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GEOL 650 – Clay Mineralogy
Instructor: Prof. Ahmet Umran Dogan
Clay Minerals:
Classifications, Identifications, Structures, and Applications
Omar A. Radwan
g201306050
ESD
1
OUTLINE
• Introduction
• Structures
– T
– O
– I
• Classifications
– TO
– TOT
• Identifications
– XRD
• Applications
• Concluding remarks
2
INTRODUCTION
• Group: Phyllosilicate
• Composition: hydrous aluminosilicates
• Formation occurs under:
– surface (alterites, soils, sediments) conditions or
– subsurface (diagenesis, hydrothermal alterations) conditions
• Size: few micrometers maximum
– Difficult to observe without using electron microscopy
3
STRUCTURES - T
• The Tetrahedral Sheet (T)
• SiO4
−4 or AlO4
−5 Tetrahedra
• linked together by sharing three of
four vertices (three basal oxygens)
• Only one O-2 anion (apical oxygen)
bonds cation pair
Murray, 2007
4
STRUCTURES - O
• The Octahedral Sheet (O)
• linked together by sharing their six
vertices
• Each anion is bonded to three
cations in the trioctahedral type
• Each anion is bonded to two
cations in the dioctahedral type
Murray, 2007
5
STRUCTURES - TO
Nesse, 2012
6
STRUCTURES - I
• The Interlayer Sheet (I)
• In 2:1 phyllosilicates
• interlayer cations compensate the negative charges in excess and
insure the electrical neutrality of the 2:1 layer
– Cations not bonded to each other (X)
– Cations forming an octahedral sheet without any shared vertex
with tetrahedral sheets (O)
Velde and Meunier, 2008
7
CLASSIFICATIONS
8
Negrón-Mendoza, 2011
CLASSIFICATIONS - TO
• 1:1 in which one tetrahedral sheet is bonded to one octahedral sheet
• KAOLINITE
9
Murray, 2007
CLASSIFICATIONS - TOT
• 2:1 in which one octahedral sheet is
sandwiched and covalently coordinated
between two tetrahedral sheets
• SMECTITE
• Water molecules and cations occupy the
space between the 2:1 layers
• Spices
– Sodium montmorillonite
– Calcium montmorillonite
– Saponite (magnesium montmorillonite)
– Nontronite (iron montmorillonite)
– Hectorite (lithium montmorillonite)
– Beidellite (aluminum montmorillonite)
10Murray, 2007
CLASSIFICATIONS - TOT
• ILLITE
• structure is a 2:1 layer in which
the interlayer cation is potassium
11Murray, 2007
CLASSIFICATIONS - TOT
• CHLORITE
• 2:1 layer mineral with an
interlayer octahedral sheet.
12Murray, 2007
CLASSIFICATIONS
• Pure clay minerals
• Mixed-layer clay minerals
13Brigatti et al., 2006
IDENTIFICATIONS
14
Bergaya and Lagaly, 2013
IDENTIFICATIONS
15Callister, W.D., 2012
IDENTIFICATIONS
• 4 STEPS:
– XRD for regular random oriented powder sample
– XRD for oriented clay size fraction
– XRD after glycolation
– XRD after heating
16
Clay Mineral group Air-Dried Heated Glycolated
Kaolinite 7.16 7.16 7.16
Smectite 15 10 16.9
Illite 10.1 10.1 10.1
Vermiculite 14.4 10 14.4
Chlorite 14.2 14.2 14.2
IDENTIFICATIONS - Ex
• CHLORITE:
17Poppe et al., 2001
IDENTIFICATIONS – Ex
• SMECTITE
18
Poppe et al., 2001
APPLICATIONS
Zhu and Njuguna, 2014
1 Earth and planetary sciences
2 Materials science
3 Engineering
4 Chemistry
5 Environmental science
6 Agricultural and biological science
7 Chemical engineering
8 Physics and astronomy
9 Energy
10 Biochemistry
19
APPLICATIONS
Adams and Hooper, 2001
20
CONCLUDING REMARKS
• Based on their layered structure, clay minerals can be
categorized as types 1:1 or 2:1
• X-ray diffraction is the basic tool for clay mineral identification
• Clays alone form an entire world in which geologists,
mineralogists, agriculturist, petroleum engineers, chemists
find extraordinary subjects for research.
21
22
REFERENCES
• Adams, J.M., Hooper, J.J., 2001. Clays, in: Veyssière, K.H.J.B.W.C.C.F.I.J.K.M.
(Ed.), Encyclopedia of Materials: Science and Technology (Second Edition).
Elsevier, Oxford, pp. 1236–1242.
• Bergaya, F., Lagaly, G., 2013. Chapter 1 - General Introduction: Clays, Clay
Minerals, and Clay Science, in: Faïza Bergaya and Gerhard Lagaly (Ed.),
Developments in Clay Science, Handbook of Clay Science. Elsevier, pp. 1–19.
