
the area ranged from about 0.5 to 1.5 feet. Sampling in
S2A2 was conducted from wood planks fastened to two
aluminum ladders extended across the river channel.
Depending on the individual needs of each sampling
technician, (1) samples were collected off the side of one
ladder or (2) the sampling technician stood with one foot
on each ladder to collect samples between the ladders.
At the time of the predemonstration investigation, the top
4 to 8 inches of sediment in S2A2 contained organic
matter, primarily decomposed leaves and wood chips.
Predemonstration investigation sample analytical results
for S2A2 indicated that levels of arsenic contamination
from the bottom of the organic layer down to 12 inches bss
were nonuniform and lower than the levels in S2A1. In
S2A2, sediment in the 4- to 12-inch bss depth interval
(below the organic layer) was predominantly sand with
some silt and little clay. Sediment in this depth interval
was highly consolidated. Based on the arsenic and PSD
data from the predemonstration investigation, S2A2 did
not appear to be as chemically or physically homogenous
as S2A1. In addition, historical data provided by EPA
Region 1 indicated that a 30-foot-thick layer of peat
existed below the sediment layer in S2A2.
11
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Chapter 4
Demonstration Approach
This chapter presents the demonstration objectives
(Section 4.1), design (Section 4.2), field sampling and
measurement procedures (Section 4.3), and laboratory
sample preparation and analysis methods (Section 4.4).
4.1 Demonstration Objectives
The main intent of the SITE MMT Program is to develop
reliable performance and cost data on innovative
technologies. A SITE demonstration must provide
detailed and reliable performance and cost data so that
potential technology users have adequate information to
make sound judgments regarding a technology's
applicability to a specific site and to compare the
technology to alternatives.
The Russian Peat Borer demonstration had both primary
and secondary objectives. Primary objectives were critical
to the technology evaluation and required use of
quantitative results to draw conclusions regarding
technology performance. Secondary objectives pertained
to information that was useful but did not necessarily
require use of quantitative results to draw conclusions
regarding technology performance.
The primary objectives for the innovative sediment
sampler demonstration were as follows:
PI. Evaluate whether the sampler can consistently
collect a specified volume of sediment
P2. Determine whether the sampler can consistently
collect samples in a specified depth interval
P3. Assess the sampler's ability to collect multiple
samples with consistent physical or chemical
characteristics, or both, from a homogenous layer of
sediment
P4. Evaluate whether the sampler can collect a
representative sample from a "clean" sediment layer
that is below a contaminated sediment layer
P5. Assess the sampler's ability to be adequately
decontaminated between sampling areas
P6. Measure the time required for each activity
associated with sample collection (sampler setup,
sample collection, sampler disassembly, and
sampler decontamination)
P7. Estimate costs associated with sample collection
activities (sampler, labor, supply, IDW disposal, and
support equipment costs)
The secondary objectives for the innovative sediment
sampler demonstration were as follows:
SI. Document the skills and training required to
properly operate the sampler
S2. Evaluate the sampler's ability to collect samples
under a variety of site conditions
S3. Assess the sampler's ability to collect an
undisturbed sample
S4. Evaluate the sampler's durability based on its
materials of construction and engineering design
S5. Document the availability of the sampler and spare
parts
12
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The objectives for the demonstration were developed
based on input from MMT Program members, general user
expectations of sediment sampler capabilities,
characteristics of the demonstration areas, the time
available to complete the demonstration, and sampler
capabilities that ARI intended to highlight.
4.2 Demonstration Design
In February 1999, a predemonstration sampling and
analysis investigation was conducted to assess existing
conditions and confirm available information on physical
and chemical characteristics in each demonstration area.
Based on information from the predemonstration
investigation as well as available historical data, a
demonstration design was developed to address the
demonstration objectives. Input regarding the
demonstration design was obtained from demonstration
site representatives and ARI. Table 4-1 summarizes the
demonstration design.
ARI operated the Russian Peat Borer in each
demonstration area. The EPA made observations and took
measurements to evaluate the Russian Peat Borer in
accordance with the demonstration objectives. In
addition, a reference sampler was selected for each
demonstration area either because the sampler had been
successfully used to collect sediment samples in the
particular demonstration area or because it is typically
used to collect sediment samples under the conditions
encountered in the particular area. The Vibrocorer was
used as the reference sampler in S1A1. The Hand Corer
was used as the reference sampler in S1A2, S2A1, and
S2A2. Similarly, the sampling platforms used were
selected based on their availability but not necessarily
based on sampler requirements. For example, in S1A1,
the EPA GLNPO's Mudpuppy was used because it was
available free of charge from EPA Region 5. During the
demonstration, each reference sampler was evaluated
under the same conditions and objectives as the Russian
Peat Borer. All the sampling activities conducted by ARI
for the Russian Peat Borer were also conducted by the
sampling technicians for the reference samplers (for
example, the EPA GLNPO operated the Vibrocorer).
During the use of each reference sampler, the EPA also
took the same measurements and made the same
observations as were performed for the Russian Peat
Borer. The reference sampler for Site 2 was not designed
to collect core samples from the 9- to 11-foot bss sampling
depth interval. Therefore, in this sampling depth interval,
the reference sampler was not used.
The approach used to address each primary objective for
the innovative and reference core samplers is discussed
below. Because of varying sampler features, the
characteristics of the demonstration areas, and the limited
time available for the field demonstration, not all primary
objectives were addressed in each demonstration area.
However, the Russian Peat Borer and a reference sampler
were evaluated under three or more primary objectives in
each demonstration area.
• To address primary objective PI, a volume of
sediment to be collected was specified for each
sampling depth interval. The volume specified was
based on analytical requirements for characterizing the
sample or on the design volume of the sampler for the
particular sampling depth interval. If after one attempt
the sampler had not retrieved the specified volume of
sediment, additional attempts were made to retrieve
the specified volume. The number of attempts
required and the volume of sediment collected in each
attempt at a given location within an area were noted.
• Primary objective P2 was addressed by verifying that
each sediment sampler was able to consistently sample
a specified depth interval. For each sampler, the depth
of sampler deployment, total sample length, and
sample length within the specified depth interval were
noted. Various site conditions, including sediment
depth, water depth, and sediment composition, were
considered in addressing P2 in each demonstration
area.
• Primary objective P3 was addressed by analyzing
samples collected in a homogenous sediment layer for
arsenic or PSD. P3 was addressed in the deeper
sampling depth interval in S1A2 and in both sampling
depth intervals in S2A1. These areas and intervals
were chosen for this purpose because, according to the
analytical results for predemonstration investigation
samples, these intervals exhibited relatively consistent
chemical or physical characteristics or both.
13
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Table 4-1. Innovative Sediment Sampler Demonstration Design
Demonstration
Area
S1A1
(river mouth)
S1A2
(freshwater
bay)
S2A1
(lake)
S2A2
(wetland)
Target Sampling
Depth Interval (bss)
0 to 4 inches
6 to 12 inches
4 to 6 feet
0 to 4 inches
12 to 32 inches
0 to 4 inches
10 to 30 inches
4 to 12 inches
9 to 1 1 feet
Primary Objective
P1 Volume
P2 Depth interval
P6 Sample collection time
P1 Volume
P2 Depth interval
P5 Decontamination
P6 Sample collection time
P7 Cost
P1 Volume
P2 Depth interval
P6 Sample collection time
P1 Volume
P2 Depth interval
P6 Sample collection time
P1 Volume
P2 Depth interval
P3 Consistent samples
from a homogenous
layer
P6 Sample collection time
P1 Volume
P2 Depth interval
P3 Consistent samples
from a homogenous
layer
P4 Clean layer below
contaminated layer
P5 Decontamination
P6 Sample collection time
P7 Cost
P1 Volume
P2 Depth interval
P3 Consistent samples
from a homogenous
layer
P4 Clean layer below
contaminated layer
P6 Sample collection time
P1 Volume
P2 Depth interval
P6 Sample collection time
P1 Volume
P2 Depth interval
P6 Sample collection time
Sampling Parameter
(Matrix)
Core length and
volume (sediment)
PCBs, volume, and
core length (sediment)
PCBs (final rinsate)
Core length and
volume (sediment)
Core length and
volume (sediment)
PSD, volume, and core
length (sediment)
Arsenic, PSD, volume,
and core length
(sediment)
Arsenic (final rinsate)
Arsenic, PSD, volume,
and core length
(sediment)
Core length and
volume (sediment)
Core length and
volume (sediment)
Volume Required
per Sample
Design volume3
250 ml
1 L
Design volume
Design volume
250 ml
250 ml
500ml
250 ml
Design volume
Design volume
Sampler
Russian Peat Borer
Vibrocorer
Russian Peat Borer
Vibrocorer
Russian Peat Borer
Vibrocorer
Russian Peat Borer
Hand Corer
Russian Peat Borer
Hand Corer
Russian Peat Borer
Hand Corer
Russian Peat Borer
Hand Corer
Russian Peat Borer
Hand Corer
Russian Peat Borer
Notes:
bss =
L
ml
PCB =
PSD =
Below sediment surface
Liter
Milliliter
Polychlorinated biphenyl
Particle size distribution
For a given depth interval, the design volume corresponds to 100 percent sample recovery.
14
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Primary objective P4 was addressed by evaluating
whether a sample could be collected from a layer of
sediment with relatively low contaminant
concentrations (a "clean" layer) beneath a
"contaminated" layer of sediment that had
significantly higher contaminant concentrations
without cross-contaminating the clean layer sample.
P4 was addressed in S2A1 because, according to the
results of the predemonstration investigation, a clean
layer of sediment was present beneath a relatively
contaminated layer of sediment. During the
demonstration, sediment samples were collected from
each layer and analyzed for arsenic. The analytical
data for these samples were used to determine whether
sediment from the contaminated layer had been
carried into the clean layer during sampler deployment
and retrieval.
Primary objective P5 was addressed by collecting
samples of equipment rinsate (water) during the final
stage of core sampler decontamination. P5 was
addressed in the deeper sampling depth interval in
S1A1 and in the shallower sampling depth interval in
S2A1 because sediment in these areas and intervals
contained the highest observed concentrations of
PCBs and arsenic, respectively, among the
demonstration areas. Decontamination of each
sampler demonstrated in a given area was performed
after all samples had been collected in that area.
Primary objective P6 was addressed by measuring the
time required for each activity associated with sample
collection, including sampler setup, sample collection,
sampler disassembly, and sampler decontamination.
P6 was addressed in all demonstration areas to satisfy
this objective under a variety of site conditions.
Primary objective P7 was addressed in S1A1 and
S1A2 by estimating the costs associated with sample
collection activities, including sampler, labor, IDW
disposal, and support equipment costs. The following
costs associated with collection of all the investigative
samples in each area where P7 was addressed were
accounted for:
1. The sampler cost was estimated based on price
lists for purchasing each sediment sampler;
disposable, plastic core liners (if applicable); and
support equipment. Leasing costs for the
samplers were not considered because the
samplers are unavailable for leasing.
2. The labor cost was estimated based on the number
of people required to operate each sediment
sampler and the time required to conduct sampling
activities (sampler setup, sample collection,
sampler disassembly, and sampler
decontamination).
3. The IDW disposal cost was estimated for
specified areas. A volume of sediment to be
collected was specified for each demonstration
area where P7 was addressed. For each such area,
any sediment collected by a sampler that was not
required for analytical purposes was considered to
be IDW. For example, the sediment collected
above and below the specified depth interval and
the portion of a sample exceeding the specified
volume within a given depth interval were
considered to be IDW.
4. The support equipment cost was estimated based
on the rental or purchase cost of any additional
equipment required for sample collection, such as
generators or winches needed at the time of the
demonstration.
Secondary objectives SI, S2, and S3 were addressed in all
the demonstration areas where a given sampler was
evaluated because no additional sampling was required to
address them. Secondary objectives S4 and S5 were not
area-dependent; they were addressed based on developer
information as well as observations of sampler
performance during the demonstration. The approach used
to address each secondary objective is discussed below.
• Secondary objective SI was addressed by observing
and noting the skills required to operate each sampler
during the demonstration, how easy the sampler was
to operate, and the sampler's approximate weight and
by discussing any necessary sampling technician
training with the developer.
• Secondary objective S2 was addressed by determining
each sampler's ability to collect sediment samples
given the variety of sampling platforms, water depths,
15
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sediment depths, sediment compositions, and flow
conditions encountered in the demonstration areas.
• Secondary obj ective S3 was addressed based on visual
observations made during sampling or after a sediment
sample had been extruded from a sampler.
• Secondary objective S4 was addressed by noting each
sampler's materials of construction. Sediment
sampler failures or repairs that were necessary during
use of the sampler were also noted.
• Secondary objective S5 was addressed by discussing
the availability of replacement samplers with the
developer and determining whether spare parts were
available in a retail store or only through the
developer. In addition, when replacement samplers or
spare parts were required during the demonstration,
their availability was noted.
4.3 Field Sampling and Measurement
Procedures
This section presents field sampling and measurement
procedures used during the Russian Peat Borer
demonstration. Specifically, this section summarizes
demonstration sampling locations; sample collection,
sample preparation, and measurement procedures; and
field QC procedures. Additional details about the sample
collection, sample preparation, and measurement
procedures are presented in the demonstration plan
(EPA 1999). The demonstration plan is available on
the Internet through the ORD web site (http://
www.epa.gov/ORD/SITE).
Sediment samples were collected at Site 1 for PCB
analysis, at Site 2 for arsenic analysis, and at both sites for
PSD analysis. The sampling locations in each
demonstration area are presented in Figures 4-1 and 4-2.
Table 4-2 lists the target sampling depth intervals,
numbers of investigative samples, and analytical
parameters for each demonstration area and provides the
rationale for their selection. In general, the rationale for
choosing the number of samples to be collected in each
area was based on the objectives to be addressed, the
analyses to be conducted to address one or more
objectives, the time required to collect samples, and the
cost of each analysis. When five samples were to be
collected in a sampling area, samples were collected in the
four corners and center of the area; when ten samples were
collected in a sampling area, the additional five samples
were collected at locations randomly distributed
throughout the area.
Many of the field measurements made to support the
primary objectives (see Section 4.2) were simple, standard
measurements and do not require additional explanation.
These measurements include the volume of IDW
generated, number of sampling technicians, number of
sampling attempts per location, volume of sediment
collected, time required for sample collection activities,
volume of fuel consumed to operate motorized sampling
or support equipment, core length, sampling area grid size,
and water velocity. However, several field measurements
were made to address demonstration-specific
requirements, and additional explanation of these
measurements is warranted to enhance understanding of
the sampler performance results presented in Chapters 6
and 7. These field measurements are summarized below
by objective.
• To address primary objective PI, the volume of
sediment sample from a given depth interval was
measured, and then any unrepresentative material was
removed from the sediment sample and collected as
IDW. Unrepresentative material included sticks,
shells, and stones. After removal of unrepresentative
material, if not enough sediment was left to meet
analytical sample volume requirements, the sampling
technician collected additional cores from the
sampling location.
• To address primary obj ective P2, the depth of sampler
deployment was measured by allowing the sampling
technician to lower the sampler to the surface of the
sediment. Once the sampling technician felt that he
had identified the sediment surface, a mark was made
on the sampler cable or extension rod using a fixed
reference point (the water surface, boat side, or boat
floor). Another mark was made higher on the cable or
extension rod indicating the depth corresponding to
the sampling technician's estimate of the depth to
which the sampler should be driven to collect a
sediment sample from the specified sampling depth
interval. The sampler was then lowered to this depth,
and a sample was collected. For measurement of the
total core length retrieved and the core length
retrieved in the sampling depth interval, no correction
16
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S1A1 (river mouth)
Target sampling depth intervals:
0 to 4 inches, 6 to 12 inches,
and 4 to 6 feet
below sediment surface
Approximate scale: 1 inch = 1,200 feet
ABODE
1
2
3
4
5
*v.
0
0
0
10 feet
0
0
I
I
Based on the demonstration design,
no samples from the 0- to 4-inch and
4- to 6-foot below sediment surface
depth intervals required laboratory analysis.
S1A2 (freshwater bay)
Target sampling depth intervals:
0 to 4 inches and 12 to 32 inches
below sediment surface
Approximate scale: 1 inch = 1,200 feet
• 10 feet •
Based on the demonstration design,
no samples from the 0- to 4-inch
below sediment surface depth interval
required laboratory analysis.
Legend
O Polychlorinated biphenyls
• Particle size distribution
="" Flow direction
Figure 4-1. Site 1 sampling locations.
17
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S2A1 (lake)
Target sampling depth intervals:
0 to 4 inches and 10 to 30 inches
below sediment surface
Approximate scale: 1 inch = 1,200 feet
ABODE
1
2
\
«
O
«
O
O
«
O
e
O
•
t
I
S2A2 (wetland)
Wetland area
Target sampling depth intervals:
4 to 12 inches and 9 to 11 feet
below sediment surface
Approximate scale: 1 inch = 20 feet
Sampling locations
are represented by
shaded areas.
Based on the
demonstration design,
no samples required
laboratory analysis.
Legend
O Arsenic only
® Both arsenic and
particle size distribution
•^— Flow direction
Figure 4-2. Site 2 sampling locations.
18
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Table 4-2. Rationale for Sampling Approach
Demonstration
Area
S1A1
(river mouth)
S1A2
(freshwater bay)
S2A1
(lake)
S2A2
(wetland)
Target Sampling
Depth Interval
(bss)
0 to 4 inches
6 to 12 inches
4 to 6 feet
0 to 4 inches
12 to 32 inches
0 to 4 inches
10 to 30 inches
4 to 12 inches
9 to 1 1 feet
Number of Investigative
Samples per Sampler3
(Analytical Parameter)
5 (NA)
5 (PCBs)
1 (PCBs)
5 (NA)
5 (NA)
5 (PSD)
10 (Arsenic)
5 (PSD)
1 (Arsenic)
10 (Arsenic)
5 (PSD)
5 (NA)
5 (NA)
Matrix
Sediment
Sediment
Equipment
rinsate
Sediment
Sediment
Sediment
Sediment
Equipment
rinsate
Sediment
Sediment
Sediment
Rationale
Analytical samples not collected because only primary
objectives P1 (volume), P2 (depth interval), and P6 (sample
collection time) were addressed
Verify that contamination was present
Determine whether a sampler could be adequately
decontaminated (primary objective P5)
Analytical samples not collected because only primary
objectives P1 (volume), P2 (depth interval), and P6 (sample
collection time) were addressed
Analytical samples not collected because only primary
objectives P1 (volume), P2 (depth interval), and P6 (sample
collection time) were addressed
Determine whether a sampler could collect consistent samples
from a homogenous layer of sediment (primary objective P3)
with consistent physical characteristics
Determine whether a sampler could collect consistent samples
from a homogenous layer of sediment (primary objective P3)
with consistent physical and chemical characteristics and
determine whether a sampler could collect sediment samples
from a clean layer of sediment located below a layer of
contaminated sediment (primary objective P4)
Determine whether a sampler could be adequately
decontaminated (primary objective P5)
Determine whether a sampler could collect consistent samples
from a homogenous layer of sediment (primary objective P3)
with consistent physical and chemical characteristics and
determine whether a sampler could collect sediment samples
from a clean layer of sediment located below a layer of
contaminated sediment (primary objective P4)
Analytical samples not collected because only primary
objectives P1 (volume), P2 (depth interval), and P6 (sample
collection time) were addressed
Notes:
bss
NA
PCB
PSD
Below sediment surface
Not applicable
Polychlorinated biphenyl
Particle size distribution
The number of investigative samples varied depending on the analytical parameters and the objectives addressed in each demonstration area.
Ten investigative samples were collected and analyzed for arsenic to address primary objectives P3 and P4. However, only five investigative
samples were collected and analyzed for PSD to address primary objective P3 because the variability associated with PSD is typically less than
that associated with arsenic concentrations.
was made for sample compression or expansion that
might have taken place during sample collection.
To address primary obj ectives P3 and P4, excess water
overlying the sediment samples was carefully
decanted before the samples were transferred to
stainless-steel bowls and homogenized. The decanting
step ensured that the sediment samples would have
adequate percent solids for analysis. Homogenization
involved stirring the material with a stainless-steel spoon
for 4 minutes or longer until the sediment attained uniform
color, texture, and residual
19
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water distribution. Sample containers were then filled
using a quartering technique in which the
homogenized sample present in the stainless-steel
bowl was divided into quadrants. Each sample
container was filled by using a spoon to alternately
transfer sediment from one quadrant and then from the
opposite quadrant until the sample container was
filled. Any unused sediment was collected as IDW.
To address primary objective P5, the nondisposable
components of each sampler were decontaminated by
scrubbing them with an Alconox solution, washing
them with potable water, and then rinsing them with
deionized water. At Site 1, 3 L of rinsate per sampler
was generated to meet analytical and QC volume
requirements for PCB analysis. At Site 2, 2 L of
rinsate per sampler was generated to meet analytical
and QC volume requirements for arsenic analysis. All
deionized water used to generate rinsate samples was
from one lot of water identified by a lot number. To
verify that any contamination detected by the
laboratory in the rinsate samples was not present in
the deionized water or the result of field sample
collection procedures at Sites 1 and 2, samples of this
water were sent to the laboratory for PCB and arsenic
analyses, respectively, along with the rinsate samples.
Deionized water samples were collected once at each
demonstration site during collection of sediment
samples.
To address primary objective P6, timing of sampler
setup began when a sampling technician began
assembling a given sampler and ended when the
sampler was completely assembled and any additional
equipment necessary for sampling using the sampler
had been collected and was ready to be transported to
the sampling location. If additional time was required
to set up the sampler at the sampling location, this
time was measured and included in the total setup
time.
Timing of sample collection began when the sampler
was ready to be deployed and ended when the sample
had been retrieved; extruded from the sampler; and
submitted for measurement, preparation, and
distribution into the appropriate containers for
analysis. If additional sampling attempts were
required to collect the specified sample volume, the
time required to complete these attempts was added to
the sample collection time. If any portion of the
sampler was disassembled to extrude a sample and
reassembled before the next sample was collected, the
time required for disassembly and reassembly was
included in the total sample collection time. Between
sampling attempts and locations, if a sampler had any
sediment adhering to it, the sampler was rinsed at the
sampling location using surface water. The time
required for rinsing was also added to the total sample
collection time. Sample collection time did not
include the time needed to position the sampling
platforms at specific sampling locations.
Timing of sampler disassembly began when all
samples had been collected or extruded and the
sampling technician began disassembly of the sampler.
The timing ended when the sampler had been
completely disassembled and was ready to be
decontaminated.
Timing of sampler decontamination began when the
nondisposable components of each sampler were
decontaminated by scrubbing them with an Alconox
solution. The timing continued until the sampling
technician considered the sampler to be
decontaminated to the degree that a sample of the final
rinsate could be collected to address primary objective
P5. Sampler decontamination occurred once in each
demonstration area after all samples were collected
and the sampler was disassembled.
QC checks for field measurements were used to evaluate
the quality of field activities. In general, the QC checks
were used to assess the representativeness of the samples
and to ensure that the degree to which the analytical data
were representative of actual site conditions was known
and documented. QC checks for field parameters
consisted of the time required for sample collection
activities and the water velocity. Field QC checks for
laboratory parameters consisted of temperature blanks (in
shipments that contained samples for PCB analysis) and
field replicates. Field replicates were collected to evaluate
whether a sample was adequately homogenized in the field
prior to filling of sample containers. Field replicate
samples included field duplicates (rinsate) for PCB and
arsenic analyses and field triplicates (sediment) for PCB,
arsenic, and PSD analyses. Table 4-3 identifies the
planned numbers of investigative samples and field
replicate samples. Field replicate samples were submitted
20
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Table 4-3. Sample Matrix
Demonstration
Area
S1A1
(river mouth)
S1A2
(freshwater
bay)
S2A1
(lake)
S2A2
(wetland)
Target Sampling
Depth Interval
(bss)
0 to 4 inches
6 to 12 inches
4 to 6 feet
0 to 4 inches
12 to 32 inches
0 to 4 inches
10 to 30 inches
4 to 12 inches
9 to 1 1 feet
Sampler
Russian Peat Borer
Vibrocorer
Russian Peat Borer
Vibrocorer
Russian Peat Borer
Vibrocorer
Russian Peat Borer
Hand Corer
Russian Peat Borer
Hand Corer
Russian Peat Borer
Hand Corer
Russian Peat Borer
Hand Corer
Russian Peat Borer
Hand Corer
Russian Peat Borer
Analytical
Parameter
NA
PCBs
NA
NA
PSD
Arsenic
PSD
Arsenic
PSD
NA
NA
Sediment Samples
Number Per Sampler
Investi-
gative
Samples
5
5
5
5
5
10
5
10
5
5
5
MS/MSD
Samples3
Field
Triplicate
Samples"
Laboratory
Analyses
Total
Number of
Analyses
Equipment Rinsate Samples
Number Per Sampler
Equipment
Rinsate
Samples
Field
Duplicate
Samples0
Laboratory
Analyses
Total
Number of
Analyses
Samples were not analyzed for PCBs, arsenic, or PSD. The rationale for the number of samples is
provided in Table 4-2.
1
2
11
22
1
1
2
4
Samples were not analyzed for PCBs, arsenic, or PSD. The rationale for the number of samples is
provided in Table 4-2.
Samples were not analyzed for PCBs, arsenic, or PSD. The rationale for the number of samples is
provided in Table 4-2.
NA
2
NA
2
NA
1
3
1
3
1
7
20
7
20
7
14
40
14
40
14
NA
1
NA
0
NA
NA
1
NA
0
NA
0
2
0
0
0
0
4
0
0
0
Samples were not analyzed for PCBs, arsenic, or PSD. The rationale for the number of samples is
provided in Table 4-2.
Samples were not analyzed for PCBs, arsenic, or PSD. The rationale for the number of samples is
provided in Table 4-2.
Notes:
bss
MS/MSD
Below sediment surface
Matrix spike/matrix spike duplicate
NA = Not applicable
PCB = Polychlorinated biphenyl
PSD = Particle size distribution
MS/MSD samples were collected for PCB and arsenic analyses and were designated in the field. MS/MSD samples were not collected for equipment rinsate samples because the additional
volume required for the analysis may have diluted any contamination present to concentrations below laboratory detection limits. Sediment MS/MSD samples did not require additional sample
volume.
Field triplicate sediment samples were collected by filling three sample containers with homogenized sediment. A sufficient volume of sediment for field triplicate samples was collected as
described in the approach for addressing primary objective P1 in Section 4.2. Field triplicate samples were submitted for analysis as blind samples.
Field duplicate equipment rinsate samples were collected by filling one additional container for PCB or arsenic analysis. Field duplicate samples were submitted for analysis as blind samples.
-------
for laboratory analysis as blind samples (that is, the
laboratories did not know which samples were replicates).
Acceptance criteria and associated corrective actions for
field QC checks are presented in the demonstration plan
(EPA 1999).
During the demonstration, the EPA conducted an internal
technical system audit (TSA) of field sampling and
measurement systems. The following activities were
audited during the field TSA: sample collection; sample
preparation; field measurements; field documentation;
decontamination; and sample labeling, packaging, and
shipping.
A summary discussion of whether the field QC procedures
generated data that met the demonstration objectives is
presented in Sections 6.3 and 7.3 for the innovative
and reference samplers, respectively. More detailed
information is provided in the DER (Tetra Tech EM Inc.
[TetraTech] 1999c).
4.4 Laboratory Sample Preparation and
Analysis Methods
In selecting appropriate methods for preparing and
analyzing the demonstration samples from Sites 1 and 2,
the specific analytes of interest, the laboratories'
experience in analyzing the predemonstration samples, and
the target reporting limits required to address the
demonstration objectives were taken into account.
Table 4-4 summarizes the laboratory sample preparation
and analysis methods used for the demonstration.
Laboratory QC checks were used to demonstrate the
absence of interferants and contamination from laboratory
glassware and reagents, to verify that the measurement
systems were in control, to evaluate the precision and
accuracy of laboratory analyses, and to ensure the
comparability of data. Laboratory-based QC checks other
than those associated with instrument calibration consisted
of method blanks, surrogates, MS/MSDs, extract and
digestate duplicates, blank spike/blank spike duplicates
(BS/BSD), interference check analyses, serial dilutions,
postdigestion spikes, repeat analyses, and performance
evaluation (PE) samples. Table 4-5 summarizes the
laboratory QC checks used for the demonstration and their
purpose. The frequencies, acceptance criteria, and
corrective actions for QC checks are presented in the
demonstration plan (EPA 1999).
Predemonstration and in-process TSAs of the laboratories
used for the demonstration were conducted. The
following activities were audited: sample receipt and
sample storage; internal chain of custody; sample
extraction, digestion, and cleanup; sample analysis;
standards preparation and storage; calibration; QC
procedures; and data reduction, validation, and reporting.
Predemonstration and in-process performance audits of
laboratory activities were also conducted for PCB and
arsenic analyses. During each audit, (1) two PE samples
(one low-level and one high-level) each for PCBs and
arsenic were obtained for the sediment matrix and (2) one
low-level PE sample each for PCBs and arsenic was
obtained for the aqueous matrix. The PE samples were
submitted to the laboratory as double-blind samples for
analysis.
A summary discussion of whether the laboratory QC
procedures generated data that met the demonstration
objectives is presented in Sections 6.3 and 7.3 for the
innovative and reference samplers, respectively. More
detailed information is provided in the DER (Tetra Tech
1999c).
22
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Table 4-4. Laboratory Sample Preparation and Analysis Methods
Parameter (Matrix)
Method Reference3
Method Title
PCBs (sediment)
PCBs (equipment rinsate)
Arsenic (sediment)
Arsenic (equipment rinsate)
PSD (sediment)
SW-846 Method 3550B (extraction)
SW-846 Method 3665A" (cleanup)
SW-846 Method 36606° (cleanup)
SW-846 Method 8082 (analysis)
SW-846 Method 351OC (extraction)
SW-846 Method 3665Ab (cleanup)
SW-846 Method 8082 (analysis)
SW-846 Method 3050B (digestion)
SW-846 Method 601 OB (analysis)
SW-846 Method 301OA (extraction)
SW-846 Method 601 OB (analysis)
ASTM Method D 422-63
(Reapproved in 1990)
Ultrasonic Extraction
Sulfuric Acid/Permanganate Cleanup
Sulfur Cleanup
PCBs by Gas Chromatography
Separatory Funnel Liquid Extraction
Sulfuric Acid/Permanganate Cleanup
PCBs by Gas Chromatography
Acid Digestion of Sediment, Sludges, and Soils
Inductively Coupled Plasma-Atomic Emission Spectrometry
Acid Digestion of Aqueous Samples and Extracts for Total Metals
for Analysis by FLAA or ICP Spectroscopy
Inductively Coupled Plasma-Atomic Emission Spectrometry
Standard Method for Particle-Size Analysis of Soils (with
hydrometer option)
Notes:
ASTM
EPA
FLAA
ICP
PCB
PSD
American Society for Testing and Materials
U.S. Environmental Protection Agency
Flame atomic absorption
Inductively coupled argon plasma
Polychlorinated biphenyl
Particle size distribution
SW-846 reference: EPA 1996; ASTM reference: ASTM 1998
SW-846 Method 3665A is used whenever elevated baselines or overly complex chromatograms prevent accurate quantitation of Aroclors. The
laboratory routinely performed sulfuric acid cleanup on PCB sample extracts using SW-846 Method 3665A.
The laboratory detected elevated levels of sulfur in predemonstration investigation samples analyzed for PCBs. Therefore, the laboratory
monitored PCB chromatograms for the presence of sulfur and cleaned up the extracts using SW-846 Method 3660B when sulfur was detected.
23
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Table 4-5. Laboratory Quality Control Checks
Quality Control Check
Parameter
Matrix
Purpose
Method blanks
Surrogates
MS/MSDsa
Extract duplicates
Digestate duplicates
BS/BSDs
Interference check
analyses
Serial dilutions
Postdigestion spikes
Repeat analyses
PE samples
PCBs and arsenic Sediment and rinsate
PCBs
Sediment and rinsate
PCBs and arsenic Sediment
PCBs
Arsenic
Sediment and rinsate
Sediment and rinsate
PCBs and arsenic Sediment and rinsate
Verify that steps in the analytical procedures did not introduce
contaminants that affected analytical results
Determine whether significant matrix effects existed within the
samples and measure the efficiency of recovery of analytes in
sample preparation and analysis
Determine the accuracy and precision of the analytical results with
respect to the effects of the sample matrix
Determine the precision associated with laboratory analytical
procedures following sample extraction
Determine the precision associated with laboratory analytical
procedures following sample digestion
Determine whether observed deviations for MS/MSDs and for
extract and digestate duplicate samples were caused by a matrix
effect
Arsenic
Arsenic
Arsenic
PSD
PCBs and arsenic
Sediment and rinsate Evaluate the validity of the interelement correction factors
Sediment and rinsate
Sediment and rinsate
Sediment
Sediment and water
Determine whether significant physical or chemical interferences
existed as a result of the sample matrix
Determine whether a matrix effect should be expected
Evaluate the precision of hydrometer readings
Determine the accuracy associated with the laboratory analytical
procedures for low-level and high-level concentrations
Notes:
BS/BSD =
MS/MSD =
PCB
PE
PSD
Blank spike/blank spike duplicate
Matrix spike/matrix spike duplicate
Polychlorinated biphenyl
Performance evaluation
Particle size distribution
MS/MSD samples were not collected for equipment rinsate samples because the additional volume required for the analysis may have diluted
any contamination present to concentrations below laboratory detection limits. In addition, MS/MSDs are not typically collected for rinsate
samples.
24
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Chapter 5
Description of the Reference Sediment Samplers
This chapter describes two conventional sediment
samplers that were used as reference samplers during the
demonstration. Each reference sampler was chosen based
on its proven ability to meet the various demonstration
objectives presented in Section 4.1. Specifically, two core
samplers were selected as reference samplers: the Hand
Corer and the Vibrocorer.
The Hand Corer is a commonly used core sampler
designed to obtain sediment samples in a variety of lake
and river environments. The sampler can collect
continuous sediment cores to a depth of about 36 inches
bss. Based on the predemonstration investigation results,
demonstration objectives, and site support facilities
available, the Hand Corer was selected as the reference
sampler for S1A2, S2A1, and S2A2.
The Vibrocorer is a core sampler designed to obtain
sediment samples in a variety of shallow and deep river,
lake, and ocean environments. The sampler has been
successfully used by the EPA at several contaminated sites
in Region 5. Based on the predemonstration investigation
results, demonstration objectives, and site support
facilities available, the Vibrocorer was selected as the
reference sampler for S1A1.
Sections 5.1 and 5.2 provide descriptions, discuss general
operating procedures, and outline advantages and
limitations of the Hand Corer and Vibrocorer used in the
demonstration.
5.1 Hand Corer
The Hand Corer selected as a reference sampler for the
demonstration is designed to collect undisturbed,
cylindrical core samples from various types of sediment,
including saturated sands and silts, to a depth of about
36 inches bss in stagnant or swiftly moving water.
5.1.1 Technology Description
Components of the Hand Corer include (1) a Lexan™ nose
piece; (2) a 36-inch-long, stainless-steel core tube; (3) a
stainless-steel head piece with a flutter valve; (4) two
detachable, stainless-steel handles; and (5) a clevis (see
Figure 5-1). For deployment in deep water, the Hand
Corer can be equipped with a guide rope or extension rods
and a turning handle. The Hand Corer can also be
equipped with disposable, clear plastic core tube liners
that fit inside the core tube (these liners are not shown in
Figure 5-1).
