-
Homogeneous and Heterogeneous Mixture | Chemistry
In this animated lecture, I will teach you about homogeneous mixture and heterogeneous mixture.
#HomogeneousMixture
#HeterogeneousMixture
#Chemistry
Subscribe my channel at:https://www.youtube.com/channel/UC_ltCdLVMRZ7r3IPzF2Toyg
Youtube link: https://www.youtube.com/channel/UC_ltCdLVMRZ7r3IPzF2Toyg
Facebook link: https://www.facebook.com/Najamacademy/
published: 06 Jun 2020
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Homogeneous and Heterogeneous Mixtures Examples, Classification of Matter, Chemistry
This chemistry video tutorial explains the difference between homogeneous and heterogeneous mixtures within the subtopic of the classification of matter.
Chemistry - Basic Introduction: https://www.youtube.com/watch?v=-KfG8kH-r3Y
Chemistry Fundamentals - Video Lessons:
https://www.video-tutor.net/chemistry-fundamentals.html
published: 06 Aug 2017
-
Heterogenous vs Homogenous (Definitions, Examples, & Practice)
When we discuss mixtures we can broadly classify them as heterogenous or homogenous. This is common question on chemistry quizzes and tests where you are given a mixture, for example salt water, and asked to determine whether is a heterogenous or homogenous mixture.
The general definition is:
Heterogenous: Not uniform (unevenly distributed).
Examples: rocks in mud, salad, nails in sand
Homogenous: Uniform composition (same throughout).
Examples: salt water, smoke, alloys
Note that you can have a mixture, like rock, water, and sugar that has hetero and homo components. In this case the rocks and sugar water are a heterogenous mixture. If we look just at the sugar dissolved in the water, this has a uniform/smooth composition and is therefore a homogenous solution.
We can separa...
published: 01 Feb 2021
-
Homogeneous and Heterogeneous Mixtures
Heterogeneous mixtures do not have a uniform composition, while homogeneous mixtures (solutions) do.
published: 30 Jun 2020
-
homogeneous and heterogeneous mixture 🧬 school science experiment
homogeneous and heterogeneous mixture experiment
published: 16 Sep 2022
-
Structural Geology Course: Lecture 4 (Homogeneity & Heterogeneity of rocks in Structural Geology)
In structural geology, the concepts of homogeneity and heterogeneity refer to the uniformity or variability of rock properties at different scales, from the microscale to the macroscale. Homogeneous rocks have consistent properties throughout, such as uniform mineral composition, grain size, and texture. In contrast, heterogeneous rocks exhibit variability in their properties, often due to differences in mineralogy, grain size, or the presence of structural features like fractures and veins.
Understanding the homogeneity and heterogeneity of rocks is crucial for structural geologists because it influences how rocks deform under stress and the development of geological structures. At the microscale, homogeneity implies that the properties of the rock, such as its strength and elasticity, a...
published: 06 Jun 2024
-
Heterogeneous and Homogeneous Mixtures in Chemistry
📺 We will go through the differences between heterogeneous mixtures and homogeneous mixtures in Chemistry in this lesson, with different examples.
Like this video and subscribe: https://www.youtube.com/c/SchoolingOnline
Life is tough for thirsty pirates – the sea is filled with water that can’t be drunk! Thankfully, Blackbeard has figured out a trick. This chemistry lesson will compare heterogeneous and homogeneous mixtures. We’ll also look at solutions, which are a special type of homogeneous mixture.
Definitions included: heterogeneous mixture, homogeneous mixture, solution, solvent, solute
Get Access to our FREE English Essentials Kit: https://mailchi.mp/schoolingonline/free-english-essentials-kit
► WEBSITE: https://schoolingonline.com/
► INSTAGRAM: https://www.instagram.com/schoo...
published: 14 Jul 2020
-
Homogeneity of Error for One Factor Models (Module 2 6 2)
To view a playlist and download materials shown in this eCourse, visit the course page at: http://www.jmp.com/en_us/academic/ssms.html
published: 18 Feb 2015
-
Uji Beda Mean, Uji Chi Square, & Uji Regresi Linear di SPSS (Praktiknya 05.44) #biostatistics
Assalamu'alaikum teman''
Ini merupakan tugas untuk memenuhi mata kuliah biostatistika dengan SPSS untuk memenuhi tugas ujian biostatitik
Nama : Asfi Novelia Putri
Nim/Kelas : 2248201006/5A
Dosen Pengampu: Harry Ade Putra S.Si, M.Si
SELAMAT MENONTON!!!
published: 23 Jan 2025
-
Homogenous Vs. Homogeneous: What's The Difference?
Homogenous. Homogenous. These words are commonly confused, but Dictionary.com can help you keep them straight!
published: 03 Jun 2019
5:01
Homogeneous and Heterogeneous Mixture | Chemistry
In this animated lecture, I will teach you about homogeneous mixture and heterogeneous mixture.
#HomogeneousMixture
#HeterogeneousMixture
#Chemistry
Subscrib...
In this animated lecture, I will teach you about homogeneous mixture and heterogeneous mixture.
#HomogeneousMixture
#HeterogeneousMixture
#Chemistry
Subscribe my channel at:https://www.youtube.com/channel/UC_ltCdLVMRZ7r3IPzF2Toyg
Youtube link: https://www.youtube.com/channel/UC_ltCdLVMRZ7r3IPzF2Toyg
Facebook link: https://www.facebook.com/Najamacademy/
https://wn.com/Homogeneous_And_Heterogeneous_Mixture_|_Chemistry
In this animated lecture, I will teach you about homogeneous mixture and heterogeneous mixture.
#HomogeneousMixture
#HeterogeneousMixture
#Chemistry
Subscribe my channel at:https://www.youtube.com/channel/UC_ltCdLVMRZ7r3IPzF2Toyg
Youtube link: https://www.youtube.com/channel/UC_ltCdLVMRZ7r3IPzF2Toyg
Facebook link: https://www.facebook.com/Najamacademy/
- published: 06 Jun 2020
- views: 1434778
5:50
Homogeneous and Heterogeneous Mixtures Examples, Classification of Matter, Chemistry
This chemistry video tutorial explains the difference between homogeneous and heterogeneous mixtures within the subtopic of the classification of matter.
Che...
This chemistry video tutorial explains the difference between homogeneous and heterogeneous mixtures within the subtopic of the classification of matter.
Chemistry - Basic Introduction: https://www.youtube.com/watch?v=-KfG8kH-r3Y
Chemistry Fundamentals - Video Lessons:
https://www.video-tutor.net/chemistry-fundamentals.html
https://wn.com/Homogeneous_And_Heterogeneous_Mixtures_Examples,_Classification_Of_Matter,_Chemistry
This chemistry video tutorial explains the difference between homogeneous and heterogeneous mixtures within the subtopic of the classification of matter.
Chemistry - Basic Introduction: https://www.youtube.com/watch?v=-KfG8kH-r3Y
Chemistry Fundamentals - Video Lessons:
https://www.video-tutor.net/chemistry-fundamentals.html
- published: 06 Aug 2017
- views: 711966
3:35
Heterogenous vs Homogenous (Definitions, Examples, & Practice)
When we discuss mixtures we can broadly classify them as heterogenous or homogenous. This is common question on chemistry quizzes and tests where you are given...
When we discuss mixtures we can broadly classify them as heterogenous or homogenous. This is common question on chemistry quizzes and tests where you are given a mixture, for example salt water, and asked to determine whether is a heterogenous or homogenous mixture.
The general definition is:
Heterogenous: Not uniform (unevenly distributed).
Examples: rocks in mud, salad, nails in sand
Homogenous: Uniform composition (same throughout).
Examples: salt water, smoke, alloys
Note that you can have a mixture, like rock, water, and sugar that has hetero and homo components. In this case the rocks and sugar water are a heterogenous mixture. If we look just at the sugar dissolved in the water, this has a uniform/smooth composition and is therefore a homogenous solution.
