Hostname: page-component-586b7cd67f-tf8b9 Total loading time: 0 Render date: 2024-11-26T00:57:51.191Z Has data issue: false hasContentIssue false
  • English
  • Français

Formation of hydroxy-interlayer vermiculite (HIV) in rhizosphere soils under German camomile cultivation and manure application

Published online by Cambridge University Press:  27 February 2018

Z. Mosleh ,
M. H. Salehi ,
M. Rafieiolhossaini  and
A. Mehnatkesh
Z. Mosleh
Affiliation:
Soil Science Dept., College of Agriculture, Shahrekord University, Shahrekord, Iran
M. H. Salehi*
Affiliation:
Soil Science Dept., College of Agriculture, Shahrekord University, Shahrekord, Iran
M. Rafieiolhossaini
Affiliation:
Department of Agronomy, College of Agriculture, Shahrekord University, Shahrekord, Iran
A. Mehnatkesh
Affiliation:
Shahrekord, Iran
*
*E-mail: [email protected]
Get access Rights & Permissions [Opens in a new window]

Abstract

This study examines the effect of German camomile (Matricaria camomilla L.) cultivation on the weathering of minerals present in the clay fraction of five different soil series modified or not unmodified (control) with cattle manure. A factorial experiment was performed in a randomized complete block design (RCBD) with three replications. At harvest time the rhizosphere soil was separated from bulk soil and the mineralogy was examined by X-ray diffraction (XRD). Trioctahedral chlorite transformed to hydroxy-interlayer vermiculite (HIV), while kaolinite disappeared. The presence of HIV was identified by an increase in the intensity ratio of the 1.0 and 1.4 nm peaks after Na-citrate pretreatment and K-saturation. It is suggested that Al3+ is released during dissolution of kaolinite and subsequently enters into the interlayer sheet of chlorite, and consequently the brucite layer disappears. This was verified by a significant Mg2+ increase in the soil solution in three out of five experiments at harvest time compared to pre-planting. The pots amended with manure showed the same changes as the pots without manure. The results of this study may explain the presence of unexpected clay minerals in regions with unsuitable conditions for their formation.

Keywords

German camomilehydroxy-interlayer vermiculiterhizosphereX-ray diffraction
Type
The 14th George Brown Lecture
Information
Clay Minerals , Volume 49 , Issue 1 , March 2014 , pp. 63 - 73
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2014

