wind erosion and its control measures, factor affecting wind erosion, mechanics of wind erosion, types of soil transportation, suspension, saltation and surface creep, windbreak, shelterbelt, sand duns
wind erosion and its control measures, factor affecting wind erosion, mechanics of wind erosion, types of soil transportation, suspension, saltation and surface creep, windbreak, shelterbelt, sand duns
describes the irrigation and irrigation requirements of different crops. this ppt also describes about different methods to measure the soil moisture availability.
IN this presentation cover Erosivity and erodibilty
Different methods to calculate soil loss.
Er. Gurpreet Singh
M.tech from PAU, Ludhiana
Assistant Prof.
Khalsa college.
Universal soil loss equation, soil loss estimation, factors of USLE, its use and limitation, soil loss measurement by multi slot divisor and coshocton wheel sampler
Soil water conservation methods in agricultureVaishali Sharma
This presentation includes introduction as well as all the methods in agriculture either engineering or agronomic measures used in conservation of soil and water against erosion or other deteriorative factors.
Tillage is the mechanical manipulation of soil with tools and implements for obtaining conditions ideal for seed germination, seedling establishment and growth of crops.
This presentation is only with respect to the Parasitic Weed and their management tactics, falling under the category of Specificity while classifying weeds.
Soil water movement
Soil water movement
Soil water movement
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This presentation includes description about water erosion, types of water erosion i.e. Raindrop erosion, Sheet erosion, Rill erosion, Gully erosion, Stream bank erosion, Sea-shore erosion Landslide/ slip erosion and Tunnel erosion.
describes the irrigation and irrigation requirements of different crops. this ppt also describes about different methods to measure the soil moisture availability.
IN this presentation cover Erosivity and erodibilty
Different methods to calculate soil loss.
Er. Gurpreet Singh
M.tech from PAU, Ludhiana
Assistant Prof.
Khalsa college.
Universal soil loss equation, soil loss estimation, factors of USLE, its use and limitation, soil loss measurement by multi slot divisor and coshocton wheel sampler
Soil water conservation methods in agricultureVaishali Sharma
This presentation includes introduction as well as all the methods in agriculture either engineering or agronomic measures used in conservation of soil and water against erosion or other deteriorative factors.
Tillage is the mechanical manipulation of soil with tools and implements for obtaining conditions ideal for seed germination, seedling establishment and growth of crops.
This presentation is only with respect to the Parasitic Weed and their management tactics, falling under the category of Specificity while classifying weeds.
Soil water movement
Soil water movement
Soil water movement
Soil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movementSoil water movement
This presentation includes description about water erosion, types of water erosion i.e. Raindrop erosion, Sheet erosion, Rill erosion, Gully erosion, Stream bank erosion, Sea-shore erosion Landslide/ slip erosion and Tunnel erosion.
Wind Erosion
Effects of Wind Erosion
Factors Affecting Wind Erosion
Mechanics of Wind Erosion
Estimation of Soil Loss Due to Wind Erosion
Wind Erosion Control Measures
Wind Breaks
Shelter Belts
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Quality defects in TMT Bars, Possible causes and Potential Solutions.PrashantGoswami42
Maintaining high-quality standards in the production of TMT bars is crucial for ensuring structural integrity in construction. Addressing common defects through careful monitoring, standardized processes, and advanced technology can significantly improve the quality of TMT bars. Continuous training and adherence to quality control measures will also play a pivotal role in minimizing these defects.
Automobile Management System Project Report.pdfKamal Acharya
The proposed project is developed to manage the automobile in the automobile dealer company. The main module in this project is login, automobile management, customer management, sales, complaints and reports. The first module is the login. The automobile showroom owner should login to the project for usage. The username and password are verified and if it is correct, next form opens. If the username and password are not correct, it shows the error message.
When a customer search for a automobile, if the automobile is available, they will be taken to a page that shows the details of the automobile including automobile name, automobile ID, quantity, price etc. “Automobile Management System” is useful for maintaining automobiles, customers effectively and hence helps for establishing good relation between customer and automobile organization. It contains various customized modules for effectively maintaining automobiles and stock information accurately and safely.
