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%.
156
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
104
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%.
165
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.
138
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%.
118
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
136
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%.
121
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.
128
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
111
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
92
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.
141
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
143
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%.
130
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%.
124
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
108
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
137
Citation Formats
University of Louisiana. (2018). Brady Hot Springs Seismic Modeling Data for Push-Pull Project [data set]. Retrieved from https://dx.doi.org/10.15121/1464530.
Zhang, Rui. Brady Hot Springs Seismic Modeling Data for Push-Pull Project. United States: N.p., 31 Jul, 2018. Web. doi: 10.15121/1464530.
Zhang, Rui. Brady Hot Springs Seismic Modeling Data for Push-Pull Project. United States. https://dx.doi.org/10.15121/1464530
Zhang, Rui. 2018. "Brady Hot Springs Seismic Modeling Data for Push-Pull Project". United States. https://dx.doi.org/10.15121/1464530. https://gdr.openei.org/submissions/1082.
@div{oedi_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.}, doi = {10.15121/1464530}, url = {https://gdr.openei.org/submissions/1082}, journal = {}, number = , volume = , place = {United States}, year = {2018}, month = {07}}
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
