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Adsorption of Orthophosphate to Humic‐Fe‐Complexes and to Amorphous Fe‐Oxide

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Gerke, Jörg, Hermann, Reinhold·1992·Zeitschrift für Pflanzenernährung und Bodenkunde

Abstract

The adsorption of orthophosphate to humic surfaces was studied in a model experiment. The adsorption maximum of humic substances greatly increased with higher concentrations of organically complexed Fe (III), indicating that orthophosphate was bound to humic surfaces via metal bridges. The molar ratio P adsorbed/Fe was nearly 1 for Fe freshly complexed to humic substances, whereas the ratio for amorphous Fe‐oxide was a tenfold lower. An increase in pH from 5.2 to 6.2 lead to an increase of P‐adsorption of about 30% in the case of humic‐Fe‐surfaces, which could be explained by an increased accessibility of adsorption sites at pH 6.2. The addition of a 0.01 M CaCl 2‐matrix increased orthophosphate adsorption at pH 6.2 but not at pH 5.2. This could be explained by electrostatic interactions caused by the Ca++ ion.

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Metadata

Authors
Gerke, J., & Hermann, R.
Venue
Zeitschrift für Pflanzenernährung und Bodenkunde
Publisher
Wiley
Published
1992-01
Volume
155
Issue
3
Pages
233-236
ISSN
0044-3263 (ISSN-L)
OpenAlex
W2012205398
Cited by
199
References
0
FWCI
22.37
Type
journal article
Language
en
Open access
green

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CoChat. (2026). Citation check: Adsorption of Orthophosphate to Humic‐Fe‐Complexes and to Amorphous Fe‐Oxide. https://app.cochat.ai/papers/10.1002/jpln.19921550313
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Gerke, J., & Hermann, R. (1992). Adsorption of Orthophosphate to Humic‐Fe‐Complexes and to Amorphous Fe‐Oxide. Zeitschrift für Pflanzenernährung und Bodenkunde. https://doi.org/10.1002/jpln.19921550313

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