SOIL AND/OR GROUNDWATER REMEDIATION PROCESS
FIELD OF THE INVENTION
The present invention is directed to methods and systems for converting
contaminants contained in soil and/or groundwater to non-contaminating or harmless
compounds. The methods and systems include treatment of the contaminants with a
peroxide (e.g. hydrogen peroxide) and ozone which produce the hydroxyl radical and
other reactive species to thereby promote and control the conversion of the
contaminants to harmless by-products.
BACKGROUND OF THE INVENTION
The treatment of contaminated soils and groundwater has gained increased
attention over the past few years because of the increasing number of uncontrolled
hazardous waste disposal sites. It is well documented that the most common means
of site remediation has been excavation and landfill disposal. While these procedures
remove contaminants, they are extremely costly and in some cases difficult if not
impossible to perform.
More recently, research has focused on the conversion of contaminants
contained in soil and groundwater based on the development of on-site and in situ
treatment technologies. One such treatment has been the incineration of contaminated
soils. The disadvantage of this system is in the possible formation of harmful by-
products including polychiorinated dibenzo-p-dioxins (PCDD) and polychlohnated
dibenzofurans (PCDF).
In situ biological soil treatment and groundwater treatment is another such
system that has been reviewed in recent years. So-called bioremediation systems,
however, have limited utility for treating waste components that are biorefractory or toxic
to microorganisms.
Such bioremediation systems were the first to investigate the practical and
efficient injection of hydrogen peroxide into groundwater and/or soils. These
investigations revealed that the overriding issue affecting the use of hydrogen peroxide
in situ was the instability of the hydrogen peroxide downgradient from the injection
point. The presence of minerals and the enzyme catalase in the subsurface catalyzed
the disproportionation of hydrogen peroxide near the injection point, with rapid evolution
and loss of molecular oxygen, leading to the investigation of stabilizers as well as
biological nutrients.
During the early biological studies from the 1980s, some investigators
recognized the potential for competing reactions, such as the direct oxidation of the
substrate by hydrogen peroxide. Certain researchers also hypothesized that an
unwanted in-situ Fenton's-like reaction under native conditions in the soil was reducing
yields of oxygen through the production of hydroxyl radicals. Such a mechanism of
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contaminant reduction in situ was not unexpected, since Fenton's-type systems have
been used in ex situ systems to treat soil and groundwater contamination.
Other investigators concomitantly extended the use of Fenton's-type systems to
the remediation of in situ soil systems. These studies attempted to correlate variable
parameters such as hydrogen peroxide, iron, phosphate, pH, and temperature with the
efficiency of remediation.
As with the bioremedial systems, in situ Fenton's systems were often limited by
instability of the hydrogen peroxide in situ and by the lack of spatial and temporal
control in the formation of the oxidizing agent (hydroxyl radical) from the hydrogen
peroxide. In particular, aggressive/violent reactions often occurred at or near the point
where the source of the oxidizing agent (the hydrogen peroxide) and the metal catalyst
were injected. As a consequence, a significant amount of reagents including the source
of the oxidizing agent (hydrogen peroxide) was wasted because activity was confined
to a very limited area around the injection point. In addition, these in situ Fenton's
systems often required the aggressive adjustment of groundwater pH with acid, which
is not desirable in a minimally invasive treatment system. Finally, such systems also
resulted in the mineralization of the subsurface, resulting in impermeable soil and
groundwater phases due to the deleterious effects of the reagents on the subsurface
soils.
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Other researchers have investigated the use of ozone, either alone or in
combination with hydrogen peroxide, in ex situ advanced oxidation processes (AOPs).
These systems suffered from a similar limitation as the ex situ Fenton's systems;
namely, the necessity to pump contaminants from the in situ media to an external
reaction vessel, a requirement which was both expensive and inefficient. Ozonation
processes also suffered from low selectivity of contaminant destruction and high
instability of the ozone and reactive species generated.
It would be of significant advantage in the art of removing contaminants from soil
and/or groundwater to provide a system by which the source of the oxidizing agent can
travel from the injection point throughout the aerial extent of the contamination in order
to promote efficient destruction of the contaminant plume without the acidification of the
subsurface or the resultant mineralization of the soils. It would also be a significant
advantage in the art to generate a variety of reactive species in sufficient quantity to
allow the efficient degradation of a number of contaminants including traditionally
recalcitrant chlorinated solvents such as polychloroethylenes and trichloroethylenes.
