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समस्याग्रस्त मिट्टी का प्रबंधन कैसे करें For the management of problematic soils,  some general principles has to be considered for proper implementation of the reclamation measures. The total soluble salt concentrations in the root zone have to be decreased to control osmotic effects on plant growth. Maintenance of total soil moisture tension must be ensured at optimum level so that plant roots can absorb an adequate amount of water. Water flows through the soil in the direction of maximum decrease of hydraulic head and the flow velocity is proportional to the hydraulic gradient. The design and layout of drainage system are controlled by this principle. The availability of good quality water is of paramount for leaching and drainage of soluble salts. The Salt concentration in soil solution upward movement of salts and their accumulation increase with an increase in the evaporation and transpiration from the surface of the soil and the vegetation, especially when the ground water table is shallow. Increase or decrease of salts in the root zone depends upon whether the salt inputs are higher or lower than the salt outputs. The cations in the soil solution and those adsorbed on exchange complex are in equilibrium with each other. The dispersion and effectiveness of amendments are controlled by this principle. Management of Saline and Non saline alkali...

सेलाइन (खारा) मिट्टी के सुधार की तकनीक Accumulation of excess salts in the root zone resulting in a partial or complete loss of soil productivity is a worldwide problem. Soil salinity has caused heavy loss of national wealth in India. Out of 329 million hectares of land in the country, about 175 million ha (53 %) is suffering from degradation. The extent of this problem area as given by different sources varies from 8.56 M ha to 10.9 M ha. According to Central Soil Salinity Research Institute (CSSRI), Karnal, 1.7 M ha of land is affected by salinity among the 6.7 M ha of salt affected land. World as a whole is losing at least three hectare of arable land every minute by soil salinization. The problems of soil salinity are most widespread in the arid and semi-arid regions. Soil salinity is also a serious problem in areas where groundwater of high salt content is used for irrigation. The most serious salinity problems are being faced in the irrigated arid and semi-arid regions of the world and in these regions that irrigation is essential to increase agricultural production to satisfy food requirements. Development of saline soil There are several reasons for development of salinity in the soils such as, Excessive and uncontrolled irrigation Accumulation of salts in the...

भारत की मृदा व फसलों में बोरोन तथा मोलिब्डेनम की कमी और उर्वरकों के प्रयोग सेे उनमे सुुुुधार   Plants require eight micronutrients for their growth and development. Out of them, Boron (B) and Molybdenum (Mo) are anionic micronutrients found to be deficient in Indian soils and crops. The essentiality of the B and Mo for higher plants was first established by K. Warington in 1923 and by D. I. Arnon and P. R. Stout in 1939 respectively. The information regarding deficiency of B and Mo in soils in India, their role in plant growth and deficiency symptoms and fertilizers containing B and Mo for amelioration is being provided for the benefit of the stakeholders. Role of Boron and Molybdenum in plant growth and their deficiency symptoms Normal boron sufficient plants are having B content ranging from 10 to 200 mg/kg. Boron is neither a constituent of enzymes nor it activates any of the enzymes. Most important property of B is to form stable complexes with organic compounds. It is responsible for the cell wall formation and stabilization, lignification and xylem differentiation. It imparts drought tolerance to the crops. It plays a role in pollen germination and pollen tube growth. It facilitates ion uptake by way of increasing the activities of plasma membrane bound H+-ATPase....