农业工程学报
農業工程學報
농업공정학보
2015年
12期
132-137
,共6页
焦平金%许迪%于颖多%王兵
焦平金%許迪%于穎多%王兵
초평금%허적%우영다%왕병
模型%径流%水文%前期产流条件%潜在初损%递推关系%SCS
模型%徑流%水文%前期產流條件%潛在初損%遞推關繫%SCS
모형%경류%수문%전기산류조건%잠재초손%체추관계%SCS
models%runoff%hydrology%antecedent runoff condition%potential initial abstraction%recurrence relation%SCS
降雨径流的精准模拟和预测是开展水资源管理和水土环境质量评价的重要依据之一,但现有SCS模型不能有效表征前期降雨蓄存和消耗对产流的影响,进而限制了其径流预测精度。该文基于潜在初损和有效降雨影响系数形成日有效影响雨量的递推关系,将前期产流条件概化成前期日降雨量对降雨初损的影响函数,从而构建了改进SCS模型。其中潜在初损量明确了产流前流域的最大降雨蓄存潜力和日降雨量的有效影响阈值,而前期有效降雨影响系数则表示了在蒸发蒸腾或渗漏过程作用下前期有效日降雨量的动态消耗。在小区、田间、流域3种排水面积下的模型应用结果表明,改进SCS模型能更准确地预报产流的变化,验证期的确定系数R2和纳什系数NSE比SCS原模型分别提高了27.0%~30.9%和1.0%~78.3%。前期有效降雨影响系数的稳定性较好,两模型的曲线数的拟合值比较一致。该改进SCS模型为更准确预测蒸发蒸腾或渗漏较为剧烈地区的径流提供参考。
降雨徑流的精準模擬和預測是開展水資源管理和水土環境質量評價的重要依據之一,但現有SCS模型不能有效錶徵前期降雨蓄存和消耗對產流的影響,進而限製瞭其徑流預測精度。該文基于潛在初損和有效降雨影響繫數形成日有效影響雨量的遞推關繫,將前期產流條件概化成前期日降雨量對降雨初損的影響函數,從而構建瞭改進SCS模型。其中潛在初損量明確瞭產流前流域的最大降雨蓄存潛力和日降雨量的有效影響閾值,而前期有效降雨影響繫數則錶示瞭在蒸髮蒸騰或滲漏過程作用下前期有效日降雨量的動態消耗。在小區、田間、流域3種排水麵積下的模型應用結果錶明,改進SCS模型能更準確地預報產流的變化,驗證期的確定繫數R2和納什繫數NSE比SCS原模型分彆提高瞭27.0%~30.9%和1.0%~78.3%。前期有效降雨影響繫數的穩定性較好,兩模型的麯線數的擬閤值比較一緻。該改進SCS模型為更準確預測蒸髮蒸騰或滲漏較為劇烈地區的徑流提供參攷。
강우경류적정준모의화예측시개전수자원관리화수토배경질량평개적중요의거지일,단현유SCS모형불능유효표정전기강우축존화소모대산류적영향,진이한제료기경류예측정도。해문기우잠재초손화유효강우영향계수형성일유효영향우량적체추관계,장전기산류조건개화성전기일강우량대강우초손적영향함수,종이구건료개진SCS모형。기중잠재초손량명학료산류전류역적최대강우축존잠력화일강우량적유효영향역치,이전기유효강우영향계수칙표시료재증발증등혹삼루과정작용하전기유효일강우량적동태소모。재소구、전간、류역3충배수면적하적모형응용결과표명,개진SCS모형능경준학지예보산류적변화,험증기적학정계수R2화납십계수NSE비SCS원모형분별제고료27.0%~30.9%화1.0%~78.3%。전기유효강우영향계수적은정성교호,량모형적곡선수적의합치비교일치。해개진SCS모형위경준학예측증발증등혹삼루교위극렬지구적경류제공삼고。
The accurate simulation or prediction of precipitation runoff has been considered as one of the most important bases for resource management and environmental quality assessment of water and soil. The soil conservation service-curve number (SCS) model, one of the most popular runoff prediction models, cannot effectively determine the effect of the antecedent runoff condition (ARC) on runoff amount, which limits the accuracy of the model’s runoff prediction. Assuming that antecedent daily precipitation depleted by evapotranspiration and seepage was linear with watershed water storage amount, the new ARC was established based on the recurrence relation of daily rainfall amount and watershed maximum rainfall storage amount. The SCS model was improved by correlating the initial abstraction with the new parameters of the potential initial abstraction and effective rainfall influence coefficient. The potential initial abstraction determines the maximum watershed rainfall storage amount prior to runoff and the threshold of daily effective rainfall amount, and the effective rainfall influence coefficient describes the dynamic depletion of antecedent daily effective rainfall amount induced by evapotranspiration and seepage. To reduce the number of unknown parameters, the relationship between the potential initial abstraction and the curve number was established under the condition that there was no rainfall for a long time prior to runoff. The data of precipitation and runoff amount from 1997 to 2008 required to assess the original and improved SCS models were collected from the 3 drainage areas of 1600 m2, 0.06 km2 and 1.36 km2 in the northern part of the Huaihe River basin, China. As antecedent daily precipitation period was 5 d and initial abstraction coefficient equaled to 0.2, the least-squares estimation method was used to calibrate the model parameters, i.e. the effective rainfall influence coefficient and the curve number, and the percent bias (PBIAS), Nash-Sutcliffe efficiency (NSE) and coefficient of determination (R2) were utilized to compare and assess the performance of the original and improved SCS models. The improved SCS model predicted daily runoff amount more accurately than the original model, and the improved SCS model increased theR2 and NSE by 27.0%-30.9% and 1.0%-78.3%, respectively, compared with the original during the validation period. Both models were calibrated with the close curve number, the effective rainfall influence coefficient was relatively stable, and the coefficient variation of 25% at plot scale resulted in the runoff prediction variation of less than 5%. The improved SCS model would perform better if it is applied in the areas with high evapotranspiration and seepage.