Analysis on High Sediment Concentration Flood Occurred in the Huangpuchuan River on July 27, 2006
Zhiyong Wang
Abstract
Zhiyong Wang
Abstract
The paper analyzes the moderate flood of peak discharge 1 650 m3/s and sediment concentration 1 110 kg/ m3 happened in the Huangpuchuan River of the middle Yellow River on July 27, 2006. It considers the cause of formation is that a) the center of storm is in the feldsparthic sandstone region of the upper Yellow River where the treatment level is lower and; b) “tearing the river bed off” scour happens in the flood season because the gully bottom is covered by thicker sediment. It also points out that the probability of such high sediment concentration flood happened in the Huangpuchuan River basin is still greater.
A significance statement is not available in the OpenAlex record.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
The paper analyzes the moderate flood of peak discharge 1 650 m3/s and sediment concentration 1 110 kg/ m3 happened in the Huangpuchuan River of the middle Yellow River on July 27, 2006. It considers the cause of formation is that a) the center of storm is in the feldsparthic sandstone region of the upper Yellow River where the treatment level is lower and; b) “tearing the river bed off” scour happens in the flood season because the gully bottom is covered by thicker sediment. It also points out that the probability of such high sediment concentration flood happened in the Huangpuchuan River basin is still greater.
Key concepts: Hydrology (agriculture), Flood myth, Sediment, Storm, Drainage basin, Geology, River regime, Environmental science