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Geothermal Well Seals Subjected to Cyclic Heating and Cooling

机译:循环加热和冷却的地热井封

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This paper presents the results of a study of the effects of cyclic heating and cooling on the thermal and hydraulic conductivity properties of a geothermal well seal. In the US, bentonite is widely used in the annulus between the fluid circulating pipes and the formation for geothermal well systems and is subjected to many cycles of heating and cooling throughout the design life. In particular, the seal is expected to maintain contact with the circulating pipes and the formation in order to effect efficient transfer of heat into and out of the earth. Secondly, since many of these wells are 100 m deep and more, the seal must maintain a low hydraulic conductivity in order to isolate various aquifers over the well depth from cross-contamination. In the study, after 23 cycles of heating and cooling, the thermal conductivity remained constant but was different for cycles of heating and cooling; 0.173 W/m.K (0.1 Btu/hr ft ℉) for cooling and 0.865 W/m.K (0.5 Btu/hr ft ℉) for heating. A replicate trial yielded similar results. After 12 cycles of hydraulic conductivity testing, there appears to be some degradation in the hydraulic conductivity and intrinsic permeability.
机译:本文介绍了循环加热和冷却对地热井封的导热和水力传导特性的影响的研究结果。在美国,膨润土广泛用于流体循环管道和地热井系统地层之间的环空中,并且在整个设计生命周期中都要经历许多次加热和冷却循环。特别地,期望密封件保持与循环管和地层的接触,以实现热量有效地传递到地球和从地球传出。其次,由于许多井的深度为100 m甚至更大,因此密封件必须保持较低的水力传导率,以便将井深范围内的各种含水层与交叉污染隔离开来。在研究中,经过23个加热和冷却循环后,热导率保持不变,但加热和冷却循环则有所不同。冷却时为0.173 W / m.K(0.1 Btu / hr ft℉),加热时为0.865 W / m.K(0.5 Btu / hr ft℉)。重复试验产生了相似的结果。经过12个循环的水力传导率测试后,水力传导率和固有渗透率似乎有所下降。

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