Methodology to determine regional water demand for instream flow and its application in the Yellow River Basin.
In order to realistically reflect the difference between regional water demand for instream flow and river ecological water demand as well as to resolve the problem that water demand may be counted repeatedly, a concept of regional water demand for minimum instream flow have been developed. The concept was used in the process of determining river functions and calculating ecological water demand for a river. The Yellow River watershed was used to validate the calculation methodology for regional water demand. Calculation results indicate that there are significant differences in water demands among the different regions. The regional water demand at the downstream of the Yellow River is the largest about 14.893 X 10(9) m(3)/a. The regional water demand of upstream, Lanzhou-Hekou section is the smallest about -5.012 x 10(9) m(3)/a. The total ecological water demand of the Yellow River Basin is 23.06 X 10(9) m(3)/a, about the 39% of surface water resources of the Yellow River Basin. That means the maximum available surface water resources should not exceed 61% in the Yellow River Basin. The regional river ecological water demands at the Lower Section of the Yellow River and Longyangxia-Lanzhou Section exceed the surface water resources produced in its region and need to be supplemented from other regions through the water rational planning of watershed water resources. These results provides technical basis for rational plan of water resources of the Yellow River Basin.
Zhang
Yuan
Y
School of Environmental Sciences, State Key Laboratory of Water Environment Simulation, Beijing Normal University, Beijing 100875, China.
Yang
Zhi-feng
ZF
Wang
Xi-qin
XQ
D002681:China; D017753:Ecosystem; D014867:Water
D014867:Water