Pesticide Residues in Water From River Kaveri,South India

The residue levels of presistent chlorinated pesticides such as HCH (hexachlorocyclo-hexane) isomers and DDT (dichlorodiphenyl trichloroethane) compounds were quantified in water samples collected from the River Kaveri and its distributor River Coleroon in Tamil Nadu, South India. HCH showed higher levels in River Kaveri during premonsoon (July to September) and monsoon (October to December) months, reflecting the HCH usage during that season for paddy crops. But in the case of DDT no clear trend in residue level was observed. the α-HCH was detected as the dominant isomer in all the three sampling sites. Among DDT compounds, p,p'-DDT and p,p'-DDE showed higher percentage of the total. International comparison of residue levels revealed that the present values are comparable to the waters from Asian and South East Asian nations, but lower than some samples from other parts of India. the value of DDT is well below the EEC's maximum acceptable concentration for surface waters and lower than the recommended limit of 2000ng 1^-1 in USA water for protection of aquatic life (Water Quality Criteria, 1972).     

利用共代谢机制降解水体中的氯代芳烃

氯代芳烃及其衍生物是一类毒性强、难降解的持久性有机化合物。在我国江河水体中检出率高，其中许多是优先监测污染物。水中的难降解有机污染物，可能通过几种微生物的一系列共代谢作用得到大部分，甚至是彻底的降解。本文针对水环境中的氟代芳烃污染物，分析了共代谢的类型、发生原因及影响因素。对利用共代谢机制修复水中氯代芳烃的最新研究进展进行了综述，并对本领域的发展前景进行了探讨。     

零价铁用于水中氯代有机物还原脱氯的现状与发展

综述了零价铁作为氯代有机物的发展状况,零价铁、纳米零价铁、含铁双金属体系及固定态双金属体系还原脱氯机理、应用现状、存在问题及其未来发展趋势。     

氯乙烯在地下水和土壤中的厌氧脱氯还原降解

主要介绍了通过原位生物修复技术还原脱氯降解氯乙烯的污染。通过注射井向氯乙烯污染区域注射有机物基质作为电子供体,再加入通过富集培养的强化微生物,通过微生物的作用对污染物降解,从而达到对污染地区修复的目的。并列举了一个实例说明此修复技术目前的研究进展水平。     

同位素稀释高分辨气相色谱-高分辨质谱法测定氯化石蜡工业品中二噁英

氯化石蜡（CPs）作为一种用途广泛、产量大的有机氯化学工业品,具有组成多样、基质复杂等特点,对其中产生的二噁英（PCDD/Fs）检测是当前工作面临的难题。建立了同位素稀释高分辨气相色谱-高分辨质谱法检测CPs工业品中PCDD/Fs的分析方法。对样品净化过程进行了优化,通过提取溶剂筛选,去除固体CPs中部分基质,建立的双活性炭柱法可高效去除CPs基质。方法采用¹³ C₁₂标记的PCDD/Fs内标物进行定性和定量分析。17种PCDD/Fs同系物的检出限为0.1～3 pg/g,回收率为31.7%～100%。该方法可对高纯度工业品中痕量持久性有机污染物进行高效的定性和定量分析,能够满足国家标准方法对PCDD/Fs检测的要求。     

The need for bioaugmentation after thermal treatment of a TCE-contaminated aquifer: Laboratory experiments

A microcosm study was conducted to evaluate the need for bioaugmentation after a thermal treatment to anaerobically dechlorinate trichloroethene (TCE) to ethene. The microcosms were either: heated to 100 degrees C and slowly cooled to simulate thermal remediation while bioaugmenting when the declining temperature reached 10 degrees C; or kept at ambient groundwater temperatures (10 degrees C) and bioaugmented for comparison. Aquifer samples from three sediment locations within a TCE-polluted source zone were investigated in duplicate microcosms. In biostimulated (5 mM lactate) and heated microcosms, no conversion of TCE was observed in 4 out of 6 microcosms, and in the remaining microcosms the dechlorination of TCE was incomplete to cDCE (cis-dichloroethene). By comparison, complete TCE dechlorination to ethene was observed in 4 out of 6 heated microcosms that were bioaugmented with a highly enriched dechlorinating mixed culture, KB-1, but no electron donor, and also in 4 of 6 microcosms that were augmented with KB-1 and an electron donor (5 mM lactate). These data suggest that electron donor released during heating, was capable of promoting complete dechlorination coincident with bioaugmentation. Heated microcosms demonstrated less methanogenesis than unheated microcosms, even with elevated H2 concentrations and addition of KB-1, which contains methanogens. This suggests that the heating process suppressed the native microbial community, which can decrease competition with the bioaugmented culture and increase the effectiveness of dechlorination following a thermal treatment. Specifically, cDCE removal rates were four to six times higher in heated than unheated bioaugmented microcosms. This study confirms the need for bioaugmentation following a laboratory thermal treatment to obtain complete dechlorination of TCE.     

Batch-test study on the dechlorination of 1,1,1-trichloroethane in contaminated aquifer material by zero-valent iron

Chlorinated aliphatic hydrocarbons are common groundwater contaminants. One possible remediation option is in-situ reductive dechlorination by zero-valent iron, either by direct injection or as reactive barriers. Chlorinated ethenes (tetrachloroethene: PCE; trichloroethene: TCE) have received extensive attention in this context. However, another common groundwater pollutant, 1,1,1-trichlorethane (TCA), has attracted much less attention. We studied TCA reduction by three types of granular zero-valent irons in a series of batch experiments using polluted groundwater, with and without added aquifer material. Two types of iron were able to reduce TCA completely with no daughter product concentration increases (1,1-dichloroethane: DCA; chloroethane: CA). One type of iron showed slower reduction, with intermediate rise of DCA and CA concentrations. When evaluating the formation of daughter products, the tests on the groundwater alone showed different results than the groundwater plus aquifer batches: DCA did not temporarily accumulate in the batches with added aquifer material, contrary to the batches without added aquifer material. 1,1-dichloroethene (DCE, also present in the groundwater as an abiotic degradation product of TCA) was also reduced slower in the batches without added aquifer material than in the batches with aquifer material. Redox potentials gradually decreased to low values in batches with aquifer material without iron, while the batches with groundwater alone maintained a constant higher redox potential. Either adsorption processes or microbiological activity in the samples could explain these phenomena. Polymerase Chain Reaction (PCR: a targeted gene probe technique) for chlorinated aliphatic compound (CAH)-degrading bacteria confirmed the presence of Dehalococcoides sp. (chloroethene-degraders) but was negative for Desulfobacterium autotrophicum (a known co-metabolic TCA degrader). DCA reduction was rate determining: first-order half-lives of 300-350 h were observed. TCA was fully removed within hours. CA is resistant to reduction by zero-valent iron but it is known to hydrolyze easily. Since CA did not accumulate in our batches, it may have disappeared by the latter mechanism or it may not have formed as a major daughter product.