地下水
地下水
지하수
Underground Water
2015年
5期
156-157,169
,共3页
复式断面%水位流量关系%曼宁公式
複式斷麵%水位流量關繫%曼寧公式
복식단면%수위류량관계%만저공식
Compound cross channel%stage-discharge relation and Manning Fomula
以渭河下游华县水文站实测水位~流量点据为验证资料,对比分析单一河槽法、滩槽垂直分割法和全断面分割法三种不同形式曼宁公式在复式河段的适用性,结果表明单一河槽法及滩槽垂直分割法未充分考虑滩槽水流动量交换的特点,计算流量值在平滩水位处出现跳跃现象,不符合天然复式河段水位~流量关系的变化规律,而全断面分割法将断面分割为多股水流然后分别累加各子断面流量,计算成果基本反映天然复式河段水位~流量关系的变化规律,建议复式河段水位~流量关系计算采用全断面分割法。
以渭河下遊華縣水文站實測水位~流量點據為驗證資料,對比分析單一河槽法、灘槽垂直分割法和全斷麵分割法三種不同形式曼寧公式在複式河段的適用性,結果錶明單一河槽法及灘槽垂直分割法未充分攷慮灘槽水流動量交換的特點,計算流量值在平灘水位處齣現跳躍現象,不符閤天然複式河段水位~流量關繫的變化規律,而全斷麵分割法將斷麵分割為多股水流然後分彆纍加各子斷麵流量,計算成果基本反映天然複式河段水位~流量關繫的變化規律,建議複式河段水位~流量關繫計算採用全斷麵分割法。
이위하하유화현수문참실측수위~류량점거위험증자료,대비분석단일하조법、탄조수직분할법화전단면분할법삼충불동형식만저공식재복식하단적괄용성,결과표명단일하조법급탄조수직분할법미충분고필탄조수류동량교환적특점,계산류량치재평탄수위처출현도약현상,불부합천연복식하단수위~류량관계적변화규률,이전단면분할법장단면분할위다고수류연후분별루가각자단면류량,계산성과기본반영천연복식하단수위~류량관계적변화규률,건의복식하단수위~류량관계계산채용전단면분할법。
With measured stage-discharge data points of Huaxian hydrological station in downstream of Weihe River, three different kinds of Manning formula of single channel method, vertical division method of channel and floodplain, whole section divi-sion method are analyzed to find out the applicability in conpound channel. It's indicated that the inadequate considerration on mo-mentum exchange of flow between channel and floodplain of single channel method and vertical division method of channel and flood-plain lead to jumping phenomenon in dischasrge calculation results, this phenomenon violates the variation of stage-discharge rela-tion in natual compound channnel. While the whole section division method divises the whole cross section into several sub-sen-tions, and than accumulates discharge of each sub-section, the calculation result complies with variation of stage-discharge rela-tion in natual compound channnel. It's recommanded that whole section division method should be used in compound channel.