Chin J Plant Ecol ›› 2010, Vol. 34 ›› Issue (8): 915-923.DOI: 10.3773/j.issn.1005-264x.2010.08.004

• Research Articles • Previous Articles     Next Articles

Response of sap flow in Populus euphratica to changes in groundwater depth in the middle and lower reaches of the Tarim River of northwestern China

MA Jian-Xin1,2, CHEN Ya-Ning1,*(), LI Wei-Hong1, HUANG Xiang1, ZHU Cheng-Gang1,2, MA Xiao-Dong1,2   

  1. 1Key Laboratory of Oasis Ecology and Desert Environment, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, ürümqi 830011, China
    2Graduate University of Chinese Academy of Sciences, Beijing 100049, China
  • Received:2009-10-12 Accepted:2010-01-25 Online:2010-10-12 Published:2010-09-28
  • Contact: CHEN Ya-Ning

Abstract:

Aims Our aims were to analyze the relationship between sap flow in Populus euphratica and groundwater depth, and to determine the groundwater depth that can maintain growth in P. euphratica.

Methods Sap flow flux densities of stems of P. euphratica growing in the middle and lower reachs of the Tarim River were measured using stem heat pulse techniques in August 2008. Meteorological factors were monitored by a recording weather station. Groundwater depth data were collected from monitoring wells by the conductance method.

Important findings Sap flow flux density decreased with increased groundwater depth (correlation coefficient = -0.887). When the groundwater depth dropped to 4.5-5 m, sap flow flux density in P. euphratica was abnormal. Soil salt was not the main factor influencing sap flow in P. euphratica. Data collected from 74 vegetation plots show that cover, density and frequency decrease when the groundwater depth dropped to 4-6 m. We conclude that in order to restore P. euphratica and its ecosystem in the middle and lower reaches of the Tarim River, the groundwater depth must be kept at a minimum of 4.5 m.

Key words: groundwater depth, Populus euphratica, sap flow flux density, Tarim River