1970
DOI: 10.2136/sssaj1970.03615995003400060034x
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Adsorption of Boron by Ferromagnesian Minerals and Magnesium Hydroxide

Abstract: Arid‐zone soils are found to have appreciable boron‐sorption capacities in their silt and sand fractions. The site of this sorption is hypothesized to be magnesium‐hydroxy clusters and coatings that exist on the weathering surfaces of ferromagnesian minerals such as olivine, enstatite, diopside, augite, tremolite, and hornblende as well as micaceous layer‐silicate minerals.

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Cited by 27 publications
(12 citation statements)
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“…Rhodes and associates (43) found many arid soils to have a boronsorption capacity associated with their silt and sand fractions. They found that minerals containing magnesium sorbed more boron from solution than minerals which did not contain magnesium.…”
Section: Chapter II Literature Reviewmentioning
confidence: 99%
“…Rhodes and associates (43) found many arid soils to have a boronsorption capacity associated with their silt and sand fractions. They found that minerals containing magnesium sorbed more boron from solution than minerals which did not contain magnesium.…”
Section: Chapter II Literature Reviewmentioning
confidence: 99%
“…The examination of the fractionation scheme on a series of Ontario soils will be discussed in a following paper (Evans et al 1996). Some preliminary results on these soils have been presented previously (Hou et al 1994 Boron associated with Mn oxides (Rhoades et al 1970) was not considered in our proposed scheme because Mn oxides have a point ofnet zero proton charge less than 1.5 (Balistrieri and Chao 1990) For personal use only. Between each successive extraction, the reiidue was washed with 8 mL of water and the solution was discarded after centrifugation.…”
mentioning
confidence: 99%
“…Such materials are, ferromagnesian minerals and magnesium hydroxide (Rhoades et al, 1970), hydrous oxides and iron aluminium (McPhail et al, 1972), allophane (Su & Suarez, 1997), montmorilonite, illite and kaolinite (Chieng & Chong, 2012;Keren & O' Connor, 1982), humic acids (Gu & Lowe, 1990), fly ash and coal (Polat et al, 2004), magnesia (Dionisiou et al, 2006), activated carbon (Kluczka et al, 2007) and selective resins as Amberlite IRA-743 (Demircivi & Nasun-Saygili, 2008). …”
Section: Resultsmentioning
confidence: 99%