&EPA United States Environmental Protection Agency Industrial Environmental Research EPA-600/7-79-1 55 Laboratory July 1979 Research Triangle Park NC 27711 Total Particulate Mass Emission Sampling Errors Interagency Energy/Environment R&D Program Report ------- RESEARCH REPORTING SERIES Research reports of the Office of Research and Development, U.S. Environmental Protection Agency, have been grouped into nine series. These nine broad cate- gories were established to facilitate further development and application of en- vironmental technology. Elimination of traditional grouping was consciously planned to foster technology transfer and a maximum interface in related fields. The nine series are: 1. Environmental Health Effects Research 2. Environmental Protection Technology 3. Ecological Research 4. Environmental Monitoring 5. Socioeconomic Environmental Studies 6. Scientific and Technical Assessment Reports (STAR) 7. Interagency Energy-Environment Research and Development 8. "Special" Reports 9. Miscellaneous Reports This report has been assigned to the INTERAGENCY ENERGY-ENVIRONMENT RESEARCH AND DEVELOPMENT series. Reports in this series result from the effort funded under the 17-agency Federal Energy/Environment Research and Development Program. These studies relate to EPA's mission to protect the public health and welfare from adverse effects of pollutants associated with energy sys- tems. The goal of the Program is to assure the rapid development of domestic energy supplies in an environmentally-compatible manner by providing the nec- essary environmental data and control technology Investigations include analy- ses of the transport of energy-related pollutants and their health and ecological effects; assessments of, and development of, control technologies for energy systems; and integrated assessments of a wide range of energy-related environ- mental issues. EPA REVIEW NOTICE This report has been reviewed by the participating Federal Agencies, and approved for publication. Approval does not signify that the contents necessarily reflect the views and policies of the Government, nor does mention of trade names or commercial products constitute endorsement or recommendation for use. This document is available to the public through the National Technical Informa- tion Service, Springfield, Virginia 22161. ------- EPA-600/7-79-155 July 1979 Total Participate Mass Emission Sampling Errors by E. F. Brooks TRW Systems and Energy One Space Park Redondo Beach, California 90278 Contract No. 68-02-2165 Task No. 104 Program Element No. INE624 EPA Project Officer: Robert M. Statnick Industrial Environmental Research Laboratory Office of Energy, Minerals, and Industry Research Triangle Park, NC 27711 Prepared for U.S. ENVIRONMENTAL PROTECTION AGENCY Office of Research and Development Washington, DC 20460 ------- CONTENTS Page Foreword iii List of Tables iv Sections 1 . Conclusions 1 2. Recommendations 2 3. Introduction 3 4. Particulate Mass Transport 4 5. Error Analysis 6 6. Evaluation of Error Sources 9 7. Summary and Discussion of Results 15 References 17 Glossary 18 Appendices A. Derivation of Mass Transport Equations 20 B. Error Source Evaluation 24 C. Comments on Data and Error Analyses 42 ii ------- FOREWORD This report is an analysis of sampling errors in the determination of total participate mass emissions from stationary sources. In particular it examines the accuracy which is obtainable with EPA-IERL Level 1 assess- ment procedures and hardware. It was prepared under Task 26 of EPA Contract 68-02-2165, "Sampling and Analysis of 'Reduced1 and 'Oxidized1 Species in Process Streams". This work was conducted under the direction of Dr. R. M. Statnick, Environmental Research Center, Research Triangle Park, North Carolina. The Fluid Physics Department and Applied Chemistry Department, Applied Technology Division, TRW Systems and Energy, Redondo Beach, California, were responsible for the work performed on this task. Dr. C. A. Flegal, Applied Chemistry Department, was Program Manager, and the Task Manager was E. F. Brooks. The author wishes to thank Southern Research Institute for stratification background data and discussions on sampling techniques. m ------- List of Tables Page 1. Values for Minor Error Sources 10 2. Values for Velocity Measurement Parameter Errors 11 3. Values for Collected Particulate Mass Error 13 4. Values for Mapping Error 14 5. Single Point and System Errors for Total Particulate Mass Sampling 15 iv ------- 1. CONCLUSIONS Level 1 total participate mass emission assessments: • A SASS train operated in accordance with "IERL-RTP Procedures Manual, Level 1 Environmental Assessment" sampling at a single point will have a sampling accuracy of a factor of ±2 or better in most locations such as stacks or control device inlets. Under worst case conditions, such as at an ESP outlet, it will have an accuracy of about a factor of ±3. • The degree of anisokinetic sampling induced by the SASS train design and operation has a negligible effect on system accuracy. • In single point sampling, the mapping error (non-representative- ness of the selected point) will be the largest individual error in the system. • Sampling accuracy using the SASS train could be improved to about ±25% by using a 16 point traverse rather than sampling at a single point. General • For traverse sampling, the largest individual error will normal- ly be in collected particulate mass, due to anisokinetic sampling and flow/probe misalignment. • System accuracies of ±10% to ±16% can be achieved using com- mercially available equipment and a 16 point traverse. These accuracy levels, while not required for environmental assessment, indicate potential accuracies for control device evaluation testing. ------- 2. RECOMMENDATIONS The SASS train in its present state is recommended for Level 1 assessment work, using single point sampling. A modified traverse (along a single line) should be considered for places such as ESP outlets to minimize errors due to stratification. Additional stratification data should be obtained at sites such as full scale coal fired power plants for the three general types of most important locations: control device inlets, control device outlets, and stacks. Such data should be obtained with a single (or identical) train(s) to isolate the stratification data. Development of methodology to optimize single point sampling accuracy through judicious selection of the sampling point should be pursued through analysis of stratification data and proof of principal source testing for proposed techniques. There is a need for lightweight, high volumetric flow sampling hardware and associated procedures to perform quick (1-2 hour) surveys to determine particulate stratification in sources so that appropriate techniques can be used for longer term source assessment testing. Additional error analysis work should be performed for size fractionating sampling techniques. The present analysis applies only to the total particulate mass determination. Although this report does not deal specifically with Method 5 hardware and procedures, results suggest that for hardware of a given accuracy, there will exist specific procedures to optimize system performance (achieve close to maximum accuracy while minimizing manpower requirements and sampling times). Work should be continued to prepare an IERL-RTP Procedures Manual in this area. ------- 3. INTRODUCTION The purpose of this report is to present a "first cut" estimate of sampling errors in the measurement of total particulate mass emissions from stationary sources. In "IERL-RTP Procedures Manual: Level 1 Environmental Assessment" (Reference 1), the desire is expressed to per- form measurements which are accurate "to within a factor of ±2 to 3." Measurement errors are divided into two general categories: sampling errors and analysis errors. This report deals with evaluation of total particulate mass sampling errors, within the framework of a system error analysis. A mass transport expression is developed in terms of measured parameters to serve as the basis for the analysis. A standard explicit error analysis is performed on the derived expression for mass transport. Since there are also important non-explicit error sources, terms are added to the