Support equipment for sampler deployment may include
a tripod-mounted winch for (1) controlling the rate of
sampler deployment and retrieval; (2) minimizing the
physical stress on the sampling technician, particularly
during sampler retrieval and during intense or extended
sampling events; and (3) preventing the sampler from
sinking too deeply into the sediment to obtain a
representative sample.
The stainless-steel core tube has a 2-inch outside diameter
and is designed to collect about 50 mL of sediment per
inch of core tube length; the maximum design volume of
the core tube is about 1,800 mL. The fully equipped Hand
Corer, including the nose piece, core tube, head piece with
flutter valve, handles, and clevis, weighs about 12 Ib.
Each 5-foot-long extension rod and a turning handle weigh
about 5 and 2 Ib, respectively.
In water less than 20 feet deep, the Hand Corer may be
manually deployed and driven into the sediment using the
25
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Flutter valve
Clevis
Detachable
handles
• Head piece
, Core tube
Nose piece
Figure 5-1. Hand Corer.
handles and the necessary length of extension rods. In
water more than 20 feet deep, the sampler may be
deployed using a guide rope attached to the clevis and a
weight attached to the core tube. During sampler retrieval,
a sediment core is retained in the core tube by a partial
vacuum created by the closed flutter valve.
5.1.2 General Operating Procedures
The Hand Corer can be operated in shallow water by one
person from a platform, from a boat, or while wading. For
sampling in deep water, two sampling technicians are
recommended to control the weight of the sampler and
extension rods and to conduct efficient sampling. During
sampler assembly, a plastic core tube liner may be inserted
into the core tube. Core tube liners hold and store the
sample for later examination. Depending on the water
depth and flow conditions, either the handles and the
necessary number of extension rods or the guide rope can
be used to deploy the Hand Corer to the sediment surface.
The speed of sampler deployment to the sediment surface
should be controlled to avoid bow wave formation, which
could disturb flocculent or unconsolidated sediment that
might be near the sediment surface (Blomqvist 1991).
The sampler may be driven into the sediment by manual
force on the handles or by gravity penetration. In general,
the sampler should be driven into the sediment in a steady
and uninterrupted manner. The sampler is manually
retrieved by pulling upward on the handles, extension
rods, or guide rope, as appropriate. When samples are
being collected in shallow water depths, the flutter valve
should be manually closed once the Hand Corer reaches
the desired sediment depth. When the sampler is being
retrieved from deep water depths, the upward motion of
the submerged sampler causes the flutter valve to
automatically close. The tapered nose piece and partial
vacuum created by the flutter valve retain the sediment
core in the plastic core tube liner. When the weight of the
sampler and extension rods requires it, a tripod-mounted
winch should be used to control the rate of sampler
retrieval. The sampler should be kept vertical and the rate
of retrieval should be kept as steady as possible to
minimize resuspension and disruption of the sediment.
After sampler retrieval, the nose piece or head piece is
removed to allow removal of the plastic core tube liner.
The sediment core enclosed in the core tube liner may be
either sealed in the core tube using two core caps or
extruded for further examination and processing. The
sediment core may be removed by pushing the sample out
one end of the core tube liner with an extrusion rod. Prior
to sampling, some sampling technicians cut the core tube
liner twice longitudinally and tape the liner together with
vinyl electrical tape before inserting the liner into the core
tube. In this case, after a sample is collected, the tape
holding the two halves of the core tube liner is cut,
splitting the liner in half and exposing the sediment core.
26
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5.1.3 Advantages and Limitations
An advantage of the Hand Corer is that it is easy to
operate, requiring minimal skills and training. Sampler
assembly and sample collection procedures can be learned
in the field with a few practice attempts. In addition, a
written SOP typically accompanies the sampler when it is
procured. The sampler can be operated by one person in
shallow (wading) water depths because of its light weight
(12 Ib). Sampler operation is especially simple when a
core tube liner is used because the sampler does not
require complete disassembly to extrude the sample and
reassembly after each sampling attempt. Only the nose
piece or head piece requires detachment to remove the
plastic core tube liner containing the sediment core. Use
of the disposable liner also minimizes the risk of cross-
contamination between sampling locations.
Another advantage of the Hand Corer is the flutter valve
in the head piece. The flutter valve is designed to allow
water to exit the top of the core tube during sampler
deployment, thus minimizing potential bow wave
formation near the sediment surface. During sampler
retrieval, the sediment core is retained in the core tube by
a partial vacuum created by the closed flutter valve.
Collectively, these design features increase the likelihood
of collecting an undisturbed sample.
A limitation of the Hand Corer is that during sampler
deployment, the plastic core tube liner is exposed to
different layers of sediment contamination. Contaminants
may adhere to the exposed surface of the liner while the
sampler passes through different layers of sediment. Also,
the flutter valve may become clogged if the sampler is
deployed in such a way that the flutter valve is driven
into the sediment. Specifically, sediment and nonsedimen-
taceous materials (leaves, plant roots, or small stones) may
become trapped between the flutter valve and core tube,
resulting in partial or complete loss of vacuum and
eventually partial or complete loss of the sediment sample.
Another limitation of the Hand Corer is that it cannot
collect discrete samples from various sediment depths.
Core samples must be collected from the sediment surface
downward. Because end-filling samplers such as the Hand
Corer must collect samples from the sediment surface
downward, the Hand Corer is subject to core shortening.
Core shortening occurs when the length of sediment core
collected is less than the depth of sampler penetration into
the sediment. Core shortening may occur when the
friction of the sediment against the inside wall of the core
tube increases with increasing depth of sediment
penetration, causing lateral displacement of sediment and
resulting in gradually thinner increments of sediment
entering the sampler. Because not all layers are uniformly
sampled, core shortening can introduce sampling bias.
Furthermore, use of a tripod-mounted winch limits the
sampling platform locations from which the sampler can
be deployed. Specifically, the sampling platform must be
equipped with a hole over which the tripod-mounted
winch can be placed and through which the sampler can be
deployed.
5.2 Vibrocorer
The Vibrocorer is designed to collect sediment cores in
deep river, lake, and ocean environments. The sampler is
designed to operate in shallow and deep water conditions
and to provide complete and continuous sediment profile
collection to a maximum depth of 4,000 feet beneath the
water surface. According to the EPA GLNPO, the sampler
is designed to collect sediment cores to a depth of 15 feet
bss in packed sand and to a depth of 20 feet bss in silt and
clay; however, sediment cores have been successfully
collected to a depth of 35 feet bss using the Vibrocorer.
5.2.1 Technology Description
Components of the Vibrocorer include (1) an anodized-
aluminum, pressure-housed vibrohead with a terminal for
an electric cable; (2) a disposable, 10-foot-long, 4-inch-
diameter, clear plastic core tube; (3) a core tube clamp;
and (4) a guide rope (see Figure 5-2). The sampler is also
equipped with a check valve in the vibrohead and a core
nose at the bottom end of the core tube (the check valve
and core nose are not shown in Figure 5-2). Core tube
sectioning and extraction are performed using a hand-held
electric or battery-powered saw. The Vibrocorer requires
a three-phase, 230- or 440-volt, 50- to 60-hertz electric
current. The sampler must be supplied with power from a
power source through an electric cable and a control box.
The Vibrocorer must be operated from a boat, dock, or
platform with enough working space to accommodate an
A-frame of adequate size.
27
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Guide rope
Vibrohead
Electric cable
Core tube clamp
Core tube
Figure 5-2. Vibrocorer.
The typical weight of a fully equipped Vibrocorer,
including the vibrohead and core tube, is about 150 Ib.
Core tubes are available in lengths up to 15 feet with a
4-inch diameter and up to 20 feet with a 3-inch diameter.
If a 15-foot-long core sample is required, the core tube
must be 16 feet long because 6 inches is lost when the core
tube is inserted into the vibrohead and 6 inches is lost
when the core nose is attached.
The Vibrocorer is deployed to the sediment surface using
the A-frame and winch. Once the sampler is deployed to
the sediment surface and supplied with power, the
vibrohead vibrates at a frequency of up to 3,450 vibrations
per minute, depending on the power supply. The vibrating
motion of the vibrohead drives the core tube vertically
downward into the sediment. The sampler is retrieved
mechanically using the A-frame and winch. During
sampler retrieval, the check valve in the vibrohead creates
a vacuum that, along with the core nose, retains sediment
in the core tube.
5.2.2 General Operating Procedures
The Vibrocorer must be operated by at least two persons
from a boat, dock, or platform. To prepare for sampler
deployment, the vibrohead is raised using the A-frame and
winch, and the core tube is secured to the vibrohead at the
core tube clamp. Again using the A-frame and winch, the
sampler is deployed to the desired sampling position; the
vibrohead should then be supplied with power and allowed
to vibrate. The speed of sampler deployment to the
sediment surface should be controlled to avoid bow wave
formation, which could disturb flocculent or
unconsolidated sediment that might be near the sediment
surface (Blomqvist 1991).
As the vibrohead vibrates, the core tube is gradually forced
downward into the sediment. Once the core tube is
deployed to the desired sediment depth, the power can be
turned off and the vibrohead can be allowed to stop
vibrating. Now the sampler can be mechanically removed
from the sediment using the A-frame and winch. During
sampler retrieval, the check valve in the vibrohead creates
a vacuum that, along with the core nose, retains sediment
in the core tube. Once the core tube is retrieved from the
water, water remaining in the top of the core tube should
be drained by drilling holes in the core tube at the
sediment-water interface with an electric or battery-
powered drill. To extract the core tube from the core tube
clamp, four nuts that secure the core tube in place must be
removed. Afterward, the core tube is placed on the
sampling platform to extract the sediment. To extract the
28
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core sample, horizontal sections of the core tube should be
cut using an electric or battery-powered saw.
5.2.3 Advantages and Limitations
Advantages of the Vibrocorer include its ability to collect
sediment samples up to 4,000 feet beneath the water
surface. In addition, the vibrohead component of the
sampler allows core tube penetration into the sediment
without manual labor. Sampler deployment and retrieval
are controlled with an A-frame and winch. Furthermore,
use of new core tubes for each sampling attempt
minimizes the risk of cross-contamination between
sampling locations.
A limitation of the Vibrocorer is that during sampler
deployment, the disposable core tube is exposed to
different layers of sediment contamination. Contaminants
may adhere to the exposed surface of the core tube while
the sampler passes through different layers of sediment.
In addition, the sampler cannot collect discrete samples
from various sediment depths; core samples must be
collected from the sediment surface downward. As a
result, samples collected with the Vibrocorer are subject
to core shortening as described in Section 5.1.3.
Another limitation of the Vibrocorer is that it must be
operated by at least two persons from a boat, dock, or
platform. If the sampler is being operated from a boat and
the boat drifts away from the deployed Vibrocorer, the
tension on the winch cable could pull the Vibrocorer over
and damage it, or the electric cable could snap and cause
an electrical short circuit. Also, if the boat drifts while the
Vibrocorer is deployed, extracting the core tube from the
sediment would be difficult because the winch cable from
the sampler to the boat would not be vertical; as a result,
the core tube could be bent and the sediment sample could
be lost.
29
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Chapter 6
Performance of the Russian Peat Borer
To verify a wide range of performance attributes, the
innovative sediment sampler demonstration had both
primary and secondary objectives. Primary objectives
were critical to the technology evaluation and were
intended to produce quantitative results regarding
technology performance. Secondary objectives provided
information that was useful but did not necessarily
produce quantitative results regarding technology
performance. The approach used to address each primary
and secondary objective for the Russian Peat Borer and
reference samplers is discussed in Chapter 4. This chapter
describes the performance of the Russian Peat Borer based
on the primary obj ectives (excluding costs associated with
sample collection activities) and secondary objectives.
This chapter also discusses the data quality of
demonstration results for the Russian Peat Borer.
The performance of the reference samplers is discussed in
Chapter 7, costs associated with sample collection
activities (primary objective P7) are presented in
Chapter 8, and the performance of the Russian Peat Borer
and reference samplers is compared in summary form in
Chapter 9.
6.1 Primary Objectives
This section discusses the performance results for the
Russian Peat Borer based on the primary objectives stated
in Section 4.1 except for primary objective P7 (sampling
costs), which is addressed in Chapter 8. Primary
objectives PI through P6 required evaluation of the
Russian Peat Borer's
P1. Ability to consistently collect a specified volume of
sediment
P2. Ability to consistently collect sediment in a
specified depth interval
P3. Ability to collect multiple samples with consistent
physical or chemical characteristics, or both, from a
homogenous layer of sediment
P4. Ability to collect a representative sample from a
clean sediment layer below a contaminated sediment
layer
P5. Ability to be adequately decontaminated
P6. Time requirements for sample collection activities
To address primary objectives PI through P6, samples
were collected from four different areas: (1) S1A1, a river
mouth; (2) S1A2, a small, freshwater bay; (3) S2A1, a
lake; and (4) S2A2, a wetland. A sampling technician
designated by ARI used the Russian Peat Borer to collect
samples from the following target depth intervals: 0 to
4 inches bss, 6 to 12 inches bss, and 4 to 6 feet bss in
S1A1; 0 to 4 and 12 to 32 inches bss in S1A2; 0 to 4 and
10 to 30 inches bss in S2A1; and 4 to 12 inches bss in
S2A2. This sampler was also used to conduct sampling in
the 9- to 11-foot bss target depth interval at three of the
five S2A2 locations; the ARI sampling technician did not
attempt to collect samples in this interval at the other two
S2A2 sampling locations because of the significant effort
required to collect samples at the first three locations. In
some cases, multiple depth intervals were simultaneously
sampled in a given attempt if the sampler was long enough
to reach these intervals. The demonstration areas and
target depth intervals are described in greater detail in
Chapters 3 and 4. The numbers of investigative and QC
30
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samples collected in each demonstration area, sediment
sample volumes required, and sample analytical
parameters are discussed in Chapter 4.
During the demonstration, ARI used three different
Russian Peat Borer models to collect sediment samples:
Models A, B, and C. Model A has a 20-inch-long core
tube with a 2-inch inside diameter, Model B has a 40-inch-
long core tube with a 2-inch inside diameter, and Model C
has a 25-inch-long core tube with a 3-inch inside diameter.
ARI chose which model to use based on site and area
conditions and sampling requirements identified in the
demonstration plan (EPA 1999). The sampling technician
was also provided an opportunity to practice sample
collection at each demonstration area until he felt
confident enough to initiate demonstration sampling. The
three Russian Peat Borer models are described in
Chapter 2.
The demonstration results for the Russian Peat Borer
under primary objectives PI, P2, and P4 were evaluated
using the Wilk-Shapiro test to determine whether the
results were normally distributed. Because most of the
results were not normally distributed, the Wilk-Shapiro
test was used in an attempt to evaluate whether the results
followed a lognormal distribution. The test revealed that
the results either were not lognormally distributed or could
not be tested for lognormality because they contained
values that were equal to zero. For these reasons, a
parametric test such as the paired Student's t-test was not
used to perform hypothesis testing. The Wilcoxon signed
rank test, a nonparametric test for paired samples that
makes no assumptions regarding distribution, was used as
an alternative to the Student's t-test. Although the
Wilcoxon signed rank test has been historically accepted
as a nonparametric test, it is not as powerful as the
Student's t-test because the Wilcoxon signed rank test
does not account for the magnitude of difference between
sample pair results. Despite this limitation, the Wilcoxon
signed rank test was more appropriate than the Student's
t-test for evaluating the demonstration results. A computer
program known as Statistix® for Windows, Version 2.0
(Statistix®), developed by Analytical Software of
Tallahassee, Florida, was used to perform statistical
evaluations of the demonstration results (Analytical
Software 1996). Appendix C provides details on the
statistical methods used for data evaluation.
6.1.1 Ability to Consistently Collect a Specified
Volume of Sediment
Primary obj ective P1 involved evaluating the Russian Peat
Borer's ability to consistently collect a specified volume
of sediment. This objective was addressed by comparing
(1) the actual number of sampling attempts required to
collect a specified volume of sediment to the expected
number of attempts (rounded to the nearest higher integer)
at each sampling location in each target depth interval and
(2) the actual volume of sediment collected in the
specified target depth interval in each attempt to the
calculated sampler volume (design volume) for the depth
interval. The expected number of attempts was
determined by dividing the specified sample volume by the
design volume for the depth interval. The results of these
comparisons are summarized below.
6.1.1.1 Number of Sampling Attempts Required
Tables 6-1 and 6-2 present the expected and actual number
of sampling attempts for each depth interval at Sites 1 and
2, respectively. Initially, the Wilcoxon signed rank test
was used to determine whether the difference between the
expected and actual number of attempts was statistically
significant. However, the conclusions drawn from the
Wilcoxon signed rank test were inconsistent with the
conclusions reached in comparing the expected and actual
number of attempts. The discrepancy is primarily due to
the test's inability to account for the magnitude of the
difference between data pairs (see Appendix C for an
example).
Based on the number of sampling attempts required in
S1A1, the Russian Peat Borer performed well in the 0- to
4- and 6- to 12-inch bss depth intervals but had difficulty
meeting expectations in the 4- to 6-foot bss depth interval.
In the 0- to 4-inch bss depth interval, only one additional
attempt was required at two of the five locations. The
additional attempts may have been required because the
sampler had difficulty collecting unconsolidated surficial
sediment, which has a greater tendency to wash out
because of its high water content. In the 6- to 12-inch bss
depth interval, the expected number of attempts equaled
the actual number of attempts at all locations. However,
in the 4- to 6-foot bss depth interval, as previously
mentioned, 12 attempts were required to collect the
specified volume of sediment, whereas only 5 were
expected. The additional attempts were required because
31
-------
Table 6-1. Comparison of Expected and Actual Number of Sampling Attempts for Russian Peat Borer at Site 1
Number of Attempts in S1A1 (River Mouth)
Location
1A
1E
3C
5A
5E
Total
0- to 4-Inch
Expected
1
1
1
1
1
5
bss Depth Interval
Actual
2
1
1
2
1
7
6- to 12-Inch
Expected
1
5
2
3
2
13
bss Depth Interval
Actual
1
5
2
3
2
13
4- to 6-foot
Expected
1
1
1
1
1
5
bss Depth Interval
Actual
3
1
2
4
2
12
Number of Attempts in S1A2 (Freshwater Bay)
0- to 4-Inch bss Depth Interval
Location
1A
1E
3C
5A
5E
Total
Expected
1
1
1
1
1
5
Actual
2
1
2
1
2
8
Expected
1
1
1
1
2
6
Actual
1
1
1
1
2
6
12- to 32-Inch bss Depth Interval
Note:
bss = Below sediment surface
the sampler had difficulty fully penetrating the target depth
interval, which contained clay hardpan.
The Russian Peat Borer's performance in S1A2 was
similar to that in S1A1. For example, one additional
attempt was required in the 0- to 4-inch bss depth interval
at three of the five sampling locations in S1A2. The
additional attempts may have been required because the
sampler had difficulty collecting unconsolidated surficial
sediment. However, in the 12- to 32-inch bss depth
interval, which contained more consolidated sediment,
additional attempts were not required at any of the
locations sampled.
In S2A1, which was the first area sampled during the
demonstration, the actual number of attempts in the 0- to
4-inch bss depth interval equaled the expected number of
attempts at four of the ten locations sampled. At two of
the remaining six locations, the actual number of attempts
exceeded the expected number by more than one. Because
these locations were the first two locations sampled, the
sampling technician may have required more practice to
efficiently collect sediment samples in this demonstration
area. In the 10- to 30-inch bss depth interval, five of the
ten locations sampled required one additional attempt
beyond the expected number of attempts; the other five
locations required no additional attempts. Explanation of
the additional attempts required in this depth interval was
beyond the scope of the demonstration.
In S2A2, in the 4- to 12-inch bss depth interval, the
Russian Peat Borer's performance was similar to that in
the 0- to 4-inch bss depth intervals in S1A1 and S1A2; one
additional attempt was required in this depth interval at
three of the five sampling locations in S2A2. The
additional attempts may have been required because the
top several inches of material in this area contained
partially decomposed reeds and leaves that prevented
complete closure of the sampler, which resulted in
sediment washout in a few cases. In the 9- to 11-foot bss
depth interval, the actual number of attempts equaled the
expected number of attempts at the three locations
sampled. However, samples were not collected from this
interval at the two remaining locations because of the
32
-------
Table 6-2. Comparison of Expected and Actual Number of Sampling Attempts for Russian Peat Borer at Site 2
Number of Attempts in S2A1 (Lake)
Location
1A
1B
1E
2A
2C
2D
2E
3A
3B
3E
Total
0- to 4-Inch bss
Expected
4
2
6
5
3
5
5
3
2
4
39
Depth Interval
Actual
4
2
10
5
4
6
8
4
2
5
50
10- to 30-Inch bss Depth
Expected
1
1
2
2
1
2
2
1
1
1
14
Interval
Actual
2
1
2
2
2
2
3
2
1
2
19
Number of Attempts in S2A2 (Wetland)
4- to 12-Inch bss Depth Interval
Location
1A
1E
3C
5A
5E
Total
Expected
1
1
1
1
1
5
Actual
2
2
1
2
1
8
Expected
1
Not attempted
Not attempted
1
1
3
Actual
1
1
1
3
9- to 11 -foot bss Depth Interval
Note:
bss = Below sediment surface
significant effort required to (1) hammer the sampler into
and retrieve the sampler from the 9- to 11-foot bss depth
interval and (2) rotate the core tube 180 degrees clockwise
to cut through the consolidated sediment.
Based on the number of sampling attempts required in all
four demonstration areas and multiple sampling depth
intervals, the Russian Peat Borer demonstrated the ability
to consistently collect a specified volume of sediment.
Overall, the sampler required 33 percent more attempts
than expected (126 actual attempts versus 95 expected
attempts). The Russian Peat Borer performed better than
the reference samplers in the moderate and deep sampling
depth intervals; however, in the shallow interval, the
performance of the reference samplers was better than that
of the Russian Peat Borer (see Section 7.1.1.1).
6.1.1.2 Volume of Sediment Collected
The volume of sediment collected by the Russian Peat
Borer in each sampling attempt in a given depth interval
was divided by the corresponding design volume, and the
resulting ratio was multiplied by 100 to estimate the
percent sample recovery (PSR). The relative standard
deviation (RSD) of the PSRs was calculated to evaluate
the ability of the sampler to consistently collect a specified
volume of sediment; if the sampler were to recover an
identical volume of sediment in every attempt, the RSD
would equal zero. To properly evaluate the sampler's
performance, both PSR and RSD results should be
considered because a low RSD, which indicates that the
sampler's performance was consistent, may be based on
consistently low PSRs. Figures 6-1 and 6-2 present PSRs
for the Russian Peat Borer at Sites 1 and 2, respectively.
33
-------
S1A1 (river mouth)
0- to 4-inch bss depth interval
Oto20 >20to40 >40to60 >60to80 >80to100
Percent sample recovery
>100
S1A2 (freshwater bay)
0- to 4-inch bss depth interval
0 01
crto
c c
B£
0.0.
II2
CO w
•bo
tr
Total number of attempts: 8
Oto20 >20to40 >40to60 >60 to 80 >80to100
Percent sample recovery
S1A1 (river mouth)
6-to 12-inch bss depth interval
Total number of attempts: 13
Oto20 >20to40 >40to60 >60to80 >80to100
Percent sample recovery
>100
S1A2 (freshwater bay)
12-to 32-inch bss depth interval
Total number of attempts:
Oto20 >20to40 >40to60 >60to80 >80to100
Percent sample recovery
>100
S1A1 (river mouth)
4- to 6-foot bss depth interval
Oto20 >20to40 >40to60 >60 to 80 >80to100 >100
Percent sample recovery
Notes:
bss = Below sediment surface
Percent sample recoveries exceeding 100 resulted from the volumetric measurement error associated with the presence of void spaces when the
sediment was transferred to a graduated container.
Figure 6-1. Percent sample recoveries for Russian Peat Borer at Site 1.
34
-------
S2A1, 0- to 4-irft?l'H&*20to40 >40to60 >60to80 >80to100
Percent sample recovery
>100
S2A2, 4- to12-Bfl*B tosSaaWljth interval
4-to 12-inch bss depth interval
Oto20 >20to40 >40to60 >60to80 >80to100
Percent sample recovery
S2A1,10-to 30-inWlM^epth interval
10- to 30-inch bss depth interval
S2A2, 9-to 1l32ftft(b8!iaae'fc>th interval
9- to 11-foot bss depth interval
Total number of attempts: 3
Oto20 >20to40 >40to60 >60to80 >80to100 >100
Percent sample recovery
Oto20 >20to40 >40to60 >60to80 >80to100 >100
Percent sample recovery
Notes:
bss = Below sediment surface
Percent sample recoveries exceeding 100 resulted from the volumetric measurement error associated with the presence of void spaces when the
sediment was transferred to a graduated container.
Figure 6-2. Percent sample recoveries for Russian Peat Borer at Site 2.
Table 6-3 presents PSR summary statistics (range, mean,
and RSD) for the Russian Peat Borer at both sites.
In S1A1, the Russian Peat Borer performed well in terms
of PSR in the 0- to 4- and 6- to 12-inch bss depth intervals
but had difficulty meeting expectations in the 4- to 6-foot
bss depth interval. In the 0- to 4-inch bss depth interval,
the sampler retrieved sediment in every attempt;
difficulties in collecting unconsolidated surficial sediment
may account for the minimum PSR of 44 for this depth
interval. Because the sediment was more consolidated in
the 6- to 12-inch bss depth interval, improved sample
recoveries were observed, as is reflected by the minimum
PSR of 67. The RSDs forthe 0-to 4-and 6-to 12-inch bss
depth intervals are about the same and are less than
30 percent. Although no RSD criterion has been set for
determining the ability to consistently sample a specified
volume of sediment, an RSD of 30 percent or less is
considered to be acceptable. The RSDs show that the
Russian Peat Borer was able to consistently sample the 0-
to 4- and 6- to 12-inch bss depth intervals.
In the 4- to 6-foot bss depth interval, several additional
attempts were required to collect the specified volume of
sediment because (1) in one attempt, the core tube was not
fully rotated to the closed position and (2) in the remaining
35
-------
Table 6-3. Percent Sample Recovery Summary Statistics for Russian Peat Borer
Demonstration Area
Target Depth Interval (bss) Actual Number of Attempts
PSR Range3
Mean PSR
RSD (%)
S1A1 (river mouth) 0 to 4 inches
6 to 12 inches
4 to 6 feet
S1 A2 (freshwater bay) 0 to 4 inches
12 to 32 inches
S2A1 (lake) 0 to 4 inches
10 to 30 inches
S2A2 (wetland) 4 to 12 inches
9 to 1 1 feet
Notes:
bss = Below sediment surface
PSR = Percent sample recovery
RSD = Relative standard deviation
7
13
12
8
6
50
19
8
3
44 to 100
67 to 133
Oto 100
50 to 100
90 to 100
Oto 110
Oto 110
50 to 100
100 to 133
84
101
45
75
95
71
76
75
122
26
25
71
36
6
42
30
31
16
PSRs exceeding 100 resulted from the volumetric measurement error associated with the presence of void spaces when the sediment was
transferred to a graduated container.
attempts, the sampler had difficulties penetrating the entire
target depth interval, which contained clay hardpan. As a
result, in 9 of the 12 attempts in this interval, less than or
equal to 60 percent of the specified volume was retrieved;
in 3 of the 9 attempts, no sediment was retrieved.
Consequently, a high RSD (71 percent) was observed for
the 4- to 6-foot bss depth interval, indicating that the
Russian Peat Borer did not demonstrate the ability to
consistently collect a specified volume of sediment in this
interval.
In the S1A2 0- to 4-inch bss depth interval, the Russian
Peat Borer had slightly more difficulty in collecting
unconsolidated sediment than it did in the same interval in
S1A1. However, the sampler performed well in the 12-to
32-inch bss depth interval in S1A2, which contained
consolidated sediment. Table 6-3 shows that the mean
PSR for the 0- to 4-inch bss depth interval in S1A2 is less
than that for the 0- to 4-inch bss depth interval in S1A1.
The lower PSR values for the 0- to 4-inch bss depth
interval in S1A2 can be attributed to difficulty in
collecting unconsolidated surficial sediment, as is
reflected in the four attempts with PSRs in the greater than
40 to 60 range shown in Figure 6-1. The variability in the
PSRs for the 0- to 4-inch bss depth interval is reflected in
the RSD of 36 percent, which slightly exceeds the
30 percent RSD guideline discussed above. On the other
hand, the Russian Peat Borer achieved a mean PSR of 95
and a PSR range of 90 to 100 for samples collected in the
12- to 32-inch bss depth interval, as shown in Table 6-3.
The sampler's consistency of performance in this depth
interval was reflected in an RSD of 6 percent and may
have been achieved because the sediment in this interval
was highly cohesive.
Wide PSR ranges (0 to 110) were observed in the 0- to 4-
and 10- to 30-inch bss depth intervals in S2A1. As shown
in Table 6-3, the mean PSR of 71 and the minimum PSR
of 0 for the 0- to 4-inch bss depth interval in S2A1 were
low compared to those for the other 0- to 4-inch bss depth
intervals. Figure 6-2 shows the variability in PSR values
observed for the 0- to 4-inch bss depth interval in S2A1,
where 26 of the 50 attempts had PSRs greater than 80, but
14 attempts had PSRs in the greater than 40 to 60 range.
The high variability in the PSR results for the 0- to 4-inch
bss depth interval is further reflected by the high RSD
value of 42 percent. Although a similar mean PSR (76)
and minimum PSR (0) were observed for the 10- to
30-inch bss depth interval in S2A1, much less variability
was present in the PSR data. As shown in Figure 6-2, only
6 of the 19 attempts had PSRs outside the greater than 60
to 80 range. Because most recoveries fell into a narrow
range (greater than 60 to 80 range), an RSD value of
30 percent was observed, which met the 30 percent RSD
guideline. In both the 0- to 4- and 10- to 30-inch bss depth
intervals in S2A1, at least some sediment was collected in
most attempts; no sediment was collected in only 3 of 50
36
-------
and 1 of 19 attempts in the 0- to 4- and 10- to 30-inch bss
depth intervals, respectively.
In S2A2, the Russian Peat Borer experienced some
difficulty in the 4- to 12-inch bss depth interval but
performed well in the 9- to 11-foot bss depth interval. In
the 4- to 12-inch bss depth interval, a mean PSR of 75 and
a PSR range of 50 to 100 were observed, as shown in
Table 6-3. As shown in Figure 6-2, only three of eight
attempts in this interval had PSRs greater than 80, with
washout accounting for the low recoveries. However, an
RSD of 31 percent was calculated for the PSRs for the 4-
to 12-inch bss depth interval, which compares favorably to
the 30 percent RSD guideline. In the 9- to 11-foot bss
depth interval, a mean PSR of 122 and a PSR range of 100
to 133 were observed because PSRs for two attempts were
in excess of 100. The Russian Peat Borer performed well
at the 9- to 11-foot bss depth interval because the
cohesiveness of the peat at this depth eliminated the
possibility of washout. The RSD for the 9- to 11-foot bss
depth interval was only 16 percent.
Based on the volumes of sediment collected in all four
demonstration areas and multiple sampling depth intervals,
the Russian Peat Borer demonstrated the ability to
consistently collect a specified volume of sediment. An
RSD less than or equal to 30 percent was observed for five
of nine sampling depth intervals. Three of the remaining
depth intervals had an RSD in the greater than 30 to
50 percent range. Only one depth interval had an RSD
that exceeded 50 percent. The sampler had mixed results
in the 0- to 4-inch bss depth intervals, for which RSDs of
26, 36, and 42 percent were observed in S1A1, S1A2, and
S2A1, respectively. The sampler performed better at
moderate depth intervals, for which RSDs of 25,6, 30, and
31 percent were observed in S1A1, S1A2, S2A1, and
S2A2, respectively. Mixed results were also observed in
the deepest sampling intervals. For sample collection from
the cohesive peat of the 9- to 11-foot bss depth interval in
S2A2, an RSD of 16 percent was observed. In contrast,
the sampler's difficulty in penetrating the clay hardpan in
the 4- to 6-foot depth interval in S1A1 resulted in an RSD
of 71 percent. Overall, the Russian Peat Borer performed
better than the reference samplers in the moderate and
deep sampling depth intervals; however, in the shallow
interval, the performance of the reference samplers was
better than the Russian Peat Borer (see Section 7.1.1.2).
6.1.2 Ability to Consistently Collect Sediment in
a Specified Depth Interval
Primary objective P2 involved evaluating the Russian Peat
Borer's ability to consistently collect sediment in a
specified depth interval. This objective was addressed by
comparing actual and target core lengths for each sampling
attempt. The target core length for an attempt was equal
to the distance between the upper and lower boundaries of
a depth interval except in the case of samples collected
from the 4- to 6-foot bss depth interval in S1A1 and the 9-
to 11-foot bss depth interval in S2A2, where the target
core length was set at 20 inches to correspond to the
Russian Peat Borer Model A's core tube length. The
actual core lengths were generally 2 to 6 inches greater
than the estimated depth of sampler deployment for the
shallow and moderate depth intervals, indicating that the
sampling technician may have had minor difficulty in
assessing the location of the sediment surface. Because
the Russian Peat Borer is a side-filling sampler that, based
on visual observations, collects a relatively uncompressed
sediment sample, the error in assessing the location of the
sediment surface should have minimal effect on the core
length data. Also, the actual core length measurements
presented in this section do not account for void space in
the core, rounding error, or sediment washout.
Consequently, an attempt may have achieved an actual
core length that equaled the target core length but may not
have resulted in a PSR of 100.
Table 6-4 presents the number of attempts in which the
actual core length equaled the target core length, target
core lengths, and mean actual core lengths. Initially, the
Wilcoxon signed rank test was to be used to determine
whether differences between the actual and target core
lengths were statistically significant. However, review of
the Wilcoxon signed rank test results revealed that the test
results for many of the data sets were inconsistent with the
conclusions reached in comparing the actual and expected
core lengths for the reasons described in Section 6.1.
Therefore, primary objective P2 was addressed by
evaluating (1) the number of attempts in which the actual
core length equaled the target core length and (2) the
difference between the target core length and the mean
actual core length.
In S1A1, the sample core lengths equaled the target core
lengths for all samples collected from the 0- to 4- and 6- to
12-inch bss depth intervals. However, only 1 of 12
37
-------
Table 6-4. Comparison of Target and Actual Core Length Data for Russian Peat Borer
Demonstration Area
S1A1 (river mouth)
S1A2 (freshwater bay)
S2A1 (lake)
S2A2 (wetland)
Target Depth Interval
(bss)
0 to 4 inches
6 to 12 inches
4 to 6 feet
0 to 4 inches
12 to 32 inches
0 to 4 inches
10 to 30 inches
4 to 12 inches
9 to 1 1 feet
Number of Attempts in Which Actual
Core Length Equaled Target
Core Length/Total Attempts
7/7
13/13
1/12
8/8
6/6
49/50
16/19
8/8
3/3
Target Core Length
(inches)
4
6
20
4
20
4
20
8
20
Mean Actual Core Length
(inches)
4
6
10
4
20
18
8
20
Note:
bss = Below sediment surface
a The calculated mean actual core length (3.9 inches) was rounded to the nearest integer.
sample core lengths in the 4- to 6-foot bss depth interval
equaled the target core length. This circumstance resulted
in a mean actual core length of 10 inches, which is only
one-half the target core length of 20 inches. Because of
difficulties in penetrating the clay hardpan in the 4- to
6-foot bss depth interval, 11 of the 12 attempts obtained a
core length of less than 20 inches; in 3 of the 12 attempts,
no sediment was retrieved. The reference sampler also
had difficulty penetrating the clay hardpan to the extent
that it was unable to collect samples from this interval at
S1A1.
