The amount of reacting material in a sample investigated by differential thermal analysis can be determined from the peak area according to the Boersma equation, which accounts for heat flow through sample and thermocouple wires. This relation has been checked by experiment and it has been found that the use of different thermocouples for the calibrations may lead to variations of about 30%. The values obtained for heat transfer through a sample and thermocouple have been checked by comparison of computations and observation of base-line offset at the beginning of a run and exponential decay of the amount of heat dissipating out of a sample. It is shown that according to the equation it is not the total amount of reacting material that determines the peak area but merely the density of the material near the thermocouple. The sensitivity of the method for quantitative analysis is discussed in relation to the possible variations in the factors involved, namely, density and heat conductivity of the sample and heat transfer through the thermocouple.
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© 2006 Springer
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de Jong, G.D.J. (2006). Verification of the use of peak area for the quantitative differential thermal analysis. In: Schotting, R.J., van Duijn, H.C.J., Verruijt, A. (eds) Soil Mechanics and Transport in Porous Media. Theory and Applications of Transport in Porous Media, vol 19. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-3629-3_13
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DOI: https://doi.org/10.1007/978-1-4020-3629-3_13
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