explicit equation to handle them. The individual error terms are then evaluated on the basis of previous analyses, available empirical data, and, where no data are available, guesses. The evaluation leads to a ranking of individual error sources and estimates of total system error. For single point sampling, which is recommended in Level 1 work, the analysis shows that accuracies within a factor of two to three should normally be achieved. This conclusion is, however, tentative at present due to a shortage of quantitative data on particulate stratification. Results of this study show that particulate stratification causes the greatest individual error in the system. For traverses using sixteen or more sampling points, it can be said with reasonable certainty that the system error should be less than ±25% when proper hardware and techniques are used. For traverses, the largest error will usually be due to velocity measurement and collected mass uncertainties. Conclusions are that single point sampling will usually be acceptable for a Level 1 assessment, but additional mapping error work is needed to provide better justification. In addition, methodology development should be pursued to optimize single point sampling techniques — the present method of sampling at a point of average velocity is a step in the right direction, but further refinements are needed. ------- 4. PARTICULATE MASS TRANSPORT For cases of current interest, it is reasonable to describe the flow stream as consisting primarily of a gas, with small amounts of entrained solid and/or liquid aerosol. The mass transport of the gas is given by (Reference 2): ""G = //PG "G ' " dA 0) A where trig = total gaseous mass flow rate, g/s PQ = local gas density, g/cm3 UG = local gas velocity vector, m/s n = unit vector normal to measurement plane, dimensionless A = area of measurement plane, m2 Aerosol mass transport can be handled in a number of ways. The most exact would be to consider the particles individually, and use statistical methods dealing with single particle mass and velocity. Since the sampling hardware operates on the particle as being entrained in a gas flow, it is most appro- priate from an engineering standpoint to use an entrainment model. This allows us to represent aerosol mass transport in a manner analogous to gaseous mass transport: "A" //cAa "G • "dA A where mA = total aerosol (liquid and solid) mass flow rate, g/s C. = local aerosol concentration, g/cm3 <* = correction factor to account for local difference between mass mean aerosol velocity and gas velocity (i.e., particle slip velocity). Equation (2)-can be considered an exact representation of aerosol mass transport if the proper value of « is selected for each application. For particles of diameter 10 microns or less, we can expect 0.99 < <* < l in most streams. The correction factor « is more fully discussed in Appendix B. ------- The transformation of equation (2) into measured engineering parameters is performed in Appendix A. This transformation is needed to perform a meaningful error analysis. We are presently concerned with two cases: single point sampling and traverse sampling. For these cases, the engineer- ing representations are: mA /2Ap R ~ Single point: m. = « A g- k cos e */ —— (3) N m. "A /^prrrco Traverse: m^ = « k\/2lT^ >^ ^— cos 6 -t/— • _""• • (4) n=l 9n °°n n where k = calibration factor for S probe, dimensionless e = angle between local velocity vector and the vector normal to the measurement plane Ap = measured differential pressure, torr 2 R = universal gas constant, 8314.32 —? ' ? 6|/ mole s2 K T^ = local static temperature, °K p^ = local static pressure, torr M = local average molecular weight (of the gas), g/mole m,, = mass of collected aerosol, g V = volume of withdrawn gas at stream temperature, pressure 9 and gas composition, cm3 ( ) = value of parameters at traverse point n N = total number of traverse points These relations are in terms of parameters which are measured directly with the sampling hardware or for which values are established through prior calibration or assumption. The forms of the relations, as is shown in the next section, determine the relative contributions of the individual parameters to total system error. ------- 5. ERROR ANALYSIS The function of this error analysis is to identify individual sources which contribute to total system error, and to quantify their relative contributions to that error. The value of the analysis lies in two areas — the estimate of total error reflects reliability of the data and can be used to accept or reject individual data points; the estimates of individual errors identify leading error sources, thus indicating where resources should be allocated to improve system accuracy. The following error analysis is carried out under the assumption of a normal distribution of random errors. This assumption will be valid for most, but not all, of the parameters involved. Reference 3, "The Analysis of Physical Measurements" is a recommended text for appropriate background. The logic of the analysis below is identical to that of error analyses for total volumetric flow and gaseous emissions presented in detail in Reference 2. Consider the general relation (Reference 3); G = f (Hr H2, H3 — Hr) (5) where G = dependent variable (quantity to be calculated) H = independent variable (parameter to be measured) f = functional relationship Define the error in the measurement of variable Hr as er- The standard deviation of the measurement of Hr is then given by N V • ». •** w where ar = standard deviation of Hr N = number of measurements By derivation, the standard deviation of G is then given as 2 /af \\/3f v2 '-' v2 «< *• -^ i __ f^ i^i - r\ ------- For the present case, it is convenient to analyze the single point relation, equation (3), and then generalize to the traverse case. Applying equation (7) we obtain: 2 22 m. a a. a. m. V "A 2 1 / c (/ ^ a a-r ^*-£*- AP2 M2 p2 T2 Equation (8) is presented in a non-dimensional form which will allow us to speak of dimension!ess errors rather than the actual standard deviations, which are usually dimensional (e.g., we can consider a temperature error OT /T^ in percent rather than a-r in °K). 00 °° <» The individual error terms in equation (8) correspond to errors which will occur at each point in the stream where a sample is obtained. They are explicit errors in that they are due to identifiable performance aspects of the sampling hardware itself. In addition to these error sources there will also be non-explicit errors due to limitations of the methodology employed. Whenever possible, it is desirable to separate hardware errors from methodology errors so that appropriate hardware and technique can be selected separately to achieve optimum accuracy in any given sampling situation. To accomplish this in the present analysis, we will consider the hardware related errors in equation (8) as those which occur at a given point in the stream. Methodology error terms, introduced below, basically deal with distinctions between the sample obtained at a single point or points and the true total particulate mass emission rate. By definition, then, let a- in equation (8) be the sampling uncertainty occurring at a point in the stream. x 100% (9) °SPE - where °SPE = P°int error, percent 7 ------- We can then define a system error as °SE = °SPE + °ME + °TE + °AE where a^c = total system uncertainty, percent OJ,.E = mapping uncertainty, percent a,-r = temporal uncertainty, percent o.r = assumption uncertainty, percent Significance of the individual terms is as follows: °SPE ~~ as exPlained above> tni's represents the system's capability to extract a representative sample at any one point in the stream, and is determined by the accuracy of the hardware. OME — the mapping uncertainty is associated with stratification in the sample plane. If all other errors are zero, o.,E is a measure of how accurately the sample point or points represent the total aerosol emission. o,.,: — temporal uncertainty is that due to changes in stream condi- tions during the sampling period, and applies to traverses. aAE — the assumption error accounts for inaccuracies in the math- ematical model used in a given situation. For example, if the temperature is assumed constant