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The document discusses speed-time graphs and how they represent different types of motion: no movement, constant speed, constant speed at different rates, acceleration, and constant acceleration. It provides examples of how speed-time graphs would appear for an object falling with constant acceleration due to gravity and notes that the area under the graph represents the distance traveled.
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Dt graphs
Dt graphsaimorales
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This document discusses distance-time graphs and how they represent different types of motion. A flat line indicates no movement, a straight line with a constant positive slope represents constant speed, and a steeper line represents faster constant speed while a more gradual line represents slower constant speed. The slope of the line directly corresponds to the speed of the object.Motion in a circle
Motion in a circleCatherine He
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Angular displacement (慮) is defined as the arc length (s) divided by the radius (r) of the arc. One radian is equal to an arc length that is equal to the radius. Angular velocity () is the rate of change of angular displacement with respect to time. It describes the change in angular displacement per unit time and has units of radians per second. For uniform circular motion, the angular velocity is constant. Centripetal acceleration is the acceleration experienced by an object moving in a circular path, directed toward the center. The centripetal force causing this acceleration is given by mv^2/r.One Direction Do Physics
One Direction Do PhysicsStephen Taylor
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This presentation is for my class to work through as teachers are on a series of PD days. It is based on a very bad One Direction joke cracked in a class about vectors. G10 Reproduction
G10 ReproductionBrad Kremer
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The document appears to be notes on biological concepts related to reproduction. It includes sections on asexual and sexual reproduction with examples, mitosis and the cell cycle, meiosis, sources of genetic variation, comparisons of mitosis and meiosis, and diagrams. The document provides information on key cellular processes important for understanding reproduction and sources of variation.Revision questions 2.2. Water 
Revision questions 2.2. Water Miltiadis Kitsos
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1. The document discusses the properties of water molecules and their ability to form hydrogen bonds. It explains how hydrogen bonding between polar water molecules gives rise to water's unique thermal, solvent and adhesive properties.
2. The document presents several questions about water's properties and their significance in biology. It asks students to explain processes like transpiration, sweat cooling and solubility of substances in blood in relation to water's cohesive and solvent abilities.
3. Students are asked to describe how glucose, amino acids, oxygen, sodium chloride and other substances are transported in blood plasma depending on their solubility in water and ability to form complexes with proteins like hemoglobin.1.4. Membrane transport
1.4. Membrane transportMiltiadis Kitsos
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Phospholipid bilayers are selectively permeable membranes that control the movement of molecules into and out of cells through passive and active transport mechanisms. Passive transport includes diffusion, facilitated diffusion, and osmosis, which allow molecules to move down their concentration gradients without energy expenditure. Active transport requires energy in the form of ATP to move molecules against their concentration gradients, such as sodium-potassium pumps that repolarize neurons after firing. Membrane transport is essential for cellular functions like nutrient absorption, waste removal, and nerve signal transmission.Organic
Organicaimorales
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Coal formed around 300 million years ago from the remains of terrestrial vegetation. Oil was formed from marine plant and animal remains. Both coal and oil are extracted through industrial production and are important fossil fuels used as an energy source.Carbonates
Carbonatesaimorales
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Stalactites form from calcium carbonate deposits that accumulate on cave ceilings. Limestone forms from the accumulation of shells and skeletons of living things over time. Fossils can be found embedded in limestone, providing evidence of past life.Sedimentary rock types
Sedimentary rock typesaimorales
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Sedimentary rocks can be categorized into three main types: detrital or clastic, chemical, and organic. Detrital rocks like conglomerate and sandstone are composed of fragments and grains of older rock. Chemical rocks such as limestone, travertine, and gypsum form via precipitation from water. Organic rocks like coal and oil are derived from buried dead plants and animals.Magnitudes
Magnitudesaimorales
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The document discusses the concept of magnitudes, which are physical properties that can be measured, such as the mass or volume of an object. Magnitudes must be expressed using a number and a unit, such as 120 km/h. There is an international system that collects magnitudes and their standard units. This system identifies fundamental magnitudes as the most important ones to measure, including length, time, mass, and temperature, along with their standard units.Clastic
Clasticaimorales
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Detrital sedimentary rocks are formed through the accumulation and compaction of eroded rock fragments that have been transported by water, wind, or ice and deposited in sedimentary basins over time. As additional layers of sediment are deposited, the lower layers undergo compaction and cementation through burial and lithification, forming identifiable strata of solidified sedimentary rock.Metamorphic rocks
Metamorphic rocksaimorales
