Types of dams, geological considerations in site selection, Competency of Rocks to offer stable dam foundation, effect of geological structures on dam, selection of dam site, Reservoir, purpose of reservoir, influence of water table, geological structures, life of reservoir, geophysical studies
It includes the definition, properties, classification of groundwater with appropriate examples and figures in details. It also deals about the formation of groundwater. The properties of aquifers (all of 7) are described here in details with figures and mathematical terms.
It covers seismic method, gravity method, electromagnetic method, magnetic method and radiometric method. all these methods help in mineral exploration
Types of dams, geological considerations in site selection, Competency of Rocks to offer stable dam foundation, effect of geological structures on dam, selection of dam site, Reservoir, purpose of reservoir, influence of water table, geological structures, life of reservoir, geophysical studies
It includes the definition, properties, classification of groundwater with appropriate examples and figures in details. It also deals about the formation of groundwater. The properties of aquifers (all of 7) are described here in details with figures and mathematical terms.
It covers seismic method, gravity method, electromagnetic method, magnetic method and radiometric method. all these methods help in mineral exploration
Hjulstrom Curve(Terms)
1. Capacity: largest amount (weight) of debris that the river can carry.
2. Competence: diameter of the largest particles (size) that can be carried.
3. Critical erosion velocity: lowest velocity at which grain of a given size can be moved.
4. Settling/fall velocity: velocity falls below certain level particle (fall velocity) will be deposited.
Hjulstrom Curve
The Hjulstrøm curve is a graph used by hydrologists to determine whether a river will erode, transport, or deposit sediment.
The Hjulstrom curve is a graph that shows the relationship between the velocity of a river and the particle sizes that may be transported.
It shows the velocity needed to pick up material of a certain size (velocity needed for erosion to take place), and the settling velocity when deposition will occur.
Interpretation of the Hjulstrom curve/graph.
The x-axis shows the size of the particles in mm.
The y-axis shows the velocity of the river in cm/s.
Hjulstrom graph shows relationship between stream velocity and ability to transport materials of varying sizes. (i.e. finest
particles; clay & silt to largest boulders)
There are two curves lines drawn in a Hjulstrom curve; critical erosion velocity and settling or fall velocity.
Borehole geophysics is the science of recording and analyzing measurements of physical properties made in wells or test holes. Probes that measure different properties are lowered into the borehole to collect continuous or point data that is graphically displayed as a geophysical log. Multiple logs typically are collected to take advantage of their synergistic nature--much more can be learned by the analysis of a suite of logs as a group than by the analysis of the same logs individually. Borehole geophysics is used in ground-water and environmental investigations to obtain information on well construction, rock lithology and fractures, permeability and porosity, and water quality. The geophysical logging system consists of probes, cable and drawworks, power and processing modules, and data recording units. State-of-the-art logging systems are controlled by a computer and can collect multiple logs with one pass of the probe
A pumping test is a field experiment in which a well is pumped at a controlled rate and water-level response (drawdown) is measured in one or more surrounding observation wells and optionally in the pumped well (control well) itself; response data from pumping tests are used to estimate the hydraulic properties of aquifers, evaluate well performance and identify aquifer boundaries.
Hjulstrom Curve(Terms)
1. Capacity: largest amount (weight) of debris that the river can carry.
2. Competence: diameter of the largest particles (size) that can be carried.
3. Critical erosion velocity: lowest velocity at which grain of a given size can be moved.
4. Settling/fall velocity: velocity falls below certain level particle (fall velocity) will be deposited.
Hjulstrom Curve
The Hjulstrøm curve is a graph used by hydrologists to determine whether a river will erode, transport, or deposit sediment.
The Hjulstrom curve is a graph that shows the relationship between the velocity of a river and the particle sizes that may be transported.
It shows the velocity needed to pick up material of a certain size (velocity needed for erosion to take place), and the settling velocity when deposition will occur.
Interpretation of the Hjulstrom curve/graph.
The x-axis shows the size of the particles in mm.
The y-axis shows the velocity of the river in cm/s.
Hjulstrom graph shows relationship between stream velocity and ability to transport materials of varying sizes. (i.e. finest
particles; clay & silt to largest boulders)
There are two curves lines drawn in a Hjulstrom curve; critical erosion velocity and settling or fall velocity.
