Authors:L’. Fortunová, M. Reháková, S. Nagyová, S. Dolinská, S. C. Mojumdar, and E. Jóna
Thermalanalyses TG, DTA and DTG were carried out at temperature up to 800 °C in air on a NETZSCH STA 409 PC/PG under the conditions: sample weight 25 mg, heating rate 10 °C min −1 , and Al 2 O 3 crucible.
Authors:Sara Goñi, Francisca Puertas, María Soledad Hernández, Marta Palacios, Ana Guerrero, Jorge S. Dolado, Bruno Zanga, and Fulvio Baroni
furnace slag [ 32 ] and for quantitative determination of the chemical composition of the C–S–H gel and degree of hydration, which is the main aim of this study.
In this article, a quantitative method, based on thermalanalyses, has been used for
An attempt to prepare directly the title uranate by precipitation from uranyl solutions was successful if the preparation temperature was close to 100°C. The product was chemically and thermally analyzed, its IR spectra and X-ray patterns were taken; these results are commented and a reason for explanation of the molecular water behaviour is proposed.
Authors:M. Rusu, D. Rusu, C. Roşu, C. Crăciun, L. David, A.R. Tomşa, and Gh. Marcu
A new uranium tungstoborate heteropolyanion K12[U(BW11O39H)2]·23 H2O has been prepared and investigated by thermal analyses, IR, UV-Vis spectroscopy and magnetic susceptibility measurements. The compound obtained from Keggin monolacunary anions is 1:2 sandwich-type and exhibits a square antiprismatic stereochemistry for uranium (IV) ion.
Iron: fullerides were prepared by chemical methodes in the solution using nitric acid as activation agent. Experimental results
of thermal analyses, X-ray diffraction and Mössbauer spectroscopy of the products are presented. To interpret these results,
standard quantum chemistry calculations were used to determine the geometry and charge distribution in Fe:C60 complexes, which might be formed in the reaction.
In the previous study, it was observed that the stability of nitrocellulose (NC) cannot be determined by thermal analyses
such as differential scanning calorimetry (DSC) at heating rates of 1–10 K/min. This was because the thermal curves of NC
samples with different stabilities could not be distinguished from one another. In this study, we explain why such thermal
analyses cannot be used to evaluate the thermal stability of NC and identify the conditions under which thermal analyses can
be used for this purpose. We investigated the effect of heating rate on the thermal behavior of pure NC and NC stabilized
with diphenylamine (DPA) or akarditeII (AKII), which is a conventional stabilizer, by using the heat flux calorimeter (C80).
At high heating rates (0.2–0.3 K/min), only single exothermic peak was observed in the thermal curves of both pure NC and
NC/DPA and the thermal curve of pure NC was practically similar to that of NC/DPA. At low heating rate (0.02 K/min), two exothermic
peaks were observed for both pure NC and NC/DPA. The heat amount of the first peak depended on the partial pressure of O2 in the atmosphere. The first peak in the thermal curve of NC/DPA was slightly suppressed as compared to that of pure NC.
These results indicate that the stability of NC probably depends on the first exothermic peak that represents oxidation of
NC by atmospheric O2. From this, on the thermal analyses at high heating rates, thermal curves of pure NC and NC/DPA could not be distinguished
from one another. This is because the decomposition of NC itself occurs in the second exothermic peak before the oxidation
of NC by atmospheric O2 in the first peak, which is attributed to the stability of NC. The results of the thermal analyses under isothermal conditions
at 393 K in an O2 atmosphere revealed that the induction period of NC/DPA and NC/AKII was longer than that of pure NC. From these results,
it is speculated that the stability of NC can be evaluated by thermal analyses carried out under O2-rich conditions at low heating rates.
In this study, combustion curves of twenty-five original and demineralized Turkish lignite samples were obtained through use of a differential thermal analyser. The lignite samples were demineralized by treatment with hydrochloric and hydrofluoric acids. Samples of 20 mg were heated up to 1074 K at a constant rate of 10 K min−1 in a 40 cm3 min−1 flow of dry air. The rates of heat release from the original and demineralized samples were compared and are discussed.
Authors:S. Cebulak, A. Gawęda, and A. Langier-Kużniarowa
This paper presents the results of oxyreactive thermal analyses of organic matter in rocks, heated naturally during diagenetic
to metamorphic processes. During the experiments we traced the reactions in the temperature range up to 900C, it means from
the very beginning of diagenetic transformations to the highest real temperatures acting in the Earth's crust as a solid phase.
The results showed that TA could be a tool for the reconstruction of thermal regime in natural coal-bearing systems.
Authors:Sonia Degeratu, P. Rotaru, Gh. Manolea, H. Manolea, and A. Rotaru
For two typical actuators of intelligent systems (Ni–Ti SMA cantilever and SMA helical spring), the evaluation of their thermal
characteristics is presented. In order to determine the transformation temperatures and other thermal parameters of the two
studied elements, the attention was concentrated on thermal analysis experiments. For each actuator configuration, comprehensive
graphical interfaces have been developed, to run in Visual Basic, with respect to the results of performed thermal analyses.