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塔里木河下游地下水位变化及天然植被对输水的响应。

Changes in groundwater levels and the response of natural vegetation to transfer of water to the lower reaches of the Tarim River.

作者信息

Xu Hai-liang, Ye Mao, Li Ji-mei

机构信息

Xinjiang Institute of Ecology and Geography Research, Chinese Academic of Science, Urumqi 830011, China.

出版信息

J Environ Sci (China). 2007;19(10):1199-207. doi: 10.1016/s1001-0742(07)60196-x.

Abstract

Restoration and reconstruction of the degraded Tarim River ecosystem is an important challenge. A goal of an ecological water conveyance project is to protect and restore the natural vegetation in the lower reaches of Tarim River by transferring water from Bosten Lake, through the river channel, to the lower reaches. This study describes the changes in groundwater depth during the water transfer and the respondence of riparian vegetation to alterations in groundwater levels. The results indicate that groundwater depth along the Tarim River channel has a significant spatial-temporal component. Groundwater levels closest to the river channel show the most immediate and pronounced changes as a response to water transfer while those further away respond more slowly, although the observed change appears to be longer in duration. With a rise in the groundwater level, natural vegetation responded with higher growth rates, biomass and biodiversity. These favorable changes show that it is feasible to protect and restore the degraded natural vegetation by raising the groundwater depth. Plant communities are likely to reflect the hysteresis phenomenon, requiring higher water levels to initiate and stimulate desired growth than what may be needed to maintain the plant community. Because different species have different ecologies, including different root depths and densities and water needs, their response to increasing water availability will be spatially and temporally heterogenous. The response of vegetation is also influenced by microtopography and watering style. This paper discusses strategies for the protection and restoration of the degraded vegetation in the lower reaches of the Tarim River and provides information to complement ongoing theoretical research into ecological restoration in arid or semi-arid ecosystems.

摘要

恢复和重建退化的塔里木河生态系统是一项重大挑战。生态输水工程的一个目标是通过将博斯腾湖的水经河道输送至塔里木河下游,来保护和恢复该区域的天然植被。本研究描述了输水期间地下水位的变化以及河岸植被对地下水位变化的响应。结果表明,塔里木河河道沿线的地下水位具有显著的时空特征。距离河道最近的地下水位对输水的响应最为迅速和显著,而距离较远的地下水位响应则较为缓慢,不过观测到的变化持续时间似乎更长。随着地下水位上升,天然植被的生长速率、生物量和生物多样性均有所提高。这些有利变化表明,通过提高地下水位来保护和恢复退化的天然植被是可行的。植物群落可能会呈现滞后现象,启动和刺激理想生长所需的水位高于维持植物群落所需的水位。由于不同物种具有不同的生态特征,包括不同的根系深度、密度和需水量,它们对水资源增加的响应在时空上会存在差异。植被的响应还受到微地形和浇水方式的影响。本文讨论了塔里木河下游退化植被的保护和恢复策略,并提供相关信息以补充正在进行的干旱或半干旱生态系统生态恢复理论研究。

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