Showing posts with label Groundwater. Show all posts
Showing posts with label Groundwater. Show all posts

Factors affecting Choice & Selection of Irrigation Methods

Following are some reasons and factors which affect the selection of an irrigation system for a specific area:

Compatibility of the irrigation system:


The irrigation system for a field or a farm must be compatible with the other existing farm operations, such as land preparation, cultivation, and harvest.
  • Level of Mechanization
  • Size of Fields
  • Cultivation
  • Pest Control
The use of the large mechanized equipment requires longer and wider fields. The irrigation systems must not interfere with these operations and may need to be portable or function primarily outside the crop boundaries (i.e. surface irrigation systems).
Smaller equipment or animal-powered cultivating equipment is more suitable for small fields and more permanent irrigation facilities.

Topographical characteristics of area:


Topography is a major factor affecting irrigation, particularly surface irrigation. Of general concern are the location and elevation of the water supply relative to the field boundaries, the area and configuration of the fields, and access by roads, utility lines (gas, electricity, water, etc.), and migrating herds whether wild or domestic.

.Terraced Fields IrrigationPlain fields Irrigation

Field slope and its uniformity are two of the most important topographical factors. Surface systems, for instance, require uniform grades in the 0-5 percent range.

Restrictions on irrigation system selection due to topography include:
  • Groundwater levels
  • the location and relative elevation of the water source
  • field boundaries
  • acreage in each field
  • the location of roads
  • power and water lines and other obstructions
  • the shape and slope of the field

Economics and cost of the irrigation method:


The type of irrigation system selected is an important economic decision.
Some types of pressurized systems have high capital and operating costs but may utilize minimal labour and conserve water. Their use tends toward high value cropping patterns.
Other systems are relatively less expensive to construct and operate but have high labour requirements.
Some systems are limited by the type of soil or the topography found on a field.
The costs of maintenance and expected life of the rehabilitation along with an array of annual costs like energy, water, depreciation, land preparation, maintenance, labour and taxes should be included in the selection of an irrigation system.

Main costs include:
  • Energy
  • Water
  • Land Preparation
  • Maintenance
  • Labor
  • taxes

Soils:


The soil's moisture-holding capacity, intake rate and depth are the principal criteria affecting the type of system selected.
Sandy soils typically have high intake rates and low soil moisture storage capacities and may require an entirely different irrigation strategy than the deep clay soil with low infiltration rates but high moisture-storage capacities.
Sandy soil requires more frequent, smaller applications of water whereas clay soils can be irrigated less frequently and to a larger depth. Other important soil properties influence the type of irrigation system to use.

Soil Moisture CapacitySoil Depth Factor in Irrigation Method Selection

The physical, biological and chemical interactions of soil and water influence the hydraulic characteristics and filth. The mix of silt in a soil influences crusting and erodibility and should be considered in each design. The soil influences crusting and erodibility and should be considered in each design.
The distribution of soils may vary widely over a field and may be an important limitation on some methods of applying irrigation water.

The soil type usually defines:
  • Soil moisture-holding capacity
  • The intake rate
  • Effective soil depth

Water supply:


The quality and quantity of the source of water can have a significant impact on the irrigation practices. Crop water demands are continuous during the growing season. The soil moisture reservoir transforms this continuous demand into a periodic one which the irrigation system can service. A water supply with a relatively small discharge is best utilized in an irrigation system which incorporates frequent applications. The depths applied per irrigation would tend to be smaller under these systems than under systems having a large discharge which is available less frequently. The quality of water affects decisions similarly. Salinity is generally the most significant problem but other elements like boron or selenium can be important. A poor quality water supply must be utilized more frequently and in larger amounts than one of good quality.


Crops to be irrigated:


The yields of many crops may be as much affected by how water is applied as the quantity delivered. Irrigation systems create different environmental conditions such as humidity, temperature, and soil aeration. They affect the plant differently by wetting different parts of the plant thereby introducing various undesirable consequences like leaf burn, fruit spotting and deformation, crown rot, etc. Rice, on the other hand, thrives under ponded conditions.

