The critical role of mineral heterogeneity in low-salinity water flooding in tight sandstones: Insights from molecular dynamics simulations

The microscopic mechanisms by which mineral composition governs the efficiency of low-salinity water flooding in tight sandstone reservoirs remain inadequately understood. In this study, molecular dynamics simulations were conducted to construct crude oil (acetic acid, toluene, n-heptane, and n-decane)-mineral (quartz, K-feldspar, and kaolinite) adsorption models, along with oil–water–rock desorption models under varying salinity conditions. By analyzing parameters such as relative concentration profiles, binding energies, centroid displacements, and hydrogen bonds, the competitive adsorption mechanisms between dissolved ions and crude oil components were systematically elucidated. The results indicate that polar components (acetic acid and toluene) exhibit stronger adsorption stability on mineral surfaces than non-polar components (n-decane and n-heptane). Due to chain folding optimizing interfacial contact, n-decane shows slightly higher stability than n-heptane. On quartz surfaces, low salinity promotes efficient crude oil desorption through double-layer expansion and disruption of ionic bridges. For K-feldspar, low salinity facilitates desorption via interlayer K+ exchange. For kaolinite, however, electrostatic-dispersive synergistic adsorption restrains desorption under low-salinity conditions, leading to residual acetic acid retention. The adsorption–desorption responses to salinity are controlled by mineral-specific surface heterogeneity, manifested by polar Si–OH groups on quartz, Al–OH2+ sites on kaolinite, and interstratified K+ in K-feldspar, which lead to hydrogen bond breaking, electrostatic-dispersive synergy, and controlled K+ release, respectively. This study clarifies the coupling between mineral type, salinity, and desorption behavior, providing molecular-level theoretical underpinnings for the application of low-salinity water flooding in tight sandstone reservoirs.

Authors

Institutions

Publication Details

Journal
Physics of Fluids
Published
2025-11-01
DOI
https://doi.org/10.1063/5.0303224
Primary Topic
Enhanced Oil Recovery Techniques
Type
article
Field-Weighted Citation Impact
0.00
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

The critical role of mineral heterogeneity in low-salinity water flooding in tight sandstones: Insights from molecular dynamics simulations

Ruicheng Zhao, Maozong Gan, Pingtian Fan, Liang Xue et al.
Physics of Fluids
Enhanced Oil Recovery Techniques
article

The critical role of mineral heterogeneity in low-salinity water flooding in tight sandstones: Insights from molecular dynamics simulations

Ruicheng Zhao, Maozong Gan, Pingtian Fan, Liang Xue, Yuetian Liu, Feihe Xiang
article en

Abstract

The microscopic mechanisms by which mineral composition governs the efficiency of low-salinity water flooding in tight sandstone reservoirs remain inadequately understood. In this study, molecular dynamics simulations were conducted to construct crude oil (acetic acid, toluene, n-heptane, and n-decane)-mineral (quartz, K-feldspar, and kaolinite) adsorption models, along with oil–water–rock desorption models under varying salinity conditions. By analyzing parameters such as relative concentration profiles, binding energies, centroid displacements, and hydrogen bonds, the competitive adsorption mechanisms between dissolved ions and crude oil components were systematically elucidated. The results indicate that polar components (acetic acid and toluene) exhibit stronger adsorption stability on mineral surfaces than non-polar components (n-decane and n-heptane). Due to chain folding optimizing interfacial contact, n-decane shows slightly higher stability than n-heptane. On quartz surfaces, low salinity promotes efficient crude oil desorption through double-layer expansion and disruption of ionic bridges. For K-feldspar, low salinity facilitates desorption via interlayer K+ exchange. For kaolinite, however, electrostatic-dispersive synergistic adsorption restrains desorption under low-salinity conditions, leading to residual acetic acid retention. The adsorption–desorption responses to salinity are controlled by mineral-specific surface heterogeneity, manifested by polar Si–OH groups on quartz, Al–OH2+ sites on kaolinite, and interstratified K+ in K-feldspar, which lead to hydrogen bond breaking, electrostatic-dispersive synergy, and controlled K+ release, respectively. This study clarifies the coupling between mineral type, salinity, and desorption behavior, providing molecular-level theoretical underpinnings for the application of low-salinity water flooding in tight sandstone reservoirs.

Physics of FluidsVol. 37(11)
China University of Petroleum, Beijing (CN), China National Petroleum Corporation (China) (CN)
Openalex Percentile: Top 57%
Enhanced Oil Recovery Techniques
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.