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Origins of root-mediated pH changes in the rhizosphere and their responses to environmental constraints: A review
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Rhizosphere pH is also influenced by root exudates composition and ionic forms which may cause the acidification of alkaline soils or alkalization of acidic soils.
“The rhizosphere pH is also influenced by root exudates composition and ionic forms which may cause the acidification of alkaline soils or alkalization of acidic soils (Hinsinger et al., 2003).”
From Potentials of Miscanthus x giganteus for phytostabilization of trace element-contaminated soils: Ex situ experiment (2021) · cites this paper as Hinsinger et al., 2003
In soil-plant systems, pH is mainly driven by complex rhizosphere processes including the release of protons or hydroxyls at the root surface and in the rhizosphere during nutrient uptake.
“In soil-plant systems, pH is mainly driven by complex rhizosphere processes including the release of protons (H + ) or hydroxyls (OH - ) at the root surface and in the rhizosphere during nutrient uptake (Hinsinger et al., 2003; Blossfeld et al., 2010).”
From Potentials of Miscanthus x giganteus for phytostabilization of trace element-contaminated soils: Ex situ experiment (2021) · cites this paper as Hinsinger et al., 2003
Uptake of ions such as Fe, K and P that are necessary for plant growth may cause acidification over time and space.
“According to these authors, uptake of ions such as Fe, K and P that are necessary for plant growth may cause acidification over time and space.”
From Potentials of Miscanthus x giganteus for phytostabilization of trace element-contaminated soils: Ex situ experiment (2021) · cites this paper as Hinsinger et al., 2003
Soil alkalization occurs as part of the plant defense mechanism to mitigate toxicity as a result of acidic pH.
“Soil alkalization occurs as part of the plant defense mechanism to mitigate toxicity as a result of acidic pH (Hinsinger et al., 2003).”
From Potentials of Miscanthus x giganteus for phytostabilization of trace element-contaminated soils: Ex situ experiment (2021) · cites this paper as Hinsinger et al., 2003
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“Plant cultivation can slightly increase soil pH in acidic soils, which is attributed to root exudates that help buffer acidity [61, 62].”
Metadata
- Authors
- Hinsinger, P., Plassard, C., Tang, C., & Jaillard, B.
- Affiliations
- Institut National de Recherche pour l'Agriculture, l'Alimentation et l'Environnement (FR)
- The University of Western Australia (AU)
- Venue
- Plant and Soil
- Published
- 2003-01
- Volume
- 248
- Issue
- 1-2
- Pages
- 43-59
- ISSN
- 0032-079X (ISSN-L)
- 1573-5036
- OpenAlex
- W1984601337
- Cited by
- 1,402
- References
- 135
- Citations by year
- 2026: 91 · 2025: 88 · 2024: 63 · 2023: 84 · 2022: 92 · 2021: 112 · 2020: 87 · 2019: 78 · 2018: 78 · 2017: 75 · 2016: 67 · 2015: 62 · 2014: 52 · 2013: 55 · 2012: 50
- FWCI
- 26.82
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- Locations
- Plant and Soil (publishedVersion)
- UWA Profiles and Research Repository (UWA) (submittedVersion)
- HAL (submittedVersion)
- Topics
- Life Sciences › Agricultural and Biological Sciences › Plant Science › Plant nutrient uptake and metabolism
- Life Sciences › Agricultural and Biological Sciences › Plant Science › Plant-Microbe Interactions and Immunity
- Life Sciences › Agricultural and Biological Sciences › Soil Science › Soil Carbon and Nitrogen Dynamics
- Keywords
- rhizosphere pH, root exudates, root respiration, carbonic acid, soil pH buffering capacity, phosphorus deficiency, iron deficiency, aluminum toxicity, nutrient availability, rhizosphere microorganisms
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