Soil is a mixture of minerals from rocks and organic material from living things that have died. It covers much of Earth's surface in layers, with topsoil near the surface containing more humus. Soil forms slowly over hundreds of years and provides nutrients and housing for plants and animals. Factors like wind, water, deforestation, and overgrazing can cause soil erosion, removing the nutrient-rich topsoil. Conservation efforts like afforestation, terrace farming, and building dams can help prevent soil erosion.
This ppt explains the different adaptations of plants and the types based on the habitat. This also explains two types of plants - terrestrial plants and aquatic plants along with the adaptations of plants to live in a particular habitat.
SOIL EROSION AND CONSERVATION Copy.pptxDAMINI SAHA
It is my very fast ppt presentation. I gathered all the information from internet. Hope this will helps you to understand the whole topic in simple manner.
This ppt explains the different adaptations of plants and the types based on the habitat. This also explains two types of plants - terrestrial plants and aquatic plants along with the adaptations of plants to live in a particular habitat.
SOIL EROSION AND CONSERVATION Copy.pptxDAMINI SAHA
It is my very fast ppt presentation. I gathered all the information from internet. Hope this will helps you to understand the whole topic in simple manner.
Soil conservation problems and their managementChiter Mani
It discusses about how soil is degraded,what are the majors factors for soil degradation,problems occuring due to poor management of soil and soil management through different techniques.
This presentation explores a brief idea about the structural and functional attributes of nucleotides, the structure and function of genetic materials along with the impact of UV rays and pH upon them.
Salas, V. (2024) "John of St. Thomas (Poinsot) on the Science of Sacred Theol...Studia Poinsotiana
I Introduction
II Subalternation and Theology
III Theology and Dogmatic Declarations
IV The Mixed Principles of Theology
V Virtual Revelation: The Unity of Theology
VI Theology as a Natural Science
VII Theology’s Certitude
VIII Conclusion
Notes
Bibliography
All the contents are fully attributable to the author, Doctor Victor Salas. Should you wish to get this text republished, get in touch with the author or the editorial committee of the Studia Poinsotiana. Insofar as possible, we will be happy to broker your contact.
DERIVATION OF MODIFIED BERNOULLI EQUATION WITH VISCOUS EFFECTS AND TERMINAL V...Wasswaderrick3
In this book, we use conservation of energy techniques on a fluid element to derive the Modified Bernoulli equation of flow with viscous or friction effects. We derive the general equation of flow/ velocity and then from this we derive the Pouiselle flow equation, the transition flow equation and the turbulent flow equation. In the situations where there are no viscous effects , the equation reduces to the Bernoulli equation. From experimental results, we are able to include other terms in the Bernoulli equation. We also look at cases where pressure gradients exist. We use the Modified Bernoulli equation to derive equations of flow rate for pipes of different cross sectional areas connected together. We also extend our techniques of energy conservation to a sphere falling in a viscous medium under the effect of gravity. We demonstrate Stokes equation of terminal velocity and turbulent flow equation. We look at a way of calculating the time taken for a body to fall in a viscous medium. We also look at the general equation of terminal velocity.
The ability to recreate computational results with minimal effort and actionable metrics provides a solid foundation for scientific research and software development. When people can replicate an analysis at the touch of a button using open-source software, open data, and methods to assess and compare proposals, it significantly eases verification of results, engagement with a diverse range of contributors, and progress. However, we have yet to fully achieve this; there are still many sociotechnical frictions.
Inspired by David Donoho's vision, this talk aims to revisit the three crucial pillars of frictionless reproducibility (data sharing, code sharing, and competitive challenges) with the perspective of deep software variability.
Our observation is that multiple layers — hardware, operating systems, third-party libraries, software versions, input data, compile-time options, and parameters — are subject to variability that exacerbates frictions but is also essential for achieving robust, generalizable results and fostering innovation. I will first review the literature, providing evidence of how the complex variability interactions across these layers affect qualitative and quantitative software properties, thereby complicating the reproduction and replication of scientific studies in various fields.
I will then present some software engineering and AI techniques that can support the strategic exploration of variability spaces. These include the use of abstractions and models (e.g., feature models), sampling strategies (e.g., uniform, random), cost-effective measurements (e.g., incremental build of software configurations), and dimensionality reduction methods (e.g., transfer learning, feature selection, software debloating).
I will finally argue that deep variability is both the problem and solution of frictionless reproducibility, calling the software science community to develop new methods and tools to manage variability and foster reproducibility in software systems.
Exposé invité Journées Nationales du GDR GPL 2024
What is greenhouse gasses and how many gasses are there to affect the Earth.moosaasad1975
What are greenhouse gasses how they affect the earth and its environment what is the future of the environment and earth how the weather and the climate effects.
Remote Sensing and Computational, Evolutionary, Supercomputing, and Intellige...University of Maribor
Slides from talk:
Aleš Zamuda: Remote Sensing and Computational, Evolutionary, Supercomputing, and Intelligent Systems.
