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作 者:JIANG Xiaohui LIU Changming
机构地区:[1]Yellow River Institute of Hydraulic Research, Yellow River Cor~ervancy Commission, Zhengzhou 450003, China [2]Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101, China [3]Beijing Normal University, Beijing 100875, China
出 处:《Journal of Geographical Sciences》2013年第1期113-122,共10页地理学报(英文版)
基 金:National Key Basic Research Development of China (973 Program), No.2011CB40330305
摘 要:This note analyzes the change in water renewal time characteristics based on res- ervoir action and then establishes calculation models for the water renewal time in the Yellow River mainstream. The results indicate that the amount of renewable water with reservoir action can meet the annual water demand and that water flows naturally at the Lijin station near estuary. Initial storage dynamics is an important factor in water resource renewable capacity at a certain time, and rational reservoir action can promote sustainable water re- source utilization. When the initial storages in the Longyang Gorge reservoir are 9,343 and 5.343 billion m3, the water renewal times are 28 and 33.9 d, respectively. Flow stoppage appears in April and May.This note analyzes the change in water renewal time characteristics based on res- ervoir action and then establishes calculation models for the water renewal time in the Yellow River mainstream. The results indicate that the amount of renewable water with reservoir action can meet the annual water demand and that water flows naturally at the Lijin station near estuary. Initial storage dynamics is an important factor in water resource renewable capacity at a certain time, and rational reservoir action can promote sustainable water re- source utilization. When the initial storages in the Longyang Gorge reservoir are 9,343 and 5.343 billion m3, the water renewal times are 28 and 33.9 d, respectively. Flow stoppage appears in April and May.
关 键 词:water renewal time reservoir action Yellow River
分 类 号:TV145[水利工程—水力学及河流动力学] TN248.1[电子电信—物理电子学]
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