Field demonstration of the combined use of thermally-degrading and cation-exchanging tracers to predict thermal drawdown in a geothermal reservoir

Author:

Reimus Paul,Caporuscio Florie,Marina Oana,Janney David

Funder

Los Alamos National Laboratory New Mexico Small Business Assistance Program

U.S. Department of Energy, Office of Energy Efficiency and Renewable Energy, Geothermal Technologies Office

Publisher

Elsevier BV

Subject

Geology,Geotechnical Engineering and Engineering Geology,Renewable Energy, Sustainability and the Environment

Reference14 articles.

1. Laboratory experiments to characterize cation-exchanging tracer behavior for fracture surface area estimation at Newberry Crater, OR;Dean;Geothermics,2015

2. A HPLC method for the quantification of butyramide and acetamide at ppb levels in hydrogeothermal waters;Elias;Anal. Methods,2012

3. Geology and Geothermal Waters of Lightning Dock Region, Animas Valley and Pyramid Mountains, Hidalgo County, New Mexico, Circular 177;Elston,1983

4. Ion-product constant of water to 350 deg;Fisher;J. Phys. Chem.,1972

5. Klondike basin-late Laramide depocenter in southern New Mexico;Lawton;New Mexico Geol.,1992

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