during a traverse when in fact it varies by a few percent in the sample plane, the resulting error will show up in a^ by definition. aSE — this represents the total system error, and is the final desired quantity. Equations (8), (9), and (10) specifically identify thirteen separate error sources which occur during total particulate mass emission sampling. Of the thirteen, ten are hardware related, and three are methodology related. In the following section, the individual terms are quantitatively evaluated and the leading sources of error are specifically identified. ------- 6. EVALUATION OF ERROR SOURCES This section deals with quantitative evaluation of the thirteen error terms identified in Section 5, with the objective of producing realistic estimates of total system error. Emphasis is placed on a summary of evalu- ations and comments on leading error sources. A more detailed evaluation of individual terms is presented in Appendix B. Two points should be kept in mind when considering the data presented below: (1) The errors, presented in terms of standard deviations, are random errors, rather than systematic errors due to causes such as instrument calibration shifts or mistakes due to operator error. (2) For normally distributed errors, the standard 95% engineering confidence interval is represented by a ± 2o interval. Most, but not all, of the errors can be reasonably represented by a normal dis- tribution. For non-normally distributed errors, emphasis is placed on the "95% confidence" aspects rather than on trying to determine the appropriate type of distribution. Of the thirteen error sources, seven are generally rather small and well understood. These are treated briefly as a group. Following that is commentary on the three terms related to velocity measurement, which are well understood but are not always small. The section concludes with indi- vidual discussion of the temporal error, collected particulate mass error, and mapping error. 6.1 Generally Small, Well Understood Error Sources Errors in static pressure and temperature, duct cross-sectional area, and average molecular weight of the gas are usually small because the parameters are not difficult to measure in most applications. When sig- nificant errors do occur, they are usually systematic in nature and are due to such things as improper calibration practices, unaccounted for wall deposits which reduce the flow area, and other procedural errors. The error due to particle slip velocity is typically small due to the particle size distribution and density encountered in most process streams. The slip velocity, represented by «, is treated further in Appendix B. The other terms mentioned above are discussed at length in Reference 2. ------- The assumption error will be small as long as adequate attention is paid to sampling details. This means that each of the parameters in equation (3) should be measured at each sampling point. The form of equation (3) is sufficiently exact and inclusive that assumption errors will be relatively small. Assumption errors are also treated at greater length in Reference 2. The error in the volume of withdrawn gas will be small when adequately calibrated equipment is used and it is acknowledged that V is based upon stack temperature, pressure, and composition, which usually means that the instrument reading (e.g., from a dry test meter) must be properly corrected for temperature and pressure, and condensible and volatile stream components must be accounted for. Achievable errors for the above parameters are presented below in Table 1. The listed accuracies are not difficult to obtain with generally available equipment as long as adequate care is taken to avoid systematic errors. Table 1. Values for Minor Error Sources Parameter M Poo T A oc V9 Assumption Error 2a (95% Confidence Interval) Error, Percent ±2 ±2 ±2 ±2 ±2 ±2 ±2 6.2 Velocity Measurement Parameter Errors These are errors associated with the parameters k, 9, and Ap. They are discussed at considerable length in References 2 and 4. Errors for various types of hardware and flow conditions are given in Appendix B, and summarized in Table 2. 10 ------- Table 2. Values for Velocity Measurement Parameter Errors Parameter Related Component Error Pi tot-static probe S-type probe x 100% = ±0.5% x 100% = ±156 a. near flow disturbance b. far from flow disturbance Pitot-static S-type Pitot-static S-type 2(tan e) a0 x 100% = ±1.3% y 2(tan e) a. x 100% = ±8% t> 2(tan e) aQ x 100% = ±0.5% 2(tan e) CTQ x 100% = ±2% AP U-tube manometer SASS train1 Baratron 2aAp = ±0.065 Torr x 100% = ±14% Ap 100% = ±0.16%3 IAP read on 0-.5 or 0-4 in ^0 Magnehelic gage 2nominal velocity range 6-40 m/s 3nominal velocity range 1.7-55 m/s The SASS train, selected for Level 1 assessments, employs an S-type pi tot probe and two Magnehelic differential pressure gages. These components comprise a low cost, reasonable accuracy system. The high accuracy Baratron/pitot-static probe combination has been used in the field by TRW without handling problems (Reference 4), and is recommended, especially for very low flow velocities (< 5 m/s), in situations where accuracy takes precedence over hardware cost. 11 ------- 6.3 Temporal Variation Errors The temporal error, OT^, is difficult if not impossible to evaluate when significant changes occur during the period of traverse. The best way to handle the problem is the standard approach of being sure that plant operating conditions are held constant during the sampling period, and discarding the data if they are not. Concurrently, it is also desirable to minimize the sampling time by maximizing the sample flow rate, as is done with the SASS train. The constant attention of the sampling team is required during the sampling period to detect variations in flow or other critical parameters. The estimated value for 2aTE in sources such as power plants is ±4%. 6.4 Collected Particulate Mass Errors The term am. gives the accuracy with which the sampling probe obtains an aerosol sample representative of the point at which the probe is placed. The major error contributions result from anisokinetic sampling and from sample loss or gain within the collection system. Anisokinetic errors, due to improper sampling rate and/or probe misalignment, are treated at length in Appendix B. Sample gain or loss is usually due to improper hardware design or procedures. The appropriateness of condensing some types of vapors and considering the result as particulate is a philosophical battleground which will not be trod upon here. A 2o error of ±4% in col- lected mass due to aerosol gain or loss is considered reasonable for a sampling system such as the SASS train. Isokinetic sampling is achieved for different gas velocities through variation of the sampling rate, the nozzle orifice diameter, or both. Size fractionating devices like the SASS train require a constant, fixed flow rate so that adjustments to approximate isokinecity must be done by varying the nozzle I.D. Nozzle diameters are typically available in .32 cm (.125 in.) intervals, which allows maximum deviation from isokinetic sam- pling to be calculated, as is done in Appendix B. The magnitude of achievable isokinetic sampling errors depends on the type of hardware used (e.g., fixed or variable sample rate), component 12 ------- accuracy, and stream conditions (particle size distribution and local flow direction). Collected mass errors, as determined in Appendix B, are sum- marized below in Table 3 for several general cases. Table 3. Values for Collected Particulate Mass Error Sampling Location m. Collected Mass Error, 2—- x 100% SASS Train Maximum Accuracy Train* Control device inlet Control device outlet In stack, z 8 diameters above breeching ±20% ±16% ±10% ±8% ±6% Hypothetical train using best readily available hardware components. 