HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS		QUICK SEARCH:   [advanced] Author: Keyword(s): Year:  Vol:  Page:

This Article Abstract Full Text Free Full Text (PDF) Free Alert me when this article is cited Alert me if a correction is posted Services Similar articles in this journal Alert me to new issues of the journal Download to citation manager Citing Articles Citing Articles via Google Scholar Google Scholar Articles by Bockheim, J. G. Articles by Hinkel, K. M. Search for Related Content PubMed Articles by Bockheim, J. G. Articles by Hinkel, K. M. GeoRef GeoRef Citation Agricola Articles by Bockheim, J. G. Articles by Hinkel, K. M. Related Collections Carbon Sequestration Hillslope Analysis Frozen Soils

The Importance of "Deep" Organic Carbon in Permafrost-Affected Soils of Arctic Alaska

^a Dep. of Soil Science, Univ. of Wisconsin, Madison, WI 53706-1299
^b Dep. of Geography, Univ. of Cincinnati, Cincinnati, OH 45221-0131

View larger version (174K): [in this window] [in a new window]   Fig. 1. Soil organic C concentrated in near-surface permafrost of a drained thaw-lake basin, northern Alaska. The top of the permafrost, which includes the organic-enriched layer, occurs at the top of the shovel blade (note the segregated ice below the organic-enriched layer).