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Zmiany właściwości konsolidacyjnych, filtracyjnych i mikrostrukturalnych glin lodowcowych w przebiegu badań konsolidacji z ciągłym wzrostem obciążenia

Stajszczak Piotr, Dobak Paweł, Gendek Katarzyna

Przegląd Geologiczny

2020

Vol. 68, nr 11

843--852

The article presents results of CRL (Constant Rate of Loading) tests obtained for glacial till from the Warsaw region (Fort Służew). The analyses show that the significantfactors affecting the course of the consolidation with continuous loading (CL) of tested soils are related to the degree of water saturation of pore space, the state of soil structure, and the rate of loading. Values of filtration and consolidation parameters documented during CRL tests are dependent on the structural history and properties of soils. Before and after CRL tests, microstructure of till was studied by SEM methods. Changes in the pore space parameters in matrix microstructure, evaluated from CRL tests, are marked in different consolidation behaviours of tested natural and remould till.

Zastosowanie ziemskich izotopów kosmogenicznych w datowaniu glin lodowcowych : potencjał, ograniczenia i perspektywy badawcze

Tylmann Karol, Moskalewicz Damian

Przegląd Geologiczny

2020

Vol. 68, nr 10

764--773

Determination of numerical age for glacial till is one of the most intriguing issues in glacial geology and geomorphology. Till layers are unequivocal evidence of ice sheets advances and retreats, and therefore they are very important for Quaternary palaeoclimatic reconstructions. Herein, we present a review dedicated to the methodology of glacial till dating with in situ cosmogenic nuclides. This relatively novel approach enables direct dating of deposition of till and its exposure after deglaciation. Getting reliable numerical age (in years) of till opens a new prospect for reconstructions of past glaciations and palaeogeographic studies. Despite some limitations of applying in situ cosmogenic exposure and burial dating, we argue that this technique may be successfully employed in studies of glacial deposits in Poland.