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Manual for Soil Analysis-Monitoring and Assessing Soil Bioremediation Phần 4 doc
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98 K.S. Jørgensen et al.
The biodegradation rate can be linear or represent first order decay dependent on, e.g., the contaminant concentration and bioavailability. Field-scale
bioremediation can be classified as either in situ methods, where the treatment takes place without excavating the soil, and ex situ methods, where excavated soil is treated typically in piles. When monitoring a site undergoing
in situ treatment by drilling for subsurface samples, it is essential to remember that true replicate samples cannot be obtained and a large variation is to
be expected. When sampling stock piles or biopiles, a combination sample
consisting of subsamples from different places in the piles typically will be
assembled, and parallel combination samples can be made (Jørgensen et al.
2000). When monitoring biodegradation by laboratory microcosms, it is of
great importance that all the sample material representing a certain depth,
treatment, etc., is homogenous. This is best ensured by homogenizing and
sieving a larger batch from the field and by distributing this into separate
parallel bottles or other containers for laboratory incubations. A mesh size
of 8 mm has proven to be a good size for sieving field-moist soil (Laine
and Jørgensen 1997; Salminen et al. 2004). However, the measurement of
contaminant disappearance only shows that the parent compound has been
transformed; it does not reveal whether the degradation is complete to CO2
or CH4 or if other degradation products are produced.
Contamination with petroleum hydrocarbon products is one of the most
frequent types of soil contamination. Refineries, surface and underground
storage tanks, petrol service stations, etc., are the most common sites for
such contamination. Most petroleum products also contain minor amounts
of PAHs. No single method is reliable for the determination of all petroleum
hydrocarbons, and we therefore describe three methods for the determination of different fractions of hydrocarbons in soil samples.
Volatile hydrocarbons (Sect. 3.2) should be determined at sites where
gasoline and jet fuel are the sources of contamination. The pertinent
method here quantitatively determines these separate compounds: benzene, toluene, ethylbenzene and xylenes (BTEX compounds), naphthalene,
and gasoline additives such as MTBE (methyl tert-butyl ether) and TAME
(tert-amyl methyl ether). This method can also be used to determine halogenated volatiles, which may often be found together with fuel products
because such solvents often are used, e.g., for cleaning engines.
Contamination with oil products such as heating oil, diesel or lubricating
oil is best determined using the method (Sect. 3.3) for hydrocarbons in
the range C10 to C40. The result is a sum parameter, which does not give
concentrations of specific compounds. But still the sum of the hundreds of
compounds in this range is very useful for quantifying contamination with
them and for monitoring bioremediation. Based on the chromatogram,
a qualitative estimation of the type of contamination can be obtained.
This C10–40 parameter is often referred to as mineral oil or total petroleum
3 Quantification of Soil Contamination 99
hydrocarbons (TPH), but these terms are somewhat unspecific. Crude oil is
often determined with this method, but it also includes volatiles and PAHs
that should be determined separately with the methods for volatiles and
PAHs, respectively.
Contamination with PAHs is commonly found at gas works and at sites
where coal tar and oil shale are handled. Oil containing heavy fractions
or waste oil may also contain significant amounts of PAHs. The method
described here (Sect. 3.4) allows for a single determination of 16 different
PAH compounds. In the literature the sum of PAHs is often reported, but
the fact that different countries and different laboratories analyze different
number of compounds has made this term very unspecific. Guideline values
for clean-up needs also differ between countries, so it is important to
check which compounds require reports. Since the toxicities of the PAH
compounds differ, there may not be any guideline value set out for all
compounds.
Contamination with heavy metals is difficult to assess because clean
soil itself may contain many heavy metals, depending on the geological
structure. Furthermore, many metals are not necessarily bioavailable in
soil, and for that reason different types of less exhaustive extractions are
being developed to determine the bioavailable fractions. The background
contents of metals in soil are in many countries known and they are taken
into account when guideline values for clean-up are determined. Still today
most guideline values are based on the total or near-total content of metals.
The method described here (Sect. 3.5) reveals the near-total content and is
aiming at determining the anthropogenic contamination.
3.2
Volatile Hydrocarbons
■ Introduction
Objectives. The volatile organic compounds (VOCs) in soils primarily originate from petroleum products and solvents. The spectra of the VOCs depend on their source. The analysis of benzene, toluene, and ethylbenzene
and xylenes (BTEX) is widely used as an indicator of contamination with
light petroleum products, e.g., petrol and kerosene. Furthermore, the gasoline additives MTBE and TAME as well as halogenated volatile compounds
can be analyzed with this method.
Principle. A soil sample is extracted with methanol. A defined volume of the
methanol extract is transferred into water and the water sample is heated
to 80 ◦C in a headspace vial. When equilibrium is established between the
gaseous and liquid phases, an aliquot of the gaseous phase is injected on
100 K.S. Jørgensen et al.
a column of a gas chromatograph and the VOCs are determined with a mass
selective detector.
Theory. VOCs are a group of compounds that have a boiling point from 20
to 220 ◦C and usually they have two to ten C atoms. They are mainly unsubstituted or substituted monoaromatics and short-chain aliphatic compounds that differ in solubility and in toxicity. The individual compounds
are quantitatively determined using this method, as can also be the diaromatic compound naphthalene. We do not recommend measuring the sum
of VOCs because such a sum is unspecific and depends on the compounds
included.
The sampling (ISO 10381–1 1994; ISO 10381–2 1994; Owen and Whittle
2003) is a crucial step in the analysis of VOCs. In order to prevent their loss
during preparative steps, field-moist samples are used (ISO 14507 2003).
The sample is added into a pre-weighed glass container containing a known
amount of methanol. To control the quality of the determination, field duplicates, a procedural blank, and a control sample are analyzed. The two
main methods of analysis of VOCs are static headspace/gas chromatography (e.g., ISO/PRF 22155 in prep.) and purge and trap/gas chromatography
(e.g., ISO 15009 2002). In the analysis of volatile aliphatic and aromatic
hydrocarbons a mass selective detector (MSD) is used. VOCs can also be
detected with a photo ionization detector (PID), a flame ionization detector (FID), and an electron capture detector (ECD; Owen and Whittle 2003).
The identification of target compounds (ISO/DIS 22892 in prep.) is easy
with a MSD, and a possible matrix effect can be eliminated. The method
described here is that using static headspace/gas chromatography (MSD)
and is based on the proof of a new international standard ISO/PRF 22155
and has earlier been described by Salminen et al. (2004).
■ Equipment
• Usual laboratory glassware, free of interfering compounds
• Shaking machine
• Headspace analyzer and gas chromatograph with a mass selective detector (MSD)
– Oven temperature program: maintain 35 ◦C for 2 min, then steadily
raise by 14 ◦C/min up to 90 ◦C. Maintain 90 ◦C for 5 min, then raise
by 12 ◦C/min up to 190 ◦C. Maintain 190 ◦C for 1 min, then raise by
40 ◦C/min up to 225 ◦C, and maintain at 225 ◦C for 1 min.
– Carrier gas: helium.
– Gas flow: 10 mL/min.
– Split ratio (gas flow rate through split exit: column flow rate): 5.7:1.