Impact of long-term zero-flow and ecological water conveyance on the radial increment of Populus euphratica in the lower reaches of the Tarim River, Xinjiang, China

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• 作者：Xiaoya Deng (1) (4)
  Hailiang Xu (2)
  Mao Ye (3)
  Bailian Li (4)
  Jinyi Fu (2)
  Zhifeng Yang (1)
  
  1. State Key Laboratory of Water Environment Simulation ; School of Environment ; Beijing Normal University ; Beijing ; 100075 ; China
  4. Ecological Complexity and Modeling Laboratory ; Department of Botany and Plant Sciences ; University of California ; Riverside ; CA ; 92521-0124 ; USA
  2. Key Laboratory of Oasis Ecology and Desert Environment ; Xinjiang Institute of Ecology and Geography ; Chinese Academy of Sciences ; 818 South Beijing Road ; 脺r眉mqi ; 830011 ; People鈥檚 Republic of China
  3. School of Geographical Science and Tourism ; Xinjiang Normal University ; 102 Xinyi Road ; 脺r眉mqi ; 830054 ; People鈥檚 Republic of China
  
• 关键词：Ecological Water Conveyance Project (EWCP) ; Long ; term zero ; flow ; Tarim River ; Populus euphratica ; Radial increment
• 刊名：Regional Environmental Change
• 出版年：2015
• 出版时间：January 2015
• 年：2015
• 卷：15
• 期：1
• 页码：13-23
• 全文大小：903 KB
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• 刊物类别：Earth and Environmental Science
• 刊物主题：Environment
  Geoecology and Natural Processes
  Geology
  Oceanography
  Geography
  Nature Conservation
  Regional Science
  
• 出版者：Springer Berlin / Heidelberg
• ISSN：1436-378X

文摘

Based on the dendro-hydrology theory, we studied the impacts of two significant environmental occurrences (long-term zero-flow and ecological water conveyance) on the radial increment of Populus euphratica in the lower reaches of the Tarim River, Xinjiang, China. We also studied the relationships between radial increment and groundwater table as a function of the distance from the river channel. We found that the radial increment of P. euphratica respond significantly to both zero-flow and water conveyance, and these responses differed among four transects and they weakened with increasing distance from the Daxihaizi Reservoir. The depth to the groundwater table is a key factor that restricts P. euphratica growth in extremely arid regions, and the relationship between radial increment and the groundwater table was significant. The radial increment decreased remarkably with increasing duration of the zero-flow period. The influence of long-term zero-flows on P. euphratica growth was a long-term and slow process. The response of P. euphratica showed a delayed response to the groundwater changes after ecological water conveyance. This lag response differed among the monitoring transects and different distances away from river channel.