Impact of Climate and Parent Material on Chemical Weathering in Loess-derived Soils of the Mississippi River Valley
Author:
Affiliation:
1. U.S. Geological Survey; MS 980, Box 25046, Federal Center Denver CO 80225
2. Dep. of Geoscience; 121 Trowbridge Hall, The Univ. of Iowa Iowa City IA 52242
3. U.S. Geological Survey, MS 955; National Center; Reston VA 20192
Publisher
Wiley
Subject
Soil Science
Link
http://onlinelibrary.wiley.com/wol1/doi/10.2136/sssaj2001.1761/fullpdf
Reference51 articles.
1. Late Quaternary loess in northeastern Colorado: Part II-Pb isotopic evidence for the variability of loess sources;Aleinikoff;Geol. Soc. Am. Bull.,1999
2. Climate, organic matter and clay content relationships in the Pampa and Chaco soils, Argentina;Alvarez;Geoderma,1998
3. Holocene paleoenvironments of northeast Iowa;Baker;Ecol. Monog.,1996
4. CaO-ZrO2 molar ratios as an index of weathering;Beavers;Soil Sci. Soc. Am. Proc.,1963
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