Resumé
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.
| Originalsprog | Engelsk |
|---|---|
| Sider (fra-til) | 85-87 |
| Antal sider | 3 |
| Tidsskrift | Procedia Earth and Planetary Science |
| Vol/bind | 17 |
| DOI | |
| Status | Udgivet - 2017 |
| Begivenhed | 15th Water-Rock Interaction International Symposium - Evora, Portugal Varighed: 16 okt. 2016 → 21 okt. 2016 Konferencens nummer: 15 |
Programområde
- Programområde 2: Vandressourcer