输水前后塔里木河下游物种多样性与水因子的关系

为检验连续7a的输水对塔里木河下游生态系统稳定性的影响,根据2006年与2010年塔里木河下游地下水埋深、地下水质以及植被调查资料,分析了2006到2010年间物种多样性、地下水位和水质变化状况,利用非参数相关和RDA排序对输水间歇物种多样性与地下水位、水质关系变化作了探讨,结果发现:塔里木河下游输水停止后地下水位不断下降,地下水矿化度也有小幅度增加;物种多样性Shannon-Weiner指数、Simpson指数、Margalef指数、Patrick指数以及Cody指数都以下降为主,表明塔里木河下游受损生态系统尚不具备自维持能力;物种多样性与地下水埋深和地下水矿化度的关系为,地下水平均埋深为5 m左右时,物种多样性主要受地下水质状况的影响,而当地下水平均埋深大于6.5m时,物种多样性的制约因子则为地下水位.因此,从物种多样性角度看,塔里木河下游的合理水位应在5 m左右,大于6.5m则是物种多样性的胁迫水位.

Analysis of the relationship between species diversity and hydrologic factors during an interval of intermittent water delivery at the Lower Reaches of Tarim River, China

Tarim River is located in south Xinjiang, northwest China. With a length of 1321 km, it is one of the longest inland rivers in the world. The name translates to "Water of Life", and certainly the river plays a key role in the development of the local society and the health of the ecosystem. Water resource development driven by irrational exploitation and increases in water utilization at the upper reaches over the past five decades has greatly disturbed the natural distribution of water resources within the valley. One major consequence is that more than 321 km of the watercourse has been drained after the Daxihaizi Reservoir was built in the 1970s. Consequently, groundwater depths along the dry watercourse increased leading to continual deterioration of groundwater quality. Along with fall in groundwater level and deterioration of groundwater quality, was the deterioration of the desert riparian system at the lower reaches of Tarim River. The desert riparian system reached a state of collapse: the area of Populus euphratica forest, the main tree species of the region, declined from 5.4 × 10⁴-0.523 × 10⁴ hm² along the lower reaches of Tarim River, while the area covered by shrub and meadow decreased by 200 km². In addition, a total area of 12,300 km² experienced desertification. To prevent the continued deterioration of the ecosystem along the dried-up watercourse and to prevent further desertification, a water delivery project has been carried out. Starting from May 2000, the water in Boston Lake was intermittently supplied to the dry watercourse. By December 2006, 11 intermittent water releases had been carried out. The released water played a critical role in vegetation recovery. However, from December 2006-June 2010, the ecological water delivery ceased. This provided a research opportunity for studying the stability of the ecosystem at the lower Tarim River after seven years of introduced water deliveries. The aims of this study were to 1) describe the variations in groundwater depths and the quality of groundwater during the four year long interval of no water delivery, 2) depict the variations in vegetation species diversity during the interval, 3) explain the relationships between groundwater and species diversity. Based on the monitoring data of groundwater depths, groundwater chemistry and species of vegetation, the variations in species diversity and related factors were analyzed. It was found that the average of groundwater depths in 2006 was approximately 5 m, while they were > 6.5 m in 2010. The Shannon-Weiner, Simpson, Margalef and Pattrick and Cody indexes expressed a decreased change. In contrast, the Peilou Index showed an increased change, indicating that the ecosystem in the lower Tarim River is in a compromised state, even though seven years of introduced water delivery had been carried out. Both Non-Parameter Analysis and Redundancy Analysis confirmed that in the year 2006, species diversity had close relationships to total dissolved solids (TDS) of groundwater, while the relationship of species diversity to the depths of groundwater was not significant. In contrast, species diversity had a close relationship to the depths of groundwater in 2010 rather than TDS. Therefore, considering the relationship between variations in groundwater level and species diversity, it can be deduced that the rational groundwater depth in the lower Tarim River under the situation of water delivery is 5 m and the intimidated groundwater depth is 6.5 m.