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沉积物岩芯中来自东海沿海的滴滴涕和六氯环己烷。

DDTs and HCHs in sediment cores from the coastal East China Sea.

机构信息

State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China; State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China.

Research Centre for Toxic Compounds in the Environment, Masaryk University, Brno 62500, Czech Republic; Norwegian Institute for Water Research, Gaustadalleen 21, Oslo 0349, Norway.

出版信息

Sci Total Environ. 2016 Jan 1;539:388-394. doi: 10.1016/j.scitotenv.2015.09.010. Epub 2015 Sep 12.

Abstract

Four sediment cores were collected along the Yangtze-derived sediment transport pathway in the inner shelf of the East China Sea (ECS) for OCP analysis. The sediment records of HCHs and DDTs in estuarine environment reflected remobilization of chemicals from enhanced soil erosion associated to extreme flood events or large scale land use transformation. The sediment records in the open sea, instead, reflected long-term historical trends of OCP application in the source region. Unlike the so-called mud wedge distribution of sediment, inventories of HCHs and DDTs slightly increased from the mouth of Yangtze River alongshore toward south, suggesting the sediment deposition rate was one of factors on the exposure of chemicals within the inner shelf of the ECS. Re-suspension and transport of the Yangtze-derived sediment and consequent fractionation in grain size and TOC were also responsible for the spatial variation of inventories of catchment derived OCPs in a major repository area of the Yangtze suspended sediment. The total burdens of HCHs and DDTs in the inner shelf of the ECS were 35tons and 110tons, respectively. After 1983 (year of the official ban in China), those values were 13tons and 50tons, respectively. It appears that the Yangtze still delivers relatively high inputs of DDTs more than 30years after the official ban. High proportions of DDD+DDE and β-HCH suggested those OCPs mainly originated from historical usage in the catchment recent years.

摘要

四个沉积物岩芯沿长江在东海(ECS)的内架上采集,用于 OCP 分析。河口环境中 HCHs 和 DDTs 的沉积物记录反映了与极端洪水事件或大规模土地利用转化相关的增强土壤侵蚀中化学物质的再迁移。而开阔海域的沉积物记录则反映了 OCP 在源区的长期历史应用趋势。与所谓的沉积物泥楔分布不同,HCHs 和 DDTs 的储量从长江口沿海南下略有增加,这表明沉积速率是 ECS 内架内化学物质暴露的因素之一。长江沉积物的再悬浮和输运以及随后的粒度和 TOC 分馏也是导致长江悬浮泥沙主要储存区流域衍生 OCP 储量空间变化的原因之一。ECS 内架的 HCHs 和 DDTs 的总负荷分别为 35 吨和 110 吨。1983 年(中国官方禁止使用的年份)之后,这些数值分别为 13 吨和 50 吨。似乎在官方禁令发布 30 多年后,长江仍在输送相对较高的滴滴涕输入。DDD+DDE 和 β-HCH 的高比例表明,这些 OCP 主要来自流域近年来的历史使用。

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