We can separate both heterogenous and homogenous mixtures using their physicals properties. For example filtration, distillation, sorting based on size, or gravitational sorting based on density.
https://wn.com/Heterogenous_Vs_Homogenous_(Definitions,_Examples,_Practice)
When we discuss mixtures we can broadly classify them as heterogenous or homogenous. This is common question on chemistry quizzes and tests where you are given a mixture, for example salt water, and asked to determine whether is a heterogenous or homogenous mixture.
The general definition is:
Heterogenous: Not uniform (unevenly distributed).
Examples: rocks in mud, salad, nails in sand
Homogenous: Uniform composition (same throughout).
Examples: salt water, smoke, alloys
Note that you can have a mixture, like rock, water, and sugar that has hetero and homo components. In this case the rocks and sugar water are a heterogenous mixture. If we look just at the sugar dissolved in the water, this has a uniform/smooth composition and is therefore a homogenous solution.
We can separate both heterogenous and homogenous mixtures using their physicals properties. For example filtration, distillation, sorting based on size, or gravitational sorting based on density.
- published: 01 Feb 2021
- views: 47245
1:01
Homogeneous and Heterogeneous Mixtures
Heterogeneous mixtures do not have a uniform composition, while homogeneous mixtures (solutions) do.
Heterogeneous mixtures do not have a uniform composition, while homogeneous mixtures (solutions) do.
https://wn.com/Homogeneous_And_Heterogeneous_Mixtures
Heterogeneous mixtures do not have a uniform composition, while homogeneous mixtures (solutions) do.
- published: 30 Jun 2020
- views: 8934
19:01
Structural Geology Course: Lecture 4 (Homogeneity & Heterogeneity of rocks in Structural Geology)
In structural geology, the concepts of homogeneity and heterogeneity refer to the uniformity or variability of rock properties at different scales, from the mic...
In structural geology, the concepts of homogeneity and heterogeneity refer to the uniformity or variability of rock properties at different scales, from the microscale to the macroscale. Homogeneous rocks have consistent properties throughout, such as uniform mineral composition, grain size, and texture. In contrast, heterogeneous rocks exhibit variability in their properties, often due to differences in mineralogy, grain size, or the presence of structural features like fractures and veins.
Understanding the homogeneity and heterogeneity of rocks is crucial for structural geologists because it influences how rocks deform under stress and the development of geological structures. At the microscale, homogeneity implies that the properties of the rock, such as its strength and elasticity, are consistent in all directions. This can lead to uniform deformation behavior and the development of simple structures in response to tectonic forces. In contrast, heterogeneous rocks may exhibit localized zones of weakness or strength, leading to complex deformation patterns and the formation of diverse geological structures.
As the scale of observation increases, the effects of rock homogeneity and heterogeneity become more pronounced. At the mesoscale, geological structures such as faults, folds, and joints may be influenced by variations in rock properties across different regions. Homogeneous rocks are more likely to deform uniformly and exhibit predictable structural geometries, whereas heterogeneous rocks may deform non-uniformly, leading to the development of complex fault networks, folding patterns, and fracture systems.
On a regional scale, the homogeneity and heterogeneity of rocks play a significant role in controlling the behavior of large-scale tectonic processes and the formation of major geological structures such as mountain ranges, rift zones, and sedimentary basins. Homogeneous rocks may exhibit more uniform responses to tectonic forces, resulting in the development of broad, gentle folds and thrust faults. In contrast, heterogeneous rocks may produce more localized and complex deformation patterns, characterized by intense faulting, folding, and fracturing.
The concepts of homogeneity and heterogeneity are important to structural geologists because they influence the mechanical behavior of rocks at different scales and control the development of geological structures. By understanding the distribution and variability of rock properties, structural geologists can better interpret deformation processes, predict geological hazards, and reconstruct the tectonic history of a region.
https://wn.com/Structural_Geology_Course_Lecture_4_(Homogeneity_Heterogeneity_Of_Rocks_In_Structural_Geology)
In structural geology, the concepts of homogeneity and heterogeneity refer to the uniformity or variability of rock properties at different scales, from the microscale to the macroscale. Homogeneous rocks have consistent properties throughout, such as uniform mineral composition, grain size, and texture. In contrast, heterogeneous rocks exhibit variability in their properties, often due to differences in mineralogy, grain size, or the presence of structural features like fractures and veins.
Understanding the homogeneity and heterogeneity of rocks is crucial for structural geologists because it influences how rocks deform under stress and the development of geological structures. At the microscale, homogeneity implies that the properties of the rock, such as its strength and elasticity, are consistent in all directions. This can lead to uniform deformation behavior and the development of simple structures in response to tectonic forces. In contrast, heterogeneous rocks may exhibit localized zones of weakness or strength, leading to complex deformation patterns and the formation of diverse geological structures.
As the scale of observation increases, the effects of rock homogeneity and heterogeneity become more pronounced. At the mesoscale, geological structures such as faults, folds, and joints may be influenced by variations in rock properties across different regions. Homogeneous rocks are more likely to deform uniformly and exhibit predictable structural geometries, whereas heterogeneous rocks may deform non-uniformly, leading to the development of complex fault networks, folding patterns, and fracture systems.
On a regional scale, the homogeneity and heterogeneity of rocks play a significant role in controlling the behavior of large-scale tectonic processes and the formation of major geological structures such as mountain ranges, rift zones, and sedimentary basins. Homogeneous rocks may exhibit more uniform responses to tectonic forces, resulting in the development of broad, gentle folds and thrust faults. In contrast, heterogeneous rocks may produce more localized and complex deformation patterns, characterized by intense faulting, folding, and fracturing.
The concepts of homogeneity and heterogeneity are important to structural geologists because they influence the mechanical behavior of rocks at different scales and control the development of geological structures. By understanding the distribution and variability of rock properties, structural geologists can better interpret deformation processes, predict geological hazards, and reconstruct the tectonic history of a region.
- published: 06 Jun 2024
- views: 173
11:39
Heterogeneous and Homogeneous Mixtures in Chemistry
📺 We will go through the differences between heterogeneous mixtures and homogeneous mixtures in Chemistry in this lesson, with different examples.
Like this vi...
📺 We will go through the differences between heterogeneous mixtures and homogeneous mixtures in Chemistry in this lesson, with different examples.
Like this video and subscribe: https://www.youtube.com/c/SchoolingOnline
Life is tough for thirsty pirates – the sea is filled with water that can’t be drunk! Thankfully, Blackbeard has figured out a trick. This chemistry lesson will compare heterogeneous and homogeneous mixtures. We’ll also look at solutions, which are a special type of homogeneous mixture.
Definitions included: heterogeneous mixture, homogeneous mixture, solution, solvent, solute
Get Access to our FREE English Essentials Kit: https://mailchi.mp/schoolingonline/free-english-essentials-kit
► WEBSITE: https://schoolingonline.com/
► INSTAGRAM: https://www.instagram.com/schoolingonline/
► FACEBOOK: https://www.facebook.com/schoolingonline/
💡Do you have suggestions or questions?
✉CONTACT:
[email protected]
👍 If you liked this video please give us a thumbs up to support our channel!
🔔 Subscribe to our channel and hit the notification bell to always stay up to date with our newest uploads!
#HeterogeneousandHomogeneous #SchoolingOnline
https://wn.com/Heterogeneous_And_Homogeneous_Mixtures_In_Chemistry
📺 We will go through the differences between heterogeneous mixtures and homogeneous mixtures in Chemistry in this lesson, with different examples.
Like this video and subscribe: https://www.youtube.com/c/SchoolingOnline
Life is tough for thirsty pirates – the sea is filled with water that can’t be drunk! Thankfully, Blackbeard has figured out a trick. This chemistry lesson will compare heterogeneous and homogeneous mixtures. We’ll also look at solutions, which are a special type of homogeneous mixture.
