在中国西北的塔林河流域土壤盐度的主要驱动因素不同
Yuanli Qin1, Honghong Ma1, Chengrui Wang2
1Institute of Geophysical & Geochemical Exploration, Chinese Academy of Geological Sciences, Langfang, 065000, China; Key Laboratory of Geochemical Cycling of Carbon and Mercury in the Earth's Critical Zone, Institute of Geophysical & Geochemical Exploration, Chinese Academy of Geological Sciences, Langfang, 065000, China; Research Center of Geochemical Survey and Assessment on Land Quality, China Geological Survey, Langfang, 065000, China.
Journal of environmental management
|February 1, 2026
概括
塔林河流域的土壤盐化在空间上是异质的,向东南增加. 诸如蒸发转化,土地利用和土壤特性等关键驱动因素的相互作用复杂,影响农业的可持续性.
科学领域:
- 环境科学 环境科学
- 土壤科学 土壤科学
- 农业科学 农业科学
背景情况:
- 土壤盐化对全球农业和粮食安全构成重大威胁.
- 了解土壤盐度动态对于影响地区有效的土地管理至关重要.
研究的目的:
- 确定推动塔林河流域 (TRB) 土壤盐化的主要因素.
- 量化土壤盐度和环境变量之间的相互作用和因果关系.
主要方法:
- 机器学习模型被用来分析盐化数据.
- 谢普利添加式解释 (SHAP) 量化变量相互作用.
- 结构方程建模 (SEM) 分析了因果关系.
主要成果:
- 观察到土壤盐度的显著空间异质性,从西北向东南增加TRB.
- 确定的主要驱动因素包括-比,SiO2,Fe2O3,潜在的蒸发透气 (Pet),高度 (DEM),NDVI,土地利用 (LU) 和土壤质地.
- 这些因素之间的复杂相互作用有助于盐化异质性.
结论:
- 这项研究提供了对干旱地区土壤化的复杂驱动因素的见解.
- 这些发现支持可持续的农业发展和改善盐受影响地区的土壤管理策略.
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