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

This Article Figures Only 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 Similar articles in ISI Web of Science Alert me to new issues of the journal Download to citation manager Citing Articles Citing Articles via HighWire Citing Articles via ISI Web of Science (2) Citing Articles via Google Scholar Google Scholar Articles by Bockheim, J. G. Articles by Nelson, F. E. Search for Related Content PubMed Articles by Bockheim, J. G. Articles by Nelson, F. E. GeoRef GeoRef Citation Agricola Articles by Bockheim, J. G. Articles by Nelson, F. E. Related Collections Carbon Sequestration Frozen Soils Soil Organic Matter

DIVISION S-10—WETLAND SOILS

Predicting Carbon Storage in Tundra Soils of Arctic Alaska

^a Dep. of Soil Science, Univ. of Wisconsin, 1525 Observatory Dr., Madison, WI 53706-1299
^b Dep. of Geography, Univ. of Cincinnati, Cincinnati, OH 45221
^c Dep. of Geography, Univ. of Delaware, Newark, DE 19716

^* Corresponding author (bockheim{at}facstaff.wisc.edu)

The distribution of soil organic carbon (SOC) was determined in 60 pedons from northern Alaska by horizon, within the seasonal thaw layer, and to a depth of 1 m. Concentration of SOC, bulk density, and SOC density were remarkably uniform for a given genetic horizon and had low standard errors. With increasing degree of decomposition, the bulk density increased, the concentration of SOC decreased, and the soil horizon C density increased in organic horizons. For mineral horizons, gleying is accompanied by an increase in C density, which is due to the effect of saturation on limiting decomposition of organic matter. Cryoturbation of organic or mineral minerals into the subsoil results in an increase in C density primarily from an increase in bulk density because of compaction from the overlying layers and more closely packed soil particles from frost churning. Estimated SOC storage for individual horizons and for the seasonal thaw layer were highly correlated (p < 0.01) with measured values from an independent data set for the same region published by other investigators. Equations relating C density to percentage of visible ice enable prediction of SOC in the near-surface permafrost. The equations generated by this study will be useful in preparing a detailed soil C map of the arctic regions.

Abbreviations: OC, organic C • SOC, soil organic C

This article has been cited by other articles:

				J. G. Bockheim and K. M. Hinkel The Importance of "Deep" Organic Carbon in Permafrost-Affected Soils of Arctic Alaska Soil Sci. Soc. Am. J., October 29, 2007; 71(6): 1889 - 1892. [Abstract] [Full Text] [PDF]

				S. Fiedler, D. Wagner, L. Kutzbach, and E.-M. Pfeiffer Element Redistribution along Hydraulic and Redox Gradients of Low-Centered Polygons, Lena Delta, Northern Siberia Soil Sci. Soc. Am. J., May 1, 2004; 68(3): 1002 - 1011. [Abstract] [Full Text] [PDF]