环境科学
氮气
生态系统
生物量(生态学)
陆地生态系统
硝化作用
氮气循环
土壤肥力
生态学
农学
土壤水分
化学
土壤科学
生物
有机化学
作者
Qilin Zhu,Lijun Liu,Juan Liu,Yunxing Wan,Ruoyan Yang,Jinxia Mou,Qiuxiang He,Shuirong Tang,Xiaoqian Dan,Yanzheng Wu,Tongbin Zhu,Lei Meng,Ahmed S. Elrys,Christoph Müller,Jinbo Zhang
标识
DOI:10.1021/acs.est.3c08104
摘要
Understanding the underlying mechanisms of soil microbial nitrogen (N) utilization under land use change is critical to evaluating soil N availability or limitation and its environmental consequences. A combination of soil gross N production and ecoenzymatic stoichiometry provides a promising avenue for nutrient limitation assessment in soil microbial metabolism. Gross N production via 15N tracing and ecoenzymatic stoichiometry through the vector and threshold element ratio (Vector-TER) model were quantified to evaluate the soil microbial N limitation in response to land use changes. We used tropical soil samples from a natural forest ecosystem and three managed ecosystems (paddy, rubber, and eucalyptus sites). Soil extracellular enzyme activities were significantly lower in managed ecosystems than in a natural forest. The Vector-TER model results indicated microbial carbon (C) and N limitations in the natural forest soil, and land use change from the natural forest to managed ecosystems increased the soil microbial N limitation. The soil microbial N limitation was positively related to gross N mineralization (GNM) and nitrification (GN) rates. The decrease in microbial biomass C and N as well as hydrolyzable ammonium N in managed ecosystems led to the decrease in N-acquiring enzymes, inhibiting GNM and GN rates and ultimately increasing the microbial N limitation. Soil GNM was also positively correlated with leucine aminopeptidase and β-N-acetylglucosaminidase. The results highlight that converting tropical natural forests to managed ecosystems can increase the soil microbial N limitation through reducing the soil microbial biomass and gross N production.
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