Heat transfer at ice-water interface under conditions of low flow velocities

The heat transfer at the ice-water interface is closely related to the hydrodynamic and physical properties of the water body.It affects the ice cover thickness and the water temperature underlying the ice cover.This paper studies the heat transfer from the water to the ice cover.Based on the flume...

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Bibliographic Details
Published inJournal of hydrodynamics. Series B Vol. 28; no. 4; pp. 603 - 609
Main Author 李楠 脱友才 邓云 李嘉 梁瑞峰 安瑞冬
Format Journal Article
LanguageEnglish
Published Singapore Elsevier Ltd 01.08.2016
Springer Singapore
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Summary:The heat transfer at the ice-water interface is closely related to the hydrodynamic and physical properties of the water body.It affects the ice cover thickness and the water temperature underlying the ice cover.This paper studies the heat transfer from the water to the ice cover.Based on the flume data,a linear relationship between the ice-water heat transfer coefficient and the flow velocity beneath the ice cover is established and the calculated dimensionless ice-water heat transfer coefficient is 1.1×10-3.This empirical relationship can be applied to estimate the ice-water heat transfer of reservoirs,lakes and other freshwater bodies when the flow velocity under the ice cover is in the range of 0.024 m/s-0.110 m/s.
Bibliography:31-1563/T
reservoirs beneath hydrodynamic dimensionless freshwater turbulence turbulent deviation affects thick
Nan LI, You-cai TUO , Yun DENG , Jia LI , Rui-feng LIANG, Rui-dong AN ( State Key Laboratory of Hydraulics and Mountain River Engineering, Sichuan University, Chengdu 610065, China)
The heat transfer at the ice-water interface is closely related to the hydrodynamic and physical properties of the water body.It affects the ice cover thickness and the water temperature underlying the ice cover.This paper studies the heat transfer from the water to the ice cover.Based on the flume data,a linear relationship between the ice-water heat transfer coefficient and the flow velocity beneath the ice cover is established and the calculated dimensionless ice-water heat transfer coefficient is 1.1×10-3.This empirical relationship can be applied to estimate the ice-water heat transfer of reservoirs,lakes and other freshwater bodies when the flow velocity under the ice cover is in the range of 0.024 m/s-0.110 m/s.
ISSN:1001-6058
1878-0342
DOI:10.1016/S1001-6058(16)60664-9