Comprehensive Subsurface Solution
SeisOpt™ ReMi© and SeisOpt™ @2D Training Schedule*:
*Custom Training Available using Contact Form below
- ReMi array setup with Toughbook (VScope), DAQlink 4 24-Channel Seismograph (power cable and Ethernet cable), 24-channel array cable, 24 geophones, hammer and steel plate.
- How to determine the parameters for a seismic survey
- How to choose the best active source
- When and how to control a passive survey
- How to survey over pavement with pavement velocity inversions
- How to configure active sources
- Walkthrough of SeisOpt ReMi© or SeisOpt™ @2D
- ReMi Vspect: Imports the microtremor data recorded in the field and performs a wavefield transformation, creating a ‘‘velocity spectrum’’ in the slowness-frequency (p-f) domain.
- Understanding fundamental modes of dispersion imaging
- Computational artifacts from dispersion imaging
- How to extract dispersion curves from difficult data sets
- ReMi Disper: Model the picked dispersion curve by clicking and dragging the shear-wave velocity profiles so that the calculated dispersion curve matches the picks.
- Depth to bedrock
- Velocity inversions
- IBC Site Classification with velocity profile
- How to optimize the velocity model
- 1D Modeling: Create 1D models that represent the velocity changes with depth.
- Geometries: If the survey line is non-linear or there are rapid elevation changes greater than 7% of the line length, the correct geometries must be applied.
- Inversions: Represent an anomalous slowness-frequency (p-f) domain which will signify either an irregularly low or high velocity.
- 2D Modeling: Once the 1D models for each set of traces have been derived, they can be assembled to create a 2D shear-wave velocity cross-section under the profile.
- Client Practice Data
- 1D and 2D Modeling
- Geometries and Inversions
- Deliverable Ready Output
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