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Reassessment of Balanced and Sustainable Thermal Output Potential and Reserves Base for Stratified Low Enthalpy Geothermal System of Besenova Elevation, Northern Slovakia

机译:北斯洛伐克北部贝斯诺瓦海洋高原分层低焓地热系统重新评估平衡和可持续的热输出潜力和储备

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In conditions of stratified reservoirs involved in the Besenova elevation low enthalpy hydrogeothermal structure, volumetric method application defines 60,74 PJ for deep and 4,27 PJ for shallow zone as recoverable heat in place. The solid body of deep reservoir in Mid Triassic carbonates of the Krizna Nappe is recognized as potential for onward development only. In terms of sustainable reservoir operation given by critical coordinate of < r_(cap) = 0,5; t_(reco) = 100 years > due to reserve capacity method, the recommended rate rises up to 9,96 MWt (55,5 l.s~(-1)). Compared to actual study defining an extraction capacity for 6,3 MWt or 35,8 1.s~(-1), the potential for development represents 3,31 MWt equal to 19,9 l.s~(-1). In that case, the deep reservoir would require 66 years to recover into initial conditions after operated at the constant pace for 100 years, if energy balance approach (production ratio) is accepted.
机译:在涉及Besenova高度低焓水管地热结构的分层储层的条件下,体积方法应用为深度和4,27 PJ为浅区定义为60,74pj,作为可恢复的热量。 Krizna Nappe中三叠系碳酸盐中的深层水库的固体被认为仅作为上行发展的潜力。 就r_(帽)= 0,5的临界坐标给出的可持续水库操作而言; T_(RECO)= 100年>由于储备容量法,建议率高达9,96 MWT(55,5 L.S〜(-1))。 与实际研究相比,定义了6,3 MWT或35,8.1.S〜(-1)的提取能力,显影潜力代表3,31MWt等于19,91s〜(-1)。 在这种情况下,如果可接受能量平衡方法(生产比率),深水库将需要66年恢复到运营后的初始条件后,如果能量平衡方法(生产比率)被接受。

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