11th International Conference on Electrical, Electronics and Computer Engineering (IcETRAN), Niš, 3-6 June 2024
Inter-Society Networking Panel GRSS/MTT-S/CIS Panel Session: Promoting Connection and Cooperation
https://www.etran.rs/2024/en/home-english/
Comparing Evolved Extractive Text Summary Scores of Bidirectional Encoder Rep...University of Maribor
Slides from:
11th International Conference on Electrical, Electronics and Computer Engineering (IcETRAN), Niš, 3-6 June 2024
Track: Artificial Intelligence
https://www.etran.rs/2024/en/home-english/
2. Soil is a mixture of minerals and organic material that covers
much of Earth’s surface. Minerals are bits of rock, and organic
material is the remains of living things that have died. Soil is not
as solid as rock. It has many small spaces, called pores, that hold
water and air. In some places on Earth, a thin layer of soil only 6
inches (15 centimeters) thick lies on top of rock. In other places,
though, soil may be hundreds of feet deep.
Introduction
3. The mineral part of soil forms from rocks. Such forces as
wind, water, and temperature changes break rocks down
into tiny particles, or bits. The smallest particles are called
clay. Medium-sized particles are called silt. The largest
particles are called sand. Different types of soil contain
different mixtures of clay, silt, and sand.
COMPOSITION
4.
5.
6.
7.
8. HUMUS
The organic part of soil forms when plants and animals die.
Their bodies decay, or break down, and mix with the rock
particles. The organic material, called humus, helps to form the
pores in the soil. It keeps the soil soft and loose. Humus also
provides the nutrients used by plants.
9.
10. SOIL FORMATION
Without soil, most life on Earth could not survive. Soil provides a
place for plants to grow. It holds water in place for their roots. It
contains nutrients, or food substances, needed for their growth. Soil
also provides a home for many animals and other living things.
Soil forms slowly. A layer of soil that is 1 inch (2.5 centimeters) thick
may take 500 to 1,000 years to form. For this reason it is important to
11.
12. LAYERS OF SOIL
Soil is made up of layers. The layers rest on solid
rock, called bedrock. A layer of broken rock rests on
the bedrock. Some of this rock may have gone into
forming the soil above. The soil above the broken
rock is called subsoil. Subsoil contains mostly
minerals and a small amount of humus. Only the
deepest plant roots reach the subsoil. The top layer
is called topsoil. Topsoil contains a lot of humus. It
is the layer where plants grow.
13.
14.
15. Soil erosion
It is a process in which the top fertile layer of soil is lost. Due to
soil erosion, the soil becomes less fertile. The top layer of soil is
very light which is easily carried away by wind and water. The
removal of topsoil by the natural forces is known as soil erosion.
18. Causes of soil erosion
Various agents, like wind, water, deforestation, overgrazing by cattle,
etc., cause soil erosion. The various factors of soil erosion are:
19. Wind
When strong winds blow, the topsoil along with the organic matter is
carried away by the wind. This happens more often when the land is
not covered with grass or plants. Such conditions are very common in
desert and semi-desert regions where strong winds blow very
frequently.
20. . Water
When it rains in the hilly areas, the soil gets washed away towards
the plains. The running water deposits the mineral-rich soil in the
riverbed and over the years this deposition of soil can change the
course of the river. This can lead to floods which cause the
destruction of life and property and leads to loss of soil fertility.
21. Overgrazing
When cattle is allowed to graze on the same field repeatedly, all the
available grass, including the roots are eaten by them. This loosens
the topsoil which is taken away by wind and flowing water, leading
to soil erosion.
22. Deforestation
Humans have taken land from the forest to cultivate in order to feed
the ever-increasing population and to build houses, industries, etc.
Cutting down of trees on a large scale for these purposes is
deforestation. The roots of trees hold the soil together, thus preventing
the soil from getting uprooted. When large areas of the forest are
cleared, the topsoil gets eroded by wind and flowing water.
23.
24. Prevention of soil erosion is also called conservation of
soil. The soil erosion can be prevented by the following
ways:
Soil conservation
25. Afforestation
Planting new trees and plants is afforestation. We live because
plants live. If the plants die, all living things will also die. Thus,
whenever trees are cut down new trees should be planted. Planting
26. Terrace Farming
In hilly areas, farming is done by cutting steps on the slopes of the hills.
This slows down the flow of water and soil removed from one step is
deposited on the next step. Thus, the soil is never completely lost. This
is terrace farming.
27. The cover of plants and trees around the field also
breaks the speed of strong winds and protects the soil
from being blown away.
28. Embankments
Big strong structure called embankments along the banks of the
river can protect fields from the floods. These embankments
prevent the fast overflowing rivers and rainwater from washing
away a huge amount of rich fertile soil.
29. Van Mahotsav
It is an annual tree planting festival started by the
Government of India. The aim of this programme is to create
awareness about the need for conservation of forest and soil.
30. Building Dams
Dams are built to prevent floods, which not only damage the crops but also
wash away the topsoil.