CTS: Chemical Transformation Simulator 1.3.2.2

Calculate Physicochemical Properties

  • Chemical Editor
  • |
  • Physicochemical Calculators


Enter a SMILES, Name, or CAS#, or draw a chemical, then click the button located in the top right of the chosen method to get results. Click the "next" button below or click the "Physicochemical Calculators" link above to continue through the workflow.


Draw Chemical Structure

Results

Melting Point

The temperature at which a chemical changes from liquid to gaseous phase.

Methods:

HC: Hierarchical Clustering

NN: Nearest Neighbor

GC: Group Contribution

Boiling Point

The temperature at which a chemical changes from liquid to gaseous phase.

Methods:

HC: Hierarchical Clustering

NN: Nearest Neighbor

GC: Group Contribution

Water Solubility

The maximum concentration of a chemical compound which can result when it is dissolved in water. For solids, a correction factor has been applied to convert estimated supercooled values to the vapor pressure of the solid.

Methods:

WSKOW: QSAR model for determining water solubility

WATERNT: Fragment-based QSAR model for determining water solubility

Vapor Pressure

The force per unit area exerted by a vapor in an equilibrium state with its pure solid, liquid, or solution at a given temperature. Vapor pressure is a measure of a substance's propensity to evaporate. For solids, a correction factor has been applied to convert estimated supercooled values to the vapor pressure of the solid.

Molecular Diffusivity in Water

The proportionality constant of molar flux due to molecular diffusion in water and the concentration gradient of the chemical in water. Molecular diffusion in water is the process in which solutes are transported at the microscopic level as the result of their spontaneous movement from regions of higher concentrations to regions of lower concentrations.

Molecular Diffusivity in Air

The proportionality constant of molar flux due to molecular diffusion in air and the concentration gradient of the chemical in air. Molecular diffusion in air is the process in which gases are transported at the microscopic level as the result of their spontaneous movement from regions of higher concentrations to regions of lower concentrations.

Ionization Constant

The equilibrium constant for an acid or base dissocation reaction. The constant provides a measure of the strength of an acid or base.

Henry's Law Constant

The ratio of the concentration of a compound in air to the concentration of the compound in water under equilibrium conditions.

Octanol/Water Partition Coefficient

The ratio of the concentration of a compound inn n-octanol (a non-polar solvent) to its concentration in water (a polar solvent). The higher the Kow, the more non-polar the compound.

Methods:

KLOP: Method for determining Kow using Klopman et al. models (Klopman, G.; Li, Ju-Yun.; Wang, S.; Dimayuga, M.: J.Chem.Inf.Comput.Sci., 1994, 34, 752)

VG: Method for determining Kow derived from Viswanadhan et al. (Viswanadhan, V. N.; Ghose, A. K.; Revankar, G. R.; Robins, R. K., J. Chem. Inf. Comput. Sci., 1989, 29, 163-172)

PHYS: Method for determining Kow based on the VG model with the PHYSPROP database as a training set

Organic Carbon Partition Coefficient

The ratio of mass of a chemical adsorbed to soil organic carbon to the concentration of the chemical in water under equilibrium conditions. Can also be described as the soil-water distribution coefficient (Koc) normalized to the total organic carbon content of the soil.

Methods:

MCI: Molecular Connectivity Index method

KOW: log Kow-based method

Bioconcentration Factor

The ratio of the concentration of a chemical in an organism due to uptake from surrounding water to the concentration of the chemical in the surrounding water.

Methods:

REG: Regression method for determining bioconcentration factors

A-G: Arnot-Gobas method for determining bioconcentration and bioaccumulation factors

SM: Single Model

HC: Hierarchical Clustering

NN: Nearest Neighbor

GC: Group Contribution

Bioaccumulation Factor

The ratio of the concentration of a chemical in an organism from all uptake pathways, including respiration, dermal uptake, and diet, to the concentration of the chemical in the surrounding environment.

Methods:

A-G: Arnot-Gobas method for determining bioconcentration and bioaccumulation factors

Octanol/Water Distribution Coefficient

The ratio of the concentration of a compound in n-octanol (a non-polar solvent) to its concentration in water (a polar solvent) at a user-specified pH value. The higher the d_ow , the more non-polar the compound.

Methods:

KLOP: Method for determining d_ow using Klopman et al. models (Klopman, G.; Li, Ju-Yun.; Wang, S.; Dimayuga, M.: J.Chem.Inf.Comput.Sci., 1994, 34, 752)

VG: Method for determining d_ow derived from Viswanadhan et al. (Viswanadhan, V. N.; Ghose, A. K.; Revankar, G. R.; Robins, R. K., J. Chem. Inf. Comput. Sci., 1989, 29, 163-172)

PHYS: Method for determining d_ow based on the VG model with the PHYSPROP database as a training set

Water Solubility

The maximum concentration of a chemical compound which can result when it is dissolved in water, adjusted to a user-specified pH. For solids, a correction factor has been applied to convert estimated supercooled values to the vapor pressure of the solid.

Methods:

WSKOW: QSAR model for determining water solubility

WATERNT: Fragment-based QSAR model for determining water solubility

HC: Hierarchical Clustering

NN: Nearest Neighbor

GC: Group Contribution