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was about twice the CWG production in the region. Sharp drops
in CWG production occurred after 1949, and coke-oven gas
production and purchases dropped at slower rates. A steady
decline in retort gas production occurred between 1928 and
1950.
• Figure 48: West North Central States--CWG production was the
major gas produced by gas companies in this region, but CWG
production dropped sharply after 1930 and showed a small
increase after World War II. Coke-oven gas purchases dropped
after 1948, and coke-oven gas production dropped to zero in
1950. Only a small amount of oil gas was produced in the
region.
• Figure 49: Pacific Coast States--Gas production in States
bordering the Pacific Ocean was principally by the oil-gas
process during this period. This figure is somewhat misleading
in that by this period California was producing and dis-
tributing natural gas, and Oregon and Washington continued to
manufacture gas. Some CWG was produced and very little coal-
carbonization gas was produced in this region. The oil-gas
production shows a very rapid decline at the end of World
War II (1945). This is because the oil-gas plants were oper-
ated at relatively high levels during the war so that by-
products needed for the war effort could be produced. Gas was
still being produced at substantial levels through 1956.
* Figure 50: East South Central States—This is the only region
examined where coke-oven gas purchases were the major source of
manufactured gas. The purchases of coke-oven gas dwarfed the
gas production by gas distributors, although CWG was produced
for several years after World War II. CWG production declined
sharply in J950, and coke-oven gas was still purchased (prob-
ably for mixing with natural gas) through about 1955. No oil
gas or coke-oven gas was produced by gas companies during this
period.
• Figure 51; Mountain States—This region had very low levels of
gas production. Retort gas and CWG were produced in 1928 but
declined sharply after 1928. Oil gas and purchases of coke-
oven g<-s predominated between 1931 and 1948. Gas production
essentially stopped in 1949.
• Figure 52: West South Central States—There was no significant
gas production in this region after 1929. There would be some
gas production before this period, however.
Figures 53 and 54 show some early information on gas production in
Massachusetts (Grimwood, 1896). Figure 53 shows the amounts of coal gas, CWG,
and oil gas produced between 1886 and 1900. This figure clearly shows the
180
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182
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increase in CWG production after 1890 while coal gas production fell, due
principally to the replacement of coal-gas retorts by CWG apparatus. Simi-
larly, Figure 54 shows the use of enriching oils increasing with increased CWG
production. Naphtha was the major carburetion oil used during this period,
but gas oil and crude oil were also used. The changes in gas-oil use and
naphtha use between 1896 and 1899 are exactly opposite. When gas-oil use
increased, naphtha use decreased; likewise, when naphtha use increased, gas-
oil use decreased. This indicates that either of the two feedstocks could be
used, with the amounts of each purchased dependent on price and availability.
The regional gas production shown in this section shows clear patterns of
variation with respect to the production methods employed in the various U.S.
regions and in the relative amounts of gas produced within the regions.
1.5.3 U.S. Gas Feedstock Trends
Just as there were trends with respect to the types of gas produced,
there were also variations of the types and amounts of raw materials used in
the production of gas. Two major types of feedstocks were used in the produc-
tion of town gas—solid carbon-based fuel and liquid oils. Figure 55 shows
the use of solid fuel for gas manufacture between 1919 and 1965. Two types of
coal (anthracite and bituminous) and coke produced from bituminous coal were
used in the manufacture of gas. Anthracite coal was used as both generator
•fuel (for CWG and producer gas) and as boiler fuel. The use of anthracite
declined before 1930 because reduced supplies of anthracite increased costs of
the fuel. Coke was used primarily in the gas generators of CWG apparatus, and
some of the coke was used for producer gas and as boiler fuel. The rise in
coke use prior to 1930 is from the increased production of CWG. Coko was
produced from bituminous coal in either retorts or coke ovens. Figure 55 also
shows the characteristic drop in fuel use during the Great Depression and
increasing fuel purchases during World War 11. The decline in solid-fuel
purchases after 1950 parallels that of the gas-manufacturing trends.
Figure 56 shows the total oil used in gas manufacturing between 1919 and
1965. Oils were used primarily for the carburetion of CWG and for the produc-
tion of oil gas, but they were also used as boiler fuels by the gas producers.
Figure 57 shows the types of oils used between 1945 and 1952. The major trend,
shown in this figure is the substantially increased use of other heavy oils
183
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186
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between 1945 and 1950. Because the production of CWG also increased during
the same period, most of this increased production used other heavy oils
(which were principally the heavy residuum oils that remained after the
catalytic cracking of gas oils). The other use of other heavy oils increased
as the use of lighter Bunker "C" oils decreased during the period, indicating
that gas manufacturers switched from the C oils to heavier oils. Because
there were more tars and lampblack created and more emulsion problems
associated with the use of the residuum oils, this change in oil feedstocks
increased the amount of waste produced by the industry.
1.5.4 Historical Events_of the U.S. Gas Industry
Table 45 is a listing of the significant events in the manufactured-gas
industry. This listing includes many of the developments in gas production,
purification, markets, and feedstock usage that affected the types and charac-
ter of waste produced by the town gas industry.
1.6 DIFFERENCES BETWEEN THE U.S. AND BRITISH GAS INDUSTRIES
The redevelopment of gas production sites has occurred much more fre-
quently in Great Britain than it has in the United States. The Harwell report
on the problems arising from the redevelopment of gas sites (Wilson and
Stevens, 1981) was published several years before a somewhat similar work was
published in the United States (Handbook on Manufactured Gas Sites, Environ-
mental Research and Technology [ERT], 1984). There is a tendency to apply the
information from the British work on site redevelopment directly to U.S.
sites. This section outlines the major differences between the U.S. and
British gas industries, and it relates those differences to current waste
problems at U.S. sites.
In the United States, the availability of petroleum and petroleum distil-
lates encouraged their use for the production and enrichment of town gas.
British gas was primarily coal gas and coke-oven gas, reflecting the abundance
of coal in the United Kingdom and the absence of significant oil resources.
Because the tars produced from oil-gas and CWG production are generally less
viscous than coal tars, the problems of tar migration from the U.S. facilities
are probably greater than are the tar migration problems associated with the
U.K. coal-gas plants.
187
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TABLE 45. SIGNIFICANT EVENTS OF THE TOWN GAS INDUSTRY
Year
Event
Reference3
1806 A home and street lighted by manufactured gas in
Newport, RI
1809 Milk of lime used for H2S removal in Britain
1812 Company chartered to light London streets
1315 English patent for oil-gas production issued
1815 English patent for oil-gas process issued
1816 First U.S. coal-gas company incorporated
1816 Coal-gas plant installed in Baltimore, MD
1316 First public display of gas lighting in Baltimore, MD
1820 First coal-tar distillation plant started in England
1322 Coal-gas plant installed in Boston, MA
1325 Coal-gas plant installed in New York, NY
Tunis,
1933;
Morgan,
1926
Powel1,
1945o and
1945b
Rhodes,
1966a
Rhodes,
1966b
Hull and
Kohloff,
1952;
Rhodes,
1966b
Hull and
Kohloff,
1952
Rhodes,
1966a;
Morgan,
1926
Tunis,
1933
Rhodes,
1966a
Rhodes,
1966a;
Morgan,
1926
Rhodes,
1966a;
Morgan,
1926
(continued)
188
-------
Year
TABLE 45 (continued)
Event
Reference3
1829 Water-sealed gas holder used in England; masonry tanks Alrich,
were used to hold the water 1934
1838 First timber treated with coal tar in England
1838 Heavy oil (creosote) first used to preserve wood from
decay and marine worms
1847 First benzene recovered from coal tar in England
1849 Iron oxide process for H2S removal patented
Rhodes,
1966a
Stover
and
Chung,
1979
Rhodes,
1966a
Powell,
1945a and
1945b
Around
1850
Before
1850
1850
1856
Horizontal firebrick retorts were commonly used for
coal-gas production
Cast iron retorts used for coal-gas manufacture,
600-800 *C
Clay retorts used for coal-gas production instead of
cast iron
Dye from light-oil fraction of coal tar discovered;
analine dyes follow this discovery
1856 First coke ovens with byproduct recovery installed in
France
1857 Dye manufactured from coal-tar products in England
1860 British "Sulfur Act of 1860" limited sulfur in
gas to 22 grains per 100 cubic feet
Rhodes,
1966a
Rhodes,
1966a
Morgan,
1926
Stover
and Chung,
1979
Morgan,
1926
Rhodes,
1966a
Powell,
1945a and
1945b
1859-
1900 Air-cooled condensers used to cool manufactured gas
Downing,
1934
(continued)
189
-------
IABLL 4b (continued)
Year
Early
1860's
1861
1865
1869
1870
1870
1870
1872
1876
1877
1880
1882
1884
Event
First U.S. coal tar distilled In Boston, MA
Three-lift holder tank introduced in England
Phenol recovered from coal-gas liquids for antiseptic
purposes in England
Dyes manufactured from coal tar
Fontana identified Blue Gas by passing steam over
incandescent carbon
Water gas (blue gas) discovered; 330 Btu/ft^, very
poor luminosity
Iron oxide purification introduced to U.S.
T.S.C. Lowe invents carbureted water gas; it has higher
heating value and luminosity than does coal gas
First iron gas holder tank installed in U.S.
Antiseptic and deodorizing solutions produced from
tar-acid oils in England
Indigo produced from coal tar
A considerable percentage of the gas output of the
country was carbureted water gas
Use of down stream for carbureted water-gas production
introduced
Reference3
Lane,
1921
Alrich,
1934
Rhodes,
1966a
Stover
and Chung,
1979
Morgan,
1945
Rhodes,
1966b;
Morgan,
1926
Powell,
1945a and
1945b
Rhodes,
1966b;
Morgan,
1926
Alrich,
1934
Rhodes,
1966a
Stover
and Chung,
1979
Morgan,
1926
Morgan,
1926
(continued)
190
-------
TABLE 45 (continued)
Year
Before
1885
1886
1887
1888
1889
1885 -
1890
1892
1894
1894
1900
Before
1900
After
1900
Event
Lime used as purifying agent to remove C02, H2S, and
organic sulfur
Mantles introduced for gas lighting
First U.S. tar distillation plant installed in
Philadelphia, PA
First steel gas holder tank installed in U.S.
L.P. Lowe patents oil-gas process in the U.S.
Development of rusted iron borings (iron oxide) process
for H2S removal
First U.S. byproduct coke oven installed in Syracuse, NY
(10 years after England and Germany)
First three-lift holder tank installed in U.S.
Byproduct coke plant erected in Johnstown, PA
Pacific Coast oil -gas process developed
Tar removal by bubbling gas through strong ammonia
solution (Livisey washer)
Water-cooled condensers used to cool manufactured gas
Reference3
Downing,
1934
Forstall ,
1934
Rhodes,
1966a
Alrich,
1934
Rhodes,
1966b;
Morgan,
1926;
Hull and
Kohloff,
1952
Downing,
1934
Rhodes,
1966a;
Morgan,
1926
Alrich,
1934
Lane, 1921
Hull and
Kohlhoff,
1952
Downing,
1934
Down i ng ,
1934 i
(continued)
191
-------
TABLE 45 (continued)
Year
Before
1900
Around
1900
Early
1900's
Early
1900 's
1901
1902
1902
1902
1903
1905
1907
1907
1910
1910
1910
Event
Luminous flame burners used for lighting
Vertical retorts used to produce coal gas
Light-oil recovery scrubbers introduced
Direct-contact washer-cooled with P and A tar extractor
introduced for tar removal
Steel gas holder tanks preferred to brick holder tanks;
steel tanks were now cheaper
First use of crude oil in a carbureted water-gas plant
in California
First oil-gas plant installed in Oakland, CA
First oil-gas plant in U.S. installed 1n Oakland, CA;
uses the Pacific Coast oil-gas process
Carbureted water-gas industry begins change from
paraf fink-based oils to asphaltic-based oils
Lime scrubbing replaced by Iron Oxide Purification
in Britian
Centrifuges introduced for separation of emulsions
Washer-cooler introduced; contacted gas directly with
recirculated condensate from gas
Turbo exhauster; used to increase the pressure of
manufactured gas flowing to scrubbers
Aluminia from bauxite used for 83$ removal; this process
was not used very much
First use of water-gas tar to preserve railraod ties;
tar mixed with ZnCl prior to wood treatment
Reference3
Forstall ,
1934
Morgan,
1934
Downing,
1934
Downing,
1934
Alrich,
1934
Morgan,
1926
Morgan,
1926
Rhodes,
1966b
Fischer,
1933
Powell ,
1945
Fischer,
1933
Downing,
1934
Downing,
1934
Downing,
1934
Fulweiler,
1921
(continued)
192
-------
TABLE 45 (continued)
Year
1912
1915
1916
1916
1919-
1920
1920
1920-
1929
1921
1921
1925
1929-
1932
1929-
1932
Around
1930
1930
Event
Refiners start cracking petroleum oils to increase the
production of gasoline
World War I spurs development of tar recovery and use in
the U.S.; demand for tar products increases
Water purification process using lime and copperas
(FeS04) followed by coke filter described
Dry-gas holders introduced
Production and prices of coal-tar chemicals dropped
after World War I
Out of the 917 gas plants 1n the U.S., 596 of them are
carbureted water gas
Growing use of phenolic and alkyd resins promotes the
recovery of naphthalene and phenol
Seaboard process for h^S removal introduced
Seaboard liquid process for H2S and HCN removal
developed by the Koppers Co.
Nickel process for H2$ removal and sulfur recovery
invented
....
Great Depression cuts deeply into prices and production
of tar-based chemicals
Horizontal and vertical retorts abandoned or replaced
by oil gas, water gas, or natural gas
Use of heavy fuel oils for oil and carbureted water gas
begins
High surface area iron oxide sponges introduced; they
had double the S removal of homemade FeO
Reference3
Rhodes,
1966b
Rhodes,
1966a
Hansen,
1916
Alrich,
1934
Rhodes,
1966a
Rhodes,
1966b
Rhodes,
1966a
Denig and
Powel 1 ,
1933
Sperr,
1923
Cundall ,
1927
Rhodes,
1966a
Rhodes,
1966a
Rhodes,
1966a
Downing,
1934
(continued)
193
-------
TABLE 45 (continued)
Year
Event
Reference3
Early
1930's
Early
1930's
1932-
1945
Electrostatic precipitation for tar removal introduced
Tetralin (tetrahydronaphthalene) used to remove
naphthalenes from gas
World War II greatly increased demand and production
of tar-based chemicals
1933 Seaboard H2S removal process installed at 30 plants
1938 Catalytic cracking of crude-oil residuals by refineries
produces high yields of gasoline and gas oil
1949 Federal Power Commission allows certain pipelines that
previously transported oil to carry natural gas
Downing,
1934
Downing,
1934
Rhodes,
1966a
Denig and
Powell,
1933
Pew, 1940
Rhodes,
1966b
194
-------
Land area for the production of gas was generally more available for the
U.S. plants. There was more area for onsite disposal of waste products and
less need to use underground structures for storage (and placing other struc-
tures directly over underground structures).
British town gas sites closed when North Sea natural gas became available
(1967 through 1974). U.S. plants had closed much earlier when pipeline nat-
ural gas from western fields became available (1945 through 1955). Because
the U.K. plants closed later, during a period of increased environmental con-
sciousness, they were generally better decommissioned than were the U.S.
plants.
Britain, a relatively small country, was more homogenous in the produc-
tion techniques and purification processes employed. In the United States,
different production processes were employed In various areas of the country
to take advantage of local resources and markets. Markets for byproducts were
frequently more accessible in Great Britain than they were in the United
States. This meant that the recovery of byproducts was practiced more
extensively in the United Kingdom than it was in the United States. Products
discarded for economic reasons in the United States would frequently be
recovered in the United Kingdom.
Sale and recovery of sulfur from spent oxide was practiced (and profit-
able) in Great Britain. Spent oxide was viewed as a usable byproduct from the
manufacture of gas. The sale and recovery of spent oxide was employed at very
few U.S. plants, and spent oxide was universally viewed as a waste for dispo-
sal. Because spent oxide was utilized in Great Britain, gas plants disposed
less of it and had much less incentive to switch to liquid purification proc-
esses for H2S removal. -The quantities of spent oxide wastes disposed in the
United States were consequently a larger percentage of the spent oxides pro-
duced than were those disposed In the United Kingdom.
Tars and oils recovered from town gas production were more valuable in
Great Britain than they were in the United States (due to higher petroleum
prices in Great Britain). Disposal of tars and oils was much less likely in
Great Britain than it was In the United States. Because coal tar was
generally regarded as more valuable than CWG tars or oil tars, more of the
tars produced in the United Kingdom would have been recovered.
105
-------
The United States was much slower than was Great Britain in distilling
coal tar and recovering coal-tar byproducts. The United States did not start
recovering coal-tar chemicals on a large scale until World War I. This was
due in part to the importation of coal-tar chemicals from Germany and Europe
and also to the use of CWG in the United States. Because CWG tars did not
contain many of the most valuable chemicals in coal tar (e.g., anthracene,
used in the production of dyes), there was less incentive to process the tars
for recovery.
1.7 CONCLUSIONS FROM THE HISTORICAL REVIEW
Three major processes were used for the production of town gas in the
United States. These were (1) coal carbonization, (2) carbureted water gas
(CWG), and (3) oil gas. In general, all three processes were employed in all
areas of the United States, but each process became predominant in specific
geographical ereas in the United States. Gas plants along the West Coast
started as coal-gas plants, switched to CWG, then converted to oil-gas
production. Plants along the East Coast were generally CWG, with some coal-
gas production, and coal-gas production was predominant in the Middle States.
Because the gas purification processes, byproducts, and wastes from the gas
production varied with each production method, it is important to understand
the specific production methods and associated byproduct recovery operations
of individual gas sites.
The feedstocks used in gas production changed during the operation of gas
plants. The coal used for coal carbonization did not change substantially
over time, but the carbon and hydrocarbons used for CWG production and oil-gas
production changed substantially over time, which had a significant effect on
the wastes produced. CWG production originally used coke or anthracite coal
in the generator and low-boiling naphtha fractions «s hydrocarbon feedstock;
Later, bituminous coal often was used directly in the generator, and the
hydrocarbon feed was switched first to gas-oil fractions, and later to heavy
fuel oils and residual oils. Oil gas originally utilized either gas-oil frac-
tions of petroleum or crude oil, but later switched to heavier fuel oils and
residual oils. The choice of feedstocks was determined by the prevalent eco-
nomics of the oil industry during the production of town gas. The conversion
from lower-boiling petroleum fractions (naphtha and gas oil) to heavier oils
196
-------
'If
(fuel oil and residual oil) was accompanied by increases in the tars produced
by the processes and the increased formation of tar-water emulsions. For oil-
gas production, the amount of lampblack produced per 10& ft^ gas manufactured
increased with the conversion to feedstocks with higher carbon contents. The
emulsions that formed were often difficult to separate, and they were often
discarded when separation attempts failed.
Coal carbonization produced a fuel gas containing substantial amounts of
ammonia, cyanide, phenolic compounds, and hydrogen sulfide. The presence of.
these chemicals determined the cleanup processes for their removal from the
gas and any recovery processes. They also appeared in the wastes from coal
carbonization. In contrast, both CWG and oil gas contained only small amounts
of nitrogen compounds (ammonia and cyanide) and only trace quantities of
phenols. All three processes produced gas containing hydrogen sulfide.
Ammonia and phenol were not produced, removed, or recovered from CWG and oil
gas, but they were from coal-carbonization gases. This relatively simple
correlation explains much of the variation seen currently at sites. The
absence of phenols in tars from Stroudsburg, Pennsylvania (oil and CWG), and
Ames, Iowa (CWG), are two more prominent examples. Iron oxide was used almost
universally to remove hydrogen sulfide from town gases. The iron oxide also
reacted with hydrogen cyanide in the gas to produce blue iron cyanide
complexes. These ferriferrocyanides are relatively stable, and they persist
at gas sites that produced coal gas and disposed spent oxides onsite (an
almost universal practice). They are the most visible waste at plants that
produced coal gas, but they are absent from plants that produced only oil gas
or CWG.
The removal of hydrogen sulfide was required for all three gas production
processes, with the amount of hydrogen sulfide removal required being depen-
dent on the coal sulfur concentration for coal-carbonization gases or the
sulfur concentration in oil for oil gas and CWG. Between 1816 and 1855, lime
was used for the removal of hydrogen sulfide and other impurities from town
gas. Lime use was characterized by low conversion of the lime to CaS, diffi-
cult disposal problems, and high cost. The use of lime was essentially
replaced by iron oxide purification after 1890. Both the lime and spent i
oxide were considered wastes; although there were many attempts to use them
107
-------
for some productive purpose, they were universally disposed. Lime use
occurred primarily during a period when the cost of town gas was very high,
and it was used principally to light only streets and shops in cities. With
the introduction of iron oxide purification, gas prices dropped and gas became
a larger consumer item. Spent lime wastes were not a significant problem at
most U.S. sites because of the low gas production rates during the time that
lime was used. Spent lime was also used for agricultural purposes, which
reduced the amounts of spent lime that had to be discarded. Because lime was
also used in the recovery of ammonia from coal gas, spent lime sludges from
ammonia recovery are possible at most coal-gas plants that recovered ammonia
(but it would be present in much smaller quantities than if used for hydrogen
sulfide removal). Spent iron oxides, however, are the predominant waste from
the removal of hydrogen sulfide.
Spent iron oxides were universally regarded as wastes, and they were
often used as a general fill material around gas plants. They constitute a
major discarded waste that can be located on most sites. Unfortunately, there
is wide variation in the composition of spent oxide wastes, which hinders
characterization efforts. Organic hydrocarbon content, sulfur content, cyan-
ide content, and mixtures with woodchips are all variables affecting the cur-
rent composition of spent oxide wastes.
Alternatives to the use of iron oxide for hydrogen sulfide removal were
introduced after 1921. The Seaboard process used a solution of sodium carbon-
ate to scrub hydrogen sulfide from the gas. Solutions were regenerated by
blowing air through the.scrubbing liquid, rereleasing the hydrogen sulfide to
the atmosphere. A process usi-ng a solution of arsenic salts to remove hydro-
gen sulfide and recover it as a sulfur was introduced around 1925. This
process would be accompanied by possible arsenic contamination of sites,
especially if spent solutions were disposed. This process was frequently used
upstream of iron oxide beds (the arsenic process would remove most of the
hydrogen sulfide, and the iron oxide would reduce the hydrogen sulfide content
of the gas to very low concentrations). The spent oxide waste from this type
of operation would have potential arsenic contamination resulting from
carryover of the scrubber solution.
The composition and characteristics of coal- and water-gas tars varied
substantially among plants. Water-gas tars and oil-gas tars tend to be very
198
-------
similar In composition and properties because both are essentially produced by
the thermal cracking of petroleum fractions. They tend to be less viscous
than are coal gas tars, and they contain only trace amounts of phenolic and
base nitrogen compounds.
The formation of tar-water emulsions was a major problem of the industry,
and it frequently resulted in the disposal of these oily materials when the
emulsions could not be broken. Water and tar are condensed simultaneously in
the purification of town gas. The resulting mixture of tar, oils, and water
would usually separate into layers, and the tar and oil could be recovered.
When emulsions formed, the tar would not separate from the water, and the
gravity separators frequently used for the separation would not function.
Emulsions were rarely formed from production of coal gas, but were a frequent
problem for both carbureted water-gas production and oil-gas production.
Emulsions could generally be separated by mechanical and thermal methods, but
occasionally emulsions would form that defied all attempts at separation.
These emulsions were disposed by any means available, including the use of
open, unlined lagoons, direct discharge to bodies of water (where feasible),
or into any convenient unused well. Lagoons were frequently used for storage
of emulsions. This allowed additional time for the emulsions to separate by
gravity or for alternative batch methods of separation to be used. The plant
at Plattsbugh, New York, utilized lagoons for the storage and disposal of tar-
water emulsions.
The formation of emulsions became more prevalent when oil and CWG pro-
ducers switched from lower-boiling petroleum fractions to heavier and higher
carbon-content residual oils.
Tars and oils were generally recovered from the production of town gases.
Although early plants disposed essentially all of their tars and waste conden-
sates (usually to the nearest body of water), they rapidly discovered that
this waste was worth recovering. Coal tars could be separated by gravity from
the condensate and oils. These tars could then be either burned (as fuel in
the retorts or boilers), refined and sold, or sold as a raw byproduct. Water-
gas tars were recovered and sold as a liquid fuel, burned in the plant's own
steam boiler, or recycled back into the hydrocarbons used for cracking into
the gas. All tars had a minimum value to the plant as fuel because the tars
199
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could replace a portion of the coal that would normally be burned at the
plant.
Several specific practices contributed to the contamination of gas pro-
duction sites by tars and oils. Many of the original gas holders for plants
were partly buried below ground and frequently filled with coal tar. They
were usually not well sealed at the base, and some of the tar contained in
them leaked into the ground. Tar wells (tar storage tanks) and tar separators
were frequently constructed underground of masonry or cement, and they often
leaked. Some storage tanks were constructed of wood. Wastes were usually
disposed either at the plant site or adjacent to the plant. These practices
indicate that any former gas site will probably have some tar and oil contami-
nation, with the extent of contamination being dependent on the specific prac-
tices of the plant.
Most of the byproducts from town gas production could be considered
either products or wastes, depending on the prevailing price that could be
obtained for the byproduct. Spent iron oxide was always considered a waste,
in spite of continuing attempts to develop uses for the material. Recovered
tars could be sold, but they had a minimum fuel value that determined their
value as a fuel. Plant size and access to markets were two of the primary
factors that influenced the waste disposal practices of gas production plants.
Smaller plants did not have the same economy of scale as did the larger
plants, and frequently they did not recover materials that the larger plants
recovered extensively. This was particularly true of small water-gas and oil
plants, which sometimes let the tars and condensates flow to waste rather than
attempt to recover any o-f the tar. Transportation costs of shipping tars or
ammonia liquors to appropriate markets frequently prevented the sale of by-
products that might have b^en worth recovering.
There is a substantial tendency to apply the work done in the United
Kingdon with old town gas sites to U.S. plants. There are, however, several
substantial differences between plants in these two countries. First, the
United States had abundant petroleum resources, which made the use of CWG and
oil gas practical. The United Kingdom had only limited petroleum resources
and produced coal gas almost entirely. Coal tars and tar products also com-
manded a higher price in the United Kingdom than they did in the United
200
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States, thereby encouraging United Kingdom plants to recover these byproducts.
The market for spent oxides in the United Kingdom was well developed (it was
used for the manufacture of sulfuric acid); low sulfur prices in the United
States prevented the development of any markets for spent oxides. Similarly,
liquid-scrubbing methods for the removal of hydrogen sulfide from gas were
developed in the United States, but the United Kingdom plants continued to use
iron oxides because they could market the spent oxides. Gas plants in the
United Kingdom also were generally placed on smaller sites than were those in
the United States. Consequently, wastes from U.K. plants would be more likely
to be hauled away to disposal sites, rather than discarded onsite.
After the first natural gas pipelines were installed in an area formerly
served by manufactured gas, the natural gas was generally used to meet base-
line demand, and the manufactured-gas plant was modified to produce gas for
mixing with the natural gas to meet peak demands. As larger pipelines were
installed for natural gas delivery and better storage methods for natural gas
became available, the need for a standby gas production facility evaporated.
The manufacturing plants were generally idle for several years before they
were decommissioned. The most frequent reason for decommissioning the plants
was to remove structures from the site and reduce the site valuation for tax
purposes. The purpose of site decommissioning was to remove surface struc-
tures from the site. Gas storage tanks were cut off at ground level, and the
tanks were filled with debris from the plant site. Underground tanks and
structures were rarely removed, and some tanks and tar separators were left
filled with tar or liquid wastes. Many gas companies still own the original
sites used for the manufacture of gas, in that it is generally much cheaper to
keep the site as unused-land than it would be to clean the site for sale.
During the literature review, RTI discovered that the literature describ-
ing the operations of gas plants is very substantial. This is not surprising
in that the manufacture of town gas was once a large industry. Several refer-
ences were discovered that deal specifically with the waste disposal practices
and problems of the U.S. industry. These articles indicate that groundwater
contamination in areas around gas sites was common while the plants were in
operation and that contamination of downstream water supplies was also a com-
mon problem.
201
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2.0 INVESTIGATION AND REMEDIATION OF TOWN GAS SITES
The investigation and remediation of abandoned town gas sites is a large
task, considering the large number of sites that have been discovered and the
even larger number that remain undiscovered. Contacts made with State and
Federal agencies during the course of this project indicated that, of the
sites that have been discovered, only a few have progressed beyond preliminary
assessments, and fewer still have had remedial actions implemented to address
contamination. Thus, site investigation activities and remedial action activ-
ities at town gas sites should increase markedly over the next few years.
As with any uncontrolled site contaminated with potentially hazardous
chemicals, site investigation activities should focus on determining threats
to human health and the environment posed by the site and on generating the
information necessary to evaluate and select remedial alternatives. Selection
of remedial alternatives should concentrate on cost-effective alternatives
that effectively mitigate the threat, with an emphasis on treatment or des-
truction alternatives that eliminate the hazardous nature of the wastes. This
chapter discusses the behavior of contaminants commonly occurring at abandoned
town gas sites, reviews current practices in investigating and remediating
these sites, and presents recommended practices based on this review. The
case studies, presented in Chapter 3, provide background information support--
ing the information presented in this chapter.
2.1 CONTAMINANT BEHAVIOR AND FATE
The most commonly occurring and environmentally significant contaminants
at abandoned town gas sites are byproduct tars and oils and spent oxide
wastes. Significant aspects of the behavior of these contaminants in the
subsurface environment are discussed in the following sections.
