In the Simulator kernel:

  • It is now possible to model dimethyl ether (a solvent partially miscible with water) using the CPA-SRK equation of state.
  • It is now possible to use the GERG-2008 equation of state together with the option of multiple components’ solubility in water and the CO2 solubility option.
  • Geomechanical modeling is supported for compositional and thermal models whose primary variable is temperature.

In Geology Designer and Model Designer:

  • A version control system has been implemented in Geology Designer and Model Designer: Teamwork. This system is designed for several users to work on one project.
  • It is now possible to visualize the grid of geographic coordinates in the 2D tab.
  • An option to display well test info in a Cross-Section tab has been implemented.
  • An option to display 3D grids and their properties in Simbox View mode has been added.

In Geology Designer:

  • An option to work with several sets of markers for the same horizon has been implemented.
  • A new interpolation method has been added: Plurigaussian simulation.
  • A new object has been added: Interval Logs. This object allows work with interval core measurements, well log interpretation results, etc. The main feature of the object is storing information about the sampling interval, i.e., the MD (Measured Depth) of the top and bottom of each sample.

In Seismic:

  • A calculation for seismic horizon autotracking by surveys 2D has been added.
  • It is now possible to take into account seismic faults during autotracking of seismic horizons by survey 3D.
  • It is now possible to thin out the correlation of a seismic horizon with the given step along inlines and crosslines.
  • It is now possible to determine the optimal parameters of frequency channels automatically during Spectral Decomposition calculation.
  • When calculating misties between seismic surveys, it is now possible to create a point set with numerical attributes in which the correction values will be stored.
  • During mistie calculation between 2D seismic surveys, it is now possible to enter variable vertical corrections along a 2D line.
tNavigator 24.3
tNavigator 24.3