Geometry inversion model for sediment zones of salt cavern used for natural gas storage

0 ENERGY & FUELS
Tingting Jiang , Ziqi Chi , Dongzhou Xie , Tao He , Dongling Cao
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Abstract

The utilization of sediment pore space for gas storage is an effective measure to solve the problem of high-impurity bedded salt rock gas storage construction in China. However, the existing detection methods cannot obtain the cavern geometry at the sediment zones within the gas storage, which brings significant uncertainties to the debrining process. In response to this issue, this paper innovatively establishes a model that considers sediment porous media flow for the inversion of cavern geometry and applies the model to analyze the factors that influence the debrining parameters. The results show that the average error obtained from the model inversion calculations is less than 2 % for the cavern diameter, while for predicting the depth of the gas-brine interface, the average error is less than 2.5 %. Moreover, the research indicates that the cavern geometry, the sediment surface position, the debrining rate, and the permeability of the sediments influence the debrining process. The specific change patterns of debrining parameters are mainly influenced by the sediment surface position and the cavern geometry. This paper can provide theoretical support for the utilization of sediment pores for debrining and gas storage.
天然气储盐洞沉积带几何反演模型
利用沉积物孔隙空间储气是解决中国高杂质层状盐岩储气库建设问题的有效措施。然而,现有的探测方法无法获得储气库内沉积带的洞室几何形状,这给脱泥过程带来了很大的不确定性。针对这一问题,本文创新性地建立了考虑沉积物多孔介质流动的溶洞几何反演模型,并应用该模型分析了影响脱泥参数的因素。结果表明,模型反演计算对洞室直径的平均误差小于2%,对气盐水界面深度的平均误差小于2.5%。此外,研究表明,洞室的几何形状、沉积物的表面位置、脱砂速率和沉积物的渗透率对脱砂过程有影响。脱泥参数的具体变化规律主要受沉积物表面位置和洞室几何形状的影响。本文可为利用沉积物孔隙进行脱泥和储气提供理论支持。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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