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


     


This Article
Right arrow Figures Only
Right arrow Full Text Free
Right arrow Full Text (PDF) Free
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 Similar articles in Web of Science
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 Web of Science (3)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Allen, C. E.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Allen, C. E.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Allen, C. E.
Related Collections
Right arrow Soil Geomorphology and Geography
Right arrow Pedology
Right arrow Soil Chemistry
Published in Soil Sci. Soc. Am. J. 69:148-158 (2005).
© 2005 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA

Division S-5—Pedology

Physical and Chemical Characteristics of Soils Forming on Boulder Tops, Kärkevagge, Sweden

C. E. Allen*

222 San Lorenzo Blvd., Santa Cruz, CA 95060

* Corresponding author (callen{at}cruzio.com).

Recent pedologic studies in Kärkevagge, Swedish Lapland, have characterized soil distribution and confirmed the importance of chemical weathering in this arctic–alpine environment. However, these studies have overlooked soils that are forming on the uppermost surface of the boulders that give Kärkevagge its name, "Valley of the Boulders." The physical and chemical characteristics of the soils forming on boulder tops are therefore examined herein. Soil samples were collected from 20 large boulder tops and analyzed according to standard procedures. The boulder-top soils were weakly developed, <27-cm deep, coarse-textured, weak-structured, and well-drained. There was minimal horizonation. Physical characteristics of the boulder-top soils are comparable with the alpine soils in the region. Soil reactions were very acidic, with low base saturation and low cation exchange capacity (CEC). Chemical characteristics are similar to soils in the rest of the watershed, whereby extractable Ca > Mg > K > Na in the soils, albeit the values are substantially lower overall in the boulder-top soils than for the rest of the soils in Kärkevagge. Although the boulder-top soils were weakly developed, there was incipient pedogenesis as exemplified by the presence of pedogenic Fe. The boulder-top soils were classified as loamy-skeletal, micaceous, acid Lithic Cryorthents. Results illustrated that, like the rest of Kärkevagge, chemical weathering is an important contributing process in boulder-top soil formation, and that the boulder-tops provided a unique opportunity to evaluate incipient pedogenesis in an arctic–alpine setting.

Abbreviations: CEC, cation exchange capacity • subscript [d], dithionite-citrate-bicarbonate extractable • DCB, dithionite-citrate-bicarbonate • MSST, mean summer soil temperature • subscript [o], oxalate extractable




This article has been cited by other articles:


Home page
Soil Sci.Home page
H. A. Enloe, R. C. Graham, and S. C. Sillett
Arboreal Histosols in Old-Growth Redwood Forest Canopies, Northern California
Soil Sci. Soc. Am. J., February 2, 2006; 70(2): 408 - 418.
[Abstract] [Full Text] [PDF]




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 © 2005 by the Soil Science Society of America.