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%.
135
seis_Vx_100.dat
Seismic modeling results using surficial geophones with 1m spacing and a CO2 saturation of 100%.
129
seis_Vx_50.dat
Seismic modeling results using surficial geophones with 1m spacing and a CO2 saturation of 50%.
102
seis_Vx_nofrac.dat
Seismic modeling results in a non-fractured medium, using surficial geophones with 1m spacing.
117
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%.
141
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%.
106
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%.
115
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%.
119
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%.
108
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%.
104
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%.
76
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
102
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%.
91
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
76
seis_Vy_0.dat
Seismic modeling results using surficial geophones with 1m spacing and a CO2 saturation of 0%.
132
seis_Vy_100.dat
Seismic modeling results using surficial geophones with 1m spacing and a CO2 saturation of 100%.
143
seis_Vy_50.dat
Seismic modeling results using surficial geophones with 1m spacing and a CO2 saturation of 50%.
107
seis_Vy_nofrac.dat
Seismic modeling results in a non-fractured medium, using surficial geophones with 1m spacing.
115
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%.
87
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%.
133
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%.
94
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%.
106
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%.
123
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%.
90
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%.
77
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
108
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%.
82
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
111
vsp_Vx_0.dat
Seismic modeling results using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 0%.
118
vsp_Vx_100.dat
Seismic modeling results using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 100%.
102
vsp_Vx_50.dat
Seismic modeling results using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 50%.
126
vsp_Vx_nofrac.dat
Seismic modeling results in a non-fractured medium, using vertical seismic profiling (VSP) with 1m spacing.
109
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%.
100
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
145
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%.
120
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%.
94
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%.
107
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%.
91
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%.
120
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
91
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%.
97
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
67
vsp_Vy_0.dat
Seismic modeling results using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 0%.
90
vsp_Vy_100.dat
Seismic modeling results using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 100%.
122
vsp_Vy_50.dat
Seismic modeling results using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 50%.
103
vsp_Vy_nofrac.dat
Seismic modeling results in a non-fractured medium, using vertical seismic profiling (VSP) with 1m spacing.
115
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%.
111
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
115
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%.
104
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%.
108
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%.
142
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%.
110
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%.
99
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
83
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%.
111
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
108
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 - Open Energy Data Initiative (OEDI)
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, GDR. https://doi.org/10.15121/1464530.
Zhang, R. (2018). Brady Hot Springs Seismic Modeling Data for Push-Pull Project. [Data set]. GDR. 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 GDR. https://doi.org/10.15121/1464530
@misc{OEDI_Dataset_7233,
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 = {GDR, University of Louisiana, https://doi.org/10.15121/1464530},
note = {Accessed: 2025-05-03},
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 LafayetteOriginal Source
https://gdr.openei.org/submissions/1082Research Areas
Keywords
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