Preceding page blank 203
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?.1.1 Byproduct lars and Oils
Byproduct tars and oils represent multiple-density contaminants at gas- (
works sites. For the purpose of this discussion, byproduct oils are defined
as liquid hydrocarbon from gas manufacture with densities less than water;
byproduct tars are defined as liquid hydrocarbons with densities greater than
water. These substances are of concern environmentally because of their
potential to contain high concentrations of carcinogenic compounds, such as
PAH's and nitrogen heterocyclics. From the standpoint of groundwater contami-
nation, the byproduct oils are of most concern because of their higher solu-
bilities and tendency to float on the watertable, where soluble components may
be leached out by infiltration. The byproduct tars are also of concern, how-
ever, because of their potential to flow in density currents through subsur-
face fractures and coarse-grained deposits. A discussion of the hydrogeologic
behavior of these immiscible, variable density contaminants adapted from Alex-
ander (1984) follows.
Byproduct tars and oils from gas manufacture a e immiscible fluids and as
such do not readily mix with groundwater. The flow of immiscible fluids is
more complex than is the flow of soluble contaminants. An immiscible fluid
that is more dense (e.g., tar) than water will migrate according to the com-
bined effects of relative density and the fluid-fluid and fluid-solid inter-
facial pressures. Because of the density contrast, the fluid will generally
sink within the groundwater. Lighter hydrocarbons, such as byproduct oil,
will generally "float" on the water table or on the tension-saturated zone.
The existence of capillary pressure in a two-phase flow system means that the
migration of an immiscible fluid is not entirely dependent on the flow of
groundwater and, as a result, can migrate in an opposite direction of the
dominant flow system. It is not uncommon in spills of low-density fluids, for
example, for the fluid to migrate "upgradient" of the groundwater flow system
within the capillary fringe. The theoretical aspects of multiple-phase flow
of hydrocarbons in the subsurface are discussed in detail by van Dam (1967).
One of the biggest problems associated with the release of the lighter
hydrocarbons into the subsurface is that their relative solubility increases
204
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the volume of groundwater that is contaminated. Rainwater that percolates
through the "pancake" of light hydrocarbons typically formed over the ground-
water body eventually weakens the concentration of oil causing dissolved com-
ponents of the oil to enter and be transported by the flow of groundwater
(Dietz, 1971).
An example showing the soluble component of an immiscible contaminant is
provided in Figure 58 with the following designation of zones (from Pfannkuch,
1982):
• Zone I is the above-ground and surface zone where leaked or projec-
ted oil runs off ard collects in surface depressions, thus forming
the area from which infiltration takes place. The configuration of
this area depends on the local topography, the amount spilled, and
the conditions of release or eruption.
• Zone II is the soil profile. From Zone I the oil starts infiltra-
ting into the subsurface via the organic soil layer, if such a layer
is present. This zone is characterized by its high organic content
and high moisture content due to soil structure. If the soil is
oleophilic, it has a much higher oil retention capacity than do the
underlying nonorganic deposits.
• Zone III is the vadose or unsat'irated zone. This is the most impor-
tant zone for oil retention. Water saturates the pore space only
partially and ranges in value from zero to field capacity. Oil, as
the nonwetting phase, moves downward under the forces of gravity.
At first it moves as a more or less continuous phase or "oil body,"
displacing excess water from the larger pores. When all oil has
infiltrated from the surface, the "oil body" will move downward by
translation, but small amounts of oil will be left behind the trail-
ing end, trapped as insular disconnected droplets. The oil body
continues to move in a disintegrated fashion until all of the oil is
trapped in the pore spaces of the vadose zone if its total retention
capacity exceeds the infiltrated spill volume. Any oil in excess of
this total retention capacity reaches the groundwater body and
spreads on the water table through the capillary fringe.
• * Zone IV is the capillary fringe that is partially watersaturated,
directly connected with the groundwater body vertically, but contin-
uous laterally. When excess oil reaches this zone, it will spread
laterally under its own hydrostatic pressure and form a lens on the
water table. The spreading will halt when the hydrostatic forces in
the oil phase are counterbalanced by the capillary forces at the
outer edges of the spreading oil lens. This movement is governed by
the phenomena of relative permeabilities and multiphase flow in
porous media.
205
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SURFACE
Vwr: VVATIR TABU GROUNDWATER FLOW
CF : CAPILLARY FRINGE
I Surface zone
II Soil profile
III Vadose zone (unsaturated)
IV Capillary fringe
V Groundwater body
Source: Pfannduch, 1982.
Figure 58. Subsurface propagation of a nonmiscible containment.
206
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If the porous medium is homogeneous and Isotropic and the water
table is horizontal, then the oil lens would be perfectly circular
around the center of infiltration. In most realistic cases, the
water table has a slope that gives rise to an elliptically elongated
lens extending in the direction of the flow. The shape of this lens
depends on the water-table gradient, groundwater flow velocities,
the capillary properties of the multiphase flow system, and the
shape and orientation of the original infiltration area.
• Zone V is the groundwater body. Most hydrocarbon compounds in a
spill are lighter than water and therefore tend to float on the
water table. Under the hydrostatic head of the continuous oil
column, an actual depression and penetration of the groundwater body
below the water table occurs. This inverted mound will dissipate as
the overlying oil body spreads laterally. The penetration and sub-
sequent retraction may result in leaving trapped insular oil behind
in the groundwater body. The most important feature of Zone V in
the emplacement stage is the formation of an interface between the
bottom of the oil lens and the free-flowing groundwater. It is at
this interface that small but significant amounts of hydrocarbon
compounds go into solution with the water and are spread by convec-
tive and dispersive transport mechanisms.
Model experiments have been useful for studying the mechanism of low-
density oil spread in porous media above the water table (Schwille, 1967).
The seepage and spreading of heating oil in layers of varying hydraulic con-
ductivity and hydraulic gradients are shown in Figure 59. The oil seeps
downward under the influence of gravity, and its geometry is influenced by the
rate of infiltration, the hydraulic conductivity, capillarity, and the hydrau-
lic gradient.
Multiple discharges of different kinds of chemicals can lead to a complex
pattern of contaminant plumes (Figure 60). In this example, the heavy petro-
leum product that is denser than water is flowing down the slope of the con-
fining bed in an opposite direction to the flow of dissolved and low-density
products. Migration of heavy coal-tar derivatives through density currents is
illustrated by a case described by Berggreen (1985), in which creosote has
migrated along slickensides (fractures) in a low-permeability clay to bedrock
at a depth of 120 feet. Byproduct tar migration through density currents is
illustrated by the Brattleboro, Vermont, and St. Louis Park, Minnesota, case
studies in Chapter 3.
207
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I 3 t oil
oo
BOO
— z_-
«s«*
na°sT
fioSJ
i i 1
iii
S 3 =
1 1 1 1
s ss a
sa
goo
51 all
100cm
Source: Schwille, 1967.
Figure 59. Seepage and spreading of heating oil in porous media
above the water table.
208
-------
SOURCE OF PRODUCT
( CnqUr dinilly than woltf)
SOURCE OF PRODUCT
( UttMr <«n«itj than wttr )
OIReCTION Of
GROUND-WATER FLOW
CONFINING BED
Source: Miller, 1983.
Figure 60. Effects of variable density migration in the subsurface.
209
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2.1.2 Spent Oxides
Spent oxides are extremely heterogeneous and variable in nature, as dis™
cussed in Chapter 1. The most significant contaminants in spent oxide wastes
are sulfuric acid, arsenic, and complexed iron cyanides. These complexed
cyanides occur in the form of ferric ferrocyanide, imparting a blue color to
the spent oxide wastes.
There has been considerable research on the fate and transport of cyanide
compounds in the environment by the mining and mineral-processing industry,
which uses cyanides to leach metal-containing ores. A recent symposium (van
Zyl, 1984) summarized the state of knowledge on this subject, but it also
pointed out many gaps in the knowledge necessary to predict environmental
impacts accurately. Many of these gaps concerned iron cyanide complexes.
Conclusions from this symposium of relevance to this study are:
• Low levels of free cyanides do not persist to soils because of bio-
logical and chemical degradation. Biological degradation in soil is
inhibited by concentrations of 2 ppm free cyanide under anaerooic
conditions and 200 ppm free cyanide under aerobic conditions.
• Ferro- and ferricyanide complexes in solution are photodecomposed to
free cyanide. Their toxicity in water is related to the degree of^j
decomposition. ~
• When KCN in municipal landfill leachate is passed through saturated,
anaerobic soil, Prussian blue (ferric ferrocyanide) precipitates and
accumulates in the uppermost soil layers. This suggests that Prus-
sian blue is quite immobile in soil.
Tree cyanide migration in saturated, anaerobic soils increases with
increasing CaC03 content and decreases with increasing concentra-
tions of Mn and hydrous iron oxides.
• Complexed iron cyanide (Fe(CN)g~3) migration in saturated, anaerobic
soils is retarded by high free Fe03 and increases with increasing pH
and CaCO] content. At low pH, iron cyanide mobility decreases with
increasing clay content.
This information suggests that complex iron cyanides are relatively immobile
in a municipal landfill environment and that chemical treatments may be devel-
oped for complexed iron cyanides that will limit releases of free cyanides in
the soil environment to levels that can be biologically degraded.
210
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2.2 SITE INVESTIGATION
2.2.1 Introduction
Our review of case studies (Chapter 3) and assessment of past disposal
practices (Chapter 1) have indicated that appropriate procedures for conduct-
ing hydrogeological investigations of town gas facilities are not signifi-
cantly different from those used for investigating uncontrolled chemical and
industrial waste sites. The primary difference is that town gas sites gener-
ally tend to be older, and less background information is available about past
site activities. In many cases, the present-day site has been cleared, and
little or no evidence of past site activities is visible at the ground sur-
face. As a result, research into historical records often is necessary to
determine the physical layout and operating history of the plant. As with any
investigation of an industrial site, it is extremely important to utilize
process information to help determine what contaminants may be present at the
site and where these materials may be located.
2.2.2 Current Practices
Most investigations of manufactured-gas plant sites rely on conventional
site investigation methods that are not significantly different from contami-
nation investigations of other industrial sites. These methods include sur-
face water sampling, shallow soil and groundwater sampling (from borings and
test pits), and, when necessitated by the results of these sampling activi-
ties, more extensive groundwater monitoring. In many instances, these methods
appear adequate for an initial understanding of the potential for adverse
impacts on human health and the environment. A typical approach used in the
investigation of manufactured-gas plant sites is summarized in Table 46.
Actual case studies are presented in Chapter 3 of this report.
It is apparent from RTI's review of relevant case studies (Chapter 3)
that other potentially useful (and often cost-effective) alternative tech-
niques of investigation, such as geophysics and soil-gas sampling, have not
been extensively employed at manufactured-gas sites to date. However, based
on limited use at manufactured-gas sites and more extensive utilization at
industrial waste sites, these techniques show potential utility for screening
sites to optimize sampling and analysis plans.
211
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I
In a manufactured-gas site investigation in Wallingford, Connecticut,
ground-penetrating radar was used to estimate the location, extent, and char-
acter of tar ponds, in cases where no records were available. The ground-
penetrating radar demonstrated that the tar had migrated well beyond the orig-
inal pond location and the site boundary. Magnetometer surveys were used to
locate buried pipes extending from the tar pond to a former lake bed, which
could later be investigated by a grid of soil-test borings. Additional geo-
physical tools used in this investigation included seismic refraction to
assist in the definition of the depth to bedrock (a potential controlling
factor in the subsurface migration of high-density contaminants; see Brattle-
bo ro case study, Chapter 3) and electrical resistivity to outline locations of
potential groundwater contamination (Quinn et al., 1985). Ground-penetrating
radar also has potential for estimating the location and extent of lighter
hydrocarbons that may be floating on the groundwater table (Stanfill and
McMillan, 1985).
Soil-gas sampling has potential for delineating contamination at a gas
plant site when the more volatile fractions of gasifier tar (e.g., benzene,
toluene, xylenes, naphthalene) are present at a site. An investigation con-
ducted at the Spencer, Massachusetts, town gas site illustrates this potential
applicability. During test pit excavation, site air was screened for volatile
organics using a photoionization meter. These measurements were made to
assess potential air quality impacts' of excavation activities, which were
demonstrated to be minimal. However, air in the test pits had substantial
concentrations of volatile organics (>200 ppm), levels of concern from the
standpoint of occupational safety (Perkins Jordan, 1984). Although the small
size of this site would limit the value of using soil-gas sampling as a site
investigation technique, the levels of volatile organics suggest that it may
be used to help guide sampling and analysis activities at larger, more complex
sites.
A discrepancy commonly encountered in the gasworks site investigations
reviewed by RTI is insufficient information on the processes that operated at
the specific sites. Most site assessments reported that gas was produced by
coal pyrolysis or carbonization (i.e., retort or coke-oven gas); most of these
sites actually were carbureted water-gas (CWG) plants. The difference is
215
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significant, both in terms of waste characteristics and byproduct utilization
practices (see Chapter 1). For instance, nitrogen and sulfur compounds are
more prevalent in coal carbonization tars than in tars from CWG processes.
Tar emulsions produced by CWG processes were hard to dewater. As a result,
they were not reused and were disposed onsite, especially in smaller plants.
Spent oxides from CWG cleanup processes often do not have the brilliant blue
color often considered a characteristic of spent oxides because of the absence
of significant levels of ferrous ferricyanides. One site assessment report
reviewed under this study identified a mixture of yellow and red cinders, but
it failed to recognize the material as spent oxide from the small CWG plant.
It was not sampled or analyzed, but it could have been a source of contami-
nants at the site. Historical background information of the gas industry is
invaluable in planning and conducting gas plant site investigations because it
can provide data on the characteristics and likely disposition of potential
contaminants at site.
2.2.3 Recommendations for Site Investigations
2.2.3.1 Introduction--
As discussed in the previous section, site investigation techniques
employed for hazardous waste site investigations are generally applicable to
former manufactured-gas sites. However, some special considerations should be
taken into account when conducting site investigations in order to focus the
investigations on characteristic features of these sites. First, as described
in Chapter 1 of this report, contaminants, especially gasifier tar and oil,
often are contained in below-ground structures that were covered over and left
when the plant was decommissioned. Gasworks site investigations initially
should concentrate on identifying these structures because they often contain
almost pure contaminants. Because such contaminants are contained, they are
relatively easy to remove, and because they may be relatively pure, the mate-
rials may be reused as supplementary fuel or chemical feedstocks (see Platts-
burgh Case Study, Chapter 3). In addition, it is especially important to take
extreme care not to damage these structures during site investigation or reme-
diation because this could result in the release and spread of contaminants,
complicating and increasing the expense of cleanup operations.
216
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t
S Second, it is important to determine the real extent of contamination on
and off a site as wastes, especially solid wastes from gas cleanup operations
(e.g., woodchips, spent oxides). Such wastes were often disposed in areas
adjacent to but not actually on the original gas plant site. In addition, gas
plant sites were usually sited in low-lying areas (to facilitate gas distribu-
tion) and were adjacent to streams, lakes, or wetlands. In many cases, wastes
were accidentally or deliberately discharged into these areas; recent releases
into streams, lakes, and rivers have resulted in site discoveries in many
cases. It is important, therefore, to investigate wetlands and waterbodies
adjacent to gas plant sites for potential contamination.
Third, it is important to recognize that organic contaminants with vari-
ous densities commonly occur at gasworks sites. Multiple-density contaminants
can result in complex contaminant migration patterns in the subsurface
(Section 2.1.1) and can complicate the design and implementation of site in-
vestigation and groundwater monitoring. The relative density of potential
contaminants should be known, at least qualitatively, during the planning
stages of site investigation activities.
Fourth, it is important to understand the variety of methods used to
produce the gas and the resulting variability of byproducts and waste prod-
ucts. By knowing the gas production processes used at a given manufactured-
gas site, it is possible to determine the most appropriate chemical analyses
for development of the site investigation plan, thereby resulting in lower
investigation costs. For example, an assessment plan being developed for a
site that used a coal-carbonization process should include analysis of pheno-
lic compounds, nitrogen heterocyclics, ammonia, and cyanides. The analysis of
these substances at carbureted water-gas and oil-gas production sites is less
important because they usually were produced in low amounts in these proc-
esses. In addition, it is important to determine the potential toxicity and
other hazards that may be associated with gas plant wastes (e.g., the carcino-
genicity of coal tar and the tendency of spent oxides to spontaneously com-
bust) so that adequate provisions may be made for the health and safety of
onsite workers and the general public during site investigation and remedia-
tion.
The following is a general approach for planning and conducting site
investigations at abandoned town gas sites. Most of the site investigation
217
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) techniques and procedures are the same as those applied to investigate any
; ground contamination situation; therefore, details of the techniques are not
addressed. The approach below recommends a chronological sequence of optional
activities that may have applicability to gasworks sites. The discussion
focuses on describing how characteristics of gasworks could influence the
planning of a site investigation. Because of the heterogeneity of gasworks
sites, specific and detailed site investigation plans must be developed on a
site-by-site basis.
2.2.3.2 Information Collection and Review--
Because of the age of these sites and the fact that most of the visible
evidence on the site (including storage tanks and waste disposal areas) have
been destroyed, it is important to review as much available information as
possible. Information collection efforts should concentrate on the following:
• Identification of the processes and operating practices that
were used at a site, including plant size, gas production pro-
cesses, types of feedstocks, gas cleanup processes, waste
types, waste disposal practices, and byproduct recovery opera-
tions. The entire history of the site should be covered, if
possible.
• Locations of structures inch as retort houses, water-gas pro-
duction facilities, gas cleanup facilities, storage tanks, etc.
Also, locations of waste disposal and fuel stockpiles.
• Information on the activities and historical condition of prop-
erties adjacent to the plant, focusing on likely areas for
waste disposals (e.g., wetlands).
• Information on the geology of the site (e.g., from old con-
struction borings) and regional geological information.
, • Past incidents of contamination release into adjacent bodies of
water or encounters with contaminants during construction on
the site. •
This information can be very helpful in developing a field investigation
plan (e.g., locating surface geophysical survey lines, soil borings, and moni-
tor wells). By collecting this information early on during site assessment
efforts, one can maximize the efficiency and effectiveness of subsequent site
investigation efforts, both in terms of cost and utility of the data collec-
ted.
218
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i Information collection and review should begin by obtaining the actual
records of the town gas site, including business records, construction plans,
geotechnical reports, tax and insurance records, utility location plans, and
town plat maps. Old insurance maps can be especially valuable for determining
the locations of old buildings and other structures on the site. These maps
were published for most towns in the East and in California until the 1950's.
They were published by street address, have a scale of 1 inch for 10 feet, and
were updated at 10-year intervals. The most recent versions of these maps can
be obtained from the Sanborn Map Company, Plattsville, New York. Earlier
versions are available from the Library of Congress on microfilm.
An excellent source of information about past practices at manufactured-
gas plant sites is interviews with old-timers who worked at these sites.
Often these persons can provide a wealth of information that is not recorded
anywhere. In several cf the case studies reviewed, old-timers supplied valua-
ble information on past waste disposal practices, especially information on
the locations of old waste disposal areas.
Another important source of information to review when investigating
abandoned town gas facilities is old aerial or ground-level photographs of the
site and surrounding area. These old photographs generally provide the best
record of past site activities. If one is fortunate to obtain photographs
spanning several years of the town gas operation, it may be possible to accu-
rately locate sources of potential contamination. As an example, Figure 61
shows the Seattle gas plant on Lake Union late in its operational period
(1959); Figure 62 shows it more recently after it was developed into a park.
By comparing these photographs, one can associate areas of vegetational stress
in Figure 62 with gas plant operations in Figure 61.
U.S. Geological Survey (USGS) and Soil Conservation Service (SCS) maps
and publications, information from State geological surveys, geotechnical
records, and geological publications should be consulted during a site inves-
tigation for background information on local and regional hydrogeology.
Finally, a walk around the site often can prove valuable during informa-
tion review efforts. Even if structures have been removed above ground, often
ground-level evidence remains, such as circular features marking the sites of
old gas holders. Often waste disposal areas can be identified, as can surfi-
cial contamination by spent oxides (especially when they contain ferric ferro-
219
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cyanides) and tars and oils. Odor also can be used to identify areas of
likely contamination during these walk-around preliminary site assessments.
2.2.3.3 Field Investigation Plan Development--
Once background information has been obtained for a site, a field inves-
tigation pU"i should be prepared. This effort should be closely coordinated
with local, State, and Federal environmental agencies to ensure that all en-
vironmental concerns are properly addressed and that State and Federal site
investigation requirements are satisfied. Prior to beginning the hydrogeolog-
ical site investigation, it may be necessary to submit the field investigation
plan to the various environmental agencies for their review, comment, and
possibly their written approval.
The plan should consist of a detailed site description, past site activi-
ties (including a list of known chemicals used or produced at the site),
statement of work objectives, description of proposed fieldwork activities,
and proposed laboratory analyses. Also, a detailed health and safety plan
should be included.
The health and safety plan should be prepared by a qualified industrial
hygienist who should characterize the site for the potential risk to human
health by field personnel conducting the site investigation. Safety precau-
tions, including the level of respiratory and dermal protection, should be
addressed. Emergency plans and procedures also should be included in the
health and safety plan.
The following text describes the field activities that are specified in
the field investigation plan. The actual field investigation may deviate from
the original plan if unexpected site conditions warrant.
2.2.3.3.1 Surface geophysical survey—Conducting a surface geophysical
survey can be an excellent "first step" in a field investigation because it
can provide preliminary information about the subsurface conditions of the
site. This information may be used to modify the field investigation plan by
locating areas where more detailed subsurface investigation may be necessary.
The surface geophysical survey is a valuable tool for investigating old
town gas sites for two reasons:
• It provides a method for locating buried storage tanks, buried
lagoons, and other buried structures that may contain contami-
nants.
-------
• It provides a method for delineating contaminants (coal tar and
other chemicals) in the soil and in groundwater. However, the
ability to detect hydrocarbon compounds in soil and groundwater
is limited generally to areas-where only high concentrations of
these compounds are present.
A number of surface geophysical techniques (ground-penetrating radar, electro-
magnetics, electrical resistivity, magnetometry, and seismic surveys) can be
used to provide preliminary information about subsurface conditions at contam-
inated sites.
Ground-penetrating radar can be and has been used to detect and delineate
pools of organic compounds below ground. Howeve' , site conditions can inter-
fere with the operation of tnii equipment, and it is difficult to predict
where it can be used successfully. Applicability, cost, and equipment availa-
bility may be factors determining its utilization at specific sites.
Electromagnetic (EM) conductivity is an excellent technique for making a
fast and efficient site survey of subsurface anomalies. It can locate old
excavations (buried lagoons), buried tanks, pipes, and other metal objects.
This equipment also can detect hydrocarbon compounds (tars and oils) in the
ground if the compounds are present in high concentrations. Such concentra-
tions are typically represented by low-conductivity measurements at the ground
surface because these compounds inherently have very low electrical conductiv-
ities. Although EM equipment can locate subsurface anomalies, it may not be
able to determined accurately the size, depth, and subsurface condition caus-
ing an anomaly.
An electrical resistivity survey can be conducted in conjunction with an
EM survey to confirm the EM anomalies and to better define the size and depth
of the anomalies. Also, utilising the electrical resistivity equipment in a
sounding and profiling array can help to define subsurface geologic conditions
at a site. Electrical resistivity surveying can be used to delineate the
depth of the water table as well as the presence of subsurface layers or len-
ses of different permeability that have contrasting resistivities (e.g., clay
and sand layers). However, electrical resistivity methods cannot be applied
in certain geologic settings where general subsurface resistivity is relative-
ly high; these methods are best used in areas (e.g., the Atlantic Coastal
223
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if
Plain) where electrical resistivities of subsurface materials contrast strong-
ly (White and Brandwein, 1982). Further information on electrical surveying
may be found in reports by the U.S. Environmental Protection Agency (1978) and|
Freeze and Cherry (1979).
Magnetometry may be used to detect buried metal objects at a site.
Pipes, drum-j, buried tanks, and other metal objects may be detected by this
method. At one gasworks site, a magnetometer survey was used to locate out-
fall pipes running from a waste lagoon to a la«e adjacent to the site.
Seismic refraction surveys can give valuable information about the depth
to bedrock, the subsurface bedrock topography, and the condition (fracturing)
of the bedrock (Cichowicz et al., 1981). In addition, the seismic velocity of
a geologic material is altered by the degree of weathering and water satura-
tion and therefore can provide information about the variability of these
parameters in the subsurface. However, because of the multitude of variables
that can affect a material's characteristic seismic velocity, seismic results
can be difficult to interpret, especially in areas with complex subsurface
geology or in areas where there is little contrast in seismic propagation
velocities in the subsurface. For this reason, limited exploratory drilling
usually will be necessary in conjunction with seismic surveys to confirm
interpretations based on this technique (Cichowicz et al., 1981). More (
detailed information on seismic refraction surveying may be found in Dobrin
(1960).
The selection of geophysical techniques depends to a large degree on the
geologic setting (White and Brandwein, 1982) and local site conditions. In
general, surface geophysical methods can be utilized on most town gas facili-
ties. However, there are certain sites where geophysical methods may not be
appropriate because of local site conditions. Proximity to power lines, metal
fences, railroad tracks, and buried utilities may make it difficult to proper-
ly interpret geophysical data. In many cases, the type of geophysical tool
best suited for a specific site is often difficult to determine without onsite
testing. Further information on the application of surface geophysics to
groundwater investigation may be found in Zohdy et al. (1974).
2.2.3.3.2 Soil sampling—Soil sampling includes soil-test borings and
test pits, soil-water sampling, and soil-gas sampling. These activities are
224
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the most important means to determine the extent and nature of contamination
at a gasworks site. They provide samples for contaminant analyses and docu-
ment the subsurface conditions at the site; extensive soil sampling is neces-
sary prior to planning remedial actions at a site. A soil sampling program
should be directed toward determining subsurface stratigraphy, properties of
the subsurface materials that are important to contaminant transport (e.g.,
permeability, clay content, primary and secondary porosity), and obtaining
representative samples of wastes and contaminated soil and water for analyti-
cal characterization. This section briefly reviews the important aspects of a
soil sampling program. For more information on soil sampling and monitoring,
see U.S. EPA (1984a).
A particularly important activity in a soil sampling program is to deter-
mine the proper number, location, and depth of the soil borings. Existing
information collected during the initial phase of a site investigation as well
as surface geophysical results are extremely valuable in planning a site-spe-
cific test-boring program. This program should be directed toward delineating
the extent and characteristics of contamination at the site and in determining
the characteristics of the subsurface soil and rock material. Soil-test bor-
ings are typically drilled using hollow stem augers so that the borings can be
converted easily to groundwater monitor wells. Also, this drilling technique
minimizes the potential for aquifer contamination compared to other drilling
processes.
Down-hole geophysical methods can be utilized in soil-test borings where
complex geology (including multiple aquifer systems) is anticipated. Various
geophysical tools can be used to provide a variety of continuous down-hole
data that is useful in determining the presence of contamination and inter-
preting soil stratigraphy. Down-hole geophysical methods are especially help-
ful in delineating relatively thin clay and sand layers that may not be detec-
ted by discontinuous soil-boring sampling methods (Keys and MacCary, 1971).
Test pits, usually constructed using backhoe excavators, allow for more
complete inspection of subsurface conditions than do soil borings. Features
such as vertical fractures or sand lenses, which may present pathways for
contaminant transport and can be difficult to detect in soil boring, can be
readily observed in test pits. Test pits offer a means to determine the
225
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continuity and persistence of such features in the subsurface. They also may
be used to delineate pockets of contamination and to investigate buried
structures on the site. Test pits require the excavation of considerable
amounts of soil. Because this soil can be contaminated, adequate provisions
should be made prior to excavation for the safe handling, transportation, and
storage of contaminated soil.
Other reconnaissance techniques that may be used during soil sampling
efforts are soil-gas monitoring and soil-water sampling in open boreholes and
in the vadose zone. So~"!-gas monitoring is generally accomplished in one of
two ways. One method •» /olves penetrating the partially saturated and capil-
lary fringe zones au 'e the water table with a pressure-driven probe or auger
through which soil gas is withdrawn and collected. Soil-gas samples are then
analyzed for volatile components onsite, commonly with mobile gas chromatog-
raphy, or taken to a laboratory for later analysis. An alternative soil-gas
sampling method requires that passive vapor collectors be installed within
5 feet of the ground surface. The vapor collectors remain buried for a period
of days to weeks; when exhumed, they are taken to a laboratory where the
vapors are released and analyzed. Although both methods are relatively quick
and inexpensive ways of qualitatively characterizing subsurface organic con-
taminants, they are limited to compounds with relatively low water solubili-
ties and high vapor pressures that are capable of diffusing through porous
media. In general, soil-gas monitoring has little utility at sites that lack
the more volatile fractions of coal tar, e.g., benzene, toluene, xylene, or
naphthalene. If these components are present, however, soil-gas monitoring
may prove successful in qualitatively characterizing the extent of contamina-
tion at a site.
Soil-water sampling is very similar to soil-gas sampling except that a
water sample is collected. Drill-stem sampling collects the sample in open
boreholes at the top of the water table. Drill-stem sampling offers some
advantages over soil-gas sampling in that dissolved nonvolatile and volatile
organic and inorganic contaminants can be measured. The method offers cost
savings when compared to conventional groundwater monitoring techniques using
permanent well installations. Soil-moisture profiling in the partially satur-
ated or vadose zone can be accomplished by a modified soil-gas sampling probe
j 226
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or by a number of geophysical methods (e.g., neutron scattering or gamma-ray
absorption). Once a sufficiently moist horizon is located,'suction lysimeters
with porous clay cups can be installed in the vadose zone for sampling soil
water. In practice, soil-gas sampling probes have a water-sampling capabil-
ity, so the advantages of both methods can be combined.
