Translation of illite
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IPA (International Phonetic Alphabet) of illite
The International Phonetic Alphabet (IPA) is an alphabetic system of phonetic notation based primarily on the Latin alphabet. With phonetic transcriptions, dictionarie tell you about the pronunciation of words, because the spelling of an English word does not tell you how you should pronounce it. Below is the phonetic transcription of illite:
/ɪlajt/
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illite on Youtube
- and Illite. So these Kaolinite, Montmorillonite and Illite dominate in soils.
- or Montmorillonite or Illite or the amount of clay mineral present.
- very low activity value and Sodium Montmorillonite exhibits a value in between 4 to 7. Illite
- In this slide, particle size distribution of the bentonite, illite and kaolinite are
- sizes compared to illite and bentonite. The similar thing can be seen here which is represented
- illite clay and this is the sodium bentonite. Sodium bentonite is observed to be the finest
- among bentonite, illite and kaolinite family.
- different type of clay minerals, for example Kaolinite, Illite and Montmorillonite.
- in the previous lesson namely kaolinite, illite
- and what we found is that under certain conditions, smectite mineral actually convert into illite
- higher in comparison with kaolinite and illite. In
- ambient condition and that is followed by illite and smectite is the least stable of
- the range of 34 to 39 percent. Illite is falling in between kaolinite and Montmorillonite.
- than 0.38 for kaolinite and in between greater than 0.38 and 0.9 for illite and greater than
- So here, if you see the kaolinite is exhibiting the value of 0.38 and illite has the value
- in between 0.38 and 0.9. So this is actually the illite line. Somewhere here the montmorillonite
- I also used orange illite clay, mixing about 1 teaspoon with distilled water.
- Finally for the last shade of red, I added a few drops of orange illite clay plus some pink kaolin clay to get a reddish orange color
- The three basic clay minerals are Kaolinite, Illite and Montmorillonite. Kaolinite is generally
- prevalent in sedimentary and residual soils. Illite is common in stiff clays and shales
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