首页> 外文期刊>Chemosphere >Study Of The Spatial Variation Of The Biodegradation Rate Of The Herbicide Bentazone With Soil Depth Using Contrasting Incubation Methods
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Study Of The Spatial Variation Of The Biodegradation Rate Of The Herbicide Bentazone With Soil Depth Using Contrasting Incubation Methods

机译:对比孵化法研究除草剂五氮酮生物降解率随土壤深度的空间变异。

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Vertical and horizontal spatial variability in the biodegradation of the herbicide bentazone was compared in sandy-loam soil from an agricultural field using sieved soil and intact soil cores. An initial experiment compared degradation at five depths between 0 and 80cm using sieved soil. Degradation was shown to follow the first-order kinetics, and time to 50% degradation (DT_(50)). declined progressively with soil depth from 56d at 0-10cm to 520d at 70-80 cm. DT_(50) was significantly correlated with organic matter, pH and dehydrogenase activity. In a subsequent experiment, degradation rate was compared after 127 d in sieved soil and intact cores from 0 to 10 and 50 to 60 cm depth from 10 locations across a 160 × 90 m portion of the field. Method of incubation significantly affected mean dissipation rate, although there were relatively small differences in the amount of pesticide remaining in intact cores and sieved soil, accounting for between 4.6% and 10.6% of that added. Spatial variability in degradation rate was higher in soil from 0 to 10cm depth relative to that from 50 and 60cm depth in both sieved soil and intact core assessments. Patterns of spatial variability measured using cores and sieved soil were similar at 50-60cm, but not at 0-10cm depth. This could reflect loss of environmental context following processing of sieved soil. In particular, moisture content, which was controlled in sieved soil, was found to be variable in cores, and was significantly correlated with degradation rate in intact topsoil cores from 0 to 10 cm depth.
机译:使用筛分的土壤和完整的土壤核心,比较了农田的沙壤土中除草剂苯达松生物降解的垂直和水平空间变异性。初步实验比较了使用筛分土壤在0至80厘米之间的五个深度处的降解情况。降解遵循一级动力学,降解时间达到50%(DT_(50))。土层深度从0-10cm处的56d逐渐减小到70-80cm处的520d。 DT_(50)与有机质,pH和脱氢酶活性显着相关。在随后的实验中,比较了127天后在160×90 m区域内10个位置的0到10和50到60 cm深度的完整岩心中的降解速率。孵化方法显着影响平均耗散率,尽管完整芯和筛分土壤中残留的农药量差异较小,占添加量的4.6%至10.6%。在0至10cm深度的土壤中,降解速度的空间变异性高于筛分土壤和完整岩心评估中50cm和60cm深度的土壤降解速度。使用岩心和筛分土壤测得的空间变异性模式在50-60cm处相似,但在0-10cm深度处不相似。这可能反映了经过筛分的土壤处理后环境环境的损失。特别是,在筛分土壤中控制的水分含量在岩心中是可变的,并且与完整的表土从0至10 cm深度的降解速率显着相关。

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