Effects of nitrogen enrichment on soil enzyme activities in grassland ecosystems in China: A multilevel meta-analysis

IF 5.2 2区 农林科学 Q1 SOIL SCIENCE
Jibo SHI , Muhammad KHASHI U RAHMAN , Ruonan MA , Qiang LI , Yingxin HUANG , Guangdi LI
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引用次数: 0

Abstract

Nitrogen (N) enrichment has resulted in widespread alteration of grassland ecosystem processes and functions mainly through disturbance in soil enzyme activities. However, we lack a comprehensive understanding of how N deposition affects specific key soil enzymes that mediate plant-soil feedback of grassland. Here, with a meta-analysis on 1 446 cases from field observations in China, we show that N deposition differently affects soil enzymes associated with soil biochemical processes. Specifically, N-promoted C, N, and P-acquiring hydrolase activities significantly increased by 8.73%, 7.67%, and 8.69%, respectively, related to an increase in microbial-specific enzyme secretion. The increased relative N availability and soil acidification were two potential mechanisms accounting for the changes in soil enzyme activities with N enrichment. The mixed N addition in combination of NH4NO3 and urea showed greater stimulation effect on soil enzyme activities. However, the high rate and long-term N addition tended to weaken the positive responses of soil C-, N- and P-acquiring hydrolase activities to N enrichment. Spatially increased mean annual precipitation and temperature primarily promoted the positive effects of N enrichment on N- and P-acquiring hydrolase activities, and the stimulation of C- and N-acquiring hydrolase activities by N enrichment was intensified with the increase in soil depth. Finally, multimodal inference showed that grassland type was the most important regulator of responses of microbial C, N, and P-acquiring hydrolase activities to N enrichment. This meta-analysis provides a comprehensive insight into understanding the key role of N enrichment in shaping soil enzyme activities of grassland ecosystems.
氮富集对中国草地生态系统土壤酶活性的影响:一个多水平荟萃分析
氮(N)富集主要通过干扰土壤酶活性导致草地生态系统过程和功能的广泛改变。然而,我们对氮沉降如何影响介导草地植物-土壤反馈的特定关键土壤酶缺乏全面的了解。通过对中国1446例野外观测数据的荟萃分析,我们发现氮沉降对土壤生化过程相关酶的影响存在差异。其中,氮促进的C、N和p获取水解酶活性分别显著提高了8.73%、7.67%和8.69%,这与微生物特异性酶分泌增加有关。相对氮有效性的增加和土壤酸化是土壤酶活性随氮富集变化的两个潜在机制。铵硝和尿素混合施氮对土壤酶活性有较大的刺激作用。然而,高速率和长期施氮往往会削弱土壤C、N和p获取水解酶活性对N富集的积极响应。在空间上,年平均降水和温度的增加主要促进了N富集对N-和p -水解酶活性的正向作用,并且随着土壤深度的增加,N富集对C-和N-水解酶活性的促进作用增强。最后,多模态推断表明,草地类型是微生物C、N和p获取水解酶活性对N富集响应的最重要调节因子。这一荟萃分析为理解氮富集在草地生态系统土壤酶活性形成中的关键作用提供了全面的见解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Pedosphere
Pedosphere 环境科学-土壤科学
CiteScore
11.70
自引率
1.80%
发文量
147
审稿时长
5.0 months
期刊介绍: PEDOSPHERE—a peer-reviewed international journal published bimonthly in English—welcomes submissions from scientists around the world under a broad scope of topics relevant to timely, high quality original research findings, especially up-to-date achievements and advances in the entire field of soil science studies dealing with environmental science, ecology, agriculture, bioscience, geoscience, forestry, etc. It publishes mainly original research articles as well as some reviews, mini reviews, short communications and special issues.
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