Definitions included: heterogeneous mixture, homogeneous mixture, solution, solvent, solute
Get Access to our FREE English Essentials Kit: https://mailchi.mp/schoolingonline/free-english-essentials-kit
► WEBSITE: https://schoolingonline.com/
► INSTAGRAM: https://www.instagram.com/schoolingonline/
► FACEBOOK: https://www.facebook.com/schoolingonline/
💡Do you have suggestions or questions?
✉CONTACT:
[email protected]
👍 If you liked this video please give us a thumbs up to support our channel!
🔔 Subscribe to our channel and hit the notification bell to always stay up to date with our newest uploads!
#HeterogeneousandHomogeneous #SchoolingOnline
- published: 14 Jul 2020
- views: 49220
4:32
Homogeneity of Error for One Factor Models (Module 2 6 2)
To view a playlist and download materials shown in this eCourse, visit the course page at: http://www.jmp.com/en_us/academic/ssms.html
To view a playlist and download materials shown in this eCourse, visit the course page at: http://www.jmp.com/en_us/academic/ssms.html
https://wn.com/Homogeneity_Of_Error_For_One_Factor_Models_(Module_2_6_2)
To view a playlist and download materials shown in this eCourse, visit the course page at: http://www.jmp.com/en_us/academic/ssms.html
- published: 18 Feb 2015
- views: 790
16:18
Uji Beda Mean, Uji Chi Square, & Uji Regresi Linear di SPSS (Praktiknya 05.44) #biostatistics
Assalamu'alaikum teman''
Ini merupakan tugas untuk memenuhi mata kuliah biostatistika dengan SPSS untuk memenuhi tugas ujian biostatitik
Nama : Asfi No...
Assalamu'alaikum teman''
Ini merupakan tugas untuk memenuhi mata kuliah biostatistika dengan SPSS untuk memenuhi tugas ujian biostatitik
Nama : Asfi Novelia Putri
Nim/Kelas : 2248201006/5A
Dosen Pengampu: Harry Ade Putra S.Si, M.Si
SELAMAT MENONTON!!!
https://wn.com/Uji_Beda_Mean,_Uji_Chi_Square,_Uji_Regresi_Linear_Di_Spss_(Praktiknya_05.44)_Biostatistics
Assalamu'alaikum teman''
Ini merupakan tugas untuk memenuhi mata kuliah biostatistika dengan SPSS untuk memenuhi tugas ujian biostatitik
Nama : Asfi Novelia Putri
Nim/Kelas : 2248201006/5A
Dosen Pengampu: Harry Ade Putra S.Si, M.Si
SELAMAT MENONTON!!!
- published: 23 Jan 2025
- views: 448
1:51
Homogenous Vs. Homogeneous: What's The Difference?
Homogenous. Homogenous. These words are commonly confused, but Dictionary.com can help you keep them straight!
Homogenous. Homogenous. These words are commonly confused, but Dictionary.com can help you keep them straight!
https://wn.com/Homogenous_Vs._Homogeneous_What's_The_Difference
Homogenous. Homogenous. These words are commonly confused, but Dictionary.com can help you keep them straight!
- published: 03 Jun 2019
- views: 29944
-
New Frontiers in Mathematics: Prof Emmanuel Breuillard, “Homogeneous flows and diophantine geometry”
New Frontiers in Mathematics: Imperial College London and CNRS international symposium
Professor Breuillard from the University of Cambridge, discusses Homogeneous flows and diophantine geometry.
For more information visit: http://www3.imperial.ac.uk/newsandeventspggrp/imperialcollege/newssummary/news_10-1-2018-16-41-35
published: 17 Jan 2018
-
Stratum (disambiguation)
A stratum is a geologic formation.
Stratum may also refer to:
Source: https://en.wikipedia.org/wiki/Stratum_(disambiguation)
Created with WikipediaReaderReborn (c) WikipediaReader
published: 09 Nov 2021
-
Empty space (disambiguation) | Wikipedia audio article
This is an audio version of the Wikipedia Article:
https://en.wikipedia.org/wiki/Empty_space
00:00:03 1 Physics
00:00:48 2 Arts and literature
00:01:13 3 Music
00:01:21 3.1 Albums
00:01:38 3.2 Songs
00:02:09 4 See also
Listening is a more natural way of learning, when compared to reading. Written language only began at around 3200 BC, but spoken language has existed long ago.
Learning by listening is a great way to:
- increases imagination and understanding
- improves your listening skills
- improves your own spoken accent
- learn while on the move
- reduce eye strain
Now learn the vast amount of general knowledge available on Wikipedia through audio (audio article). You could even learn subconsciously by playing the audio while you are sleeping! If you are planning ...
published: 03 May 2019
-
DomainNet: Homograph Detection for Data Lake Disambiguation
Talk recorded for EDBT 2021
Develops a method to detect homographs (i.e. data values with multiple meanings) in data lakes
Group web page:
https://db.khoury.northeastern.edu
EDBT 2021 paper:
https://northeastern-datalab.github.io/table-as-query/download/EDBT21-DomainNet-Homograph-Detection.pdf
published: 16 Mar 2021
-
Learning to Disambiguate Strongly Interacting Hands via Probabilistic Per-Pixel Part Segmentation
3DV 2021 Oral Presentation: In natural conversation and interaction, our hands often overlap or are in contact with each other. Due to the homogeneous appearance of hands, this makes estimating the 3D pose of interacting hands from images difficult. In this paper we demonstrate that self-similarity, and the resulting ambiguities in assigning pixel observations to the respective hands and their parts, is a major cause of the final 3D pose error. Motivated by this insight, we propose DIGIT, a novel method for estimating the 3D poses of two interacting hands from a single monocular image. The method consists of two interwoven branches that process the input imagery into a per-pixel semantic part segmentation mask and a visual feature volume. In contrast to prior work, we do not decouple the s...
published: 30 Nov 2021
-
Natural Language Understanding by means of current Word Sense Disambiguation. EurASc 2019 (7)
Roberto Navigli, Sapienza University
Symposium Artificial Intelligence and Ceremony of Awards. 21 and 22 October 2019.
Understanding language is a hard task for a computer even in the era of deep learning. In this talk I will advocate the importance of interdisciplinary work for multilingual Natural Language Understanding: I will present current state-of-the-art results attained by joining forces between computer scientists and (computational) linguists, in order to address the knowledge acquisition bottleneck and scale up key tasks in word- and sentence-level semantics which enable computers to understand what is written in a text. I will also showcase innovative multilingual solutions developed in my research group and at Babelscape, a Sapienza startup company I co-founded.
Vídeo prod...
published: 22 Nov 2019
-
Google’s Quantum AI Chip Just Tapped Into Parallel Universes but there's a Catch...
#QuantumAI #QuantumScience #WillowChip
Google’s Quantum AI Chip Just Tapped Into Parallel Universes but there's a Catch...
Google’s latest quantum chip, Willow, is making waves and stirring debate. This 105-qubit marvel tackled a problem in under five minutes that would take classical supercomputers an unimaginable 10 septillion years to solve. Some researchers suggest it might even hint at the existence of parallel universes! However, not everyone is convinced. From the foundations of the multiverse theory to the controversies surrounding quantum supremacy, we explore it all. Get ready for an eye-opening look into the revolutionary world of quantum computing!
Chapters:
00:00 Introduction
00:42 The Quantum Leap: Google’s Groundbreaking Achievement
03:37 The Multiverse Link: Exploring the ...
published: 03 Jan 2025
-
uhhh na na edit ✨ #shorts
Wikipedia
Search
Join the Wikidata contest and help improve geographically located items in 16 countries!
Coordinate Me ❭ MAY 2024
Mercury (planet)
Article Talk
Language
Download PDF
Watch
View source
"First planet" redirects here. For other systems of numbering planets, see Planet § History and etymology. For other uses, see Mercury (disambiguation).