When the automobile is sold to the customer, stock will be reduced automatically. When a new purchase is made, stock will be increased automatically. While selecting automobiles for sale, the proposed software will automatically check for total number of available stock of that particular item, if the total stock of that particular item is less than 5, software will notify the user to purchase the particular item.
Also when the user tries to sale items which are not in stock, the system will prompt the user that the stock is not enough. Customers of this system can search for a automobile; can purchase a automobile easily by selecting fast. On the other hand the stock of automobiles can be maintained perfectly by the automobile shop manager overcoming the drawbacks of existing system.
Immunizing Image Classifiers Against Localized Adversary Attacksgerogepatton
This paper addresses the vulnerability of deep learning models, particularly convolutional neural networks
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introduce a novel volumization algorithm, which transforms 2D images into 3D volumetric representations.
When combined with 3D convolution and deep curriculum learning optimization (CLO), itsignificantly improves
the immunity of models against localized universal attacks by up to 40%. We evaluate our proposed approach
using contemporary CNN architectures and the modified Canadian Institute for Advanced Research (CIFAR-10
and CIFAR-100) and ImageNet Large Scale Visual Recognition Challenge (ILSVRC12) datasets, showcasing
accuracy improvements over previous techniques. The results indicate that the combination of the volumetric
input and curriculum learning holds significant promise for mitigating adversarial attacks without necessitating
adversary training.
Forklift Classes Overview by Intella PartsIntella Parts
Discover the different forklift classes and their specific applications. Learn how to choose the right forklift for your needs to ensure safety, efficiency, and compliance in your operations.
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Event Management System Vb Net Project Report.pdfKamal Acharya
In present era, the scopes of information technology growing with a very fast .We do not see any are untouched from this industry. The scope of information technology has become wider includes: Business and industry. Household Business, Communication, Education, Entertainment, Science, Medicine, Engineering, Distance Learning, Weather Forecasting. Carrier Searching and so on.
My project named “Event Management System” is software that store and maintained all events coordinated in college. It also helpful to print related reports. My project will help to record the events coordinated by faculties with their Name, Event subject, date & details in an efficient & effective ways.
In my system we have to make a system by which a user can record all events coordinated by a particular faculty. In our proposed system some more featured are added which differs it from the existing system such as security.
TECHNICAL TRAINING MANUAL GENERAL FAMILIARIZATION COURSEDuvanRamosGarzon1
AIRCRAFT GENERAL
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The A318, A319, A320 and A321 are twin-engine subsonic medium range aircraft.
The family offers a choice of engines
Industrial Training at Shahjalal Fertilizer Company Limited (SFCL)MdTanvirMahtab2
This presentation is about the working procedure of Shahjalal Fertilizer Company Limited (SFCL). A Govt. owned Company of Bangladesh Chemical Industries Corporation under Ministry of Industries.
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Presented at NUS: Fuzzing and Software Security Summer School 2024
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COLLEGE BUS MANAGEMENT SYSTEM PROJECT REPORT.pdfKamal Acharya
The College Bus Management system is completely developed by Visual Basic .NET Version. The application is connect with most secured database language MS SQL Server. The application is develop by using best combination of front-end and back-end languages. The application is totally design like flat user interface. This flat user interface is more attractive user interface in 2017. The application is gives more important to the system functionality. The application is to manage the student’s details, driver’s details, bus details, bus route details, bus fees details and more. The application has only one unit for admin. The admin can manage the entire application. The admin can login into the application by using username and password of the admin. The application is develop for big and small colleges. It is more user friendly for non-computer person. Even they can easily learn how to manage the application within hours. The application is more secure by the admin. The system will give an effective output for the VB.Net and SQL Server given as input to the system. The compiled java program given as input to the system, after scanning the program will generate different reports. The application generates the report for users. The admin can view and download the report of the data. The application deliver the excel format reports. Because, excel formatted reports is very easy to understand the income and expense of the college bus. This application is mainly develop for windows operating system users. In 2017, 73% of people enterprises are using windows operating system. So the application will easily install for all the windows operating system users. The application-developed size is very low. The application consumes very low space in disk. Therefore, the user can allocate very minimum local disk space for this application.
