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Significance of Microtopography and Cryoturbation in Mature Larch<br />

Forest near Yakutsk, Eastern Siberia, Russia<br />

Yuki Sawada 1 , Go Iwahana 2 , Tetsuoh Shirota 1 , Ryusuke Hatano 3<br />

Masami Fukuda 1 , Alexander N. Fedorov 4<br />

(1. Institute of Low Temperature Science, Hokkaido University, Sapporo, Japan; 2. Graduate School of<br />

Engineering, Hokkaido University, Sapporo, Japan; 3. Graduate School of Agriculture, Hokkaido<br />

University, Sapporo, Japan; 4. <strong>Permafrost</strong> Institute, Russian Academy of Science, Yakutsk, Russia.)<br />

Abstract: The microtopography (earth hummocks) and cryoturbation structures are measured<br />

and described by digital photogrammetry and sketch on pit sections. A study plot was<br />

established in mature larch forest near Yakutsk, eastern Siberia. The 1cm DEM and contour<br />

map of 2cm interval of a 4m 2 quadrat revealed the existence of a number of small mounds and<br />

surrounding troughs on the mineral soil surface, which was covered with an organic soil layer.<br />

Mean diameter of the mounds and mean intervals are approximately 30-50cm, and relative<br />

height is 10-20cm. Sidewalls of the troughs have an apparent straight shape. The dead root and<br />

funnels were found within the troughs, indicating the root expansion into the troughs, and it<br />

forced trough edges being straight.<br />

Cryoturbation structures were appeared in the sidewalls on the quadrat pit. Upper and<br />

lower boundaries of the mixed layer have a wave-like form. The concave, bowl-shaped<br />

depressions in the lower boundary are located under the convex mounds on the mineral soil<br />

surface. The wave length of the lower boundary is approximately 1m. Black mineral soils are<br />

deposited in the troughs, and they had an extension down to the large pools of the black mineral<br />

soil. These structures indicate that the surficial mineral soil darkened with organic matter<br />

submerged into the active layer, and these finally stored in the pools of black mineral soil<br />

within the active layer. Large amount of organic-affected black soils can be stored within the<br />

active layer.<br />

The soil movements can be explained by the circulation model, which is proposed for<br />

earth hummock growth by Mackay (1980). He demonstrated that the cell-like soil circulation<br />

occurs if there are bowl-shaped frozen table, because of the upward and downward movement<br />

of melting soil with the driving force of the gravity. Bowl-shaped lower boundaries appeared in<br />

the sections were probably associated with the frost table when soil circulation occurred.<br />

Key words: Siberia, Continuous permafrost, microtopography, cryoturbation, soil carbon pool,<br />

digital photogrammetry<br />

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