Origins of root-mediated pH changes in the rhizosphere and their responses to environmental constraints: A review
By P. Hinsinger, C. Plassard, Caixian Tang, B. Jaillard. Plant and Soil, 2004
1,357 citations recorded by the source corpus.
Subfields: Plant Science
View Paper: https://www.semanticscholar.org/paper/3d53e455182d15b70569d7f83c3c818845dbbc0b
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Citations in the corpus
- Carboxylate release of wheat, canola and 11 grain legume species as affected by phosphorus status (2006, background): “The rhizosphere pH affects the bioavailability of many nutrients and toxic elements, root physiology and rhizosphere micro-organisms (Hinsinger et al. 2003).”
- Rhizosphere processes and management in plant-assisted bioremediation (phytoremediation) of soils (2009, background): “Nitrogen fixation has been shown to result in substantial acidification in alder rhizospheres (Van Miegroet and Cole 1984) because nitrogen uptake relying on N2-fixation rather than anionic nitrate results in enhanced proton exudation to maintain the cation–anion balance (Hinsinger et al. 2003).”
- Root structure and functioning for efficient acquisition of phosphorus: Matching morphological and physiological traits. (2006, background): “In addition to P immobilization, acidification can influence the extent of ionization of carboxylates (Jones, 1998b; Hinsinger et al., 2003), which can reduce their chelating ability, potentially rendering them ineffective in acidified soil (Pearse et al., 2006)”
- Rock phosphate-solubilizing Actinomycetes: screening for plant growth-promoting activities (2008, background): “The result demonstrated that the plant on its own has a very weak ability to solubilize RP. Several reports indicate the ability of the plant to produce organic acids that have often been referred to as a possible source of rhizosphere acidification ( Hinsinger et al. 2003 ) and so to the phosphate ”
- Intercropping with legume for agroecological cropping systems: Complementarity and facilitation processes and the importance of soil microorganisms. A review (2017, background): “Studies on cereal/legume intercropping assume that the main process affecting N and P facilitation is the change in root-induced pH through fixation of N2 by the legume (Bargaz et al., 2015b; Betencourt, 2012; Hinsinger, 2001; Hinsinger et al., 2003; Latati et al., 2014).”
- Rhizosphere engineering and management for sustainable agriculture (2009, background): “In addition to generating a driving force for membrane transport, H efflux can contribute to nutrient acquisition by acidifying the rhizosphere (Hinsinger et al. 2003).”
- Root exudate components change litter decomposition in a simulated rhizosphere depending on temperature (2006, background): “Many studies have shown that organic acids enhance plant nutrient mobilization in the rhizosphere by the formation of organometallic complexes (e.g. P, Fe, Cu, Mn; Hinsinger et al. 2003; Dakora and Phillips 2002).”
- Dynamics of phosphorus fractions in the rhizosphere of common bean (Phaseolus vulgaris L.) and durum wheat (Triticum turgidum durum L.) grown in monocropping and intercropping systems (2008, background): “2003), such as rhizosphere acidification (Hinsinger et al. 2003; Neumann and Römheld 1999; Tang et al. 2004; Shen et al. 2004), exudation of carboxylates (Dinkelaker et al.”
- Indole-3-acetic acid in microbial and microorganism-plant signaling. (2007, background): “The rhizosphere is generally considered to be a weakly acid environment (Hinsinger et al., 2003), and therefore it is expected that a considerable part of IAA is in its protonated form in the rhizosphere.”
- Variation in morphological and physiological parameters in herbaceous perennial legumes in response to phosphorus supply (2010, neutral): “Organic acids have often been referred to as a possible source of rhizosphere acidification (Hinsinger et al. 2003).”
- Rhizospheric organic compounds in the soil–microorganism–plant system: their role in iron availability (2014, background): “In addition, in nutrient-deficient conditions plant roots enhance the qualitative and quantitative root-exudate pattern, increasing mineral dissolution and thus Fe mobilization even more (Hinsinger et al., 2003).”
- Phosphorus uptake and rhizosphere properties of intercropped and monocropped maize, faba bean, and white lupin in acidic soil (2010, background): “N2-fixing legumes often acidify the rhizosphere due to excess cation over anion uptake (Hinsinger et al. 2003; Tang et al. 1997, 2001, 2004).”