This document discusses soil bulk density, particle density, and porosity and factors that influence them. It defines each term and provides typical values. Bulk density is the weight of soil per unit volume and is affected by mineral content, organic matter, compaction, and depth. Particle density is the weight of soil solids per unit volume and is influenced by mineral and organic matter content. Porosity refers to pore space and is classified by pore size. Factors like texture, moisture, and compaction impact porosity. The relationship between bulk density, particle density, and porosity is expressed through equations calculating percent solid and pore space. An example calculation is provided.
THIS SLIDES SHOWS ABOUT THE KNOWLEDGE ABOUT THE HOW SOIL AIR ARE TRANSMITTED FROM ENVIRONMENT TO SOIL AND ALSO TEMPERATURE CONDUCTION AND CONVECTION AND RADIATION.
Introduction
enlist of problematic soil
Salt affected soil
Characteristic of salt affected soil
Comparison between salt affected soil
Reclamation of Saline soils
Reclamation of sodic soils
Reclamation of saline-sodic soils
Acidic soils
Reclamation of acidic soil
Acid Sulphate soils and its management
Calcareous soil
THIS SLIDES SHOWS ABOUT THE KNOWLEDGE ABOUT THE HOW SOIL AIR ARE TRANSMITTED FROM ENVIRONMENT TO SOIL AND ALSO TEMPERATURE CONDUCTION AND CONVECTION AND RADIATION.
Introduction
enlist of problematic soil
Salt affected soil
Characteristic of salt affected soil
Comparison between salt affected soil
Reclamation of Saline soils
Reclamation of sodic soils
Reclamation of saline-sodic soils
Acidic soils
Reclamation of acidic soil
Acid Sulphate soils and its management
Calcareous soil
Soil is the home of million of organisms. In agriculture, from seed to grain, soil is a prima factor. It also acts a medium to store water for plants and form of water in soil called soil moisture. Some parameters to check the soil moisture called soil moisture constants. So, soil and water relationship is essential in agriculture.
introduction about acidic soil and area distribution ,classification of acidic soil and source of acidic soil formation , characteristic of acid soil ,what are the impact on soil properties . Reclamation of acid soil , conclusion about acidic soil
describes the irrigation and irrigation requirements of different crops. this ppt also describes about different methods to measure the soil moisture availability.
QUALITY OF IRRIGATION WATER AND MANAGEMENT OF SALINE WATER FOR IRRIGATION
GOVARDHAN LODHA
Enroll. No. (160111017)
Department of Agronomy
M.Sc. (Ag) Agronomy 2nd semester
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
A soil is composed primarily of minerals which are produced from parent material that is weathered or broken into small pieces. Like the classification systems for plants and animals, the soil classification system contains several levels of details, from the most general to the most specific types. The most general level of classification system is the soil order, of which there are 12 major types. This module explains these classes.
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.
Tillage is the manipulation of soil with tools & implements for loosening the surface crust & bringing about conditions favorable for the germination of seeds and the growth of crops.
soil condition resulting from tillage
good Tilth - soft, friable & properly aerated
crop emergence, establishment, growth and development
easy infiltration of water & are retentive of moisture for satisfactory growth of plants
To prepare the seed bed to a satisfactory level which promotes good germination and establishment of the seedlings
To control weeds and improve close plant-soil interaction in the rooting zone.
To loosen the soil for easy penetration and proliferation
To remove the other sprouting materials in the soil
To modify the soil temperature
To break hard soil pans and improve drainage facilities
To manage the plant residues by incorporating into the soil or to retain on the top layer to reduce erosion.
To improve the physical conditions of the soil
To harvest rain water easily and soil erosion can be minimised.
To establish specific surface configurations for sowing, irrigation, drainage, etc.
To incorporate and mix applied fertilizers and manures into the soil.
To destroy the eggs and larvae of insects and their breeding places.
