TY -的A2 -徐,金泽国际非盟-气,王盟,Dongxu周盟——佳佳,廖盟——Yuntao刘盟-信义,王PY - 2023 DA - 2023/06/19 TI -储层温度计算和建模对流地热系统:案例研究的五大温泉在庐山,河南,中国SP - 7149973六世- 2023 AB -蓄热器的温度和水岩相互作用过程的庐山对流地热系统(在中国秦岭地层分带断裂带)澄清表面用冷水和地热流体为研究对象。在这项研究中,温度曲线的概念模型研究区地热系统的开发使用表面温度反演,阳离子温标,SiO₂温标法、矿物平衡阶段法,silicon-enthalpy模型,FixAl方法,和Cl-enthalpy模型。表面的转化温度的范围33-39°C,和温度差异表明Checun-Lushan断裂的方向。从大气降水研究领域是充电,充电区域的温度大约是5.8 - -7.7°C(碱场的温度大约是10°C),和充电海拔约1200米。蓄热器模式在研究区近地表热液蓄热器转移到浅蓄热器,然后深蓄热器。近地表热液蓄热器温度的恒温60°C,和浅热存储温度计算K-Mg和Li-Mg地温计99到112°C。蓄热器的温度使用FixAl模拟方法,用偏差值从2.9%到15.0%不等。silicon-enthalpy模型计算深蓄热器温度之间的181和230°C。在研究区地热水的混合比非常高,冷水混合比为85.4 -94.8%。主场流体温度估计大约282°C使用Cl-enthalpy模型。主热导电率控制信道的研究区域是Checun-Lushan断裂带。 The water vapor formed by convection at depth moves upward to approximately 5 km to form a deep thermal reservoir, and this convection and upward movement cause it to mix with cold water from the fracture zone to form a shallow thermal reservoir, which moves to the near-surface, forming a hydrothermal-type reservoir, which is later discharged in the form of a spring. The conceptual model of geothermal system temperature established in this study provides a basis for further development and utilization of Lushan hot springs and provides guidance for future thermal storage temperature calculations of convection-type geothermal systems in uplifted mountains. SN - 1468-8115 UR - https://doi.org/10.1155/2023/7149973 DO - 10.1155/2023/7149973 JF - Geofluids PB - Hindawi KW - ER -