FEFLOW 6.1 DOWNLOAD

If you are interested in learning more about what our software can do for you, these online presentation are at your assistance. Among these are the improvements in simulation of the annual variation of soil infiltration capacity due to freezing and thawing dynamics. Please read it carefully before proceeding with the installation. With 10 subscription packages and three types of perpetual licenses available, there is sure to be an option that is right for your projects. Go to the 3D view.

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Define a Snap distance of Select by All Map m and click Geometries again in order to create a selection covering the refinement zone and its adjancent Smooth Mesh button to perarea. Click on Record in the Simulator toolbar. The cross section is based on a 2D Surface Line. FEFLOW enables you to simulate a multitude of processes involving fluid flow, groundwater-age, contaminant and heat transport in saturated and unsaturated porous media.

FEFLOW Release is here!

It will be conducted in English. To give this selection a recognizable name, choose Rename from its context menu and change the name to Northern Boundary. Northern Boundary II Zoom to the northern boundary. After the run, it does not contain the initial conditions any more, but the final results.

The elevations are given in meters ASL. Deadline for registration for training course: This kind of well, which stretches along a number of layers, is called a multilayer well. This may take several minutes.

FEFLOW® |

The nodal parameters of the old slice 2 are inherited to the new slices 2 and 3, while the information from the old slice 3 is to be inherited by slices 4 and 5. As the fefllw parameters depend on the model type, the general problem settings are typically done in the beginning.

Click on Add Link to establish a connection between the values in the map and the elevation data, or - alternatively - double click on Elevation to set the link. The other slices are placed below with a distance of 1 m each.

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The values of all properties currently visible in the active view are shown in the Inspection panel. Containing the target slice number as a point attribute, the file can ffflow used as the basis for regionalization of elevations for all slices at once. Layers are three-dimensional bodies that typically represent geological formations like aquifers and aquitards.

For additional editing, different tools are available to manually modify the supermesh. Open the Slice view again if it has been closed. Make sure to select Domain in the panel afterwards. The demonstration exercise is not intended as an fefkow to groundwater modeling itself.

I In the demo data installation there are the following packages: Missing chart windows can be added to the user interface 14 In this exercise, different file types are used as data source at the different stages of modelling to show the number of options. FEFLOW is automatically installed as a 32 bit version on 32 bit systems, and as 32 and 64 bit versions on 64 bit operating systems.

Type a value of 0. In the Hostname or IP address field, insert localhost if the dongle is installed locally, or insert the name or the IP number of the remote license manager.

For the sake of simplicity, they will be kept in a rather simple way: In order to change this, double click on the number box showing 5 in the new column. Choose the option Select by Map Polygon from the dropdown selector of the Selection toolbar.

At the top of the dialog several toolbars provide basic mathematical operations.

If running FEFLOW in demo mode, this model cannot be saved as the number of nodes per slice exceeds the allowed maximum of Click The current simulation time is displayed in the dropdown box of the Simulator toolbar. The user group meeting will include a combination of presentations of new software features and technologies, as well feflkw practical case studies presented by Swiss users.