In S1A2, the Russian Peat Borer successfully collected the
target core lengths in all attempts in both the 0- to 4- and
12- to 32-inch bss depth intervals.
The Russian Peat Borer also performed well in S2A1,
where the core lengths of 49 of 50 and 16 of 19 samples
equaled the target core lengths in the 0- to 4- and 10- to
30-inch bss depth intervals, respectively. In the 0- to
4-inch bss depth interval, one attempt where no sediment
was collected was the only failure to obtain the target core
length. Despite this attempt, the mean actual core length
was about 4 inches (3.9 inches). In the 10- to 30-inch bss
depth interval, there was also one attempt in which no
sediment was collected. This failed attempt accounts for
most of the mean actual core length's deviation from the
target core length. The mean actual core length was
18 inches, which still compares favorably to the target core
length of 20 inches.
In S2A2, the Russian Peat Borer successfully collected the
target core lengths in all attempts in both the 4- to 12-inch
and 9- to 11-foot bss depth intervals. As discussed in
Section 7.1, the reference sampler was not used for the 9-
to 11-foot bss depth interval because it is not designed to
collect samples below 3 feet bss.
In summary, the data indicate that the Russian Peat Borer
was able to consistently collect sediment from the shallow
(0- to 4-inch bss) and moderate (6- to 12-inch bssinSlAl,
12- to 32-inch bss in S1A2, 10- to 30-inch bss in S2A1,
and 4- to 12-inch bss in S2A2) depth intervals. In the 0- to
4-inch bss depth interval, only 1 of 65 actual core lengths
did not match the target core length. In the moderate
depth intervals, only 3 of 46 actual core lengths did not
match the target core length. The Russian Peat Borer
performed as well as or better than the reference samplers
(see Section 7.1.2).
A general conclusion could not be drawn regarding the
Russian Peat Borer's ability to consistently collect
sediment from the deep (4- to 6-foot bss in S1A1 and 9- to
11-foot bss in S2A2) depth intervals. In S1A1, only 1 of
12 actual core lengths in the 4- to 6-foot bss depth interval
equaled the target core length, but in S2A2, all 3 actual
core lengths in the 9- to 11-foot bss depth interval equaled
the target core length. As discussed in Section 7.1, the 4-
to 6- and 9- to 11-foot bss depth intervals could not be
sampled using the reference sampler.
38
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6.1.3 Ability to Collect Multiple Samples with
Consistent Physical or Chemical
Characteristics, or Both, from a
Homogenous Layer of Sediment
Primary objective P3 involved evaluating the Russian Peat
Borer's ability to collect multiple samples with consistent
physical or chemical characteristics, or both, from a
homogenous layer of sediment. This objective was
addressed by calculating the RSD values for the sample
analytical results for the 12-to 32-inch bss depth interval
in S1A2 and the 0- to 4- and 10- to 30-inch bss depth
intervals in S2A1. Based on the predemonstration
investigation results, these three depth intervals were
determined to be homogenous in terms of their physical
characteristics, and the two S2A1 depth intervals were
determined to be homogenous in terms of their physical
and chemical characteristics.
Figure 6-3 presents the demonstration analytical results for
PSD in the 12- to 32-inch bss depth interval in S1A2.
Figure 6-4 presents the demonstration analytical results for
arsenic and PSD in the 0- to 4- and 10- to 30-inch bss
depth intervals in S2A1. The demonstration analytical
results for arsenic contain statistical outliers that indicate
that the two S2A1 depth intervals may not be chemically
homogenous. For this evaluation, the outliers are defined
as sample analytical results that are not within two
standard deviations of the mean; the outliers include the
12 milligrams per kilogram (mg/kg) of arsenic in the 0- to
4-inch bss depth interval and the 29 mg/kg of arsenic in
the 10- to 30-inch bss depth interval in S2A1. Outliers
were also found in the arsenic analytical results for
samples collected by the reference sampler (see
Section 7.1.3), providing further evidence that the two
S2A1 depth intervals may not be chemically homogenous.
A similar analysis performed for the PSD data revealed no
statistical outliers. Therefore, the Russian Peat Borer was
evaluated based only on its ability to collect multiple
samples with consistent physical characteristics. RSDs
were calculated for each depth interval based on the PSD
results for all locations sampled.
RSDs calculated for the PSD data were compared to the
laboratory acceptance criterion of 15 percent for field
triplicates (which was based on historical information)
because RSDs less than or equal to 15 percent for all
samples collected in a given depth interval and area may
be more attributable to the laboratory's precision than the
sampler's ability to collect multiple samples with
consistent physical characteristics. When the RSD for all
samples from a given depth interval was greater than
15 percent, it was compared to the measured RSD for the
field triplicates, which were prepared by first
homogenizing and then subsampling the sediment
collected in a given depth interval, location, and area. An
RSD for all samples that is less than the RSD for field
triplicates may be more attributable to the laboratory's
analytical procedure or the sample homogenization
procedure implemented in the field, or both, rather than
the sampler's ability to collect physically consistent
samples. However, PSD parameters with means less than
10 percent were not evaluated in this manner because at
low levels, the analytical method is not as precise; as a
result, it will generate high RSD values and may not
actually reveal whether multiple samples with consistent
physical characteristics were collected. Table 6-5 presents
PSD summary statistics (range, mean, and RSD)
calculated for the samples and field triplicates collected in
each depth interval relevant to primary objective P3.
For the 12- to 32-inch bss depth interval in S1A2, the
mean sand level was less than 10 percent and was not
evaluated using the laboratory acceptance criterion of
15 percent RSD. Although the mean sand level was less
than 10 percent, all investigative samples contained some
sand level as indicated by 0 percent RSD. The RSDs for
sand and silt results were below the 15 percent laboratory
acceptance criterion. However, the 18 percent RSD for
clay results for this depth interval was 3 percentage points
above the laboratory acceptance criterion and
15 percentage points above the measured RSD for field
triplicates. Therefore, some of the variation in the clay
results may be attributable to the Russian Peat Borer's
ability to collect samples with consistent physical
characteristics. The variation, however, was not
considered significant because it was only 3 percentage
points greater than the laboratory acceptance criterion.
For both of the S2A1 depth intervals, the RSDs for sand
and silt results were below the 15 percent laboratory
acceptance criterion. The mean clay levels were less than
10 percent and were not evaluated using this criterion.
However, the clay levels exhibited tight ranges (2 to
8 percent in the 0- to 4-inch bss depth interval and 2 to
9 percent in the 10- to 30-inch bss depth interval).
39
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12- to 32 -inch bss de
Location 1A
Sand: 1%
Silt: 74%
Clay: 25%
Location 5A
Sand: 1%
Silt: 73%
Clay: 26%
3th interval
Location 3C
Sand: 1%
Silt: 79%
Clay: 20%
Location 1 E
Sand: 1%
Silt: 82%
Clay: 17%
Location 5E
Sand: 1%
Silt: 79%
Clay: 20%
Note:
bss = Below sediment surface
Figure 6-3. Russian Peat Borer sample particle size distribution results for S1A2 (freshwater bay).
In summary, the Russian Peat Borer met primary objective
P3 criteria except for (1) a 3 percentage point exceedance
in the RSD for clay results for S1A2 and (2) exceedances
up to 44 percentage points in the RSDs for clay results for
S2A1. The S2A1 exceedance may be due to a low mean
clay content at which the analytical method's precision is
generally low. Therefore, it was concluded that the
Russian Peat Borer was able to collect multiple samples
with consistent physical characteristics. Similar
performance results were observed for the reference
sampler (see Section 7.1.3).
6.1.4 Ability to Collect a Representative Sample
from a Clean Sediment Layer Below a
Contaminated Sediment Layer
To evaluate whether the Russian Peat Borer could collect
representative samples from a clean sediment layer that
was below a contaminated layer (primary objective P4),
samples were collected from both clean and contaminated
layers using the Russian Peat Borer and the Hand Corer
(reference sampler). Because the predemonstration
40
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0- to 4-inch bss depth interval
Location 1A
Arsenic: 220 mg/kg
Sand: 31%
Silt: 66%
Clay: 2%
Location 2A
Arsenic: 230 mg/kg
Location 3A
Arsenic: 300 mg/kg
Sand: 30%
Silt: 63%
Clay: 3%
Location 1 B
Arsenic: 21 0 mg/kg
Location 3B
Arsenic: 250 mg/kg
Location 2C
Arsenic: 12 mg/kg
Sand: 29%
Silt: 60%
Clay: 8%
Location 2D
Arsenic: 240 mg/kg
Location 1 E
Arsenic: 180 mg/kg
Sand: 26%
Silt: 48%
Clay: 7%
Location 2E
Arsenic: 190 mg/kg
Location 3E
Arsenic: 190 mg/kg
Sand: 35%
Silt: 55%
Clay: 3%
10- to 30-inch bss der
Location 1A
Arsenic: 12 mg/kg
Sand: 37%
Silt: 58%
Clay: 5%
Location 2A
Arsenic: 10 mg/kg
Location 3A
Arsenic: 11 mg/kg
Sand: 34%
Silt: 62%
Clay: 4%
5th interval
Location 1 B
Arsenic: 9 mg/kg
Location 3B
Arsenic: 9.9 mg/kg
Location 2C
Arsenic: 18 mg/kg
Sand: 34%
Silt: 57%
Clay: 9%
Location 2D
Arsenic: 10 mg/kg
Location 1 E
Arsenic: 29 mg/kg
Sand: 37%
Silt: 57%
Clay: 4%
Location 2E
Arsenic: 14 mg/kg
Location 3E
Arsenic: 11 mg/kg
Sand: 37%
Si It: 61%
Clay: 2%
Notes:
bss = Below sediment surface
mg/kg = Milligram per kilogram
The particle size distribution results for a given sample may not total 100 percent because of rounding or because some sediment did not pass through
a U.S. Standard No. 4 sieve and was classified as gravel rather than sand, silt, or clay.
Figure 6-4. Russian Peat Borer sample arsenic and particle size distribution results for S2A1 (lake).
41
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Table 6-5. Particle Size Distribution Summary Statistics for Russian Peat Borer
Demonstration Area
S1A2 (freshwater bay)
S2A1 (lake)
Target Depth Interval
(inches bss)
12 to 32
Oto4
10 to 30
Number of
Samples
5
5
5
5
5
5
5
5
5
Parameter
Sand
Silt
Clay
Sand
Silt
Clay
Sand
Silt
Clay
Range (%)
1
73 to 82
17 to 26
26 to 35
48 to 66
2 to 8
34 to 37
57 to 62
2 to 9
Mean (%)
1
77
22
30
58
5
36
59
5
RSD (%)
(All Samples)
0
5
18
11
12
59
5
4
55
RSD (%)
(Field Triplicates)
0
1
3
19
9
33
12
8
83
Notes:
bss = Below sediment surface
RSD = Relative standard deviation
investigation results indicated that the 10- to 30-inch bss
depth interval in S2A1 contained arsenic concentrations
that were an order of magnitude less than those in the 0- to
4-inch bss depth interval in S2A1, the 10- to 30- and 0- to
4-inch bss depth intervals were considered to be clean and
contaminated layers, respectively. Difficulties were
encountered in assessing the location of the sediment
surface in this demonstration area because a black,
gelatinous material was present near the sediment surface.
In addition, the location of the sediment surface varied
significantly at several of the grid locations. This
variation may have been caused by previous sampling
attempts made during the demonstration.
Samples collected from both sediment layers were
analyzed for arsenic. The contaminated layer
concentrations were used only to document that a
contaminated layer existed above the clean layer. The
clean layer concentrations were used to compare the
Russian Peat Borer's performance with that of the Hand
Corer. To make this comparison, the null hypothesis was
that the mean difference between the Russian Peat Borer
and Hand Corer sample arsenic concentrations for the
clean layer equaled zero. The alternative hypothesis was
that the mean difference between the Russian Peat Borer
and Hand Corer sample arsenic concentrations for the
clean layer was not equal to zero. A two-tailed Wilcoxon
signed rank test was used to compare the Russian Peat
Borer and Hand Corer sample concentrations.
Figure 6-5 presents the arsenic concentrations in the
samples collected by the Russian Peat Borer and the Hand
Corer in both depth intervals in S2A1. Figure 6-5 also
presents the difference between the arsenic concentrations
in the samples collected by the samplers in the 10- to
30-inch bss depth interval at each sampling location by
subtracting the arsenic concentration in the Hand Corer
sample from that in the Russian Peat Borer sample. Each
negative difference indicates that the sample collected by
the Russian Peat Borer was less impacted by the
contaminated layer than the sample collected by the Hand
Corer; each positive difference indicates that the reverse
was true.
The sample analytical results showed that the 0- to 4-inch
bss depth interval contained arsenic at levels an order of
magnitude greater than the 10- to 30-inch bss depth
interval, although a few anomalies were noted. Two of
these anomalies are the (1) 12 mg/kg of arsenic in the
Russian Peat Borer sample collected from the 0- to 4-inch
bss depth interval and (2) 52 mg/kg of arsenic in the Hand
Corer sample collected from the 10- to 30-inch bss depth
interval. Explanation of these anomalies was beyond the
scope of the demonstration.
A statistical comparison of the Russian Peat Borer and
Hand Corer sample arsenic concentrations for the clean
layer using the Wilcoxon signed rank test showed that
there was a 61 percent probability that the concentrations
were not different. This conclusion seems reasonable
based on the average difference between the Russian Peat
Borer and Hand Corer sample concentrations, which was
about -2.0 mg/kg. This average was skewed by the
anomalous paired observation at location 3E (11 and
42
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0- to 4-inch bss depth interval
Location 1A
RPB: 220 mg/kg
HOC: 250 mg/kg
Location 2A
RPB: 230 mg/kg
HOC: 190 mg/kg
Location 3A
RPB: 300 mg/kg
HOC: 140 mg/kg
Location 1 B
RPB: 210 mg/kg
HOC: 130 mg/kg
Location 3B
RPB: 250 mg/kg
HOC: 140 mg/kg
Location 2C
RPB: 12 mg/kg
HOC: 120 mg/kg
Location 2D
RPB: 240 mg/kg
HOC: 130 mg/kg
Location 1 E
RPB: 180 mg/kg
HOC: 190 mg/kg
Location 2E
RPB: 190 mg/kg
HOC: 150 mg/kg
Location 3E
RPB: 190 mg/kg
HOC: 130 mg/kg
10- to 30-inch bss depth interval
Notes:
bss
Diff
HOC
mg/kg
RPB
Location 1A
RPB: 12 mg/kg
HOC: 24 mg/kg
Diff: -1 2 mg/kg
Location 2A
RPB: 10 mg/kg
HOC: 8.3 mg/kg
Diff: 1 .7 mg/kg
Location 3A
RPB: 11 mg/kg
HOC: 7.2 mg/kg
Diff: 3.8 mg/kg
Location 1 B
RPB: 9 mg/kg
HOC: 8.5 mg/kg
Diff: 0.5 mg/kg
Location 3B
RPB: 9.9 mg/kg
HOC: 8.2 mg/kg
Diff: 1 .7 mg/kg
Location 2C
RPB: 18 mg/kg
HOC: 9.7 mg/kg
Diff: 8.3 mg/kg
Location 2D
RPB: 10 mg/kg
HOC: 13 mg/kg
Diff: -3 mg/kg
Location 1 E
RPB: 29 mg/kg
HOC: 16 mg/kg
Diff: 1 3 mg/kg
Location 2E
RPB: 14 mg/kg
HOC: 7.2 mg/kg
Diff: 6.8 mg/kg
Location 3E
RPB: 11 mg/kg
HOC: 52 mg/kg
Diff: -41 mg/kg
Below sediment surface
Difference between arsenic concentrations in Russian Peat Borer and Hand Corer samples
Hand Corer
Milligram per kilogram
Russian Peat Borer
Figure 6-5. Comparison of Russian Peat Borer and reference sampler sample arsenic concentration results for S2A1 (lake).
43
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52 mg/kg of arsenic in the Russian Peat Borer and Hand
Corer samples, respectively). If the paired observation at
location 3E is not considered, the average difference in
concentrations is about 2.3 mg/kg, which is still
comparable to zero because the reporting limit for arsenic
was 1.0 mg/kg.
In summary, the Russian Peat Borer collected samples
from the clean layer that were at least as representative as
those collected by the Hand Corer.
6.1.5 Ability to be Adequately Decontaminated
Primary objective P5 involved evaluating the Russian Peat
Borer's ability to be adequately decontaminated (see
Section 4.3). This objective was addressed by collecting
equipment rinsate samples after sampler decontamination
activities in S1A1 and S2A1. Specifically, the 6- to
12-inch bss depth interval in S1A1 and the 0- to 4-inch bss
depth interval in S2A1 were chosen as the depth intervals
where P5 was evaluated because they contained high
concentrations of PCBs and arsenic, respectively.
Although it was intended that the evaluation of P5 be
limited to these depth intervals, this was not possible
because ARI simultaneously collected samples in multiple
depth intervals. However, this deviation did not impact
the primary objective. If the sampler were adequately
decontaminated, the analytical results for the equipment
rinsate samples would be below the analytical laboratory's
reporting limits. To ensure that the water used to
decontaminate the sampler was not contaminated,
decontamination water blanks were also analyzed.
Contaminant concentrations in both the equipment rinsate
samples and decontamination water blanks were below the
laboratory reporting limits for PCBs (1 part per billion)
and arsenic (10 parts per billion). Thus, the Russian Peat
Borer demonstrated the ability to be adequately
decontaminated.
6.1.6 Time Requirements for Sample Collection
Activities
Primary objective P6 involved evaluating the Russian Peat
Borer's time requirements for sample collection activities.
These requirements were evaluated in all four
demonstration areas but were not specifically evaluated by
depth interval because samples were simultaneously
collected in multiple depth intervals to reduce the total
sample collection time. One technician was required for
sampler setup, sample collection, sampler disassembly,
and sampler decontamination in each area. The amounts
of time measured to complete these activities are shown in
Table 6-6. The time measured for sample collection
activities did not include the time taken for mobilization,
demobilization, and maneuvering the sampling platforms
to access sampling locations because these activities were
not specific to the sampler; they were either site- or
weather-related.
A comparison of sampler setup time results showed that
the setup time ranged from 1 to 30 minutes. In S1A1,
samples were collected using Russian Peat Borer
Models A and C. Similarly, S2A1 samples were collected
using Models B and C, but a longer setup time was
required in S2A1, perhaps because S2A1 was the first area
sampled during the demonstration and because three more
extension rods were used in S2A1 than in S1A1. Only one
Russian Peat Borer model was used in S1A2 (Model B)
and S2A2 (Model A). However, more time was required
in S2A2 because three extension rods were required to
reach the 9- to 11-foot bss depth interval, whereas only
one extension rod was required in S1A2. Use of the
additional extension rods in S2A2 contributed to the
additional 8 minutes of setup time.
Table 6-6. Time Required to Complete Sampling Activities for Russian Peat Borer
Time Required (minutes)
Activity
Sampler etup
Sample Collection
Sampler Disassembly
Sampler Decontamination
Total
S1A1 (River Mouth)
13
52
10
13
88
S1A2 (Freshwater Bay)
1
8
3
Not evaluated
12
S2A1 (Lake)
30
80
9
30
149
S2A2 (Wetland)
9
120
9
Not evaluated
138
44
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Sample collection times ranged from 8 to 120 minutes.
Sample collection time was a function of how many
attempts were required in each depth interval and of
demonstration area characteristics such as water depth and
target sampling depth intervals. Sampling attempts in
depth intervals other than the 4- to 6-foot bss depth
interval in S1A1 and the 9- to 11 -foot bss depth interval in
S2A2 required 1 minute or less except in S2A1. Again,
additional time was necessary for sample collection in
S2A1 because it was the first area sampled and because
the water depth was 18 feet. Sample collection times in
S2A1 ranged from 1 to 4 minutes per attempt. Sample
collection times in the 4- to 6-foot bss depth interval in
S1A1 and the 9- to 11-foot bss depth interval in S2A2
ranged from 2 to 4 and 30 to 51 minutes per attempt,
respectively. The additional time required to sample these
intervals can be attributed to their greater depths.
The sampler disassembly time was fairly consistent.
About 10 minutes was required for sampler disassembly in
all areas except S1A2, where 3 minutes was required. The
time required to disassemble one sampler model in S2A2
was comparable to the time required to disassemble two
sampler models in S1A1 and S2A1 because of the
numerous extension rods required to sample the 9- to
11-foot bss depth interval in S2A2. Less time was
expended in sampler disassembly in S1A2 than in the
other areas because only one sampler model and one
extension rod were required in S1A2.
The amount of time spent on Russian Peat Borer
decontamination was evaluated only in S1A1 and S2A1.
In both areas, the amounts of time required for sampler
setup and sampler decontamination were identical
(13 minutes in S1A1 and 30 minutes in S2A1). Although
two sampler models were used in both areas, more
decontamination time was necessary in S2A1 because it
was the first area where the sampling technician
implemented the decontamination procedure and because
more extension rods had to be decontaminated. Four
extension rods were required in S1A1, and six were
required in S2A1.
Based on the demonstration results, a sampling technician
with some previous experience with the Russian Peat
Borer would need 5 to 10 minutes per sampler model for
each of the following activities: (1) sampler setup,
(2) sampler disassembly, and (3) sampler
decontamination. The actual amount of time required for
these activities would depend on the sampling technician's
familiarity with the Russian Peat Borer and on the number
of extension rods needed to collect samples.
Approximately 1 to 2 minutes per sampling attempt could
be expected for sample collection. However, sample
collection time increases as the degree of sediment
compaction, the water depth, and the depth of the interval
to be sampled increase. When sediment sampling is
planned, the time required for setting up the sampling
platform and for maneuvering the platform to position the
sampler at the sampling location would have to be
considered in addition to the times presented above.
6.2 Secondary Objectives
This section discusses the performance results for the
Russian Peat Borer based on the secondary objectives
stated in Section 4.1. Secondary objectives S1 through S5
required evaluation of the Russian Peat Borer's
SI. Skill and training requirements for proper sampler
operation
S2. Ability to collect samples under a variety of site
conditions
S3. Ability to collect an undisturbed sample
S4. Durability based on materials of construction and
engineering design
S5. Availability, including spare part availability
Secondary objectives were addressed based on
(1) observations of the Russian Peat Borer's performance
during the demonstration and (2) information provided by
ARI and by a developer of material used in the
construction of the Russian Peat Borer.
6.2.1 Skill and Training Requirements for
Proper Sampler Operation
The Russian Peat Borer is easy to operate, requiring
minimal skills and training. Although ARI currently does
not have a training video or written SOP for the sampler,
sampler assembly and sample collection procedures can be
learned in the field with a few practice attempts. The
sampler can be operated by one person because of its
lightness (see Table 2-1). Sampler operation is simple
45
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because it has only one moving part (the core tube rotates
180 degrees). Moreover, the sampler does not require
disassembly to extrude the samples and reassembly after
each sampling attempt. The sampler requires no support
equipment other than two sawhorses for supporting the
sampler during sample extrusion, a slide-hammer
mechanism, and a safe sampling platform.
During the demonstration, minimal strength and stamina
were required to collect samples from shallow and
moderate depth intervals containing both unconsolidated
and consolidated sediments. Specifically, minimal
strength and stamina were required to drive the sampler
into and retrieve it from the 0- to 4-inch bss depth intervals
in S1A1, S1A2, and S2A1 and the moderate depth
intervals ranging from 4 to 12 (S2A2), 6 to 12 (S1A1), 10
to 30 (S2A1), and 12 to 32 (S1A2) inches bss. However,
moderate to significant strength and stamina were required
to collect samples from deep sampling intervals containing
highly consolidated sediment. Specifically, moderate to
significant strength and stamina were required to drive the
sampler into and retrieve it from the 4- to 6-foot bss depth
interval in S1A1 and the 9- to 11-foot bss depth interval in
S2A2 using the 10-lb ARI slide-hammer mechanism.
Moderate to significant strength was also required to rotate
the core tube 180 degrees clockwise in order to cut
through the consolidated sediment in these depth intervals.
Sediment in the 4- to 6-foot bss depth interval was
predominantly clay with low water content, and sediment
in the 9- to 11-foot bss depth interval was predominantly
silty loam with peat and low water content. These
consolidated intervals required an increased amount of
torque to rotate the core tube.
Previous sediment sampling experience would be
beneficial in selecting the most appropriate Russian Peat
Borer model for a given application. Model A (with its
2-inch-inside diameter, 20-inch-long core tube) encounters
the least resistance during sampler deployment and
retrieval through the sediment because of its short length
and small turning radius. As a result, this model was used
to collect samples in the 4- to 6- (S1A1) and 9- to 11-
(S2A2) foot bss depth intervals, where the degree of
sediment compaction was high. Model B (with its 2-inch-
inside diameter, 40-inch-long core tube) was selected to
collect sediment in the shallow and moderate depth
intervals in S1A2 and S2A1 because of its greater length
and ability to collect sediment in both intervals in one
attempt. Model C (with its 3-inch-inside diameter,
25-inch-long core tube) was used to collect sediment in
situations requiring larger sample volume because of its
larger core tube diameter. Regardless of the sampler
model used, previous sediment sampling experience is also
beneficial for accurately assessing sediment surface using
the sampler and for positioning the sampler in such a way
that sample material is not lost during retrieval.
6.2.2 Ability to Collect Samples Under a Variety
of Site Conditions
The Russian Peat Borer demonstrated its ability to collect
sediment samples under all conditions encountered during
the demonstration, which included a variety of sampling
platforms, water depths, sediment depths, and sediment
compositions. To operate the sampler, the only primary
support facility required is a safe sampling platform.
During the demonstration, the range of sampling platforms
used included wooden planks fastened to ladders in S2A2;
an 18-foot-long, 4-foot-wide Jon boat in S1A2; a sturdier
30-foot-long, 8-foot-wide pontoon boat in S2A1; and the
EPA GLNPO Mudpuppy in S1A1. Because the sampler
does not require electricity or a tripod-mounted winch for
deployment, sampler operation was feasible from any
location on the sampling platforms used.
Because of the lightness of the sampler and extension rods,
water depth had no significant impact on the sampling
technician's ability to deploy and retrieve the sampler.
Sampling location water depths encountered during the
demonstration ranged from about 0.5 foot in S2A2 to
about 18 feet in S2A1. As with all sediment samplers, the
ability to assess the sediment surface with the Russian Peat
Borer diminished with increasing water depth and
turbidity. Because of the water depth and turbidity in
S1A1, S1A2, and S2A1, the sampling technician could not
see the sediment surfaces from the sampling platforms.
An underwater video camera may have enabled the
sampling technician to accurately assess the location of the
sediment surfaces in these areas (Blomqvist 1991).
The sampler was able to collect sediment samples in all
shallow and moderate depth intervals (up to 36 inches bss)
in each demonstration area. However, during a few
attempts in S2A2, partially decomposed cattails and leaves
became caught between the core tube and cover plate,
causing the core tube to remain in the open position during
46
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sampler retrieval and resulting in washout of the
unconsolidated surficial sediment. Similarly, a small stone
prevented complete core tube closure and caused partial
washout of unconsolidated sediment during
1 of 39 attempts in S2A1. In addition, to sample the
unconsolidated sediment in the 0- to 4-inch bss depth
interval in S2A1, the sampling technician had to drive the
sampler beyond the 0- to 4-inch bss depth interval into
layers of sedimentthat offered enough resistance (support)
to hold the cover plate stationary, thus allowing rotation of
the core tube. The unconsolidated surficial sediment did
not offer adequate resistance.
The sampler also demonstrated its ability to collect
sediment samples from deep intervals (greater than 4 feet
bss). In S1A1, the sampler successfully collected
sediment in the 4- to 6-foot bss depth interval during each
attempt at all sampling locations. Because of the degree
of sediment compaction in this area, the sampling
technician used a 10-lb slide-hammer mechanism to drive
the sampler into the target depth interval. As discussed in
Section 6.1.1.2, 12 attempts were made to collect the
specified volume of sediment, whereas only 5 were
expected. The additional attempts were required because
(1) in one attempt, the core tube was not fully rotated to
the closed position and (2) in the remaining attempts, the
sampler had difficulties in penetrating the entire target
depth interval, which contained clay hardpan.
In S2A2, the sampler collected sediment in the 9- to
11-foot bss depth interval at three of the five designated
locations. Because of the degree of sediment compaction
in this area, the sampling technician used a 10-lb slide-
hammer mechanism to drive the sampler into the target
depth interval. Given the significant effort required to
drive and retrieve the sampler using the slide-hammer
mechanism, ARI chose not to complete sampling at the
remaining two locations. At the locations sampled, the
sampler could not be hammered down to the 9-to 11-foot
bss depth interval in one attempt. As a result, ARI needed
multiple sampling attempts to bore a hole down to the 9-
to 11-foot bss depth interval. The depth of sampler
deployment achieved during the first attempts ranged from
about 3 to 4.5 feet bss. Four to six additional attempts
were needed to hammer the sampler into the 9- to 11-foot
bss depth interval.
6.2.3 Ability to Collect an Undisturbed Sample
Based on visual observations, the Russian Peat Borer
consistently collected relatively uncompressed, discrete
cores of sediment in all depth intervals up to 11 feet bss.
In addition, the Russian Peat Borer collected sediment
samples containing shells and biological deposits in S1A1
and live biota such as earthworms in S2A2. Sediment
stratification for consolidated sediment deposits was also
preserved in all samples collected. In general, the Russian
Peat Borer demonstrated a unique ability to collect
relatively uncompressed and representative core samples
of consolidated sediments. However, as discussed above,
partially decomposed cattails, leaves, and a small stone
prevented complete closure of the core tube during a few
attempts in S2A1 and S2A2, resulting in partial washout
of unconsolidated surficial sediment. In addition, layering
of unconsolidated surficial sediment was not typically
preserved after the sampler was retrieved from the water
and positioned horizontally for sample extrusion.
Specifically, laying the sampler in a horizontal position
caused unconsolidated surficial sediment (generally in the
0- to 4-inch bss depth interval) to smear laterally away
from the consolidated core segment, thus disturbing the
sediment stratification.
6.2.4 Durability Eased on Materials of
Construction and Engineering Design
The primary components of the Russian Peat Borer
include a stainless-steel core tube and a Delrin® core head
and bottom point that support a stainless-steel cover plate,
which freely rotates in the core tube (see Figure 2-1). The
core tube is hinged to the cover plate by two stainless-steel
pivot pins at the top and bottom of the plate. Based on
observations made during the demonstration, the Russian
Peat Borer is a sturdy sampler; none of the Delrin® or
stainless-steel components of the sampler was damaged or
required repair or replacement during the demonstration.
However, occasional filing of the edge of the internal wall
of the core tube was necessary to maintain the sharp
cutting edge and thus minimize disturbance of the
sediment. Delrin®, a thermoplastic polymer, is self-
lubricating and has a high modulus of elasticity as well as
strength, stiffness, and resistance to abrasion and moisture.
Earlier sediment samplers with a similar design were
47
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typically made entirely of stainless steel, which according
to the developer of Delrin®, DuPont, would offer greater
hardness and abrasion resistance than Delrin® over the life
of the sampler. However, according to DuPont, Delrin®
offers a cheaper, lightweight alternative to a sampler with
entirely stainless-steel components (Tetra Tech 1999b).
The Russian Peat Borer is also equipped with aluminum
extension rods of varying lengths for collection of
sediment samples. The extension rods are light in weight
and designed to float in water. Each 40-inch-long, 1-inch-
diameter extension rod is equipped with a threaded,
stainless-steel, male coupling nut riveted to one end of the
rod and a threaded, polyethylene, female receptor riveted
to the other. During the demonstration, no bending or
bowing of the extension rods was observed, even when the
rods were coupled together to a total length of about
21 feet for sampling in S2A1. The rigidity of the
extension rods is largely due to their relatively large
diameter to length ratio. However, compared to the body
of the sampler, the extension rods did not exhibit the same
degree of durability. In S2A2, the sampling technician
noticed a few rivets gradually coming loose from an
extension rod during successive attempts to retrieve
sediment from the 9- to 11- foot bss depth interval. The
damage observed was caused by excessive shear force
from the 10-lb slide-hammer mechanism used to drive the
sampler to the desired depth and the torque required to
rotate the core tube 180 degrees through highly
consolidated, stiff peat at a depth of 9 to 11 feet bss. ARI
chose to replace the damaged extension rod with a spare
one available on site. These observations indicate that the
extension rods may require repair or replacement during
extended use in highly consolidated sediment.
6.2.5 Availability of Sampler and Spare Parts
As discussed above, no Russian Peat Borer component or
support equipment required off-site replacement or
servicing during the demonstration; therefore, secondary
objective S5 could not be addressed in the field. Had the
sampler or its support equipment required replacement, the
replacement would not have been available in local retail
stores. Replacement parts may be obtained from ARI by
overnight courier in 2 days or less, depending on the
location of the sampling site.
6.3 Data Quality
The overall QA objective for the demonstration was to
produce well-documented data of known quality. The
TS As conducted to evaluate data quality did not reveal any
problems that would make the demonstration data
unusable. The scope of these TSAs is described in
Sections 4.3 and 4.4 of this ITVR.
This section briefly discusses the data quality of
demonstration results for the Russian Peat Borer; more
detailed information is provided in the DER (Tetra Tech
1999c). Specifically, the data quality associated with the
field measurement activities is discussed first, followed by
the data quality associated with the laboratory analysis
activities.
6.3.1 Field Measurement A ctivities
Field measurement activities conducted during the
demonstration included measurement of the time
associated with sample collection activities, water
velocity, water depth, core length, volume of IDW, volume
of sediment collected in a given sampling attempt, and
depth of sampler deployment. Of these measurement
parameters, specific acceptance criteria were set for the
precision associated with the time and water velocity
measurements only (EPA 1999). All time and water
velocity measurements made during the demonstration met
their respective criteria (see Table 6-7). Of the remaining
parameters, some difficulties were encountered in
measuring the volume of sediment collected in a given
sampling attempt and the depth of sampler deployment,
which are discussed below.
To measure the volume of sediment collected in a given
sampling attempt, the sediment sample was transferred
into a 2-L container graduated in increments of 20 mL.
The container was tapped on a hard surface to minimize
the presence of void spaces in the sample, the sample
surface was made even using a spoon, and the volume of
the sample was measured. However, because the void
spaces could not be completely eliminated, the volumetric
measurements are believed to have a positive bias that
resulted in overestimation of PSRs. Because the total
volume of the void spaces could not be measured, its
48
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impact on the PSR results could not be quantified.
However, because the same volumetric measurement
procedure was used for both the innovative and reference
samplers, the PSR results could still be compared.
The depth of sampler deployment was measured with
reference to the sediment surface. To identify the location
of the sediment surface, the sampling technician lowered
the sampler into the water and used the bottom end of the
sampler to feel the sediment surface. Subsequently, the
technician drove the sampler into the sediment to a depth
that he estimated to be appropriate to collect a sediment
sample in the specified depth interval. Overall during the
demonstration, this approach resulted in actual core
lengths that were up to 6 inches greater than the estimated
depth of sampler deployment, indicating that the sampling
technician may have had some difficulty assessing the
location of the sediment surface. Because the Russian
Peat Borer is a side-filling sampler that collects a
relatively uncompressed sediment sample, the error in
assessing the location of the sediment surface should have
minimal effect on the core length results. However, the
reference samplers used in the demonstration are end-
filling samplers that do not have the advantage of
collecting uncompressed sediment samples. Therefore,
conclusions drawn from a comparison of the sediment
characteristics of the samples collected by the reference
samplers with those of the samples collected by the
Russian Peat Borer should be carefully interpreted.
