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Behavior of arsenic and geochemical modeling of arsenic enrichment in aqueous environments
KTH, Superseded Departments, Land and Water Resources Engineering.ORCID iD: 0000-0003-4350-9950
KTH, Superseded Departments, Land and Water Resources Engineering.
KTH, Superseded Departments, Land and Water Resources Engineering.ORCID iD: 0000-0001-8771-7941
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2004 (English)In: Applied Geochemistry, ISSN 0883-2927, E-ISSN 1872-9134, Vol. 19, no 2, 169-180 p.Article in journal (Refereed) Published
Abstract [en]

Arsenic is present in aqueous environments in +III and +V oxidation states. In oxidizing environments, the principle attenuation mechanism of As migration is its adsorption on Fe(III) oxide and hydroxides. The adsorption affinity is higher for As(V) under lower pH conditions and for As(III) under higher pH conditions. Ferric oxide and hydroxides can dissolve under low Eh and pH conditions releasing adsorbed As. Oxidation-reduction processes often involve high organic matter content in sediments and also contamination by organics such as BTEX. Arsenic may desorb under high pH conditions. Changes of pH can be related to some redox reactions, cation exchange reactions driving dissolution of carbonates, and dissolution of silicates. In very reducing environments, where SO4 reduction takes place, secondary sulfide minerals like As-bearing pyrite and orpiment, As2S3, can incorporate As. Geochemical modeling can be divided into two principal categories: (a) forward modeling and (b) inverse modeling. Forward modeling is used to predict water chemistry after completion of predetermined reactions. Inverse modeling is used to suggest which processes take place along a flowpath. Complex coupled transport and geochemistry programs, which allow for simulation of As adsorption, are becoming available. A common modeling approach is based on forward modeling with surface complexation modeling (SCM) of As adsorption, which can incorporate the effect of different adsorbent/As ratios, adsorption sites density, area available for adsorption, pH changes and competition of As for adsorption sites with other dissolved species such as phosphate. The adsorption modeling can be performed in both batch and transport modes in codes such as PHREEQC. Inverse modeling is generally used to verify hypotheses on the origin of As. Basic prerequisites of inverse modeling are the knowledge of flow pattern (sampling points used in model have to be hydraulically connected) and information about mineralogy including As mineral phases. Case studies of geochemical modeling including modeling of As adsorption are presented.

Place, publisher, year, edition, pages
2004. Vol. 19, no 2, 169-180 p.
Keyword [en]
ground-water, reactive transport, united-states, competitive adsorption, west-bengal, bangladesh, phosphate, aquifers, surface, acid
National Category
Civil Engineering
URN: urn:nbn:se:kth:diva-23122DOI: 10.1016/j.apgeochem.2003.09.005ISI: 000188550600002ScopusID: 2-s2.0-0842267453OAI: diva2:341820
QC 20100525 QC 20111019Available from: 2010-08-10 Created: 2010-08-10 Last updated: 2011-10-19Bibliographically approved

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Bhattacharya, ProsunJacks, GunnarGustafsson, Jon Pettervon Brömssen, Mattias
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