As stated previously, it is very important to take special care when
using invasive site investigation techniques (e.g., borings, test pits) at
abandoned gasworks sites to avoid penetrating or otherwise damaging buried
structures such as tanks, gas holder foundations, or tar separators. These
structures often contain tars, oils, or other contaminants. Structural damage
could result in their release and spread of contaminants, complicating cleanup
efforts.
2.2.3.3.3 Groundwater monitoring—The major objectives for installing a
groundwater monitoring system are to:
• Measure watpr levels for the purpose of determining gradient
and direction of groundwater movement
Perform in-situ permeability tests
• Sample groundwater for chemical analysis.
This section discusses the means to achieve these objectives with specific
emphasis on monitoring considerations for abandoned gasworks sites. More
detailed information on the design and installation of groundwater monitoring
systems may be found in Barcelona et al. (1983), Barcelona et al. (1985), Todd
(1980), Fetter (1980), Freeze and Chowy (1979), Johnson Division (1975),
Villaume (1985), and NV/WA/API (1984).
The number, spacing, depth, and well screen length of monitoring wells
may be determined based on background information collected about a site and
on the findings of the soil sampling and surface geophysical monitoring pro-
grams.
It is important to properly space the monitor wells across the site so
that the gradient and direction of groundwater movement can be measured to
determine groundwater flow directions and velocity at a site. On small sites
it may be necessary to locate monitor wells offsi'te to discern measurable
differences in groundwater levels. If multiple aquifers or perched water
227
r •;
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table conditions are suspected, it is suggested that nested piezometers be
installed at selected depths to measure vertical gradients. In-situ variable
head permeability tests should be performed in selected monitor wells repre-
senting various geologic conditions across the site. The permeability meas-
urements along with the groundwater gradient data are useful in estimating the
average velocity of groundwater movement across the site.
For groundwater quality sampling and analysis, it is important to have a
good distribution of monitor wells upgradient and downgradient from the
suspected source of groundwater contamination. The upgradient monitor wells
provide the background (uncontaminated) water sample. It may be necessary on
small old town gas sites to use offsite wells upgradient of the site as back-
ground wells. The downgradient monitor wells should be well spaced and have
variable-depth well screens for the purpose of determining the vertical and
lateral extent of groundwater contamination. It is also suggested that a
downgradient monitor well be placed near the property boundary to determine if
the suspected contaminant plume has migrated offsite.
Variable density contaminants have been observed in the subsurface inves-
tigations of several manufactured-gas sites and can result in complex contami-
nant migration patterns in aquifers. The potential for variable density
fluids needs to be recognized to the appropriate design of groundwater moni-
toring systems at manufactured-gas sites. Adequate groundwater monitoring in
flow fields with significant density contrasts requires careful monitoring
well design and placement to avoid costly redrilling efforts or the creation
of undesirable conduits for contaminant migration. Although single well in-
stallations that are properly screened within a groundwater flow system may be
adequate for some variable density situations, it may be necessary to supple-
ment single wells with multiple-level sampling to fully characterize the ver-
tical extent of contamination. It is also important to compensate measure-
ments and sampling activities for differences in density where significant
contrasts exist. Because the variable density contaminants commonly occur at
abandoned town gas plants, special monitoring considerations for immiscible,
multiple density fluids in gro- ndwater are discussed below.
The relative density of potential contaminants at a gasworks site should
be understood, at least qualitatively, before implementation of a groundwater
228
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monitoring program. In some cases, the relative density contrast may be obvi-
ous, such as with low-density (coal oil) or high-density (coal tar) immiscible
contaminants. However, soluble components of the contaminant also may be
present, especially when low-density immiscible contaminants occur (as discus-
sed in Sections 2.1.1 and 2.3.3.3.5), and these need to be considered in the
design of the monitoring system (Figure 63). In this example, the downgradi-
ent well closest to the source area may encounter immiscible and soluble com-
pounds, whereas further downgradient, the monitoring well will encounter only
soluble compounds. A multilevel groundwater sampler would be useful in this
example to detect migration of the soluble component and its stratification
within the groundwater. Lysimeters or similar in-situ pore-water samplers
might be useful in delineating the dimensions of the contaminant plume above
the water table (Figure 63).
In other situations, contaminants migrating from a gasworks site muy
consist of constituents with multiple densities (Figure 64). In this example,
downgradient well A will detect an intermediate density zone, and well B will
detect the higher density zone. A multilevel sampler (well C) can be used to
further delineate the two relative density zones.
The position of the screened interval of monitoring wells (or intake
ports of multilevel samplers) is one of the most important aspects of detect-
ing variable density contaminants in the subsurface. This is illustrated in
Figure 65 where examples of appropriate and inappropriate monitoring tech-
niques are compared for variable density contaminant situations in a uniform
flow field. In example 1, the high-density contaminant solution could be
overlooked as a result of shallow screen settings of the monitoring wells.
Deeper-screened settings would be more appropriate in this example (nested
wells A, B, and C), or a multilevel sampler (well D) would allow for more
complete definition of the vertical extent of contamination. For example 2,
the low-density immiscible contaminant could be largely overlooked if screened
intervals were too deep below the water table. Shallow monitoring wells would
be more appropriate in this situation, particularly for defining the depth of
the depressed water table. In example 3, the contaminant solution has a simi-
lar relative density as the groundwater, but it is not detected by the shallow
screen setting of well A. The long screen interval of well B intercepts the
229
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Inappropriate Monitoring
Appropriate Monitoring
Example 1. High relative density contaminant solution.
Example 2. Low relative density immiscible contaminant.
Example 3. Contaminant solution with similar relative density as ground water.
Source: Alexander, 1984.
Figure 65. Comparative groundwater monitoring of variable density
contaminants in uniform flow field.
232
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contaminant plume, but it also draws in uncontaminated groundwater, as does
well C. The results of groundwater analysis from these wells may not reveal
the presence of contamination because of dilution of the samples. More appro-
priately, the carefully screened intervals of wells A and B would detect the
contamination, but that would require prior knowledge of the plume's vertical
extent. This knowledge could be gained by the installation of a multilevel
sampler (well C).
The presence of high-density tars at gas sites in the subsurface requires
special care when constructing monitoring wells into deeper aquifers below a
site. These wells can provide pathways for such tars to move, under density
gradients, into deeper aquifers, even against an upward hydraulic gradient
between the confined aquifer and the surface. At St. Louis Park, Minnesota,
coal tar flowed down a multiaquifer well, resulting in contamination of multi-
ple aquifers (see Chapter 3). Because of this contamination potential, moni-
toring wells for aquifers beneath a gasworks site should not pass through
zones of tar contamination. If tar is encountered during the construction of
such a well, the well should be moved to an area with no underlying coal tar.
If this is not possible, extreme care should be taken to seal off the tar-
containing zone to prevent migration of tar into the borehole and down into
the aqui fer.
2.3 SITE REMEDIATION
2.3.1 Introduction
Remediation options for gasworks sites are basically the same as those
for other Industrie.; hazardous waste sites: no action; onsite containment,
with or without stabilization or fixation; removal and disposal of contamina-
ted material; in-situ treatment; removal and treatment or destruction of con-
taminated materials. The selection and implementation of remedial alterna-
tives for specific gasworks sites are the same as for other hazardous waste
sites. This discussion does not go into detail about site remediation.
Instead, it concentrates on the unique features of gasworks sites that may
affect site remediation, case studies of actual gasworks site remediation, and
listing remedial action alternatives for specific gasworks wastes. For more
information on the selection and evaluation of remedial action alternatives
233
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for specific sites, the reader is referred to Cochran and Hodge (1985a,
1985b), Boutwell et al. (1985), U.S. EPA (1982), Ehrenfeld and Bass (1983),
and Sims et al. (1984).
2.3.2 Factors Affecting Site Remediation
Gasworks sites have certain unique features that can influence the selec-
tion of remedial alternatives. First, the sites are old: Many were abandoned
more than 50 years ago, and almost all are more than 30 years old. This age
can affect remediation in several ways. It can result in a low-priority rank-
ing for the site in terms of cleanup. If the site owner can demonstrate that
there is no history of contaminant migration and that wastes currently are
remaining onsite, it is possible that site remediation efforts could be post-
poned without damage to human health or the environment. The fact that a site
has existed for decades without problems may be taken as evidence that post-
poning remediation will cause no further problems. If cleanup is postponed,
however, groundwater monitoring should be employed to detect contaminant
release, and measures such as restricted site access should be taken to avoid
exposure of the public to contaminants at the site.
On the other hand, the age of these sites can afford a long period of
time for contaminants to move offsite, thereby resulting in a significant
spreading of contaminants and an increase in the volume of material that must
be cleaned up. This was the case at Brattleboro, Vermont, where coal tar has
moved through a porous gravel layer along a bedrock surface, underneath a
river adjacent to the former plant site. At St. Lou.is Park, Minnesota, where
a coal tar refinery operated for more than 50 years, contaminants have spread
to several aquifers to a depth of over 900 feet, and a plume of contaminants
extends over one-half mile from the site. At Ames, Iowa, lighter tar constit-
uents from a gas plant closed in the 1930's have contaminated the municipal
well field, resulting in the closure of five municipal wells since contamina-
tion w.->s first detected in 1927. In contrast, at Stroudsburg, Pennsylvania
(Brodhead Creek), favorable geological conditions resulted in the containment
of over 8,000 gallons of free coal tar in the subsurface for about 40 years,
until excavation of the adjacent creek bank caused release of the tar into the
creek.
234
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Many of the case studies reviewed in this study (see Chapter 3) illus-
trate the fact that gasworks were often built in low-lying areas adjacent to . (
waterbodies or wetlands. In some cases, discharges into these waterbodies
resulted in a site discovery. Proximity to waterbodies or wetlands can
require barrier construction to prevent surface water contamination during
site remediation. In addition, contaminants may have been disposed of or
migrated into these waterbodies, which can result in accumulation in river or
lake sediments. This could necessitate underwater cleanup operation, compli-
cating and increasing the cost of site remediation.
Gasworks also usually occur in downtown areas or old industrial dis-
tricts. The recent trend to redevelop these areas has resulted in the discov-
ery of many former gasworks sites across the country. Redevelopment pressures
and priorities can affect site remediation efforts and vice versa. The
following cases illustrate how redevelopment and remediation were handled in
different areas of the country.
In Newport, Rhode Island, two multimillion dollar apartment buildings
were being constructed across the street from one another when tar from a
former gas plant was discovered in the subsurface at both construction sites.
One building was being constructed on pilings. The only contaminated material
removed from this site was that actually excavated for the pilings. It was
disposed offsite, and the lower floors of the building were designated for
nonresidential use (parking garage). At the other site, a buried concrete
structure was discovered and accidentally ruptured during construction of the
foundation. It was full of coal tar. In this case, the structure was
repaired, the coal tar left in place, and a ventilation system installed to
prevent organic vapors from accumulating in the basement of the apartment
buiIding.
In San Francisco, California, coal-tar contamination was encountered
during construction of an addition to EPA's Region 9 headquarters. This mate-
rial was removed and disposed in a secure landfill. There was suspicion that
the soil under the existing building also could be contaminated, but this has
not been verified.
Cases of contamination discovery under existing buildings constructed
after a gas plant was removed were not uncovered in this study. However, the
235
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downtown location of most plants makes the existence of such a situation pos-
sible, if not probable. The presence of an existing building over a contami-
nated gasworks site would be considerably complicated and could prevent reme-
diation of a site. In such cases, onsite containment may be the best option.
Case studies in Chapter 3 that illustrate the interaction of redevelop-
ment and site remediation are GasWorks Park, Seattle, Washington; Brattleboro,
Vermont; Plattsburgh, New York; Everett, Massachusetts; and Mendon Rd., Attle-
boro, Massachusetts.
When gasworks were decommissioned, surface structures often were removed,
but structures below the surface usually were left in place. These structures
often contain contaminants, usually tars, oils, or tar/water emulsions.
Because of this, it is important to determine the locations of these struc-
tures during a site investigation and to consider their locations when plan-
ning site remediation activities. In some cases, free tars and oils occur in
these structures; such gasification byproducts may be reused as supplementary
boiler fuel or chemical feedstocks. If reuse is not a viable alternative,
careful recovery of the material from the structures results in a more concen-
trated waste stream for treatment or disposal. If subsurface structures are
damaged during remediation efforts, contamination can spread into surrounding
soils, increasing the expense and complexity of remediation efforts.
Another feature of gasworks sites that can affect remediation efforts is
the presence of injection wells that were used for waste disposal (e.g., for
tar residues and emulsions). At least one site reviewed in this study,
Stroudsburg, Pennsylvania, may have had one of these wells. Research by the
Stroudsburg site investigators suggested that other gasworks in the area may
have used wells for waste disposal. Maps for the Lowell, Massachusetts, plant
showed a "deep well" on the site. However, it is not clear whether this well
was used for waste disposal. Additionally, it is important when reviewing old
site maps not to confuse tar wells, which are underground structures
containing tar, with injection wells used for disposing of wastes.
The location and depth of all wells on a site should be •>.••*c.-.:ined during
remedial investigations. These wells nay be reopened and sampled for contami-
nation. Care should be taken during reopening to prevent them from adding to
the spread of contaminants. If no contamination is detected, they should be
236
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properly closed and sealed to prevent them from becoming pathways for contami-
nant migration. If contaminated, they can complicate site remediation
efforts. However, if wastes were pumped down a well, it may be possible to
pump them back out. This was accomplished at Stroudsburg, where over 8,000
gallons of free coal tar was removed from the subsurface. However, consider-
able tar remains bound up in subsurface material at Stroudsburg; this necessi-
tated containment (slurry wall) to prevent migration of contaminants offsite.
2.3.3 Remedial Action Alternatives
2.3.3.1 Introduction--
As previously stated, remedial action alternatives for gasworks sites are
similar to those for other uncontrolled hazardous waste sites. Containment,
removal and disposal, and treatment all are applicable. Some containment
generally will be required for all remedial actions to prevent the release and
spread of contaminants. Slurry walls and caps have been used to contain gas-
works wastes. Removal and disposal is a simple but expensive option that also
has been used to clean up gasworks sites. Treatment to stabilize, detoxify,
or destroy gasworks wastes has not been employed to a great extent, but it is
attractive because it can destroy a waste's hazardous nature, enabling safe
disposal of residues in nonhazardous waste landfills and eliminating future
liability. Treatment alternatives with potential applicability to gasifica-
tion wastes are summarized in Table 47.
The following discussion focuses on remediation techniques actually ap-
plied to gasification wastes or similar substances. For more general informa-
tion on the evaluation and selection of remedial action alternatives, the
reader is referred to the Deferences listed at the end of Section 2.3.1.
2.3.3.2 Oils, Tars, and Lampblack--
The most prevalent and persistent contaminants at gasworks sites are
organic byproducts of the gas manufacturing process--tars, oils, and lamp-
black. Tars and oils could be produced in any process; lampblack was most
commonly produced in oil-gas processes. Tars and oils can contaminate soils
and groundwater (see following sections), but they also occur as free products
at gasworks sites, especially in buried tanks and other structures, buried
lagoons, and in coarse sands and gravel in the subsurface. Lampblack may
237
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TABLE 47. POTENTIAL TREATMENT TECHNOLOGIES FOR CONTAMINATED SOILS
Method
In-situ methods
Neutralization
Solvent extraction
Chemical oxidation
Immobilization
Attenuation
Description
Applicability
Addition of base to soil to
neutralize acid; base could be
spread or injected into soil
as a solution or spread as a
powaer and tilled into soil
Flush with chemical solution to
remove contaminants, then collect
and treat solvent; solvent could
be acidic, basic, or surfactant,
injected or percolated into soil
and collected in drain or with-
drawal wells
Addition of chemicals such as
ozone or peroxide to break down
compounds into harmless forms
or forms more readily attenuated
by natural microbial activity;
lack of selectivity may lead to
high dosage requirements
Reduces rate of release of con-
taminants into environment; pH
adjustment or chemical addition
promotes sorption or precipita-
tion onto organic materials such
as sawdust or agricultural
byproducts; may have already
occurred at gas manufacturing
sites through reaction with
organic "fluff"
Mixing of contaminated soils with
clean soil, municipal refuse, or
sewage sludge; may be acceptable
for low-risk wastes, also may
promote natural biological
degradation
Acids or acid-forming
wastes
Organics or metals,
depending on solvent
Primarily organics,
may mobilize metals,
requiring leachate
collection and treat-
ment
Metals and organics
Compatible wastes
of low mobility and
toxicity
(continued)
238
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TABLE 47 (continued)
Method
Description
Applicability
Biological oxidation
Occurs naturally in soils; may be
enhanced by addition of nutrients,
oxygen, or specially developed
microbes; contaminants are
metabolized by bacteria and/or
fungi to harmless forms
Methods requiring excavation
Thermal treatment
Evaporation
Incineration
Chemical treatment
Biological treatment
Landfarming
Composting
Contaminated soils heated to
drive off volatiles that are
destroyed in an afterburner
Entire waste matrix heated to
over 1,000 °C to destroy con-
taminants
Neutralization, extraction, oxi-
dation, immobilization similar
to description under in-situ
methods, carried out in a
reactor under controlled
conditions
Waste incorporated into upper
layers of soil, biological
degradation stimulated, cover
or livestock feed crops grown
Waste biologically stabilized
above ground, may be mixed with
municipal refuse or sewage
sludge; result may be used as
a soil amendment
Primarily organics
although sulfur and
nitrogen also may be
oxidized
Organics, cyanides,
sulfides; auxiliary
fuel required
Same as evaporation
Various wastes
Organics, cyanides;
not suitable for
wastes containing
heavy metals, which
may build up in soil
or crops
Primarily organics or
cyanides; disposal of
metals depends on
final disposition of
product
SOURCES: Sims et al., 1984; Hoogendoorn, 1984.
239
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occur at or below the surface. If these contaminants can be recovered in pure
form, they may be reused as supplementary fuels or chemical feedstocks.
Alternatively, they are easily incinerated.
Removal of tars or oils from underground containment structures is rela-
tively straightforward, but care must be exercised to avoid rupturing the
structure. Once the substances have been removed from tanks, the tanks can be
either cleaned using steam or aqueous surfactants or removed and disposed of.
At Stroudsburg, 8,000 gallons of free tar was pumped from the ground
using techniques developed for control of distribution of tar in the surface
(Villaume et al., 1983; Roberts et al., 1982). Poor understanding of these
phenomena at Stroudsburg resulted in overestimation of free coal tar in the
subsurface and overscaling of the coal tar recovery system. Original esti-
mates of 35,000 gallons of free tar resulted from a failure to realize that
the tar was present in several different "phases" or zones. Much of the tar
was held up in the subsurface by capillary forces so that no coal tar could be
removed by pumping, or it was associated with water in a fashion that would
result in recovery of coal tar and water if this zone was for heavy oil recov-
ery (see case study in Chapter 3). In this case, recovery by pumping was
possible because the tar was contained in a coarse, highly permeable aquifer
that enabled it to move relatively freely. The feasibility of this approach
at other sites may be determined from the characteristics of the porous medium
(e.g., porosity and permeability), the characteristics of the tar (e.g., vis-
cosity, density, interfacial tension between tar and water, and wetting angle
of tar on aquifer material in the presence of water), and an awareness of how
viscous and capillary pressure forces can be pumped. Figure 66 illustrates
the zoned distribution of water and coal tar in the subsurface at Stroudsburg,
inferred from capillary pressure theory, and it indicates the types of
material that may be pumped from the different zones. Failure to perform this
sort of analysis can result in overestimation of the amount of free tar in the
subsurface; tar in water emulsions and tar held by capillary forces in the
subsurface material may be included in the free coal tar estimates.
As previously mentioned, free products recovered from gasworks sites may
be used as fuel (as at Str.oundsburg) or as chemical feedstocks. It also may
240
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PUMP
PRODUCT
WATER
WATER
WATER AND
COAL TAR
COAL TAR
WATER
LIQUID PHASE(S)
T
GROUND WATER WITH
DISSOLVED ORGANIpS
GROUND WATER AND
TRAPPED COAL TAR
GROUND WATER
AND COAL TAR
COAL TAR AND
'IRREDUCIBLE' WATER
GROUND WATER WITH
DISSOLVED ORGANICS
POROUS
MEDIUM
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Figure 66. Ideal distribution of coal tar in porous materials at the
Stroudsburg contamination site, as inferred from
capillary pressure theory.
241
-------
be easily incinerated (heating value -17,736 Btu/lb) or may be amenable to
land treatment, as described in the following section on contaminated soil.
Lampblack is solid, sooty material that was commonly produced in oil-gas
plants. It is composed of very heavy organic compounds, including PAH. It is
essentially immobile and insoluble in the subsurface. Because of this, it can
be safely contained onsite, as was done at an unnamed site in southern Cali-
fornia. If it is removed, it can be briquetted and used as solid fuel or
possibly used as a blackening agent in certain industrial processes. Alterna-
tively, it may be easily incinerated. Lampblack contains PAH's and is car-
cinogenic; its powdery form makes it necessary to exercise care to prevent
dust emissions when excavating and handling the material. Inhalation and skin
contact also should be avoided.
2.3.3.3 Spent Oxide Wastes--
Spent oxide wastes, as described in Section 2.1.2, are extremely hetero-
geneous in nature from site to site and within specific sites. This variabi-
lity occurs both in terms of the wastes' physical characteristics and types of
contaminants that may be present. Because of this variability, and because
they have not been extensively characterized by composition or occurrence, it
is difficult to evaluate remedial alternatives for these wastes. This discus-
sion concentrates on the characteristics of the wastes that can affect their
treatment and handling during remedial actions and on two cases in which sites
containing spent oxide wastes were remediated.
Spent oxide wastes are pyrophoric, i.e., when exposed to air they have a
tendency to self-heat and spontaneously combust. For instance, Downing (1932)
reports:
t
The disposal of spent oxide is a vexatious problem for many gas
plants. Because of a possibility of fires starting through heat
generated by revivification, it is necessary to hold the spent mate-
rial at the plant until this danger is past. As soon as city
authorities learn of this menace the material is prohibited at pub-
lic dumps. Continuous storage on gasworks land eventually becomes
impossible. The material makes excellent filling for roads or pri-
vate property when properly handled. It should be covered with
ashes or soil immediately to prevent the access of air and conse-
quent combustion.
242
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M
This pyrophoric nature probably is due to the presence of reduced sulfur com-
pounds that oxidize exothermically when exposed to air. At one unnamed gas-
works site, a gas cleanup box that was left full of oxide material years ago
when the plant closed was opened during site cleanup activities. It subse-
quently caught on fire. In this case, the fire was easy to extinguish because
it was contained. However, care should be taken to avoid combustion when
excavating, moving, or storing spent oxide wastes at a gas plant site. The
material should be covered as much as possible with soil, plastic, or other
material to prevent contact with air. In addition, when it is to be stored or
transported, it should be carefully placed and compacted into the pile or
transportation vehicles to prevent, air from permeating the waste materials.
Alternatively, it may be possible to separate combustible materials (e.g.,
woodchips) from the sulfur-containing oxides to prevent combustion of these
materials. Physical separation, followed by incineration of the combustible
material, may be an appropriate alternative for treating these wastes.
Spent oxides can have elevated levels of arsenic associated with wastes
from the Thylox gas cleanup process. They also have significant acid-generat-
ing potential, leachates from these wastes having a pH of 1.5. This low pH
can result in release of arsenic or other trace metals. At the Birmingham,
Alabama, gasworks site, arsenic levels of 8.0 mg/L were reported for 1.5 pH
leachate from spent oxide wastes that contained 160 ppm arsenic (Harry Hendon
and Associates, Inc., 1982).
Total cyanide levels as high as 8,900 ppm were measured in spent oxides
at the Birmingham site. However, the highest levels of free cyanides in water
reported at sites contaminated with these spent oxides was 2.6 ppm for a sam-
ple with a pH of 1.5 (Harry Hendon and Associates, Inc., 1982); free cyanide
levels less than 1 ppm were more commonly associated with spent oxide wastes
at Birmingham. This is because most of the cyanides are present as complex
iron cyanides. These compounds are very stable in the environment and have a
low toxicity. They do appear to release small concentrations of free cya-
nides; however, these concentrations are well below the 200 ppm level that
limits degradation of free cyanides in aerobic soils, and most are below the
2 ppm limit for the anaerobic degradation of free cyanide (Fuller, 1984). The
persistence of complexed ferric ferrocyanides remaining for decades in spent
243
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oxide wastes disposed at or near the surface is further evidence of their
stability in the soil environment.
The persistence of the cyanide materials in spent oxides and the relative
stability of ferric ferrocyanide compounds is an encouraging observation from
the standpoint of treating these wastes. Although the complete destruction of
cyanides in spent oxide might be the most ideal solution, the cost associated
with destruction options, along with potential for the liberation and release
of free cyanide during treatment, may make stabilization or fixation a more
desirable choice. The long-term survival of ferric ferrocyanides at gas plant
sites, along with the use of this material in table salt, highway deicing
salt, paints, pigments, and laundry bluing, suggests that treatments to elimi-
nate any hazards under the Resource Conservation and Recovery Act (RCRA), and
containment onsite or disposal in a municipal landfill may be an environmen-
tally acceptable and cost-effective alternative for dealing with these wastes.
At the Alabama Gas Corporation Gas Works site in Birmingham, Alabama,
in-place stabilization was selected as the remedial alternative for an onsite
spent oxide disposal area (Harry Hendon and Associates, 1982). Stabilization
of the 2.4-acre site involved excavating and stockpiling the contaminated
material, then mixing agricultural lime (CaCC>3) and soil in 1-foot lifts
across the site, not exceeding 80 tons of lime per acre-foot of soil. In
addition to lime, fertilizer and sewage sludge was added to the top 6 inches
to promote the growth of vegetation. The lime neutralized the acidic condi-
tions formerly present at the site, thereby reducing trace metal (As) release
to environmentally safe levels. The remediation plan was successful: The
once barren site has been revegetated, and soil samples indicate that acidic
conditions and high arsenic concentrations have abated. The cost of remedia-
tion was about 5100,000; removal, disposal in a secure landfill, and refilling
was estimated to cost S2 million to $5 million.
At the Mendon Road site in Attleboro, Massachusetts, 1,083 yd3 (about
one-third of the volume of material at Birmingham) of spent oxide material
from gasworks manufacture had been disposed in an abandoned gravel pit. The
site was discovered during residential development of the area. The waste was
similar to that found at Birmingham (pH = 1.61; total cyanide = 7,500 ppm,
free CN~ = 0.7 ppm) except that high arsenic levels were not detected and low
244
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ppm levels of PAH compounds were found. The waste was excavated, removed from
the site, and disposed in a secure hazardous waste disposal facility ?t a cost
of over SI.6 million.
The difference in costs in the two spent oxide site remediations is not
insignificant. In-place stabilization appears to be a desirable remedial
alternative for cyanide-containing spent oxide wastes on both technical and
cost bases. If site use plans rule out onsite stabilization as a viable
alternative (as at Mendon Road), removal, stabilization, and disposal at a
nonhazardous waste landfill may be an environmentally acceptable alternative
that is more economical than disposal as a hazardous waste. Studies demon-
strating the low mobility in soils of ferrocyanides in municipal waste leach-
ate suggest that stabilization and disposal in municipal landfills may be
acceptable (Fuller, 1984). However, more research is needed on the mobility
of complex iron cyanides before this can be proven safe. In addition, the
extreme variability and heterogeneity of spent oxide wastes necessitate waste-
specific evaluations of remedial alternatives. Other methods for treating
cyanide-containing wastes are discussed in the following section on remedia-
ting contaminated soils.
The characteristic blue color of complex ferric ferrocyanides can be used ^
both to identify areas of spent oxide contamination during site investigations™
and to guide remediation efforts; however, some question exists as to cr^or-
threshold-contaminated levels. At the Mendon Road site, color was used to
delineate contaminated soil with greater than 2 ppm total cyanide during
cleanup efforts. Wilson and Stevens (1981) report that blue color may be
detected in soils containing about 270 ppm total cyanide (or 500 ppm ferric
ferrocyanide). Further analyses of samples of soil contaminated with complex
iron cyanides is necessary to resolve this discrepancy.
Spent oxide wastes that do not contain complex cyanides are usually red
to yellow. They may be more common at U.S. gas plant sites than are cyanide-
containing wastes because of the prevalence of water-gas and oil-gas processes
that produced gas that characteristically had low levels of cyanide compounds.
The major hazards associated with these wastes is their acid-producing poten-
tial and their potential to release toxic trace elements. These hazards may
be reduced by additives, such as CaC03, that can reduce acid and limit trace
metal release.
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Spent oxide materials may be contaminated with tar and/or may have been
codisposed with tar-contaminated shavings from shavings scrubbers used during
gas cleanup to tar mist prior to the oxide boxes. At one site visited by the
authors, oyster shells contaminated with tar were seen onsite; these probably
were used in place of shavings for tar removal. Methods for treating solid
materials contaminated with tars and oils are discussed in the following sec-
tion.
2.3.3.4 Contaminated Soil--
Our review of gas plant site investigations revealed that the most com-
monly occurring soil contaminants are byproduct tars and oils from gas manu-
factured. Spent oxide waste containing complex iron cyanides, sulfur com-
pounds, and arsenic is another significant but less prevalent soil contami-
nant.
Treatment techniques that may have applications at gas plant sites are
summarized in Table 46. A complete review of treatment technologies for
contaminated soils is beyond the scope of this study. The following discus-
sion considers techniques actually applied on contaminated soil from gasworks
plants or on soils contaminated with substances similar to gas plant wastes
(i.e., creosote). More information on soil treatment techniques in general
may be found in Sims et al. (1984), Hoogendoorn (1984), Cull inane and Jones
(1984), Spooner (1984), Rulkens and Assnik (1984), and Wagner and Kosh (1984).
