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This study aims to identify the water flux in an earth dam using heat flux due to convection. Sixteen earth dams model was constructed in a hydraulic flume by varyinggeometrical and flow input parameters to identify heat and water flux.Homogeneous as well was earth dam with the clay core was built-in a hydraulic flume. Temperature measurements were doneto calculate heat flux in the experimental model. A finite element model of the earth dam using Seep/w was developed to obtain water flux,while temp/wwas to obtain heat flux. These results were used as input in Temp/w and Seep/w in Geostudio 2020. Significant reduction of the heat and water fluxwas seen while comparing the homogeneous models with central impervious core models. An increase in the heat and water flux was observed on increasing the downstream filter's length, longitudinal slope,and vice versa with the upstream slope and the thickness of the clay core. Comparing fluxesina homogeneous dam model (model 1) with the clay core model (model 9) with top width 2.4 m and bottom width 18 m in model 9, both water flux and heat flux were reduced78.46%. While comparing it with model 10, with bottom core width of 18 m and top core width of 1.9 m, both water flux and heat flux reduced by 77.72%. Heat flux measurements were found a valuable alternative to detecting water flux and seepage in an earth dam at a reduced cost.

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