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,Soils in West Bengal

(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).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 are other potential areas for further development. 

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.

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. 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.