6.3.2 Laboratory Analysis Activities
The laboratory analyses conducted for the demonstration
included the following: (1) PCB, arsenic, and PSD
analyses of sediment samples and (2) PCB and arsenic
analyses of equipment rinsate samples. To evaluate the
data quality of the laboratory analysis results, field-
generated QC samples, PE samples, and laboratory QC
check samples were analyzed. The field-generated QC
samples included the field replicates and temperature
blanks described in Section 4.3 of this ITVR. The PE
samples and laboratory QC check samples are described in
Section 4.4. The acceptance criteria for the QC samples
are presented in Table 6-7.
All temperature blanks and field replicates subjected to
PCB and arsenic analyses met the acceptance criteria,
indicating that the sample homogenization procedure
(field replicates) and sample preservation procedure
(temperature blanks) implemented in the field met the
demonstration requirements. However, as stated in
Section 6.1.3, in a few cases the results of field triplicate
sample analyses for PSD did not meet the acceptance
criterion. Despite the failures to meet the acceptance
criterion, the PSD results are considered to be valid for the
reasons detailed in Section 6.1.3.
The PE sample results for both the PCB and arsenic
analyses met the acceptance criteria, indicating that the
analytical laboratory accurately measured both PCBs and
arsenic.
The analytical results for all laboratory QC check samples
except the following met the acceptance criteria:
(1) MS/MSD samples for analysis for PCBs in the
sediment matrix and (2) equipment rinsate samples for
PCB analysis. These issues and their likely impact on data
quality are discussed below.
For the sediment matrix, in all MS/MSD samples analyzed
for PCBs, Aroclor 1016 was recovered at levels higher
than the upper limit of the acceptance criterion, indicating
a positive bias in PCB results for sediment samples.
However, the analytical laboratory had no problem
meeting the acceptance criteria for control samples such as
BS/BSDs. For this reason, the failure to meet the
acceptance criterion for MS/MSD sample analysis was
attributed to matrix interference. Because Aroclor 1016
was recovered at levels higher than the upper limit of the
acceptance criterion in all MS/MSD samples associated
with both the innovative and reference samplers, the PCB
results could still be compared.
In all equipment rinsate samples analyzed for PCBs,
decachlorobiphenyl (the surrogate) was recovered at levels
lower than the lower limit of the acceptance criterion,
indicating a negative bias in the PCB results for equipment
rinsate samples. However, the analytical laboratory had
no problem meeting the acceptance criteria for control
samples such as PE samples and deionized water blanks.
For this reason, the failure to meet the surrogate recovery
acceptance criterion for equipment rinsate sample analysis
was attributed to matrix interference. Because the
surrogate was recovered at levels lower than the lower
limit of the acceptance criterion in all equipment rinsate
samples associated with both the innovative and reference
samplers, the PCB results could still be compared.
49
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Table 6-7. Summary of Quality Control Checks and Acceptance Criteria for Field and Laboratory Parameters
Parameter
Quality Control Check
Matrix
Acceptance Criterion
Field
Time required for sample
collection activities
Water velocity
Cooler temperature
Simultaneous measurements
Consecutive measurements
Temperature blank
Not applicable
Water
Water
RPD < 10
RPD < 20
4±2°C
Laboratory
PCBs
Arsenic
Method blank
Surrogate
MS/MSD
Extract duplicates
BS/BSD
Field triplicates
Field duplicates
PE samples
Interference check solution A
Interference check
solution AB
Serial dilution
Method blank
MS/MSD
Postdigestion spike
Digestate duplicates
BS/BSD
Field triplicates
Field duplicates
Sediment and equipment rinsate
Sediment and equipment rinsate
Sediment
Sediment
Equipment rinsate
Sediment
Equipment rinsate
Sediment
Equipment rinsate
Soil
Water
Sediment and equipment rinsate
Sediment and equipment rinsate
Sediment and equipment rinsate
Sediment and equipment rinsate
Sediment
Sediment and equipment rinsate
Sediment and equipment rinsate
Sediment
Equipment rinsate
Sediment
Equipment rinsate
50 times the
instrument detection limit
< Reporting limit
RPD < 10
Percent recovery: 67 to 1 09
Percent recovery: 75 to 1 25
RPD < 10
RPD < 10
Percent recovery: 80 to 1 20
RPD < 10
Percent recovery: 81 to 1 13
RSD < 30
RPD < 20
50
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Table 6-7. Summary of Quality Control Checks and Acceptance Criteria for Field and Laboratory Parameters (Continued)
Parameter
Quality Control Check
Matrix
Acceptance Criterion
Laboratory (Continued)
Arsenic (continued)
PSD
PE samples
Repeat analysis
Field triplicates
Soil
Water
Sediment
Sediment
Actual concentration = 239 mg/kg
Expected recovery3 = 199 mg/kg
Actual recovery11 = 183 mg/kg
Actual concentration = 6.02 mg/kg
Expected recovery3 = 5 mg/kg
Actual recovery11 = 4.81 mg/kg
25.0 to 39.4 parts per billion (certified value:
33.4 parts per billion)
± 1 hydrometer unit
RPD < 15 for sand, silt, and clay
Notes:
±
BS/BSD
mg/kg
MS/MSD
Greater than PCB =
Less than or equal to PE =
Plus or minus PSD =
Blank spike/blank spike duplicate RPD =
Milligram per kilogram RSD =
Matrix spike/matrix spike duplicate
Polychlorinated biphenyl
Performance evaluation
Particle size distribution
Relative percent difference
Relative standard deviation
The expected recovery is based on typical recoveries of arsenic in soil during multiple interlaboratory studies.
The actual recovery is the mean arsenic concentration in the PE sample based on four replicate analyses by the proficiency testing laboratory.
51
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Chapter 7
Performance of the Reference Samplers
To verify a wide range of performance attributes, the
innovative sediment sampler demonstration had both
primary and secondary objectives. Primary objectives
were critical to the technology evaluation and were
intended to produce quantitative results regarding
technology performance. Secondary objectives provided
information that was useful but did not necessarily
produce quantitative results regarding technology
performance. The approach used to address each primary
and secondary objective for the Russian Peat Borer and
reference samplers is discussed in Chapter 4. This chapter
describes the performance of the reference samplers based
on the primary obj ectives (excluding costs associated with
sample collection activities) and secondary objectives.
This chapter also discusses the data quality of
demonstration results for the reference samplers.
The performance of the Russian Peat Borer is discussed in
Chapter 6, costs associated with sample collection
activities (primary objective P7) are presented in
Chapter 8, and the performance of the Russian Peat Borer
and reference samplers is compared in summary form in
Chapter 9.
7.1 Primary Objectives
This section discusses the performance results for the
reference samplers based on the primary objectives stated
in Section 4.1 except for primary objectives P4 and P7,
which are addressed in Section 6.1.4 and Chapter 8,
respectively. Otherwise, the primary objectives discussed
in this section are the same as those discussed in
Section 6.1. During the demonstration, the sampling
technicians were provided an opportunity to practice
sample collection at each demonstration area until they felt
confident enough to initiate demonstration sampling.
To address primary objectives, samples were collected
using two different reference samplers, the Vibrocorer in
S1A1 and the Hand Corer in the other areas. The areas
and depth intervals sampled are the same as those
described in Section 6.1 except that the 4- to 6-foot bss
and 9- to 11-foot bss depth intervals in S1A1 and S2A2,
respectively, were not sampled using the reference
samplers. The Vibrocorer had difficulty fully penetrating
the 4- to 6-foot bss depth interval because of the presence
of clay hardpan and was thus unable to collect samples
from this interval in S1A1; the sampling technicians made
only a few attempts and decided not to complete sampling
in this depth interval. In S2A2, the Hand Corer was not
used for the 9- to 11-foot bss depth interval because it is
not designed to collect samples at depths below 3 feet bss.
Consequently, the reference samplers were not evaluated
with respect to these two depth intervals. The numbers of
investigative and QC samples collected in each area,
sediment sample volumes required, and sample analytical
parameters are discussed in Chapter 4.
The demonstration results for the reference samplers under
primary objectives PI and P2 were evaluated using the
Wilk-Shapiro test to determine whether the results were
normally distributed. Because most of the results were not
normally distributed, the Wilk-Shapiro test was used in an
attempt to evaluate whether the results followed a
lognormal distribution. The test revealed that the results
either were not lognormally distributed or could not be
tested for lognormality because they contained values that
were equal to zero. For these reasons, the Student's t-test,
a parametric test, was not used to perform hypothesis
testing; the Wilcoxon signed rank test, a nonparametric
test, was used as an alternative to the Student's t-test. As
described in Section 6.1, Statistix® was used to perform
statistical evaluations of the demonstration results
52
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(Analytical Software 1996). Appendix C provides details
on the statistical methods used for data evaluation.
7.1.1 Ability to Consistently Collect a Specified
Volume of Sediment
Primary objective PI involved evaluating the reference
samplers' ability to consistently collect a specified volume
of sediment. This objective was addressed by comparing
(1) the actual number of sampling attempts required to
collect a specified volume of sediment to the expected
number of attempts (rounded to the nearest higher integer)
at each sampling location in each target depth interval and
(2) the actual volume of sediment collected in the
specified target depth interval in each attempt to the
calculated sampler volume (design volume) for the depth
interval. The expected number of attempts was
determined by dividing the specified sample volume by the
design volume for the depth interval. The results of these
comparisons are summarized below.
7.1.1.1 Number of Sampling Attempts Required
Tables 7-1 and 7-2 present the expected and actual number
of reference sampler sampling attempts for each depth
interval at Sites 1 and 2, respectively. Initially, the
Wilcoxon signed rank test was used to determine whether
the difference between the expected and actual number of
attempts was statistically significant. However, the
conclusions drawn from the Wilcoxon signed rank test
were inconsistent with the conclusions reached in
comparing the expected and actual number of attempts
(see Appendix C for an example).
In S1A1, the Vibrocorer performed well in the 0- to 4- and
6- to 12-inch bss depth intervals, where the expected
number of attempts equaled the actual number of attempts.
As stated above, the Vibrocorer had difficulty fully
penetrating the 4- to 6-foot bss depth interval because of
the presence of clay hardpan and was thus unable to
collect samples from this interval in S1A1; the sampling
technicians made a few attempts and decided not to
complete sampling in this depth interval.
In S1A2, the Hand Corer performed well in the 0- to
4-inch bss depth interval, where the expected number of
attempts equaled the actual number of attempts, but did
not perform as well in the 12- to 32-inch bss depth
interval. In the 12-to 32-inch bss depth interval, the Hand
Corer required three additional attempts. The additional
attempts in this depth interval may be attributable to
(1) error in assessing the location of the sediment surface,
which might have resulted in the actual depth of
penetration being less than the measured depth of
penetration; (2) deficient entry of sediment into the core
tube (core shortening); (3) the sediment consisting of high
levels of silt (63 to 72 percent) and clay (22 to 31 percent),
which might have caused plug formation in the coring tip
that inhibited further sediment retrieval; or (4) sediment
loss during sampler retrieval.
In S2A1, the Hand Corer again performed better in the
shallower of the two depth intervals sampled. In the 0- to
4-inch bss depth interval, the Hand Corer required
39 attempts, whereas 33 attempts were expected. In the
10- to 30-inch bss depth interval, the Hand Corer required
more than three times the expected number of attempts to
collect adequate sample volumes, and the actual number
Table 7-1. Comparison of Expected and Actual Number of Sampling Attempts for Reference Samplers at Site 1
Location
1A
1E
3C
5A
5E
Total
Number of Attempts in S1A1 (River Mouth) Using Vibrocorer
0- to 4-Inch bss Depth Interval
Expected Actual
1 1
1 1
1 1
1 1
1 1
5 5
6- to 12-Inch bss Depth Interval
Expected Actual
1 1
1 1
1 1
1 1
1 1
5 5
Number of Attempts in S1A2 (Freshwater Bay) Using Hand Corer
0- to 4-Inch bss Depth Interval
Expected Actual
1 1
1 1
1 1
1 1
1 1
5 5
12- to 32-Inch bss Depth Interval
Expected Actual
1 1
1 2
1 3
1 1
1 1
5 8
Note:
bss = Below sediment surface
53
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Table 7-2. Comparison of Expected and Actual Number of Sampling Attempts for Reference Sampler at Site 2
Number of Attempts in
S2A1 (Lake) Using Hand Corer
Location
1A
1B
1E
2A
2C
2D
2E
3A
3B
3E
Total
0- to 4-Inch bss
Expected
3
4
3
2
5
2
2
5
4
3
33
Depth Interval
Actual
3
4
4
2
7
2
2
7
5
3
39
10- to 30-Inch
Expected
1
1
1
1
1
1
1
1
1
1
10
bss Depth Interval
Actual
4
5
3
2
3
1
2
6
3
2
31
Location
1A
1E
3C
5A
5E
Total
Number of Attempts in
S2A2 (Wetland) Using Hand Corer
4-to 12-Inch bss Depth Interval
Expected Actual
Notes:
bss = Below sediment surface
a Sampling was discontinued after the 12 attempts made at this location failed to collect the specified sediment volume.
20
of attempts equaled the expected number of attempts at
only one of the ten sampling locations. The sampler
failures in S2A1 may be attributable to the reasons cited
above for S1A2 except that in S2A1, the sediment does not
consist of as much clay as does the sediment in S1A2 and
thus exhibited less tendency for plug formation in the
coring tip. Also, during sampler retrieval in S2A1, the
sampler's flutter valve did not seat properly in a few
attempts. This malfunction resulted in partial or complete
loss of vacuum in the core tube and subsequent sample
loss.
In the 4- to 12-inch bss depth interval in S2A2, the Hand
Corer had significant difficulty in collecting sediment;
20 attempts were recorded, whereas 5 were expected. Of
the 20 attempts, more than half (12) were recorded at
Location IE. Eight attempts were recorded at the
remaining four locations, whereas four were expected.
Moreover, more than 20 attempts would have been
necessary to complete sampling in this depth interval
because sampling was discontinued at Location IE after
the 12 attempts made at this location failed to collect the
specified sediment volume. The Hand Corer experienced
the greatest number of problems in S2A2, perhaps because
this area contained significant amounts of partially
decomposed reeds and leaves and live vegetation. As a
result, the sediment matrix was highly heterogenous and
was difficult to cut through, capture, and retain. The
sampler failures in S2A2 may also be attributed to the
reasons cited above for S1A2.
In summary, the demonstration results indicate that the
Vibrocorer demonstrated the ability to consistently collect
a specified volume of sediment in the 0- to 4- and 6- to
12-inch bss depth intervals because the number of actual
attempts equaled the number of expected attempts.
However, the Vibrocorer did not collect samples in the 4-
to 6-foot bss depth interval. The Hand Corer collected
surficial sediment well but had difficulty collecting
samples at depths greater than 4 inches bss. In the two 0-
to 4-inch bss depth intervals, the Hand Corer required only
16 percent more attempts than expected (44 actual
attempts versus 38 expected attempts). In contrast, in the
deeper intervals, the Hand Corer required nearly
200 percent more attempts than expected (59 actual
attempts versus 20 expected attempts), indicating a high
level of inconsistency in collecting specified volumes of
sediment.
54
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7.1.1.2 Volume of Sediment Collected
The volume of sediment collected by the reference
samplers in each sampling attempt in a given depth
interval was divided by the corresponding design volume,
and the resulting ratio was multiplied by 100 to estimate
the PSR. The RSD of the PSRs was calculated to evaluate
the ability of the reference samplers to consistently collect
a specified volume of sediment; if a sampler were to
recover an identical volume of sediment in every attempt,
the RSD would equal zero. Both PSR and RSD results
should be considered to properly evaluate the sampler's
performance because a low RSD, which indicates that the
sampler's performance was consistent, may be based on
consistently low PSRs. Figures 7-1 and 7-2 present PSRs
for the reference samplers at Sites 1 and 2, respectively.
Table 7-3 presents PSR summary statistics (range, mean,
and RSD) for both sites.
The Vibrocorer performed well in the 0- to 4- and 6- to
12-inch bss depth intervals in S1A1. Each attempt in the
0- to 4-inch bss depth interval had a PSR of 100. In the 6-
to 12-inch bss depth interval, a narrow PSR range of 79 to
83 resulted in an RSD of 3 percent, which is less than the
30 percent RSD guideline. Although the Vibrocorer
collected a consistent volume of sediment in this depth
interval, it did not collect more than 83 percent of its
design volume.
S1A1, 0- to ilrM^m^aph interval
0- to 4-inch bss depth interval
Total number of attempts: 5
Oto20 >20to40 >40to60 >60to80 >80to100
Vibrocorer percent sample recovery
S1A2, O-tofaebf interval
0- to 4-mcn bss depth interval
Total number of attempts: 5
Oto20 >20to40 >40to60 >60to80 >80to100
Hand Corer percent sample recovery
S1A1, 6- to 1^M20to40 >40to60 >60to80 >80to100
Vibrocorer percent sample recovery
S1A2, 12-tc£3S3tf{^tB!S&:afejbfri interval
12-to 32-inch bss depth interval
Total number of attempts: 8
Oto20 >20to40 >40to60 >60to80 >80to100
Hand Corer percent sample recovery
Note:
bss = Below sediment surface
Figure 7-1. Percent sample recoveries for Vibrocorer and Hand Corer at Site 1.
55
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Oto20 >20to40 >40to60 >60to80 >80to100
Percent sample recovery
>100
- to 3-mcn ss ept inerva
Oto20 >20to40 >40to60 >60to80 >80to100 >100
Percent sample recovery
S2A2,
S2A2 (wetland)
Oto20 >20to40 >40to60 >60to80 >80to100 >100
Percent sample recovery
Notes:
bss = Below sediment surface
Percent sample recoveries exceeding 100 resulted from the volumetric
measurement error associated with the presence of void spaces when
the sediment was transferred to a graduated container.
Figure 7-2. Percent sample recoveries for Hand Corer at Site 2.
In S1A2, the Hand Corer performed well in the 0- to
4-inch bss depth interval but performed poorly in the 12-
to 32-inch bss depth interval. In the 0- to 4-inch bss depth
interval, the Hand Corer achieved a PSR of 100 in every
attempt. However, in the 12-to 3 2-inch bss depth interval,
PSRs ranged from 15 to 55 and had a mean of only 31, as
shown in Table 7-3. As shown in Figure 7-1, five of the
eight attempts in this interval fell in the greater than 20 to
40 percent range, and two of the eight attempts fell in the
0 to 20 percent range. Because the recoveries fell in a
narrow range, the RSD of 35 percent exceeded the RSD
guideline of 30 percent by only 5 percentage points.
In S2A1, the Hand Corer performed well in the 0- to
4-inch bss depth interval but did not perform well in the
10- to 30-inch bss depth interval. As shown in Table 7-3,
PSRs for the 0- to 4-inch bss depth interval ranged from 0
to 100 with a mean of 85. As shown in Figure 7-2, 27 of
the 39 attempts in this interval had PSRs of 80 to 100, and
34 of the 39 attempts had PSRs greater than 60. Because
most of the PSRs fell in a narrow range, the RSD of
33 percent compared favorably to the 30 percent RSD
guideline. In the 10- to 30-inch bss depth interval, the
PSRs ranged from 0 to 50 with a mean of 21. As shown in
Figure 7-2, most of the PSRs fell in the 0 to 20 range. An
RSD of 62 percent was calculated for the 10- to 30-inch
bss depth interval, which indicates a high degree of
inconsistency.
In the 4- to 12-inch bss depth interval in S2A2, the Hand
Corer had difficulty collecting sediment. As shown in
Table 7-3, PSRs for S2A2 ranged from 0 to 125 with a
mean of 22. This wide range of PSRs resulted in an
extremely high RSD of 161 percent. Figure 7-2 shows that
70 percent of the attempts fell in the 0 to 20 PSR range,
which indicates consistently low recoveries.
In summary, the Vibrocorer performed well in the 0- to 4-
and 6-to 12-inch bss depth intervals, and the Hand Corer
performed well in the shallow depth intervals but not in
the deeper intervals. In the 0- to 4- and 6- to 12-inch bss
depth intervals in S1A1, the Vibrocorer had RSDs that
were less than the 30 percent RSD guideline. The Hand
Corer performed well in the 0- to 4-inch bss depth
intervals, in S1A2 and S2A1 for which low RSDs (0 and
33 percent, respectively) were observed. In the 10- to 30-
and 4- to 12-inch bss depth intervals in S2A1 and S2A2,
the RSDs of 62 and 161 percent, respectively, were well
above the 30 percent RSD guideline.
56
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Table 7-3. Percent Sample Recovery Summary Statistics for Reference Samplers
Demonstration Area
S1A1 (river mouth)
S1A2 (freshwater bay)
S2A1 (lake)
S2A2 (wetland)
Reference Sampler
Vibrocorer
Hand Corer
Hand Corer
Hand Corer
Target Depth Interval
(inches bss)
Oto4
6 to 12
Oto4
12 to 32
Oto4
10 to 30
4 to 12
Actual Number
of Attempts
5
5
5
8
39
31
b
20
PSR Range3
100
79 to 83
100
15 to 55
0 to 100
OtoSO
0 to 125
Mean PSR
100
82
100
31
85
21
22
RSD (%)
0
3
0
35
33
62
161
Notes:
bss = Below sediment surface
PSR = Percent sample recovery
RSD = Relative standard deviation
a PSRs exceeding 100 resulted from the volumetric measurement error associated with the presence of void spaces when the sediment was
transferred to a graduated container.
after the 12 attempts made at this location failed to collect the specified sediment volume.
7.1.2 Ability to Consistently Collect Sediment in
a Specified Depth Interval
Primary objective P2 involved evaluating the reference
samplers' ability to consistently collect sediment in a
specified depth interval. This objective was addressed by
comparing actual and target core lengths for each depth
interval. The target core length for a sample was equal to
the distance between the upper and lower boundaries of a
depth interval. Because the core length measurements
presented in this section do not account for void space, an
attempt may have achieved an actual core length that
equaled the target core length but may not have resulted in
a PSR of 100.
Because of difficulties in assessing the location of the
sediment surface, the sampling technicians chose to push
the samplers beyond the specified depth intervals.
Consequently, accuracy in determining a specified depth
interval may have been compromised. To assess overall
accuracy in determining specified depth intervals, core
lengths were compared to depths of sampler deployment;
if a core length equals the depth of deployment, one may
conclude that the core length accurately reflects the
specified depth interval. However, in most cases for the
reference samplers, the core lengths were shorter than the
depths of deployment, indicating the occurrence of core
shortening or loss of sample during sampler retrieval.
Because core shortening plays a significant role in
sediment sampling using end-filling samplers and because
both reference samplers are end-filling samplers, core
shortening is briefly described below.
Core shortening, which primarily involves deficient entry
of sediment into the core tube during sampler penetration,
occurs because friction between sediment and the inside
wall of the sampler gradually increases as the core tube
penetrates the sediment, resulting in gradual thinning of
the core by lateral extrusion in front of the core tube. As
the friction changes with the depth of penetration, the
extent of core shortening also changes. Thus, not all
sediment layers may be uniformly represented within a
given sample, and the actual core length will be less than
the depth of sampler deployment (Blomqvist 1991). Core
shortening is more likely to affect sampling attempts in
deeper intervals than in shallower intervals. Core
shortening is expected to be less prevalent for the
Vibrocorer, because the vibrations produced by this
sampler reduce the friction generated upon sediment entry
into the core tube.
Table 7-4 presents the number of attempts in which the
actual core length equaled the target core length, target
core lengths, and mean actual core lengths. Initially, the
57
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Table 7-4. Comparison of Target and Actual Core Length Data for Reference Samplers
Demonstration Area
S1A1 (river mouth)
S1A2 (freshwater bay)
S2A1 (lake)
S2A2 (wetland)
Number of Attempts in Which
Reference Target Depth Interval Actual Core Length Equaled Target Target Core Length
Sampler (inches bss) Core Length/Total Attempts (inches)
Vibrocorer
Hand Corer
Hand Corer
Hand Corer
Oto4
6 to 12
Oto4
12 to 32
Oto4
10 to 30
4 to 12
5/5
5/5
5/5
0/8
36/39
0/31
3/20
4
6
4
20
4
20
8
Mean Actual Core
Length (inches)
4
6
4
7
5
2
Notes:
bss = Below sediment surface
a The calculated mean actual core length (3.7 inches) was rounded to the nearest integer.
Wilcoxon signed rank test was to be used to determine
whether differences between the actual and target core
lengths were statistically significant. However, review of
the Wilcoxon signed rank test results revealed that the
results for many of the data sets were inconsistent with the
conclusions reached in comparing the target and actual
core lengths for the reasons described in Section 6.1.
Therefore, primary objective P2 was addressed by
evaluating (1) the number of attempts in which the actual
core length equaled the target core length and (2) the
difference between the target core length and the mean
actual core length.
In S1A1, samples collected by the Vibrocorer equaled the
target core length in five out of five attempts in both the 0-
to 4- and 6- to 12-inch bss depth intervals. However,
these results are not surprising because the depth of
sampler deployment was at least 52 inches for these
attempts. The Vibrocorer had difficulty fully penetrating
the 4- to 6-foot bss depth interval in S1A1 because of the
presence of clay hardpan and was thus unable to collect
samples in this interval; the sampling technicians made a
few attempts and then decided not to complete sampling in
this interval. The average core length retrieved in this area
was about 23 percent shorter than the depth of sampler
deployment.
In S1A2, samples collected by the Hand Corer equaled the
target core length in all attempts in the 0- to 4-inch bss
depth interval but failed to do so in any of the attempts in
the 12-to 32-inch bss depth interval. Samples collected in
the latter interval ranged in core length from 3 to
11 inches, with a mean core length of 7 inches. The
additional attempts in this interval may be attributable to
(1) error in assessing the location of the sediment surface,
which might have resulted in the actual depth of
penetration being less than the measured depth of
penetration; (2) core shortening; (3) the sediment
consisting of high levels of silt and clay, resulting in
formation of a plug in the coring tip that inhibited further
sediment retrieval; or (4) sediment loss during sampler
retrieval. The average core length retrieved in this area
was about 52 percent shorter than the depth of sampler
deployment.
The results observed in S2A1 were similar to those
observed in S1A2. In the 0- to 4-inch bss depth interval in
S2A1, samples collected by the Hand Corer equaled the
target core length in 36 of 39 attempts; consequently, the
mean actual core length calculated for this interval
(3.7 inches rounded to 4 inches) compared favorably to the
target core length of 4 inches. However, none of the
samples collected during the 31 attempts in the 10- to
30-inch bss depth interval equaled the target core length.
The actual core lengths in this depth interval ranged from
0 to 12 inches, resulting in a mean core length of 5 inches
that compared unfavorably to the target core length of
20 inches. The sampler failures in the deeper interval in
S2A1 may be attributable to the reasons cited for S1A2
except that in S2A1, the sediment does not consist of as
much clay as does the sediment in S1A2 and thus provides
less opportunity for plug formation in the coring tip. In
58
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S2A1, during sampler retrieval the sampler's flutter valve
did not seat properly in a few attempts. This malfunction
resulted in partial or complete loss of vacuum in the core
tube and thus sample loss. The average core length
retrieved in this area was about 41 percent shorter than the
depth of sampler deployment.
In S2A2, only 3 of the 20 core lengths collected by the
Hand Corer in the 4- to 12-inch bss depth interval equaled
the target core length. The actual core lengths ranged
from 0 to 8 inches, with a mean core length of 2 inches
that compared poorly to the target core length of 8 inches.
As mentioned above, the Hand Corer experienced the
greatest number of problems in S2A2, perhaps because
this area contained significant amounts of partially
decomposed reeds and leaves and live vegetation. As a
result, the sediment matrix was heterogenous and was
difficult to cut through, capture, and retain. The average
core length retrieved in this area was about 78 percent
shorter than the depth of sampler deployment.
In summary, the demonstration results indicate that the
Vibrocorer was able to consistently collect sediment from
the 0- to 4- and 6- to 12-inch bss depth intervals in S1A1
because the core lengths for all attempts in both depth
intervals equaled the target core lengths. The Hand Corer
collected surficial sediment well but had difficulty
collecting samples from depths greater than 4 inches bss.
Specifically, samples collected in the 0- to 4-inch bss
depth intervals equaled the target core length in 41 of
44 attempts. However, the actual core lengths did not
equal the target core length for any of the samples
collected in the 12- to 32- and 10- to 30-inch bss depth
intervals in S1A2 and S2A1, respectively, and equaled the
target core length in only 3 of 20 attempts in the 4- to
12-inch bss depth interval in S2A2.
7.1.3 Ability to Collect Multiple Samples with
Consistent Physical or Chemical
Characteristics, or Both, from a
Homogenous Layer of Sediment
Primary objective P3 involved evaluating the Hand
Corer's ability to collect multiple samples with consistent
physical or chemical characteristics, or both, from a
homogenous layer of sediment. This objective was
addressed by calculating the RSD values for the sample
analytical results for the 12-to 32-inch bss depth interval
in S1A2, and the 0- to 4- and 10- to 30-inch bss depth
intervals in S2A1. Based on the predemonstration
investigation results, these three depth intervals were
determined to be homogenous in terms of their physical
characteristics, and the two S2A1 depth intervals were
determined to be homogenous in terms of their chemical
characteristics.
For the Hand Corer samples, Figure 7-3 presents the
demonstration analytical results for PSD in the 12- to
32-inch bss depth interval in S1A2, and Figure 7-4
presents the demonstration analytical results for arsenic
and PSD in the 0- to 4- and 10- to 30-inch bss depth
intervals in S2A1. The demonstration analytical results
for arsenic contain statistical outliers that indicate that the
two S2A1 depth intervals may not be chemically
homogenous. For this evaluation, the outliers are defined
as sample analytical results that are not within two
standard deviations of the mean; the outliers include the
250 mg/kg of arsenic in the 0- to 4-inch bss depth interval
and the 5 2 mg/kg of arsenic in the 10-to 3 0-inch bss depth
interval in S2A1. Outliers were also found in the
analytical results for samples collected by the Russian Peat
Borer (see Section 6.1.3), providing further evidence that
the two S2A1 depth intervals may not be chemically
homogenous. A similar analysis performed for the PSD
results revealed no statistical outliers. Therefore, the Hand
Corer was evaluated based only on its ability to collect
multiple samples with consistent physical characteristics.
RSDs were calculated for each depth interval based on the
PSD analytical results for all locations sampled.
Table 7-5 presents the PSD summary statistics (range,
mean, and RSD) calculated for the samples and field
triplicates collected using the Hand Corer in each depth
interval relevant to primary objective P3. As stated in
Section 6.1.3, RSDs calculated for the PSD results were
compared to the laboratory acceptance criterion of
15 percent for field triplicates. When the RSD for all
samples from a given depth interval was greater than
15 percent, it was compared to the measured RSD for
the field triplicates. An RSD for all samples that is less
than the RSD for field triplicates may be more
attributable to the laboratory's analytical procedure or
the sample homogenization procedure implemented in
the field, or both, rather than the sampler's ability to
collect physically consistent samples. However, PSD
parameters with means less than 10 percent were not
evaluated in this manner because at low levels, the
analytical method is not as precise; as a result, it will
59
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12- to 32 -inch bss de
Location 1A
Sand: 6%
Silt: 72%
Clay: 22%
Location 5A
Sand: 4%
Silt: 68%
Clay: 28%
3th interval
Location 3C
Sand: 3%
Silt: 70%
Clay: 27%
Location 1 E
Sand: 6%
Silt: 63%
Clay: 31%
Location 5E
Sand: 3%
Silt: 67%
Clay: 30%
Note:
bss = Below sediment surface
Figure 7-3. Hand Corer sample particle size distribution results for S1A2 (freshwater bay).
generate high RSD values and may not actually reveal
whether multiple samples with consistent physical
characteristics were collected.
For the 12- to 32-inch bss depth interval in S1A2, the
RSDs for silt and clay results were below the 15 percent
laboratory acceptance criterion. The mean sand level was
less than 10 percent and was not evaluated using the
criterion. However, the sand levels exhibited a tight range
(3 to 6 percent).
For the 0- to 4-inch bss depth interval in S2A1, the RSD
for silt levels (15 percent) met the laboratory acceptance
criterion, but the RSD for sand levels (23 percent) did not.
Because the RSD for sand levels exceeded the criterion
but the RSD for sand levels in the field triplicates
(3 percent) met the criterion, some of the variation in the
sand results may be attributable to the Hand Corer's ability
to collect multiple samples with consistent physical
characteristics. The mean clay level in samples collected
in the 0- to 4-inch bss depth interval in S2A1 was less than
10 percent and was not evaluated using the criterion.
60
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0- to 4-inch bss depth interval
Location 1A
Arsenic: 250 mg/kg
Sand: 32%
Silt: 63%
Clay: 2%
Location 2A
Arsenic: 190 mg/kg
Location 3A
Arsenic: 140 mg/kg
Sand: 32%
Silt: 63%
Clay: 5%
Location 1 B
Arsenic: 130 mg/kg
Location 3B
Arsenic: 140 mg/kg
Location 2C
Arsenic: 120 mg/kg
Sand: 46%
Silt: 48%
Clay: 2%
Location 2D
Arsenic: 130 mg/kg
Location 1 E
Arsenic: 190 mg/kg
Sand: 26%
Silt: 72%
Clay: 2%
Location 2E
Arsenic: 150 mg/kg
Location 3E
Arsenic: 130 mg/kg
Sand: 29%
Si It: 71%
Clay: 0%
10- to 30-inch bss de|
Location 1A
Arsenic: 24 mg/kg
Sand: 38%
Si It: 61%
Clay: 0%
Location 2A
Arsenic: 8.3 mg/kg
Location 3A
Arsenic: 7.2 mg/kg
Sand: 37%
Silt: 58%
Clay: 4%
5th interval
Location 1 B
Arsenic: 8.5 mg/kg
Location 3B
Arsenic: 8.2 mg/kg
Location 2C
Arsenic: 9.7 mg/kg
Sand: 43%
Silt: 53%
Clay: 3%
Location 2D
Arsenic: 13 mg/kg
Location 1 E
Arsenic: 16 mg/kg
Sand: 35%
Silt: 62%
Clay: 3%
Location 2E
Arsenic: 7.2 mg/kg
Location 3E
Arsenic: 52 mg/kg
Sand: 35%
Silt: 62%
Clay: 3%
Notes:
bss = Below sediment surface
mg/kg = Milligram per kilogram
The particle size distribution results for a given sample may not total 100 percent because of rounding or because some sediment did not pass through
the U.S. Standard No. 4 sieve and was classified as gravel rather than sand, silt, or clay.
Figure 7-4. Hand Corer sample arsenic and particle size distribution results for S2A1 (lake).
61
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Table 7-5. Particle Size Distribution Summary Statistics for Hand Corer
Demonstration Area
S1A2 (freshwater bay)
S2A1 (lake)
Depth
(inches bss)
12 to 32
Oto4
10 to 30
Parameter
Sand
Silt
Clay
Sand
Silt
Clay
Sand
Silt
Clay
Number of
Samples
5
5
5
5
5
5
5
5
5
Range (%)
3 to 6
63 to 72
22 to 31
26 to 46
48 to 72
Oto5
35 to 43
53 to 62
Oto4
Mean (%)
4
68
28
33
63
2
38
59
3
RSD (%)
(All Samples)
34
5
13
23
15
18
9
6
60
RSD (%)
(Field Triplicates)
0
3
8
3
6
29
14
2
71
Notes:
bss =
RSD =
Below sediment surface
Relative standard deviation
However, the clay levels exhibited a tight range (0 to
5 percent).
