Vonberg David, Hofmann Diana, Vanderborght Jan, Lelickens Anna, Köppchen Stephan, Pütz Thomas, Burauel Peter, Vereecken Harry
J Environ Qual. 2014 Jul;43(4):1450-9. doi: 10.2134/jeq2013.12.0497.
Atrazine (2-chloro-4-ethylamino-6-isopropylamino-1,3,5-triazine) groundwater monitoring in the Zwischenscholle aquifer in western Germany revealed concentrations exceeding the threshold value of 0.1 μg L and increasing concentration trends even 20 yr after its ban. Accordingly, the hypothesis was raised that a continued release of bound atrazine residues from the soil into the Zwischenscholle aquifer in combination with the low atrazine degradation in groundwater contributes to elevated atrazine in groundwater. Three soil cores reaching down to the groundwater table were taken from an agricultural field where atrazine had been applied before its ban in 1991. Atrazine residues were extracted from eight soil layers down to 300 cm using accelerated solvent extraction and analyzed using liquid chromatography-tandem mass spectrometry. Extracted atrazine concentrations ranged between 0.2 and 0.01 μg kg for topsoil and subsoil, respectively. The extracted mass from the soil profiles represented 0.07% of the applied mass, with 0.01% remaining in the top layer. A complete and instantaneous remobilization of atrazine residues and vertical mixing with the groundwater body below would lead to atrazine groundwater concentrations of 0.068 μg L. Considering the area where atrazine was applied in the region and assuming instantaneous lateral mixing in the Zwischenscholle aquifer would result in a mean groundwater concentration of 0.002 μg L. A conservative estimation suggests an atrazine half-life value of about 2 yr for the soil zone, which significantly exceeds highest atrazine half-lives found in the literature (433 d for subsurface soils). The long-term environmental behavior of atrazine and its metabolites thus needs to be reconsidered.
在德国西部的Zwischenscholle含水层中对莠去津(2-氯-4-乙氨基-6-异丙氨基-1,3,5-三嗪)进行的地下水监测显示,其浓度超过了0.1微克/升的阈值,甚至在其被禁用20年后浓度仍呈上升趋势。因此,有人提出这样的假设:土壤中结合态莠去津残留持续释放到Zwischenscholle含水层中,再加上地下水中莠去津降解缓慢,导致了地下水中莠去津含量升高。从一片1991年莠去津被禁用之前曾施用该除草剂的农田中,采集了三个直达地下水位的土壤岩芯。采用加速溶剂萃取法从八个深度达300厘米的土壤层中提取莠去津残留,并使用液相色谱-串联质谱法进行分析。表层土壤和下层土壤中提取的莠去津浓度分别在0.2至0.01微克/千克之间。从土壤剖面中提取的质量占施用质量的0.07%,其中0.01%残留在表层。莠去津残留的完全且即时的再迁移以及与下方地下水体的垂直混合,将导致地下水中莠去津浓度达到0.068微克/升。考虑到该地区施用莠去津的面积,并假设在Zwischenscholle含水层中即时进行横向混合,将导致平均地下水浓度为0.002微克/升。保守估计表明,土壤层中莠去津的半衰期约为2年,这大大超过了文献中报道的最高莠去津半衰期(地下土壤为433天)。因此,需要重新考虑莠去津及其代谢物的长期环境行为。