Articles | Volume 9, issue 12
Biogeosciences, 9, 5181–5197, 2012
Biogeosciences, 9, 5181–5197, 2012

Research article 17 Dec 2012

Research article | 17 Dec 2012

Density fractions versus size separates: does physical fractionation isolate functional soil compartments?

C. Moni et al.

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Cited articles

Amelung, W., Bol, R., and Friedrich, C.: Natural C-13 abundance: A tool to trace the incorporation of dung-derived carbon into soil particle-size fractions. Rapid Commun. Mass. Sp., 13, 1291–1294, 1999.
Arnarson, T. S. and Keil, R. G.: Organic-mineral interactions in marine sediments studied using density fractionation and X-ray photoelectron spectroscopy. Org. Geochem., 32, 1401–1415, 2001.
Baisden, W. T., Amundson, R., Cook, A. C., and Brenner, D. L.: Turnover and storage of C and N in five density fractions from California annual grassland surface soils, Global Biogeochem. Cy., 16, 1117,, 2002.
Balabane, M. and Plante, A. F.: Aggregation and carbon storage in silty soil using physical fractionation techniques, Eur. J. Soil Sci., 55, 415–427, 2004.
Balesdent, J.: The significance of organic separates to carbon dynamics and its modelling in some cultivated soils, Eur. J. Soil Sci., 47, 485–493, 1996.
Final-revised paper