Law Sheryl A, Bidleman Terry F, Martin Michael J, Ruby Michael V
Exponent, 15375 SE 30th Place, Suite 250, Bellevue, Washington 98007, USA.
Environ Sci Technol. 2004 Mar 15;38(6):1633-8. doi: 10.1021/es030508c.
In the fall of 2000, 34 groundwater samples were collected from beneath an active pesticide reformulating and packaging facility in coastal northeastern Florida to measure the enantiomer fractions (EFs) of alpha-hexachlorocyclohexane (alpha-HCH) as an indicator of biodegradation of this chlorinated pesticide in groundwater. Concentrations of alpha-HCH as high as 500 microg/L were observed beneath the historical source area and decreased with distance downgradient. Seventy-eight percent of the EF values were greater than 0.504 and ranged up to 0.890, indicating that the (-)-alpha-HCH enantiomer is preferentially degraded relative to the (+)-alpha-HCH enantiomer at this site. Samples taken from the groundwater that flows north from the historical disposal facility to a local discharge point at a creek did not indicate enantioselective degradation (EF values ranged from 0.495 to 0.512). The acidity (pH 3.7-4.6) and short flow path to the creek for this lobe of the groundwater plume likely preclude biodegradation of alpha-HCH. In contrast, the neutral lobe of the groundwater plume, which flows eastward from the historical source area, demonstrated enantioselective degradation (EF values ranged from 0.500 to 0.890 and increased with distance from the source area). Groundwater conditions beneath this portion of the site are conducive to biodegradation of HCH owing to anaerobic reducing conditions and lengthy travel times, and the chiral signatures for alpha-HCH provide evidence that biological degradation is occurring beneath this portion of the site.
2000年秋季,从佛罗里达州东北部沿海一家活跃的农药重新配方和包装工厂下方采集了34份地下水样本,以测量α-六氯环己烷(α-HCH)的对映体分数(EFs),作为该氯化农药在地下水中生物降解的指标。在历史源区下方观察到α-HCH浓度高达500微克/升,并随着下游距离的增加而降低。78%的EF值大于0.504,最高可达0.890,这表明在该地点,(-)-α-HCH对映体相对于(+)-α-HCH对映体优先降解。从历史处置设施向北流向小溪局部排放点的地下水中采集的样本未显示对映选择性降解(EF值范围为0.495至0.512)。该地下水羽流这一部分的酸性(pH值3.7 - 4.6)以及到小溪的短流动路径可能阻止了α-HCH的生物降解。相比之下,从历史源区向东流动的地下水羽流的中性部分表现出对映选择性降解(EF值范围为0.500至0.890,并随着与源区距离的增加而增加)。由于厌氧还原条件和较长的流动时间,该场地这一部分下方的地下水条件有利于六氯环己烷的生物降解,并且α-HCH的手性特征提供了证据,表明该场地这一部分下方正在发生生物降解。