SOIL TYPES OF THE WORLD
Soil
is an essential part of growing own food. There are four main soil types: clay,
loam, sand, and peat, with loam being a mixture of sand and clay. Clay soil
structure is sticky when wet, and
hard as a brick when dry. In Sandy soil
the nutrients are quickly washed away. Also sandy soil suffers in drought
conditions as it drains so much faster than a heavy soil. Loam is the
intermediate between clay soil and sandy soil. It drains well, but also holds
nutrients well. With the addition of a little humus, and sometimes a little
lime, a loam is often the best soil for most growing. Peat soil is very rare
which is a pity because it contains so many nutrients. Peat forms when
vegetable matter dies and settles at the bottom of a swamp. Climate, vegetation
and soil are intimately related and soil formation is affected by vegetation
and climate.
In
the world Dokucharyev gave first
classification of soil.
He divided the soil
into 3 groups which are :
(i) Zonal
Soil :
ZONE SOIL
TYPE
1. Boreal Tundra
(dark brown soil)
2. Taiga Light
grey podsol soil
3. Forest
steppe Grey
and dark grey soil
4. Desert
steppe Chestnut
brown or white soil
5. Steppe
Chernozem
soil
6. Desert Aerial
yellow soil
7. Sub
tropical and tropical forest Laterite
and red soil
(ii) Transitional
Soil
1. Dry
land moor soil
2. Carbonate
containing soil
3. Secondary
alkaline soil
(iii) Abnormal
Soil
1. Moor
soil - Cold region soil
2. Alluvial
soil - Transported
through water
3. Aeolian
soil - Tranported
through wind
The
most recent classification of soil type is proposed by soil survey staff of
USDA (1960), which is following:
1. Entisols - Azonal
soil
2. Vertisol - Grumu
soil
3. Inceptisol - Brown
forest soil
4. Aridisol - Desert
redish desert soil
5. Mollisol - Chernozem,
chestnut, brunizem
6. Spodosol - Podsol,
brown podsolic soil
7. Uttisol - Red
yellow podsolic, laterite soil
8. Oxysol - Laterite
soil, latosols
9. Histosol - Bog
soil
10. Alfisol - Grey
brown podsol soil
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