Brady Hot Springs Seismic Modeling Data for Push-Pull Project

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%.
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.
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%.
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%.
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
113

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.
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%.
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%.
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
109

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

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.
Export Citation to RIS
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

ruizhang@louisiana.edu

337.482.6920

Authors

Rui Zhang

University of Louisiana at Lafayette

DOE Project Details

Project Name Push-pull well testing using CO2 with active source geophysical monitoring

Project Lead Arlene Anderson

Project Number EE8421554

Share

Submission Downloads