将干蒸汽注入储层而不在井中凝结的问题

IF 1 4区 物理与天体物理 Q4 PHYSICS, APPLIED
M. G. Alishaev, A. A. Aliverdiev, V. D. Beibalaev
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引用次数: 0

摘要

摘要 针对干蒸汽注入的情况,对沿井筒的温度损失进行了研究,以确定在不产生冷凝的情况下将蒸汽输送到井底的可能性。假设岩石中的温度随地热梯度的增加而增加,蒸汽流量恒定,顶部的蒸汽温度高且干燥,不含水滴。在到达底部的过程中,蒸汽温度降低,但尚未达到饱和点。岩石中的热量损失是通过公认的公式计算得出的。确定井内蒸汽开始凝结点的位置。按油田最可能的流量进行计算:25、50、75 和 100 吨/天。干蒸汽的热容量被认为是恒定的,这只有在压力较低时才能接受,最高可达 3-4 兆帕。在这种情况下,可以提出整个井串蒸汽温度分布的公式,并通过分析解决问题。然而,在压力较高的情况下,有必要考虑蒸汽热容量的热依赖性,并使用数值方法来计算温度分布。根据计算出的变量,可以得出向储层全量供应相变热量的可能性。如果储油层渗透率高且靠近地表,那么我们就有希望将相变热量完全输送到储油层。在地层深度大于 500 米时,蒸汽会在井筒中完全凝结。相变热量进入岩石。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Problem of Injection of Dry Steam into a Reservoir without Condensation in the Well

Problem of Injection of Dry Steam into a Reservoir without Condensation in the Well

Abstract

Temperature losses along a well string are investigated for the case of dry steam injection in order to determine the possibility of its delivery to the well bottom without condensation. It is assumed that in the rock, the temperature increases with increasing depth according to the geothermal gradient, the steam flow is constant, the steam at the head has a high temperature and is dry, containing no water droplets. On the way to the bottom, the steam temperature decreases, but does not yet reach the saturation point. Heat loss into rock is calculated using the generally accepted formula. The position of the point where steam condensation begins in the well is determined. Calculations are carried out for the most probable flow rates in the fields: 25, 50, 75, and 100 t/day. The heat capacity of dry steam is considered constant, which is acceptable only for low pressures, up to 3–4 MPa. In this case, a formula is proposed for the steam temperature distribution throughout the well string and the problem is solved analytically. However, at elevated pressures, it is necessary to take into account the thermal dependence of the heat capacity of steam and use a numerical method to find the temperature distribution. Based on the calculated variants, a conclusion is made about the possibility of supplying the amount of phase transition heat to the reservoir in full. If the reservoir is highly permeable and lies close to the surface, then we can hope for complete delivery of the phase transition heat to the reservoir. At formation depths greater than 500 m, steam is completely condensed in the well string. The heat of the phase transition enters the rock.

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来源期刊
High Temperature
High Temperature 物理-物理:应用
CiteScore
1.50
自引率
40.00%
发文量
0
审稿时长
4-8 weeks
期刊介绍: High Temperature is an international peer reviewed journal that publishes original papers and reviews written by theoretical and experimental researchers. The journal deals with properties and processes in low-temperature plasma; thermophysical properties of substances including pure materials, mixtures and alloys; the properties in the vicinity of the critical point, equations of state; phase equilibrium; heat and mass transfer phenomena, in particular, by forced and free convections; processes of boiling and condensation, radiation, and complex heat transfer; experimental methods and apparatuses; high-temperature facilities for power engineering applications, etc. The journal reflects the current trends in thermophysical research. It presents the results of present-day experimental and theoretical studies in the processes of complex heat transfer, thermal, gas dynamic processes, and processes of heat and mass transfer, as well as the latest advances in the theoretical description of the properties of high-temperature media.
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