Grundämnessammansättning i lössjordar på norra halvklotet

The content of atmospheric dust in ice cores from Greenland varies with changes in climate, but the exact relationship is yet unknown. To determine this correlation, the source of the Greenland dust must be known. There are several hypotheses on the location of the source, but no current methods hav...

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Bibliographic Details
Main Author: Oskar, Anna
Format: Bachelor Thesis
Language:Swedish
Published: Uppsala universitet, Institutionen för geovetenskaper 2017
Subjects:
Online Access:http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-324438
Description
Summary:The content of atmospheric dust in ice cores from Greenland varies with changes in climate, but the exact relationship is yet unknown. To determine this correlation, the source of the Greenland dust must be known. There are several hypotheses on the location of the source, but no current methods have been sufficient in determining the exact origin. This study explores the possibility of using elemental geochemical composition as an indicator for the dust origin. Major and trace element concentrations in loess and red clay samples from loess areas in Northern America, Europe, the Middle East, Central Asia and China were determined using handheld XRF. UCC-normalised values of major elements show similar trends for all areas, with depletion of Si, Al, Mg, K, Ti, Fe and Mn and enrichment of Ca and P in most samples. The elemental ratios Fe/Ti, Al2O3/SiO2, Al2O3/Ti, Fe/Al2O3, K2O/Al2O3, CaO/Al2O3, Rb/Sr and Zr/Rb display variations between areas, indicative of differences in weathering rates and grain sizes. The combined ratios Fe/Ti vs. K2O/Al2O3, Fe/Al2O3 or Al2O3/Ti can be used to differentiate loess from Canada, the US, central and eastern Europe, Israel and China. Central Asian loess however shows similar composition to Chinese loess. The results indicate that loess from different parts of the world have significant differences in elemental composition, which could potentially be used to differentiate between suggested sources of the Greenland dust. Mängden stoft i isborrkärnor från Grönland varierar med förändringar i klimat, men det exakta sambandet är ännu okänt. För att kunna rekonstruera detta samband krävs att källan till stoftet är känd. Flera hypoteser finns idag kring denna källa, men inga hittills prövade metoder har kunnat urskilja ett definitivt ursprung. I detta arbete undersöks möjligheten att använda grundämnessammansättning som en indikator för stoftets ursprung. Koncentrationer av huvudelement och spårämnen i löss och röd lera från lössområden i Nordamerika, Europa, Mellanöstern, Centralasien ...