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E) Li 42. In clay mineral, A) T; T B) T; O C) 0; 0 D) Si; O E) T; Si layer and layer can join to form sheets.

E) Li 42. In clay mineral, A) T; T B) T; O C) 0; 0 D) Si; O E) T; Si layer and layer can join to form sheets.

Applications and Investigations in Earth Science (9th Edition)
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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45. mead 41. Among the ions with different hydrated radius below, which one is most favored during the cation exchange reaction, i.e. absorbs to clay mineral more strongly? Jon Hydrated radius (nm) A) C B) NH. C) K* D) Na* E) Li D) 00 E) TT A) TO B) TOT C) OTO 0.5 XXXVXDXXV-XI 42. In clay mineral, A) T; T B) T; O C) 0; 0 D) Si: O E) T: Si 43. The picture below is an example of 0.53 layer and AT TXIXXI • oxygen • silicon ● aluminum o hydrogen 0.54 Na 0.79 layer. A) Cation Exchange Capacity (CEC) B) Total alkalinity C) pH Lit 1.03 layer can join to form sheets. 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. D) Anion Excha E) lonic stren
Transcribed Image Text:45. mead 41. Among the ions with different hydrated radius below, which one is most favored during the cation exchange reaction, i.e. absorbs to clay mineral more strongly? Jon Hydrated radius (nm) A) C B) NH. C) K* D) Na* E) Li D) 00 E) TT A) TO B) TOT C) OTO 0.5 XXXVXDXXV-XI 42. In clay mineral, A) T; T B) T; O C) 0; 0 D) Si: O E) T: Si 43. The picture below is an example of 0.53 layer and AT TXIXXI • oxygen • silicon ● aluminum o hydrogen 0.54 Na 0.79 layer. A) Cation Exchange Capacity (CEC) B) Total alkalinity C) pH Lit 1.03 layer can join to form sheets. 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. D) Anion Excha E) lonic stren
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