Water resources in the Plain of Manas River Basin have exploited and utilized with a long history.
新疆玛纳斯河流域平原区的水资源开发利用历史悠久。
Main water source of Manas River comes from the thaw on high mountains and the precipitation on its upper reaches.
高山区的冰雪融水和玛纳斯河上游的降水是该流域的主要径流水源。
This paper studied and analysed the succession process of soil characteristic along the latitude in the Manas river.
以玛纳斯河流域为案例，重点分析沿流域纬度梯度土壤特性的变化。
The annual surface flow in the Manas River of Xinjiang was chosen as object on the basis of discussion on the grey topological theory.
在进行灰色拓扑理论探讨的基础上，选取新疆玛纳斯河年径流作为预报对象。
This text fits the whole production function of the moisture and moisture production function of the crop of stage of the typical crop (cotton) of Manas river valley.
本文拟合了玛纳斯河流域典型作物(棉花)的全生育期水分生产函数及阶段作物水分生产函数。
Positive succession should be based on the temporal and spatial distribution and the coordinated utilization of oasis resource factors on the agro-ecosystem along Manas River.
玛纳斯河流域农业生态系统良性演替需建立在绿洲资源要素时空优化配置及其协调开发利用上。
Lastly, the feasibility and validity of the model was validated with the past years surface water resource quantity time series data from Kenswat Station on Xinjiang Manas River.
最后，以玛纳斯河肯斯瓦特站历年的年径流资料验证时间序列人工神经网络预测模型的可行性与有效性。
Lastly, the feasibility and validity of the model was validated with the past years surface water resource quantity time series data from Kenswat Station on Xinjiang Manas River.
最后，以玛纳斯河肯斯瓦特站历年的年径流资料验证时间序列人工神经网络预测模型的可行性与有效性。
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