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- W2380430713 abstract "Using current and sediment equation in the non-constant hydrodynamics,the paper set up a one-dimensional mathematical transport model of water and sediment in the Xia Heyan to Tou Daoguai reach.Using the hydrologic and sediment data of the Yellow River 1997 to 2000 and 2003 to 2006,it calibrated and verified the model.The use of this model simulated and calculated the impact of the irrigation area diversion to the sediment changes in riverway of the Ningxia-Inner Mongolia from 1997 to 2006.The analysis recognized: when Ningxia-Inner Mongolia irrigation area water diversion of 100 million m3 each,corresponding runoff volume will reduced 69 million m3,in Tou Daoguai section when net water diversion of 100 million m3,the Toudaoguai section runoff volume will be reduled 102 million m3;corresponding the amount of sediment will be reduced 409,000 t and 607,000 t respectively,riverway siltation changes in the amount of 1432 million t.The influence of flood season diversion to sediment change in the river course was bigger than the influence of runoff change the which the flood season diversion causes turns the Tou Daoguai section runoff decrement to account for the diversion time runoff reduction total quantity 50%,but corresponding loses the sand decrement to occupy loses the sand reduction total quantity 73%." @default.
- W2380430713 created "2016-06-24" @default.
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- W2380430713 date "2011-01-01" @default.
- W2380430713 modified "2023-09-26" @default.
- W2380430713 title "Numerical simulation of water and sediment change in Ningxia-Inner Mongolia reach and the impact of water diversion on water and sediment change in river course" @default.
- W2380430713 hasPublicationYear "2011" @default.
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