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EN
TG-DTG-DSC, FTIR, DRIFT, and Py-GC-MS studies have been conducted to determine the effect of the thermal decomposition conditions and structure of foundry binder BioCo3 in the form of a composition poly(sodium acrylate)/dextrin (PAANa/D) on the progress of degradation in terms of processes occurring in foundry sands in contact with liquid metal. TG-DTG-DSC curves of the composition allowed us to determine the temperature range in which they do not undergo degradation, by which they do not lose their binding properties. With temperature increasing, physical and chemical changes occur that are related to the evaporation of solvent water (20–110°C), followed by the release of constitution water, and finally intermolecular dehydration (110–230°C). In this temperature range, processes that are mainly reversible take place. Within a temperature range of 450–826°C, polymer chains are decomposed, including the decomposition of side chains. Within a temperature range of 399–663°C, polymer composition decomposition can be observed (FTIR, DRIFT), and gas products are generated from this destruction (Py-GC-MS).
EN
The paper presents some problems in the studies on Baltic amber (succinite) and other fossil resins. Natural resins form a large group of fossils already known from various parts of the world. However, they markedly differ in age and origin which creates problems in their systematic nomenclature. At the beginning of this paper some definitions are presented concerning the scientific nomenclature of fossil resins as well as practical terminology. The fossil resins are the objects of interest of many scientific domains, especially as they are used for many purposes. The resins are investigated by scientists representing various natural sciences as well as archeologists and representatives of other disciplines; and in the aspect of application they are widely used in jewelry making as well as in some branches of industry (e.g. chemical and pharmaceutical). Variability of fossil resins along with complexity of their structure and composition, and broad issues of genesis and various historical aspects form a vast field of for further studies. However, the studies require the use of a multilateral approach, including instrumental analysis. The paper presents several examples of selected physicochemical methods which should be highly useful in solving questions concerning origin and composition as well as properties of fossil resins.
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