KSIĄŻKI POWIĄZANE ZE SŁOWEM «GLEIZATION»
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1
Management for Freshwater Fish Culture: Ponds and water ...
Gleization Light organic layer <252> 3. lf the bottom soil is too permeable to be
sealed by this method, an alternative is to create an impervious biological plastic
layer in the bottom and on the sides of the pond. Such an impervious layer is ...
James F. Muir, Thomas L. Laughlin, 1996
2
Soils: Genesis and Geomorphology
... usually soft, calcareous material Grasses and sedges Gleization and some
calcification Swamp forest or sedges Gleization and grasses Swamp forest or
sedges Gleization and grasses Grass or forest Forest Podzolization and
gleization; ...
Randall J. Schaetzl, Sharon Anderson, 2005
3
Soils of the Past: An Introduction to Paleopedology
Burial gleization of organic matter Blue-gray or green-gray color of horizons, of
mottles or of haloes around root traces provides a striking contrast to red parts of
many paleosols. In some profiles, the light-colored surface horizon and root
traces ...
Gregory J. Retallack, 2008
Gleization (14) is a process that develops a horizon of light olive gray or gray
material immediately below the dark colored surface layer. In this county this
process occurs where a perched water table is at or slightly below the surface
layer.
United States. Bureau of Soils, United States. Bureau of Plant Industry, United States. Bureau of Plant Industry, Soils, and Agricultural Engineering, 1978
5
Eocene and Oligocene Paleosols of Central Oregon
Burial gleization Drab haloes around root traces in some of these paleosols are
best interpreted as products of the anaerobic decay of organic matter buried with
the soil, as already discussed (Figs. 12 and 13). Such burial gleization is ...
Greg John Retallack, Erick A. Bestland, Theodore J. Fremd, 1999
6
Soil survey of Blue Earth County, Minnesota
Gleization {1U) is a process that develops a horizon of light olive gray or gray
material immediately below the dark colored surface layer. In this county this
process occurs where a perched water table is at or slightly below the surface
layer.
United States. Soil Conservation Service, Richard O. Paulson, Minnesota. Agricultural Experiment Station, St. Paul, 1978
In many instances, however, relief and parent material do limit, or sup ress
entirely, the progress of podzolization, and gleization ecomes active in varyin
degrees. All of the soils of the Mississip i River Alluvia Plain are immature and the
effects ...
8
Soil Microbiology and Biochemistry
Iron oxidation-reduction plays a vital role in soil formation process known as '
gleization'. Gleying is a process involving changes in chemical speciation that
result in changes in solubility. It is characterized by iron reduction and its
subsequent ...
9
Development and Significance of the Great Soil Groups of the ...
GLEIZATION Gleization connotes the general process by which those soils
having a glei horizon are formed. This light-colored glei horizon is formed, due to
lack of oxygen, under conditions of excessive moistening in the mineral portion of
the ...
Charles Edwin Kellogg, 1936
10
Ecology and Wildlife Biology
Different kinds of soil are produced due to various mechanisms as podsolization,
laterization, calcification, gleization and salinization etc.. which support different
vegetation groups (Table 3.2). c*. □ Podsolization : This set of process is ...