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Metamorphic rocks are formed from existing rock types that have undergone intense heat and pressure, causing changes to their mineral composition and structure. There are two main categories of metamorphic rocks - foliated rocks which have a layered or banded appearance due to the development of foliations or planes of crystal alignment under pressure, and non-foliated rocks which have a crystalline structure without distinct layers. Common examples of foliated rocks include slate, schist and gneiss, while non-foliated rocks include marble and quartzite.What is a mineral
What is a mineralaimorales
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Minerals are naturally occurring inorganic solid substances that have a definite and homogeneous chemical composition. While minerals are pure substances, impurities can sometimes cause the same mineral to vary in color, such as smoky quartz, white quartz, and rose quartz which are all variations of the mineral quartz.Classification
Classificationaimorales
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Minerals are classified into two main groups - silicates and non-silicates. Silicates contain oxygen and silicon and include quartz, feldspar, mica, olivine and clay minerals. Non-silicates do not contain silicon and include native elements, oxides, sulfides, carbonates, sulfates and halides such as galena, calcite and halite.Ib
IbDasha Ermakova
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The document discusses key aspects of the International Baccalaureate (IB) Middle Years Programme (MYP). It outlines requirements for schools implementing the MYP, including developing the curriculum as a whole-school activity and articulating it with other IB programmes. It also discusses the IB's role in supporting schools and validating their assessments. The MYP aims to develop inquiring, knowledgeable and caring students through an interdisciplinary curriculum framework.Igneous rocks
Igneous rocksaimorales
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This document describes different types of volcanic and plutonic rocks. It shows that magma is a mixture of melted rock and gases that can solidify into either plutonic or volcanic rocks. Plutonic rocks like granite form deep underground, while volcanic rocks such as basalt and obsidian form above ground during volcanic eruptions and have distinct characteristics based on their composition and texture.Sedimentary rocks
Sedimentary rocksaimorales
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Sedimentary rocks form in layers or strata and are categorized into detrital, non-detrital chemical, and organic types. Detrital rocks are formed from fragments of pre-existing rocks or organic material. Chemical rocks like limestone form from precipitation of minerals from water. Organic rocks form from remains of living organisms.Evaporites
Evaporitesaimorales
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Evaporation in hot, dry climates can lead to the precipitation and accumulation of minerals like halite crystals forming rock salt or gypsum crystals. Marshes and coastal lagoons are areas where evaporation exceeds precipitation, allowing for the accumulation of minerals like gypsum in the form of crystals.Introduction to IB Diploma Biology
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A small introduction to the course of Biology in the IB Diploma. Aims, curriculum and assessment schemes. Force
Forceaimorales
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A force is a push or pull that can cause an object to move, stop, or change direction. Forces can affect an object's motion by making it start moving, move faster or slower, stop moving, or change direction. Forces cause objects with mass to accelerate.Properties
Propertiesaimorales
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This document discusses the physical properties of minerals including color, luster, hardness, streak, and cleavage. It provides examples of the properties of common minerals like quartz, feldspar, pyrite, and hematite. The properties are ranked using the Mohs hardness scale from 1 to 10.Mines
Minesaimorales
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Minerals are extracted through surface mining or underground mining. Surface mining excavates mineral beds directly from the earth's surface, while underground mining involves digging shafts and horizontal galleries below ground. Mining can negatively impact the environment through pollution, destruction of vegetation, and creation of waste dumps.Intro to Chemistry - Meet the elements
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Newton lawsaimorales
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Objects in motion will remain in motion and objects at rest will remain at rest unless acted on by an unbalanced force. Things stop moving due to forces like friction and gravity. Newton's laws state that (1) objects resist changes in motion, (2) force equals mass times acceleration, and (3) for every action there is an equal and opposite reaction.G10 genetics
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This document covers key concepts in genetics and inheritance patterns, including Mendel's experiments with pea plants, dominant and recessive traits, sex linkage of genetic disorders, and applications of biotechnology. It discusses Mendel's work breeding pea plants and identifying inheritance patterns. It defines concepts like genotype and phenotype and explains monohybrid crosses. It also covers codominance and blood types, sex linkage of traits, genetic disorders, and modern applications of genetics like genetic screening, DNA profiling, genetically modified organisms, and stem cell research.What is a rock
What is a rockaimorales
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Rocks are composed of one or more minerals, and can be classified into three main types: sedimentary, igneous, and metamorphic. Sedimentary rocks form from the compression of sediments like sand and pebbles, igneous rocks form from the cooling of magma or lava, and metamorphic rocks form from the alteration of existing rocks by heat, pressure, and chemical reactions. Some rocks like quartzite and granite contain multiple minerals, while others like gypsum and halite contain only one mineral.Grade 10 Evolution
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La geosferaaimorales
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La geosfera est叩 formada por rocas y minerales. Est叩 compuesta por la corteza, el manto y el n炭cleo. La corteza terrestre es delgada, de entre 6 y 40 km de espesor, y est叩 formada por rocas sil鱈ceas. Los minerales son cuerpos s坦lidos inorg叩nicos de composici坦n qu鱈mica y estructura cristalina definidas que se forman de forma natural.
