中国农村水利水电
中國農村水利水電
중국농촌수이수전
CHINA RURAL WATER AND HYDROPOWER
2015年
4期
82-84,89
,共4页
郭维东%孙丽玲%姚庆宇%赵光昱%刘冰%王绪刚%范远丽
郭維東%孫麗玲%姚慶宇%趙光昱%劉冰%王緒剛%範遠麗
곽유동%손려령%요경우%조광욱%류빙%왕서강%범원려
大凌河%河床形态%输水输沙%冲淤变化
大凌河%河床形態%輸水輸沙%遲淤變化
대릉하%하상형태%수수수사%충어변화
Daling River%riverbed morphology%water and sediment transport%changes of erosion and deposition
基于大凌河流域自然状况及社会经济状况,选取上窝堡、朝阳、义县、凌海等4个主要水文站实测资料统计流域特征,分析大凌河输水输沙能力,同时结合流量与输沙率变化关系图、主槽平均面积比较表、各河段主槽宽度多年变化关系图、各河段不同时期的主槽容量表,从输水输沙能力和横纵向冲淤变化的角度上分析大凌河河床形态。结果显示:大凌河的河口以凌海为顶点,先向南再向北发展,体现出反复摆动的特征;河道平滩河槽和枯水河槽的过流能力由上游到下游沿程逐步增加;河道主槽的宽度反复变化,趋于逐渐变窄,主槽面积逐年递减。
基于大凌河流域自然狀況及社會經濟狀況,選取上窩堡、朝暘、義縣、凌海等4箇主要水文站實測資料統計流域特徵,分析大凌河輸水輸沙能力,同時結閤流量與輸沙率變化關繫圖、主槽平均麵積比較錶、各河段主槽寬度多年變化關繫圖、各河段不同時期的主槽容量錶,從輸水輸沙能力和橫縱嚮遲淤變化的角度上分析大凌河河床形態。結果顯示:大凌河的河口以凌海為頂點,先嚮南再嚮北髮展,體現齣反複襬動的特徵;河道平灘河槽和枯水河槽的過流能力由上遊到下遊沿程逐步增加;河道主槽的寬度反複變化,趨于逐漸變窄,主槽麵積逐年遞減。
기우대릉하류역자연상황급사회경제상황,선취상와보、조양、의현、릉해등4개주요수문참실측자료통계류역특정,분석대릉하수수수사능력,동시결합류량여수사솔변화관계도、주조평균면적비교표、각하단주조관도다년변화관계도、각하단불동시기적주조용량표,종수수수사능력화횡종향충어변화적각도상분석대릉하하상형태。결과현시:대릉하적하구이릉해위정점,선향남재향북발전,체현출반복파동적특정;하도평탄하조화고수하조적과류능력유상유도하유연정축보증가;하도주조적관도반복변화,추우축점변착,주조면적축년체감。
Based on the natural conditions and socio-economic status of the Daling River Basin ,this paper selects the measured data of four major hydrological stations ,namely the Nest Fort ,Chaoyang ,Yixian ,Linghai ,to get the basin characteristics ,and has an a‐nalysis of the water and sediment transport capacity of Daling River .Meanwhile ,combined with the flow change and transport rate graph ,the average area of the main channel comparison table ,the width of the main channel of each reach variation diagram ,the main channel capacity of each reach in different periods'table ,this paper analyzes the riverbed morphology of Daling River from the perspective of the water and sediment transport capacity and the vertical and horizontal changes of erosion and deposition .The re‐sults show that the estuary of Daling Rriver ,starting with Linghai as the vertex ,develops towards the south first and then to the north ,reflecting the characteristics of repeated swinging ;the conveyance capacity of the bankfull channel and the low flow channel of the river course gradually increases from the upstream to the downstream along the way ;the width of the main channel of the river course repeatedly changes ,tending to narrow gradually ;the main channel area is diminishing year by year .