Different Types of Soils in India Essay

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1 ) Black soil The principal region of dark soils is the Deccan plateau and its periphery extending coming from 8°45’to 26o north lat. and 68o to 83o45? east longitude. They are created from Deccan basalt snare rocks and occur in areas under the monsoon climate, generally of semi-arid and sub-humid types. The entire climate of black soil region can be described as sizzling and dried summer, 40-100 cm rainfall per annum, moderate to modest winters and annual temp ranges via 24-30o centigrade, mean maximum temperature during April-May ranges from 36~42°C arid imply minimum temperature during winter amounts from 15-24° centigrade.

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Semi-arid to sub-humid, tropical to sub-tropical monsoon type environment with various dry and wet periods and calcification (formation of calcium carbonate) are great to the development of black soils. The soils are characterised by simply dark greyish to dark colour with 35-60% clay-based, neutral to slightly alkaline reaction, high swelling and shrinkage, plasticity, deep fractures during summer and poor status of organic subject, nitrogen and phosphorus. Impeded drainage and low permeability are the major problems.

Dark soils. are divided into short black soil of a depth of 30-50 cms, method black soil of 50-120 cm and deep black soils greater than 120 cms. The all-natural vegetation comprises dry deciduous species, viz palas (Butes frondoss), sisam (Dalbergia sisu), neem (Azadirachta indica) and teak (Tectona grandis). Silk cotton, sugarcane, groundnut, millets, maize, pulses, safflower are the common crops produced on these types of soils. Because of their inherent drainage problem, they are prone to salinity and sodicity under irrigated conditions until proper draining is guaranteed. Because of its excessive water holding onto capacity, rainfed crops just like minor millets, pulses just like horse gram are fruit and vegetables of different types and lemon or lime fruits can even be grown.

These types of soils are known as regurs, nullah regadi (a telugu word meaning black clay) and black cotton soils as cotton was the significant crop cultivated in these soil. 2 . Red soils These types of soils are derived from granitic, gneiss and also other metamorphic dirt. These soil are created under very well drained condition. The climate is semi-arid tropical with mean annual temperature of 25°C and mean annual rainfall coming from 75-100 cm. The soil are bigger textured, delicat structure and contains low soluble salts.

They may be slightly acidic to somewhat alkaline, very well drained with moderate permeability. They are generally poor in nitrogen, phosphorus, lime, humus etc . In this soil, lime green concretions and free carbonates are absent. The reddish colored colour is because of the higher amount of hydration of the fericoxide in the soils. Upon uplands, they are gravelly soft sand or rocky, flinty, pebbly and porous and light colored on which foodstuff crops like bajra may be grown.

Around the lower plains and valleys, they are darker, coloured agricultural loams, irrigated crops like maize, whole wheat, pulses, taters, fruits, millets etc could be grown. These types of soils are also found underneath forest plants. Sometimes they found along with dark soils (side by side) and also yellow soils (red and discolored soils). Extreme gravelliness, surface area crust development and susceptibility to erosion due to excessive slopes are some of the problems during these soils which is often overcome simply by adopting appropriate measures.

Morphologically the reddish soils could be divided into crimson loams which may have a cloddy structure and argillaceous soil and crimson earths with loose delicat top ground rich in sesquioxide type of minerals. 3. Laterites and lateritic soils Laterite is a geological term and means practically a rock and roll. The laterites and lateritic soils had been loosely used in the same sense. The lateritic soils happen to be enriched with oxides of iron and aluminium, underneath the conditions of high rainfall with alternate dried and rainy periods.

During rainfall silica is leached downwards and iron and aluminium oxides remains in the top layers. Laterites usually are shallow and gravelly in higher lands, but are extremely deep loam to clay-based soils in the valleys where good terme conseille crops happen to be produced. Higher landy soil are poor in nutrient status where as lower level soil are dark and richer in nutrition and organic matter. Every lateritic soils are poor in calcium supplement, magnesium, nitrogen, phosphorus and potash.

They are really generally well drained and porous. The soil reaction is more around the acidic part. On laterites, as already mentioned, rice is grown by lower elevations and at higher elevations, tea, coffee, cinchona, rubber and cashewnut can be grown below good ground management conditions.

On the whole, laterites are poor in male fertility and conveniently respond to manuring and very good cultivation. Depending on the weather lateritic soil are grouped into high rainfall areas with highly and weakly expressed dried season and humid zones with obvious dry & wet intervals. 4. Alluvial soils Limoneux soils, cover the largest place in India (approximately 7 lakh km2) and these are generally the most important soils from farming point of view. The key features of limoneux soils have already been derived while silt deposition laid down by the Of india river devices like the Indus, the Ganges, the Brahmaputra and the rivers like Narmada, Tapti: Mahanadi, Godavari, Krishna and Cauvery.

