Adsorption Characteristics and the Effect of Dissolved Organic Matter on Mercury(II) Adsorption of Various Soils in China |
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| Authors: | Fan Wu Hui Liu Mengmeng Zhang Wen Ma Xianmin Huang Shuwei Liu |
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| Affiliation: | 1. Environment Research Institute, Shandong University, Jinan, China;2. Shandong Analysis and Test Center, Shandong Academy of Sciences, Jinan, China;3. Shandong Agricultural Environmental Protection and Rural Energy Station, Jinan, China;4. College of Life Science, Shandong University, Jinan, China |
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| Abstract: | To evaluate the adsorption characteristics and effects of dissolved organic matter (DOM) from wheat straw (DOMW) and swine manure (DOMS) on mercury [Hg(II)] adsorption by soils, a series of experiments was conducted on 26 soils with different soil properties.Results showed that the values of Kd (a solid–liquid partition coefficient) of soils varied within a range of 0.768–14.386 L g?1. Kd values were mainly controlled by soil organic matter (SOM), cation exchange capacity (CEC), soil nitrogen (N), and soil sulfur (S). When DOMW and DOMS were added to the soil samples, the amount of Hg(II) adsorbed by the soils decreased significantly. Furthermore, based on the decreased percentage of adsorption of Hg(II) by soil upon adding DOMW (PDOMW) or DOMS (PDOMS), about 73.08% soils, the values of PDOMS were smaller than those of PDOMW. The PDOMW values were related to SOM, pH, free Fe oxide content, and CEC, whereas PDOMS values were related to soil free Fe/Al oxide contents. Therefore, we should pay more attention about mercury risk caused by the addition of exogenous organic matter in soils, especially for the soils with low or high pH, less SOM, low CEC, and less free Fe/Al oxide. |
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| Keywords: | Distribution coefficient soil properties sorption fate various soils |
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