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Este documento presenta la informaci坦n sobre un curso de Biolog鱈a y Geolog鱈a para estudiantes de 1oESO. Se introduce la profesora Ana Morales y se describen las 12 unidades que componen el plan de estudios para los tres trimestres. Tambi辿n se especifican los materiales necesarios y las normas de evaluaci坦n, entrega de tareas, comunicaci坦n y conducta en clase teniendo en cuenta las medidas de seguridad por el COVID-19.More Related Content
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Sedimentary rock types
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Sedimentary rocks can be categorized into three main types: detrital or clastic, chemical, and organic. Detrital rocks like conglomerate and sandstone are composed of fragments and grains of older rock. Chemical rocks such as limestone, travertine, and gypsum form via precipitation from water. Organic rocks like coal and oil are derived from buried dead plants and animals.Magnitudes
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The document discusses the concept of magnitudes, which are physical properties that can be measured, such as the mass or volume of an object. Magnitudes must be expressed using a number and a unit, such as 120 km/h. There is an international system that collects magnitudes and their standard units. This system identifies fundamental magnitudes as the most important ones to measure, including length, time, mass, and temperature, along with their standard units.Clastic
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This document describes different types of volcanic and plutonic rocks. It shows that magma is a mixture of melted rock and gases that can solidify into either plutonic or volcanic rocks. Plutonic rocks like granite form deep underground, while volcanic rocks such as basalt and obsidian form above ground during volcanic eruptions and have distinct characteristics based on their composition and texture.Sedimentary rocks
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Sedimentary rocks form in layers or strata and are categorized into detrital, non-detrital chemical, and organic types. Detrital rocks are formed from fragments of pre-existing rocks or organic material. Chemical rocks like limestone form from precipitation of minerals from water. Organic rocks form from remains of living organisms.Evaporites
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Brandon has had 3 different careers (banking, corporate finance & strategy, technology) in 7 different industries; Investment Banking, CPG, Media & Entertainment, Telecommunications, Consumer application, Automotive, & Fintech/Insuretech.
He's an idea to revenue leader and entrepreneur that helps organizations build products and processes, hire talent, test & iterate quickly, collect feedback, and grow in unregulated and heavily regulated industries.16 KALALU鏝媜ご垂鏝乞 APARAMAHASAHASRA SIMHAMAHANKALKIADIPARASAKTIBH...
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This webinar will offer you a first look at the powerful capabilities of UiPath Agent Builder, designed to streamline your automation processes and enhance your workflow efficiency.
During the session, you will:
- Discover how to build agents with low-code experience, making it accessible for both developers and business users.
- Learn how to leverage automations and activities as tools within your agents, enabling them to handle complex and dynamic workflows.
- Gain insights into the AI Trust Layer, which provides robust management and monitoring capabilities, ensuring trust and transparency in your automation processes.
- See how agents can be deployed and integrated with your existing UiPath cloud and Studio environments.
Speaker:
Zach Eslami, Sr. Manager, Product Management Director, UiPath
Register for our upcoming Dev Dives March session:
Unleash the power of macOS Automation with UiPath
AMER: https://bit.ly/Dev_Dives_AMER_March
EMEA & APJ:https://bit.ly/Dev_Dives_EMEA_APJ_March
This session was streamed live on February 27, 2025, 15:00 GMT.
Check out future Dev Dives 2025 sessions at:
https://bit.ly/Dev_Dives_2025
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Key Takeaways:
Effective Prompting: Crafting context-specific, high-quality prompts for optimal AI responses.
Advanced ChatGPT Features: Managing system prompts, conversation memory, and file uploads.
Optimizing AI Outputs: Refining responses, handling large texts, and knowing when fine-tuning is needed.
Competitive Insights: Exploring how ChatGPT compares with other AI tools.
Business & Content Use Cases: From summarization to SEO, sales, and audience targeting.
The session provided hands-on strategies to make AI a powerful tool for content creation, decision-making, and business growth.
Are you using AI effectively in your workflow? Lets discuss how it can improve efficiency and creativity!
#AI #ChatGPT #PromptEngineering #ArtificialIntelligence #LLM #Productivity #AstiostechThe Constructor's Digital Transformation Playbook: Reducing Risk With Technology
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https://www.professionalconstructorcentral.com/frs/27678427/the-constructor-s-digital-transformation-playbook--reducing-risk-with-technology
Reduce risk and boost efficiency with digital transformation in construction. Join us to explore how AI, automation, and data-driven insights can improve project safety and streamline operations.Artificial Intelligence Quick Research Guide by Arthur Morgan
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This is a Quick Research Guide (QRG).
