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Yue Hao

Researcher at Lawrence Livermore National Laboratory

Publications -  66
Citations -  2016

Yue Hao is an academic researcher from Lawrence Livermore National Laboratory. The author has contributed to research in topics: Carbonate & Geothermal energy. The author has an hindex of 20, co-authored 59 publications receiving 1732 citations.

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Active CO2 reservoir management for carbon storage: Analysis of operational strategies to relieve pressure buildup and improve injectivity

TL;DR: Active CO2 reservoir management (ACRM) as mentioned in this paper combines brine production with CO2 injection to relieve pressure buildup, increase injectivity, manipulate CO2 migration, and constrain brine leakage.
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CO2-induced dissolution of low permeability carbonates. Part I: Characterization and experiments

TL;DR: The effect of elevated dissolved CO2 concentrations on compositionally and structurally distinct carbonate sample cores from the Weyburn-Midale CO2enhanced oil recovery and storage site (Canada) was measured from analysis of 3-D sample characterization and fluid chemistry data from core-flood experiments as mentioned in this paper.
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Thermal drawdown-induced flow channeling in a single fracture in EGS

TL;DR: In this article, the authors investigated the effects of aperture heterogeneity on flow pattern evolution in a single fracture in a low-permeability crystalline formation and developed a numerical model on the platform of GEOS to simulate the coupled thermo-hydro-mechanical processes in a penny-shaped fracture accessed via an injection well and a production well.
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Geomechanical behavior of the reservoir and caprock system at the In Salah CO2 storage project.

TL;DR: It is suggested that the simplest and most likely explanation for the observations is that a portion of the lower caprock was hydrofractured, although interaction with preexisting fractures may have played a significant role.
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Geochemical detection of carbon dioxide in dilute aquifers

TL;DR: The ability to detect CO2 leakage from a storage reservoir to overlying dilute groundwater is dependent on CO2 solubility, leak flux, CO2 buoyancy, and groundwater flow, and simulations show that CO2 may not rise high enough in the aquifer to be detected.