我国七种典型生态系统土壤氮素初级转化速率及其调控研究
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中国科学院地理科学与资源研究所生态系统网络观测与模拟重点实验室

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国家自然科学基金项目(面上项目,重点项目,重大项目)


Gross Nitrogen Transformation Rates and Their Regulation in Soils of Seven typical Ecosystems in China
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Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences

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    摘要:

    土壤氮素初级转化过程是生态系统氮循环的基本与关键环节。为阐明不同土壤氮素初级转化速率的差异特征与调控机制,选取中国三种典型生态系统的七种土壤,分别来自林地(长沙、林芝、重庆)、草地(多伦、巴音布鲁克)和旱地(上庄、曲周),采用15N同位素稀释技术结合示踪模型,开展室内短期培养试验,评估了主要的土壤氮素转化过程的初级速率。结果表明,氮素矿化、固持和自养硝化是首要的转化过程。林地、草地和旱地的土壤氮初级矿化速率、初级固定速率和初级硝化速率均无显著差异。其平均速率(±标准差)分别为:初级矿化速率1.40±1.31、2.07±1.46和1.83±0.01 mg·kg?1·d?1(以N计,下同);初级固定速率4.24±3.04、6.93±3.79和5.54±2.00 mg·kg?1·d?1;初级硝化速率1.47±1.30、3.75±1.86和5.26±2.52 mg·kg?1·d?1。不同土壤之间的初级矿化速率、初级硝化速率、惰性有机氮库的矿化速率与固定速率、自养硝化速率氮素转化速率存在普遍的显著性差异,这些差异受土壤理化性质与环境因子的显著影响。相关性分析表明,初级矿化速率与土壤有机碳显著正相关(P < 0.05),与土壤容重显著负相关;初级硝化速率与土壤盐度呈显著正相关。综上,在全球变化背景下,阐明区域尺度氮素转化特征与调控机制,应采用多尺度、多因子的综合视角,系统考虑土地利用类型、土壤性质与环境条件的耦合效应,以提升生态系统氮素动态模拟与环境风险预测的科学性与准确性。

    Abstract:

    【Objective】Soil gross nitrogen (N) transformation processes are fundamental and critical components of terrestrial N cycling. However, the mechanisms controlling gross N transformation rates and their controlling factors across soils with contrasting properties and land uses remain underexplored.【Method】Seven typical soils from three major ecosystems in China were selected: forest (Changsha, Linzhi, Chongqing), grassland (Duolun, Bayanbulak), and upland (Shangzhuang, Quzhou). A short-term incubation experiment was conducted using the?1?N isotope dilution technique combined with a numerical N tracing model. Ten key gross N transformation processes were quantified. 【Result】 Mineralization, immobilization, and autotrophic nitrification were identified as the dominant gross N transformation pathways. No significant differences in gross transformation rates were found among land use types. The means (±S.D.) of gross mineralization rates were 1.40±1.31, 2.07±1.46, and 1.83±0.01 mg·kg?1·d?1 for forest, grassland, and upland soils; corresponding to gross immobilization rates of 4.24±3.04, 6.93±3.79, and 5.54±2.00 mg·kg?1·d?1, and gross nitrification rates of 1.47±1.30, 3.75±1.86, and 5.26±2.52 mg·kg?1·d?1, respectively. Significant differences were observed between individual soils in most gross N transformation rates, indicating spatial heterogeneity in soil N supply and retention capacity. Correlation analysis showed that gross mineralization rates were positively correlated with soil organic carbon and negatively correlated with bulk density, whereas gross nitrification rates were positively correlated with soil salinity. 【Conclusion】These results demonstrate that soil properties and environmental factors jointly regulate the gross N transformation process. Under the context of global change, a multi-scale and multi-factor integrative framework, explicitly accounting for land use type, soil characteristics, and environmental conditions, is essential for improving the accuracy of ecosystem N dynamics modeling and predicting nitrogen loss risks.

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郝天象,杨萌.我国七种典型生态系统土壤氮素初级转化速率及其调控研究[J].土壤学报,,[待发表]
Hao Tianxiang, YANG Meng. Gross Nitrogen Transformation Rates and Their Regulation in Soils of Seven typical Ecosystems in China[J]. Acta Pedologica Sinica,,[In Press]

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  • 收稿日期:2025-07-29
  • 最后修改日期:2025-11-13
  • 录用日期:2026-01-04
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