Zeolite nature was the compound alumino-silicate terhidrasi with the main element that consist of kation the alkali and the land alkali. This compound berstruktur three dimensions and had pores that could be filled by the water molecule.
The geology of sediment zeolite was formed because of the process of the volcanic dust sedimentation in the lake environment that was shaped like an alkali, the process diagenetik (metamorphism low-level) and the hydrothermal process.
The mineral zeolite that was most general was encountered was (Na,K)2O, Al2O3. 10 SiO2. 8H2O. Perbandingan between the atom The and Al that varied will produce many kinds or the species zeolite that was met in the wild. There were more than 50 kinds zeolite, but the framer's mineral zeolite biggest had 9 kinds, that is analsim, khabazit, klinoptilolit, erionit, mordenit, ferrierit, heulandit, laumontit and fillipsit. In Indonesia the kind zeolit the most was klinoptilolit and mordenit.
The use zeolit generally was based on the characteristics of chemistry and physics zeolit, like the absorber, change kation and the catalyst, that is used in the agricultural field, the plantation, livestock breeding, fisheries, the industry, energy
Zeolite nature was the compound alumino-silicate terhidrasi with the main element that consist of kation the alkali and the land alkali. This compound berstruktur three dimensions and had pores that could be filled by the water molecule.
The geology of sediment zeolite was formed because of the process of the volcanic dust sedimentation in the lake environment that was shaped like an alkali, the process diagenetik (metamorphism low-level) and the hydrothermal process.
The mineral zeolite that was most general was encountered was (Na,K)2O, Al2O3. 10 SiO2. 8H2O. Perbandingan between the atom The and Al that varied will produce many kinds or the species zeolite that was met in the wild. There were more than 50 kinds zeolite, but the framer's mineral zeolite biggest had 9 kinds, that is analsim, khabazit, klinoptilolit, erionit, mordenit, ferrierit, heulandit, laumontit and fillipsit. In Indonesia the kind zeolit the most was klinoptilolit and mordenit.
The use zeolit generally was based on the characteristics of chemistry and physics zeolit, like the absorber, change kation and the catalyst, that is used in the agricultural field, the plantation, livestock breeding, fisheries, the industry, energy
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