2021
DOI: 10.1016/j.geoderma.2020.114799
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Adsorption of phosphate and cadmium on iron (oxyhydr)oxides: A comparative study on ferrihydrite, goethite, and hematite

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Cited by 113 publications
(46 citation statements)
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“…Meanwhile, there is no Fe−P precipitation, meaning that electrostatic or physical adsorption has occurred. 70 Therefore, according to the above results, the reaction mechanism of Fe 3 O 4 nanoparticles accompanied by coordination can be depicted as follows: 35 − was also adsorbed by electrostatic attraction with (Fe-TEA) + . Thus, one can infer a better adsorption performance for GL-Fe 3 O 4 -TEA because of more adsorption sites (Figure 9).…”
Section: ■ Results and Discussionmentioning
confidence: 84%
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“…Meanwhile, there is no Fe−P precipitation, meaning that electrostatic or physical adsorption has occurred. 70 Therefore, according to the above results, the reaction mechanism of Fe 3 O 4 nanoparticles accompanied by coordination can be depicted as follows: 35 − was also adsorbed by electrostatic attraction with (Fe-TEA) + . Thus, one can infer a better adsorption performance for GL-Fe 3 O 4 -TEA because of more adsorption sites (Figure 9).…”
Section: ■ Results and Discussionmentioning
confidence: 84%
“…Therefore, according to the above results, the reaction mechanism of Fe 3 O 4 nanoparticles accompanied by coordination can be depicted as follows: FeCl 3 /FeCl 2 are hydrolyzed to Fe–OH, while portions of Fe 3+ /Fe 2+ are coordinated with TEA to form (Fe-TEA) + Cl – , which preserve the positive charge. On the basis of the above mechanism combined with the established phosphate adsorption mechanism on Fe 3 O 4 , the phosphate adsorption models on GL-Fe 3 O 4 -TEA could include three types of interaction (electrostatic attraction with and without H + and ion exchange with OH – ) Fe OH + normalH 2 PO 4 = Fe ( H 2 PO 4 ) + OH Cl ··· Fe TEA + normalH 2 PO 4 = ( H 2 PO 4 ) · · · ( Fe TEA ) + Cl Fe OH + normalH + + normalH 2 PO 4 = Fe OH 2 ··· normalH 2 PO 4 …”
Section: Resultsmentioning
confidence: 89%
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“…However, they are more advanced materials that require special reagents to produce. It is also a mineral that effectively adsorbs phosphates by surface complexation and precipitation [ 78 , 79 , 80 ]. As shown in Table 8 diatomite coated by hydrous iron oxide and metallic iron/iron oxides are characterized by a significant increase in the adsorption capacity of phosphates and chromates [ 27 , 28 ].…”
Section: Resultsmentioning
confidence: 99%
“…Hematite is one of the most abundant iron (oxyhydr)oxide minerals in soils, rocks and crust. [32][33][34] And the {001} facet of hematite possesses a relatively low surface energy that makes it one of the most exposed and naturally growing surfaces for natural hematite, [35][36][37] and widely studied in geochemical and environmental sciences. [38][39][40][41][42][43] Moreover, its atomic structure and properties have been extensively studied both experimentally and theoretically, which are the preconditions to clarify the mechanism of oxalate promoted iron dissolution.…”
Section: Introductionmentioning
confidence: 99%