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环丙隆在中国土壤和沉积物中的降解与迁移。

The Degradation and Migration of Cyclanilide in Soil and Sediment in China.

机构信息

Nanjing Institute of Environmental Science, Key Laboratory of Pesticide Environmental Assessment and Pollution Control, Nanjing, 210042, China.

Nanjing Foreign Language School, Nanjing, 210008, China.

出版信息

Bull Environ Contam Toxicol. 2024 Oct 5;113(4):46. doi: 10.1007/s00128-024-03958-y.

Abstract

The environmental fate of a plant growth regulator cyclanilide was studied in this paper. The degradation, adsorption, and migration behaviors of cyclanilide were detailly measured in the laboratory. The results showed that the DT of cyclanilide degradation in the Jiangxi red, Taihu paddy, Changshu wushan, Shaanxi tide, and Dongbei black soils was 42.3 d, 31.9 d, 14.4 d, 30.4 d as well as 27.4 d under aerobic conditions and 32.3 d, 37.4 d, 29.3 d, 48.9 d as well as 27.0 d under water anaerobic conditions, respectively, with the main metabolite being 2,4-dichloroaniline (2,4-D). The DT of 2,4-D ranged from 5.26 to 27.1 days under aerobic conditions, and from 10.6 to 54.1 days under anaerobic conditions. The adsorption of cyclanilide by the soils was well fitted by the empirical linear adsorption isotherm, and the adsorption constant (K) values in the Jiangxi red, Taihu paddy, Changshu wushan, Shaanxi tide, and Dongbei black soils were 7.08, 4.49, 4.05, 3.20, and 1.41, respectively. The results of a mobility test showed that cyclanilide had strong mobility in the most test soils. Furthermore, soil pH is the dominant element affecting the adsorption of cyclanilide in the soils. Under aerobic environment, the DT of total cyclanilide in river and lake water-sediment systems were 30.7 d and 34.0 d, respectively; under anaerobic environment, their DT were 30.8 d and 31.4 d, respectively. In water-sediment systems, 2,4-D mainly exists in aqueous phase and the DT ranged from 5.23 to 8.76 days. This work demonstrated that cyclanilide has the potential risk to contaminate environment and attention should be paid to its application.

摘要

本文研究了植物生长调节剂环酰菌胺在环境中的归趋。在实验室中详细测量了环酰菌胺的降解、吸附和迁移行为。结果表明,在有氧条件下,环酰菌胺在江西红壤、太湖水稻土、常熟乌山、陕西潮土和东北黑土中的降解半衰期(DT)分别为 42.3、31.9、14.4、30.4 和 27.4d,在水厌氧条件下分别为 32.3、37.4、29.3、48.9 和 27.0d,主要代谢产物为 2,4-二氯苯胺(2,4-D)。在有氧条件下,2,4-D 的 DT 范围为 5.26-27.1d,在厌氧条件下为 10.6-54.1d。环酰菌胺在土壤中的吸附较好地符合经验线性吸附等温线,在江西红壤、太湖水稻土、常熟乌山、陕西潮土和东北黑土中的吸附常数(K)值分别为 7.08、4.49、4.05、3.20 和 1.41。迁移试验结果表明,环酰菌胺在大多数测试土壤中具有很强的迁移性。此外,土壤 pH 是影响土壤中环酰菌胺吸附的主导因素。在有氧环境下,河流和湖泊水-沉积物系统中环酰菌胺的总 DT 分别为 30.7d 和 34.0d;在厌氧环境下,其 DT 分别为 30.8d 和 31.4d。在水-沉积物系统中,2,4-D 主要存在于水相中,DT 范围为 5.23-8.76d。本研究表明,环酰菌胺具有污染环境的潜在风险,应注意其应用。

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