2.3.3.4.1 Land treatment—The land treatability of PAH-contaminated
soils and PAH-containing sludges has been demonstrated for petroleum refinery
wastes (API, 1983) and for creosote used by the wood-preserving industry
(Sims, 1984; Sims and Overcash, 1983; Umfleet et al., 1984; Patnode et al.,
1985; Ryan and Smith, 1986). The fractional distillation of creosote from
coal tar (creosote has a 200 to 400 °C distilling range), suggests that land
treatment will be effective in treating soils contaminated with gasifier tars
and oils. Comparison of contamination removal rates for creosote wastes and
refinery wastes shows good agreement (Ryan and Smith, 1986); this implies that
the land treatability of PAH-containing hydrocarbons is similar regardless of
their source.
Currently, the wood-treating industry and the U.S. EPA are sponsoring
studies to demonstrate the land treatability of creosote sludge and creosote-
246
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contaminated soils [Ryan and Smith, 1986; R. C. Sims, Utah Water Research
Laboratory (UWRL), personal communication, 1986]. At one site in Minnesota,
bench-scale and pilot-scale field tests have demonstrated the feasibility of
land treatment of creosote-contaminated soils (Patnode et al., 1985; Ryan and
Smith, 1986). Important results of this study are:
• Percent removals of benzene-extractable hydrocarbons averaged
about 40 percent over 4 months, with a corresponding first-
order kinetic constant of 0.004.
• Complete toxicity reduction appeared to fall between 2.5 and
5.0 percent benzene-extractable content. Two out of five test
plots were nontoxic after 4 months (those with lowest initial
application rates). All plots showed significant degradation.
• Microbial assays suggested that initial concentrations of creo-
sote compounds would kill soil microorganisms and inhibit de-
gradation. This did not occur. In addition, seeding plots
with adapted microorganisms did not significantly enhance de-
gradation. This implies that an active, adapted microbial
population naturally developed in the contaminated soil.
• Within the range of loading rates tested (4 to 10 percent ben-
zene extractables), no correlation between loading rates and
kinetic rates was observed, with the exception of 4+ ring PAH
compounds, which showed a slight inverse relationship between
loading rates and kinetic rates.
• All loading rates tested (4 to 10 percent benzene extractables)
were feasible.
• loxicity reduction occurred at a faster rate at 4 to 5 percent
initial loading rate than at higher loading rates.
• Greater kinetic rates were observed after waste reapplication
to a treated soil.
• At this site, 3 to 5 years would be necessary to treat 12,500
tons of contaminated soil.
• Waste application rates of 2 to 3 pounds of benzene extracta-
bles per ft3 of soil per 2 months can be degraded.
This study demonstrates the feasibility of land treating sandy soils contami-
nated with creosote wastes in Minnesota. Treatment times should be lower in
warmer areas with a longer growing period. Preliminary results from an on-
going study in California suggest similar kinetic degradation rates in clayey
soils (Ryan and Smith, 1986).
247
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TABLE 48. COST ESTIMATES FOR REMEDIAL ACTION ALTERNATIVES
AT A CREOSOTE IMPOUNDMENT
Alternative
Land treatment (onsite)
Landfill
Incineration (onsite)
Incineration (offsite)
a!2,500 tons contaminated material.
SOURCE: Patnode et al., 1984.
Unit cost
(S/ton)
51
200
184
1,900
Total cost9
(SI, 000)
738
2,500
2,300
23,750
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One of the most significant results of the Minnesota study is that onsite
land treatment is very cost-effective. Table 48 compares the cost estimates
of land treatment with other options (i.e., landfill and incineration); land
treatment cost estimates were lowest at 551/ton. If onsite conditions are not
amenable to land treatment, costs will increase as a result of transportation
costs to a suitable treatment site. However, even if this results in costs
higher than landfilling, land treatment will still be preferable because it
can detoxify the waste, thereby eliminating long-term Viability. Comparison
of onsite land treatment costs with onsite incineration (Table 48) demon-
strates that land treatment is more cost-effective.
Our review of remedial alternatives for soil contaminated with tars and
oils from gas plant manufacture indicate that land treatment is the best
demonstrated treatment technology. It appears to be cost-effective, as well
as effective in detoxifying the wastes. The age of all gasworks sites further
supports this conclusion because soil microbes capable of degrading tar and
oil compounds will have had time to evolve. The Ames, Iowa, case study (see
Chapter 3) demonstrates this; organisms capable of degrading PAH compounds
have evolved in the groundwater at Ames.
Several questions remain unanswered with respect to applying the results
of the creosote studies to gas plant residuals. First, creosote is a distil-
late fraction of coal tar; the tars and oil at former gas plants tend to have
a broader boiling point range. In addition, creosote is derived from coal
tar; most gas plants operated water-gas processes, which produced tars with
different composition (e.g., no tar acids or bases), it is not clear how this
will affect soil toxicity and degradation rates. It does seem possible that
soil microbes will have adapted to whatever tar constituents are present at a
site. Other soil contaminants present at gas plant sites also could affect
the land treatability of contaminated soil. Complex iron cyanides are not
amenable to land treatment (Hoogendorn, 1984); free cyanides are rapidly
broken down by soil microbes at concentrations below 200 ppm; and, as long as
complex iron cyanides do not release free cyanides at rates sufficient to
elevate soil levels to above 200 ppm, they may not affect degradation. Sulfur
and arsenic compounds also may be present and could influence degradation
rates. Another question is the volatilization of volatile components in coal
249
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tars and oils during land treatment operations. These questions can be
addressed by site-specific land treatment demonstrations such as those
required for permitting a facility under RCRA (40 CFR 264).
Studies to demonstrate the treatability of contaminated soils and tars
and oils should include bench-scale and pilot-scale tests to evaluate the
effect of various design and operational parameters on the treat.abil ity of the
wastes in question. These parameters include:
• Soil characteristics
• Waste characteristics
• Treatment supplements
Climate
Initial loading rate
• Reapplication rate
Soil lift thickness
• Frequency of tilling.
Treatability studies should be directed toward determining the effects of
these parameters on the reduction of organics, PAH's, and toxicity for the
wastes or contaminated soils to be treated. M
When conducting a treatability study, soil conditions that promote the
degradation of hydrocarbons should be maintained. These conditions include
(Ryan and Smith, 1986):
• Soil pH of 6.0 to 7.0 in the treatment zone
• Soil carbon-to-nitrogen ratios of 25:1
• Soil moisture .near field capacity.
Other criteria that have been recommended for land treatment of creosote
wastes include:
• Small and frequent fertilizer applications
• Waste reapplication only after initial applications have been
effectively degraded.
U.S. EPA has published general guidance on land treatment demonstrations
(EPA, 1984a; EPA, 1983a; and EPA, 1983b). EPA also has released a draft tech-
nical guidance manual on hazardous waste land treatment demonstrations for
250 ™
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public comment (EPA, 1984b). This latter document currently is being revised
to address and incorporate the public comments (R. C. Sims, UWRL, personal
communication, 1986). It should be stressed that each of these EPA documents
presents guidance only and not regulations.
The detailed design of a land treatment unit for gasifier wastes will
depend on the conditions at the specific site. Although onsite land treatment
is most economical, the location of many former gas plants in populated, urban
areas may preclude onsite treatment.
Regardless of whether treatment is to be conducted onsite or offsite, the
contaminated soil to be treated must be excavated and stockpiled at the treat-
ment site. The stockpile may be covered and placed on a liner to prevent
spread of contamination. The treatment area should be lined, and a leachate
collection system installed, to prevent migration of leachate. The contami-
nated soil is then laid down in 1 to 1.5 foot lifts, and soil amendments and
water are added as necessary to reach and maintain optimum soil condition for
degradation (determined in bench-scale and pilot-scale studies). It may be
necessary to blend clean soil with the waste or contaminated soil to achieve
the desired contaminant loading rate. The soil should be cultivated regularly
during the treatment process; soil conditions (moisture, pH, nutrients, etc.)
should be carefully monitored and controlled. Once the initial lift has been
detoxified, a second lift is placed on the previous lift, and so on until all
the soil is treated.
Leachate collected from the land treatment facility may be treated or
discharged without treatment, depending on the level of contaminants. At the
Minnesota creosote treatment site, the State and EPA permitted discharge of
leachate either into the Mississippi River or into the municipal sewage sys-
tem, depending on the level of PAH compounds in the leachate. This implies
that dissolved PAH's may be successfully treated in municipal wastewater
treatment plants.
Land treatment is therefore a well demonstrated, effective technology for
degrading PAH compounds. Field and bench-scale treatability studies on creo-
sotes have demonstrated that a range of initial loading rates are acceptable
and that degradation time increases with increasing loading rate. The selec-
tion of loading rate should balance land area requirements and time require-
251
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merits for completing the treatment process (Ryan and Smith, 1976). Lower
loading rates decrease the time required for degradation, and higher loading
rates decrease the land area requirements. Further information on the design A
and demonstration of land treatment may be found in Overcash and Pal (1979),
API (1983), and EPA (1983a and b, 1984a, b, and c).
2.3.3.4.2 Extraction or thermal treatment of excavated contaminated
soil--Hoogendoorn (1984) and Rulkens and Assnik (1984) reported on the succes-
sful pilot-scale use of a hot aqueous alkali solution to clean gasworks soil
contaminated with free and complexed cyanides. The process (Figure 67) has
been scaled-up to 25 tonnes/hr and is estimated to treat soils at a cost of
S24.80 to S99.20/m3. Soil is pretreated to remove large objects (wood and
stones) and to break up clods. It is then extracted with a lye solution, the
soil and cleaning agent are separated, and the extraction agent is cleaned by
pH adjustment, coagulation, flocculation, sludge separation, sludge dewater-
ing, and a second pH adjustment. The sludge, containing free and complexed
cyanides, may be landfilled or incinerated; hydrolysis also may be practical.
However, there is little experience in applying incineration and hydrolysis to
these sludges. The alkali extraction process should be applicable to soils
contaminated with PAH compounds as well (Hoogendoorn, 1984). Current applica-
tions are limited to clean sands; difficulty in applying extraction techniques"
to loamy soils include difficulty in separating clay/silt suspensions and
strong adsorption of contaminants and clay particles.
The excavation and extraction of contaminated soils is economical in the
Netherlands because of the high cost and intensive utilization of land and the
high demand for clean fill. In the United States, this alternative may not be
the most cost-effective one. The in-situ extraction of organics by alkali
solutions has been demonstrated for industrial sludges (Kosson et al., 1986).
This technique should be more economical than excavation and extraction, may
be applicable to organic-contaminated soils at gasworks, and may be more cost-
effective than excavation and extraction. However, in-situ alkali extraction
should not be used when cyanide contamination is present at a site because
strong alkalies can dissociate complex iron cyanides into free cyanide com-
pounds.
252
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LCNTAMlNAItU
SOU
AQUEOUS
ALKAII *
ACIDS
SOIL P«l
TRtATMfcNT
» SOU
»- uiATf U
1
/
EXTRACTION
<
SEPARATION
COARSE SANO
i
?
0£ WATERING I COARSE SANO
** NEUTRAL rSAT ION **^
AOUEOUS RE-OEPCS-TO.
< ' " ALKALI — ••**• OF CLEANED
1 SOIL
: A
SEPARATION
FINE SANO
i
PRECiPi
RECYCLING j
WASHING AND
OEWATERING "FINE SANO
-t ^ f <
i
TA T ftfMLJ
IA I nJN
» OCWATFR.NT .SLUOGt
SUJOGE 0tWATERING ^ICYANOE CONTAW«MG)
SEWERAGE
**TER * ' SYSTEM
Source: Hoogendoorn, 1984.
NOTE: The arrows indicate the level of original coal tar injection.
Figure 67. Treatment of soil by extraction with an aqueous solution.
253
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\
Thermal treatment methods (high-temperature evaporation and incineration)
also are applicable to soils contaminated with cyanides and PAH's
(Hoogendoorn, 1984). Unlike the alkali extraction process, both sandy and
clayey soils are amenable to thermal treatment methods. Evaporation at 850 °C
has been used to clean cyanide and PAH-contaminated soil excavated from a
gasworks site at Tilberg in the Netherlands. However, these techniques
require excavation of the soil and are more expensive (after excavation) than
is alkali extraction (Hoogendoorn, 1984). Thus, they may not be cost-effec-
tive even though they are technically effective.
2.3.3.4.3 Fixation—A novel, patented process for fixating wastes has
been applied to gasworks wastes at Dortmund in the Federal Republic of Germany
(U.S. Patent 4,456,400). Remedial investigations at the Dortmund site
revealed extensive contamination. Liquid coal tar was clearly visible to a
depth of 10 meters along with volatile hydrocarbons and sulfur compounds.
Large quantities of spent iron oxide (containing sulfur and complexed cya-
nides) from gas purification were also present.
Remediation at this site involved excavating and treating the contami-
nated soil, contaminated water, and waste by mixing it (onsite) with lignite
fly ash using the patented process (Heide and Werner, 1984). The treated
material was finally disposed in a specially designed plastic-lined pit loca-
ted on the site. This site cleanup was the first application of the technol-
ogy on such a large scale. This cleanup approach is expected to result in
considerable cost savings over an alternative plan involving removal of the
contaminated material to an offsite licensed disposal facility.
The treatment/solidification process relies on the pozzolonic properties
of the brown lignite fly ash. The ash used at this site was obtained from
local power plants burning brown lignite coal. The contaminated soil, tars,
and water are mixed with the ash in a three-stage reactor along with addition-
al water. The exothermic reaction must be controlled carefully to maintain a
continuous flow through the mixers. The product exiting the final mixing
stage is a freely flowable slurry and is conveyed directly to the lined pit.
Within approximately 30 minutes, the slurry hardens to a solid material that
is claimed to be virtually impermeable to water «10~8 cm/sec). Data from
numerous tests indicate that metals, sulfates, cyanides, and organics are f
j . 254
i
i
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bound tightly in the treated material and are not leached even under rigorous
conditions. Solid wastes, fluid suspensions, and sludges can all be treated
by this process, being combined with the fly ash in amounts up to 50 percent
by weight. Between 20 and 40 percent water is required in the process. From
the standpoint of gasworks waste, the process is attractive because it can fix
organic contaminants, cyanides, and sulfates.
The German governmental authorities granted approval for the site cleanup
plan after 2 years of reviewing the data to support the proposed process and
considering other alternatives. Protection of groundwater was the major con-
cern. After the remediation is completed, the site will be used again for
heavy industry. The pit containing the solidified waste will be monitored to
ensure that there is no leaching of contaminants.
One limiting factor in the process is the availability of sufficient
quantities of the lignite fly ash, which must be trucked in from local power
plants. Brown coal ash is different from the ash of U.S. bituminous or
anthracite coals because of its higher content of alkali metals (e.g., Na, K)
and alkaline Earth elements (e.g., Ca, Mg). Brown coal ash contains about 10
percent CaO; it also contains calcium ferrite and calcium sulfate (Heide and
Werner, 1984). It is this high concentration of calcium that is responsible
for its pozzolanic properties. The ash of Western coals also tends to have
higher calcium contents; however, the availability of fly ash from these coals
is limited. It is possible that other fixation agents could be identified
with similar properties or could be made up (e.g., by combining conventional
coal fly ash and lime). The effectiveness of the fixation process may be
evaluated by leaching tests such as EPA's EP or TCLP in soils. It may be the
method of choice for remediating contaminated soil at gas sites.
2.3.3.5 Contaminated Groundwater--
The most significant groundwater contaminants at gasworks sites are light
aromatics (e.g., benzene, toluene, xylene, ethylbenzene, naphthalene, acenaph-
thene indene). Incidents of significant offsite migration of gasworks contam-
inants in groundwater (e.g., Ames, Iowa; Dover, Delaware) have involved the
lighter components of gasworks tars and oils that are easy to detect at ppb
levels by the water's tdste and odor. The concentrations of the heavier PAH
compounds (three or more aromatic rings) in groundwater are generally lower,
255
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being controlled principally by their aqueous solubilities. PAH concentra-
tions tend to drop off rapidly beyond the coal tar source; the persistence of
these heavier compounds in groundwater beyond the immediate site area has not
been documented.
2.3.3.5.1 Source control--The most important step in the remediation of
contaminated groundwater is destruction or removal of the source of contamina-
tion. Until this is successfully accomplished, the success of groundwater
cleanup will be limited by continuing contaminant release at the source. It
is especially important to identify and remove any lighter organics (i.e.,
oils) present at a gasworks site because their higher solubilities and usual
occurrence above the water table give these organics a high potential to con-
taminate groundwater. The heavier tars tend to cause localized groundwater
contamination that is localized around the area of tar contamination. How-
ever, it is important to clean up free tars or to ensure that they will be
effectively contained onsite; free tars can migrate significant distances from
the site under certain subsurface conditions (see Section 2.1). Coal tars,
produced in processes that involve coal pyrolysis, have more potential to
contaminate groundwater than do water-gas or oil-gas tars because they contain
significant quantities of more soluble tar acids (e.g., phenols, cresols, and
xylenols.
Inorganic contaminants that can contaminate gasworks sites include sul-
fates (which can acidify groundwater) and trace elements (e.g., arsenic) asso-
ciated with gas manufacture. The source of these contaminants includes spent
oxide wastes and other solid waste from gas manufacture. Control of these
contaminant sources may be accomplished by removal or treatment; in many
cases, pH adjustment with limestone may be adequate treatment. Neutralization
reduces acidity, raises pH, and thereby controls trace metal release. The
potential for groundwater contamination by cyanides from solid wastes at gas-
works sites also must be considered; however, no cases of significant contami-
nation of groundwater by cyanides was found in this study. At the Birmingham,
Alabama, site, leachate from untreated spent oxide wastes had free cyanide
levels well below the level that can be effectively degraded by soil microbes
(200 ppm), in spite of a'pH
-------
2.3.3.5.2 Selection of groundwater treatment a1ternat1ves--In devising
remedial actions for contaminated groundwater, one must consider the follow-
ing:
• Containment control to prevent the further spread of contaminants
and to collect groundwater for treatment
• Treatment to destroy or remove contaminants in the groundwater.
Both of these factors must be addressed when devising remedial actions for
groundwater contaminants because the long times required to treat contaminated
groundwater necessitate the containment activities, and it is often necessary
to collect the groundwater prior to treatment.
Groundwater control measures for contaminant containment include physical
barriers and hydrologic barriers. Selection of appropriate technologies
depends on the hydrogeologic characteristics of the site and the extent of
contamination. For instance, physical barriers such as slurry walls, grout
curtains, and sheetpile cutoff walls and hydrologic barriers such as intercep-
tor trenches or subsurface drains are appropriate for sites where contamina-
tion is confined to the near surface (25 to 50 feet deep) and underlain by a
low-permeability layer into which the barrier may be keyed. Examples of the
use of physical barriers (slurry walls) during gasworks site remediation may
be found in the case studies for Stroudsburg, Pennsylvania, and Plattsburgh,
New York, in Chapter 3. When contamination extends to greater depths, or
where there is no natural barrier to vertical (downward) migration of the
contaminant plume, hydrologic barriers using pumping wells may be the only
appropriate control strategy. A hydrologic barrier using pumping wells was
employed to control contamination from the Ames, Iowa, gasworks (see Case
Studies, Chapter 3).
Groundwater collection strategies include subsurface drains and intercep-
tor trenches, which are appropriate for shallow contamination, and pumping
wells, which may be used for shallow or deep contaminated groundwater. Sub-
surface drains were used at Plattsburgh, New York, to collect incoming ground-
water to prevent breaching of the slurry wall. The drain system also served
to collect contaminated groundwater leaving the site (see Chapter 3). Pumping
wells were used to collect free coal tar at Stroudsburg, Pennsylvania, and
257
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contaminated groundwater at Ames, Iowa, and may be employed to control and
collect contaminated groundwater at St. Louis Park, Minnesota (see Chapter 3).
For further Information on the selection, evaluation, and design of
groundwater control strategies, see U.S. EPA (1982), Ehrenfleld and Bass
(1983), U.S. EPA (1984d), Boutwell et al. (1985), Schafer (1984), Xanthakos
(1979), and D'Appolonia (1980).
Treatment alternatives for groundwater contaminated with aromatlcs from
byproduct tars and oils include physical methods (e.g., carbon adsorption,
reverse osmosis), chemical methods (e.g., wet air oxidation, ozonation), and
biological methods (Ehrenfield and Bass, 1983). At St. Louis Park (see
Chapter 3), the groundwater remediation plan includes the use of granular-
activated carbon to clean up contaminated groundwater. At Ames, Iowa,
recovered contaminated groundwater was used, without treatment as boiler make-
up water at a nearby power plant. Microbes capable of degrading PAH compounds
were discovered in the contaminated Ames groundwater (see Case Study, Chapter
3). This suggests that, where groundwater is contaminated with organic
compounds from gas plant wastes, indigenous microbes capable of degrading
these organics may have evolved. In these cases, in-situ remediation may be
possible by containing the groundwater and allowing natural degradation to
take its course, with or without enhancement through the addition of oxygen
(or air) and nutrients. For more information on biological treatment methods
for contaminated groundwater, see Parkin and Calabria (1985).
2.3.4 Conclusions
The following conclusions can be made concerning the investigation and
remediation of town gas sites.
• Site investigation techniques used at abandoned town gas plants do
not differ significantly from those used at other uncontrolled
hazardous waste sites.
Because of the age of the sites, collection of historical Informa-
tion from company records, insurance maps, interviews with plant
personnel, aerial photos, etc., is an important first step in site
investigations at abandoned town gas plants.
• Surface geophysical techniques can be used to Identify buried struc-
tures, pipes, and subsurface zones of coal-tar contamination at
abandoned town gas plants, and they can help guide further site
Investigation activities.
258
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It is important to identify buried structures because these can
contain tars, oils, emulsions, and other contaminants. Care should
be exercised to avoid damage to these structures when using invasive
site investigation techniques or when conducting remedial actions.
If care is not taken, these substances may be released.
The probable presence of multiple-density contaminants (i.e., tars
and oils) should be considered when planning site investigation
activities and when evaluating remedial action alternatives.
The long-term stability (i.e., no release of hazardous substances
over a period of years) of some sites may make no-action a viable
alternative at some sites.
Free tars and oils recovered at a site often may be sold for bene-
ficial use as fuel or chemical feedstocks.
Land treatment has been proven effective In treating soil contamina-
ted with byproduct tars and oils. Other treatments used for remov-
ing or destroying heavy organics in soils also may be applicable.
Spent oxide wastes and soils contaminated with complex cyanide
compounds have been treated successfully by immobilizing with lime,
or with a combination of lime and pozzolonic material, and evapora-
tion at elevated temperatures.
The presence of indigenous microbes capable of degrading aromatic
compounds in the groundwater at Ames, Iowa, suggests that in-situ
biological treatment may be feasible for groundwater contaminated
with compounds from byproduct tars and oils.
259
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3.0 SITE INVESTIGATIONS OF SPECIFIC TOWN GAS SITES
3.1 INTRODUCTION
This chapter describes the specific town gas sites reviewed by RTI. It
is divided into two sections: Section 3.2 describes the sites visited by RTI
personnel, and Section 3.3 discusses case studies of town gas sites that have
been described in recent literature. This chapter is designed as a overview
of existing town gas sites, types of contaminants, and remedial actions.
In its review, RTI also collected some historical data from pre-1960
sources on specific sites that sometimes conflicted with the site information
reported by other investigators. These contradictions are also examined in
this chapter.
3.2 SITE VISITS PERFORMED BY RTI
3.2.1 Introduction
Mr. Scott Harkins of RTI visited six gas sites and one iron oxide dis-
posal site to permit RTI personnel to collect data and site assessments on
specific sites during the course of the project. Site assessments were avail-
able for only two of these gas sites (Lowell, Massachusetts, and Spencer,
Massachusetts) and the spent oxide disposal site (near Attleboro, Massachu-
setts). One site was chosen because the authors were familiar with it, and
because many of the structures were still present on the site (Richmond, Vir-
ginia). One other site (Taunton, Massachusetts) was recommended by the Massa-
chusetts Department of Environment Quality Engineering (DEQE), and the other
two were selected because they were within traveling distance of the other
sites examined (Pawtucket, Rhode Island, and Worchester, Massachusetts). All
of these sites and the information obtained during the site visits are
described in the next section.
261
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3.2.2 Colonial Gas Company, Lowell, Massachusetts
This Colonial Gas Company 1n Lowell, Massachusetts, was visited on March
3, 1986. The site examination consisted of reviewing the Phase 1 site
assessment, visually examining the plant site and surrounding area (without
entering the site), and collecting an early site map of the plant. This
17-acre site produced coal, water, oil, and LP gas for the town of Lowell,
Massachusetts. The plant began as a coal-gas plant in 1849, added carbureted
water gas during the 1870's, converted to oil gas between 1950 and 1951, and
was placed on standby in 1951. It operated intermittently between 1951 and
1975 to supplement natural gas supplies. The site is currently used as an
operations center and storage and gas distribution center by the Colonial Gas
Company (formerly the Lowell Gas Light Company). The site is approximately
300 feet from the Pawtuckett Canal, which removes water from the Merrimack
River, flows through the town of Lowell, and then returns to the river.
An 1876 map of Lowell (available at a local national park gift shop)
clearly shows the plant layout, with five large buildings and four masonry gas
holders. Two buildings on this map currently remain onsite. A vacant area is
seen next to the plant and is now part of the plant site.
A Phase 1 site investigation (problem definition and site history) of the
site was completed in December 1985 by M. Anthony Lally Associates, and a
Phase 2 site investigation (problem evaluation and field investigation) is
currently planned. These investigations were in response to observed volatile
contamination of soil and groundwater during an investigation of PCB contami-
nation on the property adjacent to the site. VOC's were detected at 65.1 mg/L
in groundwater flowing from the gas site.
Soil samples were taken and organic vapor concentrations measured from
shallow depths (0 to 3 feet) around the plant. Organic vapor concentrations
from the probe hole varied between 0 and 96 ppm, and soil concentrations were
between 0 and 37 ppm. Analyzed soil samples showed contamination by benzene
(0.013 mg/g), toluene (0.004 mg/g), ethyl benzene (0.030 mg/g), xylenes (0.23
mg/g), and assorted PAH compounds (1.09 mg/g). RTI's examination of the site
area found two small sources of oil flowing into the canal from the canal wall
nearest the gas site. The water in the canal was lowered for routine mainte-
nance during the visit. The canal itself, and several areas around the plant,
262
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had fairly strong gaseous odors, probably from gas plant wastes. Diagrams of
the plant site contained in the Phase 1 site assessment indicate a "deep well"
was present. This well was possibly used for waste condensate disposal
because any liquid wastes dumped into the canal would flow through the center
of town and pass through water-powered factories.
A literature review by RTI revealed that several articles were written by
engineers working at the Lowell plant. One article on oxide purification of
gas stated, "Because of the possibility of fires starting through the heat
generated by revivification, it is necessary to hold the spent material at the
plant until this danger is past. As soon as city authorities learn of this
menace ths material is prohibited at public dumps. Continuous storage on
gasworks land eventually becomes impossible. The material makes excellent
filling for roads or private property when properly handled. It should be
covered with ashes or dirt immediately to prevent the access of air and conse-
quent combustion. ...The plant is indeed fortunate it has a place to store the
spent oxide and doubly so if a transportation company will agree to remove it
without charge because of its value as a filling material" (Downing, Super-
intendent of Manufacturing, Lowell Gas Light Company, 1932).
Evidence of tor and oil contamination of the site was also located in an
article on gas plant wastes. "That large quantities of gas house waste can
enter the ground is strikingly shown by investigations made at the Lowell,
Massachusetts, gas works in 1905 and 1906 by A.T. Stafford and W.H. Clark, who
estimated that there existed within the ground and within an area of a few
acres 1,600,000 gallons of tarry and oily wastes. Some of these consisted of
accumulations in old drains and porous gravel, which when tapped by excava-
tions flowed out in springs. Much waste was regularly finding its way into
sewers, and from the sewers it entered cellars along the lines of sewers at
even remote distances from the works" (Hansen, 1916). RTI has yet to locate
the articles Hansen referred to, but if accurate, they indicate possible wide-
spread contamination from the facility.
3.2.3 Massachusetts Electric Company, Spencer, Massachusetts
The Massachusetts Electric Company in Spencer, Massachusetts, was exam-
ined on March 4, 1986. The site examination consisted of viewing the fenced
portion of the site through the fence, making an examination of the perimeter
263
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of the site, and examining the site assessment prepared by Perkins Jordan in
January 1984.
The site came to the attention of the Massachusetts DEQE when a truckload
of soil (removed so that a drainage culvert could be installed) was delivered
to a landfill during a routine inspection of the landfill. The inspector
recognized the materials as being gas production wastes and ordered that they
be returned to the site. A subsequent site investigation by Perkins Jordan
used nine test pits, seven borings, and two test wells.
Tins also was the site of a very small carbureted water-gas plant.
(Brown's Directory and the 1917 report of the Massachusetts Board of Gas and
Light Commissioners show it to be a carbureted water-gas plant, but the site
assessment identifies it as coal-gas plant.) It was constructed between 1885
and 1887 and operated into the 1950's. The site is approximately 0.4 acres
and adjacent to a small stream, the "Muzzy Meadow Brook." It is currently
fenced off and is the site of a power substation. Wastes typical of carbu-
reted water-gas plants (coal, coke, ash, slag and tars) were identified at the
site. About 15 to 20 feet of soil rests on top of the bedrock at the site.
The depths of the test well and pits were limited by the bedrock under the
site.