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2. • Wind erosion is the process of
detachment, transportation and deposition
of soil particles by the action of wind.
• It occurs in all parts of the world and is a
cause of serious soil deterioration.
• In India, Rajasthan has severe wind erosion
problem. A large part of the state is affected
by sand dune formation.
• Some parts of Gujarat, Punjab and Haryana
are also affected.
3. • Some parts of coastal areas also have
such problems.
• It most commonly occurs in the regions
where temperature and wind velocity are s
high, RH and rain fall are low
• soil is dry, loose and finely divided and
sandy
• soil surface is smooth and bare
4. • About 33 m.ha in India is affected by wind
erosion.
• This includes 23.49 m.ha of desert and
about 6.5 m.ha of coastal sands.
5. • Deforestation and intensive plowing are
the main causes of accelerated wind
erosion.
• It causes soil loss, and deterioration of soil
structure, nutrient and productivity
losses and air pollution.
6.
7. Factors Affecting Wind Erosion
• Climate, soil and vegetation are the major
factors affecting wind erosion at any
particular location.
• The climatic factors that affect the wind
erosion are the characteristics of wind
itself (velocity and direction) in addition to
the precipitation, humidity and
temperature.
8. • Soil moisture conditions, texture, structure,
density of particles, organic matter content
are the soil characteristics that influence
erosion by wind.
• The coarse textured sandy loam, loamy
sands and sands are more susceptible to
wind erosion while loam, silt loam, clay
loam and silty clay loam are relatively
resistant to wind erosion.
9. • 1. Tillage:
• As the soils are loosened by the excess
tillage the blowing wind removes finer
particles.
• On an untilled surface wind erosion is very
less in comparison to tilled surface.
10. • 2. Structure:
• Soils with single-grained structure
(structure less) is more prone to wind
erosion than aggregate structure.
• 3. Organic Matter Content:
• Soils with low organic matter have low
amounts of water stable aggregate thus
facilitating wind erosion.
11. • 4. Surface roughness:
• Rough ground surface is more resistant to
wind erosion than smooth one.
• Plant cover protects the soil as plant roots
help in binding the soil and make it less
susceptible to wind erosion.
12. • 5. Weather condition:
• Continuous dry weather will increase wind
erosion because soil particles are
loosened due to lack of moisture.
• In wet and moist soils the finer particles
are held together, hence, no danger of soil
erosion by wind.
• 6. Wind Velocity and Turbulence:
• The rate of wind movement, influence
erosion.
13. Threshold velocity: For each specific soil
type and surface condition there is a
minimum velocity required to move soil
particles. This is called the threshold
velocity.
Once this velocity is reached, the quantity
of soil moved is dependent upon the
particle size and wind velocity itself.
14. • The magnitude of the threshold velocity
varies with the soil conditions and nature
of the ground surface.
• For example, for the most erodible soils of
particle size about 0.1 mm; the required
threshold velocity is 16 km/h at a height of
30 cm above the ground.
15. Surface features like vegetation or other
artificial cover (mulching etc) have the
protective effect on wind erosion problem
as surface cover increases the roughness
over the land surface and thus reduces the
erosive wind force on the land surface.
16. Mechanics of Wind Erosion
The overall occurrence of wind erosion
could be described in three distinct
phases. These are:
1. Initiation of soil Movement
2. Transportation
3. Deposition
Movement of soil particles is caused by
wind forces exerted against or parallel to
the ground surface.
17. • The erosive wind is turbulent at all heights
except very close to the surface.
• The lowest velocity occurs close to the
ground and increases in proportion to the
logarithm of the height above the surface.