It would be a further benefit in the art to provide a system which efficiently
generates the hydroxyl radical to provide a cost efficient and effective method of
oxidizing contaminants in soil and/or ground water.
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SUMMARY OF THE INVENTION
The present invention is directed to methods and systems for treating
contaminants in an in situ environment in which a reactive agent (hydroxyl radical
and/or other reactive species) obtained from the reaction of a peroxide, such as
hydrogen peroxide, with ozone, in an in situ environment reduces or eliminates
contaminants present therein in a cost efficient and effective manner.
In accordance with one aspect of the invention, there is provided a method and
system of treating contaminants in an in situ environment comprising adding an
effective amount of a peroxide to the in situ environment together or separately with an
effective amount of ozone, which by their reaction and generation of reactive species,
are capable of oxidizing at least one of the contaminants to reduce the concentration
thereof in the in situ environment. The present system enables temporal and spatial
control of the oxidation process so that the reactive species (e.g. hydroxyl radical) is
able to be generated into areas where contaminants are present. As a result,
aggressive/violent reactions at the point of injection are minimized and less reactive
species is wasted. In addition, due to the generation of hydroxyl radicals throughout
the plume and the presence of other reactive species, contaminants normally
recalcitrant to ex situ Fenton's or advance oxidation processes are now able to be
converted to harmless by-products.
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In accordance with preferred aspects of the invention, the peroxide component
is first injected into the in situ environment, either the groundwater or the soil above the
groundwater. The gaseous ozone is preferably injected into the groundwater through
multiple sparge points dispersed throughout the aerial extent of the plume where it
combines with the peroxide to generate the reactive species (e.g. hydroxyl radical).
Alternatively, the ozone can be injected into the subsurface as an aqueous solution into
the groundwater or as a gas into the vadose zone.
In accordance with another aspect of the invention, the methods and systems
herein can be applied to oxidizing contaminants in formations which are difficult to
access such as fractured bedrock. In particular, the peroxide and ozone are injected
at elevated pressures into the fractured bedrock to treat contaminants whose density
is greater than water and are often trapped in bedrock fractures.
In a further aspect of the invention, the peroxide and ozone are injected into the
in situ environment to enhance the operation and efficiency of traditional remediation
technologies such as pump and treat and solvent vapor extraction systems. The
present invention enhances these conventional systems that are based on mechanical
removal of the contaminants. This is because the oxidation reactions which convert the
contaminants to harmless compounds also enhance desorption of the contaminants
from organic carbon in soil and/or groundwater and generally result in enhanced
volatilization. The breakdown of contaminants into smaller compounds and the
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increased production of carbon dioxide in the method of the present invention also
enhances volatilization and reduces adsorption of organic carbon in the soil.
DETAILED DESCRIPTION OF THE INVENTION
The present invention is directed to methods and systems for removing
contaminants from soil and/or groundwater by converting the same to harmless by¬
products. Such contaminants typically arise from petroleum storage tank spills or from
intentional or accidental discharge of liquid hydrocarbons or compositions containing
the same. Typical examples of contaminants are hydrocarbons including, but not
limited to: gasoline, fuel oils, benzene, toluene, ethylbenzene, xylenes, naphthalene,
pesticides, herbicides and other organic compounds; lubricants; chlorinated solvents,
including polychiorinated ethylenes, trichlorinated ethylenes, vinyl chlorides, dichloro
ethylenes, polychiorinated biphenyls (PCBs), pentachlorophenol (PCP); and metals,
cyanides and the like. The list of contaminants provided herein is exemplary. It should
be understood, however, that other contaminants capable of being oxidized into
harmless compounds, such as carbon dioxide and water, is within the purview of the
present invention.
In accordance with the present invention, the methods and systems for
remediation of a contaminated environment in situ is performed by providing a stabilized
source of a peroxide, for example hydrogen peroxide, and a source of ozone so that
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they may react in situ to form a reactive species (e.g. hydroxyl radical), as hereinafter
described. It has been found that the reactive species generated in this way are found
throughout the extent of the plume with a resultant higher efficiency of contaminant
destruction.
