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Soil respiration and carbon loss relationship with temperature and land use conversion in freeze-thaw agricultural area

机译:冻融农业区土壤呼吸和碳损失与温度和土地利用转化的关系

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摘要

Soil respiration (R_s) was hypothesized to have a special response pattern to soil temperature and land use conversion in the freeze-thaw area. The R_s differences of eight types of land use conversions during agricultural development were observed and the impacts of R_s on soil organic carbon (SOC) loss were assessed. The land use conversions during last three decades were categorized into eight types, and the 141 SOC sampling sites were grouped by conversion type. The typical soil sampling sites were subsequently selected for monitoring of soil temperature and R_s of each land use conversion types. The R_s correlations with temperature at difference depths and different conversion types were identified with statistical analysis. The empirical mean error model and the biophysical theoretical model with Arrhenius equation about the R_s sensitivity to temperature were both analyzed and shared the similar patterns. The temperature dependence of soil respiration (Q_(10)) analysis further demonstrated that the averaged value of eight types of land use in this freeze-thaw agricultural area ranged from 1.15 to 1.73, which was lower than the other cold areas. The temperature dependence analysis demonstrated that the R_s in the top layer of natural land covers was more sensitive to temperature and experienced a large vertical difference. The natural land covers exhibited smaller R_s and the farmlands had the bigger value due to tillage practices. The positive relationships between SOC loss and R_s were identified, which demonstrated that R_s was the key chain for SOC loss during land use conversion. The spatial-vertical distributions of SOC concentration with the 1.5-km grid sampling showed that the more SOC loss in the farmland, which was coincided with the higher R_s in farmlands. The analysis of R_s dynamics provided an innovative explanation for SOC loss in the freeze-thaw agricultural area. The analysis of R_s dynamics provided an innovative explanation for SOC loss in the freeze-thaw agricultural area.
机译:假设土壤呼吸(R_s)对冻融地区的土壤温度和土地利用转化具有特殊的响应模式。观察了农业发展过程中八种土地利用类型转化的R_s差异,并评估了R_s对土壤有机碳(SOC)损失的影响。最近三十年的土地利用转换分为八种类型,并且将141个SOC采样点按转换类型分组。随后选择了典型的土壤采样点,以监测每种土地利用转化类型的土壤温度和R_s。通过统计分析确定了不同深度和不同转化类型下R_s与温度的相关性。分析了关于R_s对温度的敏感性的经验均值误差模型和带有Arrhenius方程的生物物理理论模型,并共享了相似的模式。土壤呼吸的温度依赖性(Q_(10))分析进一步表明,该冻融农业区的八种土地利用的平均值在1.15至1.73之间,低于其他寒冷地区。温度依赖性分析表明,自然土地覆盖层顶层的R_s对温度更敏感,并且垂直差异较大。由于耕作方式,自然土地覆盖物具有较小的R_s,而农田具有较大的价值。确定了SOC损失与R_s之间的正相关关系,表明R_s是土地利用转化过程中SOC损失的关键链。 1.5 km网格采样的SOC浓度垂直分布表明,农田中的SOC损失更多,这与农田中较高的R_s相吻合。 R_s动力学分析为冻融农业区的SOC损失提供了创新的解释。 R_s动力学分析为冻融农业区的SOC损失提供了创新的解释。

著录项

  • 来源
    《The Science of the Total Environment》 |2015年第15期|215-222|共8页
  • 作者单位

    School of Environment, State Key Laboratory of Water Environment Simulation, Beijing Normal University, Beijing 100875, China;

    School of Environment, State Key Laboratory of Water Environment Simulation, Beijing Normal University, Beijing 100875, China;

    China-ASEAN Environment Cooperation Center (CAEC), MEP, Beijing 100035, China;

    School of Environment, State Key Laboratory of Water Environment Simulation, Beijing Normal University, Beijing 100875, China;

    School of Environment, State Key Laboratory of Water Environment Simulation, Beijing Normal University, Beijing 100875, China;

    School of Environment, State Key Laboratory of Water Environment Simulation, Beijing Normal University, Beijing 100875, China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Soil respiration; Soil carbon dynamics; Soil temperature; Land use conversion; Freeze-thawing area;

    机译:土壤呼吸;土壤碳动态;土壤温度;土地用途转换;冻融区;

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