The document discusses different types of soils found in India. Alluvial soil is very fertile and found in places like Punjab, UP and Bengal, growing crops like rice, sugarcane and wheat. It is divided into Khadar soil near rivers and older Bangar soil in upper valleys. Black soil in central/south India is sticky and fertile, retaining moisture and good for cotton. Red soil contains iron and humus, found in places like Tamil Nadu and Odisha growing groundnuts and ragi. Laterite soil forms from erosion and lacks humus. Mountain soil content varies by location. Desert soil in places like Rajasthan is alkaline with little humus requiring irrigation. The diversity of soils in India results
Indian soils are generally divided into four broad types. These soil types are: 1) alluvial soils; 2) regular soils; 3) red soils and 4) laterite soils.
This is an introductory soil science presentation that I give to Master Gardeners, agribusiness personnel, farmers, and soil science students. Please feel free to contact me at andykleinschmidt@gmail.com with any comments regarding the presentation.
SOIL PROFILE DESCRIPTIONS
Soil profile descriptions are basic data in all soil surveys.
They provide a major part of the information required for
correlation and classification of the soils of an area. They are
essential for interpreting soils and for coordinating
interpretations across state and regional boundaries. The soil
descriptions and the soil map are very useful tools for developing a region in various sectors. For all applications, soil profile is the basic aspect to be understood. This module highlights the details of a soil profile.
Indian soils are generally divided into four broad types. These soil types are: 1) alluvial soils; 2) regular soils; 3) red soils and 4) laterite soils.
This is an introductory soil science presentation that I give to Master Gardeners, agribusiness personnel, farmers, and soil science students. Please feel free to contact me at andykleinschmidt@gmail.com with any comments regarding the presentation.
SOIL PROFILE DESCRIPTIONS
Soil profile descriptions are basic data in all soil surveys.
They provide a major part of the information required for
correlation and classification of the soils of an area. They are
essential for interpreting soils and for coordinating
interpretations across state and regional boundaries. The soil
descriptions and the soil map are very useful tools for developing a region in various sectors. For all applications, soil profile is the basic aspect to be understood. This module highlights the details of a soil profile.
Session two of the talk I gave in Pennsylvania on April 9th. This session covers season extension in the field as well as some warm season crops in the tunnels.
Different types of soil.Sandy Soil - This type has the biggest particles and the size of the particles does determine the degree of aeration and drainage that the soil allows. It is granular and consists of rock and mineral particles that are very small. Therefore the texture is gritty and sandy soil is formed by the disintegration and weathering of rocks such as limestone, granite, quartz and shale. Sandy soil is easier to cultivate if it is rich in organic material but then it allows drainage more than is needed, thus resulting in over-drainage and dehydration of the plants in summer.
Exposes the elementary science student to the idea there are three major kinds of soil found on earth as well as the very important remains of dead plants and animals called humus. Discusses soil and humus along with as some of the properties of each.
Soil has evolved over millions of years and is an important natural resource.
Soils in India can be classified as - Alluvial, Black, Red and Laterite soils. Their distribution, composition, characteristics such as color, texture, minerals, crops grown and it's conservation have been described.
Cancer cell metabolism: special Reference to Lactate PathwayAADYARAJPANDEY1
Normal Cell Metabolism:
Cellular respiration describes the series of steps that cells use to break down sugar and other chemicals to get the energy we need to function.
Energy is stored in the bonds of glucose and when glucose is broken down, much of that energy is released.
Cell utilize energy in the form of ATP.
The first step of respiration is called glycolysis. In a series of steps, glycolysis breaks glucose into two smaller molecules - a chemical called pyruvate. A small amount of ATP is formed during this process.
Most healthy cells continue the breakdown in a second process, called the Kreb's cycle. The Kreb's cycle allows cells to “burn” the pyruvates made in glycolysis to get more ATP.
The last step in the breakdown of glucose is called oxidative phosphorylation (Ox-Phos).
It takes place in specialized cell structures called mitochondria. This process produces a large amount of ATP. Importantly, cells need oxygen to complete oxidative phosphorylation.
If a cell completes only glycolysis, only 2 molecules of ATP are made per glucose. However, if the cell completes the entire respiration process (glycolysis - Kreb's - oxidative phosphorylation), about 36 molecules of ATP are created, giving it much more energy to use.
IN CANCER CELL:
Unlike healthy cells that "burn" the entire molecule of sugar to capture a large amount of energy as ATP, cancer cells are wasteful.
Cancer cells only partially break down sugar molecules. They overuse the first step of respiration, glycolysis. They frequently do not complete the second step, oxidative phosphorylation.
This results in only 2 molecules of ATP per each glucose molecule instead of the 36 or so ATPs healthy cells gain. As a result, cancer cells need to use a lot more sugar molecules to get enough energy to survive.
Unlike healthy cells that "burn" the entire molecule of sugar to capture a large amount of energy as ATP, cancer cells are wasteful.
Cancer cells only partially break down sugar molecules. They overuse the first step of respiration, glycolysis. They frequently do not complete the second step, oxidative phosphorylation.
This results in only 2 molecules of ATP per each glucose molecule instead of the 36 or so ATPs healthy cells gain. As a result, cancer cells need to use a lot more sugar molecules to get enough energy to survive.
introduction to WARBERG PHENOMENA:
WARBURG EFFECT Usually, cancer cells are highly glycolytic (glucose addiction) and take up more glucose than do normal cells from outside.