6.5 Mapping Errors In the case of single point sampling, which is the method recom- mended for Level 1 assessments, the mapping error will usually be the largest single error in the system. Consequently, the mapping error deserves considerable attention. The major problem encountered so far has been a shortage of particulate stratification data, which is essen- tial in evaluation of mapping techniques. The bulk of the data examined to date has been comparisons of single point impactor measurements and Method 5 type traverses. Due to significant differences between the types of sampling trains, it is difficult to isolate the differences in output which are due solely to stratification. Data examined and discus- sion thereof are presented in Appendices B and C, respectively. Mapping error estimates for single point sampling and 16 point traverses are presented in Table 4 for various types of conditions. 13 ------- Table 4. Values for Mapping Error Sampling Location Control device inlet Control device outlet In stack, *8 diameters above breeching Mapping Error, 2oME Single Point +60%, -40% +150%, -60% +50%, -33% 16 Point Traverse ±8% ±12% ±5% As Table 4 shows, maximum mapping errors tend to occur at a control device outlet, especially for electrostatic precipitators, meaning that stratifi- cation is increased by the control device. Just as it is a general rule for velocity measurement to avoid working immediately downstream of a large flow disturbance, it is wise in particulate sampling to avoid sampling immediately downstream of a stratification source. When sampling is done near such a source, such as an ESP outlet, knowledge of the ductwork and characteristics of the source can be used to select a single sampling point which would be more representative than a randomly selected point. 14 ------- 7. SUMMARY AND DISCUSSION OF RESULTS Error values in Tables 1-4 were substituted into equations 8-10 to obtain single point and system errors, which are shown in Table 5. The point error, OSPE;» is indicative of. hardware accuracy, while the system error, ar, indicates the combined hardware and procedure accuracy. Table 5. Single Point and System Errors for Total Parti culate Mass Sampling Sampling Train .^•— • "~ SASS Maximum Accuracy Sampling Location Control device inlet Control device outlet Stack, * 8 dia. above breeching Control device inlet Control device outlet Stack, > 8 dia. above breeching Error 20SPE *Jl L. ±23% ±20% ±13% ±9% ±9% ±7% 2°SE Single Point +64%, -46% +150%, -64% +52%, -36% +60%, -42% +150%, -60% +50%, -34% 16 Point ±24% ±24% ±15% ±13% ±16% ±10% Largest Error Source Single Point aMF ric. a Oijr- ME aME aME OK • ^ ME 16 Point mft a mA a mA CTME, a mA aME a mA Hypothetical train using best readily available hardware components. The "Maximum Accuracy" train in Table 5 is a train which would consist of the highest accuracy components readily available commercially. For example, it would include a high accuracy differential pressure transducer. The purpose in showing the "Maximum Accuracy" train error estimates is only to illustrate the best state of the art capabilities. 15 ------- A comparison of relative accuracies of hardware and procedures is given by aspE and o^. For single point sampling, OSE is invariably large compared with aspE, due to the single point mapping error. Thus hardware improvements in the SASS train would not improve the system accuracy when single point sampling is used. For traverses, the situation is different. The SASS train system accuracy is limited by the hardware rather than by procedure, while for the Maximum Accuracy train, the respective hardware and procedure errors are about equal. There has been a twofold reason for performing the above analyses. The first has been to determine whether hardware and procedures recommended for Level 1 assessments are adequate to produce the desired "factor of ± 2 to 3" accuracy. The second has been to determine optimum accuracy capabilities and to show where future efforts should be devoted to optimize system accuracy. Results of the analyses show that a Level 1 assessment should have a sampling accuracy of better than a factor of i 2 except at a control device outlet, where the accuracy is more likely to be a factor of 3, especially if the control device is an ESP. It is likely true that the error at a control device outlet can be reduced by making use of known device characteristics in selecting a sample point. This type of methodology should be pursued. For very high accuracy work, Table 5 indicates that there is a good match between the accuracies of currently available hardware and traverse sampling procedures. Future work in this area would involve integration of high accuracy components into a viable system for efficient traverse sampling. In conclusion on the matter of Level 1 assessments, it is recommended that sampling after a control device be done in a stack whenever feasible- rather than directly at the control device outlet. This will be the best way to optimize accuracy. In addition, development of methodology for single point sampling and/or modified traverse sampling (along a single line to minimize moving of equipment) directly at a control device outlet should be pursued to minimize the error due to particulate stratification. 16 ------- REFERENCES 1. "IERL-RTP Procedures Manual: Level 1 Environmental Assessment," EPA-600/2-76-160a, Hamersma, Reynolds, and Maddalone, June 1976. 2. "Flow and Gas Sampling Manual," EPA-600/2-76-203, Brooks and Williams, July 1976. 3. The Analysis of Physical Measurements, E. Pugh and G. Winslow; Addison-Wesley, 1966. 4. "Continuous Measurement of Total Gas Flowrate from Stationary Sources," EPA-650/2-75-020, Brooks, et al., February 1975. (See Appendices for additional references.) 17 ------- GLOSSARY SYMBOL USAGE A flow cross-sectional area, m2 C. true aerosol concentration in the stream ahead of the probe, g/cm3 C aerosol concentration inside probe entry, g/cm3 D particle diameter, cm D sample probe orifice diameter, cm f empirical functional relationship; functional relationship G dependent variable (quantity to be calculated) H independent variable (parameter to be measured) k pi tot probe calibration factor, dimensionless mA mass of collected aerosol, g m total aerosol (liquid and solid) mass flow rate, g/s ITU total gaseous mass flow rate, g/s M local gas average molecular weight, g/mole n unit vector normal to measurement plane, dimensionless N number of measurements; total number of sampling points D local static pressure, torr roo p local stagnation pressure, torr Ap P ~ POO ' tfie Pressure differential between the local stagnation and static pressures, torr g-m2 universal gas constant, 8314.32 mole S2 °K }K local gas velocity vector, m/s local gas static temperature, °K UG true gas velocity ahead of the probe, cm/s U mean velocity at probe inlet, cm/s 18 ------- SYMBOL USAGE V volume of withdrawn gas at stream temperature, pressure, 9 and gas composition, cm3 ( ) value of parameter at sample point n correction factor to account for local difference between mass mean aerosol velocity and gas veloctity (i.e., particle slip velocity). Dn Pn ur P P » 3 -^~j;— lop u e angle between local velocity vector and duct axis y gas viscosity, poise PG gas density, g/cm3 p particle density, g/cm3 a.r assumption uncertainty, percent aME mapping uncertainty, percent OSE total system uncertainty, percent a standard deviation of H point error, percent Oyr temporal uncertainty, percent 19 ------- APPENDIX A. DERIVATION OF MASS TRANSPORT EQUATIONS This appendix deals with the transformation of t!)e participate conser- vation of mass equation (equation (2) in Section 4) into the engineering representations shown in equations (3) and (4) in Section 4. The conser- vation of mass equation is: "•A = J[/CA « "G ' " dA (A-D M where m = total aerosol (liquid and solid) mass flow rate, g/s C. = local aerosol concentration, g/cm3 « = Correction factor to account for local difference between mass mean aerosol velocity and gas velocity (i.e., particle slip velocity). A = flow cross-sectional area, m2 Equation (A-l) is a convection model which states that the local aerosol concentration is convected downstream with the gas at a speed equal to the gas velocity component in the axial flow direction multiplied by a correction factor <* which accounts for inertial and gravitational forces on the particles. As the particle mass to cross-sectional area ratio becomes small, « goes to unity, which represents complete entrainment. As that ratio becomes large, <* goes to zero, representing non entrainment. For most processes of interest, <* will be very close to unity, and is not measured in practice. For purposes of the