D. Nicolás Espinoza

ORCID: 0000-0002-3418-0180
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About
Contact & Profiles
Research Areas
  • Hydraulic Fracturing and Reservoir Analysis
  • Drilling and Well Engineering
  • CO2 Sequestration and Geologic Interactions
  • Rock Mechanics and Modeling
  • Hydrocarbon exploration and reservoir analysis
  • Methane Hydrates and Related Phenomena
  • Enhanced Oil Recovery Techniques
  • Seismic Imaging and Inversion Techniques
  • Coal Properties and Utilization
  • Groundwater flow and contamination studies
  • Landslides and related hazards
  • Climate Change Communication and Perception
  • Atmospheric and Environmental Gas Dynamics
  • BRCA gene mutations in cancer
  • Reservoir Engineering and Simulation Methods
  • Geoscience and Mining Technology
  • Tunneling and Rock Mechanics
  • Geological Modeling and Analysis
  • Lattice Boltzmann Simulation Studies
  • earthquake and tectonic studies
  • Phase Equilibria and Thermodynamics
  • Geophysical Methods and Applications
  • Eosinophilic Disorders and Syndromes
  • Granular flow and fluidized beds
  • Geothermal Energy Systems and Applications

The University of Texas at Austin
2015-2024

National Institute of Allergy and Infectious Diseases
2023

National Institutes of Health
2023

National Health and Medical Research Council
2022

The University of Sydney
2022

Laboratoire Navier
2013-2014

Centre National de la Recherche Scientifique
2013-2014

Georgia Institute of Technology
2009-2012

Methane gas hydrates, crystalline inclusion compounds formed from methane and water, are found in marine continental margin permafrost sediments worldwide. This article reviews the current understanding of phenomena involved hydrate formation physical properties hydrate‐bearing sediments. Formation include pore‐scale habit, solubility, spatial variability, host sediment aggregate properties. Physical thermal properties, permeability, electrical conductivity permittivity, small‐strain elastic...

10.1029/2008rg000279 article EN Reviews of Geophysics 2009-12-01

The interfacial interaction between mineral surfaces and immiscible fluids determines the efficiency of enhanced oil or gas recovery operations as well our ability to inject store CO 2 in geological formations. Previous studies have shown that tension contact angle ‐water‐mineral systems change noticeably with fluid pressure. We compile previous results extend scope available data include saline water, different substrates (quartz, calcite, oil‐wet quartz, polytetrafluoroethylene (PTFE)), a...

10.1029/2009wr008634 article EN Water Resources Research 2010-07-01

Small pores in high specific surface clay-rich caprocks give rise to capillary entry pressures and viscous drag that hinder the migration of buoyant carbon dioxide CO2. We measured breakthrough pressure ensuing CO2 permeability through sediment plugs prepared with sand, silt, kaolinite smectite, monitored their volumetric deformation using high-pressure oedometer cells. The data show water expulsion contraction prior breakthrough, followed by preferential flow thereafter. Our experimental...

10.1016/j.ijggc.2017.09.019 article EN cc-by-nc-nd International journal of greenhouse gas control 2017-10-23

The injection of carbon dioxide, CO 2 , into methane hydrate‐bearing sediments causes the release methane, CH 4 and formation dioxide hydrate, even if global pressure‐temperature conditions remain within hydrate stability field. This phenomenon, known as ‐CO exchange or replacement, creates a unique opportunity to recover an energy resource, while entrapping greenhouse gas, dioxide. Multiple coexisting processes are involved during including heat liberation, mass transport, volume change,...

10.1029/2009jb000812 article EN Journal of Geophysical Research Atmospheres 2010-10-01

Abstract This work uses X‐ray computed micro‐tomography (μCT) to monitor xenon hydrate growth in a sandpack under the excess gas condition. The μCT images give pore‐scale distribution and pore habit space time. We use lattice Boltzmann method calculate relative permeability (k rg ) as function of saturation (S hyd structure experimental hydrate‐bearing sand retrieved from data. results suggest k ‐ S data fit well new model = (1‐S )·exp(–4.95·S rather than simple Corey model. In addition, we...

10.1002/2017wr021851 article EN publisher-specific-oa Water Resources Research 2017-12-28

10.1007/s12205-011-0011-9 article EN cc-by-nc-nd KSCE Journal of Civil Engineering 2011-04-01

10.1016/j.ijggc.2011.02.006 article EN International journal of greenhouse gas control 2011-04-14

10.1016/j.ijggc.2024.104160 article EN International journal of greenhouse gas control 2024-05-23

Understanding the adsorption‐induced swelling in coal is critical for predictable and enhanced bed methane production. The matrix a natural anisotropic disordered microporous solid. We develop an elastic transverse isotropic poromechanical model solids which couples adsorption strain through stress functions expresses isotherm as multivariate function depending on fluid pressure solid strains. Experimental data from literature help invert adsorptive‐mechanical properties of Brzeszcze samples...

10.1002/2013jb010337 article EN Journal of Geophysical Research Solid Earth 2013-12-01

Nanoparticle-Stabilized Supercritical CO2 Foams for Potential Mobility Control Applications David Espinosa; Espinosa Dept. of Petroleum & Geosystems Eng. Search other works by this author on: This Site Google Scholar Federico Caldelas; Caldelas Keith Johnston; Johnston Steven L. Bryant; Bryant Chun Huh Paper presented at the SPE Improved Oil Recovery Symposium, Tulsa, Oklahoma, USA, April 2010. Number: SPE-129925-MS https://doi.org/10.2118/129925-MS Published: 24 2010 Cite View Citation Add...

10.2523/129925-ms article EN Proceedings of SPE Improved Oil Recovery Symposium 2010-04-01
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