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Date: | Wed, 6 Aug 2003 22:05:35 -0400 |
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Dr. Hailemichael
Soils of the Past: an introduction to paleopedology (G.J. Retallack)
contains a concise answer to your question. To summarize, in dry climates
carbonate in soil builds up from dust and leftover weathering products at
the rate of .26 g/cm2/yr (for cool desert regions-Las Cruces) to half that
in a wetter and cooler climate or twice the Las Cruces value in a wetter
an somewhat warmer climate (0.51-Roswell). Hope this helps, but again the
Retallack text is more detailed, as I’m sure other texts are as well.
Dave Mrofka
UC Riverside
Earth Sciences
-----Original Message-----
From: Stable Isotope Geochemistry [mailto:[log in to unmask]] On
Behalf Of Million Hailemichael
Sent: Wednesday, August 06, 2003 2:55 PM
To: [log in to unmask]
Subject: [ISOGEOCHEM] pedogenic carbonates in semiarid soil
Dear all
How long does it takes for a pedogenic carbonate to be formed. Not
neccesarly in the form of a nodule, but even in the form of fine powder in
semi arid environment. Hundreds of years? Or do we get pedogenic
carbonate in 20 or 30 years.
Thank you
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Million Hailemichael, Ph.D.
Senior Research Associate
Texas A&M University
Department of Rangeland Ecology and Management
Stable Isotope Laboratory
2126 TAMU
College Station, TX 77843-2126
Phone: (979)845-1497
Fax: (979)845-6430
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