Mercury is the first planet from the Sun and the smallest in the Solar System. In English, it is named after the ancient Roman god Mercurius (Mercury), god of commerce and communication, and the messenger of the gods. Mercury is classified as a terrestrial planet, with roughly the same surface gravity as Mars. The surface of Mercury is heavily cratered, as a result of countless impact events that have accumulated over billions of ye...
published: 28 May 2024
-
Despacito sad 😢 template #shorts
Wikipedia
Search
Join the Wikidata contest and help improve geographically located items in 16 countries!
Coordinate Me ❭ MAY 2024
Mercury (planet)
Article Talk
Language
Download PDF
Watch
View source
"First planet" redirects here. For other systems of numbering planets, see Planet § History and etymology. For other uses, see Mercury (disambiguation).
Mercury is the first planet from the Sun and the smallest in the Solar System. In English, it is named after the ancient Roman god Mercurius (Mercury), god of commerce and communication, and the messenger of the gods. Mercury is classified as a terrestrial planet, with roughly the same surface gravity as Mars. The surface of Mercury is heavily cratered, as a result of countless impact events that have accumulated over billions of ye...
published: 12 Jun 2024
-
definition of causality
This simple example of causality is given as public service for those, like me, who struggle a little with the plethora of wikipedia disambiguation articles on the term, all full of mathematical formulae, discussion of things like causal dynamical triangulation, and sentences like:
"Causality should not be confused with Newton's second law, which is related to the conservation of momentum, and is a consequence of the spatial homogeneity of physical laws. The name causality suggests that all effects must have specific causes, which is a concept unrelated to the common use of causality in physics, and is violated in some mainstream interpretations of quantum mechanics."
Anyhoo, you can read through the whole thing here: https://en.wikipedia.org/wiki/Causality
... but don't worry if you d...
published: 29 Jul 2017
48:19
New Frontiers in Mathematics: Prof Emmanuel Breuillard, “Homogeneous flows and diophantine geometry”
New Frontiers in Mathematics: Imperial College London and CNRS international symposium
Professor Breuillard from the University of Cambridge, discusses Homogen...
New Frontiers in Mathematics: Imperial College London and CNRS international symposium
Professor Breuillard from the University of Cambridge, discusses Homogeneous flows and diophantine geometry.
For more information visit: http://www3.imperial.ac.uk/newsandeventspggrp/imperialcollege/newssummary/news_10-1-2018-16-41-35
https://wn.com/New_Frontiers_In_Mathematics_Prof_Emmanuel_Breuillard,_“Homogeneous_Flows_And_Diophantine_Geometry”
New Frontiers in Mathematics: Imperial College London and CNRS international symposium
Professor Breuillard from the University of Cambridge, discusses Homogeneous flows and diophantine geometry.
For more information visit: http://www3.imperial.ac.uk/newsandeventspggrp/imperialcollege/newssummary/news_10-1-2018-16-41-35
- published: 17 Jan 2018
- views: 2081
1:02
Stratum (disambiguation)
A stratum is a geologic formation.
Stratum may also refer to:
Source: https://en.wikipedia.org/wiki/Stratum_(disambiguation)
Created with WikipediaReaderReborn...
A stratum is a geologic formation.
Stratum may also refer to:
Source: https://en.wikipedia.org/wiki/Stratum_(disambiguation)
Created with WikipediaReaderReborn (c) WikipediaReader
https://wn.com/Stratum_(Disambiguation)
A stratum is a geologic formation.
Stratum may also refer to:
Source: https://en.wikipedia.org/wiki/Stratum_(disambiguation)
Created with WikipediaReaderReborn (c) WikipediaReader
- published: 09 Nov 2021
- views: 0
2:37
Empty space (disambiguation) | Wikipedia audio article
This is an audio version of the Wikipedia Article:
https://en.wikipedia.org/wiki/Empty_space
00:00:03 1 Physics
00:00:48 2 Arts and literature
00:01:13 3 ...
This is an audio version of the Wikipedia Article:
https://en.wikipedia.org/wiki/Empty_space
00:00:03 1 Physics
00:00:48 2 Arts and literature
00:01:13 3 Music
00:01:21 3.1 Albums
00:01:38 3.2 Songs
00:02:09 4 See also
Listening is a more natural way of learning, when compared to reading. Written language only began at around 3200 BC, but spoken language has existed long ago.
Learning by listening is a great way to:
- increases imagination and understanding
- improves your listening skills
- improves your own spoken accent
- learn while on the move
- reduce eye strain
Now learn the vast amount of general knowledge available on Wikipedia through audio (audio article). You could even learn subconsciously by playing the audio while you are sleeping! If you are planning to listen a lot, you could try using a bone conduction headphone, or a standard speaker instead of an earphone.
Listen on Google Assistant through Extra Audio:
https://assistant.google.com/services/invoke/uid/0000001a130b3f91
Other Wikipedia audio articles at:
https://www.youtube.com/results?search_query=wikipedia+tts
Upload your own Wikipedia articles through:
https://github.com/nodef/wikipedia-tts
Speaking Rate: 0.8226963113908115
Voice name: en-AU-Wavenet-D
"I cannot teach anybody anything, I can only make them think."
- Socrates
SUMMARY
=======
Empty space may refer to:
https://wn.com/Empty_Space_(Disambiguation)_|_Wikipedia_Audio_Article
This is an audio version of the Wikipedia Article:
https://en.wikipedia.org/wiki/Empty_space
00:00:03 1 Physics
00:00:48 2 Arts and literature
00:01:13 3 Music
00:01:21 3.1 Albums
00:01:38 3.2 Songs
00:02:09 4 See also
Listening is a more natural way of learning, when compared to reading. Written language only began at around 3200 BC, but spoken language has existed long ago.
Learning by listening is a great way to:
- increases imagination and understanding
- improves your listening skills
- improves your own spoken accent
- learn while on the move
- reduce eye strain
Now learn the vast amount of general knowledge available on Wikipedia through audio (audio article). You could even learn subconsciously by playing the audio while you are sleeping! If you are planning to listen a lot, you could try using a bone conduction headphone, or a standard speaker instead of an earphone.
Listen on Google Assistant through Extra Audio:
https://assistant.google.com/services/invoke/uid/0000001a130b3f91
Other Wikipedia audio articles at:
https://www.youtube.com/results?search_query=wikipedia+tts
Upload your own Wikipedia articles through:
https://github.com/nodef/wikipedia-tts
Speaking Rate: 0.8226963113908115
Voice name: en-AU-Wavenet-D
"I cannot teach anybody anything, I can only make them think."
- Socrates
SUMMARY
=======
Empty space may refer to:
- published: 03 May 2019
- views: 1
10:16
DomainNet: Homograph Detection for Data Lake Disambiguation
Talk recorded for EDBT 2021
Develops a method to detect homographs (i.e. data values with multiple meanings) in data lakes
Group web page:
https://db.khoury.n...
Talk recorded for EDBT 2021
Develops a method to detect homographs (i.e. data values with multiple meanings) in data lakes
Group web page:
https://db.khoury.northeastern.edu
EDBT 2021 paper:
https://northeastern-datalab.github.io/table-as-query/download/EDBT21-DomainNet-Homograph-Detection.pdf
https://wn.com/Domainnet_Homograph_Detection_For_Data_Lake_Disambiguation
Talk recorded for EDBT 2021
Develops a method to detect homographs (i.e. data values with multiple meanings) in data lakes
Group web page:
https://db.khoury.northeastern.edu
EDBT 2021 paper:
https://northeastern-datalab.github.io/table-as-query/download/EDBT21-DomainNet-Homograph-Detection.pdf
- published: 16 Mar 2021
- views: 157
2:01
Learning to Disambiguate Strongly Interacting Hands via Probabilistic Per-Pixel Part Segmentation
3DV 2021 Oral Presentation: In natural conversation and interaction, our hands often overlap or are in contact with each other. Due to the homogeneous appearanc...
