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14C戊唑醇在哥伦比亚土壤中的降解

14C tebuconazole degradation in Colombian soils.

作者信息

Mosquera C S, Martínez M J, Guerrero J A

机构信息

Universidad Nacional de Colombia, Facultad de Ciencias. Dpto Química, Colombia.

出版信息

Commun Agric Appl Biol Sci. 2010;75(2):173-81.

PMID:21542480
Abstract

Tebuconazole is a fungicide used on onion crops (Allium Fistulosum L) in Colombia. Persistence of pesticides in soils is characterized by the half-life (DT50), which is influenced by their chemical structure, the physical and chemical properties of the soil and the previous soil history. Based on its structural and chemical properties, tebuconazole should be expected to be relatively persistent in soils. Laboratory incubation studies were conducted to evaluate persistence and bond residues of 14C tebuconazole in three soils, two inceptisol (I) and one histosol (H). Textural classifications were: loam (101), loamy sand (102) and loam (H03), respectively. Data obtained followed a first-order degradation kinetics (R2 > or = 0.899) with DT50 values between 158 and 198 days. The production of 14CO2 from the 14C-ring-labelled test chemicals was very low and increased slightly during 63 days in all cases. The methanol extractable 14C-residues were higher than aqueous ones and both decreased over incubation time for the three soils. The formation of bound 14C-residues increased with time and final values were 11.3; 5.55 and 7.87% for 101, 102 and H03 respectively. Soil 101 showed the lowest mineralization rate and the highest bound residues formation, which might be explained by the clay fraction content. In contrast, an inverse behavior was found for soils 102 and H03, these results might be explained by the higher soil organic carbon content.

摘要

戊唑醇是一种用于哥伦比亚洋葱作物(葱)的杀菌剂。农药在土壤中的持久性以半衰期(DT50)为特征,其受农药化学结构、土壤理化性质及土壤既往历史的影响。基于其结构和化学性质,预计戊唑醇在土壤中相对持久。开展了实验室培养研究,以评估14C标记的戊唑醇在三种土壤中的持久性和结合残留,其中两种是始成土(I),一种是有机土(H)。质地分类分别为:壤土(101)、壤质砂土(102)和壤土(H03)。获得的数据符合一级降解动力学(R2≥0.899),DT50值在158至198天之间。在所有情况下,14C环标记测试化学品产生的14CO2非常低,且在63天内略有增加。甲醇可提取的14C残留量高于水提取的残留量,且在三种土壤的培养过程中均随时间减少。结合14C残留量随时间增加,101、102和H03的最终值分别为11.3%、5.55%和7.87%。土壤101的矿化率最低,结合残留量形成最高,这可能由粘粒含量来解释。相反,在土壤102和H03中发现了相反的情况,这些结果可能由较高的土壤有机碳含量来解释。

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