spodosols वाक्य
उदाहरण वाक्य
मोबाइल
- Spodic may also refer to the taxonomic soil order spodosols.
- Spodosols over mafic rock may have a medium brown E horizon underlain by a darker B.
- Entisols, Inceptisols, Mollisols, Spodosols, Alfisols, Ultisols, Oxisols, Aridisols, Vertisols, Andisols and Histosols.
- Spodosols are also found in warm, moist environments such as Florida and in fact are the most prominent soil order of the state.
- Spodosols have a B horizon containing a relatively high concentration of illuviated aluminum with accompanying illuviated organic matter, and in many cases, illuviated iron.
- The above soil orders in sequence of increasing degree of development are Entisols, Inceptisols, Aridisols, Mollisols, Alfisols, Spodosols, Ultisols, and Oxisols.
- The Spodosols correspond to the Podzols of Russia, Central Europe and Northern Europe and to the Podzolic soils found in much of Canada's boreal forest .)
- The U . S . Soil Taxonomy classifies Inceptisols, Mollisols, and Spodosols as good soils that can support temperate forests that like mature soils that can support deep root systems1.
- Though they are known from as far back as the Carboniferous, there are few examples surviving from before the first Pleistocene glaciation, and some of these may not be true spodosols.
- Spodosols often occur under coniferous forest in cool, moist climates, such as southeastern Alaska, the Great Lakes region, the northeastern states, and higher elevations of the northwestern states.
- Spodosols are known only from the Carboniferous and from a few periods since that time-though less acidic soils otherwise similar to spodosols are known from the Mesozoic and Tertiary and may constitute an extinct suborder.
- Spodosols are known only from the Carboniferous and from a few periods since that time-though less acidic soils otherwise similar to spodosols are known from the Mesozoic and Tertiary and may constitute an extinct suborder.
- There are also some forest soils of more recent times that cannot clearly be classified as Alfisols or as Spodosols because, despite their sandy horizons, there are not nearly acidic enough to have the typical features of a Spodosol.
- With the aid of X-ray diffraction, paleosols can now be classified into one of the 12 orders of Soil Taxonomy ( Oxisols, Ultisols, Alfisols, Mollisols, Spodosols, Aridisols, Entisols, Inceptisols, Gelisols, Histosols, Vertisols and Andisols ).
- This process of podzolisation results in the characteristic soil profile of spodosols, in which the E horizon is usually an ashen grey or white colour without structure and there is a distinctive hardpan oxide layer in the B horizon ( which is always darker than the E horizon ).
- In soil science, "'podzols "'( known as "'spodosols "'in China and the United States of America and "'podosols "'in Australia ) are the typical soils of coniferous, or E horizon ) during first plowing of a virgin soil of this type.
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