3DV 2021 Oral Presentation: In natural conversation and interaction, our hands often overlap or are in contact with each other. Due to the homogeneous appearance of hands, this makes estimating the 3D pose of interacting hands from images difficult. In this paper we demonstrate that self-similarity, and the resulting ambiguities in assigning pixel observations to the respective hands and their parts, is a major cause of the final 3D pose error. Motivated by this insight, we propose DIGIT, a novel method for estimating the 3D poses of two interacting hands from a single monocular image. The method consists of two interwoven branches that process the input imagery into a per-pixel semantic part segmentation mask and a visual feature volume. In contrast to prior work, we do not decouple the segmentation from the pose estimation stage, but rather leverage the per-pixel probabilities directly in the downstream pose estimation task. To do so, the part probabilities are merged with the visual features and processed via fully-convolutional layers. We experimentally show that the proposed approach achieves new state-of-the-art performance on the InterHand2.6M dataset. We provide detailed ablation studies to demonstrate the efficacy of our method and to provide insights into how the modelling of pixel ownership affects 3D hand pose estimation.
https://wn.com/Learning_To_Disambiguate_Strongly_Interacting_Hands_Via_Probabilistic_Per_Pixel_Part_Segmentation
3DV 2021 Oral Presentation: In natural conversation and interaction, our hands often overlap or are in contact with each other. Due to the homogeneous appearance of hands, this makes estimating the 3D pose of interacting hands from images difficult. In this paper we demonstrate that self-similarity, and the resulting ambiguities in assigning pixel observations to the respective hands and their parts, is a major cause of the final 3D pose error. Motivated by this insight, we propose DIGIT, a novel method for estimating the 3D poses of two interacting hands from a single monocular image. The method consists of two interwoven branches that process the input imagery into a per-pixel semantic part segmentation mask and a visual feature volume. In contrast to prior work, we do not decouple the segmentation from the pose estimation stage, but rather leverage the per-pixel probabilities directly in the downstream pose estimation task. To do so, the part probabilities are merged with the visual features and processed via fully-convolutional layers. We experimentally show that the proposed approach achieves new state-of-the-art performance on the InterHand2.6M dataset. We provide detailed ablation studies to demonstrate the efficacy of our method and to provide insights into how the modelling of pixel ownership affects 3D hand pose estimation.
- published: 30 Nov 2021
- views: 296
36:01
Natural Language Understanding by means of current Word Sense Disambiguation. EurASc 2019 (7)
Roberto Navigli, Sapienza University
Symposium Artificial Intelligence and Ceremony of Awards. 21 and 22 October 2019.
Understanding language is a hard task f...
Roberto Navigli, Sapienza University
Symposium Artificial Intelligence and Ceremony of Awards. 21 and 22 October 2019.
Understanding language is a hard task for a computer even in the era of deep learning. In this talk I will advocate the importance of interdisciplinary work for multilingual Natural Language Understanding: I will present current state-of-the-art results attained by joining forces between computer scientists and (computational) linguists, in order to address the knowledge acquisition bottleneck and scale up key tasks in word- and sentence-level semantics which enable computers to understand what is written in a text. I will also showcase innovative multilingual solutions developed in my research group and at Babelscape, a Sapienza startup company I co-founded.
Vídeo producido por el Gabinete de Tele-Educación de la Universidad Politécnica de Madrid
https://wn.com/Natural_Language_Understanding_By_Means_Of_Current_Word_Sense_Disambiguation._Eurasc_2019_(7)
Roberto Navigli, Sapienza University
Symposium Artificial Intelligence and Ceremony of Awards. 21 and 22 October 2019.
Understanding language is a hard task for a computer even in the era of deep learning. In this talk I will advocate the importance of interdisciplinary work for multilingual Natural Language Understanding: I will present current state-of-the-art results attained by joining forces between computer scientists and (computational) linguists, in order to address the knowledge acquisition bottleneck and scale up key tasks in word- and sentence-level semantics which enable computers to understand what is written in a text. I will also showcase innovative multilingual solutions developed in my research group and at Babelscape, a Sapienza startup company I co-founded.
Vídeo producido por el Gabinete de Tele-Educación de la Universidad Politécnica de Madrid
- published: 22 Nov 2019
- views: 189
13:33
Google’s Quantum AI Chip Just Tapped Into Parallel Universes but there's a Catch...
#QuantumAI #QuantumScience #WillowChip
Google’s Quantum AI Chip Just Tapped Into Parallel Universes but there's a Catch...
Google’s latest quantum chip, Willow,...
#QuantumAI #QuantumScience #WillowChip
Google’s Quantum AI Chip Just Tapped Into Parallel Universes but there's a Catch...
Google’s latest quantum chip, Willow, is making waves and stirring debate. This 105-qubit marvel tackled a problem in under five minutes that would take classical supercomputers an unimaginable 10 septillion years to solve. Some researchers suggest it might even hint at the existence of parallel universes! However, not everyone is convinced. From the foundations of the multiverse theory to the controversies surrounding quantum supremacy, we explore it all. Get ready for an eye-opening look into the revolutionary world of quantum computing!
Chapters:
00:00 Introduction
00:42 The Quantum Leap: Google’s Groundbreaking Achievement
03:37 The Multiverse Link: Exploring the Theoretical Basis
06:09 Skepticism and Boundaries: Verifying the Claims
08:12 Other Theories of the Universe
11:31 Outro
💼 Business Inquiries and Contact
• For business inquiries, copyright matters or other inquiries please contact us at:
[email protected]
⚠️ Copyright Disclaimers
• We use images and content in accordance with the YouTube Fair Use copyright guidelines
• Section 107 of the U.S. Copyright Act states: “Notwithstanding the provisions of sections 106 and 106A, the fair use of a copyrighted work, including such use by reproduction in copies or phonorecords or by any other means specified by that section, for purposes such as criticism, comment, news reporting, teaching (including multiple copies for classroom use), scholarship, or research, is not an infringement of copyright.”
• This video could contain certain copyrighted video clips, pictures, or photographs that were not specifically authorized to be used by the copyright holder(s), but which we believe in good faith are protected by federal law and the fair use doctrine for one or more of the reasons noted above.
https://wn.com/Google’S_Quantum_Ai_Chip_Just_Tapped_Into_Parallel_Universes_But_There's_A_Catch...
#QuantumAI #QuantumScience #WillowChip
Google’s Quantum AI Chip Just Tapped Into Parallel Universes but there's a Catch...
Google’s latest quantum chip, Willow, is making waves and stirring debate. This 105-qubit marvel tackled a problem in under five minutes that would take classical supercomputers an unimaginable 10 septillion years to solve. Some researchers suggest it might even hint at the existence of parallel universes! However, not everyone is convinced. From the foundations of the multiverse theory to the controversies surrounding quantum supremacy, we explore it all. Get ready for an eye-opening look into the revolutionary world of quantum computing!
Chapters:
00:00 Introduction
00:42 The Quantum Leap: Google’s Groundbreaking Achievement
03:37 The Multiverse Link: Exploring the Theoretical Basis
06:09 Skepticism and Boundaries: Verifying the Claims
08:12 Other Theories of the Universe
11:31 Outro
💼 Business Inquiries and Contact
• For business inquiries, copyright matters or other inquiries please contact us at:
[email protected]
⚠️ Copyright Disclaimers
• We use images and content in accordance with the YouTube Fair Use copyright guidelines
• Section 107 of the U.S. Copyright Act states: “Notwithstanding the provisions of sections 106 and 106A, the fair use of a copyrighted work, including such use by reproduction in copies or phonorecords or by any other means specified by that section, for purposes such as criticism, comment, news reporting, teaching (including multiple copies for classroom use), scholarship, or research, is not an infringement of copyright.”