Definition of Cash Crops:

Some crops have high economic value and allow the application of more capital-intensive practices, these are called "cash crops" or Cash crop farming. Deep-rooted crops are more amenable to low-frequency, high-application rate systems than shallow-rooted crops. Examples of cash crops are Rice, Wheat, Seed Oils, Tobacco, cotton, sugar cane, etc.

Crops Covered Wheat Cash Crop irrigationTea Cash Crop irrigation
Cash Crop Water Requirement

Crop characteristics that influence the choice of irrigation system are:
  • The tolerance of the crop during germination, development and maturation to soil salinity, aeration, and various substances, such as boron
  • The magnitude and temporal distribution of water needs for maximum production
  • The economic value of the crop

Social influences on the selection of irrigation method:


Beyond the confines of the individual field, irrigation is a community enterprise. Individuals, groups of individuals, and often the state must join together to construct, operate and maintain the irrigation system as a whole. Within a typical irrigation system there are three levels of community organization.

There is the individual or small informal group of individuals participating in the system at the field and tertiary level of conveyance and distribution. There are the farmer collectives which form in structures as simple as informal organizations or as complex as irrigation districts. These assume, in addition to operation and maintenance, responsibility for allocation and conflict resolution. And then there is the state organization responsible for the water distribution and use at the project level.

Irrigation system designers should be aware that perhaps the most important goal of the irrigation community at all levels is the assurance of equity among its members. Thus the operation, if not always the structure, of the irrigation system will tend to mirror the community view of sharing and allocation.

Irrigation often means a technological intervention in the agricultural system even if irrigation has been practiced locally for generations. New technologies mean new operation and maintenance practices. If the community is not sufficiently adaptable to change, some irrigation systems will not succeed.

External influences:


Conditions outside the sphere of agriculture affect and even dictate the type of system selected. For example, national policies regarding foreign exchange, strengthening specific sectors of the local economy, or sufficiency in particular industries may lead to specific irrigation systems being utilized. Key components in the manufacture or importation of system elements may not be available or cannot be efficiently serviced. Since many irrigation projects are financed by outside donors and lenders, specific system configurations may be precluded because of international policies and attitudes.

(Courtesy: http://www.aboutcivil.org/)

Seminar Topics

  1. Feasibility Of Drip Irrigation
  2. Methods Of Ground Water Recharge & It’s Effect On Quality Of Ground Water
  3. Technological Potential For Improvements Of Water Harvesting
  4. Coastal   Protection Structures
  5. Relevance Of Remote Sensing And GIS In Civil Engineering
  6. Surge Tanks
  7. Sewage Water As The Source Of Irrigation And Plant Nutrients
  8. Study Of Coastal Villages Affected By  Salinity Ingress In Amreli District
  9. Socio Economic Analysis Of The Kalpsar Project
  10. Soil Erosion And It’s Controlling Techniques
  11. Land Reclamation For Agricultural Purpose
  12. A Case Study On: Social And Environmental Impacts Of Sardar Sarovar Dam Project
  13. Advanced Technologies In Sewer Maintenance
  14. Review And Analysis Of Drought Monitoring And Management In India
  15. Digital Elevation Model
  16. Seminar On Subsurface Dams
  17. Impact Of Climate Change On Groundwater Resources
  18. Reclamation Of Waterlogged And Saline Soils For Agricultural Purpose
  19. Recycling Of Waste Water
  20. Importance of Liners For Canals
  21. Qyality Analysis Of Ground Water
  22. Qualitative Anlysis Of Irrigation Water
  23. Roof Rainwater Harvesting – A Case Study
  24. Groundwater Potential And Problems : A Case Study
  25. Rain Water Harvesting And Ground Water Conservation
  26. Interlinking Of Indian Rivers -Challenges And Prospects OR Interlinking Of Indian Rivers intrusion Detection System
  27. Surface Water Pre-treatment Using Floating Media Filter
  28. GIS – For Rain Water Recharge To Enhance The Ground Water
  29. Ground Water Conservation By Artificial Recharge Techniques
  30. Impact Of Urbanization On Groundwater Resources
  31. Application Of Remote Sensing & G.I.S. In Groundwater Prospecting
  32. Water Evaporation And Weeds Control By Mulching In Drip Irrigation System
  33. Sediment And Water Quality Analysis
  34. Remote Sensing , GIS And Its Applications
  35. Water Resources Development in Developing Countries
  36. Piano Key Spillways for Dams
  37. Proposed site for Bandhara In order to Raise Ground Water level.
  38. Fusegate System for Ungated Irrigation Scheme

