
Mention two similarities between the red soil and laterite soil?
Answer
554.7k+ views
Hint:
Red soil is a type of soil that develops in a warm, temperate, moist climate under deciduous or mixed forest. Laterite is both dirt and a stone sort wealthy in iron and aluminium and is normally considered to have shaped in hot and wet tropical territories.
Complete solution:
Two similarities between red soil and laterite soil are:
(I) Both are red in shading as they are wealthy in iron oxide.
(ii) Both are inadequate in nitrogen.
•The two soils are red as a result of the presence of Iron oxides.
Red soil is a significant soil asset, which bears considerable ramifications for economical improvement of horticulture and solid development of the economy. Red soils are exceptionally filtered soils of the muggy jungles having a high substance of sesquioxides. Red soils are prevalent in South America, Central Africa, South and Southeast Asia, China, India, Japan and Australia. All in all, these dirt have great states of being for plant development in spite of the fact that they frequently have exceptionally low water-holding limits. Laterite soils are generally the final results of weathering. They are framed under states of high temperature and hefty precipitation with substitute wet and dry periods. Heavy precipitation advances draining (supplements moves washed away by water) of soil whereby lime and silica are filtered away and dirt wealthy in oxides of iron and aluminium mixes is left behind. ‘Laterite' signifies a block in Latin. They solidify extraordinarily on losing moisture. Laterite soils are red in shading because of little dirt and more rock of red sand-stones. Laterite, soil layer that is wealthy in iron oxide and gotten from a wide assortment of rocks enduring under emphatically oxidising and draining conditions. It structures in tropical and subtropical districts where the atmosphere is sticky. Lateritic soils may contain dirt minerals yet they will, in general, be silica-poor, for silica is drained out by water going through the territory.
Note:
A basic element for the development of laterite is the reiteration of wet and dry seasons. Red soil is Seen principally in low precipitation territory and they are otherwise l called Omnibus gathering.
Red soil is a type of soil that develops in a warm, temperate, moist climate under deciduous or mixed forest. Laterite is both dirt and a stone sort wealthy in iron and aluminium and is normally considered to have shaped in hot and wet tropical territories.
Complete solution:
Two similarities between red soil and laterite soil are:
(I) Both are red in shading as they are wealthy in iron oxide.
(ii) Both are inadequate in nitrogen.
•The two soils are red as a result of the presence of Iron oxides.
Red soil is a significant soil asset, which bears considerable ramifications for economical improvement of horticulture and solid development of the economy. Red soils are exceptionally filtered soils of the muggy jungles having a high substance of sesquioxides. Red soils are prevalent in South America, Central Africa, South and Southeast Asia, China, India, Japan and Australia. All in all, these dirt have great states of being for plant development in spite of the fact that they frequently have exceptionally low water-holding limits. Laterite soils are generally the final results of weathering. They are framed under states of high temperature and hefty precipitation with substitute wet and dry periods. Heavy precipitation advances draining (supplements moves washed away by water) of soil whereby lime and silica are filtered away and dirt wealthy in oxides of iron and aluminium mixes is left behind. ‘Laterite' signifies a block in Latin. They solidify extraordinarily on losing moisture. Laterite soils are red in shading because of little dirt and more rock of red sand-stones. Laterite, soil layer that is wealthy in iron oxide and gotten from a wide assortment of rocks enduring under emphatically oxidising and draining conditions. It structures in tropical and subtropical districts where the atmosphere is sticky. Lateritic soils may contain dirt minerals yet they will, in general, be silica-poor, for silica is drained out by water going through the territory.
Note:
A basic element for the development of laterite is the reiteration of wet and dry seasons. Red soil is Seen principally in low precipitation territory and they are otherwise l called Omnibus gathering.
Recently Updated Pages
Why are manures considered better than fertilizers class 11 biology CBSE

Find the coordinates of the midpoint of the line segment class 11 maths CBSE

Distinguish between static friction limiting friction class 11 physics CBSE

The Chairman of the constituent Assembly was A Jawaharlal class 11 social science CBSE

The first National Commission on Labour NCL submitted class 11 social science CBSE

Number of all subshell of n + l 7 is A 4 B 5 C 6 D class 11 chemistry CBSE

Trending doubts
What is meant by exothermic and endothermic reactions class 11 chemistry CBSE

10 examples of friction in our daily life

One Metric ton is equal to kg A 10000 B 1000 C 100 class 11 physics CBSE

1 Quintal is equal to a 110 kg b 10 kg c 100kg d 1000 class 11 physics CBSE

Difference Between Prokaryotic Cells and Eukaryotic Cells

What are Quantum numbers Explain the quantum number class 11 chemistry CBSE

