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In understanding the movement and distribution of chlorinated solvents in source zones and plumes it is critical to recognize that chlorinated solvents in subsurface environments occur in four different phases:. A gas phase in soil vapor. Dense Nonaqueous Phase Liquid (DNAPL). A dissolved phase in water. A sorbed phase on aquifer solids. Furthermore, each phase can exist in either transmissive or low permeability geologic media, that may be present in both source zones and plumes. The theory, development...

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In understanding the movement and distribution of chlorinated solvents in source zones and plumes it is critical to recognize that chlorinated solvents in subsurface environments occur in four different phases:. A gas phase in soil vapor. Dense Nonaqueous Phase Liquid (DNAPL). A dissolved phase in water. A sorbed phase on aquifer solids. Furthermore, each phase can exist in either transmissive or low permeability geologic media, that may be present in both source zones and plumes. The theory, development...
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In understanding the movement and distribution of chlorinated solvents in source zones and plumes it is critical to recognize that chlorinated solvents in subsurface environments occur in four different phases:. A gas phase in soil vapor. Dense Nonaqueous Phase Liquid (DNAPL). A dissolved phase in water. A sorbed phase on aquifer solids. Furthermore, each phase can exist in either transmissive or low permeability geologic media, that may be present in both source zones and plumes. The theory, development...

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In understanding the movement and distribution of chlorinated solvents in source zones and plumes it is critical to recognize that chlorinated solvents in subsurface environments occur in four different phases:. A gas phase in soil vapor. Dense Nonaqueous Phase Liquid (DNAPL). A dissolved phase in water. A sorbed phase on aquifer solids. Furthermore, each phase can exist in either transmissive or low permeability geologic media, that may be present in both source zones and plumes. The theory, development...

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About the 14 Compartment Model Website. Web Development / Administrator. GSI Environmental Inc.). GSI Environmental Inc.). Charles J. Newell. GSI Environmental Inc.). Geosyntec Consultants, Inc.). Geosyntec Consultants, Inc.). Matt Vanderkooy (Geosyntec Consultants, Inc.). This project has been made possible by the following companies and organizations. Cite the 14-compartment model toolkit using:. Cite the User’s Guide using:. PHP MVC base framework, ActiveRecord database link layer).

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14 Compartment Model Site Help. The following help topics can be accessed while navigating the application by either clicking on an information bubble or by selecting a topic from the drop down help menu at the top right of most pages. If you have questions that are not covered below or by the Guide for Selecting Remedies for Subsurface Releases of Chlorinated Solvents (ESTCP Project ER-200530). 2013 GSI Current Session ID:.

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In understanding the movement and distribution of chlorinated solvents in source zones and plumes it is critical to recognize that chlorinated solvents in subsurface environments occur in four different phases:. A gas phase in soil vapor. Dense Nonaqueous Phase Liquid (DNAPL). A dissolved phase in water. A sorbed phase on aquifer solids. Furthermore, each phase can exist in either transmissive or low permeability geologic media, that may be present in both source zones and plumes. The theory, development...

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