• This video could contain certain copyrighted video clips, pictures, or photographs that were not specifically authorized to be used by the copyright holder(s), but which we believe in good faith are protected by federal law and the fair use doctrine for one or more of the reasons noted above.
- published: 03 Jan 2025
- views: 9699
0:12
uhhh na na edit ✨ #shorts
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Mercury (planet)
Ar...
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Mercury (planet)
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"First planet" redirects here. For other systems of numbering planets, see Planet § History and etymology. For other uses, see Mercury (disambiguation).
Mercury is the first planet from the Sun and the smallest in the Solar System. In English, it is named after the ancient Roman god Mercurius (Mercury), god of commerce and communication, and the messenger of the gods. Mercury is classified as a terrestrial planet, with roughly the same surface gravity as Mars. The surface of Mercury is heavily cratered, as a result of countless impact events that have accumulated over billions of years. Its largest crater, Caloris Planitia, has a diameter of 1,550 km (960 mi) and one-third the diameter of the planet (4,880 km or 3,030 mi). Similarly to the Earth's Moon, Mercury's surface displays an expansive rupes system generated from thrust faults and bright ray systems formed by impact event remnants.
Mercury
Mercury in true color (by MESSENGER in 2008)
Designations
Pronunciation
/ˈmɜːrkjʊri/ ⓘ
Adjectives
Mercurian /mərˈkjʊəriən/,[1]
Mercurial /mərˈkjʊəriəl/[2]
Symbol
☿
Orbital characteristics[3]
Epoch J2000
Aphelion
0.466697 AU (69.82 million km)
Perihelion
0.307499 AU (46.00 million km)
Semi-major axis
0.387098 AU (57.91 million km)
Eccentricity
0.205630[4]
Orbital period (sidereal)
87.9691 d
0.240846 yr
0.5 Mercury synodic days
Orbital period (synodic)
115.88 d[4]
Average orbital speed
47.36 km/s[4]
Mean anomaly
174.796°
Inclination
7.005° to ecliptic
3.38° to Sun's equator
6.35° to invariable plane[5]
Longitude of ascending node
48.331°
Argument of perihelion
29.124°
Satellites
None
Physical characteristics
Mean radius
2,439.7±1.0 km[6][7]
0.3829 Earths
Flattening
0.0009[4]
Surface area
7.48×107 km2[6]
0.147 Earths
Volume
6.083×1010 km3[6]
0.056 Earths
Mass
3.3011×1023 kg[8]
0.055 Earths
Mean density
5.427 g/cm3[6]
Surface gravity
3.7 m/s2 (0.38 g0)[6]
Moment of inertia factor
0.346±0.014[9]
Escape velocity
4.25 km/s[6]
Synodic rotation period
176 d[10]
Sidereal rotation period
58.646 d
1407.5 h[6]
Equatorial rotation velocity
10.892 km/h (3.026 m/s)
Axial tilt
2.04′ ± 0.08′ (to orbit)[9]
(0.034°)[4]
North pole right ascension
18h 44m 2s
281.01°[4]
North pole declination
61.45°[4]
Albedo
0.088 (Bond)[11]
0.142 (geom.)[12]
Temperature
437 K (164 °C) (blackbody temperature)[13]
Surface temp. min mean max
0°N, 0°W [14] −173 °C 67 °C 427 °C
85°N, 0°W[14] −193 °C −73 °C 106.85 °C
Apparent magnitude
−2.48 to +7.25[15]
Absolute magnitude (H)
−0.4[16]
Angular diameter
4.5–13″[4]
Atmosphere[4][17][18]
Surface pressure
trace (≲ 0.5 nPa)
Composition by volume
atomic oxygen
sodium
magnesium
atomic hydrogen
potassium
calcium
helium
Trace amounts of iron, aluminium, argon, dinitrogen, dioxygen, carbon dioxide, water vapor, xenon, krypton, and neon
Mercury's sidereal year (88.0 Earth days) and sidereal day (58.65 Earth days) are in a 3:2 ratio. This relationship is called spin–orbit resonance, and sidereal here means "relative to the stars". Consequently, one solar day (sunrise to sunrise) on Mercury lasts for around 176 Earth days: twice the planet's sidereal year. This means that one side of Mercury will remain in sunlight for one Mercurian year of 88 Earth days; while during the next orbit, that side will be in darkness all the time until the next sunrise after another 88 Earth days.
Combined with its high orbital eccentricity, the planet's surface has widely varying sunlight intensity and temperature, with the equatorial regions ranging from −170 °C (−270 °F) at night to 420 °C (790 °F) during sunlight. Due to the very small axial tilt, the planet's poles are permanently shadowed. This strongly suggests that water ice could be present in the craters. Above the planet's surface is an extremely tenuous exosphere and a faint magnetic field that is strong enough to deflect solar winds. Mercury has no natural satellite.
As of the early 2020s, many broad details of Mercury's geological history are still under investigation or pending data from space probes. Like other planets in the Solar System, Mercury was formed approximately 4.5 billion years ago. Its mantle is highly homogeneous, which suggests that Mercury had a magma ocean early in its history, like the Moon. According to current models, Mercury may have a solid silicate crust and mantle overlying a solid outer core, a deeper liquid core layer, and a solid inner core. There are many competing hypotheses about Mercury's origins and development, some of which incorporate collision with planetesimals and rock vaporization.
Nomenclature
Physical characteristics
Orbit, rotation, and longitude
Observation
Observation history
See also
Notes
References
External links
Last edited 12 hours ago by 1Martin33
Wikipedia
Content is available under CC BY-SA 4.0 unless
https://wn.com/Uhhh_Na_Na_Edit_✨_Shorts
Wikipedia
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Join the Wikidata contest and help improve geographically located items in 16 countries!
Coordinate Me ❭ MAY 2024
Mercury (planet)
Article Talk
Language
Download PDF
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View source
"First planet" redirects here. For other systems of numbering planets, see Planet § History and etymology. For other uses, see Mercury (disambiguation).
Mercury is the first planet from the Sun and the smallest in the Solar System. In English, it is named after the ancient Roman god Mercurius (Mercury), god of commerce and communication, and the messenger of the gods. Mercury is classified as a terrestrial planet, with roughly the same surface gravity as Mars. The surface of Mercury is heavily cratered, as a result of countless impact events that have accumulated over billions of years. Its largest crater, Caloris Planitia, has a diameter of 1,550 km (960 mi) and one-third the diameter of the planet (4,880 km or 3,030 mi). Similarly to the Earth's Moon, Mercury's surface displays an expansive rupes system generated from thrust faults and bright ray systems formed by impact event remnants.
