• 论文
主办单位:煤炭科学研究总院有限公司、中国煤炭学会学术期刊工作委员会
风沙采煤沉陷区地表生物结皮土壤碳排放对水热因子变化的响应
  • Title

    Response of soil carbon emission of biological crust to hydrothermal factors in mining subsidence area in aeolian

  • 作者

    党晓宏刘阳蒙仲举高永魏亚娟翟波刘禹辛

  • Author

    DANG Xiaohong,LIU Yang,MENG Zhongju,GAO Yong,WEI Yajuan,ZHAI Bo,LIU Yuxin

  • 单位

    内蒙古农业大学 沙漠治理学院内蒙古杭锦荒漠生态系统国家定位观测研究站内蒙古自治区水利科学研究院中央与地方共建高校特色优势学科“风沙物理”重点实验室

  • Organization
    Institute of Desert Contol Science and Engineering,Inner Mongolia Agricultural University,Hohhot; Inner Mongolia Hangjin Dsert Ecological Position Rsearch Station; Institute of Water Conservancy Science Inner Mongolia Municipality; Center and Local Co-building “Aeolian Physics” Key Laboratory of Special Dominant Discipline in University
  • 摘要

    生物结皮是干旱区土壤碳排放的重要参与者,为阐明毛乌素沙地采煤沉陷区典型生物结皮土壤碳排放规律及其对土壤水热因子变化的响应,以藓类结皮、藻类结皮和地衣结皮为研究对象,通过Automated Soil CO2 Exchange Station(简称ACE)土壤碳通量自动监测系统分别测定了3类生物结皮土壤碳排放速率、土壤温湿度,并对2者关系进行探究。结果表明:① 3类生物结皮土壤碳排放速率的日变化特征曲线总体上均呈现“不对称钟形”的“单峰”曲线特征,峰值在12:00~13:00。土壤碳排放速率日均值由大到小依次为藻类结皮(0.47 μmol/(m2·s))>藓类结皮(0.45 μmol/(m2·s))>地衣结皮(0.44 μmol/(m2·s));② 3类生物结皮的土壤碳排放速率与表层土壤温度均呈现二次函数关系,其决定系数分别为0.59,0.46和0.64(P<0.01);③ 生物结皮土壤碳排放速率与表层土壤含水量均呈二次函数关系,其中藓类结皮的最优拟合关系为二次函数关系,其决定系数R2达到了0.45的极显著水平(P<0.01);④ 土壤含水量与土壤温度可以较好地解释土壤碳排放速率,拟合方程中2者对于土壤碳排放速率的解释度均在57.8%以上。

  • Abstract

    Soil carbon emission of the lands covered by biocrusts is an important component in the carbon cycle.To clarify the carbon emission pattern of typical biocrusts in the coal mining subsidence area of Mawwusu sand and its response to changes in soil hydrothermal factors,the soil carbon emission rate,soil temperature and humidity were measured by the Automated Soil CO2 Exchange Station (ACE),and the relationship between them was explored.The results show that:① on the whole,the diurnal variation characteristic curves of soil carbon emission rates of three typical biologically-crusted soils generally show the characteristics of asymmetrical bell single peak’curve,with the peak value between 12:00-13:00.The daily average soil carbon emission rate order is algae overlying crust (0.47 μmol/(m2·s)) > moss overlying crust (0.45 μmol/(m2·s)) > lichen crust (0.44 μmol/(m2·s)).② The soil respiration rate of three typical biologically-crusted soils shows a quadratic function relationship with the surface soil temperature,and their determination coefficients are 0.59,0.46 and 0.64,respectively,all of which reach extremely significant positive correlation levels (P<0.01).③ The relationship between soil carbon emission rate and surface soil water content is quadratic function,and the best fitting relationship between the soil water content of moss overlying soil is quadratic function,and its coefficient R2 reaches a very significant level of 0.45 (P

  • 关键词

    生物结皮碳排放土壤温湿度林分类型采煤沉陷区毛乌素沙地

  • KeyWords

    biocrust;carbon emission rate;soil temperature and soil moisture;forest type;mining subsidence area;Mu Us Desert

  • 基金项目(Foundation)
    内蒙古自治区科技重大专项资助项目(zdzx2018058);国家自然科学基金资助项目(41967009)
  • 文章目录

    1 研究区域与研究方法

      1.1 研究区概况

      1.2 研究方法

    2 结果与分析

       2.1 生物结皮土壤碳排放速率及环境因子日动态变化规律

       2.2 土壤碳排放速率与主要环境因子的关系

    3 讨论

    4 结论

  • 引用格式
    党晓宏,刘阳,蒙仲举,等.风沙采煤沉陷区地表生物结皮土壤碳排放对水热因子变化的响应[J].煤炭学报,2021,46(5):1511-1520.
    DANG Xiaohong,LIU Yang,MENG Zhongju,et al.Response of soil carbon emission of biological crust to hydrothermal factors in mining subsidence area in Mu Us Desert[J].Journal of China Coal Society,2021,46(5):1511-1520.
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