铁酸盐上的氧气空隙促进了由草衍生的分解溶解有机物质的表面聚合:对土壤碳封存的影响
Yu Huang1, Shoupeng Li1,2, Ke Song3
1School of Environmental Science and Engineering, Guangdong University of Technology, Guangzhou 510006, China.
Environmental science & technology
|August 7, 2025
概括
铁酸盐中的矿物质缺陷激活了有机物分解中的自由基,在无氧条件下增强了碳稳定性. 这揭示了土壤有机碳捕获的新途径.
科学领域:
- 环境化学环境化学
- 土壤科学 土壤科学
- 地质化学 地质化学
背景情况:
- 土壤有机物 (SOM) 对于碳循环至关重要,并与矿物相互作用.
- 了解氧物种和矿物质缺陷如何在无氧条件下影响SOM转换是有限的.
研究的目的:
- 在无毒条件下研究分解的米溶解有机物 (DOM) 和铁 (Fh) 之间的分子级相互作用.
- 阐明矿物质缺陷在SOM激活和转化中的作用.
主要方法:
- 在各种分解阶段从大米中提取DOM.
- 无氧和有氧批量实验与铁化物.
- SUVA254测量用于DOM移除.
- 里叶变换离子循环子共振质谱 (FTICR-MS) 用于分子分析.
主要成果:
- 更分解的DOM在无氧和氧条件下显示出更高的去除率.
- 铁酸盐空缺缺陷激活了DOM中的持久性自由基.
- 自由基反应导致了通过基转换和希夫基形成的宏分子聚合物形成.
结论:
- 矿物质缺陷显著调节氧化还原活性有机物转化.
- 铁化物诱导的自由基反应聚合DOM,稳定土壤有机碳.
- 这些发现为外源性有机物分解和碳封存提供了分子层面的见解.
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