Extensive subsurface contamination by dense non-aqueous phase liquid (DNAPL) organic solvents and heavy metals is common place at many DOE facilities. Poor performances and excessive costs have made traditional technologies and approaches less than satisfactory for remediation of such sites. It is increasingly apparent that marginal improvements in conventional methods and approaches will not suffice for clean up of many contaminated DOE sites. Innovative approaches using new and/or existing technologies in more efficient and costeffective ways are thus urgently required.The irreversible in-situ immobilization and inactivation concept proposed in this study is an innovative and promising approach. The concept is predicated on the hypothesis that natural geosorbents, either as they exist or as appropriately modified, can be employed to bind and sequester chlorinated organic solvents, other hydrophobic organic compounds and heavy metals irreversibly, and thereby eliminate or greatly reduce their associated environmental risks. The technologies that can be brought to bear on the implementation of this concept are for the most part readily available, but in neither organized form nor optimized state. The research described here effectively addresses both deficiencies.Common components of dense non-aqueous-phase liquid (DNAPL) contaminants, including chlorinated organic solvents and polycyclic aromatic hydrocarbons (PAHs), and most heavy metals are known to be sorbed by various types of natural organic matter (NOM), mineral, and/or clay components of typical soils and sediments. It is also known that the specific physicochemical properties of these geosorbents significantly effect the relative strength and extent of their respective sorption reactions with different organic and inorganic contaminants.The more aromatic and chemically condensed (i.e. "hard carbon") forms of soil/sediment NOM have much higher and less reversible sorption capacities for organic chemicals and heavy metals than do the more aliphatic and highly amorphous (i.e., "soft carbon") forms (Weber et.al,1992).The sorption properties of soil NOM matrices are thus directly related to the degree of geochemical diagenesis they have undergone in the terrestrial and aquatic environment. It has recently demonstrated in our laboratories that the sorption energies and capacities of soil sediment NOM matrices for organic chemicals can be greatly increased by treatment with superheated water at accelerated temperatures and pressures to simulate and accelerate geochemical diagenesis of SOM. The sorption capacities of many other naturally occurring 2 materials (e.g., bark, peanut husks, peat, bentonite, zeolites, etc.) for heavy metals also have been shown to be improved by thermal treatment.There is mounting evidence that many sorbed hydrophobic organic contaminants and heavy metals become more strongly sequestrated and thus less mobile and bioavailable to environmental receptors after prolonged periods of contact with soils, i.e., the so-called "aging effect"....