Three Dimensional Thermal Model of Newberry Volcano, Oregon
Abstract
Final results of a 3D finite difference thermal model of Newberry Volcano, Oregon. Model data are formatted as a text file with four data columns (X, Y, Z, T). X and Y coordinates are in UTM (NAD83 Zone 10N), Z is elevation from mean sea level (meters), T is temperature in deg C. Model is 40km X 40km X 12.5 km, grid node spacing is 100m in X, Y, and Z directions. A symmetric cylinder shaped magmatic heat source centered on the present day caldera is the modeled heat source. The center of the modeled body is a 1700 m (elevation) and is 600m thick with a radius of 8700m. This is the best fit results from 2D modeling of the west flank of the volcano. The model accounts for temperature dependent thermal properties and latent heat of crystallization. For additional details, assumptions made, data used, and a discussion of the validity of the model see Frone, 2015 (Link below).
 Authors:
 Publication Date:
 Other Number(s):
 730
 DOE Contract Number:
 EE0002833
 Research Org.:
 USDOE Geothermal Data Repository (United States); AltaRock Energy Inc
 Sponsoring Org.:
 USDOE Office of Energy Efficiency and Renewable Energy (EERE), Geothermal Technologies Program (EE2C)
 Collaborations:
 AltaRock Energy Inc
 Subject:
 15 Geothermal Energy
 Keywords:
 geothermal; Newberry Volcano; 3D Model; NEWGEN; EGS; thermal; model; Newberry; 3D; finite difference; IET; exploration
 Geolocation:
 43.91666667,121.033333343.51666667,121.033333343.51666667,121.433333343.91666667,121.433333343.91666667,121.0333333
 OSTI Identifier:
 1254442
 DOI:
 https://doi.org/10.15121/1254442
 Project Location:

Citation Formats
Cladouhos, Trenton. Three Dimensional Thermal Model of Newberry Volcano, Oregon. United States: N. p., 2015.
Web. doi:10.15121/1254442.
Cladouhos, Trenton. Three Dimensional Thermal Model of Newberry Volcano, Oregon. United States. doi:https://doi.org/10.15121/1254442
Cladouhos, Trenton. 2015.
"Three Dimensional Thermal Model of Newberry Volcano, Oregon". United States. doi:https://doi.org/10.15121/1254442. https://www.osti.gov/servlets/purl/1254442. Pub date:Fri Jan 30 00:00:00 EST 2015
@article{osti_1254442,
title = {Three Dimensional Thermal Model of Newberry Volcano, Oregon},
author = {Cladouhos, Trenton},
abstractNote = {Final results of a 3D finite difference thermal model of Newberry Volcano, Oregon. Model data are formatted as a text file with four data columns (X, Y, Z, T). X and Y coordinates are in UTM (NAD83 Zone 10N), Z is elevation from mean sea level (meters), T is temperature in deg C. Model is 40km X 40km X 12.5 km, grid node spacing is 100m in X, Y, and Z directions. A symmetric cylinder shaped magmatic heat source centered on the present day caldera is the modeled heat source. The center of the modeled body is a 1700 m (elevation) and is 600m thick with a radius of 8700m. This is the best fit results from 2D modeling of the west flank of the volcano. The model accounts for temperature dependent thermal properties and latent heat of crystallization. For additional details, assumptions made, data used, and a discussion of the validity of the model see Frone, 2015 (Link below).},
doi = {10.15121/1254442},
journal = {},
number = ,
volume = ,
place = {United States},
year = {2015},
month = {1}
}