Environmental Data Diffusion
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Contaminant transport models are critical
to your environmental project. The results of your calculations
are dependant on the validity of soil properties. Let SoilVision
provide you with sound theoretical estimations of diffusion as
a function of soil suction.
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Features:
- Management of diffusion data
- Comprehensive querying capabilities
- Two theoretical estimations to provide you adsorption
or diffusion curves
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Application:
- Contaminant transport modeling
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Plotting/Graphing:
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Unfrozen Volumetric Water Content
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For modeling soil conditions in frozen
environments, a description of how the unfrozen water content varies
with temperature is required. Database functionality is capable
of storing both cooling and warming laboratory data while Blacks
theoretical estimation will provide an estimate of the unfrozen
water content curve when experimental data is limited.
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Features:
- Comprehensive plotting
- Comprehensive querying capabilities
- Support for English and Metric units
- Non-linear regression of experimental laboratory data
provides mathematical representation of experimental
data
- Blacks pedo-transfer function allows estimates of unfrozen
volumetric water content as a function of temperature
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Plotting/Graphing:
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Specific Heat
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Modeling of thermal processes such as evaporative
flux boundary conditions requires the specific heat of a soil at
all soil suction levels. SoilVision has implemented a theoretical
method to provide this calculation.
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Features:
- Estimation of specific heat by the Farouki method allows
mathematical representation as a function of soil suction
- Enhanced plotting
- Comprehensive querying capabilities
- Support for English and Metric units
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Application:
- Evaporation flux modeling such as soil cover design and evapotranspiration.
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Plotting/Graphing:
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Thermoconductivity
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Similar to specific heat, this soil property
is required for the modeling of evaporative flux boundary conditions.
Full database functionality is provided to manage your experimental
data. Johansens theoretical estimation has also been implemented
to provide a thermoconductivity model dependant on soil suction.
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Features:
- Non-linear regression provides mathematical representation
of warming and cooling soil property functions
- The Johansen pedo-transfer function provides an estimation
of the thermoconductivity function when experimental
data is limited
- Enhanced plotting
- Comprehensive querying capabilities
- Support for English and Metric units
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Application:
- Evaporation flux modeling such as soil cover design
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Plotting/Graphing:
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