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中国西南两个喀斯特流域九种微量元素的质量平衡。

Mass balance of nine trace elements in two karst catchments in southwest China.

机构信息

State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China; University of Chinese Academy of Sciences, Beijing 100049, China.

State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China; CAS Centre for Excellence in Quaternary Science and Global Change, Xi'an 710061, China.

出版信息

Sci Total Environ. 2021 Sep 10;786:147504. doi: 10.1016/j.scitotenv.2021.147504. Epub 2021 May 4.

DOI:10.1016/j.scitotenv.2021.147504
PMID:33975112
Abstract

High geological background levels of trace elements (TEs) and high population density in the karst areas of southwest China have imposed environmental pressure on the fragile ecosystems in this region. Understanding the mass budget of TEs, especially the toxic ones, is of great importance to sustain future developments. This study investigates the mass balance and fate of nine TEs (cadmium, arsenic, lead, chromium, copper, nickel, zinc, thallium, and antimony) in two karst catchments (Huilong and Chenqi) in southwest China through estimation of their mass budgets in throughfall, open field precipitation, total suspended particulate matter (TSP), litterfall, fertilization, harvested crops, surface runoff, and underground runoff. The estimated net fluxes are positive, indicating a source region, for four elements (Cu, Cr, Ni, and Tl) and negative, indicating a sink region, for five elements (As, Cd, Pb, Sb, and Zn) in both catchments. The net fluxes for the nine elements in Chenqi catchment are within a relatively small range (2.6, 2.0, 1.6, 0.6, -0.05, -0.5, -0.5, -2.9, and -3.3 mg m yr for Cu, Ni, Cr, Tl, Cd, Zn, Sb, Pb, and As, respectively), but in Huilong catchment in quite a large range (15.5, 6.0, 1.0, 0.8, -0.3, -0.9, -4.5, -7.5, and -8.7 mg m yr for Tl, Cr, Ni, Cu, Cd, Sb, As, Pb, and Zn, respectively). Rainfall (12.3%-66.2%) and litterfall (18.4%-81.3%) are the major input flux pathways, while crops harvest (16%-99%) is the major output flux pathway for the TEs in both catchments, indicating that the fate of TEs is shaped by both natural factors such as precipitation and litterfall and human activities such as fertilization and crop harvesting in these forestland-farmland compound karst catchments. Results from this study suggest that restoring forests from low-yield sloping farmlands will be useful for controlling TEs pollution in these fragile karst regions with high geological background TEs.

摘要

在中国西南部的喀斯特地区,由于地质背景中微量元素(TEs)含量高且人口密度大,这对该地区脆弱的生态系统造成了环境压力。了解 TEs 的物质收支情况,尤其是有毒 TEs 的物质收支情况,对于维持未来的发展至关重要。本研究通过估算两种喀斯特集水区(回龙和陈旗)中 TEs 的物质收支情况,即穿透雨、开阔场地降水、总悬浮颗粒物(TSP)、凋落物、施肥、收获作物、地表径流和地下径流中的 TEs 质量平衡,研究了 9 种 TEs(镉、砷、铅、铬、铜、镍、锌、铊和锑)的物质平衡和归宿。估计的净通量为正,表明两个集水区的四个元素(Cu、Cr、Ni 和 Tl)为源区,而五个元素(As、Cd、Pb、Sb 和 Zn)为汇区。陈旗集水区 9 种元素的净通量范围较小(Cu、Ni、Cr、Tl、Cd、Zn、Sb、Pb 和 As 的净通量分别为 2.6、2.0、1.6、0.6、-0.05、-0.5、-0.5、-2.9 和-3.3mg m yr),但在回龙集水区的净通量范围较大(Tl、Cr、Ni、Cu、Cd、Sb、As、Pb 和 Zn 的净通量分别为 15.5、6.0、1.0、0.8、-0.3、-0.9、-4.5、-7.5 和-8.7mg m yr)。降雨(12.3%-66.2%)和凋落物(18.4%-81.3%)是主要的输入通量途径,而作物收获(16%-99%)是两种集水区中 TEs 的主要输出通量途径,这表明 TEs 的归宿既受降水和凋落物等自然因素的影响,也受施肥和作物收获等人类活动的影响。本研究结果表明,在这些地质背景 TEs 含量高的脆弱喀斯特地区,从低产坡耕地恢复森林将有助于控制 TEs 污染。

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