clay - a natural mother, the main warehouse of the Yaki MITHDOVOVAI oxidi aluminia that flint. Until the warehouse, such a molecules are the same, and from SPIVVIVISHYA the Tsich component is to be in the deposit of the VID of the Missa Vidobutka. Call, vm and fluster oxide (silica) to become near 45-50%, oxide aluminia (clay)-40-45%, and the drive-up to 15%.
Character of the Glini Klini, natural Barvniki: Oxidi Zaliza, Titan, Magniy, Midі, Nikel that chrome. Vidtyinki clay grunted by nyd Zhovnoy that brown to the blue, cherry il
Troximum of 50% clay part -on, May, the rosemer than 0.01 mm, and the pond is 25% - more than 0.001 mm. The shape of the cycle is a plane of a plane, luxurious. The charge of the superficial superficial negative, the zumyaguvnna is positively charged molecules of the drive, explanatory gigroscope of clay - the building of the plug -in the utrymuvati Vologa.
The basis of the clay warehouse is Gidrosludi, Kaolin, Chlorite I Montmolilonite.
Mineral warehouse of clay є is the key to the factor, the vicious riznitsu mіzh ї species of the same spheres of the gap. Counting, gydrosrodisti clay Mayut Nizka Plasticity, Ale Zdatni simply zbilshuvat in the circuit when contacted (up to 9 times), I am the meaning of the doskoshkh ulamkovih pork. Kaolinovi clay is characterized by a plastic part of the plastic, and widely vicoristovo at the Vobronitvi Kerami. Montmorollenitovi clay Mayut Viralzhenі Sorbtsiyni Power.
YakIsni characteristics of clay:
dispersion (strap of subporal):
- Vosokodispersni (PAHA 85% Partnok