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Environmental chemistry, geochemistry, and reactive transport; with focused application on subsurface energy technologies such as sequestration of carbon dioxide.
Her work focuses on the environmental challenges of subsurface energy technologies such as geologic sequestration of carbon dioxide, geothermal energy production, and hydrofracking for shale gas extraction.
The ability to form C/W foams at high temperatures is of interest for a variety of applications in chemical synthesis, separations, materials science, and subsurface energy production.
To assess possible environmental impacts and manage subsurface energy resources, collecting data from operating shallow geothermal systems is becoming mandatory in Europe.
Fracture of heterogeneous materials has emerged as a critical issue in many engineering applications, ranging from subsurface energy to biomedical applications, and requires a rational framework that allows linking local fracture processes with global fracture descriptors such as the energy release rate, fracture energy and fracture toughness.
Haehnlein et al. (2010) reviewed the legal status of the use of geothermal energy in 46 countries and found that in 35 of those countries, there were no regulations or recommendations for subsurface energy use.
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Existing approaches for exploration of shallow subsurface geothermal energy storage often lack the ability to provide information concerning the spatial variability of thermal storage parameters.
Cliff Voss, a senior scientist with the hydrological research program of the U.S. Geological Survey (USGS), has over 30 years of project management/implementation and research experience in groundwater resources development and in use of the subsurface for energy production and waste isolation.
It discusses the importance of quantifying flow processes in porous and fractured reservoirs to scientific understandings and engineering applications in many fields, including petroleum engineering, groundwater and vadose zone hydrology, soil sciences, geothermal energy, subsurface contamination investigation and remediation, and resource storage or waste disposal.
These equations are used to the modeling of transformation of pollutants, energy, subsurface water flows, deeper river flows, streams, and groundwater [4, 11, 12, 19, 23].
The distribution of temperature anomalies within the subsurface during geothermal energy production depends on the rate of injection, operational methods and subsurface conditions, which if not properly assessed, may not only influence the performance of neighboring geothermal systems but also pose a serious threat to surrounding ecosystems.
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