Mercury distribution in the surface soil of China is potentially driven by precipitation, vegetation cover and organic matter

被引:10
|
作者
Zhang, Zhao-Yang [1 ,3 ]
Li, Gang [2 ]
Yang, Lei [1 ]
Wang, Xin-Jun [4 ]
Sun, Guo-Xin [1 ,3 ]
机构
[1] Chinese Acad Sci, Res Ctr Ecoenvironm Sci, State Key Lab Urban & Reg Ecol, Beijing 100085, Peoples R China
[2] Chinese Acad Sci, Inst Urban Environm, Key Lab Urban Environm & Hlth, Xiamen 361021, Peoples R China
[3] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[4] China Acad Transportat Sci, Res Ctr Environm Protect & Water & Soil Conservat, 240 Huixinli, Beijing 100029, Peoples R China
关键词
Soil mercury distribution; Wet and dry deposition; Vegetation cover; Emissions; Soil organic matter; Solar radiation; GASEOUS ELEMENTAL MERCURY; TERRESTRIAL BACKGROUND SURFACES; REMOTE UPLAND FOREST; ATMOSPHERIC MERCURY; WET DEPOSITION; AIR/SURFACE EXCHANGE; NATURAL SURFACES; TIBETAN PLATEAU; METHYL MERCURY; NATURE-RESERVE;
D O I
10.1186/s12302-020-00370-1
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Background Understanding the mechanism of Hg accumulation in soil, which is a net Hg sink, at a national scale is important for protecting the environment and improving food safety. The mercury (Hg) distribution in surface soil in China is quite uneven, with relatively high concentrations in southeastern China and low concentrations in northwestern China. The reason for this distribution is inconclusive, especially at the continental scale. In this study, the relative contributions of the key impact factors, including dry and wet deposition, soil organic matter (SOM) and solar radiation to soil Hg, were evaluated. Results Wet and dry deposition associated with precipitation and vegetation cover and emissions influenced by SOM are key factors controlling Hg distribution in surface soil. In southeastern China, high levels of wet deposition associated with the South Asia monsoon and dry deposition, enhanced by vegetation canopies, together with low levels of emissions caused by highly vegetated surfaces and solar radiation, are responsible for the high Hg levels in soil (> 0.08 mg/kg). In northeastern China, moderate levels of wet Hg deposition, high levels of dry deposition via throughfall and litterfall, low emissions due to weak solar radiation and high levels of SOM are responsible for high Hg accumulation in soil. In northwestern China, low levels of wet deposition, together with high emissions levels, low vegetation cover (bare soil) and SOM and strong solar radiation, contributed to the low Hg level in the surface soil (< 0.03 mg/kg). Conclusions We suggest that wet deposition derived from the Asian monsoon, dry deposition linked to vegetated surfaces and Hg emissions associated with vegetation cover, SOM and solar radiation play key roles in the soil Hg level in China. In other terrestrial environments worldwide, especially in regions with significantly high levels of wet deposition and high amounts of vegetation cover and soil SOM, high Hg concentrations may exist in the surface soil.
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页数:10
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