For the 10- to 30-inch bss depth interval in S2A1, the
RSDs for sand and silt levels were below the 15 percent
laboratory acceptance criterion. The mean clay level in
samples collected in the depth interval was less than
10 percent and was not evaluated using the criterion.
However, the clay levels exhibited a tight range (0 to
4 percent).
In summary, the Hand Corer met the primary objective P3
criteria except for an exceedance in the RSD for sand
levels in the 0- to 4-inch bss depth interval in S2A1.
Therefore, it was concluded that the Hand Corer is
generally able to collect multiple samples with consistent
physical characteristics.
7.1.4 Ability to be Adequately Decontaminated
Primary objective P5 involved evaluating the reference
samplers' ability to be adequately decontaminated. This
objective was addressed by collecting equipment rinsate
samples after sampler decontamination activities in S1A1
and S2A1. Specifically, the 6- to 12-inch bss depth
interval in S1A1 and the 0- to 4-inch bss depth interval in
S2A1 were chosen as the depth intervals where P5 was
evaluated because they contained high concentrations of
PCBs and arsenic, respectively. Although it was intended
that the evaluation of P5 be limited to these depth
intervals, because samples were simultaneously collected
in multiple depth intervals, the primary objective was
addressed for a given area, not for a given depth interval.
However, this deviation did not impact the evaluation of
primary objective P5.
If the reference samplers were adequately decontaminated,
the analytical results for the equipment rinsate samples
would be below the analytical laboratory's reporting
limits. To ensure that the water used to decontaminate the
samplers was not itself contaminated, decontamination
water blanks were also analyzed. Contaminant
concentrations in both the equipment rinsate samples and
decontamination water blanks were below the laboratory
reporting limits for PCBs (1 part per billion) and arsenic
(10 parts per billion). Thus, both the Vibrocorer and Hand
Corer demonstrated the ability to be adequately
decontaminated.
7.1.5 Time Requirements for Sample Collection
Activities
Primary objective P6 involved evaluating the reference
samplers' time requirements for sample collection
activities. These requirements were evaluated in all four
demonstration areas but were not specifically evaluated by
depth interval because samples were simultaneously
collected in multiple depth intervals to reduce the overall
sample collection time. For the Hand Corer, one
technician was required for sampler setup, sample
collection, sampler disassembly, and sampler
decontamination, except in S2A1 where two technicians
were required for sample collection. For the Vibrocorer,
two technicians were required for sampler setup and
62
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sample collection, and one technician was required for
sampler decontamination in S1A1. Sampler disassembly
was not necessary because the Vibrocorer is a permanent
fixture aboard the EPA GLNPQ'sMudpuppy and does not
contain components that require disassembly.
The amounts of time required to complete the sampling
activities are shown in Table 7-6. The time measured for
sample collection activities did not include the time taken
for mobilization, demobilization, and maneuvering the
sampling platforms to sampling locations because these
latter activities were not sampler-specific; rather, they
were either site- or weather-related.
To complete sampling activities in S1A1, the Vibrocorer
required 8 minutes for sampler setup, 124 minutes for
sample collection in the 0- to 4- and 6- to 12-inch bss
depth intervals (15 to 16 minutes per attempt), and
10 minutes for sampler decontamination.
For the Hand Corer, sampler setup required 4 minutes in
S1A2. Sampler setup times are not available for S2A1 and
S2A2. In S2A1, the setup time was included in the sample
collection time for one particular sample, and in S2A2, the
setup time was not recorded. However, the setup time
recorded at S1A2 is probably representative of the time
needed for a moderately experienced technician to set up
the Hand Corer; S1A2 was the last demonstration area
sampled with the Hand Corer, so the technician had ample
opportunity to practice sampler setup in other areas.
Sample collection times for the Hand Corer ranged from
47 to 550 minutes in S1A2, S2A1, and S2A2. Sample
collection with the Hand Corer required 4 to 7 minutes per
attempt in S1A2 and S2A2 but 10 to 16 minutes per
attempt in S2A1. More extension rods were required in
S2A1 than in the other two areas because of the water
depth; five rods were required in S2A1, but only one rod
was required in S1A2 and S2A2. The weight of the
additional extension rods made use of a tripod-mounted
winch necessary to hold the sampler steady during
sampling; incorporating the tripod-mounted winch into the
sampling process in S2A1 accounted for the extra time
necessary for sample collection.
Hand Corer disassembly required 2 minutes in S1A2 and
S2A2 but 4 minutes in S2A1. The additional time
required in S2A1 can again be attributed to the use of
additional extension rods in this area.
Decontamination of the Hand Corer was evaluated only in
S2A1 and required 40 minutes. Because of the numerous
extension rods required in this area, the decontamination
time measured in S2A1 may not be representative. In
addition, S2A1 was the first demonstration area sampled,
and decreased decontamination times were observed for
the other samplers as the technicians became more familiar
with the decontamination procedures required for the
demonstration.
In summary, a technician familiar with the Vibrocorer
would be expected to require 8 minutes for sampler setup,
15 to 16 minutes for each sampling attempt, and
10 minutes for sampler decontamination. A technician
familiar with the Hand Corer would be expected to require
4 minutes for sampler setup, 4 to 7 minutes for each
Table 7-6. Time Required to Complete Sampling Activities for Reference Samplers
Time Required (minutes)
Activity
Sampler setup
Sample collection
Sampler disassembly
Sampler decontamination
Total
S1A1 (River Mouth)
Vibrocorer
8
124
0
10
142
S1A2 (Freshwater Bay)
Hand Corer
4
47
2
Not evaluated
53
S2A1 (Lake)
Hand Corer
Included in sample collection
550
4
40
594
S2A2 (Wetland)
Hand Corer
Not recorded
163a
2
Not evaluated
165a
Note:
Hand Corer sampling was completed at four of five sampling locations. At the fifth location, sampling was discontinued after 12 attempts failed
to collect the specified sediment volume.
63
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sampling attempt, and 2 to 4 minutes for sampler
disassembly. However, more time may be necessary for
sample collection depending on the water depth. It is
uncertain how much time an experienced technician would
need to adequately decontaminate the Hand Corer, but it
is likely that the technician would require less than the
40 minutes observed in S2A1. The amount of
decontamination time would likely have been less in the
other areas because the technician would have had more
practice in implementing the required decontamination
procedures as well as fewer extension rods to
decontaminate. When sediment sampling activities are
planned, the time required for setting up the sampling
platform and for maneuvering the platform to position the
sampler at the sampling location would have to be
considered in addition to the times presented above.
7.2 Secondary Objectives
This section discusses the performance results for the
reference samplers based on secondary objectives SI
through S5 stated in Section 4.1. Secondary objectives
were addressed based on observations of the reference
samplers' performance during the demonstration and on
information provided by the EPA GLNPO.
7.2.1 Skill and Training Requirements for
Proper Sampler Operation
The Hand Corer is easy to operate, requiring minimal
skills and training. Sampler assembly and sample
collection procedures can be learned in the field with a
few practice attempts. In addition, a written SOP
accompanies the sampler when it is procured. The
sampler can be operated by one person in shallow
(wading) water depths because of its lightness (12 Ib).
Sampler operation with plastic core liners is simple
because the sampler does not require complete
disassembly and reassembly after each sampling attempt.
Only the nose piece requires removal to extrude the plastic
core liner containing the sediment core. In water depths
requiring use of extension rods, sampler operation
becomes more cumbersome because of the combined
weight of the stainless-steel sampler and the galvanized-
steel extension rods (5 Ib each). Because of the heaviness
of the sampler equipped with five extension rods, two
personnel and a tripod-mounted winch were needed to
deploy and retrieve the sampler at each sampling location
in S2A1, where the water depth was about 18 feet.
During the demonstration, minimal strength and stamina
were required to collect samples with the Hand Corer from
shallow and moderate depth intervals containing both
unconsolidated and consolidated sediments. Specifically,
minimal strength and stamina were required to drive the
sampler into and retrieve it from the 0- to 4-inch bss depth
interval in S1A2 and S2A1 and the moderate depth
intervals ranging from 10 to 30 and 12 to 32 inches bss in
S2A1 and S1A2, respectively. However, moderate to
significant strength and stamina were required to collect
samples from a depth interval containing partially
decomposed reeds and leaves and live vegetation.
Specifically, moderate to significant strength and stamina
were required to drive the sampler into and retrieve it from
the 4- to 12-inch bss depth interval in S2A2. Sediment in
this interval was consolidated and was predominantly sand
with low water content. The consolidated interval
increased the amount of force required to drive the Hand
Corer. However, the difficulty in driving the sampler was
likely attributable to the sampler's inability to cut through
the sediment that contained significant amounts of
partially decomposed reeds and leaves and live vegetation.
Previous sediment sampling experience is beneficial in
selecting the most appropriate support equipment for a
given Hand Corer application. For example, the sampling
technicians chose to use a tripod-mounted winch in S2A1
because of the significant strength and stamina that would
have been required to deploy and retrieve the sampler in
that area if a winch was not used. Previous sediment
sampling experience is also beneficial in accurately
assessing the location of the sediment surface using the
sampler, as is the case with other samplers.
Operation of the Vibrocorer requires moderate skills and
training, and the sampler must be operated by at least two
persons using a sampling platform. Several hours of
hands-on training with an experienced Vibrocorer
sampling technician is recommended to learn the proper
operation of the sampler and its support equipment. In
addition, during the demonstration, the power supply for
the Vibrocorer malfunctioned during sample collection.
The source of the malfunction was identified and corrected
by on-site personnel. Therefore, it is recommended that at
least one of the sampling technicians have electrical
and mechanical experience to be able to correct
malfunctioning support equipment for the Vibrocorer.
Also, previous sediment sampling experience is beneficial
64
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in assessing the location of the sediment surface using the
sampler, as is the case with other samplers.
During the demonstration, minimal strength and stamina
were required to collect samples with the Vibrocorer in
S1A1. Although the vibrohead and core tube weigh about
150 Ib, sampler deployment and retrieval were controlled
with an A-frame and winch on the EPA GLNPO's
Mudpuppy. The physical effort required to remove the
core tube from the vibrohead and to extract the sample
from the core tube was minimal.
7.2.2 Ability to Collect Samples Under a Variety
of Site Conditions
The Hand Corer demonstrated its ability to collect
sediment samples under all conditions encountered during
the demonstration, which included a variety of sampling
platforms, water depths, sediment depths, and sediment
compositions. The range of sampling platforms used
included wooden planks fastened to ladders in S2A2; an
18-foot-long, 4-foot-wide Jon boat in S1A2; and a sturdier,
30-foot-long, 8-foot-wide pontoon boat in S2A1. Because
the sampler does not require electricity or a tripod-
mounted winch for deployment in shallow water, sampler
operation was feasible from any location on the sampling
platforms used in S1A2 and S2A2. At S2A1, however,
where the water depth was about 18 feet, two sampling
technicians and a tripod-mounted winch were needed to
properly operate the sampler because of the combined
weight of the sampler (12 Ib) and the five extension rods
and turning handle (27 Ib). Use of the tripod-mounted
winch required that a 6-inch-diameter hole be cut in the
center of the pontoon boat to deploy and retrieve the
sampler.
As with other samplers, the ability to assess the location of
the sediment surface with the Hand Corer decreases with
increasing water depth and turbidity. Because of the
significant water depth in S2A1 and turbidity in S1A2, the
sampling technicians could not see the sediment surface
from the sampling platforms. An underwater video
camera may have enabled the sampling technicians to
accurately assess the location of the sediment surface in
these areas (Blomqvist 1991).
The Hand Corer was able to collect sediment samples in
all shallow and moderate depth intervals (less than
36 inches bss) in each demonstration area where the
sampler was deployed. However, as discussed in
Section 7.1.1.1, the actual number of attempts required to
collect the specified volume of sediment exceeded the
expected number at most sampling locations. The
additional attempts may be attributable to (1) error in
assessing the location of the sediment surface, which may
have resulted in the actual depth of penetration being less
than the measured depth of penetration; (2) deficient entry
of sediment into the core tube (core shortening); (3) plug
formation in the coring tip that inhibited further sediment
retrieval; or (4) partial or complete loss of the sediment
core through the bottom end of the sampler as a result of
partial or complete loss of vacuum in the core tube caused
by incomplete closure of the flutter valve. Incomplete
closure of the flutter valve was observed during a few
attempts in S2A2 when partially decomposed plant matter
in the 0- to 4-inch bss depth interval became lodged
between the flutter valve and core tube. Core shortening
(in which the actual core length retrieved is less than the
depth of sediment penetration) primarily involves deficient
entry of sediment into the core tube during core tube
penetration. Physically, sediment friction against the
inside wall of the core tube causes thinning of the core by
lateral extrusion in front of the core tube. As the friction
changes with depth, not all sediment layers may be
uniformly represented in the sample (Blomqvist 1991).
The Vibrocorer demonstrated its ability to consistently
collect sediment samples in the 0- to 4- and 6- to 12-inch
bss depth intervals at all locations in S1A1. As discussed
in Section 7.1.1.1, the actual number of attempts required
to collect the specified volume of sediment in these depth
intervals did not exceed the expected number at any
sampling locations. However, the sampler could not
collect cores longer than 4.4 feet. The Vibrocorer's
difficulty in collecting sediment in the 4- to 6-foot bss
depth interval may be attributed to the sampler not being
able to penetrate clay hardpan observed in the sampling
area about 5 feet bss.
The Vibrocorer was unable to collect samples in S1A2, as
was originally intended. The sampler was installed on the
EPA GLNPO's Mudpuppy, which requires a minimum
water depth of 3 feet for maneuvering. Because the water
depth in S1A2 was only about 2 feet during the
demonstration, fas Mudpuppy was unable to enter the area.
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7.2.3 Ability to Collect an Undisturbed Sample
During the demonstration, both the Hand Corer and
Vibrocorer consistently collected sediment samples in
which the sediment stratification was preserved; however,
based on visual observations, the samples appeared to have
been compacted. Bow wave disturbance near the sediment
surface did not occur in S2A2; the water depth (0.5 to 1.5
feet) and low turbidity in this area allowed visual
confirmation of the location of the sediment surface. Bow
wave disturbance near the sediment surface in the
remaining demonstration areas was unlikely because the
speed of sampler deployment was controlled for each
sampler. As mentioned above, sediment stratification was
preserved for samples collected in these areas.
For both samplers, the total core length retrieved in each
attempt was less than the depth of sampler deployment.
The difference between the total core length retrieved and
the depth of sampler deployment for the Hand Corer
ranged from 15 to 25 inches in S1A2, 1 to 36 inches in
S2A1, and 12 to 67 inches in S2A2. For the Vibrocorer,
the difference ranged from 10.5 to 38.5 inches. As
discussed above, these differences may have resulted for
the reasons described in Section 7.2.2. Furthermore, these
differences indicate that sampling bias might have
occurred during sample collection in a given target depth
interval.
7.2.4 Durability Eased on Materials of
Construction and Engineering Design
The primary components of the Hand Corer include (1) a
Lexan™ nose piece; (2) a 36-inch-long, stainless-steel
core tube; (3) a stainless-steel head piece with a flutter
valve; (4) two detachable, stainless-steel handles; and (5) a
clevis (see Figure 5-1). Based on observations made
during the demonstration, the Hand Corer is a sturdy
sampler; none of the sampler components was damaged or
required repair or replacement during the demonstration.
The Hand Corer was also equipped with varying lengths
of galvanized-steel extension rods during the
demonstration. One extension rod was used to collect
samples in shallow water at S1A2 and S2A2. In both
areas, no bending or bowing of the extension rod was
observed. In S2A1, five extension rods were coupled
together to a combined length of about 25 feet.
Throughout most of the sampling in S2A1, minimal
bowing of the coupled extension rods was observed during
sediment penetration. During one sampling attempt in
S2A1, the pontoon boat drifted after the sampler had been
deployed through the 6-inch-diameter hole in the middle
of the boat and had been driven into the sediment. The
resulting stress on the extension rods caused one of the
rods to be damaged at the threads.
The primary components of the Vibrocorer include (1) an
anodized-aluminum, pressure-housed vibrohead with a
terminal for an electric cable; (2) a disposable, 10-foot-
long, 4-inch-diameter, plastic core tube equipped with a
plastic core catcher; (3) a core tube clamp; and (4) a guide
rope (see Figure 5-2). Based on observations made during
the demonstration, the Vibrocorer is a sturdy sampler;
none of the primary components of the sampler was
damaged or required repair or replacement during the
demonstration. The primary component of the Vibrocorer,
the vibrohead, has an operating expectancy of about
10,000 hours. However, as discussed above, the power
supply for the Vibrocorer malfunctioned during sample
collection. The source of the malfunction (moisture in the
control box between the power source and vibrohead) was
identified and corrected by on-site personnel.
7.2.5 Availability of Sampler and Spare Parts
No primary component of the Hand Corer required
replacement or servicing during the demonstration. Had
a primary sampler component required replacement, it
would not have been available in local retail stores. As
discussed above, an extension rod was damaged at the
threads during sampling in S2A1 and required
replacement. The replacement rod was acquired within a
few hours in a local retail store. Replacement extension
rods and primary sampler components may be obtained
from the developer by overnight courier in 2 days or less,
depending on the location of the sampling site. During
sampling in S1A2, the sampling technician was able to
acquire additional plastic core tube liners from the
developer by overnight courier. The developer precut the
plastic core tube liners in response to a special request
from the sampling technician. During sampling in S2A1
and S2A2, the sampling technician was able to have
plastic core tube liners precut at a local machine shop.
No primary component of the Vibrocorer required
replacement or servicing during the demonstration.
However, as discussed above, the power supply for the
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Vibrocorer malfunctioned and required servicing. The
source of the malfunction was identified and corrected by
on-site personnel within a few hours. Had on-site
personnel been unable to correct the malfunction,
servicing of the power supply by an off-site electrician
would have been necessary. Had the vibrohead
malfunctioned, it would have been packaged and shipped
to the developer for servicing. Because the vibrohead is
pressure-sealed, servicing of the vibrohead is not
recommended in the field or by an unskilled sampling
technician. Plastic core tubes for the Vibrocorer may be
available from a local plastic manufacturer; however, their
availability should be verified prior to a sampling event,
especially one in a remote location. Core tube catchers
used by GLNPO can be made from materials readily
available in a hardware store.
7.3 Data Quality
The overall QA objective for the demonstration was to
produce well-documented data of known quality. The
TSAs conducted to evaluate data quality did not reveal any
problems that would make the demonstration data
unusable. The scope of these TSAs is described in
Sections 4.3 and 4.4 of this ITVR.
This section briefly discusses the data quality of
demonstration results for the reference samplers; more
detailed information is provided in the DER (Tetra Tech
1999c). Specifically, the data quality associated with the
field measurement activities is discussed first, followed by
the data quality associated with the laboratory analysis
activities.
7.3.1 Field Measurement A ctivities
Field measurement activities conducted during the
demonstration included measurement of the time
associated with sample collection activities, water
velocity, water depth, core length, volume of IDW, volume
of sediment collected in a given sampling attempt, and
depth of sampler deployment. Of these measurement
parameters, specific acceptance criteria were set for the
precision associated with the time and water velocity
measurements only (EPA 1999). All time and water
velocity measurements made during the demonstration met
their respective criteria (see Table 6-7). Of the remaining
parameters, some difficulties were encountered in
measuring the volume of sediment collected in a given
sampling attempt and the depth of sampler deployment,
which are discussed below.
To measure the volume of sediment collected in a given
sampling attempt, the sediment sample was transferred
into a 2-L container graduated in increments of 20 mL.
The container was tapped on a hard surface to minimize
the presence of void spaces in the sample, the sample
surface was made even using a spoon, and the volume of
the sample was measured. However, because the void
spaces could not be completely eliminated, the volumetric
measurements are believed to have a positive bias that
resulted in overestimation of PSRs. Because the total
volume of the void spaces could not be measured, its
impact on the PSR results could not be quantified.
However, because the same volumetric measurement
procedure was used for both the innovative and reference
samplers, the PSR results could still be compared.
The depth of sampler deployment was measured with
reference to the sediment surface. To identify the location
of the sediment surface, the sampling technicians lowered
the sampler into the water and used the bottom end of the
sampler to feel the sediment surface. Subsequently, the
technicians drove the sampler into the sediment to a depth
that they estimated to be appropriate to collect a sediment
sample in the specified depth interval. For the Vibrocorer
in S1A1, this approach resulted in an average core length
that was about 23 percent shorter than the estimated depth
of sampler deployment, indicating that the sampling
technicians may have had difficulty assessing the location
of the sediment surface. For the Hand Corer in the
remaining three areas, the average core length retrieved
was shorter than the estimated depth of sampler
deployment, again indicating that the sampling technicians
may have had difficulty assessing the location of the
sediment surface. Specifically, for the Hand Corer in
S1A2, S2A1, and S2A2, the average core length was
shorter than the estimated depth of sampler deployment by
52, 41, and 78 percent, respectively. Because the
reference samplers used in the demonstration are end-
filling samplers that do not have the advantage of
collecting uncompressed sediment samples as does the
Russian Peat Borer, which is a side-filling sampler,
conclusions drawn from a comparison of the sediment
characteristics of the samples collected by the reference
samplers with those of the samples collected by the
Russian Peat Borer should be carefully interpreted.
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7.3.2 Laboratory Analysis Activities
The laboratory analyses conducted for the demonstration
included the following: (1) PCB, arsenic, and PSD
analyses of sediment samples and (2) PCB and arsenic
analyses of equipment rinsate samples. To evaluate the
data quality of the laboratory analysis results, field-
generated QC samples, PE samples, and laboratory QC
check samples were analyzed. The field-generated QC
samples included the field replicates and temperature
blanks described in Section 4.3 of this ITVR. The PE
samples and laboratory QC check samples are described in
Section 4.4. The acceptance criteria for the QC samples
are presented in Table 6-7.
All temperature blanks and field replicates subjected to
PCB and arsenic analyses met the acceptance criteria,
indicating that the sample homogenization procedure (field
replicates) and sample preservation procedure
(temperature blanks) implemented in the field met the
demonstration requirements. However, as stated in
Section 7.1.3, in a few cases the results of field triplicate
sample analyses for PSD did not meet the acceptance
criterion. Despite the failures to meet the acceptance
criterion, the PSD results are considered to be valid for the
reasons detailed in Section 7.1.3.
The PE sample results for both PCB and arsenic analyses
met the acceptance criteria, indicating that the analytical
laboratory accurately measured PCBs and arsenic.
The analytical results for all laboratory QC check samples
except the following met the acceptance criteria:
(1) MS/MSD samples for analysis for PCBs in the
sediment matrix and (2) equipment rinsate samples for
PCB analysis. These issues and their likely impact on data
quality are discussed below.
For the sediment matrix, in all MS/MSD samples analyzed
for PCBs, Aroclor 1016 was recovered at levels higher
than the upper limit of the acceptance criterion, indicating
a positive bias in the PCB results for sediment samples.
However, the analytical laboratory had no problem
meeting the acceptance criteria for control samples such as
BS/BSDs. For this reason, the failure to meet the
acceptance criterion for MS/MSD sample analysis was
attributed to matrix interference. Because Aroclor 1016
was recovered at levels higher than the upper limit of the
acceptance criterion in all MS/MSD samples associated
with both the innovative and reference samplers, the PCB
results could still be compared. The MS/MSD spiking
compounds (Aroclors 1016 and 1260) were selected based
on the Aroclors detected during the predemonstration
investigation and as recommended in SW-846
Method 8082.
Also for the sediment matrix, in one out of three MS/MSD
pairs analyzed for PCBs, Aroclor 1260 was recovered at a
level less than the lower limit of the acceptance criterion
in the MS sample, but the recovery in the associated MSD
sample was acceptable. Because the investigative samples
contained only Aroclor 1242, of the two spiking
compounds used to prepare the MS/MSD samples, only
the Aroclor 1016 recoveries were considered to be relevant
based on the PCB congener distribution; the Aroclor 1260
recoveries were not considered to be relevant. Therefore,
the low recovery associated with Aroclor 1260 had no
impact on data quality.
In all equipment rinsate samples analyzed for PCBs,
decachlorobiphenyl (the surrogate) was recovered at levels
lower than the lower limit of the acceptance criterion,
indicating a negative bias in the PCB results for equipment
rinsate samples. However, the analytical laboratory had
no problem meeting the acceptance criteria for control
samples such as PE samples and deionized water blanks.
For this reason, the failure to meet the surrogate recovery
acceptance criterion for the equipment rinsate sample
analysis was attributed to matrix interference. Because the
surrogate was recovered at levels lower than the lower
limit of the acceptance criterion in all equipment rinsate
samples associated with both the innovative and reference
samplers, the PCB results could still be compared.
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Chapter 8
Economic Analysis
As discussed throughout this ITVR, the Russian Peat
Borer was demonstrated at two sites, each consisting of
two areas. This chapter presents an economic analysis of
sediment sample collection using the Russian Peat Borer
in two of the four demonstration areas: (1) a river mouth
contaminated with PCBs (S1A1) and (2) a lake
contaminated with arsenic (S2A1). These areas were
selected for the economic analysis because the varied
sampling conditions in these areas provide a range of costs
involved in conducting sediment sampling using the
Russian Peat Borer. For example, during the
demonstration in S1A1, the water depth was about 5 to
6 feet, and sediment samples were collected in three depth
intervals: 0 to 4 inches bss, 6 to 12 inches bss, and 4 to
6 feet bss. On the other hand, in S2A1, the water depth
was about 18 feet, and sediment samples were collected in
two depth intervals: 0 to 4 and 10 to 30 inches bss.
The purpose of this economic analysis is to estimate the
costs of using the Russian Peat Borer to collect sediment
samples in environments similar to S1A1 and S2A1. The
analysis is based on the results of the demonstration, unit
costs in published cost data sources, and costs provided by
the technology developers or equipment vendors.
This chapter provides information on the issues and
assumptions involved in the economic analysis (Section
8.1), discusses the costs associated with using the Russian
Peat Borer (Section 8.2), discusses the costs associated
with using the reference samplers (Sections 8.3 and 8.4),
and presents a comparison of the economic analysis results
for the Russian Peat Borer and reference samplers
(Section 8.5).
8.1 Issues and Assumptions
Several factors affect sediment sampling costs. In this
economic analysis, wherever possible, these factors are
identified such that decision-makers can independently
complete a site-specific economic analysis. Costs
included in the analysis are divided into four categories:
sampler, labor, IDW disposal, and support equipment
costs. The issues and assumptions associated with these
categories and the costs not included in this analysis are
briefly discussed below.
8.1.1 Sampler Costs
Sampler costs include the costs of samplers and associated
equipment used during the demonstration, such as
extension rods and core tube liners, as applicable. These
costs were provided by the technology developers or
equipment vendors.
8.1.2 Labor Costs
Labor costs cover the time required for sampler setup,
sample collection, sampler disassembly, and sampler
decontamination. In this analysis, the actual amount of
time required for sample collection activities during the
demonstration is used as the labor requirement, and all
labor times are rounded off to the nearest half-hour.
Because it may not be feasible to hire sampling
technicians for a fraction of a day, a site-specific analysis
should consider the local availability of such technicians
and modify labor cost estimates accordingly. In this
analysis, an hourly rate of $13.51 is used for a technician
(R.S. Means Company [Means] 1999), and a
multiplication factor of 2.5 is applied to labor costs in
order to account for general and administrative and
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overhead costs. Thus, an hourly rate of $34 is used for a
technician.
8.1.3 WWDisposal Costs
IDW disposal costs cover disposal of unused sediment and
spent core tube liners. Unused sediment was assumed to
be a nonhazardous waste because during the
demonstration, the sediment PCB concentrations in S1A1
did not exceed 3.7 parts per million, and wastes containing
PCB concentrations less than 50 parts per million can be
disposed of as nonhazardous waste (40 Code of Federal
Regulations [CFR] 761). Similarly, arsenic-contaminated
wastes that are not listed wastes with toxicity
characteristic leaching procedure (TCLP) extract
concentrations less than 5 milligrams per liter (mg/L) can
be disposed of as nonhazardous waste (40 CFR 261).
During the demonstration, the maximum and average
arsenic concentrations in sediment in S2A1 were 300 and
70 mg/kg, respectively. Based on the average arsenic
concentration and the dilution factor (20) associated with
the TCLP, the TCLP extract concentration for the
sediment waste generated during the demonstration was
estimated to be about 3.5 mg/L. Therefore, unused
sediment in S2A1 was also assumed to be a nonhazardous
waste.
During the demonstration, insignificant quantities of
sediment were present on the spent core tube liners.
Therefore, the spent core tube liners were also assumed to
be a nonhazardous waste. Also, as shown in Table 8-1, the
samplers generated different quantities of IDW in each
demonstration area. However, the volume of IDW
generated by each sampler in each area was less than
55 gallons. Because the cost to package, load, transport,
and dispose of smaller containers is generally the same as
the cost to perform these activities for one 55-gallon drum,
it is assumed that the IDW in each area would be collected
in a 55-gallon drum. As a result, the cost for IDW
disposal is the same for each sampler. However, if larger
numbers of samples were to be collected and the resulting
IDW volume were larger, differences in IDW disposal
costs among samplers would become apparent. The cost
to package, load, transport, and dispose of one 55-gallon
drum of nonhazardous waste is $182 (Means 1999).
8.1.4 Support Equipment Costs
Support equipment includes equipment used for sampler
preparation, sample extrusion, and other activities
associated with sample collection. Examples of support
equipment are a tripod-mounted winch and an electrical
power generator.
8.1.5 Costs Not Included
Items whose costs are not included in this analysis are
identified below along with a rationale for the exclusion of
each.
Oversight of Sampling Activities. A typical user of a
sampler would not be required to pay for customer
oversight of sample collection. EPA representatives
audited all activities associated with sample collection
during the demonstration, but costs for EPA oversight are
not included in this analysis because they are project-
specific and not sampler-dependent. In addition, if
physical characterization of sediment samples is required
to be performed in the field, a soil scientist may be
necessary. However, costs for such oversight are not
Table 8-1. Comparison of Investigation-Derived Waste Quantities Generated by Russian Peat Borer and Reference Samplers
Quantity of Investigation-Derived Waste
Demonstration Area
S1A1 (river mouth)
S2A1 (lake)
Sampler
Russian Peat Borer
Vibrocorer
Russian Peat Borer
Hand Corer
Unused Sediment (liters)
4
45
20
12
Number of Core Tubes
Not applicable
5a
Not applicable
Not applicable
Number of Core Tube Liners
Not applicable
Not applicable
Not applicable
41"
Notes:
a 10-foot-long, 4-inch-diameter, plastic core tubes
b 36-inch-long, 2-inch-diameter, plastic core tube liners
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included in this analysis because they are project-specific
and not sampler-dependent.
Health and Safety Personnel. Health and safety
personnel are required to be present during hazardous
waste site operations, but they are not directly involved in
sample collection activities.
Analyses of Samples Collected. Analytical costs can
vary greatly depending on site-specific contaminants and
are not directly related to sample collection costs.
Personal Protective Equipment. The type of personal
protective equipment required can vary greatly depending
on site-specific contamination and hazards, and the cost of
such equipment is not sampler-dependent.
Disposal of Decontamination Water. Decontamination
water may frequently be disposed of without incurring
additional costs (as was the case during the demon-
stration).
Travel and Per Diem for the Sampling Team. Members
of the sampling team may be available locally. For the
demonstration, the sampling team consisted of both local
and nonlocal staff. Because the availability of sampling
team members is a function of the geographic location of
the sampling site and does not depend on the samplers,
travel and per diem costs for the sampling team are not
included in this analysis.
Boat Rental. A boat may or may not be necessary for
sediment sampling, depending on site conditions and the
sampler chosen. Because the cost of boat rental is not
included in this analysis, other costs associated with using
a boat, such as fuel costs, are also not included.
Time Spent in Maneuvering the Sampling Platform.
The time required to maneuver the sampling platform
varies greatly depending on site conditions such as water
depth and weather. For example, when the wind velocity
was high during the demonstration, a significant amount of
time was spent maneuvering the EPA GLNPO's
Mudpuppy (in S1A1) and the pontoon boat (in S2A1); as
a result, the sampling sometimes had to be discontinued
for the day. Because these delays were not sampler-
dependent, the time spent in maneuvering the sampling
platforms is not included in this analysis.
Time Spent in Managing the Samples. The time
required to homogenize the sediment, fill and label sample
containers, prepare sample containers for shipment, fill out
chain-of-custody forms, and ship the samples varies
greatly depending on the number of samples collected and
site location. Therefore, the time spent in managing the
samples is not included in this analysis because it is
project-specific and not sampler-dependent.
Mobilization and Demobilization. Mobilization and
demobilization costs vary greatly depending on the site
location and conditions. For the demonstration,
mobilization and demobilization activities were mainly
associated with procuring sampling platforms and setting
up sample management areas. The sampling platforms
used were selected based on their availability but not
necessarily based on sampler requirements. For example,
in S1A1, the EPA GLNPQ's Mudpuppy was used because
it was available free of charge from EPA Region 5. Also,
two tents were set up for sample management in S1A1 and
S2A1 to avoid delays resulting from inclement weather but
not based on sampler requirements. Therefore,
mobilization and demobilization costs are not included in
this analysis.
Commonly Available Support Equipment. The cost of
support equipment that is commonly available and likely
would not be purchased specifically for sampling is not
included in this analysis. For example, the cost of
wrenches and tape measures is not included in this
analysis because it is assumed that a field sampling team
would already have such tools as part of its field sampling
gear.
Support Equipment That Costs Less Than $10. The
cost of inexpensive support equipment, such as stainless-
steel spoons and mixing bowls used to homogenize
sediment samples is not included in this analysis. In
addition, the cost of fuel consumed to operate support
equipment such as a generator is not included because,
based on the fuel consumed during the demonstration, the
fuel cost was estimated to be less than $10.
8.2 Russian Peat Borer Costs
This section presents information on sampler, labor, IDW
disposal, and support equipment costs for the Russian Peat
Borer as well as a summary of these costs. Table 8-2
presents these costs.
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Table 8-2. Russian Peat Borer Cost Summary
Item
Quantity
Unit Cost ($)
Total Cost ($)
S1A1 (River Mouth) Costs
Sampler
Model A
Model C
40-inch-long, aluminum extension rods
Labor
I DW disposal
Support equipment
Slide-hammer mechanism
Total"
1 unit
1 unit
4 units
1.5 hours
1 55-gallon drum
1 unit
835
1,350
55
34
182
95
835
1,350
220
51
182
95
$2,730
S2A1 (Lake) Costs
Sampler
Model B
Model C
3-foot-long, aluminum extension rods
4-foot-long, aluminum extension rods
Labor
I DW disposal
Support equipment
Sawhorses
Totala
1 unit
1 unit
3 units
3 units
2.5 hours
1 55-gallon drum
2 units
1,250
1,350
55
65
34
182
15
1,250
1,350
165
195
85
182
30
$3,260
Notes:
IDW = Investigation-derived waste
a The total dollar amount is rounded to the nearest $10.
8.2.1 Sampler Cost
In S1A1, ARI used two different models of the Russian
Peat Borer: (1) a 2-inch-diameter, 20-inch-long model (A)
and (2) a 3-inch-diameter, 25-inch-long model (C). The
purchase costs for Models A and C were $835 and $1,350,
respectively. In addition, ARI used four 40-inch-long,
aluminum extension rods costing $55 each. The total
sampler cost for S1A1 was estimated to be $2,405 (Tetra
Tech 1999a).
