Solubilization of rock phosphate by rape
By E. Hoffland, G. Findenegg, J. Nelemans. Plant and Soil, 2005
161 citations recorded by the source corpus.
Subfields: Biomaterials, Industrial and Manufacturing Engineering, Soil Science
View Paper: https://www.semanticscholar.org/paper/71726afb35e023df96e707cb1ccc07c57092a146
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In Biomaterials
In Industrial and Manufacturing Engineering
In Soil Science
Citations in the corpus
- Low-P tolerance by maize (Zea mays L.) genotypes: Significance of root growth, and organic acids and acid phosphatase root exudation (2004, background): “…under P-deficient conditions, the release of citric and malic acids, both determined in the literature as efficient in the P mobilization from soil (Hoffland et al., 1989; Jones and Darrah, 1994b; Nagarajah et al., 1970), was significantly higher for NST than for the other genotypes (p < 0.001).”
- Solubilization of Insoluble Inorganic Phosphate by Hyphal Exudates of Arbuscular Mycorrhizal Fungi (2006, unknown): “Under P-deficient conditions, lupin (Lupinus albus) (Gardner et al., 1983), rape (Brassica napus) (Hoffland et al., 1989), and alfalfa (Medicago sativa) (Lipton et al., 1987) released organic acids.”
- Root exudates as mediators of mineral acquisition in low-nutrient environments (2002, background): “Root exudation of high concentrations of organic acid anions as a result of P deficiency (Hoffland et al., 1989) does lower rhizosphere pH, making P (Haynes, 1990; Jones and Darrah, 1994) and micronutrients such as Mn, Fe and Zn to be more available in cal-”
- Organic Anion Exudation by Lowland Rice (Oryza sativa L.) at Zinc and Phosphorus Deficiency (2006, background): “Similar to white lupin (Gardner et al., 1983), alfalfa (Lipton et al., 1987) and rape (Hoffland et al., 1989) citrate exudation by rice is increased as a response to phosphorus (P) deficiency, leading to increased P uptake (Kirk et al., 1999).”
- Origins of root-mediated pH changes in the rhizosphere and their responses to environmental constraints: A review (2004, background): “…in response to the same environmental stresses as above-mentioned for the release of H+, namely Fe deficiency (Ohwaki and Sugahara, 1997), P deficiency (Hoffland et al., 1989; Imas et al., 1997b; Keerthisinghe et al., 1998; Neumann and Römheld, 1999) and Al toxicity (Delhaize et al., 1993).”
- Development of specific rhizosphere bacterial communities in relation to plant species, nutrition and soil type (2004, background): “Canola is considered to be a P efficient plant species that exudes organic acids in response to P deficiency (Hoffland et al., 1989).”
- Importance of rhizodeposition in the coupling of plant and microbial productivity (2003, background): “…in natural systems the cycling of N through herbivore excreta will contribute to this effect, similar findings are # 2003 Blackwell Publishing Ltd, European Journal of Soil Science, 54, 741–750 reported for experimental systems where the grass is simply cut and not grazed (Holland & Detling, 1990).”
- Carbon flow in the rhizosphere: carbon trading at the soil–root interface (2009, background): “Generally, rates of exudate loss are greater at root tips in comparison to mature root regions (McDougal and Rovira 1970; Hoffland et al. 1989).”
- Wheat, canola and grain legume access to soil phosphorus fractions differs in soils with contrasting phosphorus dynamics (2009, background): “P-deficient canola and N-fixing legumes typically acidify the rhizosphere (Hoffland et al. 1989; Tang et al. 2004); however, all species in our study generally increased rhizosphere pH (except in the highly buffered Harvey soil) presumably due to preferential uptake of NO3 − as the N source (Tang et”