Brady Hot Springs Seismic Modeling Data for Push-Pull Project
DOI
10.15121/1464530
Publicly accessible
License 
This submission includes synthetic seismic modeling data for the Push-Pull project at Brady Hot Springs, NV. The synthetic seismic is all generated by finite-difference method regarding different fracture and rock properties.
seis_Vx_0.dat
Seismic modeling results using surficial geophones with 1m spacing and a CO2 saturation of 0%.
157
seis_Vx_100.dat
Seismic modeling results using surficial geophones with 1m spacing and a CO2 saturation of 100%.
151
seis_Vx_50.dat
Seismic modeling results using surficial geophones with 1m spacing and a CO2 saturation of 50%.
126
seis_Vx_nofrac.dat
Seismic modeling results in a non-fractured medium, using surficial geophones with 1m spacing.
141
seis_Vx_sig_frac_0.dat
Seismic modeling results in a single-fractured media (ten parallel fractures aligned), using surficial seismic data with 1m spacing and a CO2 saturation of 0%.
167
seis_Vx_sig_frac_50.dat
Seismic modeling results in a single-fractured media (ten parallel fractures aligned), using surficial seismic data with 1m spacing and a CO2 saturation of 50%.
131
seis_Vx_ten_frac_0.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 0%.
133
seis_Vx_ten_frac_0_1m_spacing.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 0%.
146
seis_Vx_ten_frac_50.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 50%.
128
seis_Vx_ten_frac_50_1m_spacing.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 50%.
130
seis_Vx_tencluster_frac_0_1m_spacing.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 0%.
102
seis_Vx_tencluster_frac_0_1m_spacing_newgeometry.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 0%. This model uses a a ... more
126
seis_Vx_tencluster_frac_50_1m_spacing.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 50%.
118
seis_Vx_tencluster_frac_50_1m_spacing_newgeometry.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 50%. This model uses a a... more
105
seis_Vy_0.dat
Seismic modeling results using surficial geophones with 1m spacing and a CO2 saturation of 0%.
152
seis_Vy_100.dat
Seismic modeling results using surficial geophones with 1m spacing and a CO2 saturation of 100%.
166
seis_Vy_50.dat
Seismic modeling results using surficial geophones with 1m spacing and a CO2 saturation of 50%.
133
seis_Vy_nofrac.dat
Seismic modeling results in a non-fractured medium, using surficial geophones with 1m spacing.
139
seis_Vy_sig_frac_0.dat
Seismic modeling results in a single-fractured media (ten parallel fractures aligned), using surficial seismic data with 1m spacing and a CO2 saturation of 0%.
111
seis_Vy_sig_frac_50.dat
Seismic modeling results in a single-fractured media (ten parallel fractures aligned), using surficial seismic data with 1m spacing and a CO2 saturation of 50%.
159
seis_Vy_ten_frac_0.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 0%.
119
seis_Vy_ten_frac_0_1m_spacing.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 0%.
128
seis_Vy_ten_frac_50.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 50%.
143
seis_Vy_ten_frac_50_1m_spacing.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 50%.
111
seis_Vy_tencluster_frac_0_1m_spacing.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 0%.
102
seis_Vy_tencluster_frac_0_1m_spacing_newgeometry.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 0%. This model uses a a ... more
128
seis_Vy_tencluster_frac_50_1m_spacing.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 50%.
104
seis_Vy_tencluster_frac_50_1m_spacing_newgeometry.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 50%. This model uses a a... more
138
vsp_Vx_0.dat
Seismic modeling results using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 0%.
142
vsp_Vx_100.dat
Seismic modeling results using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 100%.
122
vsp_Vx_50.dat
Seismic modeling results using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 50%.
150
vsp_Vx_nofrac.dat
Seismic modeling results in a non-fractured medium, using vertical seismic profiling (VSP) with 1m spacing.
129
vsp_Vx_sig_frac_0.dat
Seismic modeling results in a single-fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 0%.
124
vsp_Vx_sig_frac_50.dat
Seismic modeling results in a single-fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 50... more
162
vsp_Vx_ten_frac_0.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 0%.
144
vsp_Vx_ten_frac_0_1m_spacing.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 0%.
113
vsp_Vx_ten_frac_50.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 50%.
128
vsp_Vx_ten_frac_50_1m_spacing.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 50%.
114
vsp_Vx_tencluster_frac_0_1m_spacing.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 0%.
142
vsp_Vx_tencluster_frac_0_1m_spacing_newgeometry.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 0%. This mo... more
114
vsp_Vx_tencluster_frac_50_1m_spacing.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 50%.
