SSSAJ Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in Soil Sci Soc Am J 39:1125-1132 (1975)
© 1975 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Rutledge, E. M.
Right arrow Articles by Wilding, L. P.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Rutledge, E. M.
Right arrow Articles by Wilding, L. P.
Agricola
Right arrow Articles by Rutledge, E. M.
Right arrow Articles by Wilding, L. P.

Loess in Ohio in Relation to Several Possible Source Areas: I. Physical and Chemical Properties1

E. M. Rutledge, N. Holowaychuk, G. F. Hall and L. P. Wilding2

ABSTRACT

Thin loess deposits east of the Little Miami, Scioto, and Muskingum rivers in Ohio were investigated (i) to test the hypothesis that these river valleys were source areas for the loess that adjoins them, (ii) to determine if multiple loess strata occurred within any of the loess deposits, and (iii) to approximate, where possible, the geologic age of the loess. The loessial materials were investigated using morphological, chemical, and physical parameters. Particle-size data were expressed on a fine earth and clay-free basis. The fine earth basis was useful in detecting pedogenic development. Clay-free data were used in establishing changes in parent material with depth and, perhaps more importantly, in development of relations between particle-size and distance from proposed source areas.

Scioto and Muskingum river valleys were the chief source areas for the loess in the adjoining study areas, but the Little Miami Valley was not the primary source of the loess in the study area adjacent to it. Multiple loess deposits were identified only adjacent to the Muskingum River. All upper loess units were considered to be of comparable age; Late Wisconsin (Peoria Loess). The middle loess adjacent to the Muskingum River was considered to be Farmdale (Roxanna Silt) and the lower loess at the same site was considered to be Loveland loess (Loveland Silt) and contained a well-developed Sangamon paleosol.


NOTES

1 Contribution of the Agronomy Department, Ohio Agric. Res. & Development Center, State Project 106, Journal Paper no. 110-74. Part of a thesis submitted by the senior author in partial fulfillment of the requirements of the Ph.D. degree at The Ohio State Univ. Presented before Div. S-5, Soil Sci. Soc. Am., New Orleans, La., 14 Nov. 1968.

2 Formerly Assistant in Agronomy, the Ohio State Univ., presently Associate Professor of Agronomy, Univ. of Arkansas, Fayetteville 72701; and Professor of Agronomy, Associate Professor of Agronomy, and Professor of Agronomy, The Ohio State Univ., respectively.

Received for publication October 22, 1974. Accepted for publication July 18, 1975.







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
Copyright © 1975 by the Soil Science Society of America.