In S2A1, ARI used two different models of the Russian
Peat Borer: (1) a 2-inch-diameter, 40-inch-long model (B)
and Model C. The purchase costs for Models B and C
were $1,250 and $1,350, respectively. In addition, ARI
used three 4-foot-long and three 3-foot-long, aluminum
extension rods costing $65 and $55 each, respectively.
The total sampler cost for S2A1 was estimated to be
$2,960 (Tetra Tech 1999a).
8.2.2 Labor Cost
In S1A1, the time for sampler setup, sample collection,
sampler disassembly, and sampler decontamination totaled
88 minutes or about 1.5 hours for one technician. In this
area, five investigative samples each were collected in the
0- to 4- and 6- to 12-inch bss depth intervals as well as in
the 4- to 6-foot bss depth interval using the Russian Peat
Borer. Table 4-3 presents additional information on the
total number of samples collected. The labor cost for
sampling in S1A1 was estimated to be $51.
In S2A1, the time for sampler setup, sample collection,
sampler disassembly, and sampler decontamination totaled
149 minutes or about 2.5 hours for one technician. In this
area, 15 investigative samples each were collected in the
0- to 4- and 10- to 30-inch bss depth intervals using the
Russian Peat Borer. The labor cost for sampling in S2A1
was estimated to be $85.
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8.2.3 IDWDisposal Cost
Sampling in S1A1 generated IDW consisting of 4 L of
unused sediment. The cost for disposal of one 55-gallon
drum of nonhazardous waste is $182.
Sampling in S2A1 generated IDW consisting of 20 L of
unused sediment. The cost for disposal of one 55-gallon
drum of nonhazardous waste is $182.
8.2.4 Support Equipment Cost
Support equipment used during Russian Peat Borer
sampling in S1A1 included a 10-lb ARI slide-hammer
mechanism, two slip wrenches, two window ice scrapers
for sample extrusion, and one file used to sharpen the core
tube edge. The cost of the slip wrenches is not included in
this analysis because a field sampling team would already
have such tools as part of its field sampling gear. The ice
scrapers and file individually cost less than $10. The cost
of the slide-hammer mechanism used in S1A1 was
estimated to be $95.
Support equipment used during Russian Peat Borer
sampling in S2A1 included two slip wrenches, two
window ice scrapers for sample extrusion, one file used to
sharpen the core tube edge, and two sawhorses. The cost
of the slip wrenches is not included in this analysis
because a field sampling team would already have such
tools as part of its field sampling gear. The ice scrapers
and file individually cost less than $10. The total cost of
the sawhorses used in S2A1 was estimated to be $30.
8.2.5 Summary of Russian Peat Borer Costs
In summary, for the Russian Peat Borer, the costs to
collect the number of samples listed in Table 4-3 were
estimated to be $2,730 and $3,260 for S1A1 and S2A1,
respectively. This economic analysis shows that most of
the total cost (about 80 percent) was associated with the
purchase of samplers. The remaining 20 percent was
associated with labor, IDW disposal, and support
equipment costs.
8.3 Hand Corer Costs
This section presents information on sampler, labor, IDW
disposal, and support equipment costs for the Hand Corer
as well as a summary of these costs. Table 8-3 presents
these costs.
Table 8-3. Hand Corer Cost Summary for S2A1 (Lake)
Item
Quantity
Unit Cost I
Total Cost ($)
Sampler
Hand Corer
Core tube liners3
Galvanized-steel extension rods
Labor
Technicians
Cut liners
IDW disposal
Support equipment
Tripod-mounted winch
Total"
1 unit
4 dozen
5 units
20 hours
41 units
1 55-gallon drum
1 unit for 3 days
329
192
93
34
3
182
40
329
768
465
680
123
182
120
$2,670
Notes:
IDW = Investigation-derived waste
a Consumable supplies
b The total dollar amount is rounded to the nearest $10.
73
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8.3.1 Sampler Cost
8.3.3 IDWDisposal Cost
The Hand Corer purchase cost was approximately $329.
During the demonstration, 41 core tube liners and five
5-foot-long, galvanized-steel extension rods were used in
S2A1. Liners were purchased in four packages of 12 at a
cost of $192 per package. The purchase cost of each
extension rod was $93. The total sampler cost was
estimated to be $1,562.
8.3.2 Labor Cost
In S2A1, the time required for sampler setup, sample
collection, sampler disassembly, and sampler
decontamination totaled 594 minutes or about 10 hours for
each of two technicians. In addition, to facilitate sample
extrusion, 41 core tube liners were cut at a local machine
shop at a cost of $3 each, for a total cost of $ 123. In this
area, 15 investigative samples each were collected in the
0- to 4- and 10- to 30-inch bss depth intervals using the
Hand Corer. Table 4-3 presents additional information on
the total number of samples collected. The labor cost for
sampling was therefore estimated to be $803. When field
technicians work more than 8 hours in one day, overtime
costs may be incurred. This estimate, however, includes
no overtime costs.
Sampling in S2A1 generated IDW consisting of 12 L of
unused sediment and 41 core tube liners. The total volume
of IDW generated was less than 55 gallons. The cost for
disposal of one 5 5-gallon drum of nonhazardous waste is
$182.
8.3.4 Support Equipment Costs
Support equipment used during Hand Corer sampling
included a tripod-mounted winch. The tripod-mounted
winch was rented for 3 days at a daily rate of $40 (Hazco
1999). The total cost of the support equipment was
estimated to be $120.
8.3.5 Summary of Hand Corer Costs
In summary, for the Hand Corer, the costs to collect the
number of samples listed in Table 4-3 were estimated to be
$2,670. This economic analysis shows that most of the
total cost was associated with sampler purchase
(59 percent) and labor (30 percent). The remaining
11 percent was associated with IDW disposal and support
equipment costs.
Table 8-4. Vibrocorer Cost Summary for S1A1 (River Mouth)
Item
Quantity
Unit Cost ($)
Total Cost ($)
Sampler
Vibrocorer
Core tubes3
Labor
IDW disposal
Support equipment
A-frame and winches
Drill
Saw
Total"
1 unit
5 units
6 hours
1 55-gallon drum
1 unit
1 unit for 1 day
1 unit for 1 day
24,500
25
34
182
3,500
12
15
24,500
125
204
182
3,500
12
15
$28,540
Notes:
IDW = Investigation-derived waste
a Consumable supplies
b
The total dollar amount is rounded to the nearest $10.
74
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8.4 Vibrocorer Costs
This section presents information on sampler, labor, IDW
disposal, and support equipment costs for the Vibrocorer
as well as a summary of these costs. Table 8-4 presents
these costs.
8.4.1 Sampler Cost
The Vibrocorer purchase cost was approximately $24,500.
Also, 4-inch-diameter, 10-foot-long, plastic core tubes
were required for sample collection. During the
demonstration, five tubes were used, and the purchase cost
of each tube was $25. The total sampler cost was
estimated to be $24,625. Because the Vibrocorer's
purchase cost is relatively high and because the Vibrocorer
is not available for rental, the Vibrocorer should be
considered for sediment sampling only when the sampling
program is expected to be of long duration, which will
allow recovery of the sampler purchase cost.
8.4.2 Labor Cost
The time required for sampler setup, sample collection,
sampler disassembly, and sampler decontamination totaled
142 minutes or about 2.5 hours for each of two
technicians. In addition, one technician spent about 1 hour
preparing core catchers at an off-site location. In S1A1,
five investigative samples each were collected in the 0- to
4- and 6- to 12-inch bss depth intervals using the
Vibrocorer. Table 4-3 presents additional information on
the total number of samples collected. The labor cost for
sampling was estimated to be $204.
8.4.3 IDW Disposal Cost
Sampling in S1A1 generated IDW consisting of 45 L of
unused sediment and five plastic core tubes. The total
volume of IDW generated was less than 55 gallons. The
cost for disposal of one 55-gallon drum of nonhazardous
waste is $182.
8.4.4 Support Equipment Cost
Support equipment costs for the Vibrocorer included a
purchase price of $3,500 for an A-frame and two electric
(12-volt direct current) winches with steel cable for raising
and lowering the sampler; a 1-day rental cost of $12 for
one portable drill (Cincy Tool Rental 1999); and a 1-day
rental cost of $ 15 for one portable circular saw (Falls Tool
Rental 1999). Two 3/4-inch socket wrenches, each costing
less than $ 10, were also used. The total cost of the support
equipment was estimated to be $3,527.
8.4.5 Summary of Vibrocorer Costs
In summary, for the Vibrocorer, the costs to collect the
number of samples listed in Table 4-3 for the top two
depth intervals in S1A1 were estimated to be $28,540.
This economic analysis shows that most of the total cost
was associated with sampler purchase (86 percent). The
remaining 14 percent was associated with labor, IDW
disposal, and support equipment costs.
8.5 Comparison of Economic Analysis Results
The costs for each sampler used in S1A1 and S2A1 are
summarized in Table 8-5. For S1A1, the total costs for the
Russian Peat Borer were 90 percent less than the costs for
the reference sampler, the Vibrocorer. This difference was
due mainly to the costs involved in purchasing the
samplers. However, costs that were dependent on the
number of samples collected or the amount of time
required (which is itself dependent on the number of
samples collected), such as labor and support equipment
costs, were also higher for the Vibrocorer. In addition, of
the two samplers, only the Russian Peat Borer collected
samples in the 4- to 6-foot bss depth interval in S1A1; the
Vibrocorer's sampling costs would likely have been higher
if it had collected samples in this interval because of
greater sample collection times and possibly higher IDW
disposal costs.
For S2A1, the total costs for the Russian Peat Borer were
22 percent more than the costs for the reference sampler,
the Hand Corer. This difference was mainly the result of
higher purchase costs for the Russian Peat Borer. Two
different Russian Peat Borer models were used during the
demonstration to minimize the volume of IDW generated.
Minimization of IDW volume did not impact the cost of
IDW disposal because no cost benefit is realized when the
volume is less than the capacity of one 55-gallon drum.
However, if a larger number of samples were to be
collected, the volume of IDW generated would increase
and could become more significant. If only one Russian
Peat Borer model were used, sampler costs would be
significantly reduced, but the impact on sample collection
time is difficult to estimate.
75
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Table 8-5. Comparison of Costs for Russian Peat Borer and Reference Samplers
S1A1 (River Mouth) S2A1 (Lake)
Item
Sampler
Labor
IDW Disposal
Support Equipment
Total"
Russian Peat Borer
$2,405
51
182
95
$2,730
Vibrocorer
$24,625
204
182
3,527
$28,540
Russian Peat Borer
$2,960
85
182
30
$3,260
Hand Corer
$1 ,562
803
182
120
$2,670
Notes:
IDW = Investigation-derived waste
a Each total dollar amount is rounded to the nearest $10.
76
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Chapter 9
Summary of Demonstration Results
As discussed throughout this ITVR, the Russian Peat
Borer was demonstrated at two sites in EPA Regions 1
and 5. At the Region 1 site, the Russian Peat Borer was
demonstrated in two areas: a lake (S2A1) and a wetland
(S2A2). At the Region 5 site, the Russian Peat Borer was
also demonstrated in two areas: a river mouth (S1A1) and
a freshwater bay (S1A2). Collectively, the four areas
provided a variety of sampling conditions such as different
water depths, sediment types, sediment contaminant
characteristics, and sediment thicknesses necessary to
properly evaluate the sampler. Based on the
predemonstration investigation results, demonstration
objectives, and site support facilities available, (1) the
Hand Corer was selected as the reference sampler for
S1A2, S2A1, and S2A2, and (2) the Vibrocorer was
selected as the reference sampler for S1A1.
This chapter compares the performance and cost results
for the Russian Peat Borer with those for the reference
samplers. Tables 9-1 and 9-2 summarize the demon-
stration results for the primary and secondary objectives,
respectively. As shown in these tables, the Russian Peat
Borer was the only sampler that was able to collect
samples in the deep depth interval (4 to 11 feet bss). Key
demonstration findings are summarized below for the
primary and secondary objectives.
9.1 Primary Objectives
Key demonstration findings are summarized below for
primary objectives PI through P7.
PI. In the shallow depth interval (0 to 4 inches bss), to
collect a specified number of samples, the Russian
Peat Borer required 33 percent more attempts than
expected (65 actual versus 49 expected), whereas
the reference samplers required 14 percent more
attempts than expected (49 actual versus 43
expected).
PI. In the moderate depth interval (4 to 32 inches bss),
the Russian Peat Borer required 21 percent more
attempts than expected (46 actual versus 38
expected), but the reference samplers required
156 percent more attempts than expected (64 actual
versus 25 expected).
PI. For the shallow depth interval, mean PSRs ranging
from 71 to 84 were achieved by the Russian Peat
Borer, whereas the reference samplers' mean PSRs
ranged from 85 to 100. The variation in PSRs as
measured by their RSDs ranged from 26 to
42 percent for the Russian Peat Borer, whereas the
reference samplers' RSDs ranged from 0 to
33 percent.
PI. Forthe moderate depth interval, mean PSRs ranging
from 75 to 101 were achieved by the Russian Peat
Borer, whereas the reference samplers' mean PSRs
ranged from 21 to 82. The RSDs for the Russian
Peat Borer ranged from 6 to 31 percent, whereas the
reference samplers' RSDs ranged from 3 to
161 percent.
P2. For the shallow depth interval, the Russian Peat
Borer's actual core lengths equaled the target core
length in 98 percent of the total sampling attempts.
The reference samplers' actual core lengths equaled
the target core length in 94 percent of the total
sampling attempts. However, the results for the
samplers were significantly different for the
moderate depth interval: 93 percent for the Russian
77
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Table 9-1. Summary of Results for Primary Objectives
Primary Objective
P1 Ability to consistently
collect a specified
volume of sediment
P2 Ability to consistently
collect sediment in a
specified depth interval
P3 Ability to collect
samples with
consistent
characteristics from a
homogenous layer of
sediment
P4 Ability to collect a
representative sample
from a clean sediment
layer below a
contaminated sediment
layer
P5 Ability to be adequately
decontaminated
Evaluation Criterion
Actual versus expected
number of sampling
attempts
Volume of sediment
sampled versus design
volume
Number of sampling
attempts in which
actual core length
equaled target core
length
Variability of sample
characteristics in terms
of PSD
Mean difference
between innovative
and reference sampler
arsenic concentrations
for clean layer is zero
Contaminant
concentrations in
equipment rinsate
samples are below
reporting limits
Sampling Depth Interval/
Demonstration Area3
Shallow (0 to 4 inches bss)/S1 A1 , S1 A2,
and S2A1
Moderate (4 to 32 inches bss)/S1 A1 , S1 A2,
S2A1 , and S2A2
Deep (4 to 11 feet bss)/S1A1 and S2A2
Shallow (0 to 4 inches bss)/S1 A1 , S1 A2,
and S2A1
Moderate (4 to 32 inches bss)/S1 A1 , S1 A2,
S2A1 , and S2A2
Deep (4 to 11 feet bss)/S1A1 and S2A2
Shallow (0 to 4 inches bss)/S1 A1 , S1 A2,
and S2A1
Moderate (4 to 32 inches bss)/S1 A1 , S1 A2,
S2A1 , and S2A2
Deep (4 to 11 feet bss)/S1A1 and S2A2
0 to 4 inches bss/S2A1
1 0 to 30 inches bss/S2A1
12to32inchesbss/S1A2
1 0 to 30 inches bss/S2A1
Objective addressed by area: one PCB-
contaminated area (S1A1) and one arsenic-
contaminated area (S2A1)
Performance Results
Russian Peat Borer
65 actual attempts versus 49 expected
attempts (33% more than expected)
46 actual attempts versus 38 expected
attempts (21% more than expected)
15 actual attempts versus 8 expected
attempts (88% more than expected)
Mean PSRs: 71 to 84
RSDs of PSRs: 26 to 42%
Mean PSRs: 75 to 101d
RSDs of PSRs: 6 to 31%
Mean PSRs: 45 and 122d
RSDs of PSRs: 71 and 16%
64 of 65 attempts (98%)
43 of 46 attempts (93%)
4 of 15 attempts (27%)
Sand: 26 to 35%
Silt: 48 to 66%
Clay: 2 to 8%
Sand: 34 to 37%
Silt: 57 to 62%
Clay: 2 to 9%
Sand: 1%
Silt: 73 to 82%
Clay: 17 to 26%
Reference Sampler11
49 actual attempts versus 43 expected
attempts (14% more than expected)
64 actual attempts versus 25 expected
attempts (156% more than expected)
Unable to collect samples0
Mean PSRs: 85 to 100
RSDs of PSRs: 0 to 33%
Mean PSRs: 21 to 82
RSDs of PSRs: 3 to 161%
Unable to collect samples0
46 of 49 attempts (94%)
8 of 64 attempts (13%)
Unable to collect samples0
Sand: 26 to 46%
Silt: 48 to 72%
Clay: 0 to 5%
Sand: 35 to 43%
Silt: 53 to 62%
Clay: 0 to 4%
Sand: 3 to 6%
Silt: 63 to 72%
Clay: 22 to 31 %
According to the Wilcoxon signed rank test, there was a 61 percent probability that the
innovative and reference sampler arsenic concentrations were not different.
The contaminant concentrations in the equipment rinsate samples for the Russian Peat
Borer and reference samplers were below the reporting limits (1 part per billion for PCBs
and 10 parts per billion for arsenic).
-------
Table 9-1. Summary of Results for Primary Objectives (Continued)
Primary Objective
P6 Time requirements for
sample collection
activities
P7 Sampling costs
Evaluation Criterion
Total time required for
sampler setup, sample
collection, sampler
disassembly, and
sampler
decontamination
Total cost, including
sampler, labor, IDW
disposal, and support
equipment costs
Sampling Depth Interval/
Demonstration Area3
Objective addressed by area: S1A1
Objective addressed by area: S1A2
Objective addressed by area: S2A1
Objective addressed by area: S2A2
Objective addressed by area: S1A1
Objective addressed by area: S2A1
Performance Results
Russian Peat Borer
88 minutes6
12 minutes
149 minutes
138 minutes'
$2,730e
$3,260
Reference Sampler11
142 minutes6
53 minutes
594 minutes
165 minutes'
$28,540e
$2,670
Notes:
bss = Below sediment surface
IDW = Investigation-derived waste
PCB = Polychlorinated biphenyl
PSD = Particle size distribution
PSR = Percent sample recovery
RSD = Relative standard deviation
S1A1 = River mouth
S1A2 = Freshwater bay
S2A1 = Lake
S2A2 = Wetland
Based on the PSD results, the shallow depth interval contained silty sand in S1A1, predominantly sand and silt with some clay in S1A2, and sandy silt in S2A1. The moderate depth interval
contained sandy silt in both S1A1 and S2A1, clayey silt in S1A2, and predominantly silt with some sand and clay inS2A2. Also, inS2A2, the (1) shallow and moderate depth intervals contained
significant amounts of partially decomposed reeds and leaves and live vegetation and (2) deep depth interval contained peat. The sediment in the deep depth interval was not analyzed for
PSD.
The Hand Corer was used as the reference sampler in S1A2, S2A1, and S2A2. The Vibrocorer was used as the reference sampler in S1A1.
The Hand Corer is not designed to collect samples in the deep depth interval. The Viborocorer was unable to collect samples below Sfeet bss because of the presence of clay hardpan in S1A1.
PSRs exceeding 100 resulted from the volumetric measurement error associated with the presence of void spaces when the sediment was transferred to a graduated container.
In S1A1, the Russian Peat Borer collected samples in all three depth intervals (shallow, moderate, and deep), but the reference sampler collected samples in only the shallow and moderate
depth intervals.
In S2A2, the Russian Peat Borer collected samples in both depth intervals (moderate and deep), but the reference sampler collected samples in only the moderate depth interval.
-------
Table 9-2. Summary of Results for Secondary Objectives
Secondary Objective
Performance Results
Russian Peat Borer
Reference Sampler3
Hand Corer
Vibrocorer
S1 Skills and training
requirements for proper
sampler operation
Easy to operate; requires minimal skills and
training
Can be operated by one person because of its
lightness and because it has only one moving
part
Easy to operate; requires minimal skills and
training
Can be operated by one person when up to
two extension rods are used; two persons and
a tripod-mounted winch are recommended
when more extension rods are used
Relatively complicated to operate; requires
moderate skills and training
Requires two persons and a motor-operated
winch because of the heaviness of the
sampler (about 150 Ib)
S2 Ability to collect samples
under a variety of site
conditions
oo
o
Collected samples in a river mouth (S1A1),
freshwater bay (S1A2), lake (S2A1), and
wetland (S2A2) where water depths ranged
from 0.5 foot to 18 feet
Collected samples in shallow (0- to 4-inch
bss), moderate (4- to 32-inch bss), and deep
(4- to 11 -foot bss) depth intervals
Collected samples from a variety of sampling
platforms: wooden planks fastened to ladders,
a Jon boat, a pontoon boat, and the EPA
GLNPO's Mudpuppy
Collected samples in a freshwater bay
(S1A2), lake (S2A1), and wetland (S2A2)
where water depths ranged from 0.5 foot to 18
feet
Collected samples in shallow (0- to 4-inch
bss) and moderate (4- to 32-inch bss) depth
intervals; sampler is not designed to collect
samples in depth intervals below 3 feet bss
Collected samples from a variety of sampling
platforms: wooden planks fastened to ladders,
a Jon boat, and a pontoon boat
Material caught between core tube and flutter
valve could cause partial or complete loss of
sample
Collected samples in a river mouth (S1A1)
where water depths ranged from 5 to 6 feet
Collected samples in shallow (0- to 4-inch
bss) and moderate (4- to 32-inch bss) depth
intervals but was unable to penetrate clay
hardpan in order to collect samples in 4- to
6-foot bss depth interval
Collected samples from the EPA GLNPO's
Mudpuppy
S3 Ability to collect an
undisturbed sample
Collected discrete, relatively uncompressed,
representative core samples of consolidated
sediment, based on visual observations
Sediment stratification preserved for
consolidated sediment but not for
unconsolidated sediment
Material caught between core tube and cover
plate could prevent complete closure of core
tube, resulting in partial or complete washout
of unconsolidated sediment
Collected relatively compressed core samples
of both unconsolidated and consolidated
sediments from the sediment surface
downward, based on visual observations
Sediment stratification preserved for both
unconsolidated and consolidated sediments
Samples collected in and below moderate
depth interval may be of questionable
representativeness because of core
shortening and core compression; sampler is
not designed to collect samples in depth
intervals below 3 feet bss
Collected relatively compressed core samples
of both unconsolidated and consolidated
sediments from the sediment surface
downward, based on visual observations
Sediment stratification preserved for both
unconsolidated and consolidated sediments
Samples collected in moderate and deep
depth intervals may be of questionable
representativeness because of core
shortening and core compression
-------
Table 9-2. Summary of Results for Secondary Objectives (Continued)
Secondary Objective
Performance Results
Russian Peat Borer
Reference Sampler3
Hand Corer
Vibrocorer
S4 Durability based on
materials of construction
and engineering design
Sampler is sturdy; its primary components are
made of stainless steel and Delrin®
Aluminum extension rods are rigid and float;
no bending or bowing was observed when
rods were coupled to a total length of 21 feet
During sample collection in 9- to 11-foot bss
depth interval in S2A2, excessive stress
associated with sampling caused a few rivets
on one extension rod to gradually come loose
Sampler is sturdy; most of its primary
components are made of stainless steel
Galvanized extension rods are rigid; minimal
bending or bowing was observed when rods
were coupled to a total length of 25 feet
During sample collection in S2A1, where
water depth was about 18 feet, the pontoon
boat drifted; the resulting stress damaged one
extension rod at the threads
Sampler is sturdy; its primary component, the
vibrohead, is made of anodized aluminum and
has a life expectancy of 10,000 operating
hours
During sample collection in S1A1, the power
supply for the sampler malfunctioned; the
source of the malfunction was identified and
corrected by on-site personnel
S5 Availability of sampler
and spare parts
Sampler and its support equipment are not
expected to be available in local retail stores
but may be obtained from technology
developer by overnight courier in 2 days or
less, depending on the location of the
sampling site
Primary components of sampler are not
expected to be available in local retail stores
but may be obtained from technology
developer by overnight courier in 2 days or
less, depending on the location of the
sampling site; extension rods are expected to
be available in local retail stores
Primary sampler component, the vibrohead, is
not available in local retail stores; because the
vibrohead is pressure-sealed, if it
malfunctions, it should be packaged and
shipped to the developer for servicing
Notes:
bss
EPA
GLNPO =
Below sediment surface
U.S. Environmental Protection Agency
Great Lakes National Program Office
The Hand Corer was used as the reference sampler in S1A2, S2A1, and S2A2. The Vibrocorer was used as the reference sampler in S1A1.
-------
Peat Borer compared to 13 percent for the reference
samplers.
P3. Based on the PSD results, both the Russian Peat
Borer and reference samplers collected samples with
consistent physical characteristics from a
homogenous layer of sediment.
P4. The Russian Peat Borer collected samples from a
clean sediment layer below a contaminated sediment
layer that were at least as representative as the
samples collected from the clean layer by the
reference sampler (the Hand Corer); contaminant
concentrations in the samples collected by both
samplers were not statistically different at a
significance level of 0.05.
P5. Both the Russian Peat Borer and reference samplers
demonstrated the ability to be adequately
decontaminated after sampling in areas
contaminated with either PCBs or arsenic.
P6. Compared to the reference samplers, the Russian
Peat Borer not only was able to collect samples in
all depth intervals and areas but also reduced
sampling time by 16 to 77 percent, depending on the
area.
P7. Sampling costs were estimated for two of the four
areas sampled. In one area, the sampling costs for
the Russian Peat Borer were 90 percent less than
those for the reference sampler (the Vibrocorer); in
the other area, the sampling costs for the Russian
Peat Borer were 22 percent more than those for the
reference sampler (the Hand Corer).
9.2 Secondary Objectives
Key demonstration findings are summarized below for
secondary objectives SI through S5.
S1. The Russian Peat Borer, like the Hand Corer, is easy
to operate and requires minimal skills and training.
However, operation of the Vibrocorer is relatively
complicated and requires moderate skills and
training.
S1. The Russian Peat Borer was operated by one person,
whereas the Hand Corer was operated by one or two
persons and the Vibrocorer was operated by two
persons. In addition, when more than two extension
rods were required, the Hand Corer was operated
using a tripod-mounted winch. Also, the Vibrocorer
operation required a motor-operated winch, whereas
the Russian Peat Borer was operated without a
winch throughout the demonstration.
S2. The Russian Peat Borer collected samples in all
depth intervals and demonstration areas. The
reference samplers were unable to collect samples in
deep depth intervals (4 to 11 feet bss).
S2. Neither the Russian Peat Borer nor the Hand Corer
requires a power supply. In contrast, the Vibrocorer
requires a three-phase, 230- or 440-volt, 50- to
60-hertz power supply, which is a sampler limitation
if the power supply fails.
S3. The Russian Peat Borer collected representative
core samples of consolidated sediment in discrete
depth intervals. Visual observations indicated that
these samples were relatively uncompressed. The
reference samplers collected relative compressed
core samples of both consolidated and
unconsolidated sediments from the sediment surface
downward. In addition, in moderate and deep depth
intervals, samples collected by the reference
samplers may be of questionable representativeness
because of core shortening and core compression.
S3. In the samples collected by the Russian Peat Borer,
sediment stratification was preserved for
consolidated sediment but not for unconsolidated
sediment. Sediment stratification was preserved for
both consolidated and unconsolidated sediments in
the samples collected by the reference samplers.
S4. Based on their materials of construction and
engineering designs, both the Russian Peat Borer
and reference samplers are considered to be sturdy.
S5. The Russian Peat Borer and its support equipment
are not expected to be available in local retail stores.
Similarly, the primary components of the Hand
Corer and Vibrocorer are not expected to be
available in local retail stores; extension rods for the
Hand Corer may be locally available.
82
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Chapter 10
References
Aaby, B., and G. Digerfeldt. 1986. "Sampling
Techniques for Lakes and Bogs." Chapter 8 in
Handbook of Holocene Palaeoecology and
Palaeohydrology. B.E. Berglund, Editor. John Wiley
& Sons, New York.
Analytical Software. 1996. Statistix8
Version 2.0. Tallahassee, Florida.
for Windows.
ASTM. 1998. "ASTM Standards in Building Codes."
Volumes. C 962-D 2940.
Belokopytov, I.E., and V.V. Beresnevich. 1955.
"Giktorf s Peat Borers." TorfyanayaPromyflilennost.
Number 8. Pages 9 and 10.
Blomqvist, S. 1991. "Quantitative Sampling of Soft-
Bottom Sediments: Problems and Solutions." Marine
Ecology Progress Series. Volume 72. Pages 295
through 304.
Cincy Tool Rental. 1999. "Electric Tools." On-Line
Address: http://www.cincytool.com/cgi-bin/
hackmai!4.cgi?electric. Accessed on August 4.
Downing, J.A. 1984. "Sampling the Benthos of Standing
Waters." Chapter 4 in Manual on Methods for the
Assessment of Secondary Productivity in Fresh
Waters. J.A. Downing and F.H Rigler, Editors.
Blackwell Scientific Publications. Oxford, England.
Environment Canada. 1994. "Guidance Document on
Collection and Preparation of Sediment for
Physicochemical Characterization and Biological
Testing." Environmental Protection Series. Report
EPS l/RM/29. December.
EPA. 1996. "Test Methods for Evaluating Solid Waste."
Volumes 1A through 1C. SW-846. Third Edition.
Update III. OSWER. Washington, DC. December.
EPA. 1999. "Sediment Sampling Technologies Demon-
stration Plan." ORD. Washington, DC. April.
Faegri, K., and J. Iversen. 1989. Textbook of Pollen
Analysis. Knut Faegri, Peter Emil Kaland, and Knut
Krzywinski, Editors. Fourth Edition. Pages 60
through 63.
Falls Tool Rental. 1999. "Power Tool Rental Rates."
On-Line Address: http://www.fallstoolrental.com/
powertools.html. Accessed on August 4.
Gilbert, R. 1987. Statistical Methods for Environmental
Pollution Monitoring. Van Nostrand Reinhold
Company, Inc. New York.
Hazco. 1999. Equipment Management Program Price
List. Dayton, Ohio.
Jowsey, P.C. 1966. "An Improved Peat Sampler." New
Phytologist. Volume 65. Pages 245 through 248.
Means. 1999. Environmental Remediation Cost Data—
Unit Price. Kingston, Massachusetts.
Tetra Tech. 1999a. Record of Telephone Conversation
Regarding Sampler Costs. Between Amy Stephen,
Environmental Engineer, and Will Young, President
and Owner, ARI. August 9.
83
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Tetra Tech. 1999b. Record of Telephone Conversation Tetra Tech. 1999c. "Sediment Sampling Technologies
Regarding Delrin®. Between Eric Monschein, Data Evaluation Report." Prepared for ORD, EPA.
Environmental Scientist, and DuPont Technical October.
Support Staff. August 10.
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Appendix A
Developer's Claims for the
ARI Russian Peat Borer
This appendix was written to comment on ARI's recent
participation in the EPA SITE demonstration of the
Russian Peat Borer. First, ARI would like to extend its
thanks to the EPA and Tetra Tech for a job well done. As
a technology developer and business owner, ARI cannot
stress enough the importance of such verification programs
in its efforts to simplify current sediment sampling
methods. ARI hopes the information herein can help field
technicians choose a proper sediment sampler, understand
the demonstration sampling problems encountered, and be
aware of options available for use with the Russian Peat
Borer.
ARI constructs several sediment sampling devices that fall
into two basic groups: side-filling, chambered samplers
and end-filling, core tube samplers. Customers often ask
ARI to compare and contrast these two groups in order to
select the best sampler for a specific sampling scenario.
Below are some important points to consider when a
sediment sampler is chosen.
1. ARI Russian Peat Borer, a Side-Filling, Chambered
Sampler
Advantages
• Simple design: the ARI Russian Peat Borer
contains one moving part.
Quality of samples: the close-open-close design
produces uncompressed and undisturbed samples
with a quality rivaled only by freeze-coring
techniques.
Discrete point sampling: the sampler is capable of
recovering intact, consecutive core profiles to a
depth of 100 feet bss.
Versatility: the ARI Russian Peat Borer was the
only sampler participating in the demonstration to
collect samples in all areas and target depth
intervals identified in the demonstration plan.
The Russian Peat Borer has been successfully
used in wetlands, bogs, lakes, and estuaries.
History: the sampler has been used extensively for
detailed paleoecological analyses including
studies of microfossil sequencing, annual
laminations, and paleomagnetism.
Time: ARI Russian Peat Borer samples can be
recovered and sectioned in a fraction of the time
required for samples collected using end-filling,
core samplers. Collected material is available for
immediate inspection, sectioning, and archiving.
Cost: a complete ARI Russian Peat Borer is priced
competitively as compared to most core
Appendix A was written solely by ARI. The statements presented in this appendix represent the developer's point of view and summarize the
claims made by the developer regarding the ARI Russian Peat Borer. Publication of this material does not represent the EPA's approval or
endorsement of the statements made in this appendix; performance assessment and economic analysis results for the ARI Russian Peat Borer
are discussed in the body of this ITVR.
85
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2.
samplers meeting similar depth and volume
requirements.
• Portability: the ARI Russian Peat Borer is
lightweight, ergonomic, and suitable for one-
person operation on a small sampling platform.
Minimal training or support equipment is required
for its operation.
Disadvantages
• Sampler operation: the ARI Russian Peat Borer is
limited to deployment on extension rods to a
maximum depth of 100 feet bss.
• Cross-contamination: the sampler's cover plate
(fin) is exposed to sediments in various horizons
during deployment. Deposits near the cover plate
must be suspected of contamination and
discarded. However, the rest of the sample can
be used for analysis. Gross decontamination of
the sampler is required to reduce cross-
contamination between samples.
• Coupling and uncoupling extension rods: this
process may be difficult after the threaded
couplers are tightened by the twisting action of the
sampler in compact sediment.
ARI End-Filling, Core Samplers (Gravity Corers,
Percussion Corers, and Piston Corers)
Advantages
• The samplers allow transportation
preservation of intact core samples.
and
The samplers allow precise, incremental core
extruding and sectioning.
The samplers allow in vitro incubations to assess
biochemical oxygen demand, benthic carbon, and
methane and ammonia diagenesis.
• The samplers allow pressurized core squeezing
and pore water sampling.
Disadvantages
• Piston corers can recover discrete samples only
under certain conditions and with considerable
difficulty.
• Core shortening may occur. Inferior sample
quality and possible intermittent sampling may
lead to serious misinterpretations of sediment
stratification and contaminant concentrations.
• Sample smearing and swirling may occur as a
result of use of core catchers.
• Cross-contamination may occur, particularly
during core extrusion. Deposits near the core tube
wall must be suspected of contamination and
discarded.
• Expendables are costly.
During the demonstration, S2A2 presented several
interesting sampling problems because of its very compact
wetland deposits. Three intact, consecutive sediment
profiles were recovered in the 9- to 11-foot bss depth
interval before sampling was terminated because of partial
extension rod failure and excessive work requirements for
sampler deployment. Both of these problems were
associated with stress created by slide-hammering,
particularly upon retrieval of the sampler from compact
sediment.
ARI deep-water extension rods (see below) were
employed in all demonstration areas because they are
lightweight and ergonomic. They are moderately priced
and particularly well suited for intensive sampling at deep
sites. After three of five samples were recovered in the 9-
to 11 -foot bss depth interval in S2A2, ARI noticed that the
stainless-steel rivets used to fasten internal, threaded
bushings to the aluminum extensions began to distort and
Appendix A was written solely by ARI. The statements presented in this appendix represent the developer's point of view and summarize the
claims made by the developer regarding the ARI Russian Peat Borer. Publication of this material does not represent the EPA's approval or
endorsement of the statements made in this appendix; performance assessment and economic analysis results for the ARI Russian Peat Borer
are discussed in the body of this ITVR.