• Brigatti, M.F., Galán, E., Theng, B.K.G., 2013. Chapter 2 - Structure and
Mineralogy of Clay Minerals, in: Faïza Bergaya and Gerhard Lagaly (Ed.),
Developments in Clay Science, Handbook of Clay Science. Elsevier, pp. 21–81.
• Callister, W.D., 2012. Fundamentals of Materials Science and Engineering: An
Integrated Approach, 4 edition. ed. Wiley, Hoboken, N.J.
• Meunier, A., 2010. Clays, Softcover reprint of hardcover 1st ed. 2005 edition.
ed. Springer
• Moore, D.M., Reynolds, R.C., 1997. X-Ray Diffraction and the Identification and
Analysis of Clay Minerals, 2 edition. ed. Oxford University Press, Oxford; New
York.
23
REFERENCES
• Murray, H.H., 2007. Applied Clay Mineralogy, Volume 2: Occurrences, Processing
and Applications of Kaolins, Bentonites, Palygorskitesepiolite, and Common Clays,
1 edition. ed. Elsevier Science, Boston.
• Negrón-Mendoza, A., 2011. Clay, in: Gargaud, M., Amils, P.R., Quintanilla, J.C., II,
H.J. (Jim) C., Irvine, W.M., Pinti, P.D.L., Viso, M. (Eds.), Encyclopedia of
Astrobiology. Springer Berlin Heidelberg, pp. 316–319.
• Nesse, W.D., 2012. Introduction To Mineralogy. Oxford University Press, New York.
• Poppe, L. J., Paskevich, V. F., Hathaway, J. C., Blackwood, D. S., 2001. A laboratory
manual for X-ray powder diffraction. US Geological Survey Open-File Report,
1(041), 1-88.
• Velde, B.B., Meunier, A., 2008. The Origin of Clay Minerals in Soils and Weathered
Rocks, 2008 edition. ed. Springer, Berlin.
• Zhu, H., Njuguna, J., 2014. 7 - Nanolayered silicates/clay minerals: uses and
effects on health, in: Njuguna, J., Pielichowski, K., Zhu, H. (Eds.), Health and
Environmental Safety of Nanomaterials. Woodhead Publishing, pp. 133–146.
24
25
Meunier, 2010
Meunier, 2010 26
27
28
29
30
31
Brigatti et al., 2013
32
33
Guggenheim et al., 2006
34Meunier, 2010
M: montmorillonite
B: beidellite
S: saponite
V: vermiculite
Velde, 2013 35

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Clay Minerals: Classifications, Identifications, Structures, and Applications

  • 1. GEOL 650 – Clay Mineralogy Instructor: Prof. Ahmet Umran Dogan Clay Minerals: Classifications, Identifications, Structures, and Applications Omar A. Radwan g201306050 ESD 1
  • 2. OUTLINE • Introduction • Structures – T – O – I • Classifications – TO – TOT • Identifications – XRD • Applications • Concluding remarks 2
  • 3. INTRODUCTION • Group: Phyllosilicate • Composition: hydrous aluminosilicates • Formation occurs under: – surface (alterites, soils, sediments) conditions or – subsurface (diagenesis, hydrothermal alterations) conditions • Size: few micrometers maximum – Difficult to observe without using electron microscopy 3
  • 4. STRUCTURES - T • The Tetrahedral Sheet (T) • SiO4 −4 or AlO4 −5 Tetrahedra • linked together by sharing three of four vertices (three basal oxygens) • Only one O-2 anion (apical oxygen) bonds cation pair Murray, 2007 4
  • 5. STRUCTURES - O • The Octahedral Sheet (O) • linked together by sharing their six vertices • Each anion is bonded to three cations in the trioctahedral type • Each anion is bonded to two cations in the dioctahedral type Murray, 2007 5
  • 7. STRUCTURES - I • The Interlayer Sheet (I) • In 2:1 phyllosilicates • interlayer cations compensate the negative charges in excess and insure the electrical neutrality of the 2:1 layer – Cations not bonded to each other (X) – Cations forming an octahedral sheet without any shared vertex with tetrahedral sheets (O) Velde and Meunier, 2008 7
  • 9. CLASSIFICATIONS - TO • 1:1 in which one tetrahedral sheet is bonded to one octahedral sheet • KAOLINITE 9 Murray, 2007
  • 10. CLASSIFICATIONS - TOT • 2:1 in which one octahedral sheet is sandwiched and covalently coordinated between two tetrahedral sheets • SMECTITE • Water molecules and cations occupy the space between the 2:1 layers • Spices – Sodium montmorillonite – Calcium montmorillonite – Saponite (magnesium montmorillonite) – Nontronite (iron montmorillonite) – Hectorite (lithium montmorillonite) – Beidellite (aluminum montmorillonite) 10Murray, 2007
