Investigation of formation water evaporation behavior and its impact on CO2 storage within aquifers

0 ENERGY & FUELS
Fuzhen Chen , Lijuan Yang , Xiaohu Bai , Pengfei Liu , Zhihao He , Jianwei Gu
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引用次数: 0

Abstract

Evaporation is one of the primary mechanisms in subsurface fluid migration, prevalent in gas-liquid multiphase flow processes within porous media. However, less emphasis has been placed on fluid evaporation during its flow from well to formation. This study investigates the behavior of formation water evaporation and its impact on CO2 storage through high-volume CO2 displacement experiments coupled with online nuclear magnetic resonance testing. The retrograde crossover phenomenon of water recovery under varying temperatures is observed during high-volume CO2 displacement. The color change in silica gel provides clear evidence of formation water evaporation which leads to the crossover. Initially, formation water migration is primarily driven by CO2 displacement; however, as gas saturation exceeds 40 %, evaporation replacing displacement becomes the dominant migration mechanism. The primary migration mechanism shifts during this process. Evaporation typically occurs at inlet of the core, or near-wellbore area in field applications. Pronounced CO2 override flow phenomenon is observed, which significantly enhances the water evaporation and gas channeling in the upper part of porous media. A sufficient cumulative CO2 injection volume is necessary for significant formation water evaporation. Increasing temperature within an enclosed space does not significantly enhance water evaporation. Conversely, both isothermal depressurization and vacuum evacuation with an open boundary can markedly increase water evaporation. These outcomes document that open boundary, fluid flow, and high-volume CO2 injection are prerequisites for effective formation water evaporation. Furthermore, high formation temperature, large pressure difference, and slow injection speed promote earlier and more intense formation water evaporation. The effects of evaporation on filtration are twofold: on one hand, the reduction in irreducible water saturation enhances permeability; on the other hand, salt precipitation resulting from evaporation decreases permeability. Therefore, rationally utilizing formation water evaporation mechanism can lower flow resistance near wellbore, reduce injection pressure, improve sweep efficiency, and increase CO2 storage capacity.
地层水蒸发行为及其对含水层CO2储存影响的研究
蒸发是地下流体运移的主要机制之一,普遍存在于多孔介质中的气液多相流过程中。然而,很少有人重视流体从井流向地层过程中的蒸发。本研究通过大容量CO2驱油实验结合在线核磁共振测试,研究地层水蒸发行为及其对CO2储存量的影响。在大排量CO2驱替过程中,观察到不同温度下水采收率的逆行交叉现象。硅胶的颜色变化提供了地层水蒸发导致交叉的明确证据。最初,地层水运移主要由CO2驱替驱动;当含气饱和度超过40%时,蒸发取代驱替成为主导运移机制。在此过程中,主要迁移机制发生了变化。在现场应用中,蒸发通常发生在岩心入口或近井区域。明显的CO2超流现象显著增强了孔隙介质上部的水分蒸发和气体窜动。足够的累积CO2注入量对于显著的地层水蒸发是必要的。提高封闭空间内的温度不会显著提高水的蒸发。相反,等温降压和开放边界的真空抽真空都能显著增加水的蒸发。这些结果表明,开放边界、流体流动和大量二氧化碳注入是有效蒸发地层水的先决条件。此外,较高的地层温度、较大的压差和较慢的注入速度会促使地层水蒸发得更早、更强烈。蒸发对过滤的影响是双重的:一方面,降低不可还原水饱和度提高渗透率;另一方面,蒸发引起的盐沉淀降低了渗透率。因此,合理利用地层水蒸发机制,可以降低井筒附近流动阻力,降低注入压力,提高波及效率,增加CO2储存量。
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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