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1
Photosynthesis and Productivity in Different Environments
... SEMIARID REGIONS Steppe on typical and leached chernozems 1300 Steppe
on ordinary and southern chernozems 800 Steppe on solonets chernozems 800
Steppified formations on solonets 500 Halophytic formations on solonchak 400 ...
2
Productivity of World Ecosystems: Proceedings of a Symposium ...
... semiarid regions Steppe on typical and leached chernozems 25 1,607.5 13
1,355.9 Same, on ordinary and southern chernozems 20 2,942.0 8 1,176.8 Same
, on solonets chernozems 20 500.0 8 200.0 Steppified formations on solonets 16
...
3
Trace Elements in Soils
... gray brown soils orthid 5-7 cobalt accumuUstyurt loam deposit lates in surof
quaternary face crust age and humus horizon U.S.S.R. ancient weather-
solonchakous natric salorthid 140 A Or'-Kumak ing crust solonets 140 B1
Watershed 60 B2 ...
H. Aubert, M. Pinta,
1980
4
Environmental Chemistry: Asian Lessons
In local depressions, salini/ation processes develop with formation of meadow-
steppe solod and solonets complex and even peaty-swampy solonchaks. The
acidification processes are more pronounced in those parts of the South Siberian
...
5
Israel Program for Scientific Translations?
Bogdanov (1954), Migutskii (1955, 1959) and other workers showed that the
contents of nitrogen and phosphorus in solonets soils correspond to their humus
reserves. The solonets soils of the steppe zones are more depleted than those of
the ...
United States. National Technical Information Service,
1971
6
Genesis and classification of semidesert soils
Moreover, subtypes are distinguished by stages of development of the solonets
profile, namely : solonchak, typical, solodized, and residual solonets. Most
common are the solonchak solonets soils. Due to the heterogeneity of material
and the ...
Evgenii︠a︡ Nikolaevna Ivanova, Pochvennyĭ institut imeni V.V. Dokuchaeva,
1970
7
Central Asia, 130 Years of Russian Dominance: A Historical ...
If this water is not carried away an intermediate stage of salinization may occur
and a solonets soil be formed, where the lower layers of the soil harden into
columnar units which are impervious to water. Such soils are unfit for the growth
of ...
The solonets are completely desalinized in horizon A. The data shows that the
salts begin to occur in the depth of 20 — 40 cm and frequently reach their
maximum in horizon C in the solonets of Vojvodina. The lower horizons of these
solonets ...
Ǵorǵi Filipovski, Milivoje Ćirić,
1969
Solonets formations that differ from the dominant component mainly through a
more clearly defined solonets horizon and a shallower depth of salt deposition
are associated with black wormwood and prostrate summer cypress on the talus
of ...
10
Agrochemistry of the soils of the USSR: Western Siberia
Solonets soils in southern subzones have a much thinner solonets layer, the
color is weaker, effervescence begins at a higher level and the sulfates occur at a
higher level. The soils occurring in nature often deviate to a considerable extent ...
Andreĭ Vasilʹevich Sokolov, S. S. Trofimov, Roman Viktorovich Kovalev,
1971
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