Mowing aggravates the adverse effects of nitrogen addition on soil acid neutralizing capacity in a meadow steppe

酸中和容量 农学 化学 土壤pH值 硝化作用 浸出(土壤学) 阳离子交换容量 硫酸铵 放牧 尿素 氮气 环境化学 环境科学 土壤水分 土壤科学 生物 有机化学 酸沉积 色谱法
作者
Z. W. Wang,Tianpeng Li,Changming Lu,Cong Wang,Hui Wu,Xinyue Li,Jiangping Cai,Feng Xue,Heyong Liu,Yuge Zhang,Xingguo Han,Hui Li,Yong Jiang
出处
期刊:Journal of Environmental Management [Elsevier]
卷期号:362: 121293-121293 被引量:7
标识
DOI:10.1016/j.jenvman.2024.121293
摘要

Soil acidification induced by reactive nitrogen (N) inputs is a major environmental issue in grasslands, as it lowers the acid neutralizing capacity (ANC). The specific impacts of different N compound forms on ANC remain unclear. Grassland management practices like mowing and grazing can remove a considerable amount of soil N and other nutrients, potentially mitigating soil acidification by removing N from the ecosystem or aggravating it by removing base cations. However, empirical evidence regarding the joint effects of adding different forms of N compounds and mowing on ANC changes in different-sized soil aggregates is still lacking. This study aimed to address this knowledge gap by examining the effects of three N compounds (urea, ammonium nitrate, and ammonium sulfate) combined with mowing (mown vs. unmown) on soil ANC in different soil aggregate sizes (>2000 μm, 250–2000 μm, and <250 μm) through a 6-year field experiment in Inner Mongolia grasslands. We found that the average decline in soil ANC caused by ammonium sulfate (AS) addition (−78.9%) was much greater than that by urea (−25.0%) and ammonium nitrate (AN) (−52.1%) as compared to control. This decline was attributed to increased proton (H+) release from nitrification and the leaching of exchangeable Ca2+ and Mg2+. Mowing aggravated the adverse effects of urea and AN on ANC, primarily due to the reduction in soil organic matter (SOM) contents and the removal of exchangeable Ca2+, K+, and Na + via plant biomass harvest. This pattern was consistent across all aggregate fractions. The lack of variation in soil ANC among different soil aggregate fractions is likely due to the contrasting trend in the distribution of exchangeable Ca2+ and Mg2+. Specifically, the concentration of exchangeable Ca2+ increased with increasing aggregate size, while the opposite was true for that of exchangeable Mg2+. These findings underscore the importance of considering the forms of N compounds when assessing the declines of ANC induced by N inputs, which also calls for an urgent need to reduce N emissions to ensure the sustainable development of the meadow ecosystems.
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