error analysis, we need to take equation (A-l) and put it in terms of actual engineering parameters. In most cases, it is not practical to take the entire gas stream and process it to determine the particulate content. Standard techniques involve obtaining samples from one or more discrete points in the stream. For these two cases, single point and traverse sampling, equation (A-l) becomes 20 ------- Single point: m^ % CA « UG • n A (A-2) N , A Traverse: rhA £ V* (CA <*n UG • njAAn (A-3) n=l where N = total number of sampling points ( ) = value of parameter at sample point n. For a typical sampling train, the aerosol concentration is measured as CA = r- (A-4) g where m. = mass of collected aerosol, g V = volume of withdrawn gas at stream temperature, pressure, 9 and gas composition, cm3 The aerosol mass mA is determined by weighing the collected samples, and the gas volume is measured with a dry gas meter or similar device, with correction being made for moisture removed ahead of the meter. The flow cross-sectional area, A, is usually determined from blue- prints, especially in the case of rectangular ducts. For traverses, all common techniques divide the area up into segments of equal size, so that AAn = ff (A"5) The axial component of the gas velocity is usually measured by means of a pitot probe and differential pressure device for the primary measurement. The transformation is as follows: uG-n = |UG| cos e (A-6) where e = angle between local velocity vector and duct axis 21 ------- For notational simplicity, define UG E "G (A-7) We will normally be dealing with incompressible gas flows, so that 2Ap ur = k 6 - >G where Ap = pQ - p^ , the pressure differential between the local stagnation and static pressures, torr PG = gas density, g/cm3 k = pi tot probe calibration factor Substituting the equation of state, P . fT where p^ = local static pressure, torr R = universal gas constant, 8314.32 mole S2 °K M = local gas average molecular weight, g/mole T^ = local gas static temperature, °K for P£, we obtain V2Ap R T -^ UG "n = UG COS 9 = p M roo Substituting into equations (A-2) and (A-3), we obtain Single point: R T 00 A \rk cos e (A-9) 22 ------- Traverse: n=l n I °°n n The conservation of mass equation is now presented in terms of normal engineering parameters. Of the terms in equations (A-ll) and (A-12), the following are usually measured directly with sample train components and support equipment: mA> V , Ap, T^. The area A is either measured or determined from blueprints. The static pressure p^ is often determined by adding (or subtracting, as required) the differential pressure between the stream pressure and ambient pressure to barometric pressure, which is usually available. The average molecular weight, fT, is either measured or estimated from plant operating conditions. The pitot probe calibration constant should be determined by pre- and post-test calibration. The slip velocity factor « is usually ignored (therefore considered to be unity). Flow angularity is also typically ignored, meaning cos 8=1, but it is possible to use a velocity probe which automatically compensates for angularities up to 30°, as is discussed in Appendix B. Equations (A-ll) and (A-12), which appear as equations (3) and (4) in Section 4, serve as the basis for the error analysis in Section 5. 23 ------- APPENDIX B. ERROR SOURCE EVALUATION The purpose of this appendix is to provide background to support the summaries of evaluations presented in Section 6. Emphasis here will be placed on understanding the physics of some of the key parameters, and on presentation of empirical data, in particular for stratification. Emphasis is placed on three areas: velocity measurement, collected particulate mass, and stratification. 1. Particle Slip Velocity Factor Of the "generally small, well understood error sources", only the slip velocity factor a warrants additional treatment here. Particle velocities will differ from the gas velocity due to gravity forces and inertial forces, the latter arising when there is a change in flow direction. The magnitude of the particle/gas velocity differen- tial is most easily illustrated for the case of a flow going directly up a vertical stack. In this situation, gravity produces a downward force which makes the particle velocity less than the gas velocity. The result is a local Stokes flow condition in which the differential velocity is identified as the settling velocity of the particles. Settling velocity is plotted in Figure B-l as a function of particle size (spherical particles) for two different values of particle density and gas viscosity. The slip velocity factor would then be calculated from the particle settling (terminal) velocity and the gas velocity. As Figure B-l shows, the settling velocity will be at most a few centimeters/second for particles smaller than 10 microns. A vertical flow represents the worst case in terms of gravitational effects. Inertial effects can usually be ignored due to the velocities involved. It typically takes a special effort, as in the case of cyclones and impactors, to produce the high velocities and sharp turning angles required to make inertial effects important. 24 ------- 60 r- ro tn 50 40 30 a. oo cu 10 IN A STACK, WE HAVE CURVE 1 8.0 -4 j , poise 1.7x10 10 20 40 70 PARTICLE DIAMETER, MICRONS 100 MOST PROCESS STREAM CONDITIONS FALL IN THIS REGION 200 Figure B-l. Settling speed of spherical particles in a combustion stream as a function of particle size ------- 2. Gas Velocity Measurement Present concern is limited to measurement techniques involving a pitot probe and differential pressure measurement device. The most common types of pitot probes are the S-type probe typically used in field testing, and the pi tot-static probe, which has tended to acquire a reputation of being acceptable for use only in the laboratory. The 2a calibration factor accuracies of +_ .5% and + 1% for the pitot-static probe and S probe, respectively, shown in Table 2 in the main text were obtained from References B-l and B-2. Angularity sensitivity data in Table 2 were obtained from the same sources. The data are shown in Table B-l below. Table B-l. Errors due to Flow Angularity for S-Type and Pi tot-Static Probes Flow Angularity yaw, degrees ± 5 ±10 ±20 ±30 pitch, degrees + 5 +10 +20 +30 - 5 -10 -20 -30 2a Velocity Error, 2 (tan e) a0xlOO% t) "S" Pitot Probe +1.6 +3.5 +4.5 +7.5 +1.5 +2.0 +3.5 +4.5 -1.5 -2.5 -5.0 -8.0 Pitot Static Probe +0.3 +1.0 +1.3 +0.2 +0.3 + 1.0 +1.3 +0.2 +0.3 +1.0 +1.3 +0.2 26 ------- For the "near flow disturbance" case in Table 2, a flow angu- larity range of ±30° was assumed, while the range was selected to be ±5° for the "far from flow disturbance" case. As the data show, the pitot static probe has the more desirable characteristics. Accuracy of differential pressure measurement devices is presented in Figure B-2. The zig-zag in the SASS train curve corresponds to a switch from the low range to the high range Magnehelic gage. Summary data in Table 2 were taken from this plot. 3. Collected Particulate Mass The Level 1 particulate collection procedure has been questioned (Reference B-3) for single point sampling and for not sampling in a strictly isokinetic manner. The isokinetic problem is addressed here, while single point sampling (mapping) errors are discussed in the fol- lowing section. The term am gives the accuracy with which the sampling probe obtains an aerosol sample representative of the point at which the probe is placed. The major contributions to error come from anisoki- netic sampling and from sample loss or gain within the probe. Loss of sample could occur due to poor system design or procedural errors, while sample gain is due to vapor condensation, which would also be hardware and/or procedure related. Sample alteration should not be a major problem in a properly designed and operated system. Isokinetic sampling errors will occur in even the most careful work due to equipment random errors and stream conditions. Some general comments about the concept of isokinetic sampling are in order here. Textbook explanations of isokinetic sampling show smooth streamlines in the flow around the sample probe inlet, with streamline deviations illustrating anisokinetic conditions. In reality, such a situation exists