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Thermo-Physical and Mechanical Properties of Al Hashimiyya Basaltic Rocks, Jordan

机译:约旦Al Hashimiyya玄武岩的热物理和力学性质

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Geothermal exploration in northern Jordan is in juvenile phase. North eastern basaltic desert is expected to host, with other rock formations, a shallow geothermal field. For efficient geothermal potential evaluation, a complete understanding of thermo-physical properties of deep reservoir rocks is of utmost importance. Due to the complex technical thermo-physical evalua tions of basalts in depth, surficial basalts extending to the west were evaluated . Accordingly, six basaltic sub-flows from Al Hashimiyya were examined into their thermo-physical and mechanical properties. The flows represent the western extinction of large olivine basalt eruption. Different properties were evaluated for oven dried samples: thermal conductivity, permeability, porosity, density and specific heat capacity. In addition, basalts mechanical properties were examined : compressional wave velocity, unconfined compressive strength, indirect tensile strength and point load tests. The results were correlated in proportional patterns. They indicated that thermal conductivity of the studied basalts is dependent on porosity and permeability in parallel with mineral composition. It’s found that mechanical properties are controlled by porosity and permeability, too. The studied basalt properties exhibit slight deviation from the continental basalts thermo-physical and mechanical properties reported in the region. Thermal conductivity ranges between 1.89 and 1.32 W·m ~(-1) ·K ~(-1) , whereas the porosity and permeability averages at 10.64% and 9.75899E - 15 m ~( 2 ) , respectively. Additionally, unconfined compressive strength averages at 104.9 Mpa and it’s almost 20 times higher than indirect tensile strength which ranges from 8.73 to 2.21 Mpa. As the samples were tested under laboratory conditions, in situ conditions will not be reflected by such values. At greater depth, temperature, pressure and hydrothermal activities will certainly affect rock properties. Micro fractures, whether it will be filled or not, will affect basalts properties, too. The results of this work will be used to develop a comprehensive thermo-physico-mechanical model, and improve the ability to predict rock properties at greater depths of Jordanian basalts. ~( )
机译:约旦北部的地热勘探处于少年阶段。东北玄武岩沙漠有望与其他岩层一起形成浅层地热田。对于有效的地热潜力评估,对深层储层岩石的热物理性质的完整理解至关重要。由于对玄武岩进行了复杂的技术热物理评估,因此对延伸到西部的玄武岩进行了评估。因此,检查了来自Al Hashimiyya的6个玄武质子流的热物理性质和机械性质。洋流代表了大范围橄榄石玄武岩喷发的西部灭绝。对烘箱干燥的样品评估了不同的性能:导热率,渗透率,孔隙率,密度和比热容。此外,还检查了玄武岩的机械性能:压缩波速度,无侧限抗压强度,间接抗拉强度和点载荷试验。结果按比例相关。他们指出,所研究的玄武岩的热导率取决于孔隙率和渗透率,并与矿物组成平行。发现机械性能也受孔隙率和渗透率的控制。所研究的玄武岩性质与该地区报道的大陆玄武岩的热物理和力学性质略有偏差。导热系数在1.89和1.32 W·m〜(-1)·K〜(-1)之间,而孔隙率和渗透率分别平均为10.64%和9.75899E-15 m〜(2)。此外,无侧限抗压强度平均为104.9 Mpa,几乎比间接抗拉强度(8.73至2.21 Mpa)高20倍。由于样品是在实验室条件下测试的,因此原位条件不会反映在这些值上。在更大的深度,温度,压力和热液活动肯定会影响岩石特性。微裂缝无论是否充满,都会影响玄武岩的性质。这项工作的结果将用于建立一个综合的热物理力学模型,并提高预测约旦玄武岩深处岩石性质的能力。 〜()

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