Soil is the home of million of organisms. In agriculture, from seed to grain, soil is a prima factor. It also acts a medium to store water for plants and form of water in soil called soil moisture. Some parameters to check the soil moisture called soil moisture constants. So, soil and water relationship is essential in agriculture.
introduction about acidic soil and area distribution ,classification of acidic soil and source of acidic soil formation , characteristic of acid soil ,what are the impact on soil properties . Reclamation of acid soil , conclusion about acidic soil
describes the irrigation and irrigation requirements of different crops. this ppt also describes about different methods to measure the soil moisture availability.
QUALITY OF IRRIGATION WATER AND MANAGEMENT OF SALINE WATER FOR IRRIGATION
GOVARDHAN LODHA
Enroll. No. (160111017)
Department of Agronomy
M.Sc. (Ag) Agronomy 2nd semester
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
A soil is composed primarily of minerals which are produced from parent material that is weathered or broken into small pieces. Like the classification systems for plants and animals, the soil classification system contains several levels of details, from the most general to the most specific types. The most general level of classification system is the soil order, of which there are 12 major types. This module explains these classes.
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.
Tillage is the manipulation of soil with tools & implements for loosening the surface crust & bringing about conditions favorable for the germination of seeds and the growth of crops.
soil condition resulting from tillage
good Tilth - soft, friable & properly aerated
crop emergence, establishment, growth and development
easy infiltration of water & are retentive of moisture for satisfactory growth of plants
To prepare the seed bed to a satisfactory level which promotes good germination and establishment of the seedlings
To control weeds and improve close plant-soil interaction in the rooting zone.
To loosen the soil for easy penetration and proliferation
To remove the other sprouting materials in the soil
To modify the soil temperature
To break hard soil pans and improve drainage facilities
To manage the plant residues by incorporating into the soil or to retain on the top layer to reduce erosion.
To improve the physical conditions of the soil
To harvest rain water easily and soil erosion can be minimised.
To establish specific surface configurations for sowing, irrigation, drainage, etc.
To incorporate and mix applied fertilizers and manures into the soil.
To destroy the eggs and larvae of insects and their breeding places.
The Physical Properties of the Soil
Inckuding,
1. Soil Texture
2. Soil Structure
3. Soil Color
4. Soil Density
5. Soil Porosity
6. Soil Consistence
7. Soil Temperature
Properties of Soil Agricultural and Water Availability Impa.docxwoodruffeloisa
Properties of Soil: Agricultural
and Water Availability Impacts
Investigation
Manual
ENVIRONMENTAL SCIENCE
Made ADA compliant by
NetCentric Technologies using
the CommonLook® software
Key
Personal protective
equipment
(PPE)
goggles gloves apron
follow
link to
video
photograph
results and
submit
stopwatch
required
warning corrosion flammable toxic environment health hazard
PROPERTIES OF SOIL: AGRICULTURAL AND WATER
AVAILABILITY IMPACTS
Overview
Earth’s soil plays a major role in the world’s agriculture and has a
substantial effect on water availability in a given area. In this inves-
tigation, students will analyze the natural porosity and particle size
of soil samples along with the chemical composition and profile of
different soil types.
Outcomes
• Examine the properties of soil and their effects on agriculture
and water availability.
• Describe and identify soil horizons based on their chemical and
physical composition.
• Distinguish between the particle sizes of three different types of
soil: sand, silt, and clay.
• Determine the porosity of different soil types.
• Analyze soil samples for a variety of nutrients to determine soil
fertility.
Time Requirements
Preparation ....................................................................... 5 minutes
Activity 1: Particle Size Distribution and Determination of Soil
Texture
Day 1 ...................... 20 minutes, then let sit for 24 hours
Day 2 ............................................................. 30 minutes
Activity 2: Porosity of Different Soil Types ...................... 60 minutes
Activity 3: pH Test Comparison of Soil Samples ............ 30 minutes
Activity 4: Nitrogen, Phosphorus, and Potash Test Comparisons of
Soil Samples
Day 1 ...................... 20 minutes, then let sit for 24 hours
Day 2 ............................................................. 60 minutes
2 Carolina Distance Learning
Table of Contents
2 Overview
2 Outcomes
2 Time Requirements
3 Background
10 Materials
11 Safety
11 Preparation
12 Activity 1
13 Activity 2
14 Activity 3
16 Submission
16 Disposal and Cleanup
17 Lab Worksheet
Background
Soil Horizons and Chemical Composition
The type of dirt that makes up the dry
surfaces of the earth has numerous effects on
humans and the environment, and vice versa.
