摘要
三门峡水库修建后 ,潼关处于水库库区 ,河床淤积抬高。抬高过程与三门峡水库的运用方式及泄流规模密切相关。本文从实测资料入手 ,主要分析了三门峡水库控制运用以来 ,潼关河床高程的变化。非汛期水库高水位运行时间长 ,潼关河床淤积抬高 ,汛期冲刷历时短 ,溯源冲刷发展不到潼关 ,潼关河床得不到有效冲刷 ,且不利于汛期输沙 。
After builded of Sanmenxia Reservoir, Tongguan is in the reservoir region. The bed level is rise with sedimentation. The process of the rising is closely related with reservoir operation. From the survey data, the variation of Tongguan river level after the reservoir been controlled filling is studied. The result shows, that the high-stage period of time of Sanmenxia Reservoir in non-flood season is too long, so the river bed deposit, that the erosion period time in flood season is too short , so the retrogressive erosion can not reach up to Tongguan section.
出处
《西北水资源与水工程》
2001年第1期32-36,共5页
Northwest Water Resources & Water Engineering
关键词
水库淤积
溯源冲刷
潼关河床
三门峡水库
reservoir sedimentation
retrogressive erosion
Tongguan bed level
Sanmenxia Reservoir
