Soils in West Bengal

Soils in West Bengal

The soils of Bengal have been studied widely by different scholars. The studies carried out so far lead to the convenient grouping of soils as

(i) Laterites,

(ii) Red Earths,

(iii) Tarai soils,

(iv) Alluvial soils and

(v) The Coastal soils

To attain scientific management of regional Resources and sustainable agricultural development, the country has been divided into 15 broad agro climatic zones and the physiographic setting of the State come under three Agro climatic Regions. Agriculturally, the three broad regions are Eastern Himalayan Region (Zone II), Lower Gangetic Plain Region (Zone III) and Eastern Plateau & Hilly Region (Zone VIII).

Three broad regions are further stratified into six agro-climatic sub regions. Salient features of these sub regions are as follows:

Zone II: Eastern Himalayan Region

a.) Hills sub region: Covering Darjeeling district. Mainly brown forest Soil, acidic in nature (pH 3.5-5.0), annual rainfall varies from 2500-3500mm., high humidity, less sunshine hours, poor soil depth and quality limits crop productivity. Pre-monsoon showers commences from March.

b.) Teri sub region: Covering Jalpaiguri and Coochbehar district. Soils are mostly sandy to sandy loams, porous, low in base content, poor in available nutrients; acidic(pH 4.2 to 6.2); rainfall varies from 2000-3200mm; high water table, low water holding capacity, high humidity, less sunshine hours during the monsoon months and marginality of lands in some parts limit crop productivity. Chronically deficient in micronutrients, like Boron, Molybdenum and Zinc, in particular.

Zone III: Lower Gangetic Region

a.) Old alluvium: Comprising North and South Dinajpur and Malda districts. Soils are lighter in higher situations and heavier in lower situations, mildly acidic to neutral in reaction (pH 5.2 to 7.0); fairly fertile over most of the sub region; rainfall 1500-2000mm in upper and 1300-1500m in lower parts, considerable area is flood prone.

b.) New alluvium: Covering Murshidabad, Nadia, Hoogly, Burdwan and North 24 Parganas. Soils are deep, mostly neutral in reaction (pH 5.5 to 7.0) and fertile; rainfall 1350- 1450 mm; most productive area of the State.

c.) Coastal saline: Covering South 24 Parganas, Howrah and Midnapore (E). Soils are mostly heavy clay containing higher salts of sodium, magnesium, potassium with organic matter at different stages of decomposition. Mostly neutral soils (pH 6.5 to 7.5). Electrical conductivity varies from3.0 to 18.0 mm, rainfall 1600-1800 mm; salinity and water congestion limit good crop productivity.

d.) Red laterite: Covering Birbhum, Bankura and Midnapore (W) districts. Soils are coarse in texture, highly drained with honeycomb type of ferruginous concentration at a depth of 15 to 30cm.; erosion prone; acidic in nature (pH 5.5 to 6.2); poor available nutrients; Average rainfall 1100-1400mm., low moisture holding capacity and poor nutrient status limit crop productivity.

Zone VII: Eastern Plateau & Hill Region

The region covers Purulia district. Soils shallow modulated gravely, coarse textured, well drained with low water holding capacity. Upload soils are highly susceptible to erosion; acidic in reaction (pH 5.5 to 6.2). Rainfall varies from 1100 to 1400mm. which is spread over only three months, mid June to mid September. Due to high slopes of the hill region of the northern part of the State with high rainfall and cooler temperature round the year, this area is almost covered with forests, plantation and orchard crops. Only one third area of this region is being cultivated with crops. The crop productivity is poor due to high slopes, high rainfall and erosion, shallow and acidic nature of the soils. The region offers good scope for extension of cultivation of ginger, summer vegetables, peach, plum etc., adopting a sustainable approach.

The soils of Terai and Teesta region are Light textured, strongly acidic due to high rainfall. Rice, jute and tobacco are the major Kharif Crops of this region, while in winter a number of winter Vegetable Crops, potato and a few pulses and oilseed crops are being grown with poor productivity. This agro-climatic region is also suitable for extension of cultivation of wheat, potato, groundnut, superfine & scented rice, high value spices like black pepper, cinnamon, ginger, turmeric, garlic etc. Cultivation of medicinal and aromatic Plants and allied sectors like Animal Husbandry and Fisheries-2/”>Fisheries are other potential areas for further development. The development of agriculture rests in the timely supply of good quality seeds and propagation materials of good varieties with a developed Marketing channel. Small & marginal farmers of North Bengal also have tradition for large scale cultivation of winter vegetables. However, they do not get adequate remunerative price for want of easy and cheap transport system, strong marketing system, cold storages and agro-processing units. This region is located at the centre of the eastern region of India and strategically positioned with three international frontiers- Bangladesh, Nepal and Bhutan and also borders the States of Jharkhand, Bihar, Orissa, Sikim and Assam. As a matter of fact, there are good prospects for agro-processing units for primary processing of vegetables, fruits and spices and at the same time bringing them in a semi-processed condition or secondary processed material with backward linkages to small rural centers.

