HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS		QUICK SEARCH:   [advanced] Author: Keyword(s): Year:  Vol:  Page:

This Article Full Text (PDF) Alert me when this article is cited Alert me if a correction is posted Services Similar articles in this journal Alert me to new issues of the journal Download to citation manager Citing Articles Citing Articles via HighWire Citing Articles via Google Scholar Google Scholar Articles by Feng, Z.-D. Search for Related Content PubMed Articles by Feng, Z.-D. Agricola Articles by Feng, Z.-D.

Geochemical Characteristics of a Loess-Soil Sequence in Central Kansas

Department of Earth and Environmental Studies, Montclair State Univ., Upper Montclair, NJ 07043

*Corresponding author (fengzd{at}saturn.montclair.edu).

ABSTRACT

This study focuses on a Barton County loess-soil section in central Kansas in an attempt to retrieve the geochemical signature of the late Quaternary environmental change in the arid-semiarid region and provide a data base of loess geochemical characteristics in the Great Plains. The data indicate that the elements (expressed as oxides) of the windborne fraction (<63 µm) that are easily solubilized and lost from the soil by chemical weathering and leaching are relatively sensitive to soil-forming processes, whereas the insoluble elements of that fraction are controlled primarily by the chemical composition of the parent material. The geochemical imprint of pedogenesis superimposed on that of the loess parent material can be distinguished by comparing the magnetic susceptibility signature with the Fe₂O₃/Al₂O₃ ratio. Based on the geochemical imprint and radiometric dates (¹⁴C and thermoluminescence), the Bignell Loess (8000–5000 yr) is poorly weathered and the Brady Soil (10 000–8000 yr) is strongly weathered. The Peoria Loess (20 000–10 000 yr) has neither a traceable leaching nor weathering marker, and the Gilman Canyon pedocomplex (35 000–20 000 yr) is strongly leached. The reddish pedocomplex (70 000–35 000 yr) is the most strongly weathered, probably due to stable land surface conditions in a mild climate, and the Barton sand (92 000–70 000 yr) seems to have been subjected to a moderate weathering. Within the exposed portion of the Loveland Loess (260 000–92 000 yr), weathering indices are inversely correlated with the carbonate content and the carbonate-rich soils were developed under warm dry environments before 92 000, around 193 000, and before 260 000 yr. The data also show that the geochemical background of Fe₂O₃ and Al₂O₃ is high in two portions of the section: from the Brady Soil to the Gilman Canyon pedocomplex and from LL1 to LL2 within the Loveland Loess. The geochemical background of Fe₂O₃ and Al₂O₃ in the loess-soil sequence might have been dictated by that of eolian sources.

Received for publication July 31, 1995.

This article has been cited by other articles:

				Z.-D. Feng and H. B. Wang Pedostratigraphy and Carbonate Accumulation in the Last Interglacial Pedocomplex of the Chinese Loess Plateau Soil Sci. Soc. Am. J., June 2, 2005; 69(4): 1094 - 1101. [Abstract] [Full Text] [PDF]