86
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dislodge because of excessive upward forces created by
the slide-hammer mechanism. Also, considerable twisting
force was applied to rotate the core tube 180 degrees (to
the closed position), which probably contributed to rivet
failure. The rivets were reset, and the rods performed well
at the remaining sampling sites. Use of ARI magnesium-
zirconium extension rods (see below) would be necessary
for intensive sampling of the compact deposits found in
S2A2.
Use of proper extension rods is a key element when
employing the ARI Russian Peat Borer, and care must be
taken when the rods are chosen. When sampling deep or
compact deposits, one should be prepared to pay a
premium price for extension rods that are designed to
endure such conditions. Heavy pounding with a slide-
hammer, particularly during retrieval, puts tremendous
stress on threaded couplers. Also, the clockwise turning
of the core tube in dense material requires considerable
force, thus tightening the threaded couplers. As a result,
uncoupling may require use of pipe and strap wrenches.
Listed below are several types of extension rods currently
available for deploying the ARI Russian Peat Borer.
1. ARI Standard Extension Rods
• Aluminum hollow bar construction:
2.5 centimeters (cm) in diameter with 7/8-inch-
diameter, stainless-steel, coarse-threaded couplers
• Standard lengths: 1.0 and 2.0 meters (m)
• Function and advantages: general sampling of
lakes, wetlands, and bogs at shallow depths;
suitable for moderately compact sediments
• Maximum sampling depth: 33 feet bss
• Cost: $45 per 1-m length
2. ARI Deep-Water Extension Rods
• Aluminum hollow bar construction: 4.2 cm in
diameter with 7/8-inch-diameter, stainless-steel,
coarse-threaded couplers
• Standard lengths: 1.0, 2.0, 3.0, and 6.0 m
• Function and advantages: deeper water
deployments; lightweight, buoyant, larger
diameter for easy turning without "T"-handle,
increased rigidity, suitable for moderate slide-
hammer deployments, suitable for moderately
compact sediments
• Maximum sampling depth: 67 feet bss
• Cost: $75 per 1-m length
3. ARI Magnesium-Zirconium Extension Rods
• Magnesium-zirconium hollow bar construction:
4.5 cm in diameter with machined, coarse-
threaded, acme-type couplers; rods couple
together in approximately four revolutions
• Standard length: 2.0m
• Function and advantages: deep water sampling,
suitable for heavy slide-hammer deployments,
cold weather sampling (through ice), suitable for
very compact sediments, suitable for extreme
duty; rigidity, easy coupling and uncoupling
• Maximum sampling depth: 100 feet bss
• Cost: $110 per 1-m length
Appendix A was written solely by ARI. The statements presented in this appendix represent the developer's point of view and summarize the
claims made by the developer regarding the ARI Russian Peat Borer. Publication of this material does not represent the EPA's approval or
endorsement of the statements made in this appendix; performance assessment and economic analysis results for the ARI Russian Peat Borer
are discussed in the body of this ITVR.
87
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Considerable work was required to recover samples in the
9- to 11-foot bss depth interval in S2A2. The slide-
hammer mechanism was undersized (10 Ib, 50 cm in
height) and insufficient for sampling the compact sediment
in this interval. Simple modifications, including
increasing the weight and height of the assembly, may aid
in driving and removing the sampler under similar
conditions. Winches and electric rotary hammers are
workable options but are unnecessary in most applications.
Soft, organic sediment encountered in S2A1 also presented
some interesting problems with respect to sampling the
water-sediment interface. TheARI Russian Peat Borer is
a side-filling, chambered-type sampler that mechanically
retains sediment in the core tube upon retrieval. A very
thin slot that is present between the cover plate and core
tube to allow free rotation of the core
tube may cause some leaking and washout of interface
samples. Of course, the best way to avoid this problem is
to deploy the sampler deeper and minimize collection of
water at the interface. An option derived from the
literature is installation of a watertight, rubber "wiper
seal" on the cover plate, which could reduce leaking.
Since 1986, ARI has been proud to be involved in
hundreds of sediment sampling projects in over
35 countries. Based on experience and good advice from
customers, ARI focuses on two matters with regard to
sediment samplers: simplicity and sample quality.
Considering the time and money spent on sample analyses,
it is clear that recovery of clean, uncompressed,
undisturbed sediment samples is essential to any
investigation using sediment for depositional and
historical reconstruction.
Appendix A was written solely by ARI. The statements presented in this appendix represent the developer's point of view and summarize the
claims made by the developer regarding the ARI Russian Peat Borer. Publication of this material does not represent the EPA's approval or
endorsement of the statements made in this appendix; performance assessment and economic analysis results for the ARI Russian Peat Borer
are discussed in the body of this ITVR.
-------
Appendix B
Performance and Cost of the Ekman Grab
The EPA conducted a demonstration of an innovative
sediment sampler known as the Russian Peat Borer, a core
sampler designed and fabricated by ARI of Lemhi, Idaho.
The demonstration was conducted under the EPA SITE
Program at two sites during the last week of April and first
week of May 1999. The purpose of this demonstration
was to obtain reliable performance and cost data on the
Russian Peat Borer in order to (1) achieve a better
understanding of the sampler's capabilities relative to
conventional sediment samplers and (2) provide an
opportunity for the sampler to enter the marketplace and
compete with conventional samplers without long delays.
In addition to the Russian Peat Borer and the reference
samplers, a conventional grab sampler was included in the
demonstration because grab samplers are commonly used
to collect surficial sediment in order to assess the
horizontal distribution of sediment characteristics. The
Ekman Grab, a commonly used sampler, was chosen for
the demonstration. Performance and cost data collected
for the Ekman Grab are not intended to be compared to
those for the Russian Peat Borer but rather are presented
in this appendix as supplemental information.
Specifically, this appendix describes the Ekman Grab that
was demonstrated (Section B.I), two demonstration sites
(Section B.2), demonstration approach (Section B.3),
performance of the Ekman Grab (Section B.4), and
references used to prepare this appendix (Section B.5).
B.I Description of the Ekman Grab
The Ekman Grab is a "box" sampler whose bottom end
collects sediment as the sampler penetrates the sediment.
The sampler is designed to collect samples of soft, finely
divided sediment that is free of vegetation, stones, and
other coarse debris. A technical description, general
operating procedures, and advantages and limitations of
the Ekman Grab are presented below.
B. 1.1 Sampler Description
Components of the Ekman Grab selected for the
demonstration included (1) two stainless-steel scoops; (2)
two stainless-steel springs attached to four scoop buttons;
(3) two stainless-steel scoop cables; (4) a stainless-steel
messenger; (5) a 3/16-inch-diameter, braided, polyester
line or 5-foot-long, galvanized-steel extension handle; (6)
a release mechanism consisting of a stainless-steel strike
pad and two stainless-steel pins; and (7) two hinged,
overlapping, stainless-steel lids (see Figure B-l).
Optional accessories include a 10-foot-long extension
handle and weights that can be fastened to either side of
the Ekman Grab. Top screens designed to prevent
sediment from escaping from the top of the Ekman Grab
are also available.
In water depths up to 10 feet, the Ekman Grab can be
manually deployed using the extension handle. In water
up to 60 feet deep and with low velocity, the sampler can
be deployed using the polyester line and messenger.
During sampler deployment, the two lids at the top of the
sampler open to allow water to pass through the sampler
in order to minimize bow wave formation, thus minimizing
disturbance of the sediment. Once the sampler is deployed
to the desired sampling location, the release mechanism is
actuated using the extension handle or the messenger on
the polyester line. Once actuated, the mechanism releases
the scoop cables, allowing the springs to close the scoops
and collect a sediment sample. During
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Scoop cable
Messenger
3/16-inch-diameter,
braided line
Lids
Scoop
Spring
Scoop button
Figure B-1. Ekman Grab.
sampler retrieval, the lids automatically close to minimize
sample washout.
The Ekman Grab is available in many sizes; however, for
this demonstration, the standard-size Ekman Grab was
chosen because of its ability to collect a sample volume
that met the demonstration objectives while generating
relatively little IDW. The standard-size Ekman Grab
contains a 6-inch-long, 6-inch-wide, and 6-inch-high
sample chamber with a volume of 3,460 mL. The area
below the chamber created by the two scoops when closed
constitutes an additional 630 mL. The fully assembled
Ekman Grab, not including the extension handle, weighs
about 10 Ib.
B. 1.2 General Operating Procedures
The Ekman Grab can be manually operated by one person
from a sampling platform or while wading in shallow
water. Prior to sampler deployment, each of the two
springs must be manually attached to the two scoop
buttons on either side of the sampler. Also, before the
Ekman Grab is lowered into the water, each scoop cable
must be manually hooked to one of the two pins in order
to hold the sampler in an open position. During and after
sampler preparation for deployment, care must be used to
avoid catching any body parts such as fingers or feet
between the scoops.
The sampler can be manually lowered to the sediment
surface using the extension handle or polyester line. In
either case, the speed of sampler deployment needs to be
controlled in order to avoid bow wave formation. If the
polyester line is used, the sampler should not be allowed
to fall freely for a significant distance. The sampler
should be manually lowered to the sediment surface and
then slightly raised before it is released; this procedure
allows the weight of the sampler to control sediment
penetration.
Once the sampler penetrates the sediment, the release
mechanism is actuated using the extension handle or by
placing the messenger on the polyester line and allowing
it to slide down the line to the strike pad. When the strike
pad is depressed, the pins are lowered, the scoop cables
are released, and the springs close the scoops to collect a
sediment sample. After the scoops are fully closed, the
Ekman Grab should be raised slowly from the sediment
and then raised steadily to the water surface.
There are several ways to process grab samples collected
using the Ekman Grab. Upon removal of the sampler from
the water, the grab sample may be discharged into a bucket
or bowl. Another way of processing the sample is to keep
the scoops closed and open the lids on top of the sampler;
then small-diameter tubes can be inserted into the top
portion of the sampler to collect subsamples.
B.1.3 Advantages and Limitations
An advantage of the Ekman Grab is that it is easy to
operate, requiring minimal skills and training. Sampler
assembly and collection procedures can be learned in the
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field with a few practice attempts. In addition, a written
SOP typically accompanies the sampler when it is
procured. The sampler can be operated by one person in
shallow (wading) and deep water depths because of its
lightness (10 Ib, not including the weight of the extension
handle). Sampler operation is simple because the sampler
does not require complete disassembly and reassembly
after each sampling attempt. Only the scoops have to be
opened in order to retrieve the sediment sample. The
sampler also requires no support equipment.
Another advantage of the Ekman Grab is that during
sampler deployment, the two lids at the top of the sampler
open to allow water to pass through the sampler and to
minimize the bow wave formation, thus minimizing
disturbance of the sediment. The sampler's scoops are
designed to overlap in the closed position in order to
minimize sample loss during sampler retrieval. In
addition, the release mechanism and pivoting scoops are
designed to minimize sediment disturbance when a sample
is collected.
A limitation of the Ekman Grab is that because of its
lightness, the sampler may not be able to penetrate
consolidated sediment if the sampler is deployed by
gravity penetration with a polyester line. In addition,
small stones or vegetation may become caught between the
scoops, causing the scoops to remain in the open position
during sampler retrieval, resulting in partial or complete
loss of the sample. Also, during and after sampler
preparation for deployment, care must be used to avoid
catching any body parts such as fingers or feet between the
scoops.
B.2 Description of the Demonstration Sites
The Ekman Grab was demonstrated at two sites in EPA
Regions 1 and 5. At the Region 1 site, Ekman Grab
sampling was conducted in one sampling area (S2A1) that
represented lake conditions and had a water depth of about
18 feet. At the Region 5 site, Ekman Grab sampling was
conducted in two areas. One area (S1A1) was in a river
mouth and had a water depth of about 5 to 6 feet. The
other area (S1A2) was in a freshwater bay along a river
and had a water depth of about 2 feet.
Additional information on demonstration site and area
characteristics and the sampling platforms used is
provided in Chapter 3 of the ITVR.
B.3 Demonstration Approach
This section presents the demonstration objectives, design,
and field sampling and measurement procedures, for the
Ekman Grab.
B. 3.1 Demonstration Objectives
The demonstration had both primary and secondary
objectives. Primary objectives were critical to the
technology evaluation and were intended to produce
quantitative results regarding technology performance.
Secondary obj ectives provided information that was useful
but did not necessarily produce quantitative results
regarding technology performance.
As stated in Section 4.1 of the ITVR, the primary
objectives for the demonstration were as follows:
PI. Evaluate whether the sampler can consistently
collect a specified volume of sediment
P2. Determine whether the sampler can consistently
collect samples in a specified depth interval
P3. Assess the sampler's ability to collect multiple
samples with consistent physical or chemical
characteristics, or both, from a homogenous layer of
sediment
P4. Evaluate whether the sampler can collect a
representative sample from a "clean" sediment layer
that is below a contaminated sediment layer
P5. Assess the sampler's ability to be adequately
decontaminated between sampling areas
P6. Measure the time required for each activity
associated with sample collection (sampler setup,
sample collection, sampler disassembly, and
sampler decontamination)
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P7. Estimate costs associated with sample collection
activities (sampler, labor, IDW disposal, and support
equipment costs)
Primary objective P4 was not addressed for the Ekman
Grab because this sampler is not designed in such a way
that it can be evaluated under P4. The secondary
objectives for the demonstration were as follows:
SI. Document the skills and training required to
properly operate the sampler
S2. Evaluate the sampler's ability to collect samples
under a variety of site conditions
S3. Assess the sampler's ability to collect an
undisturbed sample
S4. Evaluate the sampler's durability based on its
materials of construction and engineering design
S5. Document the availability of the sampler and spare
parts
B.3.2 Demonstration Design
Samples were collected using the Ekman Grab to obtain
supplemental performance and cost data. Table B-l
summarizes the demonstration design for collecting grab
samples. Sediment samples were collected using the
Ekman Grab only in the 0- to 4-inch bss depth intervals in
S1A1, S1A2, and S2A1. The Ekman Grab is designed to
collect surficial sediment samples in areas that are largely
free of vegetation. According to the findings of the
predemonstration investigation, most of the surficial
material in S2A2 was composed of decomposed leaves and
wood chips. Therefore, grab samples were not collected
in S2A2. The approach for addressing the primary
objectives using the Ekman Grab was generally the same
as that for the Russian Peat Borer presented in Section 4.2
of the ITVR. Differences in the approach for the Ekman
Grab are discussed below.
• Primary objective PI was generally addressed as
described for the Russian Peat Borer. The volume of
sediment collected was noted. However, measurement
of core lengths was not appropriate for the Ekman
Grab and was not conducted.
Table B-1. Ekman Grab Demonstration Design
Target Sampling
Depth Interval
Demonstration Area (inches bss)
S1A1 (river mouth) Oto4
S1 A2 (freshwater bay) 0 to 4
S2A1 (lake) 0 to 4
P1
P2
P3
P6
P1
P2
P5
P6
P7
P1
P2
P3
P5
P6
P7
Primary Objective
Volume
Depth interval
Consistent samples from a homogenous layer
Sample collection time
Volume
Depth interval
Decontamination
Sample collection time
Cost
Volume
Depth interval
Consistent samples from a homogenous layer
Decontamination
Sample collection time
Cost
Sampling Volume Required
Parameter (Matrix) per Sample
PSD and volume
(sediment)
PCBs and volume
(sediment)
PCBs (final rinsate)
Arsenic, PSD, and
volume (sediment)
Arsenic (final
rinsate)
250 ml
250 ml
1 L
250 ml
500ml
Notes:
bss =
L
ml
PCB =
PSD =
Below sediment surface
Liter
Milliliter
Polychlorinated biphenyl
Particle size distribution
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• Primary objective P2 was generally addressed as
described for the Russian Peat Borer. The volume of
sediment collected and the approximate sampler
penetration depth were noted. However, measurement
of core lengths was not appropriate for the Ekman
Grab and was not conducted.
• Primary objective P3 was addressed as described for
the Russian Peat Borer except that sample collection
was limited to the 0- to 4-inch bss depth intervals in
SlAlandS2Al.
• Primary objectives P5, P6, and P7 were addressed in
the 0- to 4-inch bss depth intervals in S1A2 and S2A1
as described for the Russian Peat Borer. P6 was also
addressed in the 0- to 4-inch bss depth interval in
S1A1.
Secondary objectives SI, S2, and S3 were addressed for
the Ekman Grab in all three demonstration areas because
no additional sampling was required to address them.
Secondary objectives S4 and S5 were not area-dependent;
they were addressed for the Ekman Grab based on
information provided by the sampling technician as well
as observations of sampler performance during the
demonstration. The approach for addressing each
secondary objective was the same as that for the Russian
Peat Borer presented in Section 4.2 of the ITVR.
B. 3.3 Field Sampling and Measurement
Procedures
Using the Ekman Grab, sediment samples were collected
in S1A1 for PSD analysis, in S1A2 for PCB analysis, and
in S2A1 for PSD and arsenic analyses. The sampling
locations in each of these demonstration areas are
presented in Figure B-2. Additional information on these
areas and the sampling platforms used is presented in
Chapter 3 of the ITVR. Table B-2 lists the target sampling
depth interval, planned numbers of investigative samples,
and analytical parameters for each demonstration area and
provides the rationale for their selection. In general, the
rationale for choosing the number of samples to be
collected in each area was based on the objectives to be
addressed, the analyses to be conducted to address one or
more objectives, the time required to collect samples, and
the cost of each analysis. When five samples were to be
collected in a sampling area, samples were collected in the
four corners and center of the area; when ten samples were
to be collected in a sampling area, the additional five
samples were collected at locations randomly distributed
throughout the area.
Many of the field measurements made to support the
primary objectives were simple, standard measurements
and do not require additional explanation. These
measurements included the volume of IDW generated,
number of sampling technicians, number of sampling
attempts per location, volume of sediment collected, time
required for sample collection activities, sampling area
grid size, and water velocity. However, several field
measurements were made to address demonstration-
specific requirements, and additional explanation of these
measurements is warranted to enhance understanding of
the sampler performance results presented in Section B.4.
Information regarding sample preparation, sampler
decontamination, and measurement of the time required to
conduct sample collection activities (sampler setup,
sample collection, sampler disassembly, and sampler
decontamination) is presented in Section 4.3 of the ITVR.
The depth of Ekman Grab deployment was measured after
the sampling technician had lowered the sampler to the
sediment surface. Once the technician identified the
location of the sediment surface using the sampler, a mark
was made on the extension handle or polyester line with
reference to a fixed point (the boat side or floor). For
extension handle applications, another mark was made
higher on the extension handle indicating the depth to
which the sampler should be pushed in order to collect a
sediment sample in the target sampling depth interval.
The sampler was pushed to this depth, and a sample was
collected. For polyester line applications, the depth of
sampler deployment was dictated by gravity penetration.
Once the sampling technician had lowered the sampler to
the sediment surface using the polyester line, he allowed
the sampler to penetrate the sediment by its own weight.
The depth of sampler deployment was then measured by
making another mark on the polyester line with reference
to the fixed point.
Field and laboratory QC checks for the demonstration are
discussed in Sections 4.3 and 4.4 of the ITVR,
respectively. Section 4.4 of the ITVR also presents the
laboratory sample preparation and analysis methods.
Table B-3 identifies the planned numbers of sediment and
equipment rinsate samples. Acceptance criteria and
associated corrective actions for field QC checks are
93
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S1A1 (river mouth)
Target sampling depth interval:
0 to 4 inches below sediment surface
S1A2 (freshwater bay)
Target sampling depth interval:
0 to 4 inches below sediment surface
S2A1 (lake)
Target sampling depth interval:
0 to 4 inches below sediment surface
2
3
4
5
"V
1
2
3
4
5
X
*
*
A B
o
o
•
10 feet
C
O
*
*
D E
o
o
L— infect -J
1
1
1
1
-10 feet.
A
A
A
A
A
A
A
A
A
A
I
1
Legend
O Polychlorinated biphenyls
• Particle size distribution
A Arsenic
^ Arsenic and particle size distribution
^- Flow direction
Note: Approximate scale: 1 inch = 1,200 feet
Figure B-2. Sampling locations for Ekman Grab demonstration.
94
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Table B-2. Rationale for Sampling Approach
Demonstration Area
Target Sampling Number of
Depth Interval Investigative Samples3
(inches bss) (Analytical Parameter)
Matrix
Rationale
S1A1 (river mouth) Oto4
S1A2 (freshwater bay) 0 to 4
S2A1 (lake) 0 to 4
5 (PSD) Sediment Determine whether an Ekman Grab could collect
multiple samples from a homogenous layer of sediment
(primary objective P3) with consistent characteristics
5 (PCBs) Sediment Determine whether an Ekman Grab could be adequately
decontaminated (primary objective P5)
1 (PCBs) Equipment Determine whether an Ekman Grab could be adequately
rinsate decontaminated (primary objective P5)
10 (Arsenic) Sediment Determine whether an Ekman Grab could collect
5 (PSD) multiple samples from a homogenous layer of sediment
(primary objective P3) with consistent characteristics
1 (Arsenic) Equipment Determine whether an Ekman Grab could be adequately
rinsate decontaminated (primary objective P5)
Notes:
bss =
PCB =
PSD =
Below sediment surface
Polychlorinated biphenyl
Particle size distribution
The number of investigative samples varied depending on the analytical parameters and the objectives addressed in each demonstration area.
Ten investigative samples were collected and analyzed for arsenic to address primary objective P3. However, only five investigative samples were
collected and analyzed for PSD to address primary objective P3 because the variability associated with PSD is less than that associated with
arsenic concentrations.
presented in the demonstration plan (EPA 1999). A
summary discussion of whether the field and laboratory
QC procedures generated scientifically valid and legally
defensible data that met the demonstration objectives is
presented in Section B.4.3.
B.4 Performance of the Ekman Grab
This section describes the performance of the Ekman Grab
based on the primary objectives (Section B.4.1) and
secondary objectives (Section B.4.2); this section also
discusses the data quality of the demonstration results for
the Ekman Grab (Section B.4.3).
B.4.1 Primary Objectives
This section discusses the performance results for the
Ekman Grab based on the primary objectives specified in
Section B.3.1. To address these primary objectives,
samples were collected in three different areas: (1) S1A1,
a river mouth; (2) S1A2, a small, freshwater bay; and
(3) S2A1, a lake. Samples were collected only in the 0- to
4-inch bss depth interval in these areas because the Ekman
Grab is capable of collecting surficial sediment only. The
numbers of investigative and QC samples collected in each
area, sediment sample volumes required, and sample
analytical parameters are presented in Table B-3.
During the demonstration, because the water depth in
S1A1 and S2A1 exceeded the length of the extension
handle (5 feet), the sampling technician deployed the
Ekman Grab by gravity penetration using a polyester line.
In S1A2, where the water depth was about 2 feet, the
sampler was deployed with the 5-foot-long extension
handle. The sampling technician was provided an
opportunity to practice sample collection at each
demonstration area until he felt confident enough to
initiate demonstration sampling.
The demonstration results for the Ekman Grab under
primary objectives PI and P2 were evaluated using the
Wilk-Shapiro test to determine whether the results were
normally distributed. Because most of the data sets were
not normally distributed, the Wilk-Shapiro test was used
in an attempt to evaluate whether the results followed a
lognormal distribution. The test revealed that the results
95
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Table B-3. Ekman Grab Sample Matrix
Demonstration
Area
S1A1
(river mouth)
S1A2
(freshwater
bay)
S2A1
(lake)
Target Sampling
Depth Interval
(inches bss)
Oto4
Oto4
Oto4
Analytical
Parameter
PSD
PCBs
Arsenic
PSD
Investi-
gative
Samples
5
5
10
5
Sediment
MS/MSD
Samples3
NA
1
2
NA
Samples
Field
Triplicate
Samples"
1
2
3
1
Laboratory
Analyses
7
11
20
7
Equipment Rinsate Samples
Equipment
Rinsate
Samples
NA
1
1
NA
Field
Duplicate
Samples0
NA
1
1
NA
Laboratory
Analyses
0
2
2
0
Notes:
bss =
MS/MSD =
NA
PCB
PSD
Below sediment surface
Matrix spike/matrix spike duplicate
Not applicable
Polychlorinated biphenyl
Particle size distribution
MS/MSD samples were collected for PCB and arsenic analyses and were designated in the field. MS/MSD samples were not collected for
equipment rinsate samples because the additional volume required for the analysis may have diluted any contamination present to concentrations
below laboratory detection limits. Sediment MS/MSD samples did not require additional sample volume.
Field triplicate sediment samples were collected by filling three sample containers with homogenized sediment. A sufficient volume of sediment
for field triplicate samples was collected as described in the approach for addressing primary objective P1 in Section 4.2 of the innovative
technology verification report. Field triplicate samples were submitted for analysis as blind samples.
Field duplicate equipment rinsate samples were collected by filling one additional container for PCB or arsenic analysis. Field duplicate samples
were submitted for analysis as blind samples.
either were not lognormally distributed or could not be
tested for lognormality because the results contained
values equal to zero. For these reasons, the Student's
t-test, a parametric test, was not used to perform the
hypothesis testing; the Wilcoxon signed rank test, a
nonparametric test, was used as an alternative to the
Student's t-test. As described in Section 6.1 of the ITVR,
Statistix® was used to perform statistical evaluations of the
demonstration results (Analytical Software 1996).
Appendix C provides details on the statistical methods
used for data evaluation.
B.4.1.1 Ability to Consistently Collect a Specified
Volume of Sediment
Primary objective PI involved evaluating the Ekman
Grab's ability to consistently collect a specified volume of
sediment. This objective was addressed by comparing
(1) the actual number of sampling attempts required to
collect a specified volume of sediment to the expected
number of attempts (rounded to the nearest higher integer)
at each sampling location and (2) the actual volume of
sediment collected in each attempt to the calculated
sampler volume (design volume). The expected number of
attempts was determined by dividing the specified sample
volume by the design volume. The results of these
comparisons are summarized below.
Number of Sampling Attempts Required
Tables B-4 and B-5 present the expected and actual
number of sampling attempts for the Ekman Grab in S1A1
and S1A2 and in S2A1, respectively. Initially, the
Wilcoxon signed rank test was used to determine whether
the difference between the expected and actual number of
attempts was statistically significant. However, in two of
the three areas, there were too few locations where the
expected number of attempts differed from the actual
number to perform the test.
96
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Table B-4. Comparison of Expected and Actual Number of Sampling Attempts for Ekman Grab at Site 1
Location
1A
1E
3C
5A
5E
Total
Number of Attempts in S1A1
Expected
1
1
1
1
1
5
(River Mouth)
Actual
4
1
1
1
2
9
Number of Attempts
Expected
1
1
1
1
1
5
in S1A2 (Freshwater Bay)
Actual
1
1
1
1
1
5
Table B-5. Comparison of Expected and Actual Number of
Sampling Attempts for Ekman Grab in S2A1 (Lake)
Number of Attempts in S2A1
Location
1A
1B
1E
2A
2C
2D
2E
3A
3B
3E
Total
Expected
1
1
1
1
1
1
1
1
1
1
10
Actual
1
2
2
1
1
1
2
1
1
1
13
Regarding the number of sampling attempts required to
collect the specified volume, the Ekman Grab performed
well in all three areas. As shown in Tables B-4 and B-5,
the actual number of attempts equaled the expected
number of attempts at 15 of 20 locations. In S1A1,
Location 1A was the only location where the actual
number of attempts (four) exceeded the expected number
(one) by more than one attempt. In two of the four
attempts at Location 1A, only one scoop was closed after
the messenger was released, and the sediment sample was
lost through the open scoop.
Much of the sampler's overall success in terms of number
of sampling attempts required can be attributed to the
design volume for the Ekman Grab (about 2,900 mL for
the 0- to 4-inch bss depth interval, including the volume of
the scoops) being much greater than the specified sediment
sample volumes, which ranged from 250 to 1,000 mL.
Consequently, a sampling attempt with low
recovery compared to the design volume could still collect
the specified volume of sediment.
Volume of Sediment Collected
The volume of sediment collected by the Ekman Grab in
each sampling attempt was divided by the corresponding
design volume, and the resulting ratio was multiplied by
100 to estimate the PSR. The RSD of the PSRs was
calculated to evaluate the ability of the Ekman Grab to
consistently collect a specified volume of sediment; if the
sampler were to consistently recover an identical volume
of sediment in every attempt, the RSD would equal zero.
Both PSR and RSD results should be considered to
properly evaluate the sampler's performance because a
low RSD, which indicates that the sampler's performance
was consistent, may be based on consistently low PSRs.
Table B-6 presents the PSR summary statistics (range,
mean, and RSD) for all three areas. Figure B-3 presents
PSRs for the Ekman Grab in S1A1, S1A2, and S2A1.
The Ekman Grab performed well in S1A2 but had
difficulty in S1A1 and S2A1. As shown in Table B-6, for
S1A2, PSRs ranged from 100 to 145 with a mean PSR of
127. The RSD of the PSRs for S1A2 (13 percent)
compares favorably to the 30 percent RSD guideline
discussed in Section 6.1.1 of the ITVR. On the other
hand, as shown in Figure B-3, 5 of 9 attempts in S1A1 and
3 of 13 attempts in S2A1 had PSRs in the 0 to 20 range.
These low recoveries were due to the failure of one or both
scoops to close after the messenger was released or to
incomplete sampler penetration of the specified depth
interval. Unlike S1A2, where the sampler was deployed
with an extension handle, the sampler was deployed by
gravity penetration using a polyester line in S1A1 and
S2A1. As a result, the sampling technician had relatively
poor control of the depth of sampler penetration. As
97
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Table B-6. Percent Sample Recovery Summary Statistics for Ekman Grab
Demonstration Area Actual Number of Attempts PSR Range3
Mean PSR
RSD (%)
S1A1 (river mouth)
S1A2 (freshwater bay)
S2A1 (lake)
9
5
13
Oto40
100 to 145
Oto71
16
127
38
103
13
65
Notes:
PSR = Percent sample recovery
RSD = Relative standard deviation
a PSRs exceeding 100 resulted from pushing the sampler beyond the specified depth interval because of difficulty in accurately assessing the
location of the sediment, the volumetric measurement error associated with the presence of void spaces when the sediment was transferred to
a graduated container, or both.
shown in Table B-6, RSDs of 103 and 65 percent that
exceeded the 30 percent RSD guideline were observed for
S1A1 and S2A1, respectively, indicating that the Ekman
Grab did not consistently collect its design volume.
In summary, the Ekman Grab performed well with regard
to the number of attempts required, but did not perform
well with regard to consistently collecting its design
volume. The actual number of attempts equaled the
expected number of attempts at 15 of 20 locations.
However, for S1A1 and S2A1, low mean PSRs (16 and 38,
respectively) and high RSDs (103 and 65 percent,
respectively) were observed, indicating low and
inconsistent recoveries. For S1A2, a much lower RSD
(13 percent) was observed. In addition, all the PSRs for
sampling attempts in S1A2 were 100 or greater.
B.4.1.2 Ability to Consistently Collect Sediment in a
Specified Depth Interval
Primary objective P2 involved evaluating the Ekman
Grab's ability to consistently collect sediment in a
specified depth interval by comparing actual and target
core lengths for each attempt. The Ekman Grab does not
collect a core, but to facilitate its comparison to the other
samplers, the actual depth interval sampled in a given
attempt was calculated based on the Ekman Grab's design
volume and the volume of sediment collected.
The Ekman Grab's box chamber is 6 inches tall and can
hold about 580 mL of sediment per inch. The scoop
chamber has a triangular cross section; is approximately
1.5 inches tall in the middle; and can hold about 105 mL
in the bottom one-third, about 210 mL in the middle
one-third, and about 315 mL in the top one-third, which
amounts to a total volume of about 630 mL. Therefore, if
the Ekman Grab collected 2,100 mL of sediment in a given
attempt, the sampling depth interval is 0 to 4 inches bss
because the 1.5-inch-tall scoop chamber holds 630 mL,
and the remaining 1,470 mL would fill approximately
2.5 inches of the box chamber at 580 mL per inch.
However, the height of the scoop chamber was not
accounted for during demonstration sampling, and the
sampling technician tried to push the box chamber to a
depth of 4 inches bss in each attempt. Consequently, the
target sediment thickness in each area was actually
5.5 inches instead of 4 inches, which corresponds to a
sample volume of approximately 2,900 mL.
Table B-7 presents the number of attempts in which the
actual sediment thickness equaled the target sediment
thickness, target sediment thicknesses, and mean actual
sediment thicknesses. Initially, the Wilcoxon signed rank
test was to be used to determine whether differences
between the actual and target sediment thicknesses were
statistically significant. However, the Wilcoxon signed
rank test revealed that the test results for many of the
primary objective P2 data sets were inconsistent with the
conclusions reached in comparing the actual and target
sediment thicknesses for the reasons described in
Section 6.1 of the ITVR. Therefore, P2 was addressed by
evaluating (1) the number of attempts in which the actual
sediment thickness equaled the target sediment thickness
and (2) the difference between the target sediment
thickness and the mean actual sediment thickness.
The Ekman Grab did not perform well in any of the three
areas. As shown in Table B-7, sediment thicknesses
98
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S1A1, 0-to 4-inch bss depth interval
I Total number of attempts: 9
Oto20 >20to40 >40to60 >60to80 >80to100 >100
Percent sampterecovery
Figure B-3. Percent sample recoveries for Ekman Grab in S1A1
(river mouth), S1A2 (freshwater bay), and S2A1 (lake).
S1A2, 0-to 4-inch bss depth interval
Total number of attempts: 5
Oto20 >20to40 >40to60 >60to80 >80to100
Percent sample recovery
>100
S2A1, 0- to 4-inch bss depth interval
Total number of attempts: 13
Oto20 >20to40 >40to60 >60to80 >80to100 >100
Percent sample recovery
Notes:
bss = Below sediment surface
Percent sample recoveries exceeding 100 resulted from pushing the
sampler beyond the specified depth interval because of difficulty in
accurately assessing the location of the sediment surface, the volumetric
measurement error associated with the presence of void spaces when
the sediment was transferred to a graduated container, or both.
99
-------
collected by the Ekman Grab equaled the target sediment
thicknesses in only 1 of 27 attempts. Attempts in S1A1
and S2A1 generally had low recoveries (0 to 40 percent in
S1A1 and 0 to 71 percent in S2A1), which resulted in low
mean actual sediment thicknesses of 1.0 and 2.5 inches,
respectively. In S1A2, the mean actual sedimentthickness
of 6.5 inches exceeded the target sediment thickness of
5.5 inches. Although the Ekman Grab sampled the entire
target sediment thickness in all 5 attempts, in 4 of the
5 attempts in S1A2, the actual sediment thickness
exceeded the target sediment thickness by 1 inch on
average. Because of the nature of the sampler, the portion
of the sediment sample corresponding to the 5.5- to
6.5-inch bss depth interval could not be separated from
that corresponding to the target depth interval. Based on
demonstration results, the Ekman Grab did not
demonstrate an ability to consistently collect sediment in
the specified depth interval.
B.4.1.3 Ability to Collect Multiple Samples with
Consistent Physical or Chemical
Characteristics, or Both, from a Homogenous
Layer of Sediment
Primary objective P3 involved evaluating the Ekman
Grab's ability to collect multiple samples with consistent
physical or chemical characteristics, or both, from a
homogenous layer of sediment. This objective was
addressed by calculating the RSD values for the S1A1 and
S2A1 sample analytical results. Based on the
predemonstration investigation results, the 0- to 4-inch bss
depth intervals in these areas were determined to be
homogenous in terms of their physical characteristics, and
the S2A1 depth interval was determined to be homogenous
in terms of its chemical characteristics.