• The wind velocity gradient determines the
magnitude of force exerted.
• Movement of soil particles is initiated when
the pressure caused by the moving fluid
against the particle overcomes the force of
gravity and inertia.
18. • Initiation of Movement: The soil particles
are first detached from their place by the
action of wind.
• These detached particles are then ready
for movement by the wind forces.
• After this initiation of movement, soil
particles are moved or transported by
distinct mechanisms.
19. Transportation: The transportation of the
soil particles are of three distinct types and
occur depending upon size of the soil
particles.
Suspension, saltation, and surface
creep are the three types of soil movement
or transport which occur during wind
erosion.
.
20. • Deposition: Deposition of soil particles
occurs when the gravitational force is
greater than the forces holding the particle
in the air.
• This generally happens when there is a
decrease in the wind velocity caused by
vegetative or other physical barriers.
21. • Smallest detach into suspension
(<0.1 mm)
• medium move by saltation
(0.1 - 0.5 mm)
• large move by rolling and sliding (creep)
> 0.5 mm
25. • Suspension: It occurs when very fine dirt
and dust particles are lifted into the
atmosphere.
• These particles can be carried very high
and be transported over very long
distances in the atmosphere by the winds.
26. • Soil moved by suspension is the most
easiest to recognize among the three
forms of movement.
• The soil particles of less than 0.1 mm size
are subjected to suspension and around 3
to 40 % of soil weights are carried by the
suspension method of soil transport under
the wind erosion.
27. • Saltation: The major fraction of soil
moved by the wind is through the process
of saltation.
• Saltation movement is caused by the
pressure of the wind on soil particles as
well as by the collision of a particle with
other particles.
• Soil particles (0.1 to 0.5 mm) move in a
series of bounces and/or jumps.
28. • Soil particles moved in the process of
saltation can cause severe damage to the
soil surface and vegetation.
• They travel approximately four times
longer in distance than in height.
• When they strike the surface again they
either bounce back into the air or knock
other soil particles from the soil mass into
the air.
29. • Depending on soil type, about 50 to 75%
of the total weight of soil is carried in
saltation.
• The height of the jump varies with the size
and density of the soil particles, the
roughness of the soil surface, and the
velocity of the wind.
30. • Surface Creep: The large particles which
are too heavy to be lifted into the air are
moved through a process called surface
creep.
• In this process, the particles are rolled
across the surface.
• In this process the largest of the erosive
particles having diameters between 0.5 to
2 mm are transported and around 5 to
25% of the total soil weights are carried in
this fashion.
31. • The amount of soil moved/transported
depends on soil particles diameter and the
difference in threshold and actual wind
velocity.
• The mass of soil moved can be related to
the influencing parameters by the following
equation:
• Quantity of soil moved (V – Vth)3 / D0.5
• where V = wind velocity, Vth = threshold
velocity, and D = particle diameter.
36. • Crop residues left on the soil surface
protect the soil against wind erosion by
increasing the surface roughness.
• Maintaining mixtures of standing stalks
and crop residues on the soil surface is
the most effective practice to control wind
erosion.
• Wind erosion decreases in direct
proportion with the amount of residues
present on the soil surface.
37. • Residues reduce wind erosion by altering
the wind velocity profile near the soil
surface, by absorbing the wind energy,
and thereby increasing the threshold wind
velocity required to cause soil erosion
38. • Standing stalks are at least five times
more effective for controlling wind erosion
than flat residues.
• The effectiveness of standing stalks
depends on the number of stems, density
of stems, diameter of stems, etc.
• The slowly decomposing residue mulch
cover enhances formation of stable soil
aggregates and accumulation of soil
organic matter.
39. • Tillage Practices
• The tillage practices, such as ploughing
are importantly adopted for controlling
wind erosion.
• These practices should be carried out
before the start of wind erosion.
• Ploughing before the rainfall helps in
moisture conservation.
41. • Conservation Tillage
• Conservation tillage practices are important options
to conserve soil water and produce abundant
residues.
