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                 Analysis of the winter thermal transfer potential in the source reservoirs of the Middle Route
                                      of the South-to-North Water Diversion Project

                                                   1
                                                               1
                                                                             2
                                       1


                               LIU Lijin ,TUO Youcai ,DENG Yun ,KANG Jingwei ,ZHANG Xu   1





                       (1. State Key Lab. of Hydraulics and Mountain River Engineering,Sichuan University,Chengdu  610065,China;


                    2. China South-to-North Water Transfer Group Middle Route Corporation Limited. Qu Shou Branch,Nanyang  473000,China)
                Abstract:The  Danjiangkou  Reservoir,serving  as  the  source  reservoir  for  the  Middle  Route  of  the  South-to-North
                Water  Diversion  Project,its  thermal  regime  evolution  characteristics  and  winter  heat  transfer  capacity  to  the  main

                canal are recognized as critical issues requiring exploration in research on enhancing winter water conveyance capac⁃

                ity.  This  study  analyzed  monitored  water  temperature  data (2006-2022)from  surrounding  hydrological  stations  to
                reveal  thermal  characteristic  variations  before  and  after  dam  heightening,preliminarily  clarify  heat  transport  path⁃
                ways,and investigate the reservoir's winter heat transfer potential to the main canal. The results indicate that:(1)


                The Danjiangkou Reservoir is a stratified reservoir,and the stratification effect intensified after the dam was raised.

                The vertical temperature difference near the dam increased from 0.3-4.9 ℃ to 0.2-12.0 ℃,enhancing the reservoir's

                heat retention capacity. Consequently,he spring-summer cold-water effect on downstream reaches has been exacer⁃
                                              t
                bated by up to 8.0 ℃,while the winter intake temperature at the headwork has been raised by as much as 2.1 ℃. (2)

                After the dam heightening,the winter intake temperature at the Taocha headwork showed altered responses to mul⁃





                tiple  influencing  factors:(i)its  correlation  coefficient  with  air  temperature  decreased  from  0.85  to  0.78;(ii)an
                abrupt  shift  in  winter  intake  temperature  was  observed  after  2013,with  the  Mann-Kendall  trend  test  index (tau)



                changing  from  -0.11  to  0.16,indicating  a  gradual  upward  trend  under  high  water-level  operation;(iii)the  phase
                deviation  angle  between  winter  intake  temperature  and  the  inflow  temperature  from  the  Han  River (with  relatively

                large discharge)was essentially 0°,demonstrating increased coherence. (3)During winter operation,raising the res⁃



                ervoir level or increasing the flow withdrawal at the headwork can leverage spatial variations in temperature distribu⁃

                tion and heat transfer trajectories to supply additional heat to the headwork region,thereby further tapping the reser⁃
                voir's potential for heat delivery to the Middle Route. These findings offer technical support for formulating measures
                to enhance the winter water conveyance capacity of the Middle Route of the South-to-North Water Diversion Project.

                Keywords:Danjiangkou  Reservoir;Middle  Route  of  the  South-to-North  Water  Diversion  Project;thermal  energy


                transfer;heat transfer potential;water transfer capacity

                                                                                     (责任编辑:韩  昆)
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