Agriculture Knowledge for Everyone

acidic soil Tag

रासायनि‍क रूप से वि‍कृत भारतीय मृदाओं का प्रबन्‍धन।  Chemical deterioration of soils is a type of soil degradation that involves loss of nutrients or organic matter, salinity, acidification, soil pollution and fertility decline. The removal of nutrients reduces the capacity of soils to support plant growth and crop production and causes acidification. In arid and semi-arid areas problems can arise due to accumulation of salts, which impedes the entry of water in plant roots. Chemical deterioration of soils is often also due to agricultural over exploitation, relying solely on replenishing nutrient losses through harvesting by artificial chemical fertilizers. Indiscriminate irrigation for getting higher yield has led to water logging; nutrient losses and increased salinity of lands threatened the sustainability of crop yields. The increasing salinization of thousands of hectares of cultivated lands with raised water table in many canal command areas is a serious threat and needs attention failing which a significant area may be rendered unproductive and unfit for cultivation. 1. Acid Soils: In India nearly 145 million hectares of lands are cultivated and a rough estimate indicates 48 million ha of soil is acidic in nature of which 25 m ha shows pH below 5.5 while about 23 m ha has pH between 5.6 and 6.5 (Bhat, et. al. 2007). Acid soils are characterized by low soil pH which varies from strongly acidic (4.5-5.5) to extremely acidic...

मृदा की अम्‍लता भारत में फसलोंत्‍पादन सीमि‍त करने का एक बडा कारक है। Soil reaction is a very important chemical property of the soil. It is measured in terms of pH. The soils having pH 7 are neutral in reaction and those below or above 7 are acidic or alkaline respectively. In neutral soils, satisfactory plant growth can be expected, provided all other agronomic practices are followed properly. But neither acid soils nor saline soils are suitable for most of the crops except a few tolerant ones. Acidity or salinity acts as a limiting factor in crop production. When the concentration of some elements which are naturally acidic in reaction, goes too high in the soil, soils become acid and their pH goes down below 7. These elements are basically hydrogen (H), aluminium (Al) and Iron (Fe). In fact, last two elements are not directly responsible for soil acidity but they have a tremendous potential to generate hydrogen ions (H+) in the soil  which are direct cause of acidity (ion is the minutes particles and electrically charged form of an element). The more the number of hydrogen ions in a solution, the greater will be its acidity and the lesser pH count. Therefore, the soils having hydrogen ions concentration above a reasonable limit...