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%.
47
seis_Vx_100.dat
Seismic modeling results using surficial geophones with 1m spacing and a CO2 saturation of 100%.
29
seis_Vx_50.dat
Seismic modeling results using surficial geophones with 1m spacing and a CO2 saturation of 50%.
29
seis_Vx_nofrac.dat
Seismic modeling results in a non-fractured medium, using surficial geophones with 1m spacing.
33
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%.
36
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%.
25
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%.
25
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%.
40
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%.
29
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%.
26
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%.
41
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
26
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%.
33
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
26
seis_Vy_0.dat
Seismic modeling results using surficial geophones with 1m spacing and a CO2 saturation of 0%.
25
seis_Vy_100.dat
Seismic modeling results using surficial geophones with 1m spacing and a CO2 saturation of 100%.
30
seis_Vy_50.dat
Seismic modeling results using surficial geophones with 1m spacing and a CO2 saturation of 50%.
26
seis_Vy_nofrac.dat
Seismic modeling results in a non-fractured medium, using surficial geophones with 1m spacing.
26
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%.
24
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%.
27
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%.
28
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%.
27
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%.
28
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%.
26
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%.
17
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
24
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%.
26
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
31
vsp_Vx_0.dat
Seismic modeling results using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 0%.
41
vsp_Vx_100.dat
Seismic modeling results using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 100%.
28
vsp_Vx_50.dat
Seismic modeling results using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 50%.
38
vsp_Vx_nofrac.dat
Seismic modeling results in a non-fractured medium, using vertical seismic profiling (VSP) with 1m spacing.
27
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%.
25
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
27
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%.
20
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%.
24
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%.
26
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%.
30
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%.
33
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
23
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%.
15
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
26
vsp_Vy_0.dat
Seismic modeling results using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 0%.
25
vsp_Vy_100.dat
Seismic modeling results using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 100%.
30
vsp_Vy_50.dat
Seismic modeling results using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 50%.
24
vsp_Vy_nofrac.dat
Seismic modeling results in a non-fractured medium, using vertical seismic profiling (VSP) with 1m spacing.
26
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%.
34
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
30
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%.
26
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%.
39
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%.
27
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%.
26
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%.
27
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
24
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%.
24
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
32
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_3741, 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 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
