| Abstract: | 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. ?? 1970. |
| Genre: | Article |
| ProdID: | 70010189 |
| Citation Author: | Manheim, F. T. |
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| Citation End Page: | 309 |
| Citation Issue: | 4 |
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| Citation Language: | English |
| Citation Larger Work Title: | Earth and Planetary Science Letters |
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| Citation Number Of Pages: | 3 |
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| Citation Search Results Text: | The diffusion of ions in unconsolidated sediments; 1970; Article; Journal; Earth and Planetary Science Letters; Manheim, F. T. |
| Citation Start Page: | 307 |
| Citation Volume: | 9 |
| Citation Year: | 1970 |
| Type: | citation/reference |
| Text: | The diffusion of ions in unconsolidated sediments; 1970; Article; Journal; Earth and Planetary Science Letters; Manheim, F. T. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Thu, 1 Jan 1970 00:00 -0600 |
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