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ARCHIVED REPORTS_XR0008006
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2900 - Site Mitigation Program
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PR0541401
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ARCHIVED REPORTS_XR0008006
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Last modified
4/14/2020 2:25:29 PM
Creation date
4/14/2020 1:26:04 PM
Metadata
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Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0008006
RECORD_ID
PR0541401
PE
2950
FACILITY_ID
FA0006046
FACILITY_NAME
UNION OIL STATION #5098
STREET_NUMBER
5606
STREET_NAME
PACIFIC
STREET_TYPE
AVE
City
STOCKTON
Zip
95207
CURRENT_STATUS
02
SITE_LOCATION
5606 PACIFIC AVE
P_LOCATION
01
P_DISTRICT
002
QC Status
Approved
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ligands have been reported to increase the aqueous solubility of Cr(III) over that of the hydroxide <br /> complex(Palmer 1991) <br />' Controls on Chromium Solubili <br /> Cr(VI) as the chromate anion is highly soluble, and, under certain conditions, quite mobile in the <br /> aquatic environment Formation of lead chromate (PbCr04), barium chromate (BaCr04), or a barium <br /> chromate-sulfate solid solution (Ba(SO4, Cr04)) may control aqueous chromate concentrations in <br />' environments enriched in lead or barium (Rai 1989, Richard 1991) In most aquatic environments, <br /> however, chromate is removed from solution by formation of surface complexes on mineral oxides <br /> (manganese, aluminum, iron) and clay minerals The adsorption reaction is pH dependent with <br />' adsorption decreasing as pH increases Adsorption is also decreased by the presence of other anions, <br /> such as phosphate, silicate, and sulfate, which compete with chromate for surface complexation sites <br /> (Rai 1989) <br />' <br /> Cr(III) is generally II much less mobile in aquatic environments than Cr(VI) Cr(III) can form complexes <br /> with organic matter bound to aquifer solids and thus be removed from solution (Richard 1991) The <br /> Cr(ill) hydroxide complex is relatively insoluble and will precipitate to form Cr(OH)3 solid (Palmer <br /> 1991) However, if Fe(III) is present, dissolved Cr(OH)3 does not form solid Cr(OH)3, but rather forms <br /> an amorphous (Cr,Fe)(OH)3 solid solution (Palmer 1991) Amorphous (Cr,Fe)(OH)3 is believed to <br /> control Cr(III) solubility in natural systems (Rai 1989, Richard 1991) This exact solubility of chromium <br /> in amorphous (Cr,Fe)(OH)3 is related to its concentration in the solid and is less than that of Cr(OH)3 <br /> solid (Palmer 1991) At the relatively low chromium mole fractions (< 01) expected in natural <br /> environments, precipitation of (Cr, Fe)(OH)3 would maintain dissolved chromium levels below the EPA <br /> drinking water MCL over a wide range of pH values (Rai 1991) <br /> References <br /> Alloway, B J (Editor) 1990 Heavy Metals in Soils John Wiley& Sons, New York <br /> Bartlett, R and B James 1979 Behavior of chromium in soils III Oxidation Journal of Environmental <br /> Quality 8 31-35 <br /> Eary, L E and D Rai 1991 Chromate reduction by subsurface soils under acidic conditions Soil <br /> Science Society of America Joumal 55 676-683 <br /> Kroschwitz, J I (executive editor) 1992 Encyclopedia of Chemical Technology Fourth Edition Volume <br /> 6 John Wiley& Sons, New York <br />' C\Documents and 155 November 2004 <br /> Satti ngs�cgohnsen\Desktop\Unocal\GeechemEval_D <br /> oc doc <br />
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