2010
DOI: 10.1016/j.watres.2010.06.056
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The role of Al-Goethites on arsenate mobility

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Cited by 54 publications
(28 citation statements)
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“…When the solid's specific surface area is also considered, the differences in the arsenic uptake amongst the various iron oxide and oxy-hydroxides and aluminum hydroxide are not so evident. Corroborating with this observation, Silva et al (2010) found that, on a weight basis, the maximum As(V) uptake by various minerals followed the sequence: Ferrihydrite (1.258 ± 0.034 mmol g À1 ) > Gibbsite (0.228 ± 0.006 mmol g À1 ) > Hematite (0.193 ± 0.006 mmol g À1 ) > Goethite (0.101 ± 0.002 mmol g À1 ). On the other hand, when the specific surface area of the solids was also taken into account, all the Fe and Al oxy-hydroxides tested reached a maximum adsorption capacity of approximately 0.005 mmol m À2 .…”
Section: Introductionsupporting
confidence: 57%
“…When the solid's specific surface area is also considered, the differences in the arsenic uptake amongst the various iron oxide and oxy-hydroxides and aluminum hydroxide are not so evident. Corroborating with this observation, Silva et al (2010) found that, on a weight basis, the maximum As(V) uptake by various minerals followed the sequence: Ferrihydrite (1.258 ± 0.034 mmol g À1 ) > Gibbsite (0.228 ± 0.006 mmol g À1 ) > Hematite (0.193 ± 0.006 mmol g À1 ) > Goethite (0.101 ± 0.002 mmol g À1 ). On the other hand, when the specific surface area of the solids was also taken into account, all the Fe and Al oxy-hydroxides tested reached a maximum adsorption capacity of approximately 0.005 mmol m À2 .…”
Section: Introductionsupporting
confidence: 57%
“…The effects of co-existing AsO 4 3− or Cd 2+ were also studied. Because aqueous Cd 2+ can form Cd(OH) 2 and precipitate with OH − when pH increases, its precipitation curves were made to compare with the real Cd adsorption on goethite.…”
Section: Adsorption Edgementioning
confidence: 99%
“…Arsenic contamination can come from geological, industrial and agricultural sources [1,2]. Cadmium exerts pressure on the environment mainly through anthropogenic discharge [3].…”
Section: Introductionmentioning
confidence: 99%
“…the surface of oxides and hydroxides in clearly acid environments (pH between 3.5 and 5.5; Silva et al, 2010), whereas increased pH values (from above 5 for clay minerals to above 12 for calcite) favor desorption (Golberg and Glaubig 1988). Any case, most of the adsorbed As(V) did not desorb, indicating notable irreversibility of the process.…”
Section: Adsorption/desorption As a Function Of Added As(v) Concentramentioning
confidence: 99%