Soil samples were found to be contaminated with toluene, benzene, ethyl- M
benzene, PAH compounds, and xylenes. Groundwater samples contained low levels
of PAH and volatile compounds. Table 49 shows the measured concentrations of
volatile and semi volatile compounds in soil and w, samples from test pits
and brook samples. Table 50 shows the same analy -oil samples from
borings, and Table 51 shows concentrations from mo1
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TABLE 50. VOLATILE AND SEMIVOLATILE ORGANIC ASSAY
RESULTS FROM BORING SAMPLES
Chemical compounds
Volatile organics
Toluene
Benzene
Ethylbenzene
Xylenes
Semi volatile organics
Acenapthylene
Acenaphthene
Benzo(k)fluorene
Benzo(a)pyrene
Chrysene
Fluoranthene
Fluorene
Phenanthrene
Pyrene
Naphthalene
Diethylphthalate
Bis{2 ethylhexyl)phthalate
Di-n-butylphthalate
Total polynuclear aromatic
hydrocarbons (PAH's)
B-2
S-42 & 43
5.80
75.0
41.0
53.0
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
NA
Soil samples
B-2
S-41
NA
NA
NA
NA
80.0
46.0
11.0
100
31.0
130
170
370
100
670
--
--
--
1,708
(mg/kg) ppm
B-3C
S-48
NA
NA
NA
NA
4.60
9.30
—
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--
6.70
8.40
21.0
8.0
39.0
—
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98.3
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NA
NA
NA
NA
--
--
0.520
0.720
2.00
—
1.60
1.40
--
--
--
--
6.24
SOURCE: Perkins Jordan, 1984.
NA = Not analyzed.
-- = Not detected.
B = Boring identification.
S = Sample number.
266
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TABLE 51. VOLATILE AND SEMIVOLATILE ASSAY RESULTS
FROM MONITORING WELLS
Groundwater samples (mg/L) ppm
(taken on 11-30-83)
Chemical compounds MW-1 MW-2
Volatile organics
Toluene 0.0095 0.120
Benzene 0.071 0.410
Ethylbenzene 0.015 0.480
Xylenes 0.068 0.610
Semi volatile organics
Acenaphthylene ND 0.041
Acenaphthene ND 0.032
Anthracene ND 0.004
Fluorene ND 0.030
Naphthalene ND 1.000
Total polynuclear aromatic
hydrocarbons (PAH's) ND 1.147
SOURCE: Perkins Jordan, 1984.
MW = Monitoring well.
ND = Not detected.
267
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A complete investigation (documented in transcripts in "The Affairs of
the Richmond Gas Works," [no author] 1896) followed a major scandal at the gas
plant shortly after the conversion, thereby marking that year. The scandal
involved several plant supervisors who were dumping ash-coke mixtures from the
water-gas generators before most of the coke was converted to gas and ash.
This allowed the ash to be hauled from the plant and the coke recovered and
sold for the profit of those who stole it. Also during this period, the plant
operated for 9 months with no down-run on the carbureted water-gas apparatus
(the down-run valve had burned out). This caused poor heating of the appara-
tus and resulted in the inadequate cracking of carburetion oils. The creek
behind the plant was reportedly full of oil that overflowed from the relief
holder with condensate.
The report states that the fences were rotted, the roofs decayed, the
coal benches were clogged and had to be rebuilt, the water-gas plant needed to
be relined, new castings and valves were needed, the purifying house oxide
boxes were rusted and leaking, the condensers were broken, employees were A
mismanaged, and coke was constantly stolen. The report indicates that the
plant sold coke, tar, sulfate (probably ammonium sulfate), lime, and junk (the
type of junk was not defined).
When the plant switched to carbureted water gas, they also switched from
lime purification to the use of iron oxide (the new purifier house was erected
in 1894). They had previously used 9,000 to 10,000 bushels of lime per month
(415 to 460 ft^). This use dropped to 80 bushels per month after converting
to iron oxide purification. This gas plant, also referred to as the lower
gasworks, is shown on maps in the library. One map from 1888 clearly shows
another gas plant along the river, closer to the center of the city. An 1876
map of the gasworks (Figure 68) clearly shows the plant layout and structure.
The round object below the coal shed is labeled as a retort by the mapmaker,
but it is actually a gas holder for the plant.
The plant continued to produce water gas until the early 1950's, when the
plant was converted to LP gas for peak loads and standby operation. Most of
the buildings present in 1950 remain on the site, i.e., the gas house, com-
pressor building, purifier buildings, coal shed, and gas holder. The purifier^
building has been converted into a welding shop and classrooms for the
268
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Figure 68. Fulton Gas Works (1876).
269
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current, municipally owned gas company. The other buildings are not used and
probably would have been removed many years ago if the plant were not city
owned. (Cities do not collect property taxes from their buildings.) All of
the buildings, except the purifier building and the gas holder, were to be
removed during the spring of 1986.
The site is adjacent to a concrete culvert (formerly a creek) that flows
into the James River about 600 feet from the site. The area between the gas
plant and the creek shows substantial signs of being a dump area for the
plant, with contaminated woodchips, ash, coke, firebricks, and tar present.
No site or environmental assessment of the plant is currently planned prior to
removing site structures. The entire site was flooded with about 6 feet of
water from the James River during the fall of 1985.
3.2.5 Hendon Road Spent Iron Oxide Disposal Site, near Attleboro,
Massachusetts
The Mendon Road Spent Iron Oxide Disposal Site near Attleboro, Massachu-
setts, was visited on March 3, 1986. The site was evaluated by visiting the
site during site remediation and by examining two reports of the site, a geo- "
hydrologic study by Clean Harbors, Inc. (May 1985) and a hazardous waste
evaluation by Hydrosample (November 1984). This was not a gas site, but a
site where some spent oxide waste was disposed. The site was originally a
gravel pit, but it later became a dump and was recently filled and houses were
constructed on the site. When the land was purchased, the buyers sent a sam-
ple of the waste to the State health department to approve construction. The.
perk tests revealed additional waste, and this information was sent to the
Massachusetts DEQE. After two subsequent site investigations, removal of the
spent oxide wastes began with funding from the State Superfund.
The waste is spent iron oxide (mixed with woodchips) from coal-gas manu-
facture. The waste was apparently used as fill at the site, with other fill
material above and below the waste "seam." The waste material consisted of
contaminated woodchips with high concentrations of PAH compounds, iron cyan-
ides (total CN 7,500 ppm, soluble CN 0.7 ppm), and low pH (1.7 to 3.8). It
passes the EP toxicity but has a high total metal content. The waste was a
seam of material with a maximum thickness of about 3 feet, covered by between
1 and 4 feet of clean topsoil. The site remediation was to remove all cyanide™
270
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to a concentration of 2 ppm in the soil. Clean topsoil was removed and put
aside; the waste and an additional foot of soil below the waste were removed,
stabilized with calcium sulfate, and transported to a hazardous waste landfill
in Alabama. The resulting holes were filled with clean fill dirt. An early
estimate of the necessary remediation was removal of 2,500 ft^ of contamina-
tion at a cost of SI.6 million.
The solubility of the iron cyanide compounds in water was evidently very
small. The cyanide wastes were removed from the equipment used in the
remediation by physical means only. The equipment was hosed off with water,
and the water was drained, into a holding tank (approximately 200 gallons).
The solids were allowed to settle to the bottom of the tank, and the clear
water was removed from the top of the tank. This water was then run through a
sand filter, and the resulting water was discharged without further treatment.
The cyanides were essentially all removed by settling and filtration with
sand. The material that settled in the tank, and the tank itself, were to be
discarded in the Alabama landfill at the end of the remediation.
A similar disposal of spent oxide wastes is on the ground surface just
across the Rhode Island border.
3.2.6 Pawtucket, Rhode Island
The Pawtucket, Rhode Island, site was examined on March 5, 1986. It was
evaluated by only a visual examination of the plant site and by data from
Brown's Directory. This is a fairly large gas site that produced both coal
and water gas during operation and had an electrical power plant as part of
the site. The site occupies 20 to 40 acres between a residential neighborhood
and the Seekonk tidal basin, just south of Pawtucket, about 3.5 miles from the
Attleboro road site in Massachusetts. Part of the site is currently used as
an electrical substation and for the distribution of natural gas. There were
several areas of the site that contained spent oxide wastes similar to that at
Mendon Road (e.g., woodchips from spent oxide, and blue areas of soil from
ferrocyanides). A substantial amount of waste from the gas production and
power generation was visible on and around the site, evidently as fill.
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3.2.7 Taunton, Massachusetts ™
The Taunton, Massachusetts, site was visited on March 3, 1986, with a
representative of the Massachusetts DEQE. The site was examined visually. It
is a mid-sized gas plant that primarily produced coal gas but later produced
water gas (Brown's Directory, as reported by Radian Corp). Constructed around
1890, the plant added water gas around 1920. The site, approximately 15
acres, is in an industrial area south of Taunton, adjacent to the Taunton
River. All of the structures were removed in the early 1960's, but the site
has never been properly decommissioned. Gas-holding tanks were cut off at
ground level and filled with soil from the site. It is very unlikely that any
underground structures were removed. The plant was located at the northern
end of the site, and the southern part of the site was evidently used as a
waste disposal area. The State OEQE was called by the gas company in the
early 1970's to stop waste materials from eroding into the river. Eventually,
the southern half of the site was capped with a layer of clay soil and top-
soil. This southern half has a small stream that crosses it and currently
flows through a lined culvert. The northern half has remained uncovered. No A
waste materials have been removed from the site, and approximately 1 to 3 feet
of mixed wastes are under the capped area. Heavy tars, ash, and spent oxide
wastes are visible in the uncapped area. The site is currently fenced, and
the local gas company operates a standby LP gas facility across the street.
No additional remedial actions or in-depth site studies are currently planned
for the si te.
3.2.8 Worchester, Massachusetts
The Worchester, Massachusetts, site was visited on March 4, 1986. The
city was chosen because it is large, happens to be close to Spencer, and is
listed in Radian's 1984 compilation of U.S. gas sites. Some information and
maps of the plant site were located in the Worchester public library. The
Worchester Gas company, chartered in 1849, moved to a 9-acre site on
Quinsigamond Avenue in 1869. It produced both coal and water gas. Currently,
the site is used by the Commonwealth Gas Co. as a gas storage and distribution
facility. The entire site has been capped with approximately 3 feet thick of
construction refuse and fill. The site has no noticeable wastes and only a ^
272
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slight odor. An EPA pollution control project (Project C250.347-04), a new
S7.5 million (S5.5 million Federal, SI million State) sewage treatment
facility, is to be newly constructed on the gas site (as indicated by a sign
on the property).
3.3 CASE STUDIES OF TOWN GAS SITES
3.3.1 Introduction
The case studies in this chapter were selected to demonstrate the types,
modes of occurrence, and persistence of contaminants at abandoned manufactured-
gas sites, as well as applicable remedial measures for these sites. The case
studies are presented to support the material discussed in the preceding chap-
ters. They were collected from published literature, State and Federal agen-
cies, and previous work at RTI. Differences in detail between the studies
reflect different amounts of information available for specific sites. In
addition to six former gasification sites, two byproduct tar utilization
facilities, a creosoting plant (Pensacola, Florida), and a coal-tar processor
(St. Louis Park, Minnesota) are included. These two studies offer well-
documented evidence of migration and degradation of coal-tar derivatives in
the subsurface that is relevant to contamination at gas plants.
The case studies were compiled from the references presented at the
beginning of each study.
3.3.2 Norwich, Great Britain (Wood, 1962)
The Norwich, Great Britain, site is the oldest site found during this
study, having groundwater contamination from tar present for over a century.
It illustrates the potential persistence of gasworks tar in the subsurface
environment, both in terms of the tar's appearance and its potential to con-
taminate groundwater.
In 1950-1951, a 36-inch bore was sunk into the chalk aquifer underlying
Norwich for water-supply purposes. Although it produced water of sufficient
quality for its intended use, the well's yield was inadequate. To remedy
this, a horizontal adit was drilled from the bore into the chalk at a depth of
150 feet below the surface. Shortly after, the water acquired a tarry taste
and thus was rendered unusable. Subsequent colorimetric analysis Indicated
273
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that the water contained about 0.2 ppm total phenols, which appeared to be
largely cresols. Thiocyanates were below the detection limit of 0.01 ppm.
Inspection of the adit by descent into the well showed black tarry matter
eluding from the adit roof. Samples of the tar contained a small proportion
of volatile matter, which had a trace of phenols, but was mainly composed of a
yellow oil with a blue fluorescence in benzene solution (suggesting the pre-
sence of aromatic compounds). The larger portion of the tar sample was non-
volatile, tarry in consistency and odor, and contained particles of solid
carbon.
The source of the tar was originally a mystery because the site was far
from the Norwich gasworks. However, subsequent investigation revealed that
the first gasworks plant in Norwich was constructed over this site. That
plant, which operated from 1815 to 1830, produced gas from destructive distil-
lation of whale oil by the Taylor process. Thus, the well constructed in 1951
was polluted by tar that had been lying in the ground for over 120 years.
This case study illustrates that tar from town gas processes can persist
and retain its potential for environmental damage for over a century. The
amount of tar degradation that may have occurred is impossible to estimate
because there is little information on the original tar composition. However,
of signiTicance is that at least some of the tar acids (phenols and cresols)
have persisted in spite of their high solubility, and they have contaminated
groundwatcr. The absence of thiocyanates is expected because of the low sul-
fur content of whale oil. The tar's appearance and odor is similar to that of
coal tar, illustrating that, with the exception of the formation of sulfur and
nitrogen compounds, the gas production process is more important than feed-
stock composition in influencing tar formation. The "steam-volatile matter"
reported by Wood (1962) probably corresponds to the naphtha or light oil frac-
tion of tar, and it may be responsible for much of the observed groundwater
contamination.
3.3.3 Ames, Iowa (Siudyla, 1975; Yazicigil, 1977; Yazicigil and Sendlein,
1981; Burnham et al., 1972; Burnham et al., 1973; Ogawa et al., 1981)
The Ames, Iowa, case study illustrates long-term contamination of a water
supply by town gas wastes from a relatively small gas plant that served about
15,000 customers. Groundwater contamination was first detected by taste and
274
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odor problems in 1927 and has persisted into the 1980's. This case study
illustrates the following:
• Site discovery through odors in water caused by ppb levels of
dissolved tar constituents in groundwater
• Contamination of groundwater by lighter tar fractions (tar
oils) that are less dense than water and more soluble than
heavier tar components
• Contaminant sources resulting from town gas waste disposal
practices
• Contamination by tar wastes from a water-gas process, notable
by their lacK of tar acids (phenols, cresols, xylenols)
• Migration of contaminants through cracks in soil to the water
table
• Influence of pumping wells on the migration of dissolved coal
tar constituents in the groundwater
Use of historical data in a site investigation
• Degradation of PAH's by microbes naturally occurring in ground-
water at Ames
• Remediation through removal of contaminant sources, instal-
lation of barrier wells, and controlled municipal well pumpage.
3.3.3.1 Site History--
According to Siudyla (1975), who interviewed long-time residents of Ames,
town gas was produced in Ames from 1911 until 1927. The original gas plant
was in operation from 1911 until 1920, and it was located in the western sec-
tor of the Ames well field. In 1920, the plant was moved to its final loca-
tion. Although there was a waste pit at the original plant site, 70 feet of
glacial drift isolated this source from the underlying buried channel-sand
aquifer. However, the drilling of a municipal well in 1968 through the pit
and into the underlying aquifer resulted in some contamination of the aquifer
by PAH's. Contaminant levels at the well have decreased over the years
because the well has been pumped (Siudyla, 1975).
Brown's Directory indicates that the Ames plant operated from 1912 until
about 1932 when gas lines were completed from Boone, Iowa. There is no men-
tion of the plant's 1920 move, but 1t is indicated that Iowa Railway and Light
275
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purchased the gasworks in 1925. According to Brown's, the plant produced
carbureted water gas over most of its history, with some coal gas being
produced from 1916 to 1918. The directory notes that bituminous coal was used
to fuel the plant after 1924. The operating data from Brown's is compiled in
Table 52. No mention is made of fuel type prior to this entry, although coke,
anthracite, or bituminous coals would be used in the generator, and gas oil or
fuel oil would be used in the carburetor.
The appearance of a disagreeable taste and odor in groundwater from two
city wells first occurred in 1927. The timing of the appearance could be
related to the change in plant management in 1925, which could have affected
waste disposal practices, or it may just reflect the time it took the contami-
nants to reach the wells from the source. In the early 1930's, three auger
holes showed increasing concentrations of contaminants toward the waste pit at
the second gas plant site, which was then recognized as the source of contami-
nation. At that time, investigators determined that abandoning contaminated
wells and drilling new wells farther from the source was the best solution.
This practice was followed until 1961, when the wastes from the second pit
were removed to a sanitary landfill in an attempt to mitigate the problem. It
did not. By the late 1960's, five wells had been abandoned and several were
restricted to limited pumping.
In 1975, Siudyla interviewed a former gas plant employee and discovered
that an overflow channel not visible on any city maps had once flowed from the
waste pit to the Skunk River. Although now buried with fill, the channel was
described as once being "odorous...containing pools of coal tar wastes"
(Siudyla, 1975). Subsequent sampling showed that oils had collected in two
low areas in the former channel and were floating on top of the water table at
these locations. These areas were identified as the contamination sources of
the city's water supply aquifer. The type of organic contamination was thus
discovered, and its oily nature is consistent with the disposal of waste con-
densate (and floating oils) from carbureted water-gas manufacture.
3.3.3.2 Extent of Contamination--
As previously described, the taste and odor problems in Ames' groundwater
have existed since 1927. Originally attributed to phenolic compounds, analyt-
ical work in the early 1970's showed a notable lack of phenolics. The
276
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predominant contributor to taste and odor was found in the neutral component
cf the groundwater organics, which included several aromatic compounds. Table
53 presents concentrations of these organics. No basic organic compounds were
found. The lack of tar acids (i.e., phenolics) is consistent with the water-
gas process that operated at the site; water gas does not produce significant
tar acids.
Recent analysis of Ames1 groundwater for heavier PAH compounds [e.g.,
phenanthrene, benzo(a)pyrene] has shown these compounds to be present, but at
very low concentrations (Tom Neumann, Ames Municipal Water Department, per-
sonal communication, 1986). The concentrations of heavier PAH's in water from
the dewatering wells were slightly higher than those in water use wells, but
no wells showed total PAH levels above 100 + 80 ng./L, and all levels were
below levels of concern and World Health Organization (WHO) water quality
criteria. The low level of the heavier PAH's is consistent with their low
solubility in waters.
The source of contaminants in the Ames1 aquifers was the waste pit and
the overflow channels. There is no information on the type and disposition of
contaminants in the original disposal pit prior to its removal in 1961. The
overflow channel did receive some pit wastes, but these may largely represent
the lighter floating components of the tar and wastewater disposed in the pit.
Soil auger borings and test pits were used to investigate the overflow chan-
nel. The borings showed four levels of contamination: (1) odor, oil, and tar;
(2) odor and oil; (3) odor alone; and (4) no odor.
Determination of the vertical extent of contamination from the soil bor-
ings was difficult because of contamination of the auger as it passed through
the upper levels of oily and tarry materials. Test pits, dug to 10 feet,
showed that the contaminants had moved downward through vertical cracks in the
alluvial materials and that oil was floating on the groundwater table
(Yazicigil and Sendlein, 1981). Subsequent excavation of the contaminated
material indicated that heavier contaminants (heavy oil and tar) had moved
below the water table and that pockets of tar in an almost solid state existed
in the excavated material. Excavation depths were limited to 15 feet because
of the high water table (at 8 feet). However, the lighter oil, floating on
the water table, was probably largely responsible for the taste and odor
279
-------
TABLE 53. NEUTRAL COMPOUNDS IN A CONTAMINATED AMES, IOWA, WELL
Concentration Std.
Compound (ppb) Dev.
Acenaphthylene 19.3 1.4
1-Methylnaphthalene 11.0 0.6
Methylindenes 18.8 0.8
Indene 18.0 1.5
Acenaphthene 1.7 0.2
2-2-Benzothiophene 0.37 0.11
Isopropylbenzene
Ethyl benzene
Naphthalene
2,3-Dihydroindene 15
Alkyl-2,3-dihydroindene
Alkyl benzenes
Alkyl benzothiophenes
Alkyl naphthalenes
SOURCE: Burnham et al., 1972.
280
-------
i
problems in groundwater, and this was removed by the excavation of the channel
area.
The well field for Ames, to the north of the site, has been contaminated
by tar constituents in spite of a regional hydrologic gradient to the south-
east. Pumping of municipal wells appears to have locally reversed the grad-
ient, causing contaminants to flow northward from the source to the municipal
wellfield. Burnham et al. (1973) demonstrated that total concentrations of
aromatics at a given well in 1972 were directly proportional to the demand
placed on the well (total pumpage) over a period from 1935 to 1972. Drawing
on this conclusion, Yazicigil and Sendlein (1982) modeled the Ames1 aquifer
system and various remediation alternatives. Based on their investigation,
they suggested removal of the source materials, installation of pumping wells
to create a hydrologic barrier between the source and the wellfield, and con-
trolled municipal well pumpage to control the problem and prevent further well
contamination.
Ogawa et al. (1981) studied the degradation of aromatic compounds in
samples of Ames1 groundwater. They found that, at a 25 to 150 /jg/l concentra
tion, acenaphthylene, acenaphthene, 2-methylnaphthalene, 2-methylindene, 3-
methylcindene, and indene were almost totally degraded at ambient temperature
within 3 days. Decay rates were highest for acenaphthylene and lowest for
indene. Additionally, acenaphthylene was degraded even when spiked into the
Ames1 well water at its solubility limit (3 mg/L). Degradation could be pre-
vented by filtering the groundwater through a 0.45-/im filter. Samples of
distilled water and uncontaminated Ames1 groundwater that were spiked with
acenaphthylene (at 80 /jg/L) showed no degradation of this compound after 18
days. However, when similarly spiked samples when inoculated with water from
a contaminated Ames' well, the acenaphthylene was degraded within 9 days.
Inoculation with anaerobic and aerobic bacteria from a sewage treatment plant
resulted in no degradation.
These results suggest that a population of microbes capable of degrading
aromatic compounds has adapted in the contaminated Ames' groundwater. Cell
mass measurements and microorganism counts further support this conclusion.
Correlated with the decrease in aromatic constituents, Ogawa et al. (1981)
281
-------
observed an increase in both cell mass (from 2 to 20 mg/L) and microorganism
count (from 102 to 104 cells/ml).
Ogawa et al. (1981) also measured the degradation of heavier PAH com-
pounds spiked into aged Ames' groundwater that was formerly contaminated.
Acenaphthene, phenanthrene, and fluoranthene (added at a 150 /*g/L level) were
degraded within 36 days, Pyrene, which had the same concentration, was
56 percent degraded in the same period. Thus, degradation rate of the PAH
compounds decreases as the number of rings increases, as was also illustrated
by degradation rates for the lighter PAH compounds (discussed previously).
The Ogawa et al. (1981) study demonstrates that dissolved PAH compounds,
at concentrations up to their solubility limit, can be degraded by microbes
naturally occurring in groundwater and that these microbes do not normally
occur in groundwater, but may adapt in groundwater contaminated with PAH
compounds. These conclusions are important for the remediation of abandoned
coal gasification sites. Degradation of compounds by microbes suggests that
cleanup of groundwater contamination may be possible by somehow enhancing this
degradation, either by aeration and adding nutrients to the groundwater and/or
by enhancing the degradation rates of these microbes by breeding more active
strains. Additionally, groundwater with no PAH-degrading microbes may be
inoculated with water from groundwater systems where microbial degradation is
occurring.
3.3.3.3 Site Remediation--
To date, site remediation at Ames has consisted of following the recom-
mendations of Yazicigil .and Sendlein (1982), i.e., removal of the source of
contamination, installation of two dewatering wells to form a hydrological
barrier between the source and the wellfield, and careful management of the
pumpage in the individual city wells.
The sources in the overflow channel were removed in 1980-1981 by excavat-
ing a 30 x 70 x 15 foot deep trench, removing contaminated material to a land-
fill, and replacing it with clean fill along the length of the channel. Two
dewatering wells, installed to the north of the channel to permit this excava-
tion, are now pumped to create a hydrologic barrier between the overflow chan-
nel and the weM field to the north. Water from these wells is used at a near-
by power plant. It is too early to assess the effectiveness of the removal
282
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action in mitigating the contamination, but increases in contaminant levels
have not been observed in either the barrier wells or in the last two wells
closed in the municipal wellfield (Tom Neumann, Ames Municipal Water Depart-
ment, personal communication, 1986).
Questions remain about whether the source of contamination has been suf-
ficiently removed because the depth of the excavation of the channel was lim-
ited to 15 feet due to a high water table. If the source were removed or
reduced to a size that results in a slower, low-level release of contaminants,
it is possible that microbial degradation may eventually reduce contaminant
levels in the aquifer. Otherwise, it may be necessary to continually pump the
dewatering wells and carefully manage pumping of the aquifer to control con-
taminant migration.
3.3.4 STROUDSBURG, PENNSYLVANIA (Adaska and Cavalli, 1984; Berg, 1975;
Campbell et al., 1979; Hem, 1970; Hult and Schoenberg, 1981;
Lafornara et al., 1982; McManus, 1982; Schmidt, 1943; Unites and
Houseman, 1982; Villaume, 1982; Villaume et al., 1983)
The Stroudsburg, Pennsylvania, town gas site, located next to Brodhead
Creek, was in operation from the mid-1800's until 1939. During plant opera-
tions, the production byproducts (mainly byproduct tars) were disposed in open
trenches and later in an underground injection well located onsite. After
severe flooding in 1955 from Hurricane Diane, the Army Corps of Engineers
modified the Brodhead Creek Channel. In 1980, the channel was deepened to
prevent undercutting of the levee. At this time, black tarry globules were
observed emanating from the base of the dike along the western bank of Brod-
head Creek. The site was reported to the National Response Center, and the
EPA initiated an investigative study. The study found that tar was present in
the subsurface at the site; the tar was confined primarily to coarse clean
gravels and had collected in a large depression underlain by a fine silty
sand. The site was listed as a priority Superfund site and was the first one
in the nation to receive em- rgency Superfund money. This case study illus-
trates the following:
• Site discovery through discharge into an adjacent stream
• Role of capillary pressure in controlling the movement of coal
tar
283
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• Recovery of free coal tar in the subsurface by pumping through
a 30-inch gravel-packed well
• Increasing the efficiency of tar recovery by pumping the over-
lying groundwater to create a negative pressure and make the
tar upwel\
• Construction of a 648-foot bentonite-cement slurry cutoff wall
on the streamside of the western le^ee to contain the contami-
nation and prevent further seepage into the streambed
• Possible misinterpretation of historical data, leading to
erroneous conclusions about the site, the nature of the contam-
ination, and site remediation (see the next section).
3.3.4.1 Site History--
In light of the information collected during RTI's historical literature
review, some of the previous site historical information about the Stroudsburg
plant appears to be incorrect. This section compiles the site history and
processes reported in the current literature, and Section 3.3.4.4 addresses
the contradictions between this section and data collected by RTI.
The Stroudsburg coal gasification site is located in the borough of
Stroudsburg, Pennsylvania, along the western bank of Brodhead Creek (Figure
69). The geology of the area consists of limestone bedrock overlain by a
valley-fill-type deposit. The valley-fill-type deposit is made up of an
underlying, well-sorted, fine, silty sand overlain by both stratified and
unstratified, well-sorted, coarse glacial gravels. .Inside the western levee
is a single, steep-sided, gravel-filled depression, probably a kettle feature.
The median depth to groundwater previous to any remediation was 10 feet, the
hydraulic gradient was 0.015 foot per foot, and the groundwater generally
flowed to the southwest at the rate of about 2 feet oer day (Villaume et al.,
1983) (also see Figure 70).
The plant was built in the mid-1800's and was in operation until 1939.
The coal gas was manufactured by heating pulverized coal in a reaction vessel
to drive off the volatiles. Superheated steam was then passed over the hot
coal to produce a gas-steam mixture that was blown into a large holding tank.
In this tank, the steam condensed, leaving the gas at the top and a liquid
containing coal tar at the bottom. The major byproducts of this procedure
284
-------
Figure 69. Stroudsburg site map with top-of-contamination (dash) and
ground water (dot-dash) contours (in feet) shown. The
groundwater data are for June 12,1981, prior to slurry wail
construction. Almost no free coal tar occurs beyond the
374-foot contour.
Source: Villaume et al., 1983.
Figure 70. Top-of-sand contours (in feet) for the Stroudsburg
coal-tar contamination site.
Source: Villaume et al., 1983.
285
-------
were the coal tar left In the reaction vessel and the liquid containing coal
tar in the holding tank.
lafornara et al. (1982) estimate that as much as 16 million gallons of
coal -tar could have been produced over the 100-year operating life of the
Stroudsburg gas plant. Initially, the reaction vessel coal tar was disposed
in open trenches that ran along the western edge of the site, eventually
discharging into Brodhead creek, and the water and tar that collected in the
holding tanks were blown down onto the ground next to the tanks (Lafornara et
al., 1982). In the early 1900's, as coal-tar reprocessing technology devel-
oped, the coal-tar wastes were purified onsite to remove the commercially
valuable constituents. The remaining wastes were disposed in an underground
injection well onsite. This method of disposal continued until the plant shut
down in 1939.
Brodhead Creek experienced severe flooding in 1955 as a result of Hurri-
cane Diane. Between 1958 and 1960, the Army Corps of Engineers had to modify
the stream channel by straightening several reaches of the stream and placing
the channel within a floodway lined by riprapped levees. Within the next 20
years, the levees experienced significant downcutting, causing officials to
deepen the riprap another 10 feet in 1980 to protect the levees from under-
cutting. During this work, coal tar was identified in the open trenches along
the western bank of Brodhead Creek.