QRGs include the following:
- A brief, high-level overview of the QRG topic.
- A milestone timeline for the QRG topic.
- Links to various free online resource materials to provide a deeper dive into the QRG topic.
- Conclusion and a recommendation for at least two books available in the SJPL system on the QRG topic.
QRGs planned for the series:
- Artificial Intelligence QRG
- Quantum Computing QRG
- Big Data Analytics QRG (coming 2025)
- Spacecraft Guidance, Navigation & Control QRG (coming 2026)
- UK Home Computing & The Birth of ARM QRG (coming 2027)
Any questions or comments?
- Please contact Arthur Morgan at art_morgan@att.net.
100% human made.Supercharge Your Career with UiPath Certifications
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Join us on February 25th as we discuss how you can supercharge your career with the updated 2025 UiPath Certifications.
Diana Gray, UiPath Senior Community Marketing Manager, Americas, will walk us through:
-- Workforce Trends
-- Value of UiPath Certifications
-- Certification Program
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George Walkley, a publishing veteran and leading authority on AI applications, joins us for a follow-up to his presentation "Applying AI to publishing: A balanced and ethical approach". George gives a brief overview of developments since that presentation and answers attendees' pressing questions about AIs impact and potential applications in the book industry.
Link to recording and presentation slides: https://bnctechforum.ca/sessions/ai-in-publishing-your-questions-answered/
Presented by BookNet Canada on February 20, 2025 with support from the Department of Canadian Heritage.Caching for Performance Masterclass: The In-Memory Datastore
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Understanding where in-memory data stores help most and where teams get into trouble.
- Where in the stack to cache
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In short, lexical search is a way to search your documents based on the keywords they contain, in contrast to semantic search, which compares the similarity of embeddings. Well be covering:
Why, when, and how should you use lexical search
What is the BM25 distance metric
How exactly does Milvus 2.5 implement lexical search
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Bedrock Data Automation (BDA) is a cloud-based service that simplifies the process of extracting valuable insights from unstructured contentsuch as documents, images, video, and audio. Come learn how BDA leverages generative AI to automate the transformation of multi-modal data into structured formats, enabling developers to build applications and automate complex workflows with greater speed and accuracy.Revolutionizing Field Service: How LLMs Are Powering Smarter Knowledge Access...
Revolutionizing Field Service: How LLMs Are Powering Smarter Knowledge Access...Earley Information Science
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Revolutionizing Field Service with LLM-Powered Knowledge Management
Field service technicians need instant access to accurate repair information, but outdated knowledge systems often create frustrating delays. Large Language Models (LLMs) are changing the gameenhancing knowledge retrieval, streamlining troubleshooting, and reducing technician dependency on senior staff.
In this webinar, Seth Earley and industry experts Sanjay Mehta, and Heather Eisenbraun explore how LLMs and Retrieval-Augmented Generation (RAG) are transforming field service operations. Discover how AI-powered knowledge management is improving efficiency, reducing downtime, and elevating service quality.
LLMs for Instant Knowledge Retrieval How AI-driven search dramatically cuts troubleshooting time.
Structured Data & AI Why high-quality, organized knowledge is essential for LLM success.
Real-World Implementation Lessons from deploying LLM-powered knowledge tools in field service.
Business Impact How AI reduces service delays, optimizes workflows, and enhances technician productivity.
Empower your field service teams with AI-driven knowledge access. Watch the webinar to see how LLMs are revolutionizing service efficiency.Revolutionizing Field Service: How LLMs Are Powering Smarter Knowledge Access...
Revolutionizing Field Service: How LLMs Are Powering Smarter Knowledge Access...Earley Information Science
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S t graphs
- 1. Speed - time graphs speed time
- 2. No movement speed time
- 3. Constant speed speed time
- 4. Constant speed How would the graph speed look different for a faster constant speed? time
- 5. Constant speed speed fast time
- 6. Constant speed How would the graph speed look different for a slower constant speed? fast time
- 7. Constant speed speed fast slow time
- 9. Getting faster? (accelerating) speed Constant acceleration time
- 10. Getting faster? (accelerating) speed The area under the graph gives the distance travelled time
- 11. Example: speed time
- 12. A dog falling from a tall building (no air resistance) speed time
- 13. A dog falling from a tall building (no air resistance) speed time
- 14. A dog falling from a tall building (no air resistance) speed Area = height of building time
- 15. Be careful! speed distance time time
- 16. No movement speed distance time time
- 17. Constant speed speed distance time Area = distance travelled time
- 18. Constant acceleration speed distance time Area = distance travelled time