PMID- 37270981 OWN - NLM STAT- MEDLINE DCOM- 20230622 LR - 20230622 IS - 1095-8630 (Electronic) IS - 0301-4797 (Linking) VI - 342 DP - 2023 Sep 15 TI - Effect of type of ion and temperature on fines migration induced by mineral reactions during water injection into carbonate rocks. PG - 118193 LID - S0301-4797(23)00981-7 [pii] LID - 10.1016/j.jenvman.2023.118193 [doi] AB - Managed aquifer recharge is a water storage and recovery method. However, fines migration during water injection can significantly affect formation permeability. Several studies have analyzed fines migration in sandstone and soil samples, but few studies have investigated fines migration in carbonate rocks. In addition, the effect of neither temperature nor type of ion on fines migration has been investigated in carbonate rocks. Our experiments use filtered-deaired distilled water and pure salts to prepare the injection fluids. Rock samples are injected with 0.63 mol/L brine followed by four sequential injections of diluted brine: 0.21 mol/L, 0.1 mol/L, 0.05 mol/L, and 0 mol/L (distilled water). Pressure difference is recorded across the rock sample throughout each experimental run and used to calculate permeability. Effluent is collected to characterize produced fines and elements. pH and particle concentration measurements are collected frequently. Scanning electron microscope (SEM) images of inlet and outlet faces pre- and post-injection were taken to observe any changes. For the experimental runs performed at 25 degrees C, permeability decrease was 99.92% of the original permeability for seawater experimental run, 99.96% for NaCl brine experimental run, and nearly zero for CaCl(2) brine experimental run. For CaCl(2) brine experimental run, the only observed mineral reaction is mineral dissolution. For NaCl brine and seawater experimental runs, both mineral dissolution and cation exchange are observed, of which the latter appears to be the main mechanism for fines migration. Due to mineral dissolution, permeability increase is observed during 0.21 mol/L and 0.1 mol/L injection at high temperature. However, during distilled water injection, permeability decrease is found to be similar at both low and high temperatures. CI - Copyright (c) 2023 The Authors. Published by Elsevier Ltd.. All rights reserved. FAU - Almutairi, Abdulmajeed AU - Almutairi A AD - School of Minerals and Energy Resources Engineering, University of New South Wales, Sydney, NSW, 2052, Australia. FAU - Wang, Yamin AU - Wang Y AD - School of Minerals and Energy Resources Engineering, University of New South Wales, Sydney, NSW, 2052, Australia; Institute of Energy, Peking University, Beijing 100871, PR China. FAU - Le-Hussain, Furqan AU - Le-Hussain F AD - School of Minerals and Energy Resources Engineering, University of New South Wales, Sydney, NSW, 2052, Australia. Electronic address: furqan.hussain@unsw.edu.au. LA - eng PT - Journal Article DEP - 20230607 PL - England TA - J Environ Manage JT - Journal of environmental management JID - 0401664 RN - 0 (brine) RN - 059QF0KO0R (Water) RN - 451W47IQ8X (Sodium Chloride) RN - M4I0D6VV5M (Calcium Chloride) RN - 0 (Minerals) RN - 0 (Carbonates) SB - IM MH - Temperature MH - *Water MH - *Sodium Chloride MH - Calcium Chloride MH - Minerals/chemistry MH - Carbonates/chemistry OTO - NOTNLM OT - Carbonate reservoirs OT - Cation exchange OT - Fines migration OT - Permeability decrease COIS- Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper. EDAT- 2023/06/05 00:41 MHDA- 2023/06/22 06:42 CRDT- 2023/06/04 18:05 PHST- 2022/09/30 00:00 [received] PHST- 2023/05/02 00:00 [revised] PHST- 2023/05/15 00:00 [accepted] PHST- 2023/06/22 06:42 [medline] PHST- 2023/06/05 00:41 [pubmed] PHST- 2023/06/04 18:05 [entrez] AID - S0301-4797(23)00981-7 [pii] AID - 10.1016/j.jenvman.2023.118193 [doi] PST - ppublish SO - J Environ Manage. 2023 Sep 15;342:118193. doi: 10.1016/j.jenvman.2023.118193. Epub 2023 Jun 7.