Distribution and risk assessment of selected organochlorine pesticides in Kyzyl Kairat village from Kazakhstan.

Concentrations of selected organochlorine pesticides (OCPs), i.e., 4,4'-dichlorodiphenyltrichloroethane (p,p'-DDT), its metabolites (p,p'-DDE, p,p'-DDD), and hexachlorocyclohexanes (HCHs), have been determined in 100 soil samples collected from a contaminated site centered around a former storehouse in the Kyzyl Kairat village, Almaty region, Kazakhstan, which constitutes an exemplary case example. The OCPs were observed in all analyzed soil samples, with predominance of α-HCH, p,p'-DDD, p,p'-DDE, and p,p'-DDT. Total concentrations ranged from 1.38 to 11,100 µg kg(-1) with an average value of 1040 µg kg(-1) for DDT and its metabolites and 0.1 to 438 µg kg(-1) with an average value of 24 µg kg(-1) for HCHs. The observed concentrations of the OCPs were found to be in agreement with previous studies and are rationalized in terms of the possible degradation pathways of DDTs and HCHs. Spatial distribution patterns of OCPs are elucidated by contour maps. Observed concentrations of the OCPs were used to evaluate the cancer risk to humans via ingestion, dermal contact, and inhalation of soil particles. The cancer risk mainly occurs from ingestion, whereas dermal exposure contributes to a minor extent to the total cancer risk. The risk associated with inhalation was found to be negligible. The total cancer risk for the studied OCPs were found to be p,p'-DDT ˃ p,p'-DDE ˃ p,p'-DDD ˃ α-HCH ˃ ß-HCH ˃ γ-HCH.

Transformation products of 1,1-dimethylhydrazine and their distribution in soils of fall places of rocket carriers in Central Kazakhstan.

In our research, three fall places of first stages of Proton rockets have been studied for the presence and distribution of transformation products of 1,1-dimethylhydrazine (1,1-DMH). Results of identification of transformation products of 1,1-DMH in real soil samples polluted due to rocket fuel spills allowed to detect 18 earlier unknown metabolites of 1,1-DMH being formed only under field conditions. According to the results of quantitative analyses, maximum concentrations of 1-methyl-1H-1,2,4-triazole made up 57.3, 44.9 and 13.3 mg kg(-1), of 1-ethyl-1H-1,2,4-triazole - 5.45, 3.66 and 0.66 mg kg(-1), of 1,3-dimethyl-1H-1,2,4-triazole - 24.0, 17.8 and 4.9 mg kg(-1) in fall places 1, 2 and 3, respectively. 4-Methyl-4H-1,2,4-triazole was detected only in fall places 2 and 3 where its maximum concentrations made up 4.2 and 0.66 mg kg(-1), respectively. The pollution of soils with transformation products of 1,1-DMH was only detected in epicenters of fall places having a diameter of 8 to10 m where rocket boosters landed. The results of a detailed study of distribution of 1,1-DMH transformation products along the soil profile indicate that transformation products can migrate down to the depth of 120 cm, The highest concentrations of 1,1-DMH transformation products were detected, as a rule, at the depth 20 to 60 cm. However, this index can vary depending on the compound, humidity and physical properties of soil, landscape features and other conditions. In the surface layer, as a rule, only semi-volatile products of transformation were detected which was caused by fast evaporation and biodegradation of volatile metabolites.

Intermolecular potential and second virial coefficient of the water-nitrogen complex.

The authors construct a rigid-body (five-dimensional) potential energy surface for the water-nitrogen complex using the systematic intermolecular potential extrapolation routine. The intermolecular potential is then extrapolated to the limit of a complete basis set. An analytic fit of this surface is obtained, and, using this, the global minimum energy is found. The minimum is located in an arrangement in which N2 is near the H atom of H2O, almost collinear with the OH bond. The best estimate of the binding energy is 441 cm-1 (1 cm-1 approximately 1.986 43x10(-23) J). The extrapolated potential is then used to calculate the second cross virial coefficient over a wide temperature range (100-3000 K). These calculated second virial coefficients are generally consistent with experimental data, but for the most part the former have smaller uncertainties.