  • 11. CLASSIFICATIONS - TOT • ILLITE • structure is a 2:1 layer in which the interlayer cation is potassium 11Murray, 2007
  • 12. CLASSIFICATIONS - TOT • CHLORITE • 2:1 layer mineral with an interlayer octahedral sheet. 12Murray, 2007
  • 13. CLASSIFICATIONS • Pure clay minerals • Mixed-layer clay minerals 13Brigatti et al., 2006
  • 16. IDENTIFICATIONS • 4 STEPS: – XRD for regular random oriented powder sample – XRD for oriented clay size fraction – XRD after glycolation – XRD after heating 16 Clay Mineral group Air-Dried Heated Glycolated Kaolinite 7.16 7.16 7.16 Smectite 15 10 16.9 Illite 10.1 10.1 10.1 Vermiculite 14.4 10 14.4 Chlorite 14.2 14.2 14.2
  • 17. IDENTIFICATIONS - Ex • CHLORITE: 17Poppe et al., 2001
  • 18. IDENTIFICATIONS – Ex • SMECTITE 18 Poppe et al., 2001
  • 19. APPLICATIONS Zhu and Njuguna, 2014 1 Earth and planetary sciences 2 Materials science 3 Engineering 4 Chemistry 5 Environmental science 6 Agricultural and biological science 7 Chemical engineering 8 Physics and astronomy 9 Energy 10 Biochemistry 19
  • 21. CONCLUDING REMARKS • Based on their layered structure, clay minerals can be categorized as types 1:1 or 2:1 • X-ray diffraction is the basic tool for clay mineral identification • Clays alone form an entire world in which geologists, mineralogists, agriculturist, petroleum engineers, chemists find extraordinary subjects for research. 21
  • 22. 22
  • 23. REFERENCES • Adams, J.M., Hooper, J.J., 2001. Clays, in: Veyssière, K.H.J.B.W.C.C.F.I.J.K.M. (Ed.), Encyclopedia of Materials: Science and Technology (Second Edition). Elsevier, Oxford, pp. 1236–1242. • Bergaya, F., Lagaly, G., 2013. Chapter 1 - General Introduction: Clays, Clay Minerals, and Clay Science, in: Faïza Bergaya and Gerhard Lagaly (Ed.), Developments in Clay Science, Handbook of Clay Science. Elsevier, pp. 1–19. • Brigatti, M.F., Galán, E., Theng, B.K.G., 2013. Chapter 2 - Structure and Mineralogy of Clay Minerals, in: Faïza Bergaya and Gerhard Lagaly (Ed.), Developments in Clay Science, Handbook of Clay Science. Elsevier, pp. 21–81. • Callister, W.D., 2012. Fundamentals of Materials Science and Engineering: An Integrated Approach, 4 edition. ed. Wiley, Hoboken, N.J. • Meunier, A., 2010. Clays, Softcover reprint of hardcover 1st ed. 2005 edition. ed. Springer • Moore, D.M., Reynolds, R.C., 1997. X-Ray Diffraction and the Identification and Analysis of Clay Minerals, 2 edition. ed. Oxford University Press, Oxford; New York. 23
  • 24. REFERENCES • Murray, H.H., 2007. Applied Clay Mineralogy, Volume 2: Occurrences, Processing and Applications of Kaolins, Bentonites, Palygorskitesepiolite, and Common Clays, 1 edition. ed. Elsevier Science, Boston. • Negrón-Mendoza, A., 2011. Clay, in: Gargaud, M., Amils, P.R., Quintanilla, J.C., II, H.J. (Jim) C., Irvine, W.M., Pinti, P.D.L., Viso, M. (Eds.), Encyclopedia of Astrobiology. Springer Berlin Heidelberg, pp. 316–319. • Nesse, W.D., 2012. Introduction To Mineralogy. Oxford University Press, New York. • Poppe, L. J., Paskevich, V. F., Hathaway, J. C., Blackwood, D. S., 2001. A laboratory manual for X-ray powder diffraction. US Geological Survey Open-File Report, 1(041), 1-88. • Velde, B.B., Meunier, A., 2008. The Origin of Clay Minerals in Soils and Weathered Rocks, 2008 edition. ed. Springer, Berlin. • Zhu, H., Njuguna, J., 2014. 7 - Nanolayered silicates/clay minerals: uses and effects on health, in: Njuguna, J., Pielichowski, K., Zhu, H. (Eds.), Health and Environmental Safety of Nanomaterials. Woodhead Publishing, pp. 133–146. 24
  • 27. 27
  • 28. 28
  • 29. 29
  • 30. 30
  • 31. 31
  • 32. Brigatti et al., 2013 32
  • 34. 34Meunier, 2010 M: montmorillonite B: beidellite S: saponite V: vermiculite
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