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Fei Xu1, Peiyue Li1, Qiang He1

  • 1School of Water and Environment, Chang'an University, No. 126 Yanta Road, Xi'an 710054, Shaanxi, China; Key Laboratory of Subsurface Hydrology and Ecological Effects in Arid Region of the Ministry of Education, Chang'an University, No. 126 Yanta Road, Xi'an 710054, Shaanxi, China; Key Laboratory of Eco-hydrology and Water Security in Arid and Semi-arid Regions of the Ministry of Water Resources, Chang'an University, No. 126 Yanta Road, Xi'an 710054, Shaanxi, China.

概括

地下水位的变化显著影响土壤中的铁和 (Fe/Mn) 形式. 氧化物结合的Fe/Mn增加了氧化条件,而氧化还原过程驱动了Fe/Mn循环,影响了污染物的流动性.