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The Natural Vegetation Responses to the Groundwater Change Resulting from Ecological Water Conveyances to the Lower Tarim River

机译:塔里木河下游生态输水对地下水变化的自然植被响应

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This paper takes the ecological water conveyance project (EWCP) that transfers water from the Bosten Lake, to Daxihaizi Reservoir, and finally to the Taitema Lake as a case study to analyze the dynamic change of the groundwater depth, the vegetation responses to the elevation of the groundwater rndepth as well as the relationship between the groundwater depth and the natural vegetation. The results from many years' monitoring in field indicate: (1) the groundwater depth has been elevating gradually with the increase in the times of watering and the elevation range has been expanding continuously in the lower reaches of Tarim River. Correspondingly, the natural vegetation has a favorable response to the elevation of the groundwater depth. The change of the natural vegetation has accordance with that of the groundwater depth. Such facts not only show that groundwater is a key factor to the growth of the native vegetation but also prove it is feasible that the degraded ecosystem can be restored and protected by the EWCP; (2) the results of analysis of the spatial-temporal response of the natural vegetation to watering reveals that the beneficial influence of the EWCP on the ecosystem in the lower Tarim River is a long-term process; (3) in terms of the function andrnstructure of ecosystem after watering in the lower reaches of Tarim River, the EWCP does not still reach the goal of ecological restoration at a large spatial scale at present. Based on such monitoring results, some countermeasures and suggestions for the future restoration strategy are proposed so as to provide a theoretical basis for restoring and protecting the ecosystem in Tarim River, and meanwhile it can also provide some scientific references for implementing the similar ecological projects in other areas.
机译:本文以生态输水工程(EWCP)为例,分析了从博斯腾湖到大溪海子水库,最后到泰特玛湖的输水情况,分析了地下水深度的动态变化,植被对海拔高度的响应。地下水深度以及地下水深度与自然植被之间的关系。塔里木河多年的野外监测结果表明:(1)塔里木河下游地下水深度随着浇水次数的增加而逐渐升高,海拔范围不断扩大。相应地,天然植被对地下水深度的升高具有良好的响应。自然植被的变化与地下水的深度一致。这些事实不仅表明地下水是原生植被生长的关键因素,而且证明了EWCP可以恢复和保护退化的生态系统是可行的。 (2)对自然植被对浇水的时空响应分析结果表明,EWCP对塔里木河下游生态系统的有益影响是一个长期过程; (3)就塔里木河下游灌溉后生态系统的功能和结构而言,EWCP目前仍未达到在大空间尺度上恢复生态的目标。根据这些监测结果,提出了未来恢复战略的对策和建议,为塔里木河的生态恢复和保护提供理论依据,同时也为实施新疆类似生态工程提供了科学参考。其它地方。

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