In one embodiment of the invention, the peroxide and the ozone are alternately
injected (i.e. pulsed) into the soil and/or groundwater. In another embodiment of the
invention, the stabilized peroxide is allowed to disperse or migrate throughout the plume
and subsequently the ozone is bubbled into the groundwater through, preferably,
multiple sparge points.
The sources of the reactive species employed in the present invention is the
combination of a peroxide and ozone. Peroxides include, for example, hydrogen
peroxide, calcium peroxide, and sodium peroxide. Calcium peroxide generates
hydroxyl radicals under acidic conditions in the presence of iron (II) salts. Calcium
peroxide is very slightly soluble in water and is generally more expensive than hydrogen
peroxide. However, calcium peroxide can be used as an effective source of oxidizing
agent for hydrocarbon-contaminated sites. Sodium peroxide has been found to behave
in a manner similar to calcium peroxide and can be used as well. Hydrogen peroxide
is the preferred peroxide for use in the present invention.
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The peroxide (e.g. hydrogen peroxide) reacts with ozone in situ to produce
reactive species, including but not limited to hydroxyl radicals, hydroperoxide ion, and
ozonide ion. Ozone has previously been used as a disinfectant and in more recent
applications to oxidize refractory organic contaminants. The concentration of ozone
suitable for employment in the present invention can be supplied from known
commercial ozone generators (e.g. from about 3 to 15% ozone in air).
What is essential is that the system be capable of generating reactive species
in sufficient quantity and for a sufficient length of time to convert existing contaminants
(e.g. hydrocarbons) to harmless compounds (e.g. carbon dioxide and water vapor).
Prior to injection, the peroxide is preferably stabilized. Stabilization prevents the
immediate conversion of the peroxide via native iron or catalase into hydroxide radicals
or oxygen at positions only immediately adjacent to the injection points. Once stabilized
the peroxide is introduced into the in situ environment, typically in water at a
concentration of up to about 35% by weight. It will be understood that the concentration
of peroxide in the in situ environment will significantly decrease as the peroxide spreads
out through the soil and/or groundwater. Suitable stabilizers include acids and salts
thereof. The most preferred acid is phosphoric acid and the most preferred salt is
monopotassium phosphate.
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The in situ environment for most soil and/or groundwater sites includes a water
table which is the uppermost level of the below-ground, geological formation that is
saturated with water. Water pressure in the pores of the soil or rock is equal to
atmospheric pressure. Above the water table is the unsaturated zone or vadose region
comprising the upper layers of soil in which pore spaces or rock are filled with air or
water at less than atmospheric pressure. The capillary fringe is that portion of the
vadose region which lies just above the water table.
The capillary fringe is formed by contact between the water table and the dry
porous material constituting the vadose region. The water from the water table rises
into the dry porous material due to surface tension because of an unbalanced molecular
attraction of the water at the boundary.
The source of the reactive species (peroxide and ozone) can be administered
in any zone in the in situ environment by any method considered conventional in the art.
For example, administration can be directly into the groundwater through a horizontal
or vertical well or into subterranean soil through a well or infiltration trenches at or near
the site of contamination. In a preferred form of the invention, the peroxide is placed
into the subsoil where it leaches therethrough into the groundwater. Ozone can be
introduced directly to the groundwater as a gas or as an aqueous solution (preferably
through multiple sparge points) or may be injected into the vadose zone.
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As previously indicated, peroxide and ozone can be administered under elevated
pressures into hard to reach places such as fractures within underlying bedrock. These
fractures are collecting places for contaminants which are typically more dense than
water. When administered the peroxide and ozone are able to penetrate the fractures,
contact the contaminants and convert the same to harmless compounds.
Injection of the peroxide and ozone can be accomplished by installing steel or
polyvinylchloride lined wells or open hole type wells into the bedrock. Packers and
bladders conventionally employed in downhole drilling can be employed to assist in
isolating discrete fractures and accessing the contaminants with the reagents. The
reagents are then injected into the fractures at applied elevated pressures, typically in
the range of from about 40 to 100 psi.
