PRINCIPLES OF EROSION: Types of erosion, factors affecting erosion, effects of erosion on land fertility and land capability, estimation of soil loss due to erosion, Universal soil loss equation.
This presentation includes definition of Soil Erosion, Causes of Soil Erosion, Types of Soil Erosion, Agents of Soil Erosion, Factors Affecting Soil Erosion, Mechanics of Soil Erosion and
Ill Effects of Soil Erosion
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
This presentation includes definition of Soil Erosion, Causes of Soil Erosion, Types of Soil Erosion, Agents of Soil Erosion, Factors Affecting Soil Erosion, Mechanics of Soil Erosion and
Ill Effects of Soil Erosion
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
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
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.
Water Erosion Control Measures- Agricultural Lands.pptxAjay Singh Lodhi
This presentation describes about agronomical measures to control water erosion. It includes Crop rotation, crop cover, contour cultivation, strip cropping and mulch tillage practices.
CHARACTERISTICS OF WATERSHED: size, shape; physiography, slope, climate, drainage, land use, vegetation, geology and soils, hydrology and hydrogeology, socio-economic characteristics, basic data on watersheds.
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.
Stream flow representing the runoff phase of the hydrologic cycle is the most important basic data for hydrologic studies. Runoff is generated by rainstorms. Its occurrence and quantity are dependent on the characteristics of the rainfall event, i.e. intensity, duration and distribution. This module highlights about runoff components of the hydrological cycle.
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
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.
Water Erosion Control Measures- Agricultural Lands.pptxAjay Singh Lodhi
This presentation describes about agronomical measures to control water erosion. It includes Crop rotation, crop cover, contour cultivation, strip cropping and mulch tillage practices.
CHARACTERISTICS OF WATERSHED: size, shape; physiography, slope, climate, drainage, land use, vegetation, geology and soils, hydrology and hydrogeology, socio-economic characteristics, basic data on watersheds.
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.
Stream flow representing the runoff phase of the hydrologic cycle is the most important basic data for hydrologic studies. Runoff is generated by rainstorms. Its occurrence and quantity are dependent on the characteristics of the rainfall event, i.e. intensity, duration and distribution. This module highlights about runoff components of the hydrological cycle.
soil erosion is the one of the severe problem now a days. we should know about types of soil erosion , its effect on environment and how it to be prevented by various method..in these slides gives brief idea about types and erosion of soil erosion.
Water and wind erosion are natural processes that can cause the loss and movement of soil and sediment. Here's a brief description of each:
Water erosion: Water erosion occurs when rainfall or runoff flows over the land, picking up and carrying away soil particles. The intensity and duration of rainfall, the slope of the land, and the presence or absence of vegetation all contribute to the severity of water erosion. It can lead to the formation of gullies, rills, and streambank erosion, as well as the loss of fertile topsoil. Water erosion can have detrimental effects on agricultural lands, causing decreased soil fertility, reduced crop productivity, and sedimentation in water bodies.
Wind erosion: Wind erosion occurs when strong winds blow over bare or poorly protected soil surfaces, lifting and transporting soil particles. It typically affects areas with dry or arid climates and exposed soils lacking vegetation cover. Wind erosion can result in the formation of sand dunes, the removal of topsoil, and the deposition of sediment in unwanted areas. It can have significant consequences for agricultural productivity, damaging crops, reducing soil fertility, and causing desertification in severe cases.
Both water and wind erosion can be exacerbated by human activities such as deforestation, improper land management practices, overgrazing, and construction without adequate soil conservation measures. Effective erosion control measures include the implementation of erosion control structures, contour plowing, terracing, planting windbreaks or shelterbelts, establishing cover crops, and implementing proper water management techniques to minimize runoff.
A presentation on soil erosion conservation consisting of causes of erosion, need for soil conservation along with various prevention techniques for soil conservation.
Soil and water conservation engineering, water erosion, types of water erosion, splash erosion, sheet erosion, rill erosion, gully erosion, stream bank erosion, coastal erosion
Introduction to Data Science, Prerequisites (tidyverse), Import Data (readr), Data Tyding (tidyr),
pivot_longer(), pivot_wider(), separate(), unite(), Data Transformation (dplyr - Grammar of Manipulation): arrange(), filter(),
select(), mutate(), summarise()m
Data Visualization (ggplot - Grammar of Graphics): Column Chart, Stacked Column Graph, Bar Graph, Line Graph, Dual Axis Chart, Area Chart, Pie Chart, Heat Map, Scatter Chart, Bubble Chart
Overview and about R, R Studio Installation, Fundamentals of R Programming: Data Structures and Data Types, Operators, Control Statements, Loop Statements, Functions,
Descriptive Analysis using R: Maximum, Minimum, Range, Mean, Median and Mode, Variance, Standard Deviation, Quantiles, IQR, Summary
Introduction to Statistics -
Sampling Techniques, Types of Statistics, Descriptive Statistics,
Inferential Statistics,
Variables and Types of Data: Qualitative, Quantitative, Discrete,
Continuous, Organizing and Graphing Data: Qualitative Data, Quantitative Data
1. Angular Components:
Component Configuration, Building a Template, Using Constructors, Using External Templates, Angular Routing to Single Page Application (SPA)
2. Data Binding:
Introduction, Interpolation, Property Binding, Attribute Binding, Class Binding, Style Binding, Event Binding, Two-way Binding.
