Two types of commercial clay minerals from the Bidor region of Perak were studied. From the X-ray diffraction study, these clays were identified as disordered kaolinite and 2 M polymorph of illite. The morphologies, the surface properties, the pore structures and the infrared absorption properties were examined. The basis for the identification of these clays is discussed
Kaolin mineral is a commercially solid powder with a comparatively low level of purity and is regula...
The Karak mudstone, cropping out in the vicinity of Karak town, NW Pakistan, is contained within an ...
The Karak mudstone, cropping out in the vicinity of Karak town, NW Pakistan, is contained within an ...
Two types of commercial clay minerals from the Bidor region of Perak were studied. From the X-ray di...
Quaternary (Q-clay) clayey deposits are one of the dominating parts of mineral raw materials of the ...
The Bandung bentonite deposit is located in Wonosegoro District, Boyolali Regence, Central Java. Cha...
The Bandung bentonite deposit is located in Wonosegoro District, Boyolali Regence, Central Java. Cha...
This study investigates the relationship between clay minerals (kaolinite and illite) and rock prope...
X-ray diffractograms show that randomly interstratified illite-montmorillonite and kaolinite are the...
Clay minerals are common constituents of the subsurface sandstones in Malaysia sedimentary basins. K...
Abst ract--A reservoir ock is a porous geological formation in contact with 2 liquids, brine and oil...
Clay mineral is widely used in ceramic materials, building materials, paper coating materials, catal...
This study aimed at demonstrating complementary roles offered by Fourier transform infrared spectrop...
The Karak mudstone, cropping out in the vicinity of Karak town, NW Pakistan, is contained within an ...
The Karak mudstone, cropping out in the vicinity of Karak town, NW Pakistan, is contained within an ...
Kaolin mineral is a commercially solid powder with a comparatively low level of purity and is regula...
The Karak mudstone, cropping out in the vicinity of Karak town, NW Pakistan, is contained within an ...
The Karak mudstone, cropping out in the vicinity of Karak town, NW Pakistan, is contained within an ...
Two types of commercial clay minerals from the Bidor region of Perak were studied. From the X-ray di...
Quaternary (Q-clay) clayey deposits are one of the dominating parts of mineral raw materials of the ...
The Bandung bentonite deposit is located in Wonosegoro District, Boyolali Regence, Central Java. Cha...
The Bandung bentonite deposit is located in Wonosegoro District, Boyolali Regence, Central Java. Cha...
This study investigates the relationship between clay minerals (kaolinite and illite) and rock prope...
X-ray diffractograms show that randomly interstratified illite-montmorillonite and kaolinite are the...
Clay minerals are common constituents of the subsurface sandstones in Malaysia sedimentary basins. K...
Abst ract--A reservoir ock is a porous geological formation in contact with 2 liquids, brine and oil...
Clay mineral is widely used in ceramic materials, building materials, paper coating materials, catal...
This study aimed at demonstrating complementary roles offered by Fourier transform infrared spectrop...
The Karak mudstone, cropping out in the vicinity of Karak town, NW Pakistan, is contained within an ...
The Karak mudstone, cropping out in the vicinity of Karak town, NW Pakistan, is contained within an ...
Kaolin mineral is a commercially solid powder with a comparatively low level of purity and is regula...
The Karak mudstone, cropping out in the vicinity of Karak town, NW Pakistan, is contained within an ...
The Karak mudstone, cropping out in the vicinity of Karak town, NW Pakistan, is contained within an ...