Bo Liu , Weifeng Jing , Daixi Long , Jiahong Li , Dan Ding , Kunpeng Cai
{"title":"Long-term simulation of process and hydrogeochemistry of gas field produced water reinjection into a limestone reservoir","authors":"Bo Liu , Weifeng Jing , Daixi Long , Jiahong Li , Dan Ding , Kunpeng Cai","doi":"10.1016/j.pce.2025.103976","DOIUrl":null,"url":null,"abstract":"<div><div>Large water volumes have been injected to enhance oil and gas recovery. However, the generated oil or gas-produced water (GPW) may contain undesirable and harmful substances. Reinjection of GPW into suitable subsurface formations is considered an effective disposal method. In this study, a numerical model of vertical-radial two dimensional well flow was developed to explore the long-term process and hydrogeochemistry of GPW reinjection into a limestone formation, which is considered as a homogeneous equal thickness reservoir. The obtained results indicated that there was an increase in the reservoir pressure at the reinjection well from 150 to 251.4 Bar at a reinjection rate of 300 m<sup>3</sup>/day. The pressure propagation range extended up to approiximately 3300 m during the injection. Calcite volume caused a maximum volume fraction change of −0.91, corresponding to a dissolution rate of 0.083/year, which increased the reservoir porosity to over 0.9. Reservoir pH values were altered within 90 m of the reinjection well as a result of water-rock interaction. Additionally, concentrations of Ca<sup>2+</sup>, Mg<sup>2+</sup>, Na<sup>+</sup>, Cl<sup>−</sup>, HCO<sub>3</sub><sup>−</sup>, and SO<sub>4</sub><sup>2−</sup> in the reservoir were affected within 2000–3000 m from the reinjection well due to injection pressure, water-rock interactions, and diffusion. This study provides insights into assessing the environmental behaviors of GPW in reservoirs, and ensuring safe, and effective long-term GPW reinjection; though accuracy and reliability of the model requires further validation using practical monitoring data in the future.</div></div>","PeriodicalId":54616,"journal":{"name":"Physics and Chemistry of the Earth","volume":"139 ","pages":"Article 103976"},"PeriodicalIF":4.1000,"publicationDate":"2025-05-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Physics and Chemistry of the Earth","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1474706525001263","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 0
Abstract
Large water volumes have been injected to enhance oil and gas recovery. However, the generated oil or gas-produced water (GPW) may contain undesirable and harmful substances. Reinjection of GPW into suitable subsurface formations is considered an effective disposal method. In this study, a numerical model of vertical-radial two dimensional well flow was developed to explore the long-term process and hydrogeochemistry of GPW reinjection into a limestone formation, which is considered as a homogeneous equal thickness reservoir. The obtained results indicated that there was an increase in the reservoir pressure at the reinjection well from 150 to 251.4 Bar at a reinjection rate of 300 m3/day. The pressure propagation range extended up to approiximately 3300 m during the injection. Calcite volume caused a maximum volume fraction change of −0.91, corresponding to a dissolution rate of 0.083/year, which increased the reservoir porosity to over 0.9. Reservoir pH values were altered within 90 m of the reinjection well as a result of water-rock interaction. Additionally, concentrations of Ca2+, Mg2+, Na+, Cl−, HCO3−, and SO42− in the reservoir were affected within 2000–3000 m from the reinjection well due to injection pressure, water-rock interactions, and diffusion. This study provides insights into assessing the environmental behaviors of GPW in reservoirs, and ensuring safe, and effective long-term GPW reinjection; though accuracy and reliability of the model requires further validation using practical monitoring data in the future.
期刊介绍:
Physics and Chemistry of the Earth is an international interdisciplinary journal for the rapid publication of collections of refereed communications in separate thematic issues, either stemming from scientific meetings, or, especially compiled for the occasion. There is no restriction on the length of articles published in the journal. Physics and Chemistry of the Earth incorporates the separate Parts A, B and C which existed until the end of 2001.
Please note: the Editors are unable to consider submissions that are not invited or linked to a thematic issue. Please do not submit unsolicited papers.
The journal covers the following subject areas:
-Solid Earth and Geodesy:
(geology, geochemistry, tectonophysics, seismology, volcanology, palaeomagnetism and rock magnetism, electromagnetism and potential fields, marine and environmental geosciences as well as geodesy).
-Hydrology, Oceans and Atmosphere:
(hydrology and water resources research, engineering and management, oceanography and oceanic chemistry, shelf, sea, lake and river sciences, meteorology and atmospheric sciences incl. chemistry as well as climatology and glaciology).
-Solar-Terrestrial and Planetary Science:
(solar, heliospheric and solar-planetary sciences, geology, geophysics and atmospheric sciences of planets, satellites and small bodies as well as cosmochemistry and exobiology).