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Environmental fate & pathways

Biodegradation in soil

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Administrative data

biodegradation in soil
Type of information:
migrated information: read-across from supporting substance (structural analogue or surrogate)
Adequacy of study:
key study
2 (reliable with restrictions)
Rationale for reliability incl. deficiencies:
other: Non-GLP, near guideline study, published in peer reviewed literature, acceptable with restrictions

Data source

Reference Type:
Metabolism of Benzene, Toluene, and Xylene Hydrocarbons in Soil
Tsao C -W, Song H -G, Bartha R.
Bibliographic source:
Applied and Environmental Microbiology 64, 4924-4929

Materials and methods

Test guideline
equivalent or similar to guideline
OECD Guideline 304 A (Inherent Biodegradability in Soil)
only one soil type tested, higher test substance concentration than recommended, variation in apparatus, different type of control
GLP compliance:
Test type:

Test material

Constituent 1
Chemical structure
Reference substance name:
EC Number:
EC Name:
Cas Number:
Molecular formula:
Details on test material:
Ring-U-14C 0.325 mCi/mmol, purchased from Sigma Chemicals Co, purity >95%
Specific details on test material used for the study:
Details on properties of test surrogate or analogue material (migrated information):
Not applicable

Study design

Oxygen conditions:
Soil classification:
other: sandy loam
Details on soil characteristics:
Freshly collected from a lawn area of the New Jersey Agricultural Experiment Station, New Brunswick. The soil had no history of hydrocarbon exposure. Natural pH of 5.5-6 was raised to pH 7 by addition of CaCO3 at least five days prior to testing. Soil sieved to 2 mm size before use
Duration of test (contact time)
Soil No.:
28 d
Initial test substance concentration
Soil No.:
Initial conc.:
3 other: µL/g soil
Based on:
test mat.
Parameter followed for biodegradation estimation:
CO2 evolution
Details on experimental conditions:
Sealed aerobic system at 28°C. Three replicates per test concentration. 50 g (dry weight) soil samples were incubated in 1 litre flasks closed with teflon lined screw caps. Two syringe needles were inserted through cap. The long needle was closed with a stopper and attached to its lower end was a glass vial containing 10 mL of 0.5N KOH. This KOH was periodically withdrawn by syringe and replaced. The withdrawn KOH was used for counting trapped 14C02. The short syringe needle was connected by a three way valve to an oxygen reservoir and a port used to sample the flask headspace for solvent vapours. 150 µL test substance added to semi dry soil and then water added to bring soil to 60% holding capacity. Abiotic soil (autoclaved) was included as a control.

Results and discussion

Material (mass) balance
Soil No.:
% Recovery:
% Degradation
Soil No.:
% Degr.:
CO2 evolution
Sampling time:
13 d
Half-life / dissipation time of parent compound
Soil No.:
7 d
not specified
Remarks on result:
other: loss of test substance from soil based on analysis of flask headspace vapours approx 7 days (read from graph)
Transformation products:
not specified
Details on transformation products:
Not discussed, but authors note lag between 50% loss of substance from soil and 50% 14CO2 evolution.
Evaporation of parent compound:
Volatile metabolites:
Details on results:
After 4 weeks incorpation into biomass was ~3% and incorporation into soil humus ~12% (read from graph). In abiotic controls only a negligible amounts of test substance were lost to sampling process and no measurable 14CO2 was evolved. Cumulatively over the course of the experiment 2-3% of the radiolabelled test substance dissolved in the KOH trap without prior conversion to 14CO2. Corrections were not made for this.
Results with reference substance:
Not applicable

Applicant's summary and conclusion

50% of applied radiolabelled p-xylene was mineralised in 13 days.
Executive summary:

This study was selected as the key study as it approximates OECD 304A. There are several differences between the protocol followed and the standard guidelines. Only one soil type is tested and the concentration of test substance is higher than recommended (150 µL/50 g soil compared to 100 µL/50 g soil) although the amount of radioactivity applied is within the recommendation levels. The control test used autoclaved soil, rather than no soil. Despite these differences the study is well described and the mass balance of applied test substance is ~90%. This study demonstrates that p-xylene is degraded in soil.