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Bisphosphonates do not alter the rate of secondary mineralization
Bone, 2011Bisphosphonates function to reduce bone turnover, which consequently increases the mean degree of tissue mineralization at an organ level. However, it is not clear if bisphosphonates alter the length of time required for an individual bone-modeling unit (BMU) to fully mineralize.
Robyn K, Fuchs +5 more
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Quantitative analysis on the rate of secondary bone mineralization
Calcified Tissue Research, 1972The microradiographic-photometric method of studying the X-ray absorption, and the microhardness testing technique were concurrently applied to investigate the rate of secondary mineralization of bone of known age in the osteons of young immature and adult dogs.
G, Marotti, A, Favia, A Z, Zallone
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Mineralization and Decomposition Rates in Restored Pine Fens
Restoration Ecology, 2012AbstractGrowing public interest in conserving peatlands has created a need for restoration and rapid indicators of progress in peat formation. Vegetation and hydrological indicators are commonly assessed, but changes in mineralization and decomposition rates might better indicate when peat formation is underway in restored peatlands.
Tarvainen, O. +3 more
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RATE OF CRYSTALLIZATION OF MINERALS
International Geology Review, 1961Determination of the growth rate of crystals may be based on knowledge of the linear rate, the volume rate, and duration of crystallization. Direct measurements are possible where crystals are in process of growth as in the laboratory, saline waters, and at volcanic gaseous exhalations.
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1986
The nature and extent of interaction between a metamorphic rock and externally derived fluid depend on a number of physical and chemical variables. The compositions of rock and fluid and the initial degree of disequilibrium between them is obviously of prime importance.
J. V. Walther, B. J. Wood
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The nature and extent of interaction between a metamorphic rock and externally derived fluid depend on a number of physical and chemical variables. The compositions of rock and fluid and the initial degree of disequilibrium between them is obviously of prime importance.
J. V. Walther, B. J. Wood
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On the temperature dependence of mineral dissolution rates
Geochimica et Cosmochimica Acta, 1992Experimental activation energies (Eexp) for the dissolution rates of silicate and oxide minerals far from equilibrium vary by tens of kJ/mol with pH. Measured Eexprange from larger than 50 kJ/mol at pH conditions much more acidic or more basic than at the Point of Zero Net Proton Charge (PZNPC) to very small values near, but not necessarily at, the ...
William H Casey, Garrison Sposito
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Sulfur mineralization rates and potentials of soils
Biology and Fertility of Soils, 1988Field-moist soil and glass beads mixtures were packed in glass tubes and leached with 100 ml of 5 mM CaCl2 and incubated at 20 or 30°C. The leaching procedure was repeated every 2 weeks for 14 weeks. The leachates were analysed for SO inf4 sup2− and NO3 −. The S uptake by three successive croppings of
H.J. Pirela, M.A. Tabatabai
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Natural Weathering Rates of Silicate Minerals
2014This chapter presents (1) the development of rates that quantitatively describe silicate mineral and rock weathering, (2) a summary of the available literature rate data for the weathering of several common silicate minerals, and (3) a discussion of the chemical, physical, and hydrologic processes that control silicate mineral weathering at the Earth's
White, Arthur F, Buss, Heather L
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Rates of Nutrient Release by Mineral Weathering
1990Acidic deposition is capable of altering the geochemistry of several elements important to forest productivity (Reuss and Johnson 1986). Long-term effects of acidic deposition may include accelerated depletion of base cations and increased concentrations of aluminum in soil solutions.
G. Norman White +2 more
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Rate of radial bone mineral accretion in healthy children
Acta Paediatrica, 1995Radial bone width and mineral content were measured in 392 healthy Cambridge children aged 6–12 years from a cohort of 420 children studied 2 years previously. The typical rate of bone mineral accretion was 0.044 g/cm/year for boys across the whole age range and 0.042 g/cm/year for girls up to a mean age of 9 years, rising rapidly thereafter in ...
W R, Goslings +3 more
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