Dissolved organic carbon retention by coprecipitation during the oxidation of ferrous iron-Reference-Cited by-同舟云学术

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Dissolved organic carbon retention by coprecipitation during the oxidation of ferrous iron

Published:2017-12 Issue: Volume:307 Page:19-29
ISSN:0016-7061
Container-title:Geoderma
language:en
Short-container-title:Geoderma

Author:

Sodano Marcella,Lerda Cristina,Nisticò Roberto,Martin Maria^ORCID,Magnacca Giuliana^ORCID,Celi Luisella,Said-Pullicino Daniel^ORCID

Funder

MIUR

FACCE-JPI

Publisher

Elsevier BV

Subject

Soil Science

Reference57 articles.

1. Effects of silicon on the crystallization and adsorption properties of ferric oxides;Anderson;Environ. Sci. Technol.,1985

2. Particle size, charge and colloidal stability of humic acids coprecipitated with ferrihydrite;Angelico;Chemosphere,2014

3. Cycling and composition of organic matter in terrestrial and marine ecosystems;Baldock;Mar. Chem.,2004

4. Mobilization of colloidal carbon during iron reduction in basaltic soils;Buettner;Geoderma,2014

5. Si incorporation into hematite by heating Si-ferrihydrite;Campbell;Langmuir,2002

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