颗粒组成,营养含量和度决定了不同土地使用类型盐性土壤中的有机碳变化
Wei Zhang1, Tiejun Song1, Weihong Dong1
1Key Laboratory of Groundwater Resources and Environment (Jilin University), Ministry of Education, Changchun, 130021, China; Jilin Provincial Key Laboratory of Water Resources and Water Environment, Jilin University, Changchun, 130021, China.
Journal of environmental management
|October 10, 2025
概括
土地利用变化对盐地区的土壤有机碳 (SOC) 有影响. 降低土壤性,增加营养素和细颗粒可增强SOC储存,改善土地.
科学领域:
- 土壤科学 土壤科学
- 环境科学 环境科学
- 农业学是一种农业学.
背景情况:
- 土地利用变化显著影响土壤特性,包括营养含量,盐度,度,颗粒成分和土壤有机碳 (SOC).
- 虽然SOC动态得到了广泛的研究,但在土地使用变化下,它们在盐性性土壤中的行为仍然不太了解.
研究的目的:
- 调查土地利用变化 (田,干田,草原) 如何影响西宁平原的土壤特性和SOC含量.
- 确定驱动这些盐土壤中SOC动态的关键因素和机制.
主要方法:
- 在不同土地用途中对土壤总 (TN),总 (TP),C/N比,pH,电导率 (EC),颗粒成分和SOC含量进行比较分析.
- 包括相关性,随机森林和变异分区在内的统计分析被用来确定关系和影响因素.
主要成果:
- 与草原相比,大米田的SOC,TN,TP,EC和泥含量较高;干旱田的差异很小.
- SOC含量与土壤pH值和沙含量有负相关性,但与TN,TP,粘土和泥含量有正相关性.
- 土壤TN,TP,泥含量,沙含量和pH被确定为SOC含量的最有影响力的预测因素.
结论:
- 土壤营养含量和颗粒组成之间的相互作用,以及营养含量本身,显著推动了SOC的变化.
- 降低土壤度和增加土壤营养素和细颗粒含量是提高盐土壤碳沉积能力的关键策略.
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