南水北调与水利科技
南水北調與水利科技
남수북조여수리과기
SOUTH-TO-NORTH WATER
2013年
5期
6-10
,共5页
付晓花%董增川%刘晨%山成菊%方庆%刘倩
付曉花%董增川%劉晨%山成菊%方慶%劉倩
부효화%동증천%류신%산성국%방경%류천
滦河流域%径流变化%人类活动%降水量%驱动因子
灤河流域%徑流變化%人類活動%降水量%驅動因子
란하류역%경류변화%인류활동%강수량%구동인자
Luanhe River Basin%runoff variat ion%human activity%precipit ation%driving factor
根据滦河流域滦县站1950年-2009年的逐日降水资料、逐日流量资料,运用数理统计等方法系统分析了滦河流域径流的年际、代际、年内变化特征和径流的变化趋势,并对滦河流域降水变化做了相应分析,探讨了降水和人类活动对径流变化的影响。结果表明:滦河流域径流的年际变化剧烈,代际变化明显,1950年-1979年基本处于丰水期阶段,1980年后基本处于枯水期阶段;径流年内分配极不均匀,主要集中在7月-9月,几乎占全年的66.2%。滦河流域径流有显著的递减趋势,降水与径流变化趋势基本一致,不同阶段降水和人类活动对径流的影响不同,1959年-1968年,降水和人类活动均对径流的增加做出了贡献;1969年-2009年,人类活动是该时期滦河流域径流减少的主要原因。
根據灤河流域灤縣站1950年-2009年的逐日降水資料、逐日流量資料,運用數理統計等方法繫統分析瞭灤河流域徑流的年際、代際、年內變化特徵和徑流的變化趨勢,併對灤河流域降水變化做瞭相應分析,探討瞭降水和人類活動對徑流變化的影響。結果錶明:灤河流域徑流的年際變化劇烈,代際變化明顯,1950年-1979年基本處于豐水期階段,1980年後基本處于枯水期階段;徑流年內分配極不均勻,主要集中在7月-9月,幾乎佔全年的66.2%。灤河流域徑流有顯著的遞減趨勢,降水與徑流變化趨勢基本一緻,不同階段降水和人類活動對徑流的影響不同,1959年-1968年,降水和人類活動均對徑流的增加做齣瞭貢獻;1969年-2009年,人類活動是該時期灤河流域徑流減少的主要原因。
근거란하류역란현참1950년-2009년적축일강수자료、축일류량자료,운용수리통계등방법계통분석료란하류역경류적년제、대제、년내변화특정화경류적변화추세,병대란하류역강수변화주료상응분석,탐토료강수화인류활동대경류변화적영향。결과표명:란하류역경류적년제변화극렬,대제변화명현,1950년-1979년기본처우봉수기계단,1980년후기본처우고수기계단;경류년내분배겁불균균,주요집중재7월-9월,궤호점전년적66.2%。란하류역경류유현저적체감추세,강수여경류변화추세기본일치,불동계단강수화인류활동대경류적영향불동,1959년-1968년,강수화인류활동균대경류적증가주출료공헌;1969년-2009년,인류활동시해시기란하류역경류감소적주요원인。
According to the daily precipitation and the runoff data of the Luanxian station in the Luanhe River Basin from 1950 to 2009, the mathemat ical statistics methodwas applied in this study to analyze the inter-annual, inter-generation, and annual varia-tion characterist ics and trend of runoff, and to investigate the variation of precipitation in the Luanhe River Basin to help discov-er the effects of precipitat ion and human activities to runoff. The results show ed that both the inter-annual and inter-generation runoff variations are apparent in the Luanhe River Basin, and high flow period occurred from 1950 to 1979 and low flow period appeared after 1980. Furthermore, the annual runoff of the Luanhe River Basin w as unevenly distribut edwith 66· 2% of runoff occurring from July to September. Both the runoff and precipitation of the Luanhe River Basin had the significant decreasing trend. During the period of 1959 to 1968, the increasing runoff in the Luanhe River Basin can be attributed to both the precipita-tion and human act ivities;w hile during the period of 1969 to 2009, human activity was the main reason for the decreasing of run-off.