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Development of a new simple hydrostatic equilibrium model for sustainable evaluation in geothermal energy

机译:地热能可持续评价新简易静液压平衡模型的发展

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Geothermal energy is a renewable energy, that is, the energy removed from the geothermal reservoir is continuously replaced on time scales similar to those required for energy removal. Replacement energy to the geothermal reservoir is supplied by fluid of natural recharge and injection. Sustainable geothermal utilization is the ideal condition of the applied production system to sustain the stable production level over long times. It is very important to manage the mass balance between production, injection and natural recharge in the geothermal reservoir to maintain sustainability during exploitation. A new simple hydrostatic equilibrium model is developed by this mass balance model of geothermal reservoir. This paper builds up a new simple hydrostatic equilibrium model to consider hydrostatic connection between recharged reservoir and discharged reservoir. Principle of fluid-pressure transmission states that pressure exerted anywhere in a confined incompressible fluid is transmitted equally in all directions. Hydrostatic equilibrium occurs when compression due to gravity is balanced by a pressure gradient force in the opposite direction. Mass changes data in this hydrostatic equilibrium model is estimated by gravity changes from repeat gravity measurement method. The equation result between production, injection and mass change rate calculates recharge factor from discharged reservoir. This model also assessed a relatively constant of entered mass flow rate from the surface that continues working during the production and injection well activity. This new simple hydrostatic equilibrium model is applied in Kamojang Geothermal Field, the geothermal reservoir with limited natural recharge.
机译:地热能是一种可再生能源,即,从地热储存器中除去的能量在类似于能量去除所需的时间尺度上连续更换。地热储层的替代能量由天然充电和注射的流体供应。可持续地热利用是应用生产系统的理想条件,以长期维持稳定的生产水平。管理地热水库生产,注射和自然补给之间的质量平衡非常重要,以在剥削期间保持可持续性。地热储层的质量平衡模型开发了一种新的简单静水压平衡模型。本文建立了一种新的简单静液压平衡模型,以考虑充电水库和排放水库之间的静压连接。流体压力传递的原理状态,施加狭窄的不可压缩流体中的任何地方的压力在所有方向上同样地传递。当由于重力引起的压缩通过相反方向的压力梯度力而平衡时,发生静水平衡。通过重量重力测量方法的重力变化估计该静水压平衡模型中的质量变化数据。生产,注射和质量变化率之间的等式导致从排出的储存器中计算充电因子。该模型还评估了在生产和注射井活动期间继续工作的表面的相对恒定的进入质量流速。这种新的简单静水平衡模型应用于Kamojang地热场,地热储层,具有有限的自然补给。

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