45. 41. Among the ions with different bydrated radias below, which one is most favored during the cation exchange reaction, ie, alworths to clay mineral more strongly? K Na 0.54 0.79 D) OO Hydrated radius (mm) E) TT A) C A) TO B) TOT C) OTO NH₂ OK D) Na 42. In clay mineral, A) T: T E) Li B) T; O C) 0:0 D) Si; O E) T: Si 43. The picture below is an example of 0.53 layer and ● oxygen silicon ● aluminum hydrogen Li 1.03 layer can join to form sheets. layer. 44. Which statement is NOT true about kaolinite and kaolinitic soils? A) Bonding between sheets in kaolinite is very weak, thus kaolinitic soils are easy to plow. B) Kaolinitic soils do not shrink and well as there is no interlayer swelling. C) There is no interlayer welling in kaolinite, so kaolinitic soils hold less water than other clay-rich soils. D) Kaolinitic soil is useful for agriculture if nutrients are managed properly. E) There are cations in between the layers of kaolinite. is the amount of exchangeable cations per mass of soil and its unit is in milliequivelents (meq) per 100 g of oven dry soil. A) Cation Exchange Capacity (CEC) B) Total alkalinity

Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
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Related questions
Question
d
45.
42. In clay mineral,
A) T; T
D) 00
41. Among the ions with different bydrated radies below, which one is most favored during
the cation exchange reaction, i.e. aftworths to clay mineral more strongly?
Jon
Na
0.79
Hydrated
radior (mm)
B) NH
D) Na*
A) TO
B) TOT
C) OTO
E) TT
B) T; O
C) 0:0
D) Si; O
E) T; Si
43. The picture below is an example of
0.53
layer and
• oxygen
silicon
● aluminum
。 hydrogen
0.54
Lit
1.03
A) Cation Exchange Capacity (CEC)
B) Total alkalinity
C) pH
layer can join to form sheets.
layer.
44. Which statement is NOT true about kaolinite and kaolinitic soils?
A) Bonding between sheets in kaolinite is very weak, thus kaolinitic soils are easy to
plow.
B) Kaolinitic soils do not shrink and well as there is no interlayer swelling.
C) There is no interlayer welling in kaolinite, so kaolinitic soils hold less water than
other clay-rich soils.
D) Kaolinitic soil is useful for agriculture if nutrients are managed properly.
E) There are cations in between the layers of kaolinite.
is the amount of exchangeable cations per mass of soil and its unit is in
milliequivelents (meq) per 100 g of oven dry soil.
Transcribed Image Text:d 45. 42. In clay mineral, A) T; T D) 00 41. Among the ions with different bydrated radies below, which one is most favored during the cation exchange reaction, i.e. aftworths to clay mineral more strongly? Jon Na 0.79 Hydrated radior (mm) B) NH D) Na* A) TO B) TOT C) OTO E) TT B) T; O C) 0:0 D) Si; O E) T; Si 43. The picture below is an example of 0.53 layer and • oxygen silicon ● aluminum 。 hydrogen 0.54 Lit 1.03 A) Cation Exchange Capacity (CEC) B) Total alkalinity C) pH layer can join to form sheets. layer. 44. Which statement is NOT true about kaolinite and kaolinitic soils? A) Bonding between sheets in kaolinite is very weak, thus kaolinitic soils are easy to plow. B) Kaolinitic soils do not shrink and well as there is no interlayer swelling. C) There is no interlayer welling in kaolinite, so kaolinitic soils hold less water than other clay-rich soils. D) Kaolinitic soil is useful for agriculture if nutrients are managed properly. E) There are cations in between the layers of kaolinite. is the amount of exchangeable cations per mass of soil and its unit is in milliequivelents (meq) per 100 g of oven dry soil.
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