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Andrew, R.W., Jackson, M.L. & Wada, K. (1960) Intersalation as a technique for differentiation of kaolinite from chloritic minerals by X-ray diffraction. Soil Science Society of America Journal, 24, 422–424.Google Scholar
Baghernejad, M. (2000) Variation in soil clay minerals of semi-arid regions of Fars province in Southern Iran. Iran Agriculture Research, 19, 165–180.(in Persian, abstract in English).Google Scholar
Brindley, G.W. (1961) Kaolin and serpentine minerals. Pp. 51-131 in: The X-ray Identification and Crystal Structures of Clay Minerals (G. Brown, editor). Mineralogical Society, London.Google Scholar
Calveruso, C., Mareschal, L. & Turpault, M. (2009) Rapid clay weathering in the rhizosphere of Norway spruce and oak in an acid forest ecosystem. Soil Science Society of America Journal, 73, 331–338.Google Scholar
Carnicelli, S., Mirabella, A., Cecchini, G. & Sanesi, G. (1997) Weathering of chlorite to a low-charge expandable mineral in a spodosol on the Apennine Mountains, Italy. Clays and Clay Minerals, 45, 28–41.Google Scholar
Courchesne, F. & Gobran, G.R. (1997) Mineralogical variations of bulk and rhizosphere soils from a Norway spruce stand. Soil Science Society of America Journal, 61, 1245–1249.Google Scholar
Dixon, J.B. & Weed, S.B. (1989) Minerals in Soil Environments. American Society of Agronomy and the Soil Science Society of America, Madison, Wisconsin, USA.Google Scholar
Gransee, A. & Fuhrs, H. (2013) Magnesium mobility in soils as a challenge for soil and plant analysis, magnesium fertilization and root uptake under adverse growth conditions. Plant and Soil, 368, 5–21.Google Scholar
Hinsinger, P. & Jaillard, B. (1993) Root-induced release of interlayer potassium and vermiculitization of phlogopite as related to potassium depletion in the rhizosphere of ryegrass. Soil Science Society of America Journal, 44, 525–534.CrossRefGoogle Scholar
Hinsinger, P., Elsass, F., Jaillard, B. & Robert, M. (1993) Root-induced irreversible transformation of a tri - octahedral mica in rhizosphere of rape. Soil Science Society of America Journal, 44, 535–545.Google Scholar
Hosseinifard, J. (2010) Mineralogical and chemical transformations of selected K-bearing minerals in pistachio and wheat root zone. Ph.D. thesis, Isfahan University of Technology, Iran (in Persian, abstract in English).Google Scholar
Jordan, G. & Rammensee, W. (1996) Dissolution rates and activation energy for dissolution of brucite (001): a new method based on the micro-topography of crystal surfaces. Geochimica et Cosmochimica Acta, 60, 5055–5062.Google Scholar
Khademi, H. & Arocena, J.M. (2008) Kaolinite formation from palygorskite and sepiolite in rhizosphere soils. Clays and Clay Minerals, 56, 429–436.Google Scholar
Khademi, H. & Mermut, A. R. (1998) Source of palygorskite in gypsiferous Aridisols and associated sediments from central Iran. Clay Minerals, 33, 561–578.Google Scholar
Khayamim, F., Khademi, H. & Salehi, M.H. (2010) Mineralogical changes in clay-sized phlogopite and muscovite as affected by endophyte fungitall fescue symbiosis. Journal of Water and Soil, 24, 545–556.(in Persian, abstract in English).Google Scholar
Khormali, F. & Abtahi, A. (2003) Origin and distribution of clay minerals in calcareous arid and semi-arid soils of Fars Province. Clay Minerals, 38, 511–527.CrossRefGoogle Scholar
Kittrick, J.A. & Hope, E.W. (1963) A procedure for the particle size separation of soils for X-Ray diffraction analysis. Soil Science Society of America Journal, 96, 312–325.Google Scholar
Kodama, H., Nelsone, S., Yang, A. & Kohyama, N. (1994) Mineralogy of rhizospheric and non-rhizospheric soils in corn fields. Clays and Clay Minerals, 38, 755–763.Google Scholar
Lindsay, W.L. (1979) Chemical Equilibria in Soils, 442 pp. Wiley, New York.Google Scholar
Lucas, Y. (2001) The role of plants in controlling rates and products of weathering: importance of biological pumping. Annual Review of Earth and Planetary Science, 29, 135–163.CrossRefGoogle Scholar
Marschmer, H. (1995) Mineral Nutrition of Higher Plants, 889 pp. Academic Press, London.Google Scholar
Moor, D.M. & Reynolds, R.C. (1997) X-ray Diffraction and the Identification and Analysis of Clay Minerals, 378 pp. Oxford University Press, Oxford.Google Scholar
Mortland, M.M., Lawton, K. & Vehara, G. (1956) Alteration of biotite to vermiculite by plant growth. Soil Science, 82, 477–481.Google Scholar
Mosleh, Z., Salehi, M.H. & Rafieiolhossaini, M. (2013) Effect of different soil series and manure application on agro-morphological characteristics, essential oil and chamazulene content of German chamomile. Journal of Essential Oil Bearing Plants. 16, 730–739.Google Scholar
Naderizadeh, Z. & Khademi, H. (2011) Effect of organic matter on potassium uptake from di- and trioctahedral micas by alfalfa. Journal of Science and Technology Agriculture and Natural Resources, 56, 127–140.(in Persian, abstract in English).Google Scholar
Nagy, K.L. (1995) Dissolution and precipitation kinetic of sheet silicates. Pp.173-234 in: Chemical Weathering Rates of Silicate Minerals (A.F. White & S.L. Brantly, editors). Mineralogical Society of America. USA.Google Scholar
Owliaie, H.R., Heck, R.J. & Abtahi, A. (2006) Pedogenesis and clay mineralogical investigation of soils formed on gypsiferous and calcareous materials on a transect Southwestern Iran. Geoderma, 134, 62–81.Google Scholar
Pernes-Debuyser, A., Pernes, M., Velde, B. & Tessier, D. (2003) Soil mineralogy volition in the INRA 42 plots experiment (Versailles, France). Clays and Clay Minerals, 51, 577–584.Google Scholar
Rezaei, F. (2010) Transformation of minerals in the rhizosphere of soils with different mineralogy in the Golestane Province. M. Sc thesis, Gorgan University, Iran (in Persian, abstract in English).Google Scholar
Rich, C.I. (1968) Hydroxy interlayers in expansible layer silicates. Clays and Clay Minerals, 16, 15–30.Google Scholar
Ross, G.J., Hoyt, P.B. & Neilsen, G.R. (1985) Soil chemical and mineralogical changes due to acidification in Okahagen apple or chards. Soil Science Society of America Journal, 65, 347–355.Google Scholar
Rufyikiri, G., Nootens, D., Dufey, J.E. & Delvaux, B. (2004) Mobilization of aluminum and magnesium by roots of banana (Musa Spp.) from kaolinite and smectite clay minerals. Applied Geochemistry, 19, 633–643.Google Scholar
Salehi, M.H. & Tahamtani, L. (2012) Magnesium uptake and palygorskite transformation abilities of wheat and oat. Pedosphere, 22, 834–841.Google Scholar
Schaetzl, R. & Anderson, S. (2005) Soils Genesis and Geomorphology, 817 pp. Cambridge University Press, New York.Google Scholar
Soil Survey Staff. (2010) Soil Taxonomy: A basic systems of soil classification for making and interpreting soil surveys. Eleventh edition, NRCS, USDA.Google Scholar
Spyridakis, D.E., Chesters, G. & Wilde, S.A. (1967) Kaolinization of biotite as a result of coniferous and deciduous seeding growth. Soil Science Society of America Journal, 31, 205–210.Google Scholar
Tamura, T. (1958) Identification of clay minerals from acid soils. Soil Science Society of America Journal, 9,141–147.Google Scholar
Tributh, H., Boguslawski, E.V., Lieres, A.V., Steffens, D. & Mengel, K. (1987) Effect of potassium removal by crops on transformation of illitic clay minerals. Soil Science Society of America Journal, 143, 404–409.CrossRefGoogle Scholar
Ugolini, F.C. & Sletten, R.S. (1991) The role of proton donors in pedogenesis as revealed by soil solution studies. Soil Science Society of America Journal, 151, 51–75.Google Scholar
Wada, K. (1961) Lattice expansion of kaolin minerals by potassium acetate treatment. Clays and Clay Minerals, 46, 78–91.Google Scholar
Walter, R. (1965) Calcium and magnesium. Pp. 999-1009 in: Methods of Soil Analysis (C.A. Black, editor). American Society of Agronomy and the Soil Science Society of America, Madison, Wisconsin, USA.Google Scholar
Wilson, M.J. (1987) X-ray powder diffraction methods. Pp. 26-98 in: A Handbook of Determinative Methods in Clay Mineralogy (M.J. Wilson, editor). Blackie, Glasgow and London.Google Scholar