119
vsp_Vx_tencluster_frac_50_1m_spacing_newgeometry.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 50%. This m... more
93
vsp_Vy_0.dat
Seismic modeling results using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 0%.
115
vsp_Vy_100.dat
Seismic modeling results using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 100%.
147
vsp_Vy_50.dat
Seismic modeling results using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 50%.
127
vsp_Vy_nofrac.dat
Seismic modeling results in a non-fractured medium, using vertical seismic profiling (VSP) with 1m spacing.
142
vsp_Vy_sig_frac_0.dat
Seismic modeling results in a single-fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 0%.
133
vsp_Vy_sig_frac_50.dat
Seismic modeling results in a single-fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 50... more
146
vsp_Vy_ten_frac_0.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 0%.
131
vsp_Vy_ten_frac_0_1m_spacing.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 0%.
138
vsp_Vy_ten_frac_50.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 50%.
164
vsp_Vy_ten_frac_50_1m_spacing.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 50%.
136
vsp_Vy_tencluster_frac_0_1m_spacing.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 0%.
125
vsp_Vy_tencluster_frac_0_1m_spacing_newgeometry.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 0%. This mo... more
110
vsp_Vy_tencluster_frac_50_1m_spacing.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 50%.
130
vsp_Vy_tencluster_frac_50_1m_spacing_newgeometry.dat
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 50%. This m... more
138
Citation Formats
TY - DATA
AB - This submission includes synthetic seismic modeling data for the Push-Pull project at Brady Hot Springs, NV. The synthetic seismic is all generated by finite-difference method regarding different fracture and rock properties.
AU - Zhang, Rui
DB - Geothermal Data Repository
DP - Open EI | National Renewable Energy Laboratory
DO - 10.15121/1464530
KW - geothermal
KW - energy
KW - seismic
KW - geophysics
KW - active source
KW - velocity
KW - geophysical
KW - data
KW - modeling
KW - numerical
KW - synthetic
KW - Brady Hot Springs
KW - Nevada
KW - NV
KW - fracture
KW - rock
KW - geologic
KW - properties
KW - property
KW - push-pull
KW - finite difference
KW - numerical modeling
KW - VSP
KW - vertical seismic profiling
KW - borehole
KW - fractured
KW - non-fractured
KW - media
KW - CO2
KW - saturation
LA - English
DA - 2018/07/31
PY - 2018
PB - University of Louisiana
T1 - Brady Hot Springs Seismic Modeling Data for Push-Pull Project
UR - https://doi.org/10.15121/1464530
ER -
Zhang, Rui. Brady Hot Springs Seismic Modeling Data for Push-Pull Project. University of Louisiana, 31 July, 2018, Geothermal Data Repository. https://doi.org/10.15121/1464530.
Zhang, R. (2018). Brady Hot Springs Seismic Modeling Data for Push-Pull Project. [Data set]. Geothermal Data Repository. University of Louisiana. https://doi.org/10.15121/1464530
Zhang, Rui. Brady Hot Springs Seismic Modeling Data for Push-Pull Project. University of Louisiana, July, 31, 2018. Distributed by Geothermal Data Repository. https://doi.org/10.15121/1464530
@misc{GDR_Dataset_1082,
title = {Brady Hot Springs Seismic Modeling Data for Push-Pull Project},
author = {Zhang, Rui},
abstractNote = {This submission includes synthetic seismic modeling data for the Push-Pull project at Brady Hot Springs, NV. The synthetic seismic is all generated by finite-difference method regarding different fracture and rock properties.},
url = {https://gdr.openei.org/submissions/1082},
year = {2018},
howpublished = {Geothermal Data Repository, University of Louisiana, https://doi.org/10.15121/1464530},
note = {Accessed: 2025-04-25},
doi = {10.15121/1464530}
}
https://dx.doi.org/10.15121/1464530
Details
Data from Jul 31, 2018
Last updated Jan 29, 2019
Submitted Jul 31, 2018
Organization
University of Louisiana
Contact
Rui Zhang
337.482.6920
Authors
Rui Zhang
University of Louisiana at LafayetteKeywords
geothermal, energy, seismic, geophysics, active source, velocity, geophysical, data, modeling, numerical, synthetic, Brady Hot Springs, Nevada, NV, fracture, rock, geologic, properties, property, push-pull, finite difference, numerical modeling, VSP, vertical seismic profiling, borehole, fractured, non-fractured, media, CO2, saturationDOE Project Details
Project Name Push-pull well testing using CO2 with active source geophysical monitoring
Project Lead Arlene Anderson
Project Number EE8421554
