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Publication
Featured researches published by William M. Davis.
Chemosphere | 1995
James M. Brannon; Judith C. Pennington; William M. Davis; Charolett Hayes
Abstract When calculating concentrations of truly dissolved hydrophobic organic contaminants (HOCs) in sediment pore water, a common assumption is that the partition coefficient between pore water and colloidal plus dissolved organic carbon (K DOC ) equals the partition coefficient between pore water and sediment total organic carbon (K OC ). This study examined the K DOC of fluoranthene in pore water from 11 sediments. Truly dissolved fluoranthene was separated from DOC-associated fluoranthene by partitioning on C-18 Sep Paks. Measured values of K DOC were not constant over the 11 sediments examined, and were over or underestimated by assuming that K DOC = K OC . Current models used to predict the fate of HOCs may require modification to account for the observed difference between K DOC and K OC .
This Digital Resource was created from scans of the Print Resource | 1998
James M. Brannon; Judith C. Pennington; Tommy E. Myers; William M. Davis; Michael Ochman; Karen F. Myers; Charolett A. Hayes; Daniel M. Townsend
Archive | 1995
Judith C. Pennington; Tommy E. Meyers; William M. Davis; Trudy J. Olin
Archive | 2002
Karen F. Myers; William M. Davis; Jed Costanza
Archive | 2001
Jed Costanza; Karen F. Myers; William M. Davis
Archive | 1999
Karen F. Myers; Richard A. Karn; Dan Y. Eng; Karl F. Konecny; William M. Davis
Archive | 2002
Karen F. Myers; Jed Costanza; William M. Davis
Archive | 2002
George Robitaille; William M. Davis; Karen F. Myers; Jed Costanza; Marc Wise
Archive | 2001
George Robitaille; William M. Davis; Karen F. Myers; Jed Costanza; Marc Wise
Archive | 2001
William M. Davis; Karen F. Myers; Mark B. Wise; Cyril V. Thompson
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