The Hydrological Cycle

Introduction:

Earth's water is always in movement, and the natural water cycle, also known as the hydrological cycle, describes the continuous movement of water on, above, and below the surface of the Earth. Water is always changing states between liquid, vapor, and ice, with these processes happening in the blink of an eye and over millions of years.


This Information page provides an understanding of the hydrological cycle.  It describes the principal stages of the cycle, with a brief description of each stage.

Where is all the Earth’s water?

Water is the most widespread substance to be found in the natural environment and it is the source of all life on earth. Water covers 70% of the earth’s surface but it is difficult to comprehend the total amount of water when we only see a small portion of it. The distribution of water throughout the earth is not uniform. Some places have far more rainfall than others.


Notice how of the world's total water supply of about 332.5 million cubic miles of water, over 96 percent is saline. And, of the total freshwater, over 68 percent is locked up in ice and glaciers. Another 30 percent of freshwater is in the ground. Fresh surface-water sources, such as rivers and lakes, only constitute about 22,300 cubic miles (93,100 cubic kilometers), which is about 1/150th of one percent of total water. Yet, rivers and lakes are the sources of most of the water people use everyday.

The stages of the cycle are:
  • Evaporation
  • Transpiration
  • Condensation
  • Precipitation
  • Groundwater
  • Runoff



Water is transferred from the surface to the atmosphere through evaporation, the process by which water changes from a liquid to a gas. The sun’s heat provides energy to evaporate water from the earth’s surface. Land, lakes, rivers and oceans send up a steady stream of water vapour and plants also lose water to the air (transpiration).
Approximately 80% of all evaporation is from the oceans, with the remaining 20% coming from inland water and vegetation.

The release of water vapor from plants and soil into the air. Water vapor is a gas that cannot be seen.

The transported water vapour eventually condenses, forming tiny droplets in clouds.
The primary mechanism for transporting water from the atmosphere to the surface of the earth is precipitation.
When the clouds meet cool air over land, precipitation, in the form of rain, sleet or snow, is triggered and water returns to the land (or sea). A proportion of atmospheric precipitation evaporates.
Some of the precipitation soaks into the ground and this is the main source of the formation of the waters found on land - rivers, lakes, groundwater and glaciers.
Some of the underground water is trapped between rock or clay layers - this is called groundwater. Water that infiltrates the soil flows downward until it encounters impermeable rock and then travels laterally. The locations where water moves laterally are called ‘aquifers’. Groundwater returns to the surface through these aquifers, which empty into lakes, rivers and the oceans.
Under special circumstances, groundwater can even flow upward in artesian wells. The flow of groundwater is much slower than run-off with speeds usually measured in centimeters per day, meters per year or even centimeters per year.
Most of the water which returns to land flows downhill as run-off. Some of it penetrates and charges groundwater while the rest, as river flow, returns to the oceans where it evaporates. As the amount of groundwater increases or decreases, the water table rises or falls accordingly. When the entire area below the ground is saturated, flooding occurs because all subsequent precipitation is forced to remain on the surface.
Different surfaces hold different amounts of water and absorb water at different rates. As a surface becomes less permeable, an increasing amount of water remains on the surface, creating a greater potential for flooding. Flooding is very common during winter and early spring because frozen ground has no permeability, causing most rainwater and melt-water to become run-off.

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