葡萄糖输入利土壤有机碳矿化和动态与改土壤相关的动态
Muhammad Junaid Nazir1, Muhammad Mahroz Hussain1, Gadah Albasher2
1School of Emergency Management, School of Environment and Safety Engineering, Jiangsu Province Engineering Research Center of Green Technology and Contingency Management for Emerging Pollutants, Jiangsu University, Zhenjiang, 212013, People's Republic of China.
将碳 (C) 添加到土壤中会刺激分解,但 (N) 的类型和数量会显著改变土壤有机碳 (SOC) 的稳定性. 尿素和硫酸盐治疗对葡萄糖添加产生了明显的反应,影响了SOC和的动态.
科学领域:
- 土壤科学 土壤科学
- 环境科学 环境科学
- 生物地质化学生物地质化学
背景情况:
- 外源碳输入显著影响土壤有机碳 (SOC) 分解,影响气候动态.
- 碳添加对SOC分解的影响由 (N) 类型和应用水平调节,但仍然不完全理解.
研究的目的:
- 研究葡萄糖 (一种易于获得的碳来源) 对SOC矿化和动态在不同类型 (酸,尿素,硫酸) 在不同水平 (高N,低N) 处理的土壤中的影响.
主要方法:
- 进行了一项化实验,使用处理了不同类型和水平的的土壤.
- 添加葡萄糖以评估其对土壤有机碳矿化,酸盐和的度,总含量和微生物生物质碳的影响.
主要成果:
- 添加葡萄糖增加了38%的SOC矿化 (高N) 和35% (低N).
- 的动态变化很大,NO3--N和NH4+-N度分别在高N和低N下受到抑制. 用尿素处理的土壤显示出更高的呼吸能力,而硫酸土壤则增加了总.
- 较高的含量似乎抑制了微生物的矿开采,可能提高了SOM的稳定性.
结论:
- 添加葡萄糖加快了尿素修改土壤中的SOC矿化,并增加了AS修改土壤中的总.
- 高含量通常会抑制碳释放,增加总含量,除了用葡萄糖处理的土壤外.
- 类型和应用水平是控制土壤有机碳稳定性的关键因素,以应对外源碳输入.
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