An Introduction to the Study of Mineralogy by C. Aydinalp

By C. Aydinalp

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C. , 2002. Turnover and storage of C and N in five density fractions from California annual grassland surface soils. Global Biogeochemical Cycles, 16: 1117-1132. A. , 2000. Role of the soil matrix and minerals in protecting natural organic materials against biological attack. Organic Geochemistry, 31: 697-710. I. M. 1989. Chlorites and hydroxy-interlayered vermiculite and smectite. B. B. 729-779. Soil Science Society of America, Madison, Wisconsin. S. , 1985. Laboratory Data and Description for Some Typical Pedons of California Soils.

1997. Mineral control of soil organic carbon storage and turnover. Nature, London, 389: 170-173. E. 1993. Comparison of carbon dynamics in tropical and temperate soils using radiocarbon measurements. Global Biogeochemical Cycles, 7: 275-290. E. & Zheng, S. 1996. Comparison of fractionation methods for soil organic matter 14C analysis. Radiocarbon, 38: 219-229. W. & Buurman, P. 2004. Mean residence time of kaolinite and smectite-bound organic matter in Mozambiquan soils. Soil Science Society of America Journal, 68: 154-161.

This site can be vacant, partially filled, or fully occupied by Na and/or K in C2/m structure. 40 An Introduction to the Study of Mineralogy The present work was undertaken to investigate the chemical characteristic of calcic and magnesian amphiboles from upper amphibolite to granulite facies rocks in the Sittampundi complex. In addition, main objective of this work is to characterize iron ions of different valence states and their distribution within the crystal lattice, both in calcic and magnesian amphiboles of amphibolite, meta-anorthosite and chromitite respectively, using 57Fe Mössbauer spectroscopy and estimate the equilibration temperature attained by the host rock.

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