The possible structure of silicate anion in Spodumene mineral should be suggested. Concept introduction: Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals S i O 4 4 − is the basic unit. Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust. Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

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Answer 1

Question

Chapter 19, Problem 19.65SP

(a)

Interpretation Introduction

Interpretation:

The possible structure of silicate anion in Spodumene mineral should be suggested.

Concept introduction:

Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals SiO44− is the basic unit.

Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust.

Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

(b)

Interpretation Introduction

Interpretation:

The possible structure of silicate anion in Wollastonite mineral should be suggested.

Concept introduction:

Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals SiO44− is the basic unit.

Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust.

Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

(c)

Interpretation Introduction

Interpretation:

The possible structure of silicate anion in Thortveitite mineral should be suggested.

Concept introduction:

Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals SiO44− is the basic unit.

Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust.

Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

(d)

Interpretation Introduction

Interpretation:

The possible structure of silicate anion in Albite mineral should be suggested.

Concept introduction:

Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals SiO44− is the basic unit.

Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust.

Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

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Answer 2

Question

Chapter 19, Problem 19.65SP

(a)

Interpretation Introduction

Interpretation:

The possible structure of silicate anion in Spodumene mineral should be suggested.

Concept introduction:

Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals SiO44− is the basic unit.

Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust.

Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

(b)

Interpretation Introduction

Interpretation:

The possible structure of silicate anion in Wollastonite mineral should be suggested.

Concept introduction:

Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals SiO44− is the basic unit.

Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust.

Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

(c)

Interpretation Introduction

Interpretation:

The possible structure of silicate anion in Thortveitite mineral should be suggested.

Concept introduction:

Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals SiO44− is the basic unit.

Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust.

Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

(d)

Interpretation Introduction

Interpretation:

The possible structure of silicate anion in Albite mineral should be suggested.

Concept introduction:

Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals SiO44− is the basic unit.

Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust.

Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

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Answer 3

Question

Chapter 19, Problem 19.65SP

(a)

Interpretation Introduction

Interpretation:

The possible structure of silicate anion in Spodumene mineral should be suggested.

Concept introduction:

Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals SiO44− is the basic unit.

Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust.

Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

(b)

Interpretation Introduction

Interpretation:

The possible structure of silicate anion in Wollastonite mineral should be suggested.

Concept introduction:

Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals SiO44− is the basic unit.

Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust.

Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

(c)

Interpretation Introduction

Interpretation:

The possible structure of silicate anion in Thortveitite mineral should be suggested.

Concept introduction:

Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals SiO44− is the basic unit.

Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust.

Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

(d)

Interpretation Introduction

Interpretation:

The possible structure of silicate anion in Albite mineral should be suggested.

Concept introduction:

Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals SiO44− is the basic unit.

Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust.

Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

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Answer 4

Question

Chapter 19, Problem 19.65SP

(a)

Interpretation Introduction

Interpretation:

The possible structure of silicate anion in Spodumene mineral should be suggested.

Concept introduction:

Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals SiO44− is the basic unit.

Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust.

Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

(b)

Interpretation Introduction

Interpretation:

The possible structure of silicate anion in Wollastonite mineral should be suggested.

Concept introduction:

Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals SiO44− is the basic unit.

Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust.

Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

(c)

Interpretation Introduction

Interpretation:

The possible structure of silicate anion in Thortveitite mineral should be suggested.

Concept introduction:

Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals SiO44− is the basic unit.

Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust.

Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

(d)

Interpretation Introduction

Interpretation:

The possible structure of silicate anion in Albite mineral should be suggested.

Concept introduction:

Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals SiO44− is the basic unit.

Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust.

Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

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Answer 5

Chapter 19, Problem 19.65SP

(a)

Interpretation Introduction

Interpretation:

The possible structure of silicate anion in Spodumene mineral should be suggested.

Concept introduction:

Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals SiO44− is the basic unit.

Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust.

Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

(b)

Interpretation Introduction

Interpretation:

The possible structure of silicate anion in Wollastonite mineral should be suggested.

Concept introduction:

Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals SiO44− is the basic unit.

Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust.

Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

(c)

Interpretation Introduction

Interpretation:

The possible structure of silicate anion in Thortveitite mineral should be suggested.

Concept introduction:

Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals SiO44− is the basic unit.

Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust.

Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

(d)

Interpretation Introduction

Interpretation:

The possible structure of silicate anion in Albite mineral should be suggested.

Concept introduction:

Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals SiO44− is the basic unit.

Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust.

Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

Answer 6

Chapter 19, Problem 19.65SP

(a)

Interpretation Introduction

Interpretation:

The possible structure of silicate anion in Spodumene mineral should be suggested.

Concept introduction:

Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals SiO44− is the basic unit.

Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust.

Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

Answer 7

Chapter 19, Problem 19.65SP

(a)

Interpretation Introduction

Interpretation:

The possible structure of silicate anion in Spodumene mineral should be suggested.

Concept introduction:

Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals SiO44− is the basic unit.

Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust.

Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

Answer 8

(b)

Interpretation Introduction

Interpretation:

The possible structure of silicate anion in Wollastonite mineral should be suggested.

Concept introduction:

Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals SiO44− is the basic unit.

Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust.

Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

Answer 9

(b)

Interpretation Introduction

Interpretation:

The possible structure of silicate anion in Wollastonite mineral should be suggested.

Concept introduction:

Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals SiO44− is the basic unit.

Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust.

Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

Answer 10

(c)

Interpretation Introduction

Interpretation:

The possible structure of silicate anion in Thortveitite mineral should be suggested.

Concept introduction:

Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals SiO44− is the basic unit.

Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust.

Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

Answer 11

(c)

Interpretation Introduction

Interpretation:

The possible structure of silicate anion in Thortveitite mineral should be suggested.

Concept introduction:

Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals SiO44− is the basic unit.

Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust.

Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

Answer 12

(d)

Interpretation Introduction

Interpretation:

The possible structure of silicate anion in Albite mineral should be suggested.

Concept introduction:

Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals SiO44− is the basic unit.

Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust.

Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

Answer 13

(d)

Interpretation Introduction

Interpretation:

The possible structure of silicate anion in Albite mineral should be suggested.

Concept introduction:

Silicates: It is frame work based on the linkage of cation cantered coordination polyhedron. The silica tetrahedral, the building block of the silicate minerals SiO44− is the basic unit.

Silicates minerals: All silicates minerals contain some combination of Si and oxygen (O), make up 96% of Earth crust.

Non-silicate minerals: It is indicated by the name they contain no silicon and fall into one of six class of non-silicate. It only 4% of earth crust is made of non-silicates.

Answer 14

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Answer 15

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Answer 16

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Answer 17

Ch. 19.1 - Prob. 19.1P Ch. 19.2 - Prob. 19.2P Ch. 19.2 - Prob. 19.3CP Ch. 19.4 - Prob. 19.4P Ch. 19.7 - Prob. 19.5P Ch. 19.8 - Prob. 19.6CP Ch. 19.10 - Prob. 19.7P Ch. 19.13 - Prob. 19.8CP Ch. 19.13 - Prob. 19.9P Ch. 19.14 - Prob. 19.10P

Solution Summary: The author explains the structure of silicate anion in Spodumene and Wollastonite.

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Chapter 19 Solutions