Goethite Dissolution in the Presence of Phytosiderophores: Rates, Mechanisms, and the Synergistic Effect of Oxalate

By P. Reichard, S. Kraemer, S. Frazier, Ruben Kretzschmar. Plant and Soil, 2005

105 citations recorded by the source corpus.

Subfields: Plant Science, Renewable Energy, Sustainability and the Environment, Soil Science

View Paper: https://www.semanticscholar.org/paper/10f435e278a640c4c4ec804838c2066973c0c9a3

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Citations in the corpus

Release of plant-borne flavonoids into the rhizosphere and their role in plant nutrition (2010, background): “Strategy I is carried out by all higher plants, exceptGramineae, and involves physiological changes, such as increased excretion of protons (Bienfait 1985; Guerinot and Ying 1994; see Ma 2005 as review) and organic compounds (Marschner 1995), enhanced Fe (III)-reducing capacity mainly dependent on a”
Plant-microbe-soil interactions in the rhizosphere: an evolutionary perspective (2009, background): “Recently, Reichard et al. (2005) provided direct evidence for the involvement of phytosiderophores secreted by wheat (Triticum aestivum) in the ligand-promoted dissolution of goethite.”
Rhizospheric organic compounds in the soil–microorganism–plant system: their role in iron availability (2014, background): “A synergistic effect on the dissolution of goethite has been documented for oxalate, a common root exudate when P-deficiency and/or Al toxicity occurs, and deoxymugineic acid (DMA, a PS, Reichard et al., 2005); similarly, Cheah et al. (2003) detected goethite dissolution in discrete quantities but o”
Metallophores and Trace Metal Biogeochemistry (2015, background): “…of ligand-controlled dissolution (Stumm 1997), and several studies have shown metallophore-promoted dissolution rates to be proportional to the concentration of the ligand adsorbed on the mineral surface (Cheah et al. 2003; Duckworth et al. 2014; Duckworth and Sposito 2005a; Reichard et al. 2005).”
Iron dynamics in the rhizosphere as a case study for analyzing interactions between soils, plants and microbes (2009, background): “1999), the presence of organic acids (Reichard et al. 2005) or biosurfactants (Carrasco et al.”
Chapter 4 Iron Dynamics in the Rhizosphere: Consequences for Plant Health and Nutrition (2008, background): “In addition to these high-affinity ligands, microorganisms and plants also produce a range of lower-affinity ligands such as phenolics and, more abundantly, carboxylates, oxalate, and citrate, for instance ( Jones, 1998; Jones et al., 1996; Reichard et al., 2005).”
Rhizosphere: biophysics, biogeochemistry and ecological relevance (2009, background): “…thereby promote the dissolution of metal-bearing minerals as shown for Ca and Fe (Jones and Darrah 1994; Wallander 2000; Casarin et al. 2004; Reichard et al. 2005, 2007) and/or increase the total concentration of metal cations in the soil solution (Gerke et al. 2000; Reichard et al. 2005, 2007).”
Reviews and syntheses: Biological weathering and its consequences at different spatial levels – from nanoscale to global scale (2020, background): “…the steady-state dissolution of goethite by 2’-deoxymugineic acid (DMA) phytosiderophores has been demonstrated to be synergistically enhanced by oxalate (Reichard et al., 2005), and it is possible that synergistic interactions between other combinations of organic acids and siderophores may exist.”