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2009-05-19_REVISION - M1977416
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2009-05-19_REVISION - M1977416
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Last modified
6/15/2021 2:18:35 PM
Creation date
5/27/2009 2:10:46 PM
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Template:
DRMS Permit Index
Permit No
M1977416
IBM Index Class Name
REVISION
Doc Date
5/19/2009
Doc Name
EPP (AM-01) Attachment 3: Soil Adsorption (part 3)
From
Denison Mines
To
DRMS
Type & Sequence
AM1
Email Name
RCO
Media Type
D
Archive
No
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• The fraction of selenium (x) that substitutes into the phase depends on the pH and the <br />concentration of selenium in solution (the ratio of SeO3-2 to OH-). <br />Selenium Adsorption <br />Adsorption of selenium depends on the speciation of selenium, pH, and concentrations <br />of competing ions in the water, and the specific properties of the adsorption media. <br />Selenite is adsorbed to ferric hydroxide to a greater extent than selenate. As mentioned <br />previously, both selenite and selenate are negatively charged ions (anions) and tend to <br />adsorb to positively charged surfaces. <br />Selenite tends to adsorb significantly better than selenate on most solid surfaces. <br />Selenite forms a strong bond called an "inner-sphere complex", while selenate forms a <br />weaker bond with solid surfaces called an "outer-sphere complex". <br />At low pH, the surfaces of minerals tend to be positively charged, while at high pH the <br />surfaces are negative. Therefore, adsorption efficiency and capacity for selenite and <br />selenate increase with decreasing pH. <br />At low pH values, the water and mineral surfaces have higher concentrations of <br />hydronium ion (H30+) which imparts a positive charge to the surface. As the pH <br />increases, the hydronium ion concentration decreases relative to the hydroxide ion (OH-) <br />concentration in both the water and the solid materials within the water. At a specific <br />• threshold pH value called the pH of the zero-point-of-charge (ZPC), the surface charge <br />transitions from positive to neutral to negative. Once the surface charge becomes <br />negative, adsorption of the negatively charged arsenate ions become less prevalent. The <br />pH of the ZPC is different for different materials, as shown in Table 1. <br />Table 1 off of the Zero-Point-of-Charae (oH7PAfor Various Minerals <br /> <br />Material -- - - -- ---------- <br />Formula <br />HZPC <br />Magnetite Fe304 6.5 <br />Goethite Fe00H 7.8 <br />Hematite Fe203 6.7 <br />Amorphous Ferric hydroxide Fe(OH)3 8.5 <br />Amorphous Silica Si02 2.0 <br />Montmorillonite Clay Nao_2Cao.iA12Si40Io OH 2.10 H2O 2.5 <br />Kaolinite Clay A12Si2O5(OH)4 4.6 <br />The materials with a higher pHzrc are able to maintain a positive charge at a higher pH <br />than for materials with a lower pHzrc. Of the materials listed in Table 1, amorphous <br />ferric hydroxide is the best anion adsorbent at higher pH values (below 8.5). <br />Negatively charged ions or neutral species, such as phosphate and silicate, respectively, <br />can compete with selenium for adsorption sites on the media. Therefore, selenium <br />adsorption is favored for waters low in phosphate and silicate. <br />References
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