中文摘要：

基于浑河与太子河上游1998--2007年北口前站和南甸峪站水文数据以及清原、新宾和本溪县气象站点同期气象数据，应用DI-ISVM分布式水文模型模拟浑太流域的水文过程，验证模型的科学适用性，并提供最敏感模型参数的参考值．结果表明：浑河源区月径流模拟的Nash—Suttclife系数（E值）在率定期（1998--2002年）和验证期（2003--2007年）分别达到0．9675和0．8957，较好重现了研究区的月径流过程．太子河上游流域的年、月径流模拟值的E值均大于0．6，说明模型在浑太流域有较好的适用性、率定的参数方案有良好的可靠性．本文为无站点观测资料的流域水文研究建立了一个坚实的框架，并构建了合理的参数方案．

英文摘要：

Based on the hydrological data from the Beikouqian and Nandianyu stations in the up- stream of Hun River and Taizi River as well as the meteorological data from the Qingyuan, Xinbin, and Benxi County stations, Northeast China in 1998-2007, a distributed hydrological model （ DHS- VM） was applied to simulate the hydrological process in Hun-Tai basin. The scientific applicability of the model was validated, and the reference values of the most sensitive model parameters were provided. The simulated monthly runoff Nash-Suttclife coefficient （E value） for the source region of Hun River in calibration period （1998-2002） and validation period （2003-2007） was 0. 9675 and 0.8957, respectively, which could better reappear the monthly runoff process in this source region. The simulated monthly and annual runoff E values for the upstream of Taizi River were greater than 0.6, indicating that this model had good applicability in Hun-Tai basin, and the calibrated parame- ter scheme had a good reliability. This paper established a solid framework for the hydrological study over ungauged basin, and constructed a reasonable parameter scheme.