河道型水库支流库湾水温特性及对气象水文的响应研究OA
Characteristics of water temperature in river-type reservoir bays and its response to meteorological and hydrological factors
河道型水库兼具河流与湖泊的双重特性,其较为独特的水动力条件与热分层结构是库内水生态系统长期演变的主要驱动力.为明晰复杂条件下河道型水库支流库湾水温变化特性,以三峡水库香溪河支流库湾为典型案例,构建了河道型水库支流库湾水温数学模型,并基于库容、水位和垂向水温实测数据进行了充分验证,进而通过多情景模拟探究了变化气象和水文条件下风速、气温、来流流量和来流水温的作用机制.结果表明:一方面,风速和气温是影响整个水体混合程度的两个重要因素,风速增大和气温降低会提高水体混合程度,风速每增大50%,则水体稳定系数峰值减少46.2%,气温每升高10%,则水体分层强度增大10.3%;另一方面,上游来流流量和水温是引起库湾中、上游水体尤其是浅层水体混合的重要因素,以上游昭君镇处XX09 监测点为例,初始状态下整个断面均处于分层状态,而当来流流量增加20%时,其混合程度提高了50%,当来流水温降低20%时,在水深5m处趋于完全混合.
River-type reservoirs exhibit dual characteristics of both rivers and lakes,featuring unique hy-drodynamic conditions and thermal stratification structures,which serve as the primary driving forces be-hind the long-term evolution of their aquatic ecosystems.To clarify the water temperature variation char-acteristics in the tributary bays of river-type reservoirs under complex conditions,a numerical model for water temperature in the Xiangxi River tributary bay of the Three Gorges Reservoir was developed.The model was thoroughly validated based on reservoir capacity,water level,and vertical water temperature data.Furthermore,multi-scenario simulations were conducted to investigate the mechanisms of wind speed,air temperature,inflow rate,and inflow water temperature under varying meteorological and hydrological conditions.The results indicate that wind speed and air temperature are two critical factors influencing the mixing degree of the entire water body.An increase in wind speed and a decrease in air temperature both can enhance water mixing.Specifically,an increase of 50%in wind speed reduces the peak water stability coefficient by 46.2%,while an increase of 10%in air temperature increases water stratification intensity by 10.3%.In addition,upstream inflow rate and water temperature are significant factors driving hydrodynamic changes in the mixing process of the middle and upper reaches of the tribu-tary bay,particularly in shallow water layers.As for the monitoring point XX09 near the Zhaojun Town,the entire cross-section was stratified under initial conditions;however,an increase of 20%in inflow rate can improve the mixing degree by 50%;a decrease of 20%in inflow water temperature can help achieve complete mixing at a water depth of 5 meters.
王洪宇;毛劲乔;熊管乐;戴杰;卢鹏
河海大学 水利水电学院,江苏 南京 210098河海大学 水利水电学院,江苏 南京 210098河海大学 水利水电学院,江苏 南京 210098河海大学 水利水电学院,江苏 南京 210098河海大学 水文水资源学院,江苏 南京 210098
建筑与水利
河道型水库支流库湾水温分层水体稳定系数
river-type reservoirtributary baywater temperature stratificationwater body stability co-efficient
《水资源与水工程学报》 2026 (1)
160-168,177,10
国家自然科学基金项目(52279013)
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