Figure B-4 presents the Ekman Grab sample analytical
results for S1A1 and S2A1. Although no outliers were
found in the arsenic and PSD results for the samples
collected by the Ekman Grab, the sampler was evaluated
only on its ability to collect multiple samples with
consistent physical characteristics; this approach was used
to be consistent with the evaluations of the innovative and
reference samplers discussed in Sections 6.1.3 and 7.1.3,
respectively. Also, the Ekman Grab sample arsenic
concentrations for S2A1 varied over a wide range (53 to
240 mg/kg), indicating that the area may not be chemically
homogenous despite the lack of statistical outliers. The
100
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Table B-7. Comparison of Target and Actual Sediment Thickness Data for Ekman Grab
Demonstration Area
Number of Attempts in Which Actual Sediment
Thickness Equaled Target Sediment
Thickness/Total Attempts
Target Sediment Thickness
(inches)
Mean Actual Sediment
Thickness (inches)
S1A1 (river mouth)
S1A2 (freshwater bay)
S2A1 (lake)
0/9
1/5
0/13
5.5
5.5
5.5
1.0
6.5
2.5
RSDs were calculated based on the PSD analytical results
for all locations sampled in S1A1 and S2A1.
Table B-8 presents PSD summary statistics (range, mean,
and RSD) calculated for the Ekman Grab samples and
field triplicates relevantto primary objective P3. As stated
in Section 6.1.3 of the ITVR, RSDs calculated for the PSD
results were compared to the laboratory acceptance
criterion of 15 percent for field triplicates. When the RSD
for all samples was greater than 15 percent, it was
compared to the measured RSD for the field triplicates,
which were prepared by first homogenizing and then
subsampling the sediment collected in a given location and
area. An RSD for all samples that is less than the RSD for
field triplicates may be more attributable to the
laboratory's analytical procedure or the sample
homogenization procedure implemented in the field, or
both, for the sediment sampled than to the sampler's
ability to collect physically consistent samples. However,
PSD parameters with means less than 10 percent were not
evaluated in this manner because at low levels, the
analytical method is not as precise; as a result, it will
generate high RSD values and may not reveal whether
multiple samples with consistent physical characteristics
have been collected.
As shown in Table B-8, the RSDs for silt results for both
S1A1 and S2A1 were below the 15 percent laboratory
acceptance criterion. The RSD for the sand result for
S1A1 was also below the laboratory acceptance criterion,
but the sand result RSD for S2A1 (17 percent) was
2 percentage points above the laboratory acceptance
criterion and above the measured RSD for field triplicates
(8 percent). Therefore, some of the variation in the sand
results may be attributable to the Ekman Grab's ability to
collect samples with consistent physical characteristics.
However, the variation in the sand results for S2A1 was
not considered to be significant because it was only
2 percentage points greater than the laboratory acceptance
criterion. The mean clay results for samples collected in
both S1A1 and S2A1 were less than 10 percent and were
not evaluated using the criterion. However, the clay
results fell in a tight range (0 to 2 and 0 to 5 percent in
S1A1 and S2A1, respectively).
In summary, the Ekman Grab met primary objective P3
criteria except for a 2 percentage point exceedance in the
RSD for sand results for S2A1. Therefore, it was
concluded that the Ekman Grab was able to collect
multiple samples with consistent physical characteristics.
B.4.1.4 Ability to be Adequately Decontaminated
Primary objective P5 involved evaluating the Ekman
Grab's ability to be adequately decontaminated. This
objective was addressed by collecting equipment rinsate
samples after sampler decontamination activities in S1A2
and S2A1. These areas were chosen because they
contained high concentrations of PCBs and arsenic,
respectively. If the Ekman Grab were adequately
decontaminated, the analytical results for the equipment
rinsate samples would be below the laboratory's reporting
limits. To ensure that the water used to decontaminate the
sampler was not contaminated, decontamination water
blanks were also analyzed. Contaminant concentrations in
both the equipment rinsate samples and decontamination
water blanks were below the laboratory reporting limits for
PCBs (1 part per billion) and arsenic (10 parts per billion).
Thus, the Ekman Grab demonstrated the ability to be
adequately decontaminated.
B.4.1.5 Time Requirements for Sample Collection
Activities
Primary objective P6 involved evaluating the Ekman
Grab's time requirements for sample collection activities.
These requirements were evaluated in S1A1, S1A2, and
S2A1. One technician conducted sampler setup, sample
101
-------
S1A1
Location 1A
Sand: 83%
Silt: 17%
Clay: 0%
Location 5A
Sand: 85%
Silt: 15%
Clay: 0%
Location 3C
Sand: 84%
Silt: 15%
Clay: 0%
Location 1 E
Sand: 84%
Silt: 14%
Clay: 2%
Location 5E
Sand: 86%
Silt: 13%
Clay: 1%
S2A1
Location 1A
Arsenic: 110 mg/kg
Sand: 39%
Silt: 55%
Clay: 5%
Location 2A
Arsenic: 240 mg/kg
Location 3A
Arsenic: 53 mg/kg
Sand: 52%
Silt: 46%
Clay: 0%
Location 1 B
Arsenic: 87 mg/kg
Location 3B
Arsenic: 110 mg/kg
Location 2C
Arsenic: 110 mg/kg
Sand: 42%
Silt: 53%
Clay: 4%
Location 2D
Arsenic: 160 mg/kg
Location 1 E
Arsenic: 200 mg/kg
Sand: 33%
Silt: 57%
Clay: 2%
Location 2E
Arsenic: 130 mg/kg
Location 3E
Arsenic: 89 mg/kg
Sand: 48%
Silt: 51%
Clay: 0%
Notes:
mg/kg = Milligram per kilogram
The particle size distribution results for a given sample may not total 100 percent because of rounding or because some sediment did not pass through
a U.S. Standard No. 4 sieve and was classified as gravel rather than sand, silt, or clay.
Figure B-4. Ekman Grab sample analytical results for S1A1 (river mouth) and S2A1 (lake).
102
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Table B-8. Particle Size Distribution Summary Statistics for Ekman Grab
Demonstration Area
S1A1 (river mouth)
S2A1 (lake)
Parameter
Sand
Silt
Clay
Sand
Silt
Clay
Number of
Samples
5
5
5
5
5
5
Range (%)
83 to 86
13 to 17
Oto2
33 to 52
46 to 57
Oto5
Mean (%)
84
15
1
43
53
2
RSD (%)
(All Samples)
1
10
128
17
8
104
RSD (%)
(Field Triplicates)
1
8
173
8
4
35
Note:
RSD = Relative standard deviation
collection, sampler disassembly, and sampler
decontamination in each of the three demonstration areas.
The amounts of time required to complete these activities
are shown in Table B-9. The time measured for sample
collection activities did not include the time taken for
mobilization, demobilization, and maneuvering the
sampling platforms to sampling locations because these
activities were not sampler-specific; they were either site-
or weather-related.
Sampler setup times for the Ekman Grab ranged from
1 minute in S1A1 and S2A1 to 4 minutes in S1A2. The
Ekman Grab was operated using a polyester line in S1A1
and S2A1 because the water depth was greater than the
length of the extension handle available during the
demonstration. In S2A1, the sampler arrived with the
polyester line used to lower the sampler already attached;
therefore, the setup time for S2A1 was estimated to be
equal to the setup time for S1A1. An extension handle
was used instead of the polyester line in S1A2, which
required additional sampler setup time.
Sample collection times for the Ekman Grab ranged from
8 to 40 minutes during the demonstration. Sample
collection required 0.5 to 2 minutes per attempt in S1A1
and S1A2 but 1.5 to 3.5 minutes per attempt in S2A1.
Additional time was required in S2A1 because it was the
first area sampled and because the water depth was
18 feet.
Sampler disassembly times for the Ekman Grab ranged
from 1 to 3 minutes during the demonstration. Sampler
disassembly required 3 minutes in S1A2. In S1A1, the
disassembly time was estimated to be equal to the sampler
setup time. Because a disassembly time of less than
1 minute was recorded in S2A1, the time for sampler
disassembly in this area was conservatively rounded up to
1 minute.
Decontamination of the Ekman Grab required 22 minutes
in S1A2 and 13 minutes in S2A1; sampler
decontamination time was not evaluated in S1A1.
Decontamination of the extension handle used in S1A2
accounts for the difference in decontamination times
between this area and S2A1.
A technician familiar with the Ekman Grab would be
expected to require 1 to 4 minutes for sampler setup, 0.5
to 2 minutes per attempt for sample collection, about
3 minutes for sampler disassembly, and 15 to 20 minutes
for sampler decontamination. However, these activities
might take longer, depending on the number of extension
handles used at a given location. Furthermore, when
sediment sampling activities are planned, the time required
for mobilization, demobilization, and setting up and
positioning the sampling platform would have to be
considered in addition to the times presented above.
B.4.1.6 Costs Associated with Sample Collection
Activities
Primary objective P7 involved estimating costs associated
with Ekman Grab sample collection activities in S1A2 and
S2A1. Because characteristics of these two areas are
different, the sampling activities in these areas were
expected to provide a range of costs involved in
conducting sediment sampling using the Ekman Grab. For
example, during the demonstration in S1A2, the average
PCB concentration was about 310 parts per billion, and the
water depth was about 2 feet. On the other hand, in S2A1,
103
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Table B-9. Time Required to Complete Sampling Activities for Ekman Grab
Time Required (minutes)
Activity
S1A1 (River Mouth)
S1A2 (Freshwater Bay)
S2A1 (Lake)
Sampler setup
Sample collection
Sampler disassembly
Sampler decontamination
1
10
1
Not evaluated
4
8
3
22
1
40
1
13
Total
12
37
55
the average arsenic concentration was 120 mg/kg, and the
water depth was about 18 feet.
The issues and assumptions discussed in Section 8.1 of the
ITVR apply to this section as well except that unused
sediment in S2A1 was assumed to be a hazardous waste.
During the demonstration, the average arsenic
concentration in the samples collected using the Ekman
Grab was 120 mg/kg. Arsenic-contaminated wastes with
TCLP extract concentrations greater than 5 mg/L must be
disposed of as hazardous waste (40 CFR 261). Based on
the average arsenic concentration and the dilution factor
(20) associated with the TCLP, the TCLP extract
concentration for the sediment waste generated during the
demonstration was estimated to be about 6 mg/L.
Therefore, unused sediment in S2A1 was assumed to be a
hazardous waste.
This section presents information on sampler, labor, IDW
disposal, and support equipment costs for the Ekman Grab
as well as a summary of these costs. Table B-10 presents
these costs.
Sampler Cost
In S1A2, the Ekman Grab was used with one 5-foot
extension handle. The Ekman Grab and extension handle
costs were $304 and $131, respectively. The total sampler
cost for S1A2 was estimated to be $435.
In S2A1, the Ekman Grab was used with one messenger
and polyester line. The Ekman Grab and messenger costs
were $304 and $52, respectively. The polyester line cost
less than $10 and therefore was not included in the
estimate. The total sampler cost for S2A1 was estimated
to be $356.
Labor Cost
In S1A2, the time for sampler setup, sample collection,
sampler disassembly, and sampler decontamination totaled
37 minutes or about 1 hour for one technician. In this
area, five investigative samples for PCB analysis were
collected using the Ekman Grab. Table B-3 presents
additional information on the total number of samples
collected. The labor cost for sampling in S1A2 was
estimated to be $34.
In S2A1, the time for sampler setup, sample collection,
sampler disassembly, and sampler decontamination totaled
55 minutes or about 1 hour for one technician. In this
area, ten investigative samples for arsenic analysis and
five investigative samples for PSD analysis were collected
using the Ekman Grab. Table B-3 presents additional
information on the total number of samples collected. The
labor cost for sampling in S2A1 was estimated to be $34.
IDW Disposal Cost
Sampling in S1A2 generated IDW consisting of 15 L of
unused sediment. The cost for disposal of one 55-gallon
drum of nonhazardous waste is $182.
Sampling in S2A1 generated IDW consisting of 7 L of
unused sediment. The cost for disposal of one 55-gallon
drum of hazardous waste is $196.
Support Equipment Cost
Support equipment used during Ekman Grab sampling in
S1A2 and S2A1 included a crescent wrench and a Phillips-
head screwdriver. The costs of these items were not
included in the estimate because a field sampling team
would already have such tools as part of its field sampling
gear.
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Table B-10. Ekman Grab Cost Summary
Item
Quantity
Unit Cost ($)
Total Cost ($)
S1A2 (Freshwater Bay) Costs
Sampler
Ekman Grab
Extension handle
Labor
I DW disposal
Support equipment
Total"
1 unit
1 unit
1 hour
1 55-gallon drum
Not applicable
304
131
34
182
Not applicable
304
131
34
182
0
$650
S2A1 (Lake) Costs
Sampler
Ekman Grab
Messenger
Labor
I DW disposal
Support equipment
Totala
1 unit
1 unit
1 hour
1 55-gallon drum
Not applicable
304
52
34
196
Not applicable
304
52
34
196
0
$590
Notes:
IDW = Investigation-derived waste
a The total dollar amount is rounded to the nearest $10.
Summary of Ekman Grab Costs
In summary, for the Ekman Grab, the costs to collect the
numbers of samples listed in Table B-3 were estimated to
be $650 and $590 for S1A2 and S2A1, respectively. Most
of the costs were associated with the purchase of samplers
(about 67 percent for S1A2 and 60 percent for S2A1) and
IDW disposal (about 28 percent for S1A2 and 33 percent
for S2A1).
B.4.2 Secondary Objectives
This section describes the performance results for the
Ekman Grab based on the secondary objectives specified
in Section B.3.1. The secondary objectives were
addressed based on observations of Ekman Grab
performance during the demonstration.
B.4.2.1 Skill and Training Requirements for Proper
Sampler Operation
The Ekman Grab is easy to operate, requiring minimal
skills and training. Sampler assembly and sample
collection procedures can be learned in the field with a
few practice attempts. In addition, a written SOP
accompanies the sampler when it is procured. The sampler
can be operated by one person in shallow (wading) and
deep water depths because of its lightness (10 Ib, not
including the weight of the extension handle). Sampler
operation is simple because the sampler does not require
complete disassembly and reassembly after each sampling
attempt. Only the scoops or lids have to be opened in
order to retrieve the sediment sample. The sampler
requires no support equipment unless a sampling platform
is needed.
During the demonstration, minimal strength and stamina
were required to deploy the sampler into and retrieve it
from the 0- to 4-inch bss depth interval in S1A1, S1A2,
and S2A1. Previous sediment sampling experience is
beneficial in selecting the most appropriate optional
accessories (such as the extension handle length or weight
attachments) for a given Ekman Grab application.
Previous sediment sampling experience is also beneficial
for accurately assessing the location of the sediment
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surface using the sampler, as is the case with other
samplers.
B.4.2.2 Ability to Collect Samples Under a Variety of
Site Conditions
The Ekman Grab demonstrated the ability to collect
sediment samples under all conditions encountered during
the demonstration, which included a variety of sampling
platforms, water depths, sediment depths, and sediment
compositions. During the demonstration, the range of
platforms used included an 18-foot-long, 4-foot-wide Jon
boat in S1A2; a sturdier, 30-foot-long, 8-foot-wide
pontoon boat in S2A1; and the EPA GLNPO Mudpuppy in
S1A1. Because the sampler does not require electricity or
a tripod-mounted winch for deployment, sampler operation
was feasible from any location on the sampling platforms
used.
Because of the lightness of the sampler and extension
handle (when needed), water depth had no significant
impact on the sampling technician's ability to deploy and
retrieve the sampler. In S1A2, the sampler was deployed
and retrieved using a 5-foot-long extension handle because
the water depth was about 2 feet. In S1A1 and S2A1,
where water depths were about 6 and 18 feet, respectively,
the sampler was deployed and retrieved using the polyester
line and messenger. As with other samplers, the Ekman
Grab's ability to accurately assess the location of the
sediment surface decreases with increasing water depth
and turbidity. Because of the significant water depth and
turbidity in S1A1 and S2A1 and the significant turbidity
in S1A2, the sampling technician could not see the
sediment surface from the sampling platforms. An
underwater video camera may have enabled the sampling
technician to accurately assess the location of the sediment
surface in these areas (Blomqvist 1991).
Water velocity had an impact on the sampling technician' s
ability to deploy the sampler when gravity penetration was
used. As mentioned above, the sampler was deployed in
S1A1 and S2A1 using the polyester line and messenger.
During a few sampling attempts in each area, the current
carried the sampler at least 1 foot beyond the desired
sampling location near the sediment surface. The average
water velocity in S1A1 and S2A1 was ^0.07 ft/s and <0.05
ft/s, respectively. In S1A2, where the average water
velocity was less than 0.05 ft/s, the sampler was deployed
with a 5-foot-long extension handle because the water
depth was only 2 feet. Because use of the extension
handle provided more control during positioning of the
sampler, water velocity had no significant impact on the
sampling technician's ability to properly deploy the
sampler.
The sampler was able to collect surficial sediment samples
in all three demonstration areas. However, the sampler
exhibited a few limitations related to sediment
composition. As discussed in Section B.4.1.2 for primary
objective P2, the Ekman Grab performed poorly in terms
of its ability to consistently collect sediment samples in a
specified depth interval. In S1A1 and S2A1, low sediment
recoveries were attributed to the failure of one or both of
the scoops to close after the messenger was sent. In
addition, in these areas, the sampling technician was
unable to push the sampler into the sediment because the
sampler was attached only to the polyester line.
Therefore, the sampler may not have fully penetrated the
target depth interval because the weight of the sampler
may not have been adequate to overcome the degree of
sediment compaction in these areas. In S1A2, the mean
actual sediment sample thickness exceeded the target
sediment sample thickness. The excessive sample
thickness can be attributed to the sampling technician's
pushing the sampler beyond the specified depth interval
because of his difficulty in accurately assessing the
location of the sediment surface using the sampler.
B.4.2.3 Ability to Collect an Undisturbed Sample
During the demonstration, as was expected given the
nature of the sampler, the Ekman Grab did not consistently
collect sediment samples in which the sediment
stratification was preserved. Specifically, in S1A1 and
S2A1, sediment stratification was not preserved. When
the samples collected in these areas were discharged into
stainless-steel bowls, the samples were unable to retain
their form because of their high water content; as a result,
sediment from different layers was allowed to mix.
However, in S1A2, where the water content in the 0- to
4-inch bss depth interval was relatively low and the
sediment contained a relatively high clay content, the
samples were able to retain their form after discharge, and
the sediment stratification was preserved.
The disturbance associated with bow wave formation near
the water-sediment interface was not likely to be
significant in S1A2 because the speed of sampler
106
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deployment was controlled by the use of the extension
handle. However, in S1A1 and S2A1, the sampler was
deployed using the polyester line; the sampler had to be
dropped in order to allow gravity penetration into the
target depth interval. As a result, the opportunity for bow
wave formation was greater in these areas. However,
because of the water depth and turbidity in both areas, the
sampling technician was unable to observe whether bow
wave formation occurred.
B.4.2.4 Durability Based on Materials of
Construction and Engineering Design
As described in Section B.I.I, the Ekman Grab
components are made of either stainless steel or
galvanized steel. Based on observations made during the
demonstration, the Ekman Grab is a sturdy sampler; none
of the sampler components was damaged or required
repair or replacement during the demonstration.
B.4.2.5 Availability of Sampler and Spare Parts
As mentioned above, no primary component of the Ekman
Grab was damaged or required replacement during the
demonstration. Had a primary sampler component
(excluding the polyester line) required replacement, it
would not have been available in a local retail store.
Replacement components may be obtained from the
developer by overnight courier in 2 days or less,
depending on the location of the sampling site. The
polyester line, which may need occasional replacement,
should be available locally.
B.4.3 Data Quality
The overall QA objective for the demonstration was to
produce well-documented data of known quality. The
TS As conducted to evaluate data quality did not reveal any
problems that would make the demonstration data
unusable. The scope of these TSAs is described in
Sections 4.3 and 4.4 of this ITVR.
This section briefly discusses the data quality of
demonstration results for the Ekman Grab; more detailed
information is provided in the DER (Tetra Tech 1999).
Specifically, the data quality associated with the field
measurement activities is discussed first, followed by the
data quality associated with the laboratory analysis
activities.
B.4.3.1 Field Measurement Activities
Field measurement activities conducted during the
demonstration included measurement of the time
associated with sample collection activities, water
velocity, water depth, volume of IDW, volume of sediment
collected in a given sampling attempt, and depth of
sampler deployment. Of these measurement parameters,
specific acceptance criteria were set for the precision
associated with the time and water velocity measurements
only (EPA 1999). All time and water velocity
measurements made during the demonstration met their
respective criteria (see Table 6-7). Of the remaining
parameters, some difficulties were encountered in
measuring the volume of sediment collected in a given
sampling attempt and the depth of sampler deployment,
which are discussed below.
To measure the volume of sediment collected in a given
sampling attempt, the sediment sample was transferred
into a 2-L container graduated in increments of 20 mL.
The container was tapped on a hard surface to minimize
the presence of void spaces in the sample, the sample
surface was made even using a spoon, and the volume of
the sample was measured. However, because the void
spaces could not be completely eliminated, the volumetric
measurements are believed to have a positive bias that
resulted in overestimation of PSRs. Because the total
volume of the void spaces could not be measured, its
impact on the PSR results could not be quantified.
The depth of sampler deployment was measured with
reference to the sediment surface. To identify the location
of the sediment surface, the sampling technician lowered
the sampler into the water and used the bottom end of the
sampler to feel the sediment surface. Subsequently, the
technician used an extension rod to drive the sampler into
the sediment to a depth that he estimated to be appropriate
to collect a sediment sample or used a polyester line to
allow the sampler to penetrate the sediment by gravity.
Regardless of the method used to deploy the sampler, the
technician could not control the depth of sampler
deployment precisely; when the extension rod was used,
the actual depth of sampler deployment exceeded the
target depth of deployment by up to 2 inches, and when
the polyester line was used, the sampler did not fully
penetrate the target depth interval. Because of the nature
of the Ekman Grab, when the actual depth of penetration
was more than the target depth of penetration (as indicated
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by the volume of sediment sampled), the portion of the
sediment sample associated with the excessive depth of
penetration could not be removed from the sampler before
the sediment volume was measured; consequently, the
PSR results had a positive bias that could not be
quantified.
B.4.3.2 Laboratory Analysis Activities
The laboratory analyses conducted for the demonstration
included the following: (1) PCB, arsenic, and PSD
analyses of sediment samples and (2) PCB and arsenic
analyses of equipment rinsate samples. To evaluate the
data quality of the laboratory analysis results, field-
generated QC samples, PE samples, and laboratory QC
check samples were analyzed. The field-generated QC
samples included the field replicates and temperature
blanks described in Section 4.3 of this ITVR. The PE
samples and laboratory QC check samples are described in
Section 4.4. The acceptance criteria for the QC samples
are presented in Table 6-7.
All temperature blanks and field replicates subjected to
PCB and arsenic analyses met the acceptance criteria,
indicating that the sample homogenization procedure (field
replicates) and sample preservation procedure
(temperature blanks) implemented in the field met the
demonstration requirements. However, as stated in
Section B.4.1.3, in a few cases the results of field triplicate
sample analyses for PSD did not meet the acceptance
criterion. Despite the failures to meet the acceptance
criterion, the PSD results are considered to be valid for the
reasons detailed in Section B.4.1.3.
The PE sample results for both the PCB and arsenic
analyses met the acceptance criteria, indicating that the
analytical laboratory accurately measured both PCBs and
arsenic.
The analytical results for all laboratory QC check samples
except the following met the acceptance criteria:
(1) MS/MSD samples for analysis for PCBs in the
sediment matrix and (2) equipment rinsate samples for
PCB analysis. These issues and their likely impact on data
quality are discussed below.
For the sediment matrix, in all MS/MSD samples analyzed
for PCBs, Aroclor 1016 was recovered at levels higher
than the upper limit of the acceptance criterion, indicating
a positive bias in the PCB results for sediment samples.
However, the analytical laboratory had no problem
meeting the acceptance criteria for control samples such as
BS/BSDs. For this reason, the failure to meet the
acceptance criterion for MS/MSD sample analysis was
attributed to matrix interference. The MS/MSD spiking
compounds (Aroclors 1016 and 1260) were selected based
on the Aroclors detected during the predemonstration
investigation and as recommended in SW-846
Method 8082.
Also for the sediment matrix, in one out of three MS/MSD
pairs analyzed for PCBs, Aroclor 1260 was recovered at a
level less than the lower limit of the acceptance criterion
in the MS sample, but the recovery in the associated MSD
sample was acceptable. Because the investigative samples
contained only Aroclor 1242, of the two spiking
compounds used to prepare the MS/MSD samples, only
the Aroclor 1016 recoveries were considered to be relevant
based on the PCB congener distribution; the Aroclor 1260
recoveries were not considered to be relevant. Therefore,
the low recovery associated with Aroclor 1260 had no
impact on data quality.
In all equipment rinsate samples analyzed for PCBs,
decachlorobiphenyl (the surrogate) was recovered at levels
lower than the lower limit of the acceptance criterion,
indicating a negative bias in the PCB results for equipment
rinsate samples. However, the analytical laboratory had
no problem meeting the acceptance criteria for control
samples such as PE samples and deionized water blanks.
For this reason, the failure to meet the surrogate recovery
acceptance criterion for the equipment rinsate sample
analysis was attributed to matrix interference.
B.5 References
Analytical Software. 1996. Statistix11
Version 2.0. Tallahassee, Florida.
for Windows.
Blomqvist, S. 1991. "Quantitative Sampling of Soft-
Bottom Sediments: Problems and Solutions." Marine
Ecology Progress Series. Volume 72. Pages 295
through 304.
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EPA. 1999. "Sediment Sampling Technologies Demon- Tetra Tech. 1999. "Sediment Sampling Technologies
stration Plan." ORD. Washington, DC. April. Data Evaluation Report." Prepared for ORD, EPA.
October.
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Appendix C
Statistical Methods
This appendix summarizes two statistical methods used in
evaluating the Russian Peat Borer demonstration results:
the Wilk-Shapiro test for evaluating whether data are
normally or lognormally distributed (Section C.I) and the
Wilcoxon signed rank test for evaluating whether two data
sets are statistically different (Section C.2). Section C.3
lists references used to prepare this appendix. Examples
of the use of the two tests are included in each test
description. Both tests were performed using Statistix®
developed by Analytical Software of Tallahassee, Florida
(Analytical Software 1996).
C.I Wilk-Shapiro Test
The Wilk-Shapiro test is an effective method for testing
whether a data set has been drawn from an underlying
normal distribution. Furthermore, by conducting the test
on the logarithms of the data, it is an equally effective way
of evaluating the hypothesis of a lognormal distribution.
This test was used to determine whether the demonstration
results followed either the normal or lognormal
distribution in order to use a parametric test, such as the
Student's t-test, for evaluating the results for primary
objectives PI, P2, and P4. The Wilk-Shapiro test results
indicated that the data sets for PI, P2, and P4 were
generally not normally distributed or could not be tested
for lognormality because the results contained values that
were equal to zero. Therefore, the Wilcoxon signed rank
test, a nonparametric test for paired samples that makes no
assumptions regarding the distribution, was used as an
alternative to the Student's t-test.
For a given data set, the Statistix® software package first
counts the number of values in the data set and then
generates the same number of expected values as if the
data were perfectly, normally distributed. The expected
values are generated using a standard normal distribution
function (a standard normal distribution has a mean of 0
and a variance of 1). Both the actual and expected values
are ranked in numerical order and plotted; the actual
values (ordered data) are plotted on the y-axis, and the
expected values (rankits) are plotted on the x-axis. The
package performs a linear regression analysis and
calculates the square of the correlation coefficient, also
known as the approximate Wilk-Shapiro normality statistic
(W). The W values can range from 0 to 1; 0 indicates no
correlation between actual and expected values, and 1
indicates perfect correlation between actual and expected
values.
The W values calculated for each data set were compared
to critical W values corresponding to various significance
levels (a) and sample sizes (Gilbert 1987). If the W value
for a given data set was greater than the critical value
listed for the corresponding sample size at a= 0.05, the
data were assumed to be normally distributed. The
examples discussed below illustrate this test.
Table C-l presents two example data sets for primary
objective P2 that were tested for normality. Figures C-l
and C-2 provide Statistix® Wilk-Shapiro test outputs for
these data sets. The calculated W values for S1A2 and
S2A2 were 0.9509 and 0.6740, respectively. At a=0.05,
the critical W values for S1A2 and S2A2 were 0.818 and
0.905, respectively. Because the calculated W value for
S1A2 was greater than the critical W value, the S1A2 data
for primary objective P2 were considered to be normally
distributed. The opposite was true for S2A2 data.
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Table C-1. Data Sets for Example Wilk-Shapiro Test Calculations
Demonstration Area
S1A2 (freshwater bay)
S2A2 (wetland)
Depth Interval
(inches bss)
12 to 32
4 to 12
7
1.5
3
8
8
0
7
1
8
0
5
0
11
0
Core Length (inches)
6
000 2.5 00000748
8
Note:
bss = Below sediment surface
11 -
9-
7 -
5-
3-
Approximate Wilk-Shapiro
normality statistic: 0.9509
Number of cases: 8
-2 -1 0
Rankits
Figure C-1. Wilk-Shapiro test plot for core length measurements in S1A2 (freshwater bay).
C.2 Wilcoxon Signed Rank Test
The Wilcoxon signed rank test is a nonparametric test for
paired samples that makes no assumptions regarding the
distribution of data. This test was selected to evaluate the
demonstration results for primary objectives PI, P2, and
P4 as an alternative to the paired Student's t-test, which
was originally prescribed in the demonstration plan under
the assumption that the demonstration results would be
normally or lognormally distributed. The Wilcoxon
signed rank test was selected for evaluating the project
data because the Wilk-Shapiro test indicated that most of
the data sets were neither normally nor lognormally
distributed.
The primary limitation of the Wilcoxon signed rank test is
that it lacks the power of the Student's t-test because it
does not consider the magnitude of the difference between
sample pair results. For example, the test cannot
distinguish the difference between one pair in which the
expected core length was 8 inches and the actual core
length was 7.5 inches and another pair in which the
expected and actual core lengths were 8 and 0 inches,
respectively. Instead, the test first evaluates how many
pairs in a given data set have positive, negative, or zero
differences and then uses this information to test the
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4 -
2 -
0 -
Approximate Wilk-Shapiro
normality statistic: 0.6740
Number of cases: 20
0
Ran kits
Figure C-2. Wilk-Shapiro test plot for core length measurements in S2A2 (wetland).
hypothesis. In addition, the test ignores cases in which the
expected and actual core lengths are the same.
The Wilcoxon signed rank test was performed using the
Statistix® software package, which calculated the
probability value (p-value) at which the null hypothesis
was true. The p-value was compared to an a of 0.05 to
determine whether the null hypothesis should be accepted
or rejected. If the p-value exceeded a, it was concluded
that the mean difference for the paired results was not
statistically significant; otherwise, it was concluded that
the difference was statistically significant.
Several conclusions drawn from the Wilcoxon signed rank
test results for primary objectives PI and P2 did not seem
to be correct based on the magnitude of the differences
observed for sample pairs in a given data set. However,
the results for primary objective P4 were evaluated using
this test because no such problem was observed. To
illustrate this point, example calculations are presented
below.
Table C-2 and Figure C-3 provide the primary objective
PI Hand Corer sample data set for the 4- to 12-inch bss
depth interval in S2A2 and the corresponding Statistix®
output for the Wilcoxon signed rank test, respectively.
The test calculated a one-tailed p-value of 0.0625,
indicating that the difference between the expected and
actual number of attempts was not statistically significant
(the null hypothesis was that the mean difference between
the expected and actual values equals zero). Because the
expected and actual values differed for four of the five
sample pairs and particularly for the second pair, the
difference was in fact considerable. Therefore, the
conclusion drawn from the Wilcoxon signed rank test
appears to be incorrect.
Table C-2. Hand Corer Sample Data for 4- to 12-Inch Below
Sediment Surface Depth Interval in S2A2 (Wetland)
Expected Number of Attempts
Actual Number of Attempts
1
1
1
1
1
2
12
3
2
1
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4- to 12-inch below sediment surface depth interval
STATISTIX FOR WINDOWS
WILCOXON SIGNED RANK TEST FOR S2A2_4_12 - G
SUM OF NEGATIVE RANKS
SUM OF POSITIVE RANKS
NORMAL APPROXIMATION WITH CONTINUITY CORRECTION
TWO-TAILED P-VALUE for NORMAL APPROXIMATION
TOTAL NUMBER OF VALUES THAT WERE TIED
NUMBER OF ZERO DIFFERENCES DROPPED
MAX. DIFF. ALLOWED BETWEEN TIES
2
1
0.00001
CASES INCLUDED
MISSING CASES 6
8/3/99, 4:44:45 PM
0.0000
10.000
EXACT PROBABILITY OF A RESULT AS OR MORE
EXTREME THAN THE OBSERVED RANKS (1 TAILED P-VALUE) 0.0625
1.643
0.1003
Figure C-3. Statistix® output for Hand Corer sample data for S2A2 (wetland).
Table C-3 and Figure C-4 provide the primary objective
P4 Hand Corer and Russian Peat Borer sample data for the
10- to 30-inch bss depth interval in S2A1 and the
corresponding Statistix® output for the Wilcoxon signed
rank test, respectively. The test calculated a two-tailed
p-value of 0.6103, indicating that the difference between
the two sets of arsenic results was not statistically
significant (the null hypothesis was that the mean
difference between the innovative and reference sampler
sample analytical results for the clean layer equals zero).
Because the arsenic results for the Russian Peat Borer
samples were greater than those for the Hand Corer
samples in 7 of the 10 pairs and less in 3 of the 10 pairs,
the conclusion drawn from the Wilcoxon signed rank test
appears to be correct.
Table C-3. Hand Corer and Russian Peat Borer Sample Data for 10- to 30-inch Below Sediment Surface Depth Interval in S2A1 (Lake)
Sampler Arsenic Concentrations (milligrams per kilogram)
Hand Corer
Russian Peat Borer
24
12
8.5
9
16
29
8.3
10
9.7
18
13
10
7.2
14
7.2
11
8.2
9.9
52
11
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10-to 30-inch below sediment surface depth interval
STATISTIX FOR WINDOWS 8/19/99, 3:19:04 PM
WILCOXON SIGNED RANK TEST FOR REFERENCE - IS1
SUM OF NEGATIVE RANKS -33.000
SUM OF POSITIVE RANKS 22.000
EXACT PROBABILITY OF A RESULT AS OR MORE
EXTREME THAN THE OBSERVED RANKS (1 TAILED P-VALUE) 0.3262
NORMAL APPROXIMATION WITH CONTINUITY CORRECTION 0.510
TWO-TAILED P-VALUE for NORMAL APPROXIMATION 0.6103
TOTAL NUMBER OF VALUES THAT WERE TIED 2
NUMBER OF ZERO DIFFERENCES DROPPED 0
MAX. DIFF. ALLOWED BETWEEN TIES 0.00001
CASES INCLUDED 10 MISSING CASES 2
Figure C-4. Statistix® output for Hand Corer and Russian Peat Borer sample data for S2A1 (lake).
C.3 References
Analytical Software. 1996. Statistix® for Windows.
Version 2.0. Tallahassee, Florida.
Gilbert, R. 1987. Statistical Methods for Environmental
Pollution Monitoring. Van Nostrand Reinhold
Company, Inc. New York, New York.
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