Borehole geophysics is the science of recording and analyzing measurements of physical properties made in wells or test holes. Probes that measure different properties are lowered into the borehole to collect continuous or point data that is graphically displayed as a geophysical log. Multiple logs typically are collected to take advantage of their synergistic nature--much more can be learned by the analysis of a suite of logs as a group than by the analysis of the same logs individually. Borehole geophysics is used in ground-water and environmental investigations to obtain information on well construction, rock lithology and fractures, permeability and porosity, and water quality. The geophysical logging system consists of probes, cable and drawworks, power and processing modules, and data recording units. State-of-the-art logging systems are controlled by a computer and can collect multiple logs with one pass of the probe
A pumping test is a field experiment in which a well is pumped at a controlled rate and water-level response (drawdown) is measured in one or more surrounding observation wells and optionally in the pumped well (control well) itself; response data from pumping tests are used to estimate the hydraulic properties of aquifers, evaluate well performance and identify aquifer boundaries.
A hydrograph is a graph showing the rate of flow (discharge) versus time past a specific point in a river, or other channel or conduit carrying flow. The rate of flow is typically expressed in cubic meters or cubic feet per second (cms or cfs)
1. Distribution of Runoff
2. Hydrograph Analysis
a) Hydrograph & Unit Hydrograph
b) S - Hydrograph & Synthetic Unit Hydrograph
3. Computation of Design Discharge
a) Rational Formulae
b) SCS Curve Number Method
4. Flood Frequency Analysis
5. Flood Routing
Write definitions for the following terms- hydrograph- hyetograph- abs.docxkarlynwih
Write definitions for the following terms: hydrograph, hyetograph, abstractions, losses, baseflow, and excess precipitation. Cite your source for this information.
Solution
1) A hydrograph is a graph showing the rate of flow (discharge) versus time past a specific point in a river, or other channel or conduit carrying flow. The rate of flow is typically expressed in cubic meters or cubic feet per second (cms or cfs)
2) A hyetograph is a graphical representation of the relationship between the rainfall intensity and time. It is the plot of the rainfall intensity drawn on the ordinate axis against time on the abscissa axis. The hyetograph is a bar diagram
3) Abstractions/losses – difference between total rainfall hyetograph and excess rainfall hyetograph
4) Losses :
i) Depression Storage: The volume of water contained in natural depressions in the land surface, such as puddles.
ii) Interception : The process by which precipitation is caught and held by foliage, twigs, and branches of trees, shrubs, and other vegetation, and lost by evaporation, never reaching the surface of the ground. Interception equals the precipitation on the vegetation minus stream-flow and through fall.
5) Base flow:
Stream-flow which results from precipitation that infiltrates into the soil and eventually moves through the soil to the stream channel. This is also referred to as ground water flow, or dry-weather flow.
6) The volume of water from precipitation that is available for direct runoff
Direct runoff is the sum of overland flow and inter flow (water flow in the top soil layer).
.
The analysis of all of the significant processes that formed a basin and deformed its sedimentary fill from basin-scale processes (e.g., plate tectonics)
to centimeter-scale processes (e.g., fracturing)
Seismic waves are the waves of energy caused by the sudden breaking of rock within the earth or an explosion.
Response of material to the arrival of energy fronts released by rupture.
Energy that travels through the earth and is recorded on seismographs.
A fossil is the preserved remains of a once-living organism.
Fossils give clues about organisms that lived long ago. They help to show that evolution has occurred.
They also provide evidence about how Earth’s surface has changed over time.
Fossils help scientists understand what past environments may have been like.
A fossil is an impression, cast,
original material or track of any animal or plant that is preserved in rock after the original organic material is transformed or removed.
Second-largest phylum in number of species- over 100,000 described.
Ecologically widespread- marine, freshwater, terrestrial (gastropods very successful on land)
Variety of body plans (therefore, many classes within the phylum)
Variety in body size- from ~1 mm to ~18 m (60 feet). 80% are under 5 cm, but many are large and therefore significant as food for man.
A synthetic gemstone is identical to a natural gemstone in almost every way.This includes the same basic crystal structure, refractive index, specific gravity, chemical composition, colors, and other characteristics. Since the same gemological tests are used for stone identification on both natural and synthetic gems, it is sometimes even possible for a gemologist to be puzzled as to whether or not a stone is natural or synthetic. When this occurs, the best course of action is to send the stone to an accredited gem laboratory, like the Gemological Institute of America. They can positively determin ewhether a stone is synthetic or naturally occuring. Only minor internal characteristics allow separation of a synthetic gemstone from a natural gemston
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
Seminar of U.V. Spectroscopy by SAMIR PANDASAMIR PANDA
Spectroscopy is a branch of science dealing the study of interaction of electromagnetic radiation with matter.
