Pedosphere 20(4): 409--418, 2010
ISSN 1002-0160/CN 32-1315/P
©2010 Soil Science Society of China
Published by Elsevier B.V. and Science Press
Characterization of placic horizons in ironstone soils of Louisiana, USA
D. C. WEINDORF1, N. BAKR1, Y. ZHU1, B. HAGGARD1, S. JOHNSON1 and J. DAIGLE2
1 Louisiana State University Agricultural Center, 307 MB Sturgis Hall, Baton Rouge, LA 70803 (USA);
2 United States Department of Agriculture-Natural Resources Conservation Service, 3737 Government Street, Alexandria, LA 71302 (USA)
ABSTRACT
      Placic horizons, defined as thin, wavy, hardened layers of iron and organic matter, are rare within the United States, occurring only in Washington, Alaska, and Hawaii. While ironstone is common in many soils of the southeastern United States, it is not known to contain appreciable organic matter. As a pilot study evaluating the justification for a larger study on ironstone in Louisiana, a 40 m lateral exposure with suspected placic horizons was evaluated in Vernon Parish, Louisiana. Results of laboratory analysis show elevated levels of iron and organic matter in the suspect horizons that meet the criteria of placic horizons as defined by the Soil Survey Staff. Based on the results of this study, additional evaluation of multiple pedons with similar features is warranted. Should additional pedons demonstrate similar properties, a new great group of ‘Petrudepts' would be needed to describe both the placic horizons in the pedon and the udic moisture regime in which they occur.
Key Words:  ortstein, pedon, petroferric contact, Petrudepts
Citation: Weindorf, D. C., Bakr, N., Zhu, Y., Haggard, B., Johnson, S. and Daigle, J. 2010. Characterization of placic horizons in ironstone soils of Louisiana, USA. Pedosphere. 20(4): 409-418.
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