Humans can modify the suitability of some
areas for agriculture based on prior land use.
The properties of soil also determine water
availability in a given area. Areas that contain the
most suitable soil for farming are often limited.
Certain properties of soil determine whether
an area is suitable for human activity. When
considering the properties of soil, its texture,
shape, particle aggregation, and suitability for
growth come to mind. These properties all play
a major role in determining the capability of an
area to retain water and air, which are necessary
f ...
This pdf is about the Schizophrenia.
For more details visit on YouTube; @SELF-EXPLANATORY;
https://www.youtube.com/channel/UCAiarMZDNhe1A3Rnpr_WkzA/videos
Thanks...!
Multi-source connectivity as the driver of solar wind variability in the heli...Sérgio Sacani
The ambient solar wind that flls the heliosphere originates from multiple
sources in the solar corona and is highly structured. It is often described
as high-speed, relatively homogeneous, plasma streams from coronal
holes and slow-speed, highly variable, streams whose source regions are
under debate. A key goal of ESA/NASA’s Solar Orbiter mission is to identify
solar wind sources and understand what drives the complexity seen in the
heliosphere. By combining magnetic feld modelling and spectroscopic
techniques with high-resolution observations and measurements, we show
that the solar wind variability detected in situ by Solar Orbiter in March
2022 is driven by spatio-temporal changes in the magnetic connectivity to
multiple sources in the solar atmosphere. The magnetic feld footpoints
connected to the spacecraft moved from the boundaries of a coronal hole
to one active region (12961) and then across to another region (12957). This
is refected in the in situ measurements, which show the transition from fast
to highly Alfvénic then to slow solar wind that is disrupted by the arrival of
a coronal mass ejection. Our results describe solar wind variability at 0.5 au
but are applicable to near-Earth observatories.
Slide 1: Title Slide
Extrachromosomal Inheritance
Slide 2: Introduction to Extrachromosomal Inheritance
Definition: Extrachromosomal inheritance refers to the transmission of genetic material that is not found within the nucleus.
Key Components: Involves genes located in mitochondria, chloroplasts, and plasmids.
Slide 3: Mitochondrial Inheritance
Mitochondria: Organelles responsible for energy production.
Mitochondrial DNA (mtDNA): Circular DNA molecule found in mitochondria.
Inheritance Pattern: Maternally inherited, meaning it is passed from mothers to all their offspring.
Diseases: Examples include Leber’s hereditary optic neuropathy (LHON) and mitochondrial myopathy.
Slide 4: Chloroplast Inheritance
Chloroplasts: Organelles responsible for photosynthesis in plants.
Chloroplast DNA (cpDNA): Circular DNA molecule found in chloroplasts.
Inheritance Pattern: Often maternally inherited in most plants, but can vary in some species.
Examples: Variegation in plants, where leaf color patterns are determined by chloroplast DNA.
Slide 5: Plasmid Inheritance
Plasmids: Small, circular DNA molecules found in bacteria and some eukaryotes.
Features: Can carry antibiotic resistance genes and can be transferred between cells through processes like conjugation.
Significance: Important in biotechnology for gene cloning and genetic engineering.
Slide 6: Mechanisms of Extrachromosomal Inheritance
Non-Mendelian Patterns: Do not follow Mendel’s laws of inheritance.
Cytoplasmic Segregation: During cell division, organelles like mitochondria and chloroplasts are randomly distributed to daughter cells.
Heteroplasmy: Presence of more than one type of organellar genome within a cell, leading to variation in expression.
Slide 7: Examples of Extrachromosomal Inheritance
Four O’clock Plant (Mirabilis jalapa): Shows variegated leaves due to different cpDNA in leaf cells.
Petite Mutants in Yeast: Result from mutations in mitochondrial DNA affecting respiration.