Otto Heinrich Warburg (; 8 October 1883 – 1 August 1970) In 1931 was awarded the Nobel Prize in Physiology for his "discovery of the nature and mode of action of the respiratory enzyme.
WARNBURG EFFECT : cancer cells under aerobic (well-oxygenated) conditions to metabolize glucose to lactate (aerobic glycolysis) is known as the Warburg effect. Warburg made the observation that tumor slices consume glucose and secrete lactate at a higher rate than normal tissues.
Richard's entangled aventures in wonderlandRichard Gill
Since the loophole-free Bell experiments of 2020 and the Nobel prizes in physics of 2022, critics of Bell's work have retreated to the fortress of super-determinism. Now, super-determinism is a derogatory word - it just means "determinism". Palmer, Hance and Hossenfelder argue that quantum mechanics and determinism are not incompatible, using a sophisticated mathematical construction based on a subtle thinning of allowed states and measurements in quantum mechanics, such that what is left appears to make Bell's argument fail, without altering the empirical predictions of quantum mechanics. I think however that it is a smoke screen, and the slogan "lost in math" comes to my mind. I will discuss some other recent disproofs of Bell's theorem using the language of causality based on causal graphs. Causal thinking is also central to law and justice. I will mention surprising connections to my work on serial killer nurse cases, in particular the Dutch case of Lucia de Berk and the current UK case of Lucy Letby.
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.
Observation of Io’s Resurfacing via Plume Deposition Using Ground-based Adapt...Sérgio Sacani
Since volcanic activity was first discovered on Io from Voyager images in 1979, changes
on Io’s surface have been monitored from both spacecraft and ground-based telescopes.
Here, we present the highest spatial resolution images of Io ever obtained from a groundbased telescope. These images, acquired by the SHARK-VIS instrument on the Large
Binocular Telescope, show evidence of a major resurfacing event on Io’s trailing hemisphere. When compared to the most recent spacecraft images, the SHARK-VIS images
show that a plume deposit from a powerful eruption at Pillan Patera has covered part
of the long-lived Pele plume deposit. Although this type of resurfacing event may be common on Io, few have been detected due to the rarity of spacecraft visits and the previously low spatial resolution available from Earth-based telescopes. The SHARK-VIS instrument ushers in a new era of high resolution imaging of Io’s surface using adaptive
optics at visible wavelengths.
A brief information about the SCOP protein database used in bioinformatics.
The Structural Classification of Proteins (SCOP) database is a comprehensive and authoritative resource for the structural and evolutionary relationships of proteins. It provides a detailed and curated classification of protein structures, grouping them into families, superfamilies, and folds based on their structural and sequence similarities.
(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.
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.
Earliest Galaxies in the JADES Origins Field: Luminosity Function and Cosmic ...
Soil ppt
1.
2. ALLUVIAL SOIL
• Alluvial soil is seen in many parts of the country. Their fertility
is also different at different places. Such soil is very fertile. It is
found in Punjab, Uttar Pradesh, Bihar, West Bengal etc.
• Some of the crops grown in alluvial soil are:- Rice, Sugarcane,
Wheat, Jute etc.
• It can be divided into two parts:-
1. Khadar:- The soil formed due to fresh alluvial deposit is known
as Khadar Soil. This soil is formed due to the river floods, it is
found mostly nearby the river. Generally such soil is sandy.
2. Bangar:- Soil containing old alluvium in the upper valley region
of a river is called Bangar Soil. It is sticky and has dark color.
3.
4. BLACK SOIL
• This soil is mostly found in Maharashtra, western Madhya
Pradesh, Gujarat, Karnataka, Andhra Pradesh, Telangana and
Tamil Nadu.
• Black soil is the gift of peninsular plateau.
• This soil is very sticky and fertile.
• It can contain humidity for a prolonged time.
• It is formed from the metamorphic rocks and is very useful for
cotton cultivation.
• That is why it has become famous as black cotton soil.
• It is also known as regur soil.
5.
6. RED SOIL
• Such soil is found in regions of igneous and metamorphic
rocks.
• Its red colour is due to its ferrous and other humus
contents.
• The soil is porous and fertile.
• Such soil is seen in Goa, Tamil Nadu, Andhra Pradesh,
Odisha and Jharkhand.
• Some crops grown in the red soil are:- Groundnut, Ragi,
Tobacco, etc.
7.
8. LATERITE SOIL
• Laterite soil develops as a result of excessive
erosion by rain.
• Due to heavy rain, the humus contents from the
top soil descend into the lower strata which is
called leaching.
• As the soil contains less humus,it is fertile.
• Such soil is found in mountainous region of
Deccan, Karnataka, Kerala, Odisha, and some
parts of North – East .
9.
10. MOUNTAIN SOIL
• Humus content is more due to the forests,
although it differs from place to place.
• Such soil on Shivalik Range is less fertile and less
developed.
• The soil is sandy and porous and does not contain
humus.
• Such soil is found in the mountainous region of
the country, such as in Himachal Pradesh,
Arunachal Pradesh, Jammu – Kashmir states.
11.
12. DESERT SOIL
• Such soil is found in the arid and semi-arid regions
of Gujarat, Rajasthan, Punjab, and Haryana.
• The soil here is more alkaline and has less humus
contents.
• Agriculture has been made possible in such soil only
through irrigation.
• Thus , a large diversity in soils of the nation is seen
due to diversity in climate and relief features.