开都河

开都河是博斯腾湖的主要补给源，对博斯腾湖生态与环境起着至关重要的作用。

Kaidu River is the main recharge source of Bosten Lake , which plays an important role in the eco-environment of the lake .

博斯腾湖是塔里木河流域4大源流-开都河的尾闾湖，孔雀河的源地。

The Bosten Lake is the rump lake of the Kaidu River ( one of the4 main source streams of the Tarim River ) and the source of the Kongque River .

计算结果表明：开都河流域面雨量年平均为80.6×108m3，径流量与面雨量之比（R/P）平均为0.38，最大为0.53，最小为0.32。

As a result , the average annual areal precipitation is 80.6 × 108m3 , the average ratio of runoff and areal precipitation ( R / P ) is 0.38 , its maximum and minimum is 0.53 and 0.32 respectively .

气候的变化直接影响着开都河年径流量的变化。

The Climate changes have a direct impact on the river in a runoff changes .

结合新疆开都河流域水电开发情况对流域水电开发公司的企业战略问题进行了探讨。

Combined with hydropower development , the enterprise strategy has been discussed for hydro development company in catchment area .

结合新疆开都河河床地质条件，对砂土液化进行判别与评价，提出输油管道通过开都河最佳方案的建议。

Based on the geological conditions of the river bed of kaiduhe , Xinjiang , sand liquefaction was identified and evaluated , and an optimal plan of pipeline crossing the kaiduhe river was suggested .

之间的冲突忽必烈和汗国在中亚领导的开都河持续了几十年，直到年初的14世纪，当他们两个人已经死亡。

The conflicts between Kublai Khan and the khanates in Central Asia led by Kaidu had lasted for a few decades , until the beginning of the14th century , when both of them had died .