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In-situ mobilization and transformation of iron oxides-adsorbed arsenate in natural groundwater
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文摘

In situ experiments were used to delineate As mobilization from Fe(III) oxides.

Arsenic desorption occurred from ferrihydrite, goethite and hematite.

Arsenic was released from reductive dissolution of ferrihydrite.

Transformation of ferrihydrite to secondary Fe minerals favored As mobilization.

Goethite and hematite would be the major oxides controlling groundwater As content.

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