Slide 8: Importance of Extrachromosomal Inheritance
Evolution: Provides insight into the evolution of eukaryotic cells.
Medicine: Understanding mitochondrial inheritance helps in diagnosing and treating mitochondrial diseases.
Agriculture: Chloroplast inheritance can be used in plant breeding and genetic modification.
Slide 9: Recent Research and Advances
Gene Editing: Techniques like CRISPR-Cas9 are being used to edit mitochondrial and chloroplast DNA.
Therapies: Development of mitochondrial replacement therapy (MRT) for preventing mitochondrial diseases.
Slide 10: Conclusion
Summary: Extrachromosomal inheritance involves the transmission of genetic material outside the nucleus and plays a crucial role in genetics, medicine, and biotechnology.
Future Directions: Continued research and technological advancements hold promise for new treatments and applications.
Slide 11: Questions and Discussion
Invite Audience: Open the floor for any questions or further discussion on the topic.
Earliest Galaxies in the JADES Origins Field: Luminosity Function and Cosmic ...Sérgio Sacani
We characterize the earliest galaxy population in the JADES Origins Field (JOF), the deepest
imaging field observed with JWST. We make use of the ancillary Hubble optical images (5 filters
spanning 0.4−0.9µm) and novel JWST images with 14 filters spanning 0.8−5µm, including 7 mediumband filters, and reaching total exposure times of up to 46 hours per filter. We combine all our data
at > 2.3µm to construct an ultradeep image, reaching as deep as ≈ 31.4 AB mag in the stack and
30.3-31.0 AB mag (5σ, r = 0.1” circular aperture) in individual filters. We measure photometric
redshifts and use robust selection criteria to identify a sample of eight galaxy candidates at redshifts
z = 11.5 − 15. These objects show compact half-light radii of R1/2 ∼ 50 − 200pc, stellar masses of
M⋆ ∼ 107−108M⊙, and star-formation rates of SFR ∼ 0.1−1 M⊙ yr−1
. Our search finds no candidates
at 15 < z < 20, placing upper limits at these redshifts. We develop a forward modeling approach to
infer the properties of the evolving luminosity function without binning in redshift or luminosity that
marginalizes over the photometric redshift uncertainty of our candidate galaxies and incorporates the
impact of non-detections. We find a z = 12 luminosity function in good agreement with prior results,
and that the luminosity function normalization and UV luminosity density decline by a factor of ∼ 2.5
from z = 12 to z = 14. We discuss the possible implications of our results in the context of theoretical
models for evolution of the dark matter halo mass function.
(May 29th, 2024) Advancements in Intravital Microscopy- Insights for Preclini...Scintica Instrumentation
Intravital microscopy (IVM) is a powerful tool utilized to study cellular behavior over time and space in vivo. Much of our understanding of cell biology has been accomplished using various in vitro and ex vivo methods; however, these studies do not necessarily reflect the natural dynamics of biological processes. Unlike traditional cell culture or fixed tissue imaging, IVM allows for the ultra-fast high-resolution imaging of cellular processes over time and space and were studied in its natural environment. Real-time visualization of biological processes in the context of an intact organism helps maintain physiological relevance and provide insights into the progression of disease, response to treatments or developmental processes.
In this webinar we give an overview of advanced applications of the IVM system in preclinical research. IVIM technology is a provider of all-in-one intravital microscopy systems and solutions optimized for in vivo imaging of live animal models at sub-micron resolution. The system’s unique features and user-friendly software enables researchers to probe fast dynamic biological processes such as immune cell tracking, cell-cell interaction as well as vascularization and tumor metastasis with exceptional detail. This webinar will also give an overview of IVM being utilized in drug development, offering a view into the intricate interaction between drugs/nanoparticles and tissues in vivo and allows for the evaluation of therapeutic intervention in a variety of tissues and organs. This interdisciplinary collaboration continues to drive the advancements of novel therapeutic strategies.