In 1981, the site was reported to the National Response Center. The EPA
ordered all affected .-roperty owners to conduct a study to determine the
extent of the contamination and a method of rectifying the damage. The
Stroudsburg, Pennsylvania, site appears on the expanded list of 418 priority
Superfund sites (which currently number 388) and was the first site in the
nation to receive emergency Superfund money (Lafornara et al., 1982; McManus,
1982; Unites and Houseman, 1982; Villaume, 1982).
3.3.4.2 Extent of Contamination--
Based on the 1981 investigative studies, up to 1.8 million gallons of
free coal tar is estimated to be distributed over an 8-acre area (Figure 50).
The contamination extends vertically downward only to the top of the silty
sand deposit. This deposit currently cannot be penetrated by the coal tar
because of the extreme capillary-pressure forces that must be overcome. An
286
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accumulation of up to 35,000 gallons of nearly pure coal tar was estimated to
occur in a single stratigraphic depression located just below the old
gasification plant (Figure 51).
Capillary pressure (P) is defined by the equation:
P = 27 cos 0 / R
where
7 = the interfacial tension between the coal tar and water
0 = the contact (wetting) angle formed by the coal tar against a
solid surface in the presence of water
R = the radius of the water-filled pore that the coal tar is trying
to enter.
The displacement of water by coal tar is most difficult when the capillary
pressure is high, by definition indicating a high interfacial tension and low
contact angle. Once the interfacial tension and contact angle are set, the
pore size of the rock determines whether the coal tar can move into the media.
Using Hobson's Formula (Berg, 1975), the critical height of coal tar needed to
overcome the capillary pressure is calculated to be more than 10 meters. The
maximum thickness of coal tar in the contaminated zone at any location onsite
does not exceed 5.5 meters. The high capillary pressure and lack of critical
column height of the coal tar explains why the silty-sand deposit serves as an
effective barrier to the coal tar.
Hydrodynamic dispersion would be expected under onsite groundwater flow
conditions. Shallow groundwater samples from throughout the site indicate the
presence of dissolved contaminants. Partial analysis of the Stroudsburg coal
tar is shown in Table 54. The polynuclear aromatics were generally detected
at the ppb level or within the range of known aqueous solubilities of the
individual chemical species involved. Table 55 shows that the principal
control on the concentrations of these contaminants in the groundwater is
their aqueous solubility and not their concentration in the coal tar. There
is not enough data at this time to determine whether a relationship exists
between solubility and distance of transport; however, there appears to be a
rapid decrease in concentration just beyond the free coal-tar plume in the
downgradient direction. The only contaminant detected at this point is naph-
thalene at less than 10 ppb.
287
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TABLE 54. PARTIAL ANALYSIS OF THE STROUOSBURG COAL TAR
Parameter Value Units
Naphthalene 3.60 I
Fluoranthene 3.20 %
Phenanthrene 2.30 %
Anthracene 2.30 %
Dimethyl naphthalenes 2.15 %
Trimethyl naphthalenes 1.78 \
Methyl phenanthrenes 1.50 %
Trimethyl benzene 1.30 ',-
Fluorene 0.98 %
Acenaphthylene 0.74 \
Acenaphthene 0.72 %
Pyrene 0.56 i
Benzo(a)anthracene 0.31 %
Chrysene 0.31 I
Benzo(a)pyrene 0.10 %
Other 7.84 %
Total 29.69 %
Acidity
pH
Free carbon (Carbon I)
Ash
Total carbon
Total hydrogen
Total nitrogen
Sulfur
Chloride
Ammonia
Cyanide
Iron
Copper
Manganese
Zinc
Nickel
Cadmium
Lead
Arsenic
Aluminum
Vanadium
Barium
0.62
4.6
<0.01
0.00
90.77
8.12
0.17
0.65
50.0
0.26
0.18
50.3
2.48
2.11
0.13
0.19
0.01
0.5
12.7
22.4
1.6
0.5
mg KOH
standard
0
o
Q
ppm
ppm
ppm
ppm
ppm
ppm
ppm
ppm
ppm
ppm
ppm
ppm
ppm
ppm
SOURCE: Villaume et al., 1983,
238
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289
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Of the volatile organic fractions, only benzene, ethylbenzene, and tolu-
ene were found in the shallow groundwater. No acid fraction organics, most
notably phenol, were found in the shallow groundwater. These materials were
also detected in extremely low levels in the coal tar itself and were attri-
buted by Villaume (1982) to either their original absence or to prolonged
leaching by groundwater. Although the latter interpretation was supported by
the Villaume, our investigation found that the plant operating at the site was
a water-gas plant, which would produce tars with very low levels of tar acids
(phenols, cresols, and xylenols), supporting the hypothesis that these com-
oounds were not initially present in tars.
Elevated levels of certain metals and traces of cyanide were detected in
the shallow groundwater at the site. In sorre of the sampled wells, aluminum,
iron, manganese, and cyanide were detected at levels as high as 218, 460,
25.5, and 0.30 ppm, respectively. By comparison, these contaminants were
measured in the raw tar at levels of 22.4, 50.3, 2.11 and 0.184 ppm, respec-
tively. Sodium also was found in the groundwater at 26.2 ppm, but it was
never analyzed in the tar. Cyanide, probably as either HCN or NH4CN, is a
byproduct of the gas cleanup and was typically removed from an iron salt (see
Chapter 1). The source of the aluminum, on the other hand, is more problema-
tical and, at such high concentrations, is probably present as a precipitated
solid (Hem, 1970). The high sodium levels may be the result of sodium hydrox-
ide usage at the plant. Even higher levels were-found in the aquifers around
the coal-tar distillation plant studied by Hult and Schoenberg (1981), who
attributed them to such a source.
The toxic effects of tar seepage into Brodhead Creek were assessed using
a macroinvertebrate and fish survey, tissue analysis, and in-situ toxicity
testing of caged trout. These analyses revealed no apparent biological accum-
ulation of the tar constituents. Also, tar contaminants were not found in the
mixed stream flow as measured by gas chromatograph/mass spectrographic anal-
ysis.
3.3.4.3 Site Remediation--
In 1981, the State's investigative study recommended the construction of
a slurry trench cutoff wall to contain the coal tar and prevent further migra-
tion into the streambed. Also recommended was the installation of a recovery
290
-------
well system to collect tar wastes for removal. Because of the nature and
extent of contamination, the State applied for and received funds for the |
remedial work under the Superfund program.
The cutoff wall was constructed of a bentonite-cement slurry. The com-
pleted wall is 648-feet long, 1-foot wide, and 17-feet deep. The wall extends
down through the contaminated gravel stratum and 2 feet into the silty sand
layer, which serves as an effective barrier to the coal tar. The upstream end
of the wall is tied into a sheet-piling gate that is part of the existing
flood dike, and the downstream end is tied into an impermeable cement-benton-
ite grout curtain (Adaska and Cavalli, 1984).
Initially, it was estimated that 35,000 gallons of free pumpable tar had
accumulated in the single stratigraphic depression below the old coal gasifi-
cation plant at Stroudsburg. This is tar that has displaced virtually all of
the initial pore water in the gravel. Some tar also occurs above the pure
coal tar in the depression, but it is associated with free water (water not
held by strong capillary pressure forces), which could be picked up during any
pumping operation.
To recover the full tar, a 30-inch gravel-packed well cluster was
installed at the deepest point in the depression. It consists of four 6-inch
wells screened only in the coal-tar layer. In the center is a single 4-inch
monitoring well, which is screened over its entire length. Originally, prod-
uct recovery was accomplished by pumping only the tar at a very slow rate.
Using this method, approximately 100 gallons per day of nearly pure material
were recovered, although this rate decreased drastically over time .as the
volume of tar in the vicinity of the well was depleted.
To increase the efficiency of the coal-tar recovery, the central
monitoring well was modified by the installation of a packer at a depth
between the static groundwater and static tar levels, thus isolating the lower
part of the well. When groundwater is pumped from the uppermost layer, the
resulting pressure reduction combined with the density difference between the
two fluids causes the tar to upwell. If the tar is pumped at the same time as
the overlying groundwater, the tar flows into the recovery well at an
increased rate. Using this setup, a two-fold increase in the recovery rate
291
-------
was achieved. To date, approximately 8,000 gallons of product with less than
1 percent water content has been recovered.
The initial estimate of total free coal-tar contamination at Stroudsburg
is probably too high because it was based on an assumed 30 percent porosity
for the contaminated gravels and on the assumption of complete coal-tar satu-
ration. The majority of this porous material is probably only poorly
saturated. This is evidenced by field observations that could not be
explained at the time they were made, but they are consistent with the capil-
lary pressure model presented by Villaume et al. (1983). Had this been under-
stood earlier, justification for the expense of building the containment wall
may have been questioned.
The amount of tar in the stratigraphic depression below the old gasifica-
tion plant also was overestimated. The overestimation occurred because of
well-screening practices that did not account for the characteristics of the
various coal-tar phases and because these phases are virtually indistinguish-
able in split-spoon samples. Had the estimation been closer to the actual
amount present, the recovery operation may not have been undertaken or may
have been scaled down considerably.
Currently, the pumping operations have been stopped, with a total of
10,000 gallons of tar recovered. The site is still on the National Priority
List (NPL) (ranked at 388), and it is uncertain whether further cleanup action
will be required.
3.3.4.4 New Historical Data on Stroudsburg--
During RTI's historical literature review of the town gas industry, sev-
eral items were uncovered that will result in reevaluations of previously
reported information about the Stroudsburg site. These observations concern
(1) the gas production processes used at the plant, (2) the previously report-
ed method of waste disposal (injection well), (3) the source of the tar con-
tamination, and (4) the nature of tar products from the site.
The Stroudsburg site has always been reported as a coal-gas production
site. Table 56 shows the gas production at the site as compiled from Brown's
Directory, which lists the gas production process as oil and steam (1891 to
1394), Van Syckel oil process (1894 to 1904), and Lowe carbureted water gas
(1912 to 1952). The process specifics for the oil and steam gas production
292
-------
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(and the Van Syckel oil-gas process) were not found during this study, but
processes of this type generally sprayed oil and steam into an externally
heated retort. The oil cracked into lighter gaseous hydrocarbons, and the
steam reacted with carbon to produce CO and H2- The Lowe carbureted water-gas
process is described in Section 1.2.3 of this report. There is no indication
in Brown's that coal carbonization ever occurred at the Stroudsburg site.
Brown's also shows the Stroudsburg plant as operating into the 1950's, with
natural gas being installed sometime between 1952 and 1956. According to
these data, the plant was operated primarily as a carbureted water-gas plant.
It has been reported that an injection well was used to dispose of waste
tars at Stroudsburg. When tar was produced and separated from town gases, it
was usually stored in an underground tank until sold or used. These tanks
were called "tar wells," in that tar was placed into the tanks and pumped out
as if one were removing water from a well. The tar wells were labeled as "tar
well" on plans and maps of the sites. They were also sometimes completely
underground, with only a pipe visible from the surface for removal and filling
of tars from the tar well. Unless the notation on the site map was clearly
labeled as a tar disposal well or an injection well, it is possible that it
was actually a tar storage well.
There are two other possible sources that could have caused the
subsurface tar contamination. Leaks of tar and oils from carbureted water-gas
plants were very common. Underground tar wells (for tar storage) were often
constructed of masonry and leaked. Underground liquid storage tanks were
sometimes constructed of"wood. Tars were frequently placed in the gasholder
for storage (gas sometimes blew around the tar-water seal for the holder,
blowing tar out of the holder and onto the ground). The bottom of the
gasholder was frequently below the groundlevel and also was prone to leaks.
Underground pipes also leaked oil and tar materials into the ground.
The second likely source of the tar contamination is the disposal trench
' described by Lafornara et al. (1982). The tars and emulsions -draining into
: the ground from the trench would flow downward until stopped, and they would
'; have accumulated in the area where the subsurface tars were located. The
f
f amount of tar produced by the plant in 1936 was 15,000 gallons (this is about
[' 10 percent of the gas oil used that year). Thus, finding 10,000 gallons of
295
-------
free tar underground (and maybe 5,000 to 20,000 gallons of tar [this estimate
is a guess) left in the ground] is approximately 1 to 2 years of tar produc-
tion during this period.
The Stroudsburg tar (as described by VilVaume, 1982) is a carbureted
water-gas tar, not a coal tar. It is only slightly more dense than water (P =
1.02 g/cuP), contains very little nitrogen (0.17 percent), has no tar acids,
and has a viscosity of 19 cp (45 8F). Coal tar would be denser (1.1 to 1.2
g/cm^), contain more nitrogen, have some phenols, and be more viscous. The
density of the tar is so close to that of water that it would be very
difficult to separate a tar-water emulsion. Lafornara states that "Treat-
ability studies performed on a coal tar/water emulsion pumped from the back-
water revealed that no cost-effective method could be found to separate the
emulsion and treat the water." This is precisely why the water gas tar was
originally disposed during plant operation. Such an emulsion would frequently
be disposed. The distillation curve (90 percent at 662 °F) shows that the tar
did not contain very much heavier boiling organics, which probably indicates
they were removed in the washbox and not disposed with this tar.
If this tar could have been successfully recovered at the plant, it
either would have been burned or added to the carburetion oils. The water-gas
plant bought large quantities of oil that were poorer carburetion oils than
was the recovered Stroudsburg tar.
3.3.5 Pittsburgh, New York (Thompson et al., 1983)
The coal-gas and carbureted water-gas plant in Plattsburgh, New York, was
in operation from 1896 to 1957. The plant was located on 11 acres of land on
the south bank of the Saranac River. Byproduct tar was disposed in unlined
ponds just above the river. Over several decades, coal tar could be periodic-
ally observed on the south side of the riverbed as globules and as a film
along the riverbank. This case study illustrates the following:
• Site discovery through discharge into an adjacent waterbody
• Coal-tar migration during active disposal by slow downward
movement through subsurface soils along a dense till layer and
from occasional overflow of the ponds during heavy rainfall
296
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• Various influences on contaminant migration including seasonal
groundwater fluctuations causing changes in pore pressure,
increased temperatures during summers causing coal tar to
become more mobile due to decreased surface tension and viscos-
ity, and increased river flow causing a flushing of the contam-
inants from the soil
• Remediation by containing the contaminants onsite (Two con-
tainment structures include cells built of a soil-bentonite
slurry wall keyed into an underlying, low-permeability till
layer and capped with a 36-mil Hypalon liner covered with 15
centimeters of sand, topsoiled, and seeded, and a second
cement-bentonite wall built along the riverfront to prevent
migration of contaminant not contained within the soil-
bentonite cells.)
• Remediation with a groundwater collection system being built to
collect waters draining from the uncontained contaminated site
(These waters will be pumped to water treatment equipment,
treated, and discharged into the Saranac River.)
• Use of the 4 acres of reclaims that lie along the river as part
of the City of Pittsburgh's riverfront park system.
3.3.5.1 Site History—
A coal and carbureted water-gas plant was operated within the city limits
of Pittsburgh, New York, from 1896 to 1957. The New York State Electric and
Gas Corporation (NYSEG) purchased the site and coal gasification plant from
Eastern New York Electric and Gas Corporation in 1929. The plant was located
on 11 acres of land on the south bank of the Saranac River. The topography
falls gently in steps from an approximate elevation of 125 to 130 feet mean
sea level (MSL) along the south edge of the site to 102 to 107 feet MSL along
the Saranac riverbank. Other than a narrow band of trees and bushes adjacent
to the river, most of the site has been cleared and filled. Two structures
that cross the site are a 24-inch diameter concrete sanitary sewer and an
active transmission line (owned by the Plattsburgh Municipal Lighting Dis-
trict) (see Figure 71),
This land consists of two parcels. The larger parcel (approximately 9
acres owned by NYSEG) lies uphill to the south and is the old site of the gas
plant. The smaller parcel (approximately 2 acres) is a long narrow strip of
land that fronts the Saranac River just downhill (to the north) of the NYSEG
gas plant. This parcel was given to the City of Plattsburgh in 1981 by
297
-------
I Reproduced from
[best available copy.
Figure 71. Pittsburgh, New York, general site plan.
Source: Thompson et al., 1983.
298
-------
as a contribution to the city's long-range plan for recreational development
of the Saranac River inside the city.
Table 57 is a list of the gas productions as recorded in Brown's Direc-
tory. This plant produced primarily water gas over its history, although
I notations in 1906, 1924, and 1936 indicated that coal was also carbonized at
: the plant.
t
I Byproduct tar and condensate from the gas production was disposed in
unlined ponds on the NYSEG property just uphill from the Saranac River. No
records of the amount and times of tar disposal into the unlined ponds could
be found. After the plant shut down in 1957, the ponds were filled with ran-
dom material and covered with layers of cinders and ash. Over the years, this
coal tar migrated downhill across the property now owned by the city and into
the Saranac River. This migration occurred via two routes: by slow downward
movement through subsurface soils, and from occasional overflow of the ponds
during periods of heavy rainfall. Tar can be observed periodically on the
south side of the riverbed both as globules of coal tar and as film along the
riverbank. This problem, which has been in existence for some years, has been
attributed to seepage of the tar from the previously existing tar-ponding "
areas on the site.
To address the problem, NYSEG conducted a geotechnical investigation
during the summer of 1979. This fieldwork and laboratory testing, together
with preliminary, alternative strategies for site remediation, were completed
in early 1980. Following review of this work, a supplementary program of soil
boring and testing was undertaken in November 1980. Actual site remediation
occurred between September 1981 and September 1982. Remediation activities
were coordinated with the City of Pittsburgh's long-range plans for recrea-
tional development of the Saranac riverbank, including the parcel given to the
city by NYSEG. Construction plans include building scenic overlooks for fish-
; ing during trout season and a pedestrian bridge to cross the river.
3.3.5.2 Extent of Contamination--
To define the site geology, hydrology, and area of contamination, a total
of 53 boreholes were drilled across the site. In addition to these boreholes,
three test pits were excavated to obtain bulk samples of the tar and soil for
299
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laboratory testing. Nineteen standpipe piezometers were installed to monitor
groundwater levels across the site.
The borings indicated the presence of an extremely dense till underlying
the entire site. This till consist? of silt and fine sand intermixed with
medium- to coarse-grained sand and gravel. The till appears to have served as
a barrier over the years, halting vertical migration of the coal tar on the
site. No tar was observed below this till anywhere on the site.
However, in the sandy soil and fill layers above this till, tar contami-
nation was found over most of the site. In the area or the original tar
ponds, contaminated soils were found as deep as 4 meters.- From this region of
maximum soil contamination, the thickness of the contaminated soil gradually
lessened toward the NYSEG property boundaries except for a layer of contamina-
tion extending across the city's parcel to the north and into the riverbed of
the Saranac River. The data from the borings indicated that the subsurface
movement cf tar from the ponds had been downward through the permeable sands
and gravels and then laterally along the top of the till toward the river. No
tar was observed below the till layer (Thompson et a!., 1983).
A laboratory testing program was undertaken to further characterize the
contamination. Tar content (percent dry weight) in contaminated soils was
found to be as high as 9.6 percent with an average content of 1.5 percent.
Tests to determine total Teachable salts in the soil/coal tar showed low con-
centrations of metals (although Teachable arsenic was reported at 2 and 3 ppm
and lead at 0.9 and 1 ppm in two samples). Determination of total Teachable
salts in tar reported for three samples showed high chemical oxygen demand
(COD) and total organic carbon (TOC) at 850, 900, and 935 ppm. Leachable
phenol was as high as 4 ppm in a tar sample taken from the Saranac River
(Thompson et al., 1983).
The investigations determined that tar migration has decreased exponen-
tially since disposal of tars was halted in 1957. When active disposal was in
progress, the sands, silts, and gravels beneath the ponds became saturated
with tar. The higher viscosity of the tar and its immiscible properties
allowed the tar to migrate in density currents as a separate phase from the
groundwater. With continued disposal, movement of the tar occurred relatively
rapidly downgradient along the top of the till layer into the river. Once the''
302
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tar disposal stopped, the rate of migration gradually decreased. Thompson et
al. (1983) believe that the majority of the tar currently onsite is being
retained within the pores and matrix structure of the soil grains by capillary
forces, and that the mechanism causing the tar migration today is different
from that when the ponds were in operation. Although difficult to quantify,
the mechanism causing tar migration today is most likely influenced by one or
more factors, including seasonal groundwater fluctuations causing changes in
pore-water pressure, increased ground and groundwater temperature during
summer causing the tar to become more mobile due to decreased surface tension
and viscosity, and increased riverflow causing a flushing of the contaminants
from the soil.
3.3.5.3 Site Remediation--
Site remediation occurred in two phases. The Phase I Project focused on
arresting the subsurface migration of coal tar away from the area of the orig-
inal disposal ponds. The Phase II Project addressed the cleanup of the
Saranac River and the city-owned property to the north.
Phase I began in the fall of 1981 with the installation of a soil-benton- 4
ite slurry wall around the main tar pond area (735 feet in perimeter). This
wall was keyed into the underlying impervious till that was 4 to 6 meters
below grade in the main-pond area. This main-pond area was then capped with a
temporary 20-mil polyvinyl chloride (PVC) liner. It was estimated that
approximately 80 percent of the onsite coal tar was encapsulated within this
containment cell. A well was placed within the cell to monitor the effective-
ness of isolation.
Phase II remediation activities began in June 1982 with the installation
of a temporary, portable fabric cofferdam in the Saranac River. Behind this
cofferdam, tar contamination in the riverbed was excavated in the dry. Water
was pumped from the area of excavation into a triple-compartment settlement
tank before being discharged back into the river. Riverbed cleanup was per-
formed in two stages moving from upstream to downstream.
The temporary PVC liner that had been placed as a cap over the previously
constructed containment cell was perforated, and the contaminated material
excavated from the river was placed on top. Additional contaminated materials
were placed in an area just to the southwest of the original containment
303
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Later, this additional area was also surrounded with a soi1-bentonite slurry
wall and thus represented an enlargement (almost a doubling) of the size of
the original containment cell.
After excavation of all visible contamination in the riverbed and along
the riverbank, the riverbed and bank were reestablished to grade with imported
clean fill. To prevent continued migration of remaining uncontained tar into
the riverbed area, a cement-bentonite cutoff wall was constructed through the
clean fill for approximately 213 meters along the riverbank. A cement-
bentonite wall was used in this area (instead of soil-bentonite wall used
previously on the NYSEG property) because a higher strength wall was consider-
ed necessary to meet the city's plans for recreational development of this
area.
To intercept drainage of groundwater from the uphill area above the
cement-bentonite wall paralleling the river, a groundwater collection system
was installed. This system consists of a 15-centimeter perforated drainpipe
0.6 meters below grade and 3 meters upgradient of the cement-bentonite wall.
This drainpipe discharges into a precast manhole at the midpoint of the line.
Water collected by this system is pumped back uphill to water treatment equip-
ment located in the vicinity of the coal-tar containment cell. Treated
groundwater has been discharged into the Saranac River since September 1982.
After grading the contaminated soil in the areas inside the walls of the
containment cells, the cells were permanently capped with a 36-mil Hypalon
liner. This liner was then covered with 15 centimeters of sand, topsoiled,
and seeded. This site work was completed in September 1982.
Because so much tar contamination has simply been contained onsite,
future use of both the NYSEG and City of Plattsburgh parcels will have to be
carefully guarded. Specifically, certain restrictions to onsite development
have been mandated by the NYSDEC, and other restrictions have been suggested
by NYSEG, who will remain responsible for maintaining the slurry walls, con-
tainment cell, groundwater collection and treatment system, and monitoring
network on both parcels. These restrictions are:
• Sale of the lands on which the containment cell was constructed
is prohibited by NYSDEC.
304
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• No structures or other activities that could result in rupture
to the Hypalon membrane may be placed or performed on the con-
tainment cell.
• All trees or shrubs will be maintained at a distance from the
slurry walls such that their mature drip line will not inter-
sect the slurry walls.
• All construction on or near the cement-bentonite partial cutoff
wall and/or groundwater collection system must have prior engi-
neering approval of NYSEG.
3.3.6 Seattle, Washington (Cole, 1972a and b; Cole and Machno, 1971; Drew,
1984; Haag, 1971; Royer, 1984; Mayor's Committee on Gas Works Park,
1984; Orth, 1984; Steinbrueck, 1971)
The Seattle Gas Works plant was in operation for approximately 50 years.
A large portion of the waste byproducts were disposed offsite, but large quan-
tities of lampblack were disposed onsite, building up the shoreline into the
adjacent Lake Union in Seattle, Washington. This case study illustrates the
following:
• Site discovery through redevelopment as a park
• Large stockpiling of lampblack filling in Lake Union
• Conversion of the site into a public park by partial building
demolition, composting of contaminated soils in preparation for
planting, without removal of onsite contaminants
• Closing of park
• Present ongoing investigations to determine whether further
remediation is necessary.
3.3.6.1 Site History—
The GuS Works Park is located on a point projecting into Lake Union in
Seattle, Washington. The park occupies about 20.5 acres, which includes some
1,900 linear feet of waterfront. The surrounding area is mainly industrial
property.
The Lake Union site known as Brown's Point, once a popular spot for pic-
nicking, was developed in 1906 by the Seattle Lighting Company as a gas plant.
The location of the plant on Lake Union made it ideal for the barge delivery
of local and imported coal (and later, oil) for gas production. Eventually,
305
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the site became known as the Gas Company Peninsula, built by a slow process of
filling in Lake Union with cinders, unusable coal and coke, and gas production
wastes. The Seattle Lighting Company became the Seattle Gas Company in 1930
and eventually was made part of the Washington Natural Gas Company (WNG).
The original plant on Lake Union produced illuminating, heating and cook-
ing, and industrial gases for the growing Seattle community. Coke ovens were
operated, and retort gas and carbureted water gas were produced. During the
mid-1930's, six water-gas sets were in operation with a total daily capacity
of 6,600,000 ft3 of gas (Steinbrueck, 1971). The byproducts of the gas plant
operations were ammonia, light oils (benzene, toluene, xylenes), various other
hydrocarbons, and tar, which was refined into creosote. Tar and creosote
produced by the Seattle Gas Company were delivered to the American Tar
Company, which was located adjacent to the Seattle Gas Company until about
1920. The tar company refined the coal tar into various grades of tars and
pitches using steam distillation (Orth, 1984).
In 1937, oil replaced coal carbonization as the basis for gas production.
The plant continued to produce wafer gas.
Table 58 shows the gas production and byproducts from Seattle as compiled
from Brown's Directory. Oil-gas tars contained more asphaltene-type compounds
than did the coal tars produced earlier and were not suitable for the products
derived from the coal tars. Thus, the oil-gas tars were generally used as
fuel for steam production. The tar emulsion from the Jones crackers was over
90 percent water and had to be concentrated before it could be burned.
Naphthalene and related .aromatic oils were collected in the condensation from
this process. The naphthalene was sometimes combined with creosote oils and
sold, but it often was simply dumped offsite (Orth, 1984).
The lampblack from the oil-gas cracking operation was dried for bri-
quetting and used to replace coke in the water-gas sets. However, the bri-
quets would often break during the firing. As a result, thers was consider-
able waste. The lampblack production far exceeded the use, and the excess was
piled next to the lake. The pile of lampblack grew to nearly 100 feet high
and covered several acres (Orth, 1984). There were frequent complaints of
odors from the plant and from the wind dispersal of the lampblack.
306
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The company continued to produce gas until 1956, when a natural gas pipe-
line was extended to Seattle. After that, VING used the site for storage and
other activities. During the plant's operation, the shoreline on the penin-
sula had been extended some 24 meters into Lake Union. Eventually, the site
was almost flat down to the lake's edge where there was a 2.4 meter drop.
In 1962, the City of Seattle purchased the peninsula for development as a
public park. A bond resolution passed in 1968, providing funds for park
development, and planning for the park was initiated. The city hired a land-
scape architect, Mr. Richard Haag, to propose a master plan for the park.
After a study of the site, Haag determined that traditional park development
would be impractical and proposed a controversial plan that allowed for the
restoration and reuse of some of the gasworks structures. The plan for the
site demolition (to be done by WNG in 1971 under the 1962 purchase agreement)
called for leaving six generator towers, the pre-cooler towers, a boiler
house, and an exhauster building. Haag concluded that it would not be pos-
sible to remove all of the underground piping and existing soil from the site,
nor to cover the entire site sufficiently to permit the growth of large trees
essential to a more traditional park design. Despite the controversy over
allowing the former plant structures to remain, the city council finally
approved Haag's plan in 1972. '
3.3.6.2 Extent of the Contamination--
Some 50 years of heavy industrial use at a time when there was little
concern for environmental contamination had left the site on Lake Union heav-
ily contaminated with residues from production, spills, waste materials, and
air pollution fallout.- Haag, the landscape architect, expressed concern for
the ability of the site to support vegetation, noting that there was no "natu-
ral" soil on the site. He described the condition of the soil as a sterile
layer cake of hydrocarbon contamination that supports no vegetation (Haag,
1971). Studies were undertaken by the Seattle Engineering Department and by
Dr. Dale Cole and Peter Machno of the University of Washington to characterize
drainage patterns and soil conditions at the site.
3.3.6.3 Site Remediation—
The description of the remediation activities below is summarized from
information contained in a document made available by the site manager in the
311
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U.S. EPA Regional Office. The document is not commonly available but was
probably prepared in 1984.
After the removal of the above-ground structures by WNG in 1971, consid-
erable site preparation work was still needed. The primary intent was to
stockpile and/or bury onsite much of the excavated material and demolition
rubble. The stockpiling was in the central portion of the site. Portions of
the stockpile were later buried onsite. Several existing structures consid-
ered potential safety hazards were removed. WNG was required to purge certain
pipes in 1973.
