作者: Cristian Necula , Cristian Panaiotu , Gabriel Schinteie , Petru Palade , Victor Kuncser
DOI: 10.1016/J.GLOPLACHA.2015.05.009
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摘要: Abstract Previous studies have shown that the magnetic parameters of Romanian loess/paleosol sequences recorded Quaternary glacial/interglacial cycles over last 600 kyr. rock investigations pointed out enhancement in loess is mainly due to pedogenic magnetite close superparamagnetic/stable single domain boundary. We report first reconstruction grain size distribution (GSD) superparamagnetic (SP) particles for two deposits, Costinesti and Mircea Vodă, located Dobrogea Plateau between Danube River Black Sea. The GSDs were obtained using both wide-band frequency spectrum susceptibility (FSMS) method low temperature Mossbauer spectroscopy. FSMS shows SP are present paleosols. shifted slightly higher diameters with respect concentration has an opposite trend. largest value reached forest paleosol lowest samples. Both paleosols indicated almost same dominant (about 17 nm 18 nm samples). However GSD shapes different than those found In paleosols, shape seems be independent climate degree pedogenesis. These factors control only each paleosol. Temperature dependent spectroscopy also supports presence a mean diameter around 13–14 nm. Dispersion case varies from sample being probably affected by random surface defects.