Topics:
1. Introduction to GIS
2. Components of GIS
3. Types of Data
4. Spatial Data
5. Non-Spatial Data
6. GIS Operations
7. Coordinate Systems
8. Datum
9. Map Projections
10. Raster Data Compression Techniques
11. GIS Software
12. Free GIS Data Resources
Topics:
1. Mapping Concepts
2. Analysis with paper based Maps
3. Limitations of Paper based Maps
4. Computer Aided Cartography History and Development
5. GIS Definition
6. Advantage of Digital Maps
Topics:
1. Introduction to Fluid Dynamics
2. Surface and Body Forces
3. Equations of Motion
- Reynold’s Equation
- Navier-Stokes Equation
- Euler’s Equation
- Bernoulli’s Equation
- Bernoulli’s Equation for Real Fluid
4. Applications of Bernoulli’s Equation
5. The Momentum Equation
6. Application of Momentum Equations
- Force exerted by flowing fluid on pipe bend
- Force exerted by the nozzle on the water
7. Measurement of Flow Rate
a). Venturimeter
b). Orifice Meter
c). Pitot Tube
8. Measurement of Flow Rate in Open Channels
a) Notches
b) Weirs
1. Introduction to Kinematics
2. Methods of Describing Fluid Motion
a). Lagrangian Method
b). Eulerian Method
3. Flow Patterns
- Stream Line
- Path Line
- Streak Line
- Streak Tube
4. Classification of Fluid Flow
a). Steady and Unsteady Flow
b). Uniform and Non-Uniform Flow
c). Laminar and Turbulent Flow
d). Rotational and Irrotational Flow
e). Compressible and Incompressible Flow
f). Ideal and Real Flow
g). One, Two and Three Dimensional Flow
5. Rate of Flow (Discharge) and Continuity Equation
6. Continuity Equation in Three Dimensions
7. Velocity and Acceleration
8. Stream and Velocity Potential Functions
E-Waste or Electronic Waste may be defined as discarded computers, office electronic equipment, entertainment device electronics, mobile phones, television sets and refrigerators. This definition includes used electronics which are destined for reuse, resale, salvage, recycling, or disposal.
Biomedical Waste is any kind of waste that contains infectious material (or material that’s potentially infectious). This definition includes waste generated by healthcare facilities like physician’s offices, hospitals, dental practices, laboratories, medical research facilities, and veterinary clinics
A workshop hosted by the South African Journal of Science aimed at postgraduate students and early career researchers with little or no experience in writing and publishing journal articles.
Exploiting Artificial Intelligence for Empowering Researchers and Faculty, In...Dr. Vinod Kumar Kanvaria
Exploiting Artificial Intelligence for Empowering Researchers and Faculty,
International FDP on Fundamentals of Research in Social Sciences
at Integral University, Lucknow, 06.06.2024
By Dr. Vinod Kumar Kanvaria
Strategies for Effective Upskilling is a presentation by Chinwendu Peace in a Your Skill Boost Masterclass organisation by the Excellence Foundation for South Sudan on 08th and 09th June 2024 from 1 PM to 3 PM on each day.
This slide is special for master students (MIBS & MIFB) in UUM. Also useful for readers who are interested in the topic of contemporary Islamic banking.
Safalta Digital marketing institute in Noida, provide complete applications that encompass a huge range of virtual advertising and marketing additives, which includes search engine optimization, virtual communication advertising, pay-per-click on marketing, content material advertising, internet analytics, and greater. These university courses are designed for students who possess a comprehensive understanding of virtual marketing strategies and attributes.Safalta Digital Marketing Institute in Noida is a first choice for young individuals or students who are looking to start their careers in the field of digital advertising. The institute gives specialized courses designed and certification.
for beginners, providing thorough training in areas such as SEO, digital communication marketing, and PPC training in Noida. After finishing the program, students receive the certifications recognised by top different universitie, setting a strong foundation for a successful career in digital marketing.
A review of the growth of the Israel Genealogy Research Association Database Collection for the last 12 months. Our collection is now passed the 3 million mark and still growing. See which archives have contributed the most. See the different types of records we have, and which years have had records added. You can also see what we have for the future.
Macroeconomics- Movie Location
This will be used as part of your Personal Professional Portfolio once graded.
Objective:
Prepare a presentation or a paper using research, basic comparative analysis, data organization and application of economic information. You will make an informed assessment of an economic climate outside of the United States to accomplish an entertainment industry objective.
