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生物固体改良土壤中三氯生的生物降解。

Biodegradation of triclosan in biosolids-amended soils.

机构信息

Soil and Water Science Department, University of Florida, Gainesville, Florida, USA.

出版信息

Environ Toxicol Chem. 2011 Nov;30(11):2488-96. doi: 10.1002/etc.666. Epub 2011 Sep 23.

Abstract

Land application of biosolids can constitute an important source of triclosan (TCS) input to soils, with uncertain effects. Several studies have investigated the degradation potential of TCS in biosolids-amended soils, but the results vary widely. We conducted a laboratory degradation study by mixing biosolids spiked with [¹⁴C]-TCS (final concentration = 40 mg/kg) with Immokalee fine sand and Ashkum silty clay loam soils at an agronomic application rate (22 Mg/ha). Biosolids-amended soils were aerobically incubated in biotic and inhibited conditions for 18 weeks. Subsamples removed at 0, 2, 4, 6, 9, 12, 15, and 18 weeks were sequentially extracted with an operationally defined extraction scheme to determine labile and nonlabile TCS fractions. Over the 18-week incubation, the proportion of [¹⁴C] in the nonlabile fraction increased and the labile fraction decreased, suggesting decreasing availability to biota. Partitioning of TCS into labile and nonlabile fractions depended on soil characteristics. Less than 0.5% of [¹⁴C]-TCS was mineralized to carbon dioxide (¹⁴CO₂) in both soils and all treatments. A degradation metabolite, methyl triclosan (Me-TCS), was identified in both soils only in the biotic treatment, and increased in concentration over time. Even under biotic conditions, biosolids-borne TCS is persistent, with a primary degradation (TCS to Me-TCS) half-life of 78 d in the silty clay loam and 421 d in the fine sand. A half-life of approximately 100 d would be a conservative first approximation of TCS half-life in biosolids-amended soils for risk estimation.

摘要

土地施用生物固体可能是三氯生(TCS)输入土壤的一个重要来源,其影响不确定。已有几项研究调查了 TCS 在生物固体-改良土壤中的降解潜力,但结果差异很大。我们通过将含有[¹⁴C]-TCS(最终浓度=40mg/kg)的生物固体与伊莫卡莱细砂和阿什库姆粉质粘壤土混合,在农业应用率(22 Mg/公顷)下进行了实验室降解研究。生物固体-改良土壤在有氧条件下在生物和抑制条件下培养 18 周。在 0、2、4、6、9、12、15 和 18 周时取出亚样品,用操作定义的提取方案依次提取,以确定易变和非易变的 TCS 分数。在 18 周的培养过程中,非易变部分中的[¹⁴C]比例增加,易变部分减少,表明生物利用度降低。TCS 分为易变和非易变部分取决于土壤特性。在两种土壤和所有处理中,不到 0.5%的[¹⁴C]-TCS 矿化为二氧化碳(¹⁴CO₂)。只有在生物处理中,在两种土壤中都鉴定出 TCS 的降解代谢物,甲基三氯生(Me-TCS),并且随着时间的推移浓度增加。即使在生物条件下,生物固体携带的 TCS 也具有持久性,在粉质粘壤土中的主要降解(TCS 到 Me-TCS)半衰期为 78d,在细砂中的半衰期为 421d。约 100d 的半衰期将是 TCS 在生物固体-改良土壤中用于风险估计的半衰期的保守初步近似值。

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