During its life cycle the plant releases a wide variety of compounds from its roots. The composition of these compounds, known as root exudates, varies widely and includes, in addition to organic moieties of low molecular weight, inorganic ions, gases, protons and electrons, a mucilagenous substance mainly formed by uronic acid polymers and polysaccharides (Rovira et al., 1983; Uren and Reisenauer, 1988).
The mucilage mixed with material of microbiological origin envelopes the apical regions of the root in a gelatinous layer. Its distribution is somewhat variable depending on several factors such as plant species, age, environmental conditions etc. This gelatinous layer, which constitutes the soil‐root interface, plays a fundamental role in plant nutrition (Jenny and Grossenbacher, 1963). Being highly hydrated, it ensures effective contact between the root system and the soil surfaces, facilitating exchange processes, transfer of water and nutrients, and the growth of the root. The...
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Bibliography
Crowley, D.E.,Wang, Y.C., Reid, C.P.P., and Szaniszlo, P.J., 1991. Mechanisms of iron acquisition from siderophores by microorganisms and plants, Plant and Soil 130, 179–198.
Deiana, S., Gessa, C., Piu, P., and Seeber, R., 1991. Iron(III) reduction by D‐galacturonic acid. Part III. Influence of the presence of additional metal ions and of 2‐amino‐2‐deoxy‐D‐gluconic acid. J. Chem. Soc. Dalton Trans., 1237–1241.
Deiana, S., Gessa, C., Marchetti, M., and Usai, M., 1995. Phenolic acid redox properties: pH influence on iron(III) reduction by caffeic acid. Soil Sci. Soc. Am. J., 59: 1301–1307.
Deiana, S., Manunza, B., Palma, A., Premoli, A., and Gessa, C., 2001. Interaction and mobilization of metal ions at the soil–root interface. In Gobran, G.R., Wenzel, W., and Lombi, E., eds., Trace Elements in the Rhizosphere. Boca Raton, FL: CRC Press, pp. 127–148.
Deiana, S., Gessa, C., Palma, A., Premoli, A., and Senette, C., 2003a. Influence of organic acids exuded by plants on the interaction of copper with the polysaccharidic components of the root mucilages. Org. Geochem., 34: 651–660.
Deiana, S., Premoli, A., Senette, C., Gessa, C., and Marzadori, C., 2003b. Role of uronic acid polymers on the availability of iron to plants. J. Plant Nutr., 26: 1927–1941.
Didier, M., Pellet, M., Grunes, D.L., and Kochian, L.V., 1995. Organic acid exudation as an aluminum‐tolerance mechanism in maize (Zea mais). Planta, 196: 788–795.
Floyd, R.A., and Ohlrogge, A.J., 1970. Gel formation on nodal root surfaces of Zea mais. Investigation on the gel composition. Plant Soil, 33: 341–343.
Fusuo, Z., Romheld, V., and Marschner, H., 1989. Effect of zinc deficiency in wheat on the release of zinc and iron mobilizing root exudates. Z. Pflanzen. Bodenk., 152: 205–210.
Gessa, C., and Deiana, S., 1991a. Ca‐polygalacturonate as a model for soil–root interface II: fribrillar structure and comparison with natural root mucilages. Plant Soil, 140: 1–13.
Gessa, C., and Deiana, S., 1991b. Role of soil–root interface in mobilization of nutrients and their absorption by plants. Trends Soil Sci., 1: 307–313.
Gessa, C., De Cherchi, M.L., Dessi, A., Deiana, S., and Micera, G., 1983. The reduction of Fe(III) to Fe(II) and V(V) to V(IV) by polygalacturonic acid: a reduction and complexation mechanism of biochemical significance. Inorg. Chim. Acta, 80: L53–L55.
Gessa, C., Deiana, S., Premoli, A., and Ciurli, S., 1997. Redox activity of caffeic acid towars iron(III) complexed in a polygalacturonic networt. Planta Soil, 190: 289–299.
Mimmo, T., Marzadori, C., Francioso, O., Deiana, S., and Gessa, C., 2003. Effects of aluminum sorption on a Ca‐polygalacturonate network used as a soil–root interface model. Biopolymers (Biospectroscopy) 70: 655–661.
Grayston, S.J., Vaughn, D., and Jones, D., 1996. Rhizosphere carbon flow in trees in comparison with annual plants: the importance of root exudation and its impact on microbial activity and nutrient availability. Appl. Soil Ecol., 5: 29–56.
Jenny, H., and Grossenbacher, K., 1963. Root–soil boundary zones as seen in the electron microscope. Soil Sci. Am. Proc., 27: 273–277.
Jones, D.L., 1998. Organic acids in the rhizosphere: a critical review. Plant Soil, 205: 25–44.
Leppard, G.G., 1974. Rhizoplane fibrils in wheat: demonstration and derivation. Science, 185: 1066–1067.
Manunza, B., Deiana, S., and Gessa, C., 1999. Molecular dynamics of pectic substances. In Balbuena, P.B., and Seminario, J.M., eds., Molecular Dynamics: From Classical to Quantum Methods. Theor. Comput. Chem., 7: 899–932.
Marschner, H., Romheld, V., Horst, W.J., and Martin, P., 1986. Root induced changes in the rhizosphere: importance for the mineral nutrition of plants. Z. Pflanzen. Bodenk., 149: 441–456.
Ramamoorthy, S., and Leppard, G.G., 1977. Fibrillar pectin and contact cation exchange at the root surfaces. J. Theor. Biol., 66: 527–540.
Romheld, V., 1987. Existence of two different strategies for the acquisition of iron in higher plants. In Winkelmann, G., Van der Helm, D., and Neilands, J.B., eds., Iron Transport in Animals, Plants, and Microorganisms. Weinheim: VCH Chemie, pp. 353–374.
Rovira, A.D., Bowen, G.D., and Foster, R.C., 1983. The significance of rhizosphere microflora and mycorrhizas in plant nutrition. In: Lauchli, A., and Bielesky, R.L., Encyclopedia of Plant Physiology, Vol. 15A. Berlin: Springer, pp. 61–93.
Uren, N.C., and Reisenauer, H.M., 1988. The role of root exudates on nutrient acquisition. Adv. Plant Nutr., 3: 79–114
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2008 Springer
About this entry
Cite this entry
Gupta, R.K. et al. (2008). Soil‐root interface. In: Chesworth, W. (eds) Encyclopedia of Soil Science. Encyclopedia of Earth Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-3995-9_561
Download citation
DOI: https://doi.org/10.1007/978-1-4020-3995-9_561
Published:
Publisher Name: Springer, Dordrecht
Print ISBN: 978-1-4020-3994-2
Online ISBN: 978-1-4020-3995-9
eBook Packages: Earth and Environmental ScienceReference Module Physical and Materials ScienceReference Module Earth and Environmental Sciences