West Bengal has by far the largest alluvial land, being 35 lakh ha in the country of which 22 lakh ha comes under Vindhya and Gangetic alluvial soil regions. These are endowed with neutral to near neutral, deep and fertile soils with high water holding capacity. The areas have advantage of river valley Irrigation as also ground water potentials. A wide range of wet and dry season field crops, vegetables, fruits and spices are being grown with around 200% Cropping intensity. Yet the productivity levels of a majority of the crops are below the potential levels mainly on account of low input and technology application influenced by poor economic status of the farmers and their limited access to institutional credit. These two regions have great promise for large scale cultivation of a variety of winter and rainy season vegetables as well as flowers. Notwithstanding the fact that mango, litchi, guava and banana are the prosperous fruit crops of these regions, the old mango orchards in Malda and Murshidabad districts have outlived their economic life and need replacement and/or rejuvenation. Common facilities like uninterrupted power supply, good quality water supply, cold-chain facilities, Warehousing facilities, forward integration with processing Industry are the interventions required for further development of the sectors in the region.

In the western belt of West Bengal there exists a vast tract relatively arid where the lands are lateritic and undulating. Such lands represent about one third of the cultivated area in the districts of Purulia, Bankura, parts of Paschim Medinipur, Bardhaman and Birbhum. Uplands of varying sizes, from a few hectares to a few square kilometers, are interspersed with terraced rice fields in the depressions and on the slopes. The bottom terraces where moderate yields of rice are obtained, generally belong to a few comparatively better-off farmers. The majority of the inhabitants of this region are predominantly tribals and other backward communities. They have largely depended on these marginal uplands where they attempt to grow some hardy varieties of poor yielding rice, certain small Millets, a minor pulse-horse gram and a minor oilseed-niger; to eke out a living. Except in the year of good rainfall, the yields are very poor, hardly compensating for the labour and other inputs. In spite of this, however, more and more such uplands are being brought under plough due to pressure of rising Population. The nutritional status is poor partly due to leaching losses on account of high soil porosity. The productivity of the soils in the region could be improved substantially through adoption of interventions like selection of suitable crop varieties, management of soil, adoption of water harvesting and soil conservation techniques, manuring, adjustment of sowing time, etc.

The southern most areas of West Bengal in the districts of South 24-Parganas, Purba Medinipur and southern Howrah are low lying and level part of the deltas of the river system of the Ganga on the northern coast of the Bay of Bengal. The rice fields are classified as medium low and low lands which are inundated by floods and rain water with poor drainage. Water stagnates throughout the monsoon period to a level of 30 to 60 cm. The vast tracts of coastal Saline Soils occur on the fringes of Bay of Bengal. Underground water table is present at a shallow depth with high salt content. Salts are raised to the surface during the dry periods of the year rendering it unfit for cultivation of many crops needed by the local people. These areas extend to 8.4 lakh ha. Only 4% of the cultivated area is irrigated with sweet water. The region is, therefore, a mono-cropped area with 4.2 lakh ha being cultivated area in the wet season and the rest six to seven months during winter and summer remain generally fallow. Of course, a few enthusiastic farmers in the less saline areas have adopted commercial cultivation of chilli and watermelon adjacent to their homestead. Possibilities of extension of sunflower, groundnut and Cotton cultivation providing saline water (Ec 5.2 dS/m) irrigation, have been reported. During the Kharif season, this tract receives about 1600 mm rains between June to October. This amount of water is far in excess of that required for Kharif crops. The proven technique of storing the excess rain water in 1/5th excavated land of the total cultivated land of a farmer and raising the adjacent embankment and crop field (Bhattacharya,1990 and RKMLSP) is strongly suggested for large scale adoption. This technique would surely bring in prosperity with the cultivation of fruits and vegetables on pond embankment and diverse field crops both in Kharif and Rabi seasons on the raised fields and pisci-culture amongst the small and marginal farming communities of this agro climatic region.,

West Bengal is a state in eastern India. It is the third-most populous state in India, with over 91 million inhabitants. The state has a diverse landscape, ranging from the Ganges Delta in the south to the Himalayas in the north. The soil in West Bengal is also diverse, with six main types: alluvial, laterite, red, saline, swampy, forest, and mountain soils.

Alluvial soils are the most common type of soil in West Bengal. They are formed from the sediments deposited by the Ganges and Brahmaputra rivers. Alluvial soils are fertile and well-drained, making them ideal for agriculture. Rice, jute, and wheat are the main crops grown in alluvial soils.

Laterite soils are found in the hilly regions of West Bengal. They are formed from the weathering of Igneous Rocks. Laterite soils are poor in nutrients and are not well-drained. They are mostly used for grazing and Forestry.

Red soils are found in the eastern part of West Bengal. They are formed from the weathering of sandstone and shale. Red soils are acidic and poor in nutrients. They are mostly used for growing rice and jute.

Saline soils are found in the coastal areas of West Bengal. They are formed from the accumulation of salts from seawater. Saline soils are not suitable for agriculture.

