泥沙研究
泥沙研究
니사연구
JOURNAL OF SEDIMENT RESEARCH
2001年
2期
49-52
,共4页
渭河下游%水沙条件%河道淤积%潼关高程
渭河下遊%水沙條件%河道淤積%潼關高程
위하하유%수사조건%하도어적%동관고정
通过渭河下游河道历史及现代的演变规律,分析水沙条件、水库运用变化对渭河下游、潼关高程的影响。1986年以来,渭河下游淤积加剧主要是由于不利的水沙组合所造成,因此应加大渭河主要产沙区及河道的治理力度,以缓解渭河下游的淤积发展局面。
通過渭河下遊河道歷史及現代的縯變規律,分析水沙條件、水庫運用變化對渭河下遊、潼關高程的影響。1986年以來,渭河下遊淤積加劇主要是由于不利的水沙組閤所造成,因此應加大渭河主要產沙區及河道的治理力度,以緩解渭河下遊的淤積髮展跼麵。
통과위하하유하도역사급현대적연변규률,분석수사조건、수고운용변화대위하하유、동관고정적영향。1986년이래,위하하유어적가극주요시유우불리적수사조합소조성,인차응가대위하주요산사구급하도적치리력도,이완해위하하유적어적발전국면。
Based on the historical material and data in nowadays in the Lower Weihe River, the effect of water-sediment condition and reservoir operation variation on the Lower Weihe River and Tongguan elevation variation are analyzed. Since 1986, the deposition in the Lower Weihe River has been aggravated because of unfavorable combination of water and sediment conditions. So we should make every effort to control main regions of sediment yielding in the Weihe River basin in order to slow up deposition development in the Lower Weihe River.