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Characterization of ion sorption on ...

Bostick, Benjamin Carlos.

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Characterization of ion sorption on metal sulfide minerals using macroscopic and spectroscopic approaches.

Record Type:	Language materials, printed : Monograph/item
Title/Author:	Characterization of ion sorption on metal sulfide minerals using macroscopic and spectroscopic approaches./
Author:	Bostick, Benjamin Carlos.
Description:	234 p.
Notes:	Adviser: Scott Fendorf.
Contained By:	Dissertation Abstracts International63-01B.
Subject:	Biogeochemistry. -
Online resource:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3038068
ISBN:	0493516824

Characterization of ion sorption on metal sulfide minerals using macroscopic and spectroscopic approaches.
Bostick, Benjamin Carlos.

Characterization of ion sorption on metal sulfide minerals using macroscopic and spectroscopic approaches. - 234 p.

Adviser: Scott Fendorf.

Thesis (Ph.D.)--Stanford University, 2002.

Sulfide minerals commonly form in anoxic environments, often sorbing trace elements. The mechanism of such sorption is a critical factor in determining their transport and fate in the environment. Consequently, this research examines the sorption of three such elements, arsenic, molybdenum, and zinc on sulfide mineral suspensions and in soils subject to periodic reduction. Arsenite sorption to sphalerite (ZnS), galena (PbS), amorphous iron sulfide (FeS), and pyrite (FeS2) was investigated as a function of solution composition and using X-ray absorption spectroscopy (XAS). Sorption to each followed a Langmuir isotherm, and increased sharply above pH 5 to 6. Spectroscopic investigation revealed that a large change in arsenic coordination accompanied sorption on sulfide minerals. An As3S3(SH)3-type surface complex was formed on ZnS and PbS, while As(III) was reduced to As(−I) on FeS and FeS2 and a surface precipitate similar in structure to FeAsS was formed. This surface precipitate was also formed upon arsenite sorption to estuarine soils from Pescadero, California, although it was partially converted to orpiment over time. Importantly, arsenite was irreversibly retained on each of these sulfide minerals except PbS; thus, arsenic will likely be stable in sulfidic, anoxic environments. However, oxidation may release arsenic in these systems.

ISBN: 0493516824Subjects--Topical Terms:

545717
Biogeochemistry.

Characterization of ion sorption on metal sulfide minerals using macroscopic and spectroscopic approaches.
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035 $a (UnM)AAI3038068
035 $a AAI3038068
040 $a UnM $c UnM
100 1 $a Bostick, Benjamin Carlos. $3 1251697
245 1 0 $a Characterization of ion sorption on metal sulfide minerals using macroscopic and spectroscopic approaches.
300 $a 234 p.
500 $a Adviser: Scott Fendorf.
500 $a Source: Dissertation Abstracts International, Volume: 63-01, Section: B, page: 0155.
502 $a Thesis (Ph.D.)--Stanford University, 2002.
520 $a Sulfide minerals commonly form in anoxic environments, often sorbing trace elements. The mechanism of such sorption is a critical factor in determining their transport and fate in the environment. Consequently, this research examines the sorption of three such elements, arsenic, molybdenum, and zinc on sulfide mineral suspensions and in soils subject to periodic reduction. Arsenite sorption to sphalerite (ZnS), galena (PbS), amorphous iron sulfide (FeS), and pyrite (FeS2) was investigated as a function of solution composition and using X-ray absorption spectroscopy (XAS). Sorption to each followed a Langmuir isotherm, and increased sharply above pH 5 to 6. Spectroscopic investigation revealed that a large change in arsenic coordination accompanied sorption on sulfide minerals. An As3S3(SH)3-type surface complex was formed on ZnS and PbS, while As(III) was reduced to As(−I) on FeS and FeS2 and a surface precipitate similar in structure to FeAsS was formed. This surface precipitate was also formed upon arsenite sorption to estuarine soils from Pescadero, California, although it was partially converted to orpiment over time. Importantly, arsenite was irreversibly retained on each of these sulfide minerals except PbS; thus, arsenic will likely be stable in sulfidic, anoxic environments. However, oxidation may release arsenic in these systems.
520 $a Other ions react in distinct manners. Molybdate and tetrathiomolybdate are most strongly retained to pyrite under acidic conditions. Molybdate formed a weak bidentate-mononuclear sorption complex on FeS2 that was reversibly adsorbed while tetrathiomolybdate adsorption was irreversible and it formed a Mo-Fe-S cubane on the FeS2 surface, in which the Mo is triply coordinated to surface-bound sulfur atoms. Zinc was often sequestered in a contaminated wetland as ZnS, ZnCO3, ZnO and Zn adsorbed on (hydr)oxides. Zinc speciation was dynamic, responding to changes in overlying water depth. The fractions of ZnS and ZnCO3 were highest under flooded conditions, while adsorbed Zn species occurred predominantly under oxic conditions (dry or shallow water depths). Therefore, the dynamic nature of sulfidic environments needs to be considered when determining trace element partitioning.
590 $a School code: 0212.
650 4 $a Biogeochemistry. $3 545717
650 4 $a Environmental Sciences. $3 676987
650 4 $a Geochemistry. $3 539092
690 $a 0425
690 $a 0768
690 $a 0996
710 2 0 $a Stanford University. $3 754827
773 0 $t Dissertation Abstracts International $g 63-01B.
790 $a 0212
790 1 0 $a Fendorf, Scott, $e advisor
791 $a Ph.D.
792 $a 2002
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3038068