scholarly journals Assessment of Land Use Potential for Sustainable Development of Chorgali Village of Hura block, Puruliya district, West Bengal

Agropedology ◽  
2019 ◽  
Vol 27 (1) ◽  
Author(s):  
Dolan Champa Sarkar ◽  
◽  
P. P. Mitranag ◽  
S. K. Mohit Pasha ◽  
S. Roychowdhury ◽  
...  

The information on soil and land resources of Chorgali, a rainfed village, Hura block, Puruliya district, West Bengal was generated through remote Sensing and GIS to asses their productivity potential and limitations. Thirteen soil series were tentatively identified and mapped with 26 mapping units. These mapping units (phases of series) have been grouped in different land capability sub-class and soil conservation measure have been suggested.

Agropedology ◽  
2019 ◽  
Vol 28 (1) ◽  
Author(s):  
Akash Borse ◽  
◽  
M.S.S. Nagaraju ◽  
Benukantha Dash ◽  
Nisha Sahu ◽  
...  

The present investigation was carried out in Barela village of Seoni district, Madhya Pradesh to characterize, classify and evaluate the land resources using IRS-LISS-IV and GIS. Five major landforms viz. plateau; escarpments, mound, pediment and alluvial plain were identified and delineated. Based on image characteristics, seven land uses/ land cover classes’ viz., single crop, double crop, degraded forest, wasteland, river, waterbody and habitation were identified. Five slope classes viz., very gently sloping (1-3%), gently sloping (3-5%), moderately sloping (5-10%), strongly sloping (10-15%) and steeply sloping ( 15-25%) lands have been identified using Cartosat-1 DEM (30 m resolution) and topographic information. Five soil series (Barela-1, Barela-2, Barela-3, Barela-4 and Barela-5) were tentatively identified and mapped based on landform-soil relationship. Soils, in general, are shallow moderately deep, moderately well to well drained with moderate to severe erosion and clayey in texture. The soils are neutral to slightly alkaline in reaction and non-saline and qualify for Lithic Ustorthents/ Typic Haplustepts/ Typic Haplusterts at subgroup level. The soils were grouped under land capability sub-classes IIs, IIIes, IVst and VIst and land irrigability sub-classes 2s, 3st and 4st. The soils of Barela-4 (subgroup) are moderately suitable for growing gram, soybean, maize and pigeonpea. The soils of Barela-5 (subgroup) are highly suitable for growing pigeonpea and moderately suitable for growing gram, soybean and maize. Soils of Barela-1, Barela-2 and Barela-3 are not suitable for growing gram, soybean, maize and pigeonpea. Various soil and water conservation measures and alternate land use options have been suggested based on land resources information generated for management of land resources in the village.


1984 ◽  
Vol 103 (2) ◽  
pp. 377-386 ◽  
Author(s):  
J. W. S. Reith ◽  
R. H. E. Inkson ◽  
K. S. Caldwell ◽  
W. E. Simpson ◽  
J. A. M. Ross

SUMMARYTopsoils from eight different soil series were substituted for the local soil in three arrangements involving two depths of topsoil and either local or sand subsoils. A rotation of crops was grown with uniform annual N, P and K treatments for 24 years. A peaty soil produced the highest yields of grain, straw and grass, presumably because it released more N than the mineral soils, but an average yield of swedes. No mineral soil consistently produced higher yields of all crops and, although there were some significant differences, the variations in yield were generally relatively small. The deep topsoil consistently produced the highest yields. Topsoil with sand subsoil gave the lowest yields of grain, straw and swedes but not of grass.All the crops on the peaty soil had higher concentrations of P in the dry matter than those from the seven mineral soils. Crops and herbage on the Laurencekirk and Foud-land soils had consistently slightly higher P concentrations than those on the other five mineral soils. Compared with the amounts applied, the crops removed considerably more K but only 45–68% of the P. There were large differences in the proportion of the P residues extractable by acetic acid from the different soil series.The depth of topsoil was at least as important as soil type in determining yield, and the results support the use of soil depth as one of the main factors used in the Land Capability Classification for Agriculture.


2018 ◽  
Vol 115 (5) ◽  
pp. 874
Author(s):  
Subhobroto Mazumder ◽  
Kalyan Adhikari ◽  
Durga Shanker Mitra ◽  
Samiran Mahapatra ◽  
Krishan Kumar Singh Pangtey

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