Published April 6, 2025
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SILVINITNING TAVSIFI
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- 1. Termiz davlat muhandislik va agrotexnologiyalar universiteti Termiz, O'zbekiston
Description
Tyubegatan galogen qatlamining tuzilishi, konning markaziy qismida joylashgan tayanch qudug‘i misolida ko‘rib chiqiladi. Galogen qatlam 452,55m, ularning 4,55% (20,6m) kaliy gorizontini tashkil qiladi. Namunalarni kimyoviy tahlili shuni ko‘rsatdiki – asosiy tuz hosil qiluvchi minerallar – galit (NaCl) va silvin (KCl) lardir; karnallit juda oz uchraydi. Hamma joyda turli miqdorlarda angidrit va loy kuzatiladi. Loy miqdori keng me’yorlarda – yuzli ulushlardan 20%gacha va undan ortiq holda almashadi. MgCl2 va CaCl2 umuman hamma yerda uncha ko‘p bo‘lmagan miqdorlarda ishtirok etadi.
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References
- 3. Davronovna, X. M., Sadriddinovich, E. S., &YigitaliJo'rao'g, J. (2022). Dependence of Karst Processes on Physico-Chemical Properties of Salts. American Journal of Social and Humanitarian Research, 3(9), 25-28
- 4. Davronovna, X. M., Soatmurodovna, S. R., &Alizoda, M. H. (2022). Gallurgical Enrichment of Silvinite