only in steady laminar flows, as can be produced in a good wind tunnel. Laminar flows will not^ be encountered in the field. In steady, laminar flows, streamlines are 27 ------- 1.5 100 APPROXIMATE VELOCITY, M/S 5 15 r~ 45 U-TUBE MANOMETER 10 o cc. oo 3 GO CO .1 SASS TRAIN ARATRON 145 (MKS INSTRUMENTS) .01 1 .01 Figure B-2. .1 1 DIFFERENTIAL PRESSURE, TORR Differential pressure measurement accuracy of various devices 28 10 ------- steady state entities, which makes flow visualization techniques such as smoke filaments in air flow or dye filaments in liquid flow viable. In a turbulent stream, streamlines exist instantaneously only-- the streamline pattern varies greatly from millisecond to millisecond. These changes are typically not small. In a fully developed turbulent pipe flow, the turbulence is structured such that turbulent eddies tend to move downstream as units (Reference B-4). Experimental studies have shown that the size of these turbulent eddies is about 7% of the pipe diameter (Reference B-5). In a fully developed turbulent pipe flow, the velocity component parallel to the sample probe axis can be expected to fluctuate over about a ±10% (of axial flow velocity) range, with similar fluctuations in the angle of the velocity vector at the probe tip (Reference B-6). For operation near an elbow or other large disturbance, these fluctuations will be even worse due to the larger local scale of turbulence caused by flow detachment. What this all means is that in real life, isokinetic sampling is a type of averaging process. In all cases, we can expect that the stream turbulence scale will be large with respect to the sampling orifice, so there is no easy way to get around the turbulence problem. The primary reason for the above commentary is to illustrate that while isokinetic sampling*can be performed in a good laminar flow wind tunnel, it can only be approximated in actual process streams. Watson's expression for isokinetic sampling errors (Refereces B-7 and B-8), the experimental verification for which was obtained in a low turbulence wind tunnel, is as follows: ' C UG A (B-l) 29 ------- where C = aerosol concentration inside probe entry, g/cm3 C. = true aerosol concentration in the stream ahead of the probe, g/cm3 Ug = true gas velocity ahead of the probe, cm/s U = mean velocity at probe inlet, cm/s - DP PP UG " Ds f = empirical functional relationship D = particle diameter, cm p = particle density, g/cm3 u = gas viscosity, poise DS = sample probe orifice diameter, cm Equation (B-l) is plotted in Figure B-3 for different values of the various parameters. In practice, the plot says that anisokinetic sampling does not lead to concentration errors as the particles become very small, while in the limit of large, dense particles, the concen- tration error is inversely proportional to the velocity error, i.e. C U6 ~— -v TT- for large, dense particles. LA um In normal practice, the stream velocity is measured with a pitot probe and the sampling velocity Um is set equal to the measured velocity. For this mode of operation, the measured aerosol mass flux at the sampling point becomes (ignoring <* for the moment) = CmUm 30 ------- 4 i- co = UI "$»r a - K • ) UG o o o C£ _ •> f(B) DIAMETER, MI^ONS 0 >50 40 30 22 13 CP = V s FOR 1 g/cm3 10 m/s 1.27 cm -4 = 2.3 x 10 poise UG TRUE GAS SPEED Um ' SAMPLING SPEED Figure B-3. Particulate measured concentration error as a function of sampling velocity (Anisokinetic) error for various aerosol conditions (from Watson, Reference B-7) ------- while the true mass flux is = CAUG (B-3) applying the small and large particle limits of equation (B-l), we obtain 0 < meas true (B-4) where zero error occurs for the case of large particles, while non-zero error occurs for very small particles and is in fact solely a velocity measurement error unrelated to the sampling process. In other words, as long as sampling velocity and measured velocity are kept identical, anisokinetic sampling of large particles compensates for velocity measurement errors, while anisokinetic sampling of small particles does not lead to a concentration measurement error. For total particu- late measurement errors, then, we may make the following statement: Particle mass emission errors at a point will not be larger than errors in the measured stream velocity as long as the sample velocity is maintained equal to the measured velocity and the sampling probe is properly aligned with the stream. It must be noted that the above statement applies only to particle mass emission and only at individual points. The relationship between point measurements and the total emission is related to stratification, which is treated below. The important point is that isokinetic errors and velocity measurement errors are compensating rather than additive. Concentration measurement errors due to anisokinetic sampling depend, of course, on all the factors shown in equation B-l. Reference B-7 recommends the values shown in Table B-2 "for the size distribution of dusts encountered in practice". The following general rule is also 32 ------- Table B-2. Effect of Departure from Isokinetic Conditions on Sample Concentrations (from Reference B-7) UG US 0.6 0.8 1.2 1.4 1.6 1.8 C Co RANGE 0.75-0.90 0.85-0.95 1.05-1.20 1.10-1.40 1.15-1.16 1.20-1.80 TYPICAL VALUE 0.85 0.90 1.10 1.20 1.30 1.40 33 ------- recommended in Reference B-7: "Isokinetic sampling is unnecessary for smoke and fumes which are not admixed with particulate matter over 5y in size." It is clear that for purposes of error analysis, the term o- should m/\ be coupled with the velocity error terms due to the compensating aspects. Aside from the traditional isokinetic sampling aspects, we must also be concerned with misalignment of the sampling probe with respect to the local stream direction. As explained above, the flow direction goes through instantaneous changes, but these average out reasonably over the sampling period in most cases when the volumetric flow rate stays constant. Any misalignment of the sampling probe reduces the number of large particles (> 5y) collected, while collection of small particles is affected little, if at all. Failure of the sampling team to align the sampling probe parallel to the duct or stack axis within two or three degrees constitutes a mistake rather than a random error. Non- alignment of the flow itself with the stack axis must generally be considered a random error since the sampling team will usually not have the instruments to properly determine flow direction. The best way to avoid flow angularity is to use the standard "eight diameters downstream and two diameters upstream of a disturbance" approach when possible. In stacks, the flow will tend to be axially aligned within a few diameters from the breaching except in the case of swirling (cyclonic) flow, which can persist much longer. Reference B-9 makes the following statements about such flows: "....severe cyclonic motion has not been observed in large power plant stacks." Unfortunately, it is also concluded that "Little qualitative data is available defining flow angularity in large (>100 MW) power plant stacks." To summarize the above commentary and relate it to actual hard- ware, it can be said that the major error sources for collected 34 ------- particulate mass are non-isokinetic sampling, probe/flow misalignment, and sample gain or loss within the probe. For the SASS train, non- isokinetic sampling occurs because the sample flow rate must be held constant. Since a sampling crew will have a limited number of inlet nozzle sizes, there will be a differential between the nozzle inlet velocity and the local stream velocity. In addition, this configuration does not allow for adjustments in sampling rate during a run to com- pensate for any free stream velocity changes. In an optimum train, the sampling velocity would be continually adjusted so that it matched the measured stream velocity. The discussion associated with equation (B-4) says that if this can be accomplished, errors in isokinetic sampling tend to compensate for velocity measurement errors. In the turbulent flows which occur in real life, it will not be possible to match the sample flow rate to the measured velocity, since the latter will fluctuate more rapidly than the sample flow can be adjusted. The error estimates in Table 3 of the text for a are based on known SASS train characteristics, accuracies (velocity measurement in particular) of other commercially available hardware, and estimates of actual flow conditions to be encountered at the three types of designated sampling locations. For the SASS train, the greatest source of error is the anisokinetic error, while misalignment will be the largest source for the hypothetical "maximum accuracy train". The basic difference between the two trains would be greater velocity measurement accuracy and continuously variable sampling velocity for the "maximum accuracy train". Errors are predicted highest at a control device inlet due to the size distribution (maximum number of large particles) and anticipated flow angularities. (See Reference B-9 for compilations of control device inlet and outlet size distributions.) Errors will be at a minimum in a stack due to smaller flow angularities and removal of large particles in a control device. 