Exam 2 Flashcards

1
Q

Electronic Configuration

Completed shells

Ionic bond

Covalent bond

Metallic bond

Van der Waals bond

Hydrogen bond

A

list the budget of the electrons in each of the shells and subshells

Noble gas electronic configuration

opposite charges attract electron clouds together

incomple outer shell merge

electrons shared freely through lattice

weak interactions

polarized portions of molecule “stick” together

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2
Q

Ionization potential

Electron negativity

Coordination number

A

The amount of energy to deprive an atom of one or more electrons

Tendency of an atom to attract electrons into its outer shell empirical

Is the number of ions or atoms immediately surround an atom or ions of interest

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3
Q

Pauling/Goldschmidt 1st Rule

A

The distance between cation-anion = total radi
Use Rc/Ra to determine the coordination number
Pure metals have Rc/Ra =1 => PCC or HCP
If the center cation become smaller than the XII site, it drops to the next lower coordination number
It will do this even if it is slightly too large for the next lower site
It is easy to fit slightly large cation

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4
Q

Pauling/Goldschmidt 2nd Rule

A

Electronic bond strength = valance/CR (coordination number)
“the electrostatic valance principle”
an ionic structure will be stable to extent that the sum of the strengths of electrostatic bonds that reach an anion from adjacent cations = the charge of that anion

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5
Q

Pauling/Goldschmidt 3rd Rule

A

The sharing of edges, particular of faces, of adjacent polyhedra tends to decrease the stability of an ionic structure

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6
Q

Pauling/Goldschmidt 4th Rule

A

In a crystal with different cations, those of high valance and low coordination number tend not to share polyhedral elements

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7
Q

Pauling/Goldschmidt 5th Rule

A

The number of different kinds of constituents in a crystal tends to be small
Using the analogy of CP oxygens, this rule states that the number of interstitial sites that are filled in a regular and periodic array tends to be small

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8
Q

Solid Solution

Substitutional

Couple substitution

Interstitial

Omission

A

a mineral structure in which specific atomic sites are occupied in variable proportions by 2 or more different chemical elements or groups

One element substitutes for another

2 elements with different charges swap to preserve charge balance

extra atoms added to a structure

atoms omitted from the structure in a regular way

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9
Q

Interstitial solid solution

A

extra atoms added to structure

usually neutrals or occupied with an omission or subtristiution

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10
Q

Omission solid asolt

A

vacant sites in structure

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11
Q

Exolution

A

Homogeneous crystal solid seperate

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12
Q

Phase transformation
Polymorphism

Polymorph

Polymorphous or Polymorphic

A

the transformation of mineral structure in a single composition depending on extrinsic variables

one or group of minerals with a single composition

having the same composition but different structures

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13
Q

Purephase

Pseudomorphism

A

no solid solution

the replacement of 1 mineral by another while retaining characteristic (eg shape, texture) of the 1st mineral

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14
Q

Solid solid net transfer reactions

A

Involve solids only, different composition, material must diffuse from one site to another for reactions to proceed

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15
Q

Continuous (multivariate) reactions

A

Phases change proportions and composition, but do not suddenly appear or disappear

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16
Q

Quantitative mineral analysis

A

when we break down the rock, always oxide presents inside

17
Q

X-Ray Diffraction

A

important tool to study minerals, coordination, the arrangment and number of ions surrounding a central ion

18
Q

Diffraction

A

Wavelength of incoming diffracted radiation is near the spacing of the structure being imaged

19
Q

Bragg’s Law

A

lamda = 2d sin theta

20
Q

Precession picture

A

Each point is a single plane (111), shows symmetry, internsities give positions of atoms in the unit cell, used to calculate positions of atoms in structure, including very complex proteins (e.g DNA)

21
Q

Power diffractometer

A

Finely ground sample
Crystals in random orientations (often moving)
X-ray beam interacts with many crystals
All possible reflection are recorded
Simple and powerful technique for geolgy
Film image to determine d for many (hkl) planes at once

22
Q

Defractogram

A

define X-Ray structure, crystal composition
Mixtures of minerals
Reflections are not always perfectly reproduced
Instrument noises
Multiple minerals
Detective work
XRD Patterns of the soils