Mercury
Mercury in true color (by MESSENGER in 2008)
Designations
Pronunciation
/ˈmɜːrkjʊri/ ⓘ
Adjectives
Mercurian /mərˈkjʊəriən/,[1]
Mercurial /mərˈkjʊəriəl/[2]
Symbol
☿
Orbital characteristics[3]
Epoch J2000
Aphelion
0.466697 AU (69.82 million km)
Perihelion
0.307499 AU (46.00 million km)
Semi-major axis
0.387098 AU (57.91 million km)
Eccentricity
0.205630[4]
Orbital period (sidereal)
87.9691 d
0.240846 yr
0.5 Mercury synodic days
Orbital period (synodic)
115.88 d[4]
Average orbital speed
47.36 km/s[4]
Mean anomaly
174.796°
Inclination
7.005° to ecliptic
3.38° to Sun's equator
6.35° to invariable plane[5]
Longitude of ascending node
48.331°
Argument of perihelion
29.124°
Satellites
None
Physical characteristics
Mean radius
2,439.7±1.0 km[6][7]
0.3829 Earths
Flattening
0.0009[4]
Surface area
7.48×107 km2[6]
0.147 Earths
Volume
6.083×1010 km3[6]
0.056 Earths
Mass
3.3011×1023 kg[8]
0.055 Earths
Mean density
5.427 g/cm3[6]
Surface gravity
3.7 m/s2 (0.38 g0)[6]
Moment of inertia factor
0.346±0.014[9]
Escape velocity
4.25 km/s[6]
Synodic rotation period
176 d[10]
Sidereal rotation period
58.646 d
1407.5 h[6]
Equatorial rotation velocity
10.892 km/h (3.026 m/s)
Axial tilt
2.04′ ± 0.08′ (to orbit)[9]
(0.034°)[4]
North pole right ascension
18h 44m 2s
281.01°[4]
North pole declination
61.45°[4]
Albedo
0.088 (Bond)[11]
0.142 (geom.)[12]
Temperature
437 K (164 °C) (blackbody temperature)[13]
Surface temp. min mean max
0°N, 0°W [14] −173 °C 67 °C 427 °C
85°N, 0°W[14] −193 °C −73 °C 106.85 °C
Apparent magnitude
−2.48 to +7.25[15]
Absolute magnitude (H)
−0.4[16]
Angular diameter
4.5–13″[4]
Atmosphere[4][17][18]
Surface pressure
trace (≲ 0.5 nPa)
Composition by volume
atomic oxygen
sodium
magnesium
atomic hydrogen
potassium
calcium
helium
Trace amounts of iron, aluminium, argon, dinitrogen, dioxygen, carbon dioxide, water vapor, xenon, krypton, and neon
Mercury's sidereal year (88.0 Earth days) and sidereal day (58.65 Earth days) are in a 3:2 ratio. This relationship is called spin–orbit resonance, and sidereal here means "relative to the stars". Consequently, one solar day (sunrise to sunrise) on Mercury lasts for around 176 Earth days: twice the planet's sidereal year. This means that one side of Mercury will remain in sunlight for one Mercurian year of 88 Earth days; while during the next orbit, that side will be in darkness all the time until the next sunrise after another 88 Earth days.
Combined with its high orbital eccentricity, the planet's surface has widely varying sunlight intensity and temperature, with the equatorial regions ranging from −170 °C (−270 °F) at night to 420 °C (790 °F) during sunlight. Due to the very small axial tilt, the planet's poles are permanently shadowed. This strongly suggests that water ice could be present in the craters. Above the planet's surface is an extremely tenuous exosphere and a faint magnetic field that is strong enough to deflect solar winds. Mercury has no natural satellite.
As of the early 2020s, many broad details of Mercury's geological history are still under investigation or pending data from space probes. Like other planets in the Solar System, Mercury was formed approximately 4.5 billion years ago. Its mantle is highly homogeneous, which suggests that Mercury had a magma ocean early in its history, like the Moon. According to current models, Mercury may have a solid silicate crust and mantle overlying a solid outer core, a deeper liquid core layer, and a solid inner core. There are many competing hypotheses about Mercury's origins and development, some of which incorporate collision with planetesimals and rock vaporization.
Nomenclature
Physical characteristics
Orbit, rotation, and longitude
Observation
Observation history
See also
Notes
References
External links
Last edited 12 hours ago by 1Martin33
Wikipedia
Content is available under CC BY-SA 4.0 unless
- published: 28 May 2024
- views: 179
0:18
Despacito sad 😢 template #shorts
Wikipedia
Search
Join the Wikidata contest and help improve geographically located items in 16 countries!
Coordinate Me ❭ MAY 2024
Mercury (planet)
Ar...
Wikipedia
Search
Join the Wikidata contest and help improve geographically located items in 16 countries!
Coordinate Me ❭ MAY 2024
Mercury (planet)
Article Talk
Language
Download PDF
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View source
"First planet" redirects here. For other systems of numbering planets, see Planet § History and etymology. For other uses, see Mercury (disambiguation).
Mercury is the first planet from the Sun and the smallest in the Solar System. In English, it is named after the ancient Roman god Mercurius (Mercury), god of commerce and communication, and the messenger of the gods. Mercury is classified as a terrestrial planet, with roughly the same surface gravity as Mars. The surface of Mercury is heavily cratered, as a result of countless impact events that have accumulated over billions of years. Its largest crater, Caloris Planitia, has a diameter of 1,550 km (960 mi) and one-third the diameter of the planet (4,880 km or 3,030 mi). Similarly to the Earth's Moon, Mercury's surface displays an expansive rupes system generated from thrust faults and bright ray systems formed by impact event remnants.
Mercury
Mercury in true color (by MESSENGER in 2008)
Designations
Pronunciation
/ˈmɜːrkjʊri/ ⓘ
Adjectives
Mercurian /mərˈkjʊəriən/,[1]
Mercurial /mərˈkjʊəriəl/[2]
Symbol
☿
Orbital characteristics[3]
Epoch J2000
Aphelion
0.466697 AU (69.82 million km)
Perihelion
0.307499 AU (46.00 million km)
Semi-major axis
0.387098 AU (57.91 million km)
Eccentricity
0.205630[4]
Orbital period (sidereal)
87.9691 d
0.240846 yr
0.5 Mercury synodic days
Orbital period (synodic)
115.88 d[4]
Average orbital speed
47.36 km/s[4]
Mean anomaly
174.796°
Inclination
7.005° to ecliptic
3.38° to Sun's equator
6.35° to invariable plane[5]
Longitude of ascending node
48.331°
Argument of perihelion
29.124°
Satellites
None
Physical characteristics
Mean radius
2,439.7±1.0 km[6][7]
0.3829 Earths
Flattening
0.0009[4]
Surface area
7.48×107 km2[6]
0.147 Earths
Volume
6.083×1010 km3[6]
0.056 Earths
Mass
3.3011×1023 kg[8]
0.055 Earths
Mean density
5.427 g/cm3[6]
Surface gravity
3.7 m/s2 (0.38 g0)[6]
Moment of inertia factor
0.346±0.014[9]
Escape velocity
4.25 km/s[6]
Synodic rotation period
176 d[10]
Sidereal rotation period
58.646 d
1407.5 h[6]
Equatorial rotation velocity
10.892 km/h (3.026 m/s)
Axial tilt
2.04′ ± 0.08′ (to orbit)[9]
(0.034°)[4]
North pole right ascension
18h 44m 2s
281.01°[4]
North pole declination
61.45°[4]
Albedo
0.088 (Bond)[11]
0.142 (geom.)[12]
Temperature
437 K (164 °C) (blackbody temperature)[13]
Surface temp. min mean max
0°N, 0°W [14] −173 °C 67 °C 427 °C
85°N, 0°W[14] −193 °C −73 °C 106.85 °C
Apparent magnitude
−2.48 to +7.25[15]
Absolute magnitude (H)
−0.4[16]
Angular diameter
4.5–13″[4]
Atmosphere[4][17][18]
Surface pressure
trace (≲ 0.5 nPa)
Composition by volume
atomic oxygen
sodium
magnesium
atomic hydrogen
potassium
calcium
helium
Trace amounts of iron, aluminium, argon, dinitrogen, dioxygen, carbon dioxide, water vapor, xenon, krypton, and neon
Mercury's sidereal year (88.0 Earth days) and sidereal day (58.65 Earth days) are in a 3:2 ratio. This relationship is called spin–orbit resonance, and sidereal here means "relative to the stars". Consequently, one solar day (sunrise to sunrise) on Mercury lasts for around 176 Earth days: twice the planet's sidereal year. This means that one side of Mercury will remain in sunlight for one Mercurian year of 88 Earth days; while during the next orbit, that side will be in darkness all the time until the next sunrise after another 88 Earth days.
Combined with its high orbital eccentricity, the planet's surface has widely varying sunlight intensity and temperature, with the equatorial regions ranging from −170 °C (−270 °F) at night to 420 °C (790 °F) during sunlight. Due to the very small axial tilt, the planet's poles are permanently shadowed. This strongly suggests that water ice could be present in the craters. Above the planet's surface is an extremely tenuous exosphere and a faint magnetic field that is strong enough to deflect solar winds. Mercury has no natural satellite.
