Soil Profile

 

The Soil Profile command on the Calculations Panel is used for managing soil layer properties, and the minimum or maximum groundwater level.

 

Soil Profile command

Soil Profile command

 

 

Soil Profile dialog box

Soil Profile dialog box

 

 

 

Soil Layers

In this section, you can manage the soil layer properties. This multi-layer functionality allows you to set up as many soil layers as desired. The main purpose of this dialog is to keep all soil layer data organized and to provide an easy and effective means of inserting, modifying, and deleting soil layers.

 

Soil layers

Soil layers options

 

Soil components are organized in a table with editable fields, each line representing a defined soil type with different editable parameters (or checkboxes) available in each column.

Since defining individual soil layers can be a time-consuming task, the Soil Database dialog provides a library of predefined soils. These soils appear in the drop-down list of the column Soil Type.

When working with table data, the commands to add/remove layers are fast and easy to use. They are available in the form of icons in front of each row:

The characteristic parameters for each soil layer are:

 

All soil data is editable. If you modify any of the default properties of the soil layer, the Soil Type becomes Custom.

 

Custom soil type

Custom soil type

 

 

 

Stratigraphy Preview

Besides the soil grid, which is used to impose soil characteristics, the dialog contains a drawing to illustrate the succession of soil layers, in section Stratigraphy preview. The sketch contains a plot of each previously defined soil layer with its corresponding color and also displays additional info such as the level of each layer inserted in the grid. The sketch can be displayed or not using the Hide/Show preview buttons.

 

Stratigraphy preview

Stratigraphy preview

 

 

Ground Water

In this section, you can specify the maximum/minimum ground water level that may appear during the footing service life.

A drained condition occurs when there is no change in pore water pressure due to external loading. In a drained condition, the pore water can drain out of the soil easily, causing volumetric strains in the soil.

An undrained condition occurs when the pore water is unable to drain out of the soil. In an undrained condition, the rate of loading is much quicker than the rate at which the pore water can drain out of the soil. As a result, most of the external loading is taken by the pore water, increasing the porewater pressure. The tendency of soil to change volume is suppressed during undrained loading.

 

Ground water

Ground water

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

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