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Potential and environmental control of carbon sequestration in major ecosystems across arid and semi-arid regions in China

机译:中国干旱和半干旱地区主要生态系统中固碳的潜力和环境控制

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摘要

With the continuous expansion of drylands in the context of global climate change, governments have implemented a series of greening policies such as afforestation, to reduce ecological degradation. However, owing to historical conditions and technical constraints, few attempts have been made to quantitatively assess the differences in carbon sequestration capacity and the associated environmental controls among major ecosystems in the arid and semi-arid areas. Based on six flux towers located in northwestern China measuring the carbon fluxes in a maize (Zea mays L.) cropland, alpine meadow, wetland, swamp meadow, Tamarix, and gobi desert, this work revealed that all ecosystems sequestered CO2 at various magnitudes. The cropland had the highest carbon uptake, followed by the alpine meadow, swamp meadow, wetland and Tamarix, respectively. Distinct seasonal dynamics in carbon sequestration were observed across these ecosystems with the peak values in summertime, whereas the gobi desert exhibited as a weak carbon sink with considerable fluctuations around the year. In this water limited region, soil water content instead of rainfall, is expected to be the primary environmental control on the land-atmosphere carbon fluxes, and regarded as a key linkage between hydrologic and ecologic processes. Therefore, not only the appropriate vegetation types, but also the water availability controlled by the local climatic constraints and soil characteristics, should be addressed in order to identify management strategies for ecological restoration in the dry areas. (C) 2018 Elsevier B.V. All rights reserved.
机译:随着全球气候变化背景下干旱地区的不断扩大,各国政府已实施了一系列绿化政策,例如植树造林,以减少生态退化。然而,由于历史条件和技术限制,很少有人试图定量评估干旱和半干旱地区主要生态系统之间固碳能力和相关环境控制的差异。基于位于中国西北部的六个通量塔,该通量塔测量了玉米(Zea mays L.)农田,高寒草甸,湿地,沼泽草甸,塔马里克斯和戈壁沙漠中的碳通量,这项工作表明所有生态系统都以不同的程度隔离了CO2。农田的碳吸收量最高,其次是高山草甸,沼泽草甸,湿地和and柳。在这些生态系统中,固碳的季节动态有明显的季节性变化,夏季达到峰值,而戈壁沙漠则表现为弱碳汇,并在全年左右波动较大。在这个缺水地区,土壤水分而不是降雨被认为是对陆地-大气碳通量的主要环境控制,并且被视为水文和生态过程之间的关键联系。因此,不仅要确定适当的植被类型,而且要考虑受当地气候限制和土壤特征控制的水利用状况,以便确定干旱地区生态恢复的管理策略。 (C)2018 Elsevier B.V.保留所有权利。

著录项

  • 来源
    《The Science of the Total Environment》 |2018年第15期|796-805|共10页
  • 作者单位

    Southwest Univ, Sch Geog Sci, Chongqing Engn Res Ctr Remote Sensing Big Data Ap, Chongqing 400715, Peoples R China;

    Southwest Univ, Sch Geog Sci, Chongqing Engn Res Ctr Remote Sensing Big Data Ap, Chongqing 400715, Peoples R China;

    Southwest Univ, Sch Geog Sci, Chongqing Engn Res Ctr Remote Sensing Big Data Ap, Chongqing 400715, Peoples R China;

    Southwest Univ, Sch Geog Sci, Chongqing Engn Res Ctr Remote Sensing Big Data Ap, Chongqing 400715, Peoples R China;

    Southwest Univ, Sch Geog Sci, Chongqing Engn Res Ctr Remote Sensing Big Data Ap, Chongqing 400715, Peoples R China;

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

    Carbon flux; Arid and semi-arid area; Northwest China; Water balance; Climate change;

    机译:碳通量;干旱和半干旱地区;西北;水平衡;气候变化;

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