Abstract
The arsenic content in groundwater of the Red River floodplain decreases
with the burial age of the aquifer sediment over a 6000 year period.
This decrease is caused by diminishing reactivities of both sedimentary
organic carbon, Fe-oxides as well as CaCO3. Here we present a
1-D reactive transport model developed in PHREEQC-3 that quantifies the
resulting changes in groundwater bulk chemistry as well as arsenic
content over the last six millennia.
Original language | English |
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Pages (from-to) | 85-87 |
Number of pages | 3 |
Journal | Procedia Earth and Planetary Science |
Volume | 17 |
DOIs | |
Publication status | Published - 2017 |
Event | 15th Water-Rock Interaction International Symposium - Evora, Portugal Duration: 16 Oct 2016 → 21 Oct 2016 Conference number: 15 |
Programme Area
- Programme Area 2: Water Resources