gibbsite वाक्य
उदाहरण वाक्य
मोबाइल
- The aluminium hydroxide in the lateritic bauxite deposits is almost exclusively gibbsite.
- Gibbsite and bayerite are monoclinic, whereas doyleite and nordstrandite are triclinic forms.
- As well as the process of catalyst substrates from gibbsite were also investigated.
- Minerals formed in laterite nickel deposits include gibbsite.
- Now, the main question is about gibbsite formation in the middle of kaolin series.
- The basic structure of corundum is identical to gibbsite except the hydroxides are replaced by oxygen.
- Gibbsite's structure is closely related to the structure of brucite, Mg ( OH ) 2.
- The different symmetry of gibbsite and brucite is due to the different way that the layers are stacked.
- It occurs in association with basaluminite, gibbsite, epsomite, gypsum, celestine, dolomite and goethite.
- We thus should find the hyper-aluminous materials, containing gibbsite in the lower series of kaolin.
- Associated minerals include hydrobasaluminite, hydroargillite, meta-aluminite, allophane, gibbsite, gypsum and aragonite.
- Allophane can alter to form halloysite under resilicating aqueous conditions and can alter to form gibbsite under desilicating conditions.
- Gibbsite is interesting for another reason because it is often found as a part of the structure of other minerals.
- Gibbsite is also known as hydrargillite, named after the dehydrated polymorphisms respectively, with no differentiation between nordstrandite and doyleite.
- Gibbsite is an important ore of aluminium in that it is one of three main phases that make up the rock bauxite.
- If this would be the only requirement, large amounts of kaolinite could be harvested simply by adding gibbsite powder to a silica solution.
- It is the gibbsite layer that in a way forms the " floor plan " for the mineral corundum, Al 2 O 3.
- These chemical and mineralogical evolutions ( dissolution crystallization ) allow the neo-formation of kaolin and gibbsite, as well as iron sulfide.
- The individual aluminium hydroxide layers are identical to the individual layers of gibbsite and are referred to as the " gibbsite layers ".
- The individual aluminium hydroxide layers are identical to the individual layers of gibbsite and are referred to as the " gibbsite layers ".
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