Fate of the 14C-labeled herbicide prosulfocarb in a soil and in a sediment-water system

K. Braun, Ann-Katrin Luks, B. Schmidt
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引用次数: 9

Abstract

ABSTRACT The fate of 14C-labeled herbicide prosulfocarb was studied in an agricultural soil and in a sediment-water system, the sediment part of which was derived from Yangtze Three Gorges Reservoir, China. Time-course studies were performed for 28 d and 49 d, respectively. Main transformation routes of 14C-prosulfocarb were mineralization to 14CO2 and formation of nonextractable residues amounting to 12.13% and 10.43%, respectively, after 28 days (soil), and 9.40% and 11.98%, respectively, after 49 d (sediment-water system). Traces of prosulfocarbsulfoxide were detected by means of TLC, HPLC, and LC-MS; other transformation products were not found. Initial extraction of soil assays using 0.01 M CaCl2 solution showed that the bioavailability of the herbicide was considerably low; immediately after application (0.1 d of incubation), only 4.78% of applied radioactivity were detected in this aqueous fraction. DT50 values of 14C-prosulfocarb estimated from radio-TLC and -HPLC analyses were above 28 d in soil and ranged between 29 d and 49 d in the sediment-water system. Partitioning of 14C from water to sediment phase occurred with DT50 slightly above 2 d. With regard to the sediment-water system, adsorption occurred with log Koc = 1.38 (calculated from 2 day assays) and 2.35 (49 d assays). As similarly estimated from portions of 14C found in CaCl2 extracts of the 0.1 d assays, 14C-prosulfocarb's log Koc in soil was 2.96. With both experiments, similar portions of nonextractable radioactivity were associated with all soil organic matter fractions, i.e. nonhumics, fulvic acids, humic acids, and humin/minerals. Throughout all sample preparation, the experiments were severely impaired by losses of radioactivity especially with concentration of samples containing water in vacuo. All findings pointed to volatility of parent prosulfocarb in presence of water rather than volatility of transformation products. According to literature data, this behavior of prosulfocarb was not expected, though volatility was demonstrated under field conditions.
14c标记除草剂灭硫威在土壤和沉积物-水系统中的命运
摘要研究了14c标记除草剂prosulfocarb在农业土壤和沉积物-水系统中的命运,其中沉积物部分来自长江三峡水库。分别进行28 d和49 d的时程研究。14c -原硫卡韦的主要转化途径是矿化成14CO2和形成不可提取残留物,28 d(土壤)和49 d(沉积物-水体系)分别占12.13%和10.43%和9.40%和11.98%。采用薄层色谱法、高效液相色谱法、质谱法检测了亚砜的痕量;未发现其他转化产品。用0.01 M CaCl2溶液对土壤进行初步提取,表明该除草剂的生物利用度较低;施用后立即(孵育0.1 d),仅在该水溶液组分中检测到所施用放射性的4.78%。放射性薄层色谱和高效液相色谱分析估计的14c -原硫威在土壤中的DT50值在28 d以上,在沉积物-水系统中的DT50值在29 - 49 d之间。当DT50略高于2 d时,14C从水到沉积物相发生了分配。对于沉积物-水系统,logkoc = 1.38(根据2天的分析计算)和2.35(根据49天的分析计算)发生了吸附。同样,从0.1 d试验的CaCl2提取物中发现的14C部分估计,土壤中14C-原硫威的对数Koc为2.96。在这两个实验中,不可提取放射性的相似部分与所有土壤有机质组分有关,即非腐植酸、黄腐酸、腐植酸和人敏/矿物质。在整个样品制备过程中,放射性损失严重损害了实验,特别是在真空中含有水的样品浓度。所有的研究结果都表明,在存在水的情况下,母体灭虫威的挥发性高于转化产物的挥发性。根据文献数据,尽管在现场条件下证明了挥发性,但灭虫威的这种行为是意料之外的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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