TerrantaLab: Fast, Powerful Chemical Modeling for Reactive Flow

TerrantaLab streamlines complex geochemical analysis, enabling fast and intuitive modeling to support 1D, 2D, and 3D reactive flow simulations.

TerrantaLab main page. Manage your projects and collaborate.

KEY FEATURES

Explore fluid-rock interactions across pressure and temperature conditions. Analyze dissolved species, mixing reactions, and phase behavior with ease.

Calibrate fluids and rocks, simulate fluid mixing and reaction paths, and integrate results into flow models.

Visualize element stability across pH and redox conditions. Toggle between major species or full speciation views with intuitive pie-chart breakdowns.

Model non-equilibrium reactions using customizable dissolution kinetics, including plotting half-times vs. pH or temperature to pinpoint rate-limiting factors.

Build, run, and analyze geochemical flow paths directly or connect with TerrantaFlow and external flow simulators.

Coming Soon to TerrantaLab

Rapidly simulate large-scale systems by linking chemical and flow models. Compatible with TerrantaFlow and third-party flow engines. Available now as a service.

Model petroleum-related fluids with a new liquid oil phase and expanded chemical species for advanced hydrocarbon systems.

New lithology definitions and adjustable parameters like porosity, permeability, and flow rates for more accurate 1D flow simulations.

TerrantaLab empowers you to simulate complex geochemistry with speed, precision, and flexibility—anytime, anywhere.

Pourbaix diagrams in TerrantaLab showing stability of Fe-species within a given chemical system.

The right image shows the distribution of stable species, while the right image shows the stability of Fe2+ (yellow and green colors). Note the co-existence of different species in the transition zone as shown in the selected (magnified) pie-chart.

Left figure: Fluid definition and analysis of chemical compositions in TerrantaLab.

Right figure: Easy and self-explaining workflows to simulate complex rock-fluid interactions. Here is an example of a Pb-Zn deposit, explaining the zonation of such deposits into a Galena and Sphalerite dominated zone.

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