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利用沉积物中的同位素铅和锶追踪渤海的自然和人为来源。

Using isotopic lead and strontium in sediments to trace natural and anthropogenic sources in the Bohai Sea.

作者信息

Zhang Shuaiya, Li Qinyue, Zou Yu, Liu Baolin, Yang Juan, Zheng Houyi, Liu Gege

机构信息

Key Laboratory of Polar Geology and Marine Mineral Resources, Ministry of Education, China University of Geosciences in Beijing, No. 29, Xueyuan Road, Beijing, 100083, China.

School of Ocean Sciences, China University of Geosciences in Beijing, No.29, Xueyuan Road, Beijing, 100083, China.

出版信息

Sci Rep. 2024 Dec 4;14(1):30267. doi: 10.1038/s41598-024-81493-w.

Abstract

The containment history in the coastal zone of the Bohai Sea has not been sufficiently traced because of the difficulty in identifying complex sources of pollutants. This study quantitatively identified various sources of Pb and Sr in two tidal flat sediment cores from Bohai Bay (core BB) and Liaodong Bay (core LB) based on their isotope ratios to trace the natural and anthropogenic disturbance history in the Bohai Sea. The results showed that natural inputs of Pb were the main sources for cores BB and LB; however, core LB was more influenced by anthropogenic inputs. Natural inputs were derived mainly from Chinese loess and Yellow River sediments, whereas anthropogenic sources were mainly a mixture of vehicular exhaust emissions before 2000 and coal combustion after 2000. Anthropogenic influence has declined since the late 1990s, especially in Bohai Bay, but has increased in Liaodong Bay from 1998 to 2006.

摘要

由于难以确定污染物的复杂来源,渤海海岸带的污染控制历史尚未得到充分追溯。本研究基于两个来自渤海湾(BB 岩芯)和辽东湾(LB 岩芯)的潮滩沉积物岩芯中铅和锶的同位素比值,定量识别了各种来源,以追溯渤海的自然和人为干扰历史。结果表明,铅的自然输入是 BB 岩芯和 LB 岩芯的主要来源;然而,LB 岩芯受人为输入的影响更大。自然输入主要来自中国黄土和黄河沉积物,而人为来源主要是 2000 年以前的汽车尾气排放和 2000 年以后的煤炭燃烧的混合物。自 20 世纪 90 年代末以来,人为影响有所下降,特别是在渤海湾,但在 1998 年至 2006 年期间,辽东湾的人为影响有所增加。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/aa40/11618753/065219e2fe74/41598_2024_81493_Fig1_HTML.jpg

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