Nutraceutical market, scope and growth: Herbal drug technologyLokesh Patil
As consumer awareness of health and wellness rises, the nutraceutical market—which includes goods like functional meals, drinks, and dietary supplements that provide health advantages beyond basic nutrition—is growing significantly. As healthcare expenses rise, the population ages, and people want natural and preventative health solutions more and more, this industry is increasing quickly. Further driving market expansion are product formulation innovations and the use of cutting-edge technology for customized nutrition. With its worldwide reach, the nutraceutical industry is expected to keep growing and provide significant chances for research and investment in a number of categories, including vitamins, minerals, probiotics, and herbal supplements.
1. Soil Bulk density, Particle
density and Porosity-Factors
influencing-significance
K. Maheshwaran, Asst.Prof. (SS&AC)
Sethu Bhaskara Agricultural College &
Research Foundation
2. Soil bulk density
Also termed as “Apparent specific gravity”
Weight per unit volume of soil
Mass/weight of soil
Bulk density = ------------------------ Mg m-3
Volume of soil
BD of Heavy textured soil is 1.0 – 1.6 Mg m-3
BD of Sandy soil is 1.2 – 1.7 Mg m-3
BD of Organic soil is 0.5 – 0.6 Mg m-3
BD of Normal soil ranges from 1.4 – 1.6 Mg m-3
3. Factors affecting Bulk density
Factors Affecting
Mineral matter More mineral content BD will be higher
Sandy soil more BD than Clay soil
Organic matter High OM content BD will be lower
Soil compaction Compacted soil have higher BD than loose
and porous soil
Soil depth BD will be increasing with sub surface soil
or increasing with depth lower soil
horizons due to lower OM content
Cultural practices Like OM addition, ploughing, loosening
the soil will lower the BD of soil
4. Particle density
Also termed as “Absolute specific gravity or True
density”
Mass or weight of soil
Particle density = ---------------------------------- Mg m-3
Volume of soil solids
PD of organic matter is 1.2 – 1.7 Mg m-3
PD of mineral soil is 2.60 – 2.75 Mg m-3
Normal PD of soil is 2.65 Mg m-3
5. Factors Affecting
Mineral matter More mineral content PD will be higher
such as haematite, limonite, zicon,
magnetite. PD in OM is very low
Organic matter High OM content PD will be lower
Clay and Sesqioxides Presence of high clay content and
sesquioxides decreasing PD by increase
aggregation
Soil depth PD will be increasing with sub surface soil
or increasing with depth lower soil
horizons due to lower OM content
Factors affecting Particle density
6. Porosity
A soil consist of that portion of the soil volume not
occupied by solids, either mineral or organic
Also called as “voids”
Pore space under field condition always occupied with
water and air at all times
Pore space indirectly influence the amount water & air
and indirectly control the plant growth & crop
production
7. Classification of soil pores based on size
Particulars Characteristics
Macro pores
Non capillary pores
•0.2 mm diameter
•Mostly in coarse textured soil such as
sand soil having more macro pores
than micro pores
•There is no restriction of air and
water movement
•Water holding capacity is very low
Micro pores
Capillary pores
•< 0.2 mm diameter
•Mostly in heavy textured soil such as
•Clay soil having more micro pores
than macro pores
•There is restriction of air & water
movement
•Water holding capacity is high
8. Factors affecting Porosity
Factors Affecting
Texture •Fine textured soil more porosity than
coarse textured soil
•Fine textured soil with 60% porosity, 50%
of micro pores and 10% of macro pores
•Coarse textured soil with 30% porosity,
25% of macro pores and 5% micro pores
Moisture content •Well aerated soil micro pores filled with
moisture and macro pores filled with air
•Water logged soil, micro and macro pores
filled with both water and air
Soil compaction •Compacted soil pores are get reduced due
to tightly arrangement of soil particles
results in poor aeration
9. Relationship between porosity and
densities of soil
Bulk density
% Solid space = X 100
Particle density
Bulk density
% Pore space =100 1-
Particle density
Both are expressed in terms of percentage %
10. Calculation
Soil sample taken from the field for determination
of bulk density. The measurement were: Calculate
the bulk density, solid space and pore space
a) Volume of soil= 73.6
b) Soil weight= 87.8 gm
c) Particle density= 2.65 Mg m-3