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 47:715-721 (1983)
© 1983 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 HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Alexander, E. B.
Right arrow Articles by Holowaychuk, N.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Alexander, E. B.
Right arrow Articles by Holowaychuk, N.
Agricola
Right arrow Articles by Alexander, E. B.
Right arrow Articles by Holowaychuk, N.

Soils on Terraces Along the Cauca River, Colombia: I. Chronosequence Characteristics1

E. B. Alexander and N. Holowaychuk2

ABSTRACT

Soils on two floodplain and six terrace levels, developing under lowland tropical evergreen or semideciduous forest before recent deforestation, were studied to determine the properties found to vary most with relative age. They are in a sequence from a Typic Tropaquent and an Aeric Tropaquept on the two floodplain levels through Haplustults and Paleustults to a Tropeptic Haplustox on the highest terrace. The soil properties may be placed into three categories based on their variations with relative soil age. (i) Soil properties which are similar in all of the terrace soils are bulk density, clay content in the B horizons, 15 bar water retention, organic C content, and dithionite-citrate-extractable Fe. Differences in soil morphology are small, other than the relative thinness of the solum in the soil on the lowest terrace, an anomalous (with respect to age) hardpan in the soil on the next terrace, and slightly higher chroma in the soils on the two highest terraces. (ii) The proportions of different exchangeable cations exhibit age trends in the younger (lower) terrace soils but are either similar in the older (higher) terrace soils or so erratic that an age trend is not apparent. (iii) Except for properties of the clay fractions, only the extractable Fe ratio (Feo/Fed) was found to vary systematically through the entire sequence of terrace soils. It decreases from slightly > 0.4 in the lower floodplain soil to < 0.01 in the lower solum of the oldest soil.


NOTES

1 Contribution from the Agronomy Dep., Ohio State University, based on a Ph.D. Dissertation entitled "A Chronosequence of Soils on Terraces along the Cauca River, Colombia", 1970. Approved for publication as Jour. Art. 21–82 of the Ohio Agricultural Research and Development Center, Wooster, OH 44691. Copies of the Ph.D. Dissertation are available from University Microfilms (order no. 70-19, 288), Ann Arbor, Mich.

2 Soil Scientist, U.S. Forest Service, 630 Sansome Street, San Francisco, CA 94111, and Professor Emeritus, Dep. of Agron., Ohio State Univ., Columbus.

Received for publication February 12, 1982. Accepted for publication February 25, 1983.




This article has been cited by other articles:


Home page
Bulletin of the Seismological Society of AmericaHome page
Multiple Large Earthquakes in the Past 1500 Years on a Fault in Metropolitan Manila, the Philippines
Bulletin of the Seismological Society of America, February 1, 2000; 90(1): 73 - 85.





HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Vadose Zone Journal Journal of Plant Registrations
Journal of Natural Resources
and Life Sciences Education
Journal of
Environmental Quality
Copyright © 1983 by the Soil Science Society of America.