首页> 外文会议>Eleventh International Dryland Development Conference: Global Climate Change and its Impact on Food amp; Energy Security in the Drylands >Seasonal water uptake for halophytic shrubs in northwest China salinity-affected area: an isotopic investigation
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Seasonal water uptake for halophytic shrubs in northwest China salinity-affected area: an isotopic investigation

机译:中国西北盐渍化地区盐生灌木的季节性吸水量:同位素研究

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摘要

Shallow groundwater table is the main cause of salinization in the northern area of Ningxia Plain.The uptake of groundwater by halophytes can control groundwater table.Potential water sources of four halophytic shrubs,i.e.twenty-year-old Tamarix ramosissima Ledeb.,three-year-old T.ramosissima.,Lycium barbarum L.and Atriplex canescens(Pursh)Nutt.were studied using hydrogen and oxygen isotopic compositions during a whole growth period in salinity-affected area of northwest China.Irrigation was applied for comparison of contrasting water conditions on water use of the above shrubs.The result showed that the adult T.ramosissima had the phreatophytic nature.The three year old T.ramosissima and Lycium barbarum L.exhibited higher dependence on water from unsaturated soil in upper profile during early period.The the three year old Atriplex canescens was found to have phreatophytic tendency with higher deep water uptake.Apparent depletion in xylem δD values rather than δ18O,compared with water sources,was found.There was discrepancy when using δ18O or to determine water use uptake by the shrubs.This discrepancy was more obvious after irrigation.Hydrogen isotopic fractionation would occur during water uptake by halophytic shrubs.δ18O values of xylem water should be adopted to study halophytic shrub water use in salinity-affected regions.
机译:浅层地下水位是宁夏平原北部盐碱化的主要原因。盐生植物对地下水的吸收可以控制地下水位。二十年生Ta柳(Tamarix ramosissima Ledeb。),四年的四种盐生灌木的潜在水源。在西北部盐碱化地区整个生长期,利用氢和氧同位素组成研究了老T.ramosissima。,枸杞和滨藜(Atriplex canescens(Pursh)Nutt)。结果表明,成年的T.ramosissima具有发芽性.3岁的T.ramosissima和Lycium barbarum L在早期对上部剖面非饱和土壤的水依赖性较高。发现3年龄的滨藜属植物具有深水吸收的植物赘生倾向。与水相比,木质部表观损耗δD值而不是δ18O使用δ18O或确定灌木的吸水量时存在差异。灌溉后这种差异更明显。盐生灌木吸收水时会发生氢同位素分馏。应采用木质部水的δ18O值研究盐碱化地区的盐生灌木用水。

著录项

  • 来源
  • 会议地点 Beijing(CN)
  • 作者

    Lin Zhu; Shu Xin Zheng; Xing Xu;

  • 作者单位

    State Key Laboratory Breeding Base of Land Degradation and Ecological Restoration of Northwestern China,Ningxia University,Yinchuan 750021,China;

    State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau,Institute of Water and Soil Conservation,Chinese Academy of Sciences and Ministry of Water Resources,Yangling 712100,China;

    State Key Laboratory Breeding Base of Land Degradation and Ecological Restoration of Northwestern China,Ningxia University,Yinchuan 750021,China;

    Agricultural College,Ningxia University,Yinchuan 750021;

    State Key Laboratory Breeding Base of Land Degradation and Ecological Restoration of Northwestern China,Ningxia University,Yinchuan 750021,China;

  • 会议组织
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 造林学、林木育种及造林技术;
  • 关键词

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