Geochemistry and geochemical modeling of unsaturated zone in a tropical region in Urania, Sao Paulo state, Brazil
| Authors | |
|---|---|
| Year of publication | 2006 |
| Type | Article in Periodical |
| Magazine / Source | Journal of Hydrology |
| MU Faculty or unit | |
| Citation | |
| Field | Geochemistry |
| Keywords | Unsaturated zone; hydrogeochemical modeling; sediementary rocks; hydrogeochemistry; |
| Description | Unsaturated zone in Urania, Sao Paulo state, Brazil, has been investigated using pore water sampling, tenziometric measurements, and solid phase analyses. Pore water chemistry evolves from calcium-bicarbonate in shallow zone towards sodium-bicarbonate in deep zone. Principal secondary mineral is kaolinite and degree of feldspare weathering decreases with depth. Inverse geochemical modeling gave non-unique results and several reaction pathways are possible. |
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