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Title: DASH Slow Strain Rates from Brady Hot Springs Geothermal Field during PoroTomo Deployment Period

Abstract

This submission contains slow strain rates summed to radians over 30 second intervals [rad/s] derived from horizontal distributed acoustic sensing measurements (DASH) of Brady geothermal field during PoroTomo deployment (2016-Mar-14 to 2016-Mar-26). There is one file corresponding to each day written in *.mat format for use with Matlab. The format for the binary Matlab .mat files are defined at: https://www.mathworks.com/help/pdf_doc/matlab/matfile_format.pdf. One such file includes the following variables: 'flist': list of raw DASH files used in the summation 'time_tag_mdt': sample time tag in datetime format with hours given in 24-hr format (yyyy/MM/dd HH:mm:ss.SSSSSSS) 'time_tag_uts': sample time tag in Unix time 'strain_rate_summed_over30s_in_radians_per_second': slow strain rates summed over 30 second intervals in units rad/s 'sample_standard_deviation_in_radians_per_second': corresponding sample standard deviation of slow strain rates in units rad/s The PoroTomo final technical report, raw DASH data, and software repository are also available through the links below.

Creator(s)/Author(s):
ORCiD logo ; ; ORCiD logo ;
Publication Date:
Other Number(s):
1134
DOE Contract Number:  
EE0006760
Product Type:
Dataset
Research Org.:
DOE Geothermal Data Repository; University of Wisconsin
Sponsoring Org.:
USDOE Office of Energy Efficiency and Renewable Energy (EERE), Geothermal Technologies Program (EE-2C)
Subject:
15 Geothermal Energy
Keywords:
geothermal; DASH; PoroTomo; slow strain; Brady Hot Springs; DAS; horizontal; distributed acoustic sensing; Matlab; strain rate; strain; characterization; geophysics; hydrothermal; Brady; processed data; software; repository; technical; report; slow strain rate
OSTI Identifier:
1603411
DOI:
10.15121/1603411

Citation Formats

Reinisch, Elena C., Miller, Douglas E., Feigl, Kurt L., and Parker, Lesley M. DASH Slow Strain Rates from Brady Hot Springs Geothermal Field during PoroTomo Deployment Period. United States: N. p., 2018. Web. doi:10.15121/1603411.
Reinisch, Elena C., Miller, Douglas E., Feigl, Kurt L., & Parker, Lesley M. DASH Slow Strain Rates from Brady Hot Springs Geothermal Field during PoroTomo Deployment Period. United States. doi:10.15121/1603411.
Reinisch, Elena C., Miller, Douglas E., Feigl, Kurt L., and Parker, Lesley M. 2018. "DASH Slow Strain Rates from Brady Hot Springs Geothermal Field during PoroTomo Deployment Period". United States. doi:10.15121/1603411. https://www.osti.gov/servlets/purl/1603411. Pub date:Wed Jun 27 00:00:00 EDT 2018
@article{osti_1603411,
title = {DASH Slow Strain Rates from Brady Hot Springs Geothermal Field during PoroTomo Deployment Period},
author = {Reinisch, Elena C. and Miller, Douglas E. and Feigl, Kurt L. and Parker, Lesley M.},
abstractNote = {This submission contains slow strain rates summed to radians over 30 second intervals [rad/s] derived from horizontal distributed acoustic sensing measurements (DASH) of Brady geothermal field during PoroTomo deployment (2016-Mar-14 to 2016-Mar-26). There is one file corresponding to each day written in *.mat format for use with Matlab. The format for the binary Matlab .mat files are defined at: https://www.mathworks.com/help/pdf_doc/matlab/matfile_format.pdf. One such file includes the following variables: 'flist': list of raw DASH files used in the summation 'time_tag_mdt': sample time tag in datetime format with hours given in 24-hr format (yyyy/MM/dd HH:mm:ss.SSSSSSS) 'time_tag_uts': sample time tag in Unix time 'strain_rate_summed_over30s_in_radians_per_second': slow strain rates summed over 30 second intervals in units rad/s 'sample_standard_deviation_in_radians_per_second': corresponding sample standard deviation of slow strain rates in units rad/s The PoroTomo final technical report, raw DASH data, and software repository are also available through the links below.},
doi = {10.15121/1603411},
journal = {},
number = ,
volume = ,
place = {United States},
year = {2018},
month = {6}
}

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