DTU Environment (Department of Environmental Engineering, Technical University of Denmark), Miljoevej bldn 113, DK-2800 Lyngby, Denmark.
J Contam Hydrol. 2013 Mar;146:37-50. doi: 10.1016/j.jconhyd.2012.11.010. Epub 2012 Dec 30.
The degradation of chlorinated ethenes and ethanes in clay till was investigated at a contaminated site (Vadsby, Denmark) by high resolution sampling of intact cores combined with groundwater sampling. Over decades of contamination, bioactive zones with degradation of trichloroethene (TCE) and 1,1,1-trichloroethane (1,1,1-TCA) to 1,2-cis-dichloroethene (cis-DCE) and 1,1-dichloroethane, respectively, had developed in most of the clay till matrix. Dehalobacter dominated over Dehalococcoides (Dhc) in the clay till matrix corresponding with stagnation of sequential dechlorination at cis-DCE. Sporadically distributed bioactive zones with partial degradation to ethene were identified in the clay till matrix (thickness from 0.10 to 0.22 m). In one sub-section profile the presence of Dhc with the vcrA gene supported the occurrence of degradation of cis-DCE and VC, and in another enriched δ(13)C for TCE, cis-DCE and VC documented degradation. Highly enriched δ(13)C for 1,1,1-TCA (25‰) and cis-DCE (-4‰) suggested the occurrence of abiotic degradation in a third sub-section profile. Due to fine scale heterogeneity the identification of active degradation zones in the clay till matrix depended on high resolution subsampling of the clay till cores. The study demonstrates that an integrated approach combining chemical analysis, molecular microbial tools and compound specific isotope analysis (CSIA) was required in order to document biotic and abiotic degradations in the clay till system.
在丹麦 Vadsby 的一个污染场地,通过完整岩芯的高分辨率取样和地下水取样,研究了氯代乙烷和乙烷在粘土地层中的降解情况。在几十年的污染过程中,生物活性区已在大部分粘土地层基质中形成,其中三氯乙烯(TCE)和 1,1,1-三氯乙烷(1,1,1-TCA)分别降解为 1,2-顺式二氯乙烯(cis-DCE)和 1,1-二氯乙烷。在粘土地层基质中,优势菌为脱硫杆菌属(Dehalobacter),而非脱硫八叠球菌属(Dhc),这与 cis-DCE 连续脱氯停滞相对应。在粘土地层基质中(厚度为 0.10 至 0.22 米),偶尔会发现部分降解为乙烯的生物活性区。在一个子剖面中,存在携带 vcrA 基因的 Dhc,支持 cis-DCE 和 VC 的降解,而另一个子剖面中 TCE、cis-DCE 和 VC 的 δ13C 富集则记录了降解作用。1,1,1-TCA(25‰)和 cis-DCE(-4‰)的高 δ13C 富集表明,在第三个子剖面中发生了非生物降解。由于细尺度的非均质性,粘土地层基质中活性降解区的识别取决于粘土地层岩芯的高分辨率亚采样。该研究表明,为了记录粘土地层系统中的生物和非生物降解,需要结合化学分析、分子微生物工具和化合物特异性同位素分析(CSIA)等综合方法。