Alluvial soilsaresoilsdeposited by surface
water. You’ll find them along rivers, in
floodplains and deltas, stream terraces, and areas
called alluvial fans.
The Alluvial soil consists of various proportions
of sand, silt and clay.
It is formed due to the deposition of fine silt
called alluvium by the rivers.
Alluvial soils are very fertile. Itcontains soil
nutrients such aspotash, phosphoric acid and
lime.
The entire northern plains are made of alluvial soil.
These have been deposited by three important Himalayan
river systems –the Indus, the Ganga and the Brahmaputra.
These soils also extend in Rajasthan and Gujarat through a
narrow corridor.
Alluvial soil is also found in the eastern coastal plains
particularly in the deltas of the Mahanadi, the Godavari, the
Krishna and the Kaveririvers.
Sugarcane, paddy, wheat and other cereal and pulse crops
are grown with alluvial soil.
Bangar Khadar
Bangar
•It is an old alluvial.
•It has lower concentration
of kankurnodules.
•It has more fine particles.
•It is more fertile.
Alluvial soils are classified into
two types according to their age
as old alluvial (Bangar) and new
alluvial (Khadar).
Khadar
•It is an new alluvial.
•It has higher concentration
of kankurnodules.
•It has less fine particles.
•It is less fertile.