The mound area in the southwest portion of the site consisted of excava-
tion materials from offsite. This fill had been brought to the site during
the 1960's and early 1970's. It was thought at one time that this fill mate-
rial could be used to cover the entire site following the demolition of the
above-ground structures. However, the "Great Mound" became a major element of
the master plan for the park, and it was cleared, grassed, and opened to the
public for the purpose of viewing the ongoing park development.
Work contracted by the Parks Department included the following tasks:
• Demolition and burial in the northwest section of the rubble
from 13 concrete purifiers that were located just east of the
tower area
• Removal and stockpiling of the contents of the purifiers (i.e.,
woodchips coated with iron oxide and residue from the purifica-
tion process)
• Removal and burial in the northwest section of the concrete
slab remaining from the 2 million ft3 storage holder
Demolition of remaining concrete foundations and piping
• Excavation and removal or stockpiling onsite of approximately
20,000 to 30,000 yd3 of badly contaminated soils
• Regrading of demolition areas to match the surrounding ground
level.
In the process of removing contaminated material and burying rubble and
debris, there was concern of increased pollution to surrounding areas, partic-
ularly Lake Union. Of particular concern was the excavation of the contami-
nated soil in the southwest area. The contract specifications cautioned the
312
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contractor responsible for this work of the conditions there. The contract
stated, "Excavating oil-gas contaminated material at the southwest property
edge shall be performed with extreme care. This excavation extends to the
lake level and shall commence 30 feet or more inland from the water's edge.
Demolition work and pipe removal shall be completed prior to any excavating of
this 30 foot wide levee. When the inland area Is excavated, filled and/or
graded to the proposed grade the levee at the lake's edge shall be removed."
One part of the site preparation work involved efforts to improve growing
conditions by an application of a compost-like mixture containing dewatered-
sludge cake as the primary ingredient. The mixture was applied over approxi-
mately 10 to 12 acres of the southerly half of the site (about 100 tons per
acre, wet) and then worked into the top 18 to 24 inches by periodic plowing.
Sawdust and leaves were also applied and worked into the surface soil. The
surface was reworked, fertilized, and sown with a cover crop of grass about 2
weeks after the compost treatment. The first crop was plowed under, and the
area was finally rehydroseeded.
The actual park improvements were undertaken upon completion of the site
preparation work. Phase I of the park development consisted of the following
actions:
• Renovation of the former boiler house for use as an indoor/out-
door picnic shelter
• Renovation of the former exhaust building for use as a "Play
Barn"
• Creation of a grassed picnic "Bowl" projecting to the water's
edge
• Construction of paths
• Further development of an existing 170-car parking area
• Deter access to the towers and remove miscellaneous structures
• Regrade mound and hydroseed
• Plant trees and shrubs and provide sod in one small section of
the picnic area.
313
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The work delineated above was completed, and the official park opening
was held during the summer of 1976. Additional improvements were completed in
1978. Plans for further improvements were being finalized when the U.S. EPA
began an investigation of contamination at the site.
Soil testing during the park development was directed primarily at horti-
cultural aspects of the design. The park did not include any significant
amounts of fill. Cuts were made primarily in the southeast quadrant and
between the mound and tower areas. Considerable soil was removed from the
site, part of which was known to contain arsenic. No work was undertaken in
the water areas surrounding the site. According to the Gas Works Park
history:
It appears that the development was directed at reusing the site in
what was felt at the time to be an environmentally sensitive manner.
Both the general design concept and the budget were important i -:-
tors in the decisions that were made. The major controversial
issues centered on the retention and reuse of structures associated
with the former gas plant. Most of the discussion concerning the
levels of pollution centered on what would and would not grow on the
site. Public health was an issue, more in terms of access to the
towers, aquatic activity from the park, and use of the Play Barn,
than in terms of general use of the site (Gas Works Park, no date).
Recognizing the severity of the buried contamination at the gasworks
site, concern was expressed by some members of the community that opening up
the soils of the Gas Company Peninsula could only worsen the potential for
irreversible ecological damage to Lake Union. Notable among those voicing
this concern was Mr. Otto Orth, Jr., a distinguished chemist and lifelong
citizen of Seattle, who in 1984 recounted in a letter to the Seattle Times a
history of the operations at the gasworks (Orth, 1984).
During 1983 and 1984, Environmental Protection Agency and University of
Washington investigators began to sample for toxic materials in offshore
sediments and surface and subsurface soils. Because of the high levels of
polyaromatic hydrocarbons [i.e., benzo(a)pyrene] and other contaminants
reported, Mayor Charles Royer temporarily closed the park on April 21, 1984.
He established a Health Advisory Committee that reopened portions of the park
considered safe for the public. The committee agreed it would be prudent to
conduct additional testing and investigations at the site. Tetratech, a
consulting firm, was hired to carry out soil-sample and groundwater
314
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investigations. A summary of the maximum polyaromatic-hydrocarbon
concentrations found onsite is presented in Table 59. The groundwater
investigation is still in progress.
3.3.7 Brattleboro-Hinsdale Bridge: Brattleboro, Vermont (E. C. Jordan Co.,
__
The Brattleboro, Vermont, site illustrates the following:
• Site discovery during site investigation for a road construc-
tion project
Movement of dense tar components by the action of gravity along
a subsurface bedrock surface, from the original disposal area
to beneath a riverbed
• Movement of tar in a coarse sand and gravel deposit
• Limited groundwater contamination from the wastes
3.3.7.1 Site History--
During initial site explorations associated with constructing a bridge
across the Connecticut River, the State of New Hampshire discovered "odorous,
oily materials" in soil borings. Subsequent analysis indicated that the mate-
rials were similar in composition to coal tars. Further investigation indi-
cated that the site was the location of a town gas facility that was closed
around 1949. One of the original gasworks buildings remains in use as a dis-
tribution center for bottled gas. The planned bridge abutment is to be built
between this building and the river.
No detailed site history has been compiled on this plant. Table 60,
which give the gas production data as compiled by the Radian Corp., shows that
the plant produced carbureted water gas.
Currently, a site contamination audit has been completed, including
recommendations on how to remove and safely dispose of contaminated materials
encountered during construction of the bridge.
i
3.3.7.2 Extent of Contamination--
The initial exploratory borings indicated that there might be tar
<
! contamination at the site, and the site contamination audit confirmed this
1 hypothesis. This investigation showed that the site was underlain by 5 to 15
feet of fill material that grades into alluvium as one proceeds out under the
315
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TABLE 59. MAXIMUM CONTAMINANT LEVELS:
GAS WORKS PARK, SEATTLE, WASHINGTON
Soil
Compound (PPm)
Naphthalene !•&
Acenaphthylene U 1°
Acenaphthene U 20
Fluorene 7.4
Anthracene 10
Phenanthrene 26
Fluoranthene 65
Benzo(a)pyrene 28
Pyrene 10°
Benzo(b)fluoranthene 28
6enzo(a)anthracene 26
Chrysene 33
Benzo(k)fluoranthene 11
Benzo(g,h,i,)perylene 29
Dibenz(a,h)anthracene 3.1
Indeno(l,2,3-c,d)pyrene 25
U = Undetected at the detection limit shown.
316
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TABU 60. GAS PRODUCTION AT BRATTLEBORO, VERMONT
Gas Production
Year process (106 ft3/yr)
1890 Lowe 6
1900 Lowe 5
1910 Lowe 15
1920 Lowe 24
1930 Lowe 41
Lowe = Carbureted water gas.
SOURCE: Radian Corp. from Brown's Directory.
317
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river (Figure 72). Underlying this layer is about 10 feet of sand and gravel
that rest upon weathered bedrock (phyllite) and also extends out under the
river. The bedrock surface slopes downward under the western portion of the
river from about 220 feet above mean sea level (AMSL), to the eastern bank
where the bedrock surface is at about 70 feet AMSL.
Figure 72 illustrates the extent of contamination under the old gasworks
site and under the river, as far as Bridge Pier 1. It also illustrates how
the contaminants have collected in the coarse sand and gravel immediately
overlying the bedrock under the old gasworks building, and it shows that the
contaminants have migrated through this coarse layer, down the bedrock
surface, and under the river to the site of Bridge Pier 1. A borehole to the
east, at the site of Bridge Pier 2, indicates that the coal tar has continued
to migrate along the bedrock surface under the eastern portion of the river,
where it occurs under 45 feet of sediments. This contaminant distribution
clearly illustrates that the tar moved by way of density currents along the
surface of the bedrock. The high permeability of the sand and gravel layer
above the bedrock has enabled this migration to occur. Migration distance is
at least 360 feet laterally and 150 feet deep from the contaminant source.
Maximum contaminant levels for soil, river sediment, and groundwater are
presented in Table 61. Maximum levels in soil were found to the east and to
the west of the gasworks building (B-107, B-108, B-110). Maximum levels in
sediment were found at the site of Pier 1 (BIOS, B106). Maximum groundwater
contaminant levels occurred both onshore (MW-107) and at the Pier 1 site
(B-105, B-106). Sediment contamination levels at the site of Pier 2 were
about five times lower than those presented in Table 61; no PAH's were
detected in the groundwater at this location.
3.3.7.3 Site Remediation--
To address the contamination previously described, the following recom-
mendations were made:
Any contaminated soils excavated during construction of Abut-
ment A or Pier 1 should be removed and disposed in a secure
hazardous waste landfill.
• Suspended soil and visible contamination in water removed from
the above construction areas should be removed. The water may
then be discharged into the river without further treatment; no
318
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••'mi
f
WEST ABUTMENT AREA
morn.! c •>
I
••race wen i
/.WEATHERED
BEDROCK
FINE SANDY SILT
LEGEND
I I O-IOPPM
I . I IO • IOO PPM
I I IOO . PPM
SANOS AND GRAVELS
fVIUIVI ^*^^^ "•' '•
AND I
*"~ PILU I
^^IT"— -.—; -L
-TA^ ""^^
PRORLE' A-A'
rirt*j»e a
Source: E. C. Jordan, Co.. 1984.
BEDROCK (PMVLLITCI
FIGURES
INTERPRETIVE ZONE OF COAL TAR CONTAMINATION
SITE CONTAMNATON AUDIT -CONSTRUCTION PrtOCEXJBeS
BRArOEBOnCHWSOALEBBOOe
NEW IIAMPSltre DEPARTMENT OF PUDUC WORKS AND HOHWAYS
• ECJORDANOar
Figure 72. Brattleboro—Hinsdale Bridge.
319
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TABLE 61. MAXIMUM CONTAMINANT LEVELS: BRATTLEBORO, VERMONT
Compound
Benzene
Toluene
Ethylbenzenc
Xylenes
Naphthalene
Acenaphthylene
Acenaphthene
Fluorene
Anthracene, Phenanthrene
Fluoranthene
Benzo(a)pyrene
Pyrene
Benzof luoranthene(b, k)
Benzo(a)anthracene/Chrysene
Benzo(g,h, i , )perylene
Indeno(l,2,3,-c,d)pyrene
Soil
(ppm)
1.3
4.8
32
64
140
85
140
100
190
64
9.8
43
10
21
2.3
2.2
River
sediment
(ppm)
0.025
--
0.130
0.27
180
1.3
28
22
240
72
4.8
77
4.8
8.5
1.4
i.r
Groundwater
(ppm)
0.15
0.20
0.27
0.79
5.5
0.27
0.84
0.051
H.037
0.0097
0.011
0.0094
0.01
0.0095
—
—
320
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NPDES permit will be required (New Hampshire Water Supply and '
Pollution Control Commission).
• Pilings should be used to support the bridge at Pier 1 to mini-
mize the removal of contaminated material.
• Site safety and contingency plans should be developed to mini-
mize worker and public exposure to contaminated material.
The report concluded that the bridge could be constructed without signi-
ficant environmental or public health impacts and that removal of all contami-
nated materials would not be necessary.
Since the report, the New Hampshire Department of Public Works and High-
ways has decided to use pilings for both Abutment A and Pier 1, thereby avoid-
ing any excavation. However, there is also the possibility of moving the
bridge site upstream (for reasons other than site contamination), thus avoid-
ing the contaminated area entirely. Vermont's Agency of the Environment con-
siders the site to be of low priority because of low potential for release and
contamination of groundwater, surface water, or air.
3.3.8 St. Louis Park, Minnesota (Barr Engineering Co., 1976; Ehrlich et
al., 1982; Harris and Hansel, 1983; Hickok et al., 1982; Hult and
Schoenberg, 1984; May et al., 1978; Minnesota Department of Health,
1938, 1974; Rittman et al., 1980; Schwartz, 1936; Schwarz, 1977;
Sutton and Calder, 1975; U.S. Forest Products Laboratory, 1974)
The Reilly Tar and Chemical Corporation operated a coal-tar distillation
and wood preserving plant (80-acre site) in St. Louis Park, Minnesota, from
1918 to 1972. The plant wastes, consisting of solutions of phenolic compounds
and a water-immiscible mixture of PAH's, were discharged into a network of
L ditches emptying into an adjacent wetland. The contaminants entered under-
: lying aquifers via the wetlands and multiaquifer wells in the area. In 1932,
I the first well was shut down due to contamination, followed by others until
| over 35 percent of St. Louis Park's water supply was shut down. In 1975, the
Minnesota Pollution Control Agency conducted a study to assess the extent and
magnitude of the contamination. Since then, the Reilly site has been desig-
nated as the State of Minnesota's highest priority Superfund site. This case
study illustrates the following:
321
-------
!T
• Site discovery through groundwater contamination
• Contaminant transport via spill of drippings onsite, surface
runoff, plant process-water discharge into adjacent wetlands,
and movement of coal tar directly into bedrock aquifers through
one or more deep wells used to drain creosote from the site and
through one well that had experienced a spill into the well
• Contamination of several aquifers due to other water wells in
the area extending through several aquifers, thereby providing
a pathway for the contamination to travel between aquifers
• Contaminant migration in aquifers influenced by pumpage of
water supply wells
• Removal of phenolic compounds in groundwater by biodegradation
and naphthalene concentrations being reduced due to sorption
• Plan of remediation including a gradient-control well pumping
system, a granular-activated carbon-filtering system, repair of
leaking multiaquifer wells, removal of coal tar from any con-
taminated wells (in particular W23), establishment of source
control wells, and monitoring of all contaminated aquifers over
a set period of time.
3.3.8.1 Site History--
The Reilly Tar and Chemical Corporation operated a coal-tar distillation
and wood preserving plant (80-acre site) in St. Louis Park, Minnesota, from
1918 to 1972 (Figure 73). The plant wastes, consisting of solutions of
phenolic compounds and a water-immiscible PAH mixture, were discharged into a
network of ditches discharging into an adjacent wetland. The contaminants
entered underlying aquifers via the wetlands and a 909-foot deep, plant site
well (W23) (see Figure 73). Well W23 was drilled in 1917 as a source of
cooling water for the plant.
In 1932, the first St. Louis Park village well was drilled 3,500 feet
from the plant. After only several weeks of operation, the well was shut down
because of odors attributed to phenols. An investigation done by McCarthy
Well Company (USGS files) concluded that the contaminants were entering the
groundwater through old wells used to drain creosote from the site. One of
the wells, W23, had experienced a spill of tar into ihe well, leading to con-
tamination of several aquifers. By 1938, the Minnesota Department of Health
(MDH) reported nine wells contaminated with phenolic or tar-like taste. The
322
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Reproduced from
best available copy.
PM9 W1J
WETLANDS
AREA
Source: Ehrlich et al.. 1982.
figure 73. Location of former plant site, wetlands
area, hydrologic section, water table
configurations, and location of key
wells at St. Louis Park, Minnesota.
Generalized potentiometric surface,
June 5, 1979, shown.
323
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well farthest from the plant site was originally 280-feet deep {into the St.
Peter aquifer; Schwartz, 1936). This well was deepened another 130 feet,
extending into the Prairie du Chien-Jordan aquifer, and it immediately yielded
a distinct tar-like taste.
Throughout the 1960's and 1970's, the MDH and St. Louis Park monitored
municipal, commercial, and industrial wells for phenol. In 1975, the Minne-
sota Pollution Control Agency (MPCA) conducted a study to assess the extent
and magnitude of contamination. The study concluded that soil and shallow
unconsolidated sandy aquifers near the old Reilly site were seriously contami-
nated and were the source of contamination to deeper bedrock aquifers. In
1978, PAH's, including benzo(a)pyrene, were found in several St. Louis Park
municipal wells located 1/4 to 1/2 miles north of the site. These wells were
closed down, followed by - re well closures in 1979 and 1981 until over 35
percent of the city's water supply capacity was shut down.
In 1978, a USGS study of private wells in the St. Louis Park area,
including Reilly's deep Well W23, revealed a down-hole flow of contaminated
water from shallow aquifers to the Prairie du Chien-Jerdan aquifer. The flow
was estimated at greater than 150 gallons per minute (gpm). The well was
plugged to stop continuing downward water contamination. In 1982, the MPCA
cleaned out Well W23, removing over 150 feet of coal-tar wastes and debris.
All of the closed municipal wells draw from the Prairie du Chien-Jordan
aquifer, as does 80 percent of the water supply to Minneapolis-St. Paul, of
which St. Louis Park is a suburb. The Reilly site is designated as the State
of Minnesota's highest priority Superfund site.
3.3.8.2 Extent of Contamination--
The vertical strata, including five major aquifers in the area, are shown
in Figure 74. The Platteville Limestone is a nearly flat-lying, dolomite
limestone. Fractures and solution channels contain water that yield small
supplies to wells. The Glenwood Shale underlies the Platteville Limestone and
serves as a confining bed except in locations where the shale has been eroded
away. Glacial drift consisting of glacial till, outwash sand and gravel, lake
deposits, and alluvium of several ages and provenances overlies the Platte-
ville Limestone. The detailed stratigraphy of the drift at St. Louis Park is
complex, but three areally persistent units have been identified. Directly
324
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DEPTH
BELOW
LAMD HYDROGEOLOGIC
SURFACE. UNIT
IN FEET
100-
200-
300-
400-
500-
600-
700-
800-
900-
1000 J
Drift
Piaiteville aquifer
Glenwood ^~
confining bed /
St. Peter
aquifer
Basal St. Peter
confining bed
Prairie du Chien-
Jordan aquifer
S.t. Lawrence-
Franconia
confining bed
Ironton-Galesville
aquifer
Eau Claire
confining bed
Mount Simon-
Hinckley aquifer
*'•*.'.'•'*.''
,*'•.'•• •"•*.
* •
mi
•*.*.•'•'.';."•"•
K:; •':•>
^^^
C^"' ^' —
~^
?PI
^^
Hi
ife
:-:-:-::
•vAv'V'v:'-
GEOPHYSICAL LOGS
Natural . .. Current
Gamma Cahper meter
?
10-inch /
casing \
^*"
7 7 - i n c h
( casing
"""""">• — r—y. Open
_^^ hole
Present (1979)
depth 595 feet
Open-hole
well bore
filled with
coal tar. /
sand, and
(or) other
material
Original (1917)
depth 909 feet
»*•
3
-Water '
'entering
r— ' well here
—Waler
leaving
well here
L
» 4
i — r~r~' — r~> — i f
6 10 14 18 C
Well Vc
diameter, i
in inches pe
/Water level
in welt
Direction
L^.^ lof flow
Note: Flow was
measured before
installation
of t emporary
packer
1 ' I > ' i
60120
ilocity,
i feet
r minute
Figure 74. Hydrogeologic and geophysical logs of Well W23 ("Hinckley" well on the site).
Source: Hult and Schoenberg. 1984.
325
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overlying the Platteville Limestone are (1) a unit of till, outwash, valley-
fill deposits, and deeply weathered bedrock; (2) a middle unit of glacial sand
and gravel called the Middle Drift aquifer; and (3) an uppermost unit of lake
deposits and till. Below the Glenwood confining bed lies the St. Peter
aquifer, the Basal St. Peter confining bed, the Prairie du Chien-Jordan
aquifer, the St. Lawrence-Franconia confining bed, the Ironton-Galesville
aquifer, the Eau Claire confining bed, and the Mount Simon-Hinckley aquifer.
The movement of the groundwater and, consequently, contaminants over the
50 years of plant operation has most probably varied with time because of a
number of factors. A major control in groundwater movement is the draw-down
created by water demand in communities as they have grown and diminished in
population. The continuity of confining beds plays an important role in that
a conduit for water and contaminant exchange between aquifers occurs where
confining beds have been eroded. The presence of glacial valleys filled with
coarse-grained deposits may provide preferential pathways for movement of
groundwater or contaminants. Also, multiaquifer wells (wells hydraulically
connecting two or more aquifers) provide an avenue of transport for contami-
nants and water, and they can locally change potentiometric surfaces of con-
necting aquifers. Multiaquifer wells result from original open-hole construc-
tion, leaks in casing, or flow in annular space between casing and borehole.
In the St. Louis Park area, Hult and Schoenberg (1984) found that the water
level in each aquifer is higher than the level in the underlying aquifers,
causing water flow through multiaquifer wells to be downward.
The major contaminant from the Reilly plant was creosote, a complex mix-
ture of chemical compounds. Typically, creosote contains 85 percent PAH
[i.e., naphthalene, anthracene, phenanthrene; some of which are carcinogenic
(at least 12 have been identified as carcinogenic, U.S. EPA, 1980a)] and 2 to
17 percent phenolics (i.e., phenol, methylated phenols). The remaining con-
tents consist of various nitrogen- and sulfur-containing heterocyclic com-
pounds (U.S. Forest Products Laboratory, 1974).
In addition to creosote, the Reilly plant discharged approximately 80,000
gallons of 70 percent NaOH into ponds from 1940 to 1943, as well as some sul-
furic acids. [For more detail, see Table 4 in Hult and Schoenberg (1984).]
326
-------
The distinction between transport processes of most natural constituents
of groundwater and transport of coal tar is that many compounds of coal tar
are relatively insoluble (Sutton and Calder, 1975; Schwarz, 1977). PAH's tend
to adsorb strongly to soil particles and have low aqueous solubilities (Hickok
et al., 1982). Phenolic compounds are generally more soluble in water than
PAH's. The solubility of phenol is more than 10 g/L at 25 °C and pH 7.0,
while the solubility of naphthalene under the same conditions is only 0.032
g/L (May et al., 1978). Solubility behavior of hydrocarbons is poorly under-
stood. In Hult and Schoenberg (1984), dissolved constituents are defined as
those not removed by filtration through a 0.45-micrometer filter. Many coal-
tar derivatives are non-ionic and may exist as microscopic aggregates of
individual monomers known as micelles. Micelles are considered part of the
aqueous phase, and their movement is controlled by critical pore size.
Micelles may move as though they were ideal solutes or become trapped, forming
a hydrocarbon fluid phase at some distance from the source. This complicates
contaminant movement and explains the wide variation of contaminant concen-
tration throughout the area.
When creosote is mixed with water, two phases generally emerge: a light-
er aqueous phase enriched in phenolics and a more dense hydrocarbon phase
enriched in PAH's. Because the second phase has different properties (i.e.,
density and viscosity) from the aqueous phase, the hydrocarbons may move at a
different rate and in a different direction than does the groundwater. At St.
Louis Park, the dense hydrocarbon phase has percolated downward relative to
the direction of groundwater flow, allowing contaminants to dissolve in the
flowing groundwater and to be transported downgradient. The major transport
mechanism is in the aqueous phase, whether as solutes or as micelles (Hult and
Schoenberg, 1984).
There are three major paths for contaminant transport. The first is by
spill or drippings onsite, which infiltrated and percolated through the unsat-
urated zone to the water table. This has resulted in extensive contamination
of the unsaturated zone on the 80-acre Reilly site. The contaminants reaching
the groundwater vary in composition from area to area because the coal tar
used throughout the plant's operation came from different suppliers and
327
-------
subaereal decomposition of the coal-far constituents produced degradation
products dissimilar to those produced in the saturated zone.
The second path for contaminant transport is surface runoff and plant
process-water discharge to depressions and wetlands found south of the plant
site. Natural surface drainage was toward the site and south to Minnehaha
Creek. Since approximately 1938, the drainage has been disrupted by roads and
other manmade structures. Therefore, surface runoff and plant process-water
were discharged through ditches and culverts to water table ponds near Well
W13 (see Figure 73). If the rate of discharge becomes greater than the rate
of evaporation, mounding in the water table occurs and vertical movement of
the contaminated water and hydrocarbon-fluid phase into the underlying,
confined drift aquifers occurs. Visible contamination extends at least 50
feet below the water table south of the plant site near Well W13 (Minnesota
Department of Health, 1974; Barr Engineering Co., 1976). Since approximately
1938, surface water inflow to the ponds recharged to underlying peat and the
Middle Drift aquifer. Inflow included 30 to 60 gpm of wastewater (Minnesota
Department of Health, 1938) and as much as several hundred gpm of runoff
during peak periods, increasing the vertical leakage. Also included in the
plant discharge were sodium hydroxide and sulfun'c acid occasionally used in
plant processing.
The third path for contaminant transport is movement of coal tar directly
into bedrock aquifers through one or more deep wells onsite. The main pathway
is through the 909-foot deep Well W23, drilled in 1917. At some time, a coal-
tar spill into this well occurred and is probably the source of early contami-
nation reported in the Prairie du Chien-Jordan aquifer. The well was tempo-
rarily plugged and is now 595-feet deep. An unsuccessful removal of the vis-
cous material was attempted in 1958.
3.3.8.3 Site Remediation--
In 1980, the available data were studied to assess the feasibility of
(1) controlling movement of contaminated groundwater by pumping wells,
(2) excavating or otherwise remedying contaminated soils, and (3) treating and
disposing the residual waste products. A system of 12 to 15 wells in 5 to 6
aquifers was designed to flush the groundwater system. Hickok et al. (1982)
estimated that the contaminated areas could be flushed in a few decades with
328
-------
minimal sorption effects. However, leakage from the overlying drift, and
especially from the "source zone," could continue to cause significant contam-
ination of the bedrock aquifers for thousands of years, even with gradient
control wells.
Ideally, management of the "source zone" would include excavating the
highly contaminated surficial peat, removing the associated fluid, and pumping
out the body of hydrocarbon fluid generally underlying the peat in the Middle
Drift aquifer. Hickok et al. (1982) surmised that, at the time of their
study, too little information on the actual contaminant distribution was
available to design a complete remedial program for the "source zone."
As far as disposal of the "source" material, Hickok et al . (1982) con-
cluded that the hydrocarbon fluid could not feasibly be treated for discharge
to the Mississippi River or other surface waters. They concluded disposal
would probably entail transport by truck or rail tank car to a secure land-
fill, a reprocessing plant, or another option depending on the total volume of
hydrocarbon fluid. The disposal of the peat-associated fluid probably would
be similar.
In a subsequent study, Harris and Hansel (1983) completed an evaluation
of groundwater treatment and potable water supply alternatives for the City of
St. Louis Park. As part of this study were bench-scale tests conducted to
determine the efficiency of various water-treatment technologies in removing
PAH's and other coal-tar derivatives from groundwater. Of all the technol-
ogies tested, only tr-ee were shown to be effective in removing PAH compounds
to below the treatment goal of 280 ng/L total "other" PAH compounds. These
three technologies were: granular-activated carbon (GAC) , ozone/ultraviolet
(03/UV), and hydrogen peroxide/ultraviolet (H202/UV). At raw-water concentra-
tions of about 7,000 ng/L, GAC appears to be the most cost-effective, and a
GAC pilot plant was set up and successfully operated in the pump station at
one of St. Louis Park's contaminated wells. These three technologies achieved
compliance with project-specific treatment goals and provided effluent water
quality adequate for use in a potable water distribution system.
Phenolic compounds and naphthalene are disappearing downgradient from
source points (i.e., Wells W13 and W23) faster than expected if only dilution
were occurring. A study by Ehrlich et al. (1982) concludes that phenolic
329
-------
compounds in groundwater are being converted to methane and carbon dioxide by
anaerobic bacteria. Naphthalene also shows an attenuation in concentration,
but this appears to be due to sorption rather than biodegradation. Ehrlich et
al. (1982) believe that the contaminated drift is acting as a treatment zone
for removal of phenolic compounds that have penetrated the aquifer. They
characterize this zone as a continuous flow bioreactor consisting of a fixed-
film microbial population fed by a multiple nutrient stream as envisioned by
Rittmann et al. (1980).
To date, a portion of the surface contamination has been removed and
infilled with clean topsoil. The State of Minnesota is planning to build a
highway interchange that would cover an area of contamination that has not yet
been removed. If the State builds the interchange, the construction plans
will include removal of the contaminated soils. If the interchange is not
built, the Reilly Tar and Chemical Corporation is responsible for this surface
contamination removal.
Upon approval by all parties involved, a remedial action plan will go
into effect. The plan includes a gradient-control well pumping system, a GAC
filtering system, repair of leaking multiaquifer wells, removal of coal tar
from any contaminated wells (in particular W23), establishment of source
control wells, and monitoring of all contaminated aquifers over a set period
of time. The entire remedial action plan has not been completed and is still
being drafted. The Minnesota Pollution Control Agency is coordinating the
remedial action planning.
3.3.9 Pensacola, Florida (Ehrlich et al., 1982; Franks et al., 1985;
Mattraw and Franks, 1984; McCarty et al., 1984; Troutman et al.,
1984; Wilson and McNabb, 1983)
American Creosote Works Inc., an abandoned wood-treatment plant near
Pensacola, Florida, was chosen by the U.S. Geological Survey in 1983 as a
field laboratory to study the transport and environmental fate of creosote
constituents in groundwater and surface water. Also, the site was chosen as
being appropriate to apply the latest techniques for characterizing hazardous
waste problems. To quote the National Priority List (NPL) description:
The American Creosote Works, Inc., Site covers 1.5 acres in Pensa-
cola, Florida, about 0.3 miles north of where Bayou Chico and Pensa-
cola Bay meet. The facility treated wood with creosote and penta-
330
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chlorophenol (PCP) from the early 1900s to late 1981 or early 1982.
