Quantitative and Qualitative Composition of Soil Organic Matter in Samples of Ice Complex from Central Yakutia, Eastern Siberia

Figure 2

The general view of the thermokarst lake (a), formed as a result of the melting of the ice complex on the monitoring range “Chyuya”; a soil section of Cryosols Haplic Cambisols Dystric of the investigated ice complex (b).

(a)

(b)