35 ------- 4. Mapping (Handling of Stratification) There are three major difficulties involved in dealing with stratification problems: (1) The stratification level itself is often very large, which leads to large errors, especially for single point sampling. (2) More background data are needed to assess the severity of the problem. (3) There is a shortage of methodology for sampling techniques in stratified streams. The first point is illustrated in Table B-3, taken from Reference B-10. Particulate mass concentra- tion maps were taken for the four cases listed (the ESP data is true field data). Large variations from the mean concentration were ob- served in each case. Of particular interest is the ESP data, which shows that the device was definitely a source of stratification. The variations shown in Table B-3 clearly indicate that single point sampling is likely to result in large mapping errors. There is no question that much more stratification data exist than were examined for this report. As much data was examined as could be obtained within the scope of work. Comparison data between single point impactor sampling and multiple point Method 5 type sampling is shown in Tables B-4 and B-5. The data were obtained from References B-ll and B-12, respectively, supplied by Joe McCain of Southern Research Institute. The data in Table B-4 represent a summary of many runs. The "minimum" and "maximum" errors are the best and worst correlations obtained among the individual runs, while the "nominal" error was the average error for all runs in the category. The data in Table B-5 are for individual runs. A very important item to keep in mind when examining these data is that entirely different types of sampling trains were used to obtain the single point (im- pactors were used here) and multiple point (Method 5 type train) data. This makes it impossible to isolate the mapping error due to single point sampling. Data type and quality are discussed further in Appendix C. What is needed is more mapping data obtained with a single 36 ------- Table B-3. Summary of Particulate Mapping Data from Fluidyne "Particulate Sampling Strategies" Report (Reference B-9) DESCRIPTION Downstream of ESP Upstream of ESP "Theoretical" distri- bution downstream of ESP Laboratory scale model flow CENTER POINT CONCENTRATION ERROR, % -16 +13.5 -62.8 - 2.33 VARIATION IN SAMPLE PLANE FROM MEAN CONCENTRATION, % LOW -74 -35 -63 -19 HIGH +268 + 30 +160 +117 Table B-4. Summary of Comparison of Single Point Impactor Data Versus Method 5 Traverse at an ESP Outlet, from Southern Research Institute EPRI Report (Reference B-ll) OPERATING MODE* With S03 Without S03 SINGLE POINT ERROR USING METHOD 5 TRAVERSE AS A REFERENCE, % MINIMUM - 5 -68 NOMINAL -33 -75 MAXIMUM -61 -94 *SOo injection was used as a mechanism to minimize re-entrainment due to rapping. Lower loading and less stratification occurred with SO., injection. 37 ------- Table B-5. Grain Loading Errors for Single Point Impactor Sampling, Using Conventional (ASME, EPA) Mass Train Traverse Measurement As Reference Data (Data taken from Reference B-12) SITE 1 2 3 4 RUN NO. 1 2 3 4 5 6 7 1 2 3 1 2 3 1 2 3 4 SINGLE POINT MASS LOADING ERROR, % +711 +256 +227 + 26 + 6 + 5 +131 - 34 - 35 - 43 - 38 - 19 - 50 - 6 - 45 - 48 - 50 Sites: At all sites, location was control device outlet 1 - Coal fired power plant 2 - Coal fired power plant 3 - Electric arc smelting furnace 4 - Coal fired power plant 38 ------- instrument, as was done to obtain the data summarized in Table B-3. The data in Table B-4 are a good illustration of the need for better sampling methodology. The impactor sampling point used was not representative of the distribution in the stream, leading to errors of as high as a factor of 16. The Level 1 approach of using a point of average velocity as the sampling point is a step in the right direction since such a point is less likely than most to result in misalignment errors, will not be in a recirculation region, and at least will be representative of total mass transport. For stack sampling, it may be the case that further refinements to this approach will not be needed. For sampling at a control device outlet, however, Table B-4 points out the need for taking the device's characteristics into account in the selection of a sampling point or points. Particulate stratification originates where the particles originate, e.g. in the furnace of a coal fired power plant. Strati- fication can be made worse by in-leakage of air. Removal devices can make stratification either more or less severe, according to their operating characterisitics. Changes in ducting shape and direction simultaneously promote convective mixing (reduces stratification) and inertial separation (increases stratification). The combination of desired accuracy and stratification provides the answer to the ques- tion, "To single point or not to single point?". This question has been studied more extensively for flow measurement and gas sampling than for particulate sampling, but should apply to that case as well. Reference B-13, which is basically a summarization of the velocity measurement data in Reference B-10, and Reference B-14 conclude that the 2o mapping error of a 12-to-16 point traverse is about a factor of five less than that for a single point measurement for volumetric flow (References B-12 and B-13) and gas composition (Reference B-13). As the mean particle size becomes small (<5p), particulate stratifica- tion is almost identical in mechanism to gas stratification because of 39 ------- the dominance of convective mixing in both cases. In Reference B-15, the average 2o single point gas composition mapping error was found to be ±15%. There is no reason to believe the single point participate sampling mapping error would be better than this figure, and indeed will be much worse in most cases. The data which have been examined are not sufficient to establish good bounds for single point particulate sampling. Accumulated data for volumetric flow and gas composition lead to the conclusion that a properly performed traverse using about 16 points will result in o^ not being the major source of system error. The single point mapping error estimates in Table 4 in the text were derived from Tables B-3 and B-5, taking into account the difference in trains in the latter. The traverse error estimates were obtained by comparing the maps in Reference B-10 with gas composition maps in Reference B-14. The mapping error itself is independent of the sampling equipment used. The mapping error estimates must at present be considered the least firm of all the error estimates in the text, which is unfortunate since the mapping error is by far the largest error in the system for single point sampling. The need for more data to "firm up" the estimates is discussed in Appendix C. 40 ------- APPENDIX B. REFERENCES B-1. "Continuous Measurement of Total Gas Flowrate from Stationary Sources," EPA-650/2-75-020, Brooks, et al.. February 1975. B-2. The Measurement of Air Flow, E. Ower and R. C. Pankhurst; Pergamon Press, 1966. B-3. "Recent Environmental Assessment Studies," (Draft Copy), Monsanto Research Corporation, November 1976. B-4. Boundary Layer Theory, H. Schlichting; McGraw-Hill Book Company, 1968. B-5. "Correlation Measurements in a Turbulent Flow Through a Pipe," G. I. Taylor, Proc. Roy. Soc. A 157. 