The diffusion of ions in unconsolidated sediments
Diffusion in unconsolidated sediments generally proceeds at rates ranging from half to one twentieth of those applying to diffusion of ions and molecules in free solution. Diffusion rates are predictable with respect to porosity and path tortuosity in host sediments, and can be conveniently measured by determinations of electrical resistivity on bulk sediment samples. Net ion flux is further influenced by reactions of diffusing species with enclosing sediments, but such influences should not be confused with or lumped with diffusion processes.
Citation Information
Publication Year | 1970 |
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Title | The diffusion of ions in unconsolidated sediments |
DOI | 10.1016/0012-821X(70)90123-8 |
Authors | F.T. Manheim |
Publication Type | Article |
Publication Subtype | Journal Article |
Series Title | Earth and Planetary Science Letters |
Index ID | 70010189 |
Record Source | USGS Publications Warehouse |