These waterways carry the items of enduring of stones constituting the forest and first deposit them along their route as they stream down the simple land towards sea. Geologically, the deposits is split up into recent clod which is generally known as Khadar and old deposits, as bhangar. The new alluvium can be sandy and lightweight coloured whereas older clod is more clayey, dark colored and contains lime concretions.

The soils have got a wide range in soil characteristics viz. acidity to alkaline sandy to clay, normal to saline, sodic and calcareous, shallow to very deep. The climate ranges from dry to humid sub-tropical. This groupings of alluvial soil may be recognised: alluvial soil (Khadar, bhangar and remarkably calcareous), deltaic alluvium, seaside alluvium, seaside sands, calcareous sierocomic and grey-brown soils. a. Limoneux soils The alluvial soils occuring in the Indo-Gangetic flatlands and the Brahmaputra valley cover a large location. The soil are moved and placed by the rivers from the parent material. The rivers will be the Ganga, Jamuna, Brahmaputra and the tributaries.

The soils happen to be deep and hard pots and pans in the subsoil are calcareous (made of calcium carbonate) and acid. These are lacking in nitrogen, phosphorous and humus, although not in potash and lime. These soil are agricultural amongst all the soils of India.

That they produce a wide selection of crops like rice, wheat, sugarcane, jute and spud. They are allocated mainly in the northern, north-western and north-eastern parts of our country. b. Deltaic limoneux soils They can be formed by sediments taken by rivers and deposited in the jaws of rivers joining the sea. The deltas of the Bolada, Brahmaputra, Mahanadi, Godavari, Krishna and Cauvery are the most crucial ones.

In Gujarat, the deltaic limoneux soils which are sandy loam to clay-based loam happen to be locally named Goradu soil. The Godavari and Krishna rivers move through basaltic place having black soils and these soil are darker and good textured. The Cauvery delta soils will be significantly clayey and Bolada delta soil show high accumulation of organic matter, as in the Sunderbans of West Bengal, due to swampy vegetation. These soils happen to be fertile and grow lots of crops fitted to climatic conditions. c. Coastal freehold Soils designed on coastal alluvium are located along, the ocean coasts. Soil are dark coloured, rough textured and poor in fertility.

Some soils will be saline due to the inundation of sea water. Such soil in the Konkan coast of Maharashtra are called Khar soil. d. Coastal sands Soft sand soils happen prominently in the coastal part of Tanjavur area of Tamil Nadu, over the Kerala shoreline, Bapatla in Guntur distrjct of Andhra Pradesh and Puri district in Orissa. If sandy soils are certainly not saline, planting crops just like coconut, cashew and casuarina can be taken on for fostering. Other soil under clod are calcareous sierozomes and gray brown soils.

Calcareous sierozomes can be seen in the desertic location of Haryana and Punjab. The word ‘sierozem” denotes a team of soils possessing a brownish-grey surface horizon which has a sub-layer of carbonates which can be developed underneath mixed shrub vegetation in a-temperate to cool, dry climate. Grey-brown soils since the term itself indicates its characteristics, can be found in, wasteland soils of Rajasthan. 5. Desert soils In the north-western part of India, desert soils occur above an area of 0. 30 million hecta, res, which includes a major part of Rajasthan, south of Haryana and Punjab and northern element of Gujarat. Rainfall ranges from less than 10 cms to 50 cms, mostly offered during monsoon season.

The location consists of sand dunes and undulating soft sand plains. The temperature regime is very excessive throughout the year and a maximum of 50-60°C is recorded during summer. Due to temperature organic-matter developed is very low.

The soil in the flatlands are mostly created from alluvium and they are pale brown to dark brown to yellow brown and fine exotic to loamy fine sand and they are structureless. The clay material low and presence of alkaline the planet carbonates is a crucial feature. The nitrate nitrogen and phosphorus makes the wilderness soils fertile and productive under appropriate moisture source. By elevating the water having capacity, the productivity in the soils could be increased that involves addition of organic matter and clay. 6. Tarai soils The phrase “tarai” is known as a hindi term, which means moist.

Thus, i actually is a damp regime having high normal water table. Tarai soils happen to be foot hii soils and extend in strips of varying widths at the ft . of Himalayas in Jammu and Kashmir, Uttar-Pradesh, Bihar and West-Bengal. Soils beneath the natural circumstances are thickly vegetated and swampy.

Several kinds of grasses and trees in the native plants on removal of which the soils become very productive. The soils are formed from the materials that are washed straight down by the erosion of mountains. They are limoneux origin.

Large soil wetness content all through the year ends in luxuriant plants dominated simply by tall solide. They are natural to a little bit alkaline with significant amounts of organic matter. The texture varies from soft sand loam to silty loam.

Generally, these soils will be fertile through providing right drainage, the productivity can be increased.

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