Swampy soils are found in the Sundarbans region of West Bengal. They are formed from the accumulation of organic matter in waterlogged areas. Swampy soils are not suitable for agriculture.

Forest soils are found in the forested areas of West Bengal. They are formed from the weathering of rocks and the accumulation of organic matter. Forest soils are poor in nutrients and are not well-drained. They are mostly used for forestry.

Mountain soils are found in the Himalayan region of West Bengal. They are formed from the weathering of rocks and the accumulation of organic matter. Mountain soils are poor in nutrients and are not well-drained. They are mostly used for grazing and forestry.

The soil in West Bengal is a valuable resource that supports the state’s economy and Environment. It is important to protect the soil from degradation and to use it wisely.

One way to protect the soil is to practice Sustainable Agriculture. Sustainable agriculture is a system of farming that uses practices that protect the environment and conserve resources. Some practices of sustainable agriculture include:

• Using cover crops to prevent erosion
• Rotating crops to prevent the build-up of pests and diseases
• Using organic Fertilizers to improve soil Health
• Conserving water

Another way to protect the soil is to reduce soil erosion. Soil erosion is the removal of soil from the land by wind or water. Soil erosion can be caused by natural events, such as floods and storms, or by human activities, such as deforestation and agriculture. Soil erosion can lead to a loss of topsoil, which is the most fertile layer of soil. It can also lead to the contamination of water supplies and the loss of Biodiversity-2/”>Biodiversity.

There are a number of things that can be done to reduce soil erosion, including:

• Planting trees and other vegetation
• Using cover crops
• Terrace farming
• Contour farming
• No-till farming

The soil in West Bengal is a valuable resource that supports the state’s economy and environment. It is important to protect the soil from degradation and to use it wisely. There are a number of things that can be done to protect the soil, including practicing sustainable agriculture and reducing soil erosion.

Here are some frequently asked questions and short answers about soils:

1. What are the different Types of Soil?

There are three main types of soil: sand, silt, and clay. Sand is the coarsest type of soil, made up of large particles. Silt is a finer type of soil, made up of smaller particles than sand but larger than clay. Clay is the finest type of soil, made up of very small particles.

1. What are the properties of soil?

Soil has many properties, including texture, structure, color, pH, and fertility. Texture refers to the size of the particles in the soil. Structure refers to the way the particles in the soil are arranged. Color refers to the hue of the soil. pH refers to the acidity or alkalinity of the soil. Fertility refers to the ability of the soil to support plant Growth.

1. What are the factors that affect soil formation?

The factors that affect soil formation include Climate, parent material, topography, organisms, and time. Climate refers to the average weather conditions in a particular area. Parent material refers to the material from which the soil is formed. Topography refers to the shape of the land. Organisms refer to the plants and animals that live in the soil. Time refers to the length of time that the soil has been forming.

1. What are the uses of soil?

Soil is used for many purposes, including agriculture, construction, and recreation. Agriculture is the use of soil to grow crops. Construction is the use of soil to build roads, buildings, and other structures. Recreation is the use of soil for activities such as hiking, camping, and fishing.

1. How can soil be protected?

Soil can be protected by reducing erosion, conserving water, and preventing pollution. Erosion is the process of soil being carried away by wind or water. Conservation is the careful use of resources. Pollution is the contamination of the environment with harmful substances.

1. What are the challenges facing soil?

The challenges facing soil include erosion, pollution, and Climate Change. Erosion is the process of soil being carried away by wind or water. Pollution is the contamination of the environment with harmful substances. Climate change is the change in the Earth’s climate over time.

1. What is the future of soil?

The future of soil depends on how we manage it. If we continue to erode, pollute, and degrade soil, it will become less productive and less able to support life. However, if we take steps to protect and conserve soil, it will continue to be a vital resource for us and for future generations.

1. Which of the following is not a type of soil?
   (A) Alluvial soil
   (B) Black soil
   (C) Red soil
   (D) Sandy soil

2. Which of the following is the most fertile type of soil?
   (A) Alluvial soil
   (B) Black soil
   (C) Red soil
   (D) Sandy soil

3. Which of the following is the most common type of soil in India?
   (A) Alluvial soil
   (B) Black soil
   (C) Red soil
   (D) Sandy soil

4. Which of the following is the most common type of soil in West Bengal?
   (A) Alluvial soil
   (B) Black soil
   (C) Red soil
   (D) Sandy soil

5. Alluvial soil is formed by the deposition of sediments from rivers.
   (A) True
   (B) False

6. Black soil is rich in organic matter and is well-drained.
   (A) True
   (B) False

7. Red soil is rich in iron and aluminum oxides and is poor in organic matter.
   (A) True
   (B) False

8. Sandy soil is loose and well-drained, but it does not hold water well.
   (A) True
   (B) False

9. Soil is a mixture of Minerals, organic matter, water, and air.
   (A) True
   (B) False

10. Soil is essential for plant growth.
    (A) True
    (B) False