Pregled bibliografske jedinice broj: 534022
Characterization of expandable clay minerals in lake Baikal sediments by thermal dehydration and cation exchange
Characterization of expandable clay minerals in lake Baikal sediments by thermal dehydration and cation exchange // Clays and clay minerals, 53 (2005), 4; 389-400 doi:10.1346/CCMN.2005.0530407 (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 534022 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Characterization of expandable clay minerals in lake Baikal sediments by thermal dehydration and cation exchange
Autori
Grygar, Tomas ; Bezdicka, Petr ; Hradil, David ; Hruškova, Michaela ; Novotna, Katerina ; Kadlec, Jaroslav ; Pruner, Petr ; Oberhansli, Hedi
Izvornik
Clays and clay minerals (0009-8604) 53
(2005), 4;
389-400
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
cation exchange capacity; Lake Baikal; lake sediments; Paleoclimate; Russia; thermal dehydration; XRD
Sažetak
The sedimentary series from Academician Ridge, Lake Baikal, eastern Siberia, was examined using cation exchange capacity (CEC) to estimate the amount of expandable clay minerals (ECM) and high-temperature X-ray diffraction (HT-XRD) to determine their basic classification. The comparison of the magnetic susceptibility (MS) at sub-millennial resolution and the 18O record of a reference Atlantic core (ODP 980) was used to create an age model. The most closely studied part of the series covered the major part of the last glacial cycle (120–20 ky BP). The HT-XRD analysis is based on monitoring the course of ECM dehydration with 5°C steps between 25 and 250°C and enabled us to improve the discrimination between ECM, chlorite and micas. The CEC obtained at millennial resolution showed that the neoformation of ECM in warmer periods of the last interglacial was either insignificant or fully compensated by their dissolution or dilution. The CEC record was correlated with the main climatic stages in the period studied. Both MS and CEC records reflected the environmental changes at about millennial resolution, including climatic instabilities between 117 and 73 ky BP (late MIS5).
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Citiraj ovu publikaciju:
Časopis indeksira:
- Current Contents Connect (CCC)
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus