This document describes 32 cardboard models that represent the different crystal classes. It provides details on the symmetry elements that define each crystal class, including axes of rotation, planes of symmetry, and centers of symmetry. The crystal classes are grouped into cubic, tetragonal, orthorhombic, monoclinic, triclinic, and hexagonal systems. Each crystal class entry lists the symmetry elements that characterize its specific symmetry.
Derivation of 32 crystal classes If an imaginary plane divides the crystal in...abhinandpradeep2000
The theory of plate tectonics is widely accepted by scientists and provides a robust
21 framework with which to describe and predict the behavior of Earth’s rigid outer shell – the
22 lithosphere – in space and time. Expressions of plate tectonic interactions at the Earth’s
23 surface also provide critical insight into the machinations of our planet’s inaccessible interior,
24 and allow postulation about the geological characteristics of other rocky bodies in our solar
25 system and beyond. Formalization of this paradigm occurred at a landmark Penrose
In this lecture , the focus is on geological aspects of minerals. We are going to discuss about the crystal symmetry of minerals,axis of rotation , axis of rotoinversion symmetry y, and mirror plane. The crystal classes may be sub-divided into one of 6 crystal systems namely Triclinic, monoclinic, orthorhombic, tetragonal, hexagonal and isometric (cubic).
Crystallographic axis
The identification of specific symmetry operations enables one to orientate a crystal according g to an imaginary set of reference lines known as the crystallographic axis.With the exception of the hexagonal system, the axes are designated designated The ends of each a, b, and c. The ends of each axes are designated axes are designated + or -. This is important for the derivation of Miller Indices.
Derivation of 32 crystal classes If an imaginary plane divides the crystal in...abhinandpradeep2000
The theory of plate tectonics is widely accepted by scientists and provides a robust
21 framework with which to describe and predict the behavior of Earth’s rigid outer shell – the
22 lithosphere – in space and time. Expressions of plate tectonic interactions at the Earth’s
23 surface also provide critical insight into the machinations of our planet’s inaccessible interior,
24 and allow postulation about the geological characteristics of other rocky bodies in our solar
25 system and beyond. Formalization of this paradigm occurred at a landmark Penrose
In this lecture , the focus is on geological aspects of minerals. We are going to discuss about the crystal symmetry of minerals,axis of rotation , axis of rotoinversion symmetry y, and mirror plane. The crystal classes may be sub-divided into one of 6 crystal systems namely Triclinic, monoclinic, orthorhombic, tetragonal, hexagonal and isometric (cubic).
Crystallographic axis
The identification of specific symmetry operations enables one to orientate a crystal according g to an imaginary set of reference lines known as the crystallographic axis.With the exception of the hexagonal system, the axes are designated designated The ends of each a, b, and c. The ends of each axes are designated axes are designated + or -. This is important for the derivation of Miller Indices.
An Introduction to Crystallography, Elements of crystals crystal systems: Cubic (Isometric) System,Tetragonal System, Orthorhombic System, Hexagonal System; Trigonal System, Monoclinic System, Triclinic System
Three rock specimens presented at Collectors Night Gem and Mineral Society of Lynchburg, Sandstone Clinch Mountain Tennessee, Highway 221 Bedford Virginia, Kyanite Virginia
An Introduction to Crystallography, Elements of crystals crystal systems: Cubic (Isometric) System,Tetragonal System, Orthorhombic System, Hexagonal System; Trigonal System, Monoclinic System, Triclinic System
Three rock specimens presented at Collectors Night Gem and Mineral Society of Lynchburg, Sandstone Clinch Mountain Tennessee, Highway 221 Bedford Virginia, Kyanite Virginia
Learning Objective: Starting with five points do a calibration curve and linear regression analysis. Use the regression equation to calculate concentration from absorbance measurements.
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Nutraceutical market, scope and growth: Herbal drug technologyLokesh Patil
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Richard's aventures in two entangled wonderlandsRichard Gill
Since the loophole-free Bell experiments of 2020 and the Nobel prizes in physics of 2022, critics of Bell's work have retreated to the fortress of super-determinism. Now, super-determinism is a derogatory word - it just means "determinism". Palmer, Hance and Hossenfelder argue that quantum mechanics and determinism are not incompatible, using a sophisticated mathematical construction based on a subtle thinning of allowed states and measurements in quantum mechanics, such that what is left appears to make Bell's argument fail, without altering the empirical predictions of quantum mechanics. I think however that it is a smoke screen, and the slogan "lost in math" comes to my mind. I will discuss some other recent disproofs of Bell's theorem using the language of causality based on causal graphs. Causal thinking is also central to law and justice. I will mention surprising connections to my work on serial killer nurse cases, in particular the Dutch case of Lucia de Berk and the current UK case of Lucy Letby.
THE IMPORTANCE OF MARTIAN ATMOSPHERE SAMPLE RETURN.Sérgio Sacani
The return of a sample of near-surface atmosphere from Mars would facilitate answers to several first-order science questions surrounding the formation and evolution of the planet. One of the important aspects of terrestrial planet formation in general is the role that primary atmospheres played in influencing the chemistry and structure of the planets and their antecedents. Studies of the martian atmosphere can be used to investigate the role of a primary atmosphere in its history. Atmosphere samples would also inform our understanding of the near-surface chemistry of the planet, and ultimately the prospects for life. High-precision isotopic analyses of constituent gases are needed to address these questions, requiring that the analyses are made on returned samples rather than in situ.
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.
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/
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.
A brief information about the SCOP protein database used in bioinformatics.
The Structural Classification of Proteins (SCOP) database is a comprehensive and authoritative resource for the structural and evolutionary relationships of proteins. It provides a detailed and curated classification of protein structures, grouping them into families, superfamilies, and folds based on their structural and sequence similarities.
2. Crystal Classes, 32 Cardboard Models
Presenting 32 cardboard models of crystal systems as described in Crystal and
Crystal Growing by Alan Holden and Phyllis Morrison, MIT Press 1999
5. Crystal Class 4/m bar 3 2/m - Oh
Three 4-fold axes through opposite faces
Four 3-fold axes through opposite corners
Six 2-fold axes through opposite edges
Three planes parallel to faces, cubic planes
Six planes through opposite edges, dodecahedral planes
Center of symmetry
6.
7.
8. Crystal Class Bar 4 3 m - Td
Four 3-fold axes
Three 2-fold axes through opposite faces
Six dodecahedral planes
9.
10. Crystal Class 2/m bar 3 - Th
Four 3-fold axes
Three 2-fold axes through opposite faces
Three cubic planes
Center of symmetry
11.
12. Crystal Class 4 3 2 - O
Three 4-fold axes
Four 3-fold axes
Six 2-fold axes through opposite edges
13.
14. Crystal Class 2 3 - T
Four 3-fold axes
Three 2-fold axes through opposite faces
18. Crystal Class - 4/m 2/m 2/m D4h
One 4-fold axes through the two square faces
Four 2-fold axes perpendicular to the 4-fold axis, two of them throuth opposite
faces and the other two through opposite edges
Five planes (a) 0ne perpendicular to the 4-fold axis (b) two containing that axis
and parrallel to opposite faces (c) two containing that axis and passing through
opposite edges
Center of symmetry
19.
20.
21. Crystal Class - 4mm C4v
One four-fold axis
Four planes containing that axis
22.
23.
24. Crystal Class - 4/m C4h
One four-fold axis
One plane perpendicular to that axis
25.
26.
27. Crystal Class - 422 D4
One four-fold axis
Four two fold axis
28.
29.
30. Crystal Class - bar 4 2 m D2d
4-fold alternating axis
Two 2-fold axes perpendicular to the 4-fold alternating axis through opposite
edges
Two planes containing the 4-fold alternating axis parrallel to opposite faces
41. Crystal Class 2/m 2/m 2/m - D2h
Three mutually perpendicular 2 fold axes through opposite faces
Three planes parallel to opposite faces
Center of symmetry
42.
43.
44. Crystal Class mm2 - C2v
One 2 fold axis
Two planes containing that axis
71. Crystal Class 6/m 2/m 2/m D6h [1]
One 6 fold axis
Six 2 fold axes perpendicular to the 6 fold axis three of them through opposite
faces and three through opposite edges
Seven planes a) one perpendicular to the 6 fold axis
b) three containing that axis and passing through opposite faces
c) three containing that axis and passing through opposite edges
Center of gravity
72.
73.
74. Crystal Class 6mm - C6v [2]
One 6 fold axis, six planes containing that axis
75.
76.
77. Crystal Class 6/m - C6h [3]
One 6 fold axis, one palne perpendicular to that axis center of symmetry
86. Crystal Class bar 6 m 2 - D3h [6]
One 3-fold axis, three 2-fold axes through opposite faces, three planes through
opposite faces, one plane perpendicular to the 3-fold axis
87.
88.
89. Crystal Class bar 6 - C3h [7]
One 3-fold axis
One plane perpendicular to that axis
90.
91.
92. Crystal Class 8
One 3-fold axis which is a 6-fold alternating axis, inversion axis
Three 2-fold axes passing through opposite faces
Three planes passing through opposite edges
Center of symmetry
93.
94.
95. Crystal Class 3 m - C3v [9]
One 3-fold axis,three planes through opposite edges
96.
97.
98. Crystal Class bar 3 2/m - D3d [10]
One 3-fold axis
Three 2-fold axes through opposite faces
99.
100.
101. Crystal Class bar 6 - C3h [11]
One 6-fold alternating axis
Center of symmetry