Skip to main content

Distribution and production of Wheat.

Top wheat producers in 2020 Country Millions of tonnes China 134.2 India 107.6 Russia 85.9 United States 49.7 Canada 35.2 France 30.1 Pakistan 25.2 Ukraine 24.9 Germany 22.2 Turkey 20.5 Wheat is widely cultivated cereal, spread from 57ºN to 47ºS latitude. Hence, wheat is cultivated and harvested throughout the year in one country or other. China, India, Russian federation, USA, France, Canada, Germany, Pakistan, Australia and Turkey are most important wheat growing countries. ECONOMIC IMPORTANCE Wheat is the world's number one cereal in area. Cultivation of wheat is as old as civilization. It is the first mentioned crop in Bible. Wheat is eaten in various forms by more than 1000 million people in the world. In India, it is second important staple food crop next to rice. In areas wheat is staple cereal food; it is eaten in the form of 'chapattis'. In areas where rice is the staple cereal food, wheat is eaten in the form of 'puris' or in the form of 'upma' (cooked from 'suji' or 'rawa'). In addition to this, wheat is also consumed in various other preparations such as 'dalia', 'halwa', 'sweet meals', etc. In most of the urban areas of the country, the use of backed leavened bread, flakes, cakes, biscuits, etc. is increasing at a fast rate. Besides staple food to human, wheat straw is a good source of feed for a large population of cattle in the country. SOIL AND CLIMATIC REQUIREMENT Soils with a clay loam or loam texture, good structure and moderate water holding capacity are ideal for wheat cultivation. Care should be taken to avoid very porous and excessively drained soils. Soil should be neutral in its reaction. Heavy soils with good drainage are suitable for wheat cultivation under dry conditions. These soils absorb and retain in rain water well. Heavy soils with poor structure and poor drainage are not suitable as wheat is sensible to water logging. Wheat can be successfully grown on lighter soils provided their water and nutrient holding capacities are improved. Climate Wheat has hardening ability after germination. It can germinate at temperature just above 4ºC. After germination it can withstand freezing temperatures by as low as -9.4ºC (Spring wheat) and as low as -31.6ºC (Winter wheat). Normal process starts above 5ºC under the presence of adequate sunlight. Wheat can be exposed to low temperature during vegetative and high temperature and long days during reproductive phases. Optimum temperature is 20-22ºC. Optimum temperature for vegetative stage is 16-22ºC. Temperature above 22ºC decreases the plant height, root length and tiller number. Heading is accelerated as temperature rose from 22 to 34ºC, but, retarded above 34ºC. At grain development stage, temperature of 25ºC for 4-5 weeks is optimum and above 25ºC reduces the grain weight. It is long day plant. Long day hastens the flowering and short day increase the vegetative period. But, after the release of photo-insensitive varieties, no issues of photo-sensitiveness.


Comments

Popular posts from this blog

Artisan Wells Basins

Artisan Wells and Basins Artesian wells are a type of well that harnesses the natural pressure of water trapped underground to force water to the surface without pumping. This phenomenon occurs in specific geological formations known as artesian basins . Key Terminologies and Concepts Aquifer: A geological formation that can store and transmit water. It is typically made up of porous rocks or sediments like sandstone or gravel. Confined Aquifer: An aquifer that is sandwiched between two impermeable layers (like clay or shale) that prevent water from escaping. Artesian Basin: A geological structure where a confined aquifer is tilted and has a recharge area at a higher elevation than the discharge area. This creates a pressure gradient that forces water to flow upwards. Potentiometric Surface: The theoretical level to which water would rise in a well drilled into an artesian aquifer if there were no restrictions. It is determined by the pressure head in the aquifer. Flowing Artesian

Ground Water

Groundwater Terminology, Concepts, and Facts Key Terms Aquifer: A geological formation that can store and transmit significant quantities of water. Water Table: The upper surface of the saturated zone in an aquifer. Recharge: The process of replenishing groundwater through precipitation or other sources. Discharge: The process of groundwater flowing out of an aquifer, typically into surface water bodies or through wells. Hydraulic Gradient: The slope of the water table. Darcy's Law: A law that describes the flow of groundwater through porous media. Permeability: The ability of a material to transmit water. Porosity: The amount of void space in a material. Concepts Groundwater Flow: Groundwater moves from areas of higher hydraulic head to areas of lower hydraulic head. Groundwater Contamination: The introduction of pollutants into groundwater. Groundwater Depletion: The excessive extraction of groundwater, leading to a decline in water table levels. Saltwater Intrusion:

Groundwater – Porosity and Permeability

Groundwater refers to the water that resides beneath the Earth's surface in the pores and crevices of rock, sediment, and soil. Two key properties that influence the movement and storage of groundwater are porosity and permeability: 1. Porosity:    - Definition: Porosity refers to the volume percentage of void spaces (pores or openings) in a geological material, such as soil or rock.    - Role: Porosity determines how much water a subsurface material can hold. It is a measure of the material's capacity to store water.    - Factors: Porosity is influenced by the size and arrangement of particles within the material. Highly porous materials have more void spaces, while less porous materials have fewer.    - Units: Porosity is expressed as a percentage, with 0% indicating complete solidity (no pore spaces) and 100% indicating complete void space. 2. Permeability:    - Definition: Permeability refers to the ability of a geological material to transmit fluids, such as water. It meas

Water harvesting

Water harvesting 

Aquifer

  1. Aquifers:    - Definition: Aquifers are rocks and soils that possess both porosity and permeability.    - Porosity: Refers to the presence of open spaces (pores) within the material.    - Permeability: Indicates the ability of the material to transmit fluids (water, in this context) through those pores. 2. Aquicludes:    - Definition: Aquicludes are rocks and soils that have porosity but lack permeability.    - Porosity: They contain open spaces, but...    - Permeability: ...are not conducive to the easy movement of fluids due to the lack of interconnected pathways. 3. Aquitards:    - Definition: Aquitards have porosity, but their permeability is limited.    - Porosity: They have open spaces...    - Limited Permeability: ...yet the movement of fluids is slower or restricted compared to aquifers due to lower permeability. 4. Aquifuge:    - Definition: Aquifuge rocks and soils have neither porosity nor permeability.    - No Porosity: They lack open spaces for water to be stored...