537-546,1936. B-6. "The Structure of Turbulence in Fully Developed Pipe Flow," J. Laufer, NACA TN 2954, 1953. B-7. Air Pollution. Volume II, A. Stern, ed., Academic Press, 1968. B-8. H. H. Watson, Am. Ind. Hyg. Assoc. Quart. 15, 21, 1954. B-9. "Particulate Sampling Strategies for Large Power Plants Including Non-uniform Flow," EPA-600/2-76-170, Hanson, et a!.. June 1976. B-10. "Fine Particle Emissions Information System: Summary Report (Summer 1976)," EPA-600/2-76-174, Schrag and Rao, June 1976. B-ll. "Proceedings on the Workshop on Sampling, Analysis, and Monitoring of Stack Emissions," EPRI SR-41, Southern Research Institute, April 1976. B-12. "Particulate Sizing Techniques for Control Device Evaluation," EPA-650/2-74-102-a, Smith, et al.f August, 1975. B-13. "The Number of Sampling Points Needed for Representative Source Sampling," K. T. Knapp, paper presented at Fourth National Conference on Energy and Environment, October 1976. B-14. "Flow and Gas Sampling Manual," EPA-600/2-76-203, Brooks and Williams, July 1976. B-15. "Continuous Measurement of Gas Composition from Stationary Sources," EPA-600/2-75-012, Brooks, et al.. July 1975. 41 ------- APPENDIX C. COMMENTS ON DATA AND ERROR ANALYSES As stated in the text, the error analysis performed was identical in form to that in Reference C-l. The explicit portion of the error analysis is similar in concept to that in Reference C-2. A nominal 2o system error of ±16% was obtained for a total participate mass measurement involving a traverse. This estimate is similar to those for traverses in Table 5. A more encompassing error discussion is given in Reference C-3, and treats both explicit and non-explicit error sources. However, error bounds were not well established in this analysis. The nature of the measurement for total particulate mass dictates that two distinct groups of information must be consulted to determine system accuracy - sampling hardware characteristics and source characteristics. For parameters such as temperature and static pressure, it is normally the case that measurement accuracy can be determined from the hardware alone. The accuracy of parameters such as velocity and collected particulate mass usually depend on both hardware and source characteristics. At the other extreme, mapping errors depend only on source characteristics. The great variety of source characteristics makes it impossible to perform a system error analysis and arrive at a single number for system accuracy, just as it would be impossible to arrive at a single number result for an analysis of a variety of sampling trains. The final selected approach of looking at two types of trains in three generalized sampling situations was in- tended to show the relative impact of hardware and source on system accuracy. Most error analysis work deals with identification and evaluation of specific error sources. The interrelationship of hardware and source characteristics for particulate sampling necessarily complicates isolation of errors. During the present study, this problem caused the most diffi- culty in evaluation of the error terms a and o^. As was mentioned in Appendix B, evaluation of anisokinetic sampling errors has traditionally been performed in laminar flow wind tunnels. The turbulent, unsteady flows 42 ------- in process streams make it difficult to adapt laminar flow data to the real life case. That approach has been used of necessity, however, since it has not been possible to obtain high accuracy reference data needed for an error assessment in the field. The bulk of the mapping data summarized in Appendix B has the problem that the single point data was obtained with significantly different hard- ware than the traverse data. This makes it impossible to separate the hardware error from the mapping error. There is no question that mapping data of the type desired (a concentration map obtained with a single probe) is difficult, time consuming, and costly to obtain. In this instance, it is felt that the effort would be justified due to the magnitude of mapping errors, in addition to supporting error analysis work, the same data would be essential to the development of methods for obtaining representative samples through judicious selection of a single sampling point or a small number of sampling points. The functional purpose of a system error analysis, in addition to producing the bottom line number for total system accuracy, is to determine the relative importance of the individual error sources. This information tells the worker which hardware components in a given system should be upgraded to achieve a desired accuracy, and which components may be replaced with less expensive, less accurate ones without significantly altering the system accuracy. The same is true of sampling procedures, the most obvious example being selection of single or multiple point sampling techniques to achieve a given accuracy. A proper error analysis is thus the technical foundation for optimum allocation of funds and manpower to achieve sampling data of appropriate quality for the tasks at hand. 43 ------- APPENDIX C. REFERENCES C-l. "Flow and Gas Sampling Manual," EPA-600/2-76-203, Brooks and Williams, July 1976. C-2. Industrial Source Sampling. Brenchley, Turley, and Yarmac, Ann Arbor Science Publishers, Inc., 1973. C-3. "A Manual of Electrostatic Precipitator Technology, Part I - Funda- mentals," NTIS PB-196 380, Oglesby, etal., August 1970 44 ------- TECHNICAL REPORT DATA (Please read Instructions on the reverse before completing) REPORT NO. EPA-600/7-79-155 2. 3. RECIPIENT'S ACCESSION NO. 4.TITLE AND SUBTITLE I Total Particulate Mass Emission Sampling Errors 5. REPORT DATE July 1979 6. PERFORMING ORGANIZATION CODE 7. AUTHORIS) E.F. Brooks 8. PERFORMING ORGANIZATION REPORT NO. 9. PERFORMING ORGANIZATION NAME AND ADDRESS TRW Systems and Energy One Space Park Redondo Beach, California 90278 10. PROGRAM ELEMENT NO. INE624 11. CONTRACT/GRANT NO. 68-02-2165, Task 104 12. SPONSORING AGENCY NAME AND ADDRESS EPA, Office of Research and Development Industrial Environmental Research Laboratory Research Triangle Park, NC 27711 13. TYPE OF REPORT AND PERIOD COVERED Task Final; 11/76 - 4/77 14. SPONSORING AGENCY CODE EPA/600/13 is. SUPPLEMENTARY NOTES gPA project officer R. M. Statnick is no longer with for details, contact F.E. Briden, Mail Drop 62, 919/541-2557. 16. ABSTRACT The repOrt gives a first-cut estimate of sampling errors in the measure- ment of total particulate mass emissions from stationary sources. IERL-RTP Pro- cedures Manual: Level 1 Environmental Assessment expresses the desire to mea- sure at accuracies within a factor of -f or - 2 to 3. Measurement errors are divided into two general categories: sampling errors and analysis errors. The report deals with evaluation of total particulate mass sampling errors , within the framework of a system error analysis. A mass transport expression is developed in terms of measured parameters to serve as the basis for the analysis. A standard explicit error analysis is performed on the derived expression for mass transport. Since there are also important non-explicit error sources, terms are added to the explicit equation to handle them. The individual error terms are then evaluated on the basis of previous analyses, available empirical data and, where no data are available, estimates. The evaluation leads to a ranking of individual error sources and esti- mates of total system error. Analysis results show that a Level 1 should have a sam- pling accuracy of better than a factor of + or -2, with a confidence of 95%, except at a control device outlet where the accuracy is more likely to be a factor of + or -3, especially if the control device is an electrostatic precipitator. 17. KEY WORDS AND DOCUMENT ANALYSIS DESCRIPTORS b.lDENTIFIERS/OPEN ENDED TERMS Pollution Dust Emission Sampling Analyzing Error Analysis Pollution Control Stationary Sources Particulates Mass Emissions . COSATl Field/Group 13B 11G 14B 12A 8. DISTRIBUTION STATEMENT Release to Public 19. SECURITY CLASS (ThisReport/ Unclassified 21. NO. OF PAGES 49 20. SECURITY CLASS (This page} Unclassified 22. PRICE epA Form 2220-1 (9-73) ------- |