NDLI: Soil cover patterns in the northern part of the area of aspen-fir taiga in the southeast of Western Siberia

Content Provider	Springer Nature Link
Author	Loiko, S. V. Geras’ko, L. I. Kulizhskii, S. P. Amelin, I. I. Istigechev, G. I.
Copyright Year	2015
Abstract	Soil cover patterns in the northern part of the area of aspen-fir taiga on the Tom’-Yaya interfluve at 170–270 m a.s.l. are analyzed. Landscapes of the subtaiga piedmont province are found at somewhat lower heights. The three major forms of the local mesotopography include virtually flat interfluve surfaces, slopes (that predominate in area), and the network of ravines and small river valleys. Modal soil combinations on the slopes consist of the typical soddy-podzolic soils with very deep bleached eluvial horizons and dark gray (or gray) residual-humus gleyic soils with dark humus coatings. With an increase in the degree of drainage of the territory (toward the local erosional network), the portion of gleyic soil subtypes decreases from nearly 100% on the flat interfluves to 10–15% on the slopes; the portion of soils with residual humus features decreases from 80–90 to 10–15%, respectively. These two soil subtypes can be considered intergrades between typical soils of the aspen-fir taiga (soddy-podzolic soils with very deep bleached horizons) and dark gray and gray residual-humus soils characteristic of the subtaiga zone in the south of Western Siberia.
Starting Page	359
Ending Page	372
Page Count	14
File Format	PDF
ISSN	10642293
Journal	Eurasian Soil Science
Volume Number	48
Issue Number	4
e-ISSN	1556195X
Language	English
Publisher	Pleiades Publishing
Publisher Date	2015-04-15
Publisher Place	Moscow
Access Restriction	One Nation One Subscription (ONOS)
Subject Keyword	Luvisols aspen-fir taiga soil cover texture-differentiated soils soddy-podzolic soils dark gray soils Western Siberia Geotechnical Engineering & Applied Earth Sciences
Content Type	Text
Resource Type	Article
Subject	Earth-Surface Processes Soil Science

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