• No-till management is a conservation-effective
strategy to reduce wind erosion because it leaves
most of the residues and maintains an undisturbed
soil surface.
• It improves soil water storage, reduces evaporation.
• Moist soils are less susceptible to erosion.
• A combination of reduced tillage and crop residue
management is an option in arid and semiarid
regions to reduce wind erosion while maintaining
crop production.
42. Mechanical Measures
• This method consists of some mechanical
obstacles, constructed across the prevailing
wind, to reduce the impact of blowing wind
on the soil surface.
• These obstacles may be fences, walls,
stone packing etc., either in the nature of
semi-permeable or permeable barriers.
• The semi-permeable barriers are most
effective, because they create diffusion and
eddying effects on their downstream face.
43. • Terraces and bunds also obstruct the wind
velocity and control the wind erosion to
some extent.
• Generally, in practice two types of
mechanical measures are adopted to
control the wind erosion; i) wind breaks
and ii) shelter belts.
44. • Modern techniques include
- contour ploughing
- terracing
- crop rotation
- shelter belt
45. Wind Breaks
• This is a permanent vegetative measure which
helps in the reduction of wind erosion. It is most
effective vegetative measure used for controlling
severe wind erosion.
• The term wind break is defined as any type of
barrier either mechanical or vegetative used for
protecting the areas like building apartments,
orchards or farmsteads etc. from blowing winds.
The wind break acts as fencing wall around the
affected areas, normally constructed by one row
or maximum up to two rows across the
prevailing wind direction.
49. • Shelter Belts
• A shelterbelt is a longer barrier than the
wind break, is installed by using more than
two rows, usually at right angle to the
direction of prevailing winds.
• The rows of belt can be developed by
using shrubs and trees.
• It is mainly used for the conservation of
soil moisture and for the protection of field
crops, against severe wind erosion.
50.
51. • Shelterbelt is more effective for reducing
the impact of wind movement than the
wind break.
• Woodruff and Zingg (1952) developed the
following relationship between the
distance of full protection (d) and the
height (h) of wind break or shelter belt.
52. • Where, d is the distance of full protection
(m), h is the height of the wind barrier (wind
break or shelter belt) (m), vm is the minimum
wind velocity at 15 m height required to move
the most erodible soil fraction (m/s), v is the
actual velocity at 15 m height, and θ is the
angle of deviation of prevailing wind direction
from the perpendicular to the wind barrier.
• This relationship (equation) is valid only for
wind velocities below 18 m/s.
53. Solved Problem
Determine the spacing between
windbreaks that are 15 m high. 5 year
return period wind velocity at 15 m height
is 15.6 m/s and the wind direction deviates
10° from the perpendicular to the field
strip. Assume a smooth, bare soil surface
and a fully protected field.
54. Solution:
• Given: h = 15 m
• V = 15.6 m/s
• θ = 10°
Vm = 9.6 m/s (for smooth, bare soil surface)
Spacing = distance of full protection by a
windbreak,
• Spacing between windbreaks = 154.54 m.
55. • Determine the full protection strip width for
field strip cropping if the crop in the
adjacent strip is wheat, 0.9 m tall, and the
wind velocity at 15 m height is 8.9 m/sec
at 90° with the field strip.
56. • Solution:
• Given: h = 0.9 m
• v = 8.9 m/s
• θ = 0°
• Assuming vm = 8.9 m/sec (Because
theoretical vm = 9.6 m/sec which is greater
than the prevailing wind velocity). Since
the field conditions are not specified
takingvm = v.
• Full protection width-
• Thus, strip width = 15.30 m.
57. Constraints of Vegetative Barriers
• lack of tree/shrub materials
• lack of management guidelines
• absence of technical support, training, and fund
• high costs of establishment
• invasion of insects and pests
• attraction of birds which consume grains and
reduce yields
• competition of barriers with crops for light, water,
and nutrients
• difficulties in protection against grazing by
livestock