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Updated: Feb 25, 2026

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渐进的溶解氧变化通过促进基基生成来增强2,4-二二衰减:实验演示和动力热力学视角

Jingyi Zhang1, Wenfeng Huang1, Jun Liang1

  • 1School of Environmental Science and Engineering, Shanghai Jiao Tong University, Shanghai 200240, China.

Environmental science & technology
|February 24, 2026
PubMed
概括

土壤中氧气的逐渐变化通过促进基生成,显著提高了2,4-二二 (2,4-DCP) 的分解. 这与急剧的氧气转移形成鲜明对比,突出了自然污染物减弱的新途径.

关键词:
2,4-DCP的转换方式溶解的氧气是一种溶解氧气.基基是基基的重要组成部分.氧化还原波动的波动.土壤 铁矿物质 土壤 铁矿物质

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