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Observation and simulation of Xiluodu Reservoir for its vertical thermal structure

机译:Xiluodu储层为垂直热结构的观察与仿真

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Xiluodu Reservoir is newly constructed in China, and its maximum 285m depth indicates vertical thermal stratification exists inside it. To get better understanding of its vertical thermal structure and temperature variation throughout a year, observation of vertical temperature distribution in front of the dam was carried out in 2014. These data have confirmed the existence of stable vertical thermal stratification in summer and autumn. To get better view of temperature variation after impoundment, a two-dimensional longitudinal-vertical hydrodynamic and water quality model (CE-QUAL-W2) was employed to simulate water level and vertical thermal structure. The data of 2013 was used to calibrate the model. And then, a working condition of regular operation year was set. The simulation result briefly depicts the thermal structure and its variation throughout a year. Beside what have been done in this research, a further study associated with the relationship between temperature structure and discharge distribution should be made to guide the management of Xiluodu Reservoir.
机译:Xiluodu水库在中国新建,其最大285米深度表示其内部存在垂直热分层。为了更好地了解其垂直的热结构和全年温度变化,2014年在大坝前面观察垂直温度分布。这些数据确认了夏季和秋季稳定的垂直热分层的存在。为了在蓄水后获得更好的温度变化视图,采用二维纵向垂直流体动力学和水质模型(CE-Qual-W2)来模拟水位和垂直热结构。 2013年的数据用于校准模型。然后,设定了常规运营年度的工作条件。仿真结果简要地描绘了全年的热结构及其变化。除本研究中已经做过的内容,还应进一步研究与温度结构与放电分配之间的关系相关联,以指导Xiluodu水库的管理。

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