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An analytical method to determine rock spallation temperature and degree of heterogeneity in thermal spallation drilling for geothermal energy

机译:确定地热能的热剥落钻井过程中岩石剥落温度和非均质程度的分析方法

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摘要

Thermal spallation drilling is an alternative technology expected to be suitable for exploitation of geothermal energy in hard, polycrystalline rocks. The rock spallation temperature and degree of heterogeneity are two important parameters for spallation studies. The rock spallation temperature can offer guidance to provide a suitable temperature environment for different formations, and the degree of heterogeneity plays an important role in determining the spallability of rock. However, it is difficult to measure the rock's surface temperature at the onset of initial spallation and there is no universal method to determine the degree of heterogeneity of rock. This paper intends to provide a convenient analytical approach to approximate the rock spallation temperature and degree of heterogeneity for field applications. Based on the Weibull statistical theory of tensile failure, the rock temperature at spallation can be obtained by solving a set of over-determined equations. All other rock properties can be calculated based on the temperature, and then the degree of heterogeneity of rock can be determined. Compared with experimental data, the calculated rock spallation temperature and degree of heterogeneity are all within acceptable ranges. All results in this paper can provide implications for further study on thermal spallation drilling in geothermal reservoirs.
机译:热散裂钻探是一种替代技术,有望适合在硬质多晶岩石中开采地热能。岩石剥落温度和非均质程度是剥落研究的两个重要参数。岩石剥落温度可为为不同地层提供合适的温度环境提供指导,并且非均质程度在确定岩石的可剥落性方面起着重要作用。然而,在初始剥落开始时很难测量岩石的表面温度,并且没有通用的方法来确定岩石的非均质程度。本文旨在为现场应用提供一种方便的分析方法,以近似岩石剥落温度和非均质程度。基于拉力破坏的威布尔统计理论,可以通过求解一组超定方程来获得层裂时的岩石温度。可以基于温度计算所有其他岩石属性,然后可以确定岩石的非均质程度。与实验数据相比,计算出的岩片温度和非均质度均在可接受范围内。本文的所有结果可为进一步研究地热储层中的热层裂钻探提供启示。

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