|
|
||||||||
ABSTRACT
The formation of fine clay horizons over limestone in the soils studied results from illuviation and is not residual material resulting from the dissolution of limestone. This conclusion is reached on the basis of 14C dating of the carbon complexed with the clay, X-ray diffractograms, and clay size.
1 Contribution from the Department of Agronomy, University of Illinois at Urbana-Champaign, 61801. Presented before Div. S-5, Soil Science Society of America, Detroit, Michigan, Nov. 12, 1969. The results are contained in a M. S. Thesis, University of Illinois Library, 1969.
2 Formerly Research Assistant, presently 2nd Lt. USAF; and Associate Professor of Soils, University of Illinois, respectively.
Received for publication December 5, 1969. Accepted for publication March 9, 1970.
| HOME | HELP | FEEDBACK | SUBSCRIPTIONS | ARCHIVE | SEARCH | TABLE OF CONTENTS |
| The SCI Journals | Agronomy Journal | Crop Science | |||
| Journal of Natural Resources and Life Sciences Education |
Vadose Zone Journal | ||||
| Journal of Plant Registrations | Journal of Environmental Quality |
The Plant Genome | |||