The administration of the peroxide and ozone into the in situ environment
including bed rock fractures under elevated pressures can be accomplished either alone
or in conjunction with conventional treatment systems. Such systems include pump and
treat systems which pump the contaminated groundwater out of the in situ environment
and solvent vapor extraction systems in which a vacuum is applied to the site of
contamination to physically enhance volatilization and desorption of the contaminants
from soil and/or groundwater.
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The employment of ozone as a reactant for the formation of reactive species is
advantageous because ozone can be continuously generated by readily available
ozone generators which do not require excessive labor to operate. In addition, unlike
conventional Fenton's systems which are highly dependent on pH and require the
aggressive adjustment of site pH, it has been found that the present system functions
efficiently at neutral to alkaline pH, consistent with the native pH found in many
subsurface environments.
As indicated above, the peroxide and ozone can be administered directly into the
in situ environment. In a preferred form of the invention, the amount of the peroxide
and ozone and the number of treatment cycles are predetermined. For example,
samples of the contaminated soil and/or groundwater are taken and the concentrations
of the peroxide and ozone required for in situ treatment are then determined based on
the amount of each reagent needed to at least substantially rid the samples of the
contaminants contained therein.
More specifically, a sample of the soil and/or groundwater is analyzed to
determine the concentration of the contaminants of interest (e.g. hydrocarbons).
Analysis of volatile hydrocarbons can be made by gas chromatographic/mass
spectrometric systems which follow, for example, EPA Method 624. Semi-volatiles are
analyzed in a similar manner according to, for example, EPA Method 625.
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Results from these analyses are used to determine the combinations of peroxide
and ozone for treatment of the sample based on the type and concentration of the
contaminants. A specific weight ratio of the peroxide and ozone is used for the sample
based on prior research, comparative samples and the like. Typical sample volumes
can be in the range of from about 120 to 150 ml. It has been found that a weight ratio
of from about 0.2 to 1.5 w/w peroxide/ozone in the in situ environment is preferred
because operation within this ratio provides the highest efficiency of contaminant
destruction for most contaminants.
Sample analysis is also employed to determine the number of treatment cycles
which may be necessary to achieve the desired reduction in the level of contaminants.
While one treatment cycle may be used, it is often desirable to employ a plurality of
treatment cycles depending on the type and concentration of contaminants. The
number of treatment cycles is determined in part by monitoring the performance of the
peroxide and ozone once injected into the soil and/or groundwater.
In operation, the peroxide and ozone are injected into sealed vials with a syringe.
The doses of peroxide and ozone are given as hourly treatment cycles with the
expectation that the samples will typically require as few as one treatment cycle and as
many as five treatment cycles in order to substantially or completely convert the
contaminants to harmless by-products.
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A control sample is set up for each type of sample undergoing the study to
correct for any volatization loss. All experimental vials are allowed to sit overnight at
room temperature. On the following day the samples are analyzed to determine the
concentration of contaminants by the above-mentioned EPA procedures. Once the
results are obtained, they may be extrapolated to provide a suitable amount of the
peroxide and ozone necessary to treat the contaminants in situ.
Injection of the stabilized source of the peroxide may be performed under both
applied and hydrostatic pressure into the in situ environment. Flow rates will vary
depending on the subsurface soil characteristics with faster rates associated with more
highly permeable soils (e.g. gravel and/or sand). Slower rates as low as 0.1 gallons per
minute may be used for less permeable soils (e.g. clays and/or silts). The stabilized
source of the peroxide may be injected into the subsurface and allowed to disperse
over a specific period, typically about 24 hours. The length of time may be varied
depending on the soil type.
In less permeable soils, injection procedures are preferably associated with a
pressurized system. A typical system involves injection wells installed with screens set
at specific levels to allow for higher pressures and countered by pumping into less
permeable soils. The pumping system can include a low horsepower pump at
pressures ranging from between about 10 and 40 pounds per square inch. The
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stabilized peroxide may be pumped in short pulse injections or in a long steady flow as
desired.
In a preferred form of the invention, the stabilized peroxide is injected directly into
the capillary fringe, located just above the water table. This can be accomplished in a
conventional manner by installing a well screened in the capillary fringe and injecting
the reagents into the well screen.