As of the early 2020s, many broad details of Mercury's geological history are still under investigation or pending data from space probes. Like other planets in the Solar System, Mercury was formed approximately 4.5 billion years ago. Its mantle is highly homogeneous, which suggests that Mercury had a magma ocean early in its history, like the Moon. According to current models, Mercury may have a solid silicate crust and mantle overlying a solid outer core, a deeper liquid core layer, and a solid inner core. There are many competing hypotheses about Mercury's origins and development, some of which incorporate collision with planetesimals and rock vaporization.
Nomenclature
Physical characteristics
Orbit, rotation, and longitude
Observation
Observation history
See also
Notes
References
External links
Last edited 12 hours ago by 1Martin33
Wikipedia
Content is available under CC BY-SA 4.0 unless
https://wn.com/Despacito_Sad_😢_Template_Shorts
Wikipedia
Search
Join the Wikidata contest and help improve geographically located items in 16 countries!
Coordinate Me ❭ MAY 2024
Mercury (planet)
Article Talk
Language
Download PDF
Watch
View source
"First planet" redirects here. For other systems of numbering planets, see Planet § History and etymology. For other uses, see Mercury (disambiguation).
Mercury is the first planet from the Sun and the smallest in the Solar System. In English, it is named after the ancient Roman god Mercurius (Mercury), god of commerce and communication, and the messenger of the gods. Mercury is classified as a terrestrial planet, with roughly the same surface gravity as Mars. The surface of Mercury is heavily cratered, as a result of countless impact events that have accumulated over billions of years. Its largest crater, Caloris Planitia, has a diameter of 1,550 km (960 mi) and one-third the diameter of the planet (4,880 km or 3,030 mi). Similarly to the Earth's Moon, Mercury's surface displays an expansive rupes system generated from thrust faults and bright ray systems formed by impact event remnants.
Mercury
Mercury in true color (by MESSENGER in 2008)
Designations
Pronunciation
/ˈmɜːrkjʊri/ ⓘ
Adjectives
Mercurian /mərˈkjʊəriən/,[1]
Mercurial /mərˈkjʊəriəl/[2]
Symbol
☿
Orbital characteristics[3]
Epoch J2000
Aphelion
0.466697 AU (69.82 million km)
Perihelion
0.307499 AU (46.00 million km)
Semi-major axis
0.387098 AU (57.91 million km)
Eccentricity
0.205630[4]
Orbital period (sidereal)
87.9691 d
0.240846 yr
0.5 Mercury synodic days
Orbital period (synodic)
115.88 d[4]
Average orbital speed
47.36 km/s[4]
Mean anomaly
174.796°
Inclination
7.005° to ecliptic
3.38° to Sun's equator
6.35° to invariable plane[5]
Longitude of ascending node
48.331°
Argument of perihelion
29.124°
Satellites
None
Physical characteristics
Mean radius
2,439.7±1.0 km[6][7]
0.3829 Earths
Flattening
0.0009[4]
Surface area
7.48×107 km2[6]
0.147 Earths
Volume
6.083×1010 km3[6]
0.056 Earths
Mass
3.3011×1023 kg[8]
0.055 Earths
Mean density
5.427 g/cm3[6]
Surface gravity
3.7 m/s2 (0.38 g0)[6]
Moment of inertia factor
0.346±0.014[9]
Escape velocity
4.25 km/s[6]
Synodic rotation period
176 d[10]
Sidereal rotation period
58.646 d
1407.5 h[6]
Equatorial rotation velocity
10.892 km/h (3.026 m/s)
Axial tilt
2.04′ ± 0.08′ (to orbit)[9]
(0.034°)[4]
North pole right ascension
18h 44m 2s
281.01°[4]
North pole declination
61.45°[4]
Albedo
0.088 (Bond)[11]
0.142 (geom.)[12]
Temperature
437 K (164 °C) (blackbody temperature)[13]
Surface temp. min mean max
0°N, 0°W [14] −173 °C 67 °C 427 °C
85°N, 0°W[14] −193 °C −73 °C 106.85 °C
Apparent magnitude
−2.48 to +7.25[15]
Absolute magnitude (H)
−0.4[16]
Angular diameter
4.5–13″[4]
Atmosphere[4][17][18]
Surface pressure
trace (≲ 0.5 nPa)
Composition by volume
atomic oxygen
sodium
magnesium
atomic hydrogen
potassium
calcium
helium
Trace amounts of iron, aluminium, argon, dinitrogen, dioxygen, carbon dioxide, water vapor, xenon, krypton, and neon
Mercury's sidereal year (88.0 Earth days) and sidereal day (58.65 Earth days) are in a 3:2 ratio. This relationship is called spin–orbit resonance, and sidereal here means "relative to the stars". Consequently, one solar day (sunrise to sunrise) on Mercury lasts for around 176 Earth days: twice the planet's sidereal year. This means that one side of Mercury will remain in sunlight for one Mercurian year of 88 Earth days; while during the next orbit, that side will be in darkness all the time until the next sunrise after another 88 Earth days.
Combined with its high orbital eccentricity, the planet's surface has widely varying sunlight intensity and temperature, with the equatorial regions ranging from −170 °C (−270 °F) at night to 420 °C (790 °F) during sunlight. Due to the very small axial tilt, the planet's poles are permanently shadowed. This strongly suggests that water ice could be present in the craters. Above the planet's surface is an extremely tenuous exosphere and a faint magnetic field that is strong enough to deflect solar winds. Mercury has no natural satellite.
As of the early 2020s, many broad details of Mercury's geological history are still under investigation or pending data from space probes. Like other planets in the Solar System, Mercury was formed approximately 4.5 billion years ago. Its mantle is highly homogeneous, which suggests that Mercury had a magma ocean early in its history, like the Moon. According to current models, Mercury may have a solid silicate crust and mantle overlying a solid outer core, a deeper liquid core layer, and a solid inner core. There are many competing hypotheses about Mercury's origins and development, some of which incorporate collision with planetesimals and rock vaporization.
Nomenclature
Physical characteristics
Orbit, rotation, and longitude
Observation
Observation history
See also
Notes
References
External links
Last edited 12 hours ago by 1Martin33
Wikipedia
Content is available under CC BY-SA 4.0 unless
- published: 12 Jun 2024
- views: 212
0:21
definition of causality
This simple example of causality is given as public service for those, like me, who struggle a little with the plethora of wikipedia disambiguation articles on ...
This simple example of causality is given as public service for those, like me, who struggle a little with the plethora of wikipedia disambiguation articles on the term, all full of mathematical formulae, discussion of things like causal dynamical triangulation, and sentences like:
"Causality should not be confused with Newton's second law, which is related to the conservation of momentum, and is a consequence of the spatial homogeneity of physical laws. The name causality suggests that all effects must have specific causes, which is a concept unrelated to the common use of causality in physics, and is violated in some mainstream interpretations of quantum mechanics."
Anyhoo, you can read through the whole thing here: https://en.wikipedia.org/wiki/Causality
... but don't worry if you don't understand it all, just refer back to this video if you get stuck on any part of the formal definition.
https://wn.com/Definition_Of_Causality
This simple example of causality is given as public service for those, like me, who struggle a little with the plethora of wikipedia disambiguation articles on the term, all full of mathematical formulae, discussion of things like causal dynamical triangulation, and sentences like:
"Causality should not be confused with Newton's second law, which is related to the conservation of momentum, and is a consequence of the spatial homogeneity of physical laws. The name causality suggests that all effects must have specific causes, which is a concept unrelated to the common use of causality in physics, and is violated in some mainstream interpretations of quantum mechanics."
Anyhoo, you can read through the whole thing here: https://en.wikipedia.org/wiki/Causality
... but don't worry if you don't understand it all, just refer back to this video if you get stuck on any part of the formal definition.
- published: 29 Jul 2017
- views: 79