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NEWEST FEATURES
- Import of soil hydraulic properties from SVFlux™
- Additional features are listed below
FEATURE COMPARISON
| Summary Features |
Standard |
Professional |
Sieve / Hydrometer Data Storage |
Yes |
Yes |
Soils Data Warehouse |
Yes |
Yes |
Professional Reporting |
Yes |
Yes |
Support for English and Metric Units |
Yes |
Yes |
Borehole/Well Interface |
Yes |
Yes |
SWCC / Oedometer / Permeability data entry |
Yes |
Yes |
Database of 6200 soils |
|
Yes |
Estimate unsaturated soil properties |
|
Yes |
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Automatic Calculation of Grain-Size Statistics |
|
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Mode |
Yes |
Yes |
Median |
Yes |
Yes |
Graphic Mean |
Yes |
Yes |
Graphic Standard Deviation |
Yes |
Yes |
Inclusive Graphic Standard Deviation |
Yes |
Yes |
Phi Quartile Skewness |
Yes |
Yes |
Graphic Skewness |
Yes |
Yes |
Inclusive Graphic Skewness |
Yes |
Yes |
Coefficient of Curvature |
Yes |
Yes |
Coefficient of Uniformity |
Yes |
Yes |
Effective grain diameter |
Yes |
Yes |
Kurosis |
Yes |
Yes |
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Laboratory Tests |
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Grain-size distribution |
Yes |
Yes |
Volume Mass Properties |
Yes |
Yes |
Classification |
Yes |
Yes |
Mineralogy |
Yes |
Yes |
Soil Water Characteristic Curve |
Yes |
Yes |
Permeability |
Yes |
Yes |
Compression |
Yes |
Yes |
Compaction |
Yes |
Yes |
Shear Strength |
Yes |
Yes |
Shrinkage |
Yes |
Yes |
Borehole data |
Yes |
Yes |
Environmental data |
Yes |
Yes |
Diffusion |
Yes |
Yes |
Unfrozen Water Content |
Yes |
Yes |
Specific Heat |
Yes |
Yes |
Thermoconductivity |
Yes |
Yes |
Constitutive surfaces |
Yes |
Yes |
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Database |
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6200 + soil-water characteristic curves |
|
Yes |
2500 + saturated permeabilities |
|
Yes |
600 + permeability curves |
|
Yes |
100 + compression curves |
|
Yes |
50 + shrinkage curves |
|
Yes |
30 + compaction curves |
|
Yes |
25+ unsaturated shear box tests |
|
Yes |
20 + journal published estimation methods |
|
Yes |
SoilVision™ dataset |
|
Yes |
University of Saskatchewan dataset |
|
Yes |
C.H. Benson Compacted Clay Liners dataset |
|
Yes |
State of Illinois DOT Subgrade soils dataset |
|
Yes |
Al Tice unfrozen water content dataset |
|
Yes |
NCHRP Dataset |
|
Yes |
Correlation database |
|
Yes |
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Export Data Sets |
|
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To seepage (SVFlux™) |
|
Yes |
DETAILED FEATURES
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Database functionality means unlimited storage of soil tests organized by project and borehole
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Adherence to ASTM test standards separation of sieve and hydrometer data
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Ability to fit gap-graded, bimodal soils with equations from Fredlund & Wilson
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Support for English & Metric Units
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Calculation of particle-size density functions for unimodal and bimodal soils
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Professional report generation allows selection and reporting of multiple soils on the same report
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Automatic calculation of D10, D20, D30, D50, D60 and %Clay, %Silt, %Sand, and %Coarse for both USDA and USCS (ASTM) Classification standards
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Automatic classification by USDA or USCS (ASTM) methods
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Non-linear regression of unimodal or bimodal equations to represent the grain-size distribution
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Theoretical estimation of unsaturated soil properties. Over 20 theoretical and statistical methods are included for the prediction of soil-water characteristic curves and unsaturated hydraulic conductivity curves based on grain-size and other data. Estimation methods are highly valuable for the modeling of seepage through the vadose zone.
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Pre-existing laboratory database of over 6200 soils. Over 95% of theses oils have a laboratory measured soil-water characteristic curve. Laboratory data also exists for over 2500 saturated hydraulic conductivities and over 600 unsaturated hydraulic conductivity curves
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Automatic calculation of grain-size statistics
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Geostatistics module allows quick statistical analysis of your laboratory data.
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Mathematical fits of soil property functions allows soils in certain "bands" to be selected.
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Free form search wizard allows searching of the database based on almost any criteria.
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Mathematical model provides input for seepage and groundwater finite element and finite difference models.
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Software interfaces with many modeling packages, graphics packages, GIS, report writers, and borehole log programs
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