Difference in attenuation among Mn, As, and Fe in riverbed sediments

Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989592%3A15310%2F18%3A73587493" target="_blank" >RIV/61989592:15310/18:73587493 - isvavai.cz</a>
Výsledek na webu
<a href="https://www.sciencedirect.com/science/article/pii/S0304389417305277" target="_blank" >https://www.sciencedirect.com/science/article/pii/S0304389417305277</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.jhazmat.2017.07.028" target="_blank" >10.1016/j.jhazmat.2017.07.028</a>

Jazyk výsledku
angličtina
Název v původním jazyce
Difference in attenuation among Mn, As, and Fe in riverbed sediments
Popis výsledku v původním jazyce
Detailed study of sediments and pore water in three rivers at the Chianan Plain, SW Taiwan, is reported. Concentrations of As in river sediments correspond to average crustal abundances and As is mostly bound to FeOOH. Sediments are enriched in Mn. Dissolved As concentrations are much lower compared to groundwater hotspots. No As attenuation has been detected in hyporheic zone and As together with Fe is attenuated deeper than Mn.
Název v anglickém jazyce
Difference in attenuation among Mn, As, and Fe in riverbed sediments
Popis výsledku anglicky
Detailed study of sediments and pore water in three rivers at the Chianan Plain, SW Taiwan, is reported. Concentrations of As in river sediments correspond to average crustal abundances and As is mostly bound to FeOOH. Sediments are enriched in Mn. Dissolved As concentrations are much lower compared to groundwater hotspots. No As attenuation has been detected in hyporheic zone and As together with Fe is attenuated deeper than Mn.

Rok uplatnění
2018
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Podobné výsledky(10)