SVFLUX DOWNLOAD

Manual entry of region coordinate points. Volume or water volume integrals may be computed over the entire problem or any particular region of interest. New problems may draw soils from existing problems. The solver uses advanced features such as preconditioning of the convergence matrix as well as staging and automatic mesh refinement to achieve solutions with greater stability than any other software currently available. Borehole or soil survey data may be used to build 3D groundwater models resulting in the possibility of extremely complex models.

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Mesh refinement may be specified to follow any particular variable in the problem.

A central database of soil properties for all entered seepage problems is maintained; new problems may draw soils from existing problems. The program is used in the fields of civil engineering and xvflux in order to analyze seepage and groundwater regional flow.

From Wikipedia, the free encyclopedia. Sketch text or lines may be added to the model design.

SVFlux is designed to model seepage and groundwater in soils. It is svflxu most powerful and stable finite element Most users are able to learn how to use the software effectively to create 2D problems within minutes. Tutorial manual - Step-by-step svfljx guides the user through creation of 2D and 3D problems. Designed to be simple and effective, the software offers features designed to allow the user to focus on seepage solutions, not convergence problems or difficult mesh creation.

Finite element analysis by the Galerkin method. A central database of soil properties for all entered seepage problems is maintained.

This feature is only available for software listings at the Advanced or Lead Sponsorship Level. Borehole or soil survey data may be svfpux to build 3D groundwater models resulting in the possibility of extremely complex models. By using this site, you agree to the Terms of Use and Privacy Policy. Soil-water characteristic soil moisture retention curves and saturated or unsaturated hydraulic conductivities permeabilities may be determined in a laboratory or estimated using SoilVision.

Saturated or unsaturated analysis. Mesh generation may be limited by a maximum number of nodes or by a maximum specified error.

SVFlux - Wikipedia

The z-component svfflux vertical flux boundaries sfvlux be isolated to simulate precipitation on steep irregular surfaces. Create a free account and view content that fits your specific interests in geotechnical engineering Learn More. Head, flux, climatic, and cauchy boundary conditions are available in steady-state or transient models. Easy-to-use and simplified CAD-based user interface: Calculate volume flow-rates through earth structures.

Borehole or soil survey data may be used to build each groundwater model resulting in the possibility of extremely complex models. The results may also be viewed in the context of a graphical user interface.

SVFLUX PEST Interface

Design of earth covers. Tables of net flux data may be cut and pasted into SVFlux to act as boundary conditions. For example, saturated hydraulic conductivity svvflux be input as a lognormal distribution and the resulting variation output.

Add contaminant transport analysis with our ChemFlux software.

Axisymmetric analysis version 3. Capabilities Analyze saturated or unsaturated soils Stable analysis of saturated or unsaturated soils. Fully automatic mesh refinement.

SVFLUX™ |

Our CAD-based front end and automated solver allow you to spend time solving your problem, not designing your mesh. Each software provider can upgrade the sponsorship level of their software listing by visiting the sponsorship levels page. Problems may be entered in Metric or Imperial units All aspects of all models are stored in a database which may be placed on svlux server. This application is used for solutions involving calculation of pore-water pressures for slope stability, tailings dams, earth dams, reservoirs, unsaturated cover systems, and groundwater dvflux in embankments.

Free student versions of this software are available for teaching purposes.