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연속 운전 방식의 대수층 축열 시스템에 대한 수치 모델링

Numerical Modeling on the Aquifer Thermal Energy Storage System under Continuous Operation Regime

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초록

This paper presents numerical investigations and thermohydraulic evaluation on the two-well model of aquifer thermal energy storage (ATES) systems operated under continuous flow regime. A three-dimensional finite-difference model for groundwater flow and heat transport is used to analyze the thermal energy storage in the aquifer. The model includes the effects of convection and conduction heat transfer, heat loss to the adjacent confining strata, and hydraulic anisotropy. The operation scenario consists of continuous injection and recovery from two wells and four periods per year to simulate the seasonal temperature conditions. The calculated temperatures at the producing well were relatively constant within certain range through the year and fluctuating with a quarterly year period. Operation schedules, injection temperature, injection/production rate, and geometry of well arrangement used in the model are shown to impact the predicted temperature profiles at each stage and the recovery water temperature. But aquifer thickness and hydraulic anisotropy have a minimal effect on the performance of ATES systems.

Abstract

This paper presents numerical investigations and thermohydraulic evaluation on the two-well model of aquifer thermal energy storage (ATES) systems operated under continuous flow regime. A three-dimensional finite-difference model for groundwater flow and heat transport is used to analyze the thermal energy storage in the aquifer. The model includes the effects of convection and conduction heat transfer, heat loss to the adjacent confining strata, and hydraulic anisotropy. The operation scenario consists of continuous injection and recovery from two wells and four periods per year to simulate the seasonal temperature conditions. The calculated temperatures at the producing well were relatively constant within certain range through the year and fluctuating with a quarterly year period. Operation schedules, injection temperature, injection/production rate, and geometry of well arrangement used in the model are shown to impact the predicted temperature profiles at each stage and the recovery water temperature. But aquifer thickness and hydraulic anisotropy have a minimal effect on the performance of ATES systems.

참고문헌 (14)

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