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The role of earthworm communities in soil mineral weathering: a field experiment

Published online by Cambridge University Press:  05 July 2018

D. Carpenter ,
M. E. Hodson ,
P. Eggleton  and
C. Kirk
D. Carpenter*
Affiliation:
Department of Soil Science, University of Reading, Whiteknights, Reading RG6 6DW, UK
M. E. Hodson
Affiliation:
Department of Entomology, Natural History Museum, Cromwell Road, London SW7 5BD, UK
P. Eggleton
Affiliation:
Department of Entomology, Natural History Museum, Cromwell Road, London SW7 5BD, UK
C. Kirk
Affiliation:
Chemistry Department, Loughborough University, Loughborough, Leicestershire LE11 3TU, UK
*
*E-mail: [email protected]
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Extract

Minerals are an important component of the soil environment (Dixon et al., 1977). They provide a structural framework which supports plants and contribute to the physical heterogeneity of soil. Minerals also contribute to the fertility of soils. Primary minerals are a source of essential plant nutrients (Harley and Gilkes, 2000). Clay minerals impact on the water-holding capacity of soils, affect the cation exchange capacity of soils (Brown, 1977) and are able to sequester nutrients and contaminants within the soil (Dubbin, 2001).

Type
Research Article
Information
Mineralogical Magazine , Volume 72 , Issue 1 , February 2008 , pp. 33 - 36
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2008

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References

Brown, K.W. (1977) Shrinking and swelling of clay, clay strength, and other properties of clay soils and clays. In: Minerals in Soil Environment. (Dixon, J. et al., editors). Soil Science Society of America, Madison, Wisconsin, USA.Google Scholar
Carpenter, D., Hodson, M.E., Eggleton, P. and Kirk, C. (2007) Earthworm induced mineral weathering: Preliminary results. European Journal of Soil CrossRefGoogle Scholar
Dixon, J.B., Dinauer, R.C. and Weed, S.B. (editors) (1977) Minerals in Soil Environments. Soil Science Society of America, Madison Wisconsin, USA.Google Scholar
Dubbin, W. (2001) Soils. The Natural History Museum, London.Google Scholar
Gunn, A. (1992) The use of mustard to estimate earthworm populations. Pedobiologia, 36, 65–67.Google Scholar
Harley, A.D. and Gilkes, RJ. (2000) Factors influencing the release of plant nutrient elements from silicate rock powders: a geochemical overview. Nutrient Cycling in Agroecosystems, 56, 11—36 CrossRefGoogle Scholar
RJ., Haynes and Fraser, P.M. (1998) A comparison of aggregate stability and biological activity in earthworm casts and undigested soil as affected by amendment with wheat or lucerne straw. European Journal of Soil Science, 49, 629–636.Google Scholar
Lamande, M., Hallaire, V., Curmi, P., Peres, G. and Cluzeau, D. (2003) Changes in pore morphology, infiltration and earthworm community in a loamy soil under different agricultural managements. Catena, 54, 637–649.CrossRefGoogle Scholar
Lavelle, P., Bignell, D., Lepage, M., Wolters, V., Roger, P., Ineson, P., Heal, O.W. and Dhillion, S. (1997) Soil function in a changing world: the role of invertebrate ecosystem engineers. European Journal of Soil Biology, 33(4), 159–193.Google Scholar
Lawes Agricultural Trust (2006) Gensta© . version 9. VSN International, Hemel HempsteadGoogle Scholar
Marhan, S. and Scheu, S. (2006) Mixing of different mineral soil layers by endogeic earthworms affects carbon and nitrogen mineralization. Biology and Fertility of Soils, 42, 308–314.CrossRefGoogle Scholar
Mclnerney, M. and Bolger, T. (2000) Decomposition of Quercus petraea litter: influence of burial, comminution and earthworms. Soil Biology and Biochemistry, 32, 1989–2000.Google Scholar
Needham, S.J., Worden, R.H. and Mcllroy, D. (2004) Animal-sediment interactions: the effect of ingestion and excretion by worms on mineralogy. Biogeosciences, 113–121.CrossRefGoogle Scholar
Rowell, D.L. (1999) Soil Science: Methods and Applications. Prentice Hall, Harlow, Essex, UK.Google Scholar
Schofield, P.F., Knight, K.S, Covey-Crump, S.J., Cressey, G. and Stretton, I.C. (2002) Accurate quantification of the modal mineralogy of rocks when image analysis is difficult. Mineralogical Magazine, 66, 173–184.CrossRefGoogle Scholar
Soil Survey and Land Research Centre (SSLRC) (1989) The Soils of Boxworth Experimental Husbandry Farm, Cambridgeshire. Soil Survey and Land Research Centre, Cranfield, UK.Google Scholar
Stoe, and Cie, (1999) STOE WinXPO. (Version 1.06). Stoe and Cie GmbH, Darmstadt, Germany.Google Scholar
Suzuki, Y., Matsubara, T. and Hoshino, M. (2003) Breakdown of minerals grains by earthworms and beetle larvae. Geoderma, 112, 131–142.CrossRefGoogle Scholar
ter Braak, CJ.F. and Smilauer, P. (2002) CANOCO Reference Manual and CanoDraw for Windows User's Guide. Software for Canonical Community Ordination (version 4.5). Microcomputer Power, Ithaca New York, USA, 500 pp.Google Scholar