A Review of Classification, Causes, and Amelioration of Global Salt‐Affected Soil Based on the Meta‐Analysis

环境科学 生物炭 石膏 土壤水分 土壤改良剂 土壤盐分 碱土 土壤碳 钠吸附比 总有机碳 生物量(生态学) 石灰 土壤科学 土壤质量 环境工程 土壤pH值 农学 生态系统 阳离子交换容量 固碳 修正案 土壤肥力 荒漠化 海水淡化 二氧化碳 盐度 碳纤维 降水 土工试验 土壤有机质 营养物 土壤功能 无机碳总量
作者
Bing Liang,Jianbing Wei,Yukun Gao,Zhirong Ma,Xian Xue
出处
期刊:Land Degradation & Development [Wiley]
卷期号:36 (16): 5485-5504 被引量:4
标识
DOI:10.1002/ldr.5619
摘要

ABSTRACT Soil salinization poses a significant threat to sustainable global agriculture, critically impacting plant growth, soil fertility, and ecosystem stability. This paper first provides a comprehensive overview of soil salinization, including its definition, types, classifications, global distribution, historical continuity, and associated environmental impacts. Then, we examine salinization's causes, processes, and mechanisms, offering an in‐depth classification of saline, sodic, and saline‐sodic soils. Through physicochemical analysis, it characterizes the unique challenges of different types of salinized soils. A meta‐analysis of 254 global case studies demonstrates that applying soil conditioners effectively ameliorates three kinds of salt‐affected soils. Specifically, gypsum application resulted in a 13.4% reduction in pH in saline soils and a significant ( p < 0.001) decrease in the exchangeable sodium percentage. Mixed conditioners reduced the exchangeable sodium percentage of sodic soils by 58.6% through synergistic effects. Biochar showed a pronounced effect in sodic soils, increasing soil organic carbon by 65.7%, with a minimal reduction in pH (4.0%). Importantly, mixed conditioners enhanced microbial biomass carbon in saline‐sodic soils by 68.8% and increased available phosphorus by 97.6%. However, gypsum application did not consistently decrease electrical conductivity (EC); in sodic soils, it led to a 21.0% increase in EC. Additionally, field experiments exhibited superior desalination performance relative to controlled laboratory conditions, with corresponding EC effect sizes of −0.26 and 0.04, respectively. Treatments exceeding 3 years in duration yielded more significant improvements than those lasting less than 3 years. Path analysis identified soil conditioner characteristics as the primary drivers of salt reduction, with the most substantial direct effect (path coefficient = −0.847, p < 0.001), surpassing the influence of environmental factors and initial soil properties. Based on these findings, the paper proposes a soil‐type‐specific remediation framework, emphasizing the functional compatibility between soil conditioner properties and soil salinity characteristics. These findings establish a soil‐type‐specific remediation framework, guiding tailored conditioner selection to enhance ecological and agricultural sustainability in salt‐affected soil reclamation.
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