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सिलिकॉन Tag

धान की उपज में वृद्धि के लिए सिलिकॉन का महत्व Silicon (Si) is next to oxygen (O) in quantity on earth’s crust. Silicon in combination with oxygen forms silicon dioxide (SiO2) which is also known as silica. About 87% of the earth’s surface is made up of silica. There are 200 over types of silicate rocks in nature. These include quartz and mica. The white mica is made up of silicon, potassium and aluminum whereas the black mica contains iron and magnesium. The original soil minerals are predominantly silicate compounds. The silicon in sand, silt, and clay is extremely insoluble and difficult to be absorbed by plant. However, under the reaction of soil microorganism and a process called hydration, a small portion of silicon in the form of silicic acids (H4SiO4) is weakly soluble and thus become available to plants. Differential Absorption of Silicon by Rice Plants Plants vary in their ability to absorb silicon. Plants that can absorb and accumulate silicon in their tissues are known as silicon accumulators. These plants can accumulate up to 4-7% of silicon in their foliage. In contrary, the silicon non-accumulators can only absorb and store 0.5-1.5% of silicon. In general, dicot plants contain low quantity of silicon. Rice exhibits the greatest uptake of silicic acid in the grass family....

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...

Silicone: A beneficial Ingredient for plants पोधो को अपना जीवन च्रक पूरा करने के लिए कुल १८ पोषक तत्वो की आवशकता होती हे। सिलिकॉन इन्ही में से एक आवश्यक पोषक तत्व हे। सिलिकॉन मुख्य रूप से पोधो की शक्ति और कठोरता को बढ़ाने तथा पोधो के ऊतकों में अपनी उच्च क्षमता के साथ जुडा हुवा हे। सिलिकॉन रक्षा प्रतिक्रिया तंत्र द्वारा पोधो में आने वाले रोगों के प्रति प्रतिरोधक शक्ति को बढ़ाने में सक्रिय भूमिका निभाता है। यह कई पौधों मे आनुवंशिक रूप से जैविक और अजैविक तनाव दूर करने के लिए भी लाभदायक हे। सिलिकॉन का संक्षिप्त इतिहास सिलिकॉन मिट्टी में ऑक्सीजन के बाद दूसरा सबसे ज्यादा मात्रा में पाये जाने वाला तत्व है। सिलिकॉन डाइऑक्साइड मिट्टी द्रव्यमान का 50-70% भाग हैं। हालांकि पौधों की वृद्धि और विकास में सिलिकॉन की भूमिका 20 वीं सदी की शुरुआत तक अनदेखी की गई थी। क्योंकि प्रकृति में सिलिकॉन की कमी या विषाक्तता के लक्षण स्पष्ट नहीं दिखाई दे रहे थे, सिलिकॉन की बहुतायत के कारण, पोध-वेघानिको ने काफी हद तक इसे नजरअंदाज कर दिया था। नाइट्रोजन, फास्फोरस और पोटेशियम के रूप में रासायनिक उर्वरकों की लगातार मांग के कारण मिट्टी में सिलिकॉन की उपलब्धता समाप्त हो चुकी थी। मिट्टी में सिलिकॉन की कमी के बारे में जागरूकता अब सीमित नहीं समझी जाती हे। सिलिकॉन पौधों की वृद्धि, विकास,...

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...