开都河灌区灌溉引水对博斯腾湖面积影响的定量分析

开都河是注入博斯腾湖的最大河流,1958～2002年间平均入湖水量达23.62×10⁸m³,占博斯腾湖总补给量的80%以上。1958年以来开都河灌区灌溉引水量维持在8.17×10⁸m³～13.18×10⁸m³之间,其中20世纪60年代灌溉引水量平均为10.14×10⁸m³/a,占开都河径流量的31.1%;70年代引水量上升到12.15×10⁸m³/a,为开都河径流量的36.5%;80年代引水量下降到11.29×10⁸m³/a,但引水量仍占开都河径流量的36.5%;90年代灌溉引水量进一步降至9.85×10⁸m³/a,仅占径流量的27.1%。通过水量平衡分析和相关回归计算,得出开都河灌区灌溉引水对博斯腾湖面积影响的数值:20世纪60年代平均值为62.4km²;70年代平均值为80.8km²;80年代、90年代分别为90.4km²、76.7km²,2000年以来平均仅为41.3km²。由此可见,45年来开都河灌区灌溉引水对博斯腾湖面积的影响经历了弱→强→弱的变化过程。

Quantitative Analysis of the Impact of Irrigation Water from Kaidu River on the Area Change of Bosten Lake

Bosten Lake is the largest lake in Xinjiang and also the largest inland freshwater lake in China,which lies in the southeast of Yanqi Basin (41°56′～42°14′N,86°40′～87°56′E) and be-longs to the arid desert climate.It is of great value in environment,ecology and economy.The tre-mendous changes in the area of Bosten Lake have been seen in recent 45 years,and its area decreased from 1 159.9km² in 1958 to 886.5km² in 1987,and then increased to 1251.1km² in 2002. Kaidu River is the longest river which flows into Bosten Lake,and its average runoff rea-ched 23.62×10⁸m³/a during 1958 to 2002,accounting for over 80% of the recharge of Bosten Lake.Therefore the water area of Bosten Lake is chiefly controlled by the runoff volume of Kaidu River,and also affected by the amount of water diverted from Kaidu River Irrigation Area (KRIA).The quantity of the water diversion from KRIA ranging from about 8.17×10⁸m³ to 13.18×10⁸m³ has been witnessed in recent 45 years.The average amount of irrigation water reached 10.14×10⁸m³/a in the 1960s,making up 31.6% of the runoff of Kaidu River,and went up to 12.15×10⁸m³/a in the 1970s,or 36.5% of Kaidu River's runoff.The average amount decreased to 11.29×10⁸m³/a in the 1980s and further declined to 9.85×10⁸m³/a in the 1990s,only accounting for 27.1% of the runoff of Kaidu River. Based on the analysis of water balance and the calculation of correlation and regression,the data on the area change of Bosten Lake influenced by the amount of the irrigation water of KRIA are obtained.The average amount reached 62.4km² in the 1960s,80.8km² in the 1970s,90.4km² in the 1980s,and 76.7km² in the 1990s,but only 41.3km² since 2000.Those data show that the impact of irrigation water from KRIA on the area change of the Bosten Lake has undergone a weak to strong and then weak process in the past 45 years.