Ultraviolet-visible spectroscopy refers to absorption spectroscopy or reflect spectroscopy in the UV-VIS spectral region.
Ultraviolet-visible spectroscopy is an analytical method that can measure the amount of light received by the analyte.
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.
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.
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.
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/
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.
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/
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.
3. Definition.
“A hydrograph is a graph showing the rate
of flow versus time at a specific point in a
river, or other channel of flow.
Unit.
The rate of flow is typically expressed in
cubic meters or cubic feet per second (cms or
cfs).
4. Types of Hydrograph
Natural hydrograph
Unit hydrograph
Dimensionless unit hydrograph
Synthetic hydrograph
Dam breach hydrograph (Special case - natural or
synthetic)
5. Natural Hydrograph
A natural hydrograph is one recorded at a stream
gauging site and is a fingerprint of the upstream
drainage area's response to rainfall
6.
7. Unit Hydrograph
A unit hydrograph is a natural or synthetic hydrograph
representing one inch of runoff', uniformly from the
watershed during a specified time. In other words, the
area under the graph is actually a volume of one inch
of runoff.
8. Dimensionless Unit Hydrograph
A dimensionless unit hydrograph is a generic
combination of many natural unit hydrographs. The
ordinate and abscissa scales are ratios of the discharge
with respect to the peak discharge and the time
relative to the time ,to peak, respectively
9.
10. Synthetic Hydrograph
A synthetic hydrograph is calculated based on
watershed and storm characteristics.
(In SCS, soils, land use, vegetative cover, size, slope,
and time of concentration are important watershed
characteristics.)
Synthetic hydrographs are used to simulate natural
hydrographs for ungauged watersheds .
11.
12. Dam Breach Hydrograph
A dam breach hydrograph represents the sudden
release of water from the impoundment due to a
breach, followed by the draining of the reservoir.
The volume represented by the hydrograph is the
storage volume of the reservoir released during the
breach.
13.
14. Factors
Factors affecting the shape of the breach hydrograph
include:
size and shape of breach,
depth of water at the dam,
volume of stored water,
surface area of reservoir,
and shape (especially length) of reservoir.
A breach hydrograph can be natural (recorded) or
synthetic (a simulation)
15. Some Other Types of Hydro-graph
Storm Hydrographs
Flood Hydrographs
Annual Hydrographs.
16. Storm Hydrograph
“Storm hydrographs are graphs that show how a
drainage basin responds to a period of rainfall.”
They are useful in planning for….
Flood situations
Times of drought
It shows the variations in a river’s discharge over a
short period of time.
17.
18. Flood Hydrograph
“Flood hydrographs is a visual representation of the
variation in the stream or river depth over time.
Flooding normally occurs when the depth of the
stream exceeds the depth from the stream bank to the
stream bottom.”
19. Annual Hydrograph
“An annual hydrograph shows the average daily flow of
a river over the course of one year rather than a period
of hours”
It is affected by a number of controls depending on the
drainage basin concerned or the time of year.
Hydrographs provided a means for computing a runoff
hydrograph over a single drainage area based on the
curve number and SCS Unit Hydrograph methods.
20. Factors Affecting Hydrograph
The time distribution of runoff (the shape of the
hydrograph) is influenced by
Climatic conditions
Topographic and geological factors.
The climatic and topographic factors mainly affect the
“ Rising limb”
The geological factors determine the
“Recession limb”
21. Climatic factors
1) Rainfall intensity
2) Rainfall duration;
3) Distribution of rainfall on the basin;
4) Direction of storm movement;
5) Type of storm
22. Topographic and Geological Factors
1) Catchment size;
2) Catchment shape;
3) Distribution of watercourses;
4) Slope of the catchment;
5) Storage in the catchment;
6) Geology of the catchment;
7) Land use.
23. Why we use Hydrograph..??
Uses of Hydrographs include:
1. Watershed evaluations.
2. Design of structural works.
3. Flood plain management studies.
4. Emergency action plans.
5. Design of farm ponds.
6. Channel design.
7. Grade stabilization structures.