2. Learning Objectives
1. Soil Erosion
a) Types of Erosion
b) Factors affecting Erosion
c) Effect of Erosion
d) Estimation of Soil Loss
2. Measures to Control Erosion
a) Contour Techniques
b) Ploughing
c) Furrowing
d) Trenching
e) Bunding
f) Terracing
g) Gully Control
h) Rock-fill Dams
i) Brushwood Dam
j) Gabion
3. Soil Erosion
Soil erosion is a naturally occurring process that affects all
landforms. In agriculture, soil erosion refers to the wearing away
of a field's topsoil by the natural physical forces of water and
wind or through forces associated with farming activities such as
tillage.
Erosion, whether it is by water, wind or tillage, involves three
distinct actions – soil detachment, movement and deposition.
4. Types of Erosion
1. Geologic Erosion
2. Accelerated Erosion
a) Wind Erosion
b) Water Erosion
i. Raindrop Erosion
ii. Rill Erosion
iii. Gully Erosion
iv. Bank Erosion
v. Sheet Erosion
vi. Landslide Erosion
c) Tillage Erosion
5. Geologic Erosion
It is a normal process, representing erosion of land in natural
environment. It is caused by the effect of
Rainfall
Run-off
Wind
Topography
Atmospheric temperatures
Gravitation Process
6. Accelerated Erosion
Accelerated erosion is due to man-made activities, which have
brought about changes in natural cover and soil condition. The
activities includes
Land Preparation for raising crops
Land Use patterns for building houses, infrastructures,
industries, hill cutting, deforestation, lack of soil conservation and
watershed management
7. Water Erosion
The impact of raindrops causes splash erosion
Run-off water causes scouring, scrapping and transport of
soil particles, leading to sheet, rill and gully erosion.
Flood water causes erosion of River Banks
Water waves cause erosion of bank and sides of reservoir,
lakes and oceans.
Subsurface seepage water causes soil boiling, erosion and
removal by piping.
Glacial erosion causes heavy landslides
8. Wind Erosion
It is primarily responsible for creation
and maintenance of desert areas.
Finer soil particles from top soil
along with organic matter and
nutrients are easily detachable and
removed by wind velocity.
Various factors affecting wind
erosion are wind velocity, rainfall,
temperature, humidity, soil texture,
organic matter content, water holding
capacity of soil, vegetation cover etc.,
12. Sheet Erosion
Sheet erosion is the movement
of soil from raindrop splash and
runoff water.
It typically occurs evenly over a
uniform slope and goes unnoticed
until most of the productive topsoil
has been lost.
Deposition of the eroded soil
occurs at the bottom of the slope
or in low areas.
13. Rill Erosion
In general, the sheet flow is carried out by
very small definable channels called interrill.
Raindrops detach every layer of soil particles
through splash and the detached particles are
then carried through interrills by a thin layer of
overland lateral flow.
When the process of soil erosion and
deposition through interrill is prolonged, the
interrills are widened, leading to formation of
small channels called rills.
Raindrop Erosion
14. Gully Erosion
Rills are usually smaller in size
and depth. They can be destroyed by
tillage operation.
If their occurrence is prolonged,
rills become larger in size and can
not be destroyed by tillage operation,
and they are transformed into
Gullies.
Large gullies and their networks
are called Ravines.
17. Factors Affecting Erosion
Climatic Factors
a) Rainfall
b) Rainfall Intensity
c) Runoff
d) Temperature
e) Wind
Characteristics of Soil
a) Texture
b) Structure & Cohesion
c) Particle Size
d) Organic Content
Vegetation Cover
Slope of Watershed
18. Effect of Erosion
Loss in Agricultural Production
Loss of Nutrients
Reduction of Infiltration Rates
Reduction in Water holding Capacity
Increased Cost in Tillage Operation
Floods may occur in Rivers
Decrease in useful life of Reservoir
Survival of Wild Life
Land Degradation
Cost of Removal of Sedimentation
Desertification
19. Estimation of Soil Loss
The Universal Soil Loss Equation (USLE) predicts the long-term average annual
rate of erosion on a field slope based on rainfall pattern, soil type, topography,
crop system and management practices.
USLE only predicts the amount of soil loss that results from sheet or rill erosion
on a single slope and does not account for additional soil losses that might occur
from gully, wind or tillage erosion.
This erosion model was created for use in selected cropping and management
systems, but is also applicable to non-agricultural conditions such as construction
sites.
This was developed by United States Department of Agriculture (USDA) in the
20. Estimation of Soil Loss
Universal Soil Loss Equation (USLE):
A = R.K.LS.C.P
Where
A = Average Annual Soil Loss due to Sheet and Pile Erosion in Tons per Hectare
per Year
R = Rainfall & Runoff factor based on Geographical Location
K = Soil Erodability Factor depends on Texture of Soil & Organic Content in Soil
LS = Length-Gradient Factor depends on Slope Length & Slope (%)
C = Crop Management Factor = Crop Type Factor x Tillage Method Factor
P = Erosion-Control-Practice Factor
Note: check tables at http://www.omafra.gov.on.ca/english/engineer/facts/12-