After the peroxide has been injected into the in situ environment and allowed to
disperse throughout the aerial extent of the plume in this preferred embodiment, ozone
is generated on site and pumped into the subsurface as described previously.
Preferably the ozone is injected as a gas into the groundwater through multiple injection
points arranged throughout the aerial extent of the plume. In another embodiment, the
ozone and peroxide can be alternatively pulsed into the in situ environment.
In particular, the effects of naturally occurring minerals including their reactivity
with the peroxide and ozone can have a dramatic effect on the extent of the formation
of the reactive species. It has been found that injection of the stabilized source of the
peroxide followed by subsequent repeated ozone injections allows for improved
efficiency of conversion to reactive species throughout the plume in the subsurface.
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In particular, a monitoring system employs a free radical trap to directly measure
the concentration of the reactive species contained within the in situ environment. More
specifically, a sample of the soil and/or groundwater is combined with a specified
amount of a free radical trap such as methylene blue dye. The mixture is stabilized and
precipitated and/or colloidal matter removed. The absorbance of the color remaining
in the sample is measured using a spectrophotometer at a wavelength capable of
measuring the absorbance of the blue dye (e.g. 662 nm). The absorbance value is then
compared to the standard curve of absorbance vs. reagent value determined for the
particular site.
The free radical concentration of the sample is expressed as a reagent value (R)
which is proportional to the concentration of the radical and is representative of the
amount of the peroxide and ozone initially added that are remaining at that point as
shown in Table #1. This amount is expressed as a fraction proportional to the total
number of treatment cycles X, wherein X is the number of treatment cycles originally
recommended for the sample.
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TABLE 1
Reagent Explanation Value (R)
2 100% of the peroxide and ozone initially added are still present. The amount of free radicals produced in 10 minutes is highest for this sample.
1 50% of the peroxide and ozone initially added are still remaining in the sample. The amount of free radicals produced in 10 minutes for R=1 sample is one half the amount produced for R=2 sample.
0.5 25% of the peroxide and ozone initially added are still remaining in the sample. The amount of free radicals produced in 10 minutes for R=0.5 sample is one quarter the amount produced for R=2 sample.
EXAMPLE 1
The following experiments were conducted in two (2) - 1500 cm3 air-tight glass
reactors with inlets provided for ozone, hydrogen peroxide, sample collection and
venting. A representative contaminated sample as shown in Table 2 was prepared by
spiking appropriate concentrations of the contaminants into tap water. Exactly 1000
cm3 of the substrate solution was decanted into each of two reactors designated for
control and treatment purposes and placed on magnetic stirrers for a mixing operation.
The Ozonator used in the experiments had a maximum ozone generating capacity of
6 g/h. Hydrogen peroxide was introduced into the treatment reactor immediately prior
to ozonation. Ozonated oxygen (approx. 4% v/v O3) was introduced and allowed to
bubble at the bottom of the reactor.
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The control reactor was simultaneously treated by introducing distilled water in
place of hydrogen peroxide and bubbled with pure oxygen instead of ozone at similar
flow rates. Water samples were withdrawn periodically for residual hydrogen peroxide
analysis. Water and air samples for volatile organic analysis were collected after 60
minutes of ozonation at which time hydrogen peroxide was completely consumed.
Air samples were collected in tedlar bags and water samples in 40 ml VOA vials
preserved in HCI. Both air and water samples were analyzed for targeted volatile
organics by an EPA certified laboratory. Hydrogen peroxide concentration was
determined by complexing with Ti(IV) and measuring the absorbance of the yellow color
developed spectrophotometrically (FMC 1989). Ozone concentration in both air and
water was measured by iodometric titration (Standard Methods, 1989). The results are
shown in Table 2.
TABLE 2
Contaminant Before Treatment After Treatment Percent
(ppb)* (ppb)* Reduction (%)
Trichloroethene 518 7.1 98.6
Perchloroethene 472 11.3 97.6
Vinyl Chloride 610 9.0 98.5 cis-1 ,2-Dichloroethene 450 5.0 98.9
Benzene 87 3.5 95.9
* parts per billion ** Not Detected
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As shown in Table 2, the reduction in the level of contaminants after treatment
with the reactive species formed by the reaction solution containing the peroxide and
ozone was between about 95.9 and 100%.
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