PCP-contaminated waste water was discharged into two ur.lined 80,000-
gallon percolation ponds. In February, 1981, the U.S. Geological
Survey identified phenols in ground water associated with American
Creosote Works. At present, no drinking supply wells are within the
known zone of contamination.
This case study illustrates the following:
• Contamination of a sand-and-gravel aquifer from direct contact
with creosote waste
• Insignificant attention of contaminants through sorption onto
aquifer materials
• Anaerobic degradation of phenolic compounds in the groundwater
environment
• Degradation of quinative to 2-quinolinone in groundwater by
microbial oxidation
• Utilization of novel onsite groundwater sampling and analysis
method to map the extent of microbes responsible for contami-
nant degradation, and by reference, the extent of contamination
(Report is a selective summary of the USGS findings and is
entirely based on the three referenced documents)
3.3.9.1 Site History--
The wood-treatment facility located within Pensacola, Florida, had been
in operation from 1902 to 1981. Over this time, wood-preserving chemicals
were discharged into two, unlined surface impoundments. Prior to dewatering
and capping in 1982, the impoundment wastewaterb were in direct hydraulic
contact with an underlying sand-and-gravel aquifer. The aquifer was up to
about 300-feet thick and~consisted of deltaic, fine-to-coarse quartz sand
deposits interbedded with locally confining, discontinuous clays and silts
(Troutman et al., 1984). The impoundment wastes, in general, consisted of the
wood preservative creosote, a coal-tar derivative. In addition to creosote,
diesel fuel and pentachlorophenol (PCP) were discharged to the surface waste
impoundments.
3.3.9.2 Methods of Investigation--
3.3.9.2.1 Soils and qroundwater samplinq--Nine test borings were drilled
in 1981 to investigate the hydrostratigraphy beneath the site and to survey
331
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groundwater quality close to the facility. Borings were later (1983)
completed and developed as groundwater monitoring wells. At each boring site,
a well cluster of two to five wells was constructed with each well set at dif-
ferent depths. Details of well construction and materials, sampling proto-
cols, and the results of groundwater sampling for creosote constituents and
PCP's are given in Troutman et al. (1984) and Mattraw and Franks (1984).
3.3.9.2.2 Microbiological investigations--The aerobic degradation of
quinoline in soils derived from the site was evaluated by standard laboratory
batch techniques. The anaerobic degradation of phenolic compounds was also
studied using enriched bacterial cultures from contaminated groundwaters at
the facility (Mattraw and Franks, 1984).
3.3.9.2.3 Experimental/innovative investigative techniques--The research
site was used to test the practicability of several experimental,
nonconventional groundwater sampling methods:.
• A multilevel "bundle" piezometer for sampling groundwater and
measuring hydraulic heads at discrete vertical intervals within
an aquifer (Mattraw and Franks, 1984)
• A reconnaisance groundwater sampling method, whereby ground-
water within the hollow-stem auger is sampled and analyzed by
an onsite high-performance liquid chromatograph (HPLC) for
dissolved methane (Troutman et al., 1984; Franks et al., 1985).
3.3.9.3 Extent of Contamination Findings—
r Results of the 1983 groundwater analyses by gas chromatography/mass spec-
it
troscopy (GC/MS) indicate the presence of approximately 80 organic contami-
nants in groundwaters p?ar r.he facility. For classification purposes, three
compound groups were iaentified: phenols (up to 2 ppm); PAH's (up to 2 ppm);
; and heterocyclic compounds containing oxygen, nitrogen, or sulfur (up to 1.5
; ppm). Based on these general groupings, two contaminant zones were observed
I at the waste site:
:: • A highly contaminated water-table aquifer plume to approxi-
' ; mately 36 feet depth
i
• A relatively less contaminated, confined, or semiconfined
aquifer plume extending to a maximum depth of 75 feet.
332
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Questions concerning the transport of pure creosote within the unsatu-
rated zone and within the aquifer were not directly addressed in any report.
However, pools of denser-than-water, black, oily material were reported to be ™
seeping from a stream approximately 450 feet downgradient of the waste
impoundment (Mattraw and Franks, 1984).
PCP was not observed to be present in groundwater downgradient of the
waste site at concentrations greater than 0.01 ppm.
Vertical distributions of contaminants at well clusters near the impound-
ments and approximately 450 feet downgradient show that contaminants have, in
general, moved en masse (though in a dissolved state) with little or no
"chromatographic separation" of compounds because of their differential reten-
tion on the aquifer media. Based on these observations, the reports conclude
that retardation of organics because of sorption on aquifer materials and soil
organic matter provides little or no control of contaminant transport at the
site. This is not surprising considering that aquifer materials are predomi-
nantly clean sands, with minimal clays and organic matter.
Individual contaminants such as phenols do, however, decrease in concen-
tration downgradient, presumably because of microbial degradations. Phenol
biodegradation under anaerobic aquifer conditions is well established (Ehrlich M
et al.f 1982; Wilson and McNabb, 1983; McCarty et al., 1984), and results at
the Pensacola creosote site replicate these findings specifically. Godsy and
Goerlitz (Mattraw and Franks, 1984, pp. 77-84), found a sequential disappear-
ance of C-* through C^ carboxylic acids, phenol and benzoic acid, 3- and
4-methyl phenol , and 2-methylphenol "during downgradient movement within the
aquifer." In laboratory digesters containing enriched bacterial cultures from
contaminated groundwaters at the site, the same sequential disappearance was
observed with concomitant methane and carbon dioxide production.
The extent of the dissolved methane plume, and thus the extent of
methane-generating bacteria and their degradation products, was later
addressed in 1985 using an innovative drill-stem groundwater sampling techni-
que and an onsite HPLC analysis (Franks et al . , 1985). These findings indi-
cate a much wider distribution of methane in the aquifer and that some of the
byproducts of microbial degradation may have migrated farther in the aquifer
than did the more readily degraded organic contaminants. Thus, selected
333
-------
contaminant plumes may extend well beyond the trace of the specific target (or
"indicator") compounds (e.g., total phenols) if lower molecular weight organic
and inorganic byproducts of the target compounds are considered.
No evidence was presented for the anaerobic microbial degradation of
PAH's or heterocyclics, nor were any studies undertaken to examine the aerobic
microbial degradation of any compound except quinoline. In one study by
Bennett et al. (Mattraw and Franks, 1984, pp. 33-42), groundwater samples were
collected and found to contain appreciable amounts of 2-quinolinone, a princi-
pal aerobic degradation product of quinoline. Subsequent soil samples and
surface water and groundwater samples were found to contain large numbers of
aerobic bacteria that convert quinoline to 2-quinolinone. These organisms
were identified and counted.
3.3.9.4 Site Remediation (as of July 1983)--
According to the NPL description:
In March, 1982, American Creosote sold all the equipment onsite and
later filed for bankruptcy under Chapter 11 of the Federal Bank-
ruptcy Act. The state has negotiated a Consent Order requiring
American Creosote to restore the discharge areas and install onsite
monitoring wells. The company constructed higher berms around the
ponds to prevent overflow during heavy rainfall.
EPA recently completed a remedial plan outlining the investigations
needed to determine the full extent of cleanup required at the site.
EPA plans to fund (1) a $290,000 remedial investigation/feasibility
study to determine the type and extent of contamination at the site
and identify alternatives for remedial action and (2) an $85,000
initial remedial measure involving fencing the site, posting warning
signs, reconstructing the berms, and controlling flooding from the
waste ponds. The work is scheduled to start in the third quarter of
1986.
3.4 CONCLUSIONS
Each of the gas sites visited showed surface contamination by tars, ash,
and other wastes associated with gas manufacture. The amount of visible con-
tamination varied from site to site, but it appeared more widespread at the
larger sites.
Blue ferrocyanide contamination was visible at the Mendon Road, Taunton,
and Pawtucket sites. Each of these sites was known to produce gas by coal
carbonization. Spent oxides were discovered at the Spencer and Richmond
334
-------
plants. This spent oxide showed signs of sulfur and iron, but no ferro-
cyanides. Both of these were principally water-gas plants.
Some oil contamination of the water in the Pawtucket canal (in Lowell,
Massachusetts) was visible. This contamination was from the general direction
of the gas plant. No other oil contamination of surface waters was seen at
the other former gas sites.
Substantial gas odors were noted at the Lowell, Richmond, Taunton, Paw-
tucket, and Mendon Road sites. The odors indicate that contamination may be
substantial at these sites. Only slight odors were noted at the Spencer and
Worchester sites. The plant at Spencer was very small, and the Worchester
site was capped with construction refuse and soil.
The case studies indicate that sites are "discovered" when (1) surface
water is contaminated, (2) construction activities disturb the site or ground
around the site, (3) redevelopment of the site is attempted, or (4) municipal
groundwater sources are contaminated.
Phenol and PAH compounds appear to degrade in the groundwater when they
are present in dilute concentrations. In raw tars, however, the microorgan-
isms cannot survive, and the tar components do not degrade. This means that
tars can remain substantially unchanged over time.
Tars (heavier than water) sink within groundwater systems until stopped
by low permeability strata. Oils can float and spread on the surface of
groundwater, contaminating a band of soil and thereby serving as a source of
contamination to underlying groundwater. Cases of significant groundwater
contamination usually can be attributed to the lighter, more soluble aromatics
found in oiIs.
Local pumping of groundwater wells can affect the flow and transport of
tars and contaminated water. Controlled pumping can be used to limit the
spread of groundwater contamination.
Much of the historical data reported about the Stroudsburg site appears
to be incorrect. The "coal tar" at Stroudsburg actually appears to be a tar
from the production of carbureted water gas. The density of the tar is very
close to water, which later separated. The low carbon content and absence of
high-boiling organics imply that the tar was condensed after the washbox
removed the higher boiling organics. The lack of phenols and the low
335
-------
•
content of this tar identify it as a water-gas tar. The existence of an
injection well for tar disposal also has been questioned because the term "tar
well" was frequently used to describe underground tar storage tanks.
None of the case studies examined a plant that produced gas only by coal
carbonization. Possible explanations for this include the fact that the coal
carbonization plants produce tars that are not as prone to tar migration, 1t
may only indicate the widespread adoption of the carbureted water-gas process,
or coincidence. Coal carbonization tars were generally more dense and more
viscous than carbureted water-gas and oil-gas tars.
Tar viscosity decreases with temperature, and surface tars generally
become more mobile during the summer months.
The principal remediation employed at town gas sites is containment.
Slurry walls, caps, and collection wells have been used.
Site contamination differs with the processes employed for gas manufac-
ture. The principal contamination at the Seattle plant was lampblack, which
was produced in substantial amounts by oil-gas production. At carbureted
water-gas plants, the principal contaminant of concern was relatively M,ob1le
tar.
The waste disposal practices at the sites examined were generally quite
poor. Although tars were frequently recovered, the liquids that disposed were
either placed into the nearest body of water or, if they could not be disposed
into water, placed into lagoons, trenches, or allowed to flow across the soil
until absorbed. Solid wastes either were used to fill in areas along the
shoreline or piled in a dump beside the plant.
336
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4,0 STATE STATUS CF MANUFACTURED-GAS SITES
4.1 INTRODUCTION
This portion of the project was undertaken to determine the current sta-
tus of manufactured-gas sites on a national basis. Originally, this determi-
nation was to be made by comparing the Radian list of manufactured-gas sites
(compiled from Brown's Directory of American Gas Companies) to the national
Comprehensive Environmental Response, Compensation, and Liability Act (CERCLA)
CERCLIS list of sites (reported to EPA by the individual States). Such a com-
parison would have produced a list of manufactured-gas sites that Individual
States viewed as sufficiently hazardous for inclusion in CERCLIS. The
resulting list could then be used to assist in planning further EPA efforts in
the area.
The organization and nature of the information on the two lists prevented
approaching the problem as planned, and an alternative approach was used to
determine the status of manufactured-gas sites within States. Each EPA region
was contacted to identify which States had placed manufactured-gas sites on
CERCLIS and to determine what the status of the sites was. For most regions,
the persons responsible for placing State sites on CERCLIS within individual
States had to be consulted. Section 4.2 explains why the originally planned
list comparison was impractical, and Section 4.3 describes the information
acquired on the status of gas sites within States. Section 4.4 discusses the
Radian list of manufactured-gas sites.
4.2 COMPARISON OF THE RADIAN LIST AND CERCLIS
The original task of comparing the Radian list and CERCLIS of manu-
factured-gas sites proved infeasible because the data included in each were
incompatible. Figure 75 illustrates the type of data contained in the Radian
list of town gas manufacturing sites. These data were compiled from Brown's
Directory at 10-year intervals between 1890 and 1950. The information
337
-------
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338
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reported Includes the city where the plant was located, company name, plant
status, production, and byproducts. The only information recorded on plant
location is the city name where the plant was situated. Figure 76 provides
data from CERCLIS. These data indicate the EPA identification number, site
name, address, county, latitude, and longitude for each site. The list
includes no information on the type of contamination at the sites or on any
operations at the site resulting in contamination. The site name of sites on
CERCLIS can be used to determine if listed sites were former manufactured-gas
sites, but only when the site is listed specifically as a gas plant or as
owned by a gas company. Many of the sites in the list have names that do not
indicate anything about the source of site contamination. Thus, merely
compiling a list of the sites with site names that indicate they might be
manufactured-gas sites would produce many omissions and inaccuracies.
The only basis that could be used to compare the Radian list and CERCLIS
would be to compare the cities on each list and produce a list of CERCLIS
sites in cities that also had manufactured-gas sites. Table 62 shows the
number of sites resulting from this approach for the State of Alabama. There *
were 164 CERCLIS sites in cities that had manufactured-gas sites in the Radian
list. The inability to match Radian and CERCLIS sites within cities made this
type of comparison essentially worthless, so an alternative approach had to be
found to examine the status of manufactured-gas sites in the States.
4.3 EXAMINATION OF MANUFACTURED-GAS SITE STATUS IN STATES
As an alternative, individual EPA regions and States were contacted to
collect information on "manufactured-gas sites within States. Table 63 lists
the results of the inquiries and the current status of sites within each
State. The information was collected from employees of either the EPA or
State agencies who were "in a position to know" the status of CERCLIS waste
sites within their areas. Consequently, the absence of known gas-manu-
facturing sites on CERCLIS may either indicate that there are actually none on
the list for that State, or merely that the individuals contacted were not
aware of any.
Table 63 summarizes the information collected from regions and States on
the status of manufactured-gas sites. Tables 63 through 72 list the sites ^
339
-------
L.I - SITE LOCATION LISTING
06/07/1985
EPA 10 SITE NAME
STREET
CITT COUNTY CODE
COUNTY NAME ZIP CODE LATITUDE LONGITUDE SMSA HTORO UNIT
PHATTVILLE
AUGUSTA
001
AL0980710370 CALLAHAN PROPERTY
MHY 82 ROUTE 4 BOX 2
66
PRATTVILLE 001
AUTAUGA
36067
36067
322748.0 862830.0 5240
322748.0 862830.0 5240
AL09S0556245 SOUTHERN RAILWAY DERAILMENT SITE
HP 178.9
FREEHONT 001
AUTAUGA 36784
315442.0 674424.0
ALOOOS557004 UNIOII CAflP COSP MONTGOMERY MILL SITE
JENSEN RO
PRATTVILLE C01
AUTAUGA
36067
ALD980495667 BALDWIN COUNTY LANDFILL
PO BOX 150
BAY NINETTE 003
BALDWIN 36507
ALD980495709 BAY MINETTE CITY DUMP
M 7TH ST
BAY HINETTE 003
BALDWIN 36507
ALD940727929 BOLON PROPERTY
RABUH RO
BAY fllNETTE 003
BALDWIN 36507
AL0980727747 BRANTLEY E R
NEWPORT PARKWAY
BAY HINETTE 003
BALDWIN 36507
ALD000652941 051 TRANSPORTS INC
HWY 47 N
BAY HINNETTE 003
BALDWIN 36507
AL0001874254 KAISER ALUMINUM 1 CHEMICAL CORP
HWY 31 S
BAY niHETTE 003
L4RPT1 - PREPARED BY OPfl
305300.0 874624.0 5160
305300.0 874624.0 5160
3150201
3150201
3150203
322520.0 862820.0 5240 3150201
305300.0 874624.0 5160 3140106
3CSJOO.O 874624.0 5160 3140106
3140106
305300.0 874624.0 5160 3140106
3140106
Figure 76. CERCLIS waste sites.
340
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r
TABLE 62. COMPARISON OF RADIAN TOWN GAS SITES TO
CERCLIS FOR ALABAMA
County
Barbour
Calhoun
Colbert
Dallas
Etowah
Jefferson
Jefferson
Lauderdale
Madison
Mobile
Montgomery
Morgan
Talladega
Tuscaloosa
City
Eufaula
Ann is ton
Sheffield
Selma
Gasden
Bessemer
Birmingham
Florence
Huntsville
Mobile
Montgomery
Decatur
Talladega
Tuscaloosa
Number of CERCLA
sites in city
1
13
6
10
6
5
34
4
16
29
18
14
1
7
Total 164
341
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TABLE.' t.«.
P,V.
Site
G i 1 ro y
Hollister
Monterey
Sal inas
San Luis Obispo
Santa Cruz
Watsonvf lie
Bakersfield
Chi co
Chico
Coalinga
Colusa
Fowler
Fresno
Fresno
Grass Valley
Grass Valley
Lodi
Madera
Marysville
Marys vi lie
Merced
Modesto
Nevada City
Oakdale
Orovi 1 le
Red Bluff
Redding
Sacramento
:.A\ SITES IN
ciC GAS AND
No.
408-1
418-9
418-1
418-2
418-4
408-7
408-8
335-1
210-1
210-1A
325-8
212-1
325-2
325-3
325-3A
215-1
215-1A
316-6
325-4
212-2
212-2A
325-5
316-2
215-3
316-3
212-3
213-1
213-2
206-2
CALIFORNIA COMPILED BY
ELECTRIC COMPANY
County
Santa Clara
San Bern" to
Monterey
Monterey
San Luis Obispo
Santa Cruz
Santa Cruz
Kern
Butte
Butte
Fresno
Colusa
Fresno
Fresno
Fresno
Nevada
Nevada
San Joaquin
Madera
Yuba
Yuba
Merced
Stanislaus
Nevada
Stanislaus
Butte
Tehena
Shasta
Sacramento
(continued)
346
-------
TABLE 64 (continued)
Site
Sacramento
Selna
Stockton
Tracy
Turlock
Wi 1 lows
Woodland
Eureka
Eureka
Eureka
Santa Rosa
Santa Rosa
Okiah
Benicia
Daly City
Livermore
Los Gatos
Napa
Napa
Oakland
Oakland
Petaluma
Pittsburg
Redwood City
San Francisco
San Francisco
San Francisco
San Francisco
San Francisco
San Francisco
No.
206-2A
325-6
316-4
316-7
316-5
210-2
206-3
119-1
119-1A
119-18
104-6
104-6A
104-B
104-1
508-2
601-1
408-3
104-3
104-3A
601-2
601-2A
104-4
601-3
508-1
502-1
502-1A
502-1B
502-1C
502-10
502-1E
County
Sacramento
Fresno
San Joaquin
San Joaquin
Stanislaus
Glenn
Yolo
Humboldt
Humboldt
Humboldt
Sonoma
Sonoma
Mendocino
Solano
San Mateo
Alameda
Santa Clara
Napa
Napa
Alameda
Alameda
Sonoma
Contra Costa
San Mateo
San Francisco
San Francisco
San Francisco
San Francisco
San Francisco
San Francisco
(continued)
347
-------
TABLE 64 (continued)
Site
San Francisco
San Francisco
San Francisco
San Francisco
San Francisco
San Fruncisco
San Jose
San Jose
San Leandro
San Rafael
San Rafael
Santa Clara
St. Helena
Vallejo
Vallejo
No.
502-1F
502-1G
502-1H
502-11
502-1J
502-1K
408-5
408-5A
601-4
104-5
104-5A
408-6
104-7
104-9
104-9A
County
San Francisco
San Francisco
San Francisco
San Francisco
San Francisco
San Francisco
Santa Clara
Santa Clara
Alameda
Mar in
Mar in
Santa Clara
Napa
Solano
Solano
348
-------
TABLE 65. DELAWARE GAS SITES
Dover Gas Light (DES7)
Wilmington Coal Gas Co.
Coal Gas Holder Site
New Castle Gas Co.
Smyrna Gas-Coke Co.
Georgetown Gas Co.
Lewes Gas Co.
Sussex Gas Co.
349
-------
. TABLE 66. FLORIDA GAS SITES
Location
Walkover
Inspec-
tion
(PCAP)<
Comments
PER District Office
NW District
Pensacola (Municipal) Yes
Tallahassee (Municipal) Yes
NE District
Jacksonville (Peoples/ Yes
Container Corp.)
Gainesville (Gainesville No
Gas Co./Poole Roofing
Co.)
No
No
Yes
No
No visible problem.
No visible problem; known as
Cascades Park.
Coal tar present onsite,
CAP'S being prepared.
Palatka (Municipal)
St. Augustine (Municipal)
SW District
Tampa (Peoples)
Lakeland (Peoples)
St. Petersburg (Peoples;
site owned by City)
Bradenton (Southern Co.)
Clearwater (Municipal)
Winter Haven (Central
Florida Gas;
No
No
No
No
No
No
No
No
No
No
No
No
No
No
No
No
Location not known.
Location not known.
Coal tar was shipped offsite.
Field and parking lot.
Coal tar may have been barged
offsite; stadium constructed
onsite.
Coal tar sold and decomposed
by bacteria. Now a parking
lot.
Adjacent to lake.
(continued)
350
-------
TABLE 66 (continued)
Location
Walkover
inspec-
tion
(PCAP)'
Comments
St. Johns River District
Orlando (Peoples)
Sanford (FL Public
Utilities)
Ocala (Gulf Natural Gas
Corp.)
Deland (FL Public
Utilities)
Daytona Power & Light
South Florida District
Key West
Ft. Myers (Municipal)
SE Florida District
Miami (Peoples)
Ft. Lauderdale (Peoples)
Miami Beach (Peoples)
West Palm Beach (FL
Public Utilities)
No
No
No
No
No
No
Yes
No
Yes
Yes
No
No
Yes
Yes
No
Office and parking lot.
Up for sale.
No
No
No
No
No
No Location not known.
No No visible problem.
Soil and groundwater sampling
by ERM; no visible problem,
low concentrations of coal
tar constituents in ground-
water.
CAP has been prepared, but
not approved by DER and DERM.
Office and parking lot
aPCAP = Preliminary contamination assessment plan.
351
-------
TABLE 67. MARYLAND GAS SITES
Annapolis Plant (MD141)
Bayard Station (MD166)
Canton Station (MD159)
Spring Garden Station (MD145)
First Plant (M0147)
Second Plant (MD148)
Scots St. Station (MD191)
Cranberry Run Substation
Westminster Plant (MD146)
Cambridge Town Gas (MD165)
Fredrick Town Gas (MD164)
De Grace Town Gas (MD162)
Salisbury Town Gas (MD163)
Cumberland Gas Light (MD190)
Frostbury Gas Light
Elkton Gas Light
Chesterton Gas Light
Hyattsville Gas & Electric
Crisfield Gas and Light
Easton Gas and Light
Hagerstown Gas and Electric
352
-------
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354
-------
TABLE 70. NEW YORK STATE GAS SITES
New York State Electric and Gas
Oneonta site
Mechanicville sites (2)
Pittsburgh site
Cayuga Inlet site
Cortland-Homer site
Ithaca-Court Street site
Ithaca-First Street site
Elnrira site
Geneva site
Niagara-Mohawk Power Corporation
South Glens Falls site
Glens Falls site
Gloversville site
Saratoga site
Harbor Point site
Rochester Gas and Electric
Lower Falls site
355
-------
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TABLE 72. VIRGINIA GAS SITES
Site
Status
Danville Town Gas
Craghess St. RR Depot
Danville, VA 24541
Fredericksburg Town Gas
400 Charles Street
Fredericksburg, VA 22401
Fulton Bottom Town Las
Fulton & Williamsburg Road
Richmond, VA 23201
Lynchburg Town Gas
Black Water Street
Lynchburg, VA 24501
Newport News Town Gas
Terminal Blvd. & 22nd Street
Newport News, VA 23601
Norfolk Town Gas
Monticello & VA Beach Rd.
Norfolk, VA 23501
Portsmith Town Gas
Gust Lane
Portsmouth, VA 23701
Roanoke Town Gas
NE Klmbeil & Rutherford Ave.
Roanoke, VA 24001
Suffolk Town Gas
Hill Street
Suffolk, VA 23434
Alexandria Town Gas
City Yard Town Gas
Discovery (PA)
Discovery (PA)
Discovery (PA)
Discovery (PA)
Discovery (PA)
Discovery (PA)
Discovery (PA)
Site inspection
Discovery (PA)
Discovery (PA)
PA = Preliminary assessment.
359
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that have been located, are currently under investigation, or have been listed
by the States.
4.4 EVALUATION OF THE RADIAN LIST OF MANUFACTURED-GAS SITES I
The list of gas production sites compiled by Radian is a faithful compi-
lation of the site material contained in Brown's, but it has several short-
comings, most of v;hich result from the way Brown's compiled and reported
information on the manufactured-gas industry.
Sitss were listed in Brown's corporate designation. Whenever two plants
merged their management, Brown's usually stopped listing one plant, even
though it was often still in production. In Radian's compilation of the data
from Brown's, plants that merged with larger plants showed no production at
the site, even though gas was still produced there. The listing for Platts-
burgh, New York, is a good example. The plant merged with New York State
Electric and Gas Corporation in 1932, and subsequently its production was
included with that of Ithaca, New York. The Radian compilation shows that no
gas was produced under the Plattsburgh listing in 1940 and 1950, although the
plant actually operated into the 1950's.
Brown's Directrry includes only gas producers who sold their gas to con-
sumers. Facilities that supplied gas to a limited market (e.g., a large hotel
or an individual factory) did not appear in the directory. Many universities
also had their own gas plants at one time; however, because they did not sell
gas to consumers, they were not listed in Brown's. Brown's also did not list
gas production at factories that generally manufactured producer gas for
onsite heating purposes. An estimated 11,000 such gas producers were in
operation in 1921 (Chapman, 1921). Most sites using producer gas would
probably have several gas producers on each site, so the actual number of
possible sites would be much lower than 11,000. Brown's Directory, however,
reported none of these.
Brown's Directory also did not record the movement of plant operating
sites. It was common for gas companies to operate a small plant initially,
outgrow it, and then expand to a larger facility. Brown's recorded the
company's production as occurring at a single site rather than at two sites
and, as a result, the records Radian compiled indicate only a single site.
360
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Brown's generally included substantial information on plant byproducts
marketed by individual companies (in later operating years), but Radian did
not generally compile this information. The data available in Brown's could
be very useful in evaluating individual sites, but a very large effort would
be required to compile the data for all listed sites.
The Radian compilation apparently did not include any gas purchased by
gas companies from byproduct coke ovens. This was gas produced by coal car-
bonization, which was not manufactured by a gas company, but was sold
(generally locally) to a gas company by a coke manufacturer. From a waste or
site standpoint, it makes no difference if the gas were produced by a coke
company selling gas as a byproduct or by a gas company selling coke as a by-
product. A town having a gas company that produced some gas and purchased
additional gas from a local coke manufacturer would have had at least two gas
production sites, but it would be reported only as one in the Radian compila-
tion.
When the data were compiled from Brown's at 10-year intervals, signifi-
cant variations in rates of gas production were overlooked. The production of
gas dropped sharply after 1930, and it did not recover until World War II.
This would have produced errors i i the total amounts of gas reported,
particularly for the production of carbureted water gas.
4.5 CONCLUSIONS
Many States currently have active programs to examine nanufactured-gas
sites specifically for possible environmental hazards. In most cases, the
existing owners are requested to perform preliminary site assessments to
determine the extent of site contamination. Any necessary remedial actions
are determined only after the extent of contamination is known. Several
States have used the Radian list of manufactured-gas sites to assist them in
locating gas sites within their States.
In most States, the environmental authorities are initially satisfied
with determinations that no significant amounts of waste materials are moving
off a site and that no significant groundwater contamination has occurred.
Remediation is generally not performed at sites until some waste material
moves offsite or additional use of the manufactured-gas site is planned. The
site owners are generally content with leaving the sites as monitored (but
361
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unreinediated) because the cost of carrying the site as undeveloped land Is
small compared to the costs of remediation and redevelopment. In many cases,
the sites have remained undeveloped land since the surface structures were
removed.
In summary, the Radian list of manufactured-gas sites presented several
problems. Not all gas-manufacturing sites appeared in Brown's; hence, the
list is incomplete. Brown's listed gas manufacturers by corporate designa-
tion, so some companies listed as single sites in Brown's were actually com-
posed of several operating plants. In addition, several p'lu-it sites were
listed as only one when plants moved within cities. Cities having operating
coke plants (which produced gas that was sold to gas companies) and gas compa-
nies were reported as having only a single gas production site.
The Radian list is a good starting point for locating gas plants because
most of the towns listed had a gas-manufacturing plant. Local sources of
information, however, should not be overlooked, and they should take pre-
cedence over both information in Brown's Directory and in the Padian list.
362
-------
REFERENCES
Adaska, W. S., and Cavalli, N. J. 1984. Cement barriers. In: 5th National
Conference on Management of Uncontrolled Hazardous Waste Sites, October
31-November 2, 1983, Washington, DC. Hazardous Materials Control Research
Institute. Silver Spring, MD. pp. 126-130.
Addridge, W.M. 1951. Biochem. J. 48:271.
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