So the dissimilatory Fe (III) reduction has important geological and environmental significance because this process can relate with the organic metabolize and volatile element form translation.

 
  • 因而,异化铁还原过程将有效的与土壤中有机质代谢、变价元素的形态转化过程相偶连,所以其具有重要的地学和环境意义。
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