溶解有机物结构多样性和形式之间的相互作用在菌微生物影响下的基石灰尾矿中
Yunge Zhao1, Bin Zhu1, Minghao Cheng1
1Faculty of Environmental Science and Engineering, Kunming University of Science and Technology, Kunming 650500, China.
Journal of environmental sciences (China)
|November 2, 2025
概括
用真菌添加有机物质到 (PG) 中可以增加土壤的可用性. 溶解有机物 (DOM) 在这种转化中发挥着关键作用,改善土壤类基板,以可持续使用.
科学领域:
- 土壤科学 土壤科学
- 生物地质化学生物地质化学
- 环境化学环境化学
背景情况:
- 外源的有机输入影响土壤的动态.
- 溶解有机物 (DOM) 对于生物地化学过程至关重要.
- 在基石 (PG) 转化中DOM结构组成的作用尚不清楚.
研究的目的:
- 调查DOM结构组成与增强PG中的之间的相互作用.
- 评估真菌微生物和不同有机物应用对这种相互作用的影响.
- 了解基于PG的类似土壤基质中的转化.
主要方法:
- 用不同数量的外源有机物和不同的培养时间培养 (PG).
- 利用真菌微生物来促进土壤的形成.
- 分析溶解有机碳 (DOC) 度,化程度和分数 (可用的 (AP),微生物生物质 (MBP),活性池 (Active-P)).
主要成果:
- 外源有机物应用增加了PG基板中的DOC度和湿化.
- 类似蛋白质的成分 (C3) 显示出最初的增加,随后的下降.
- 观察到AP,MBP和Active-P显著增加,与DOC相关.
- 酸盐溶解的真菌促进了的分解和激活.
结论:
- 在增强基于PG的类似土壤基质中的可用性方面,DOM是一个关键因素.
- 菌活动增强了PG中的的转化和利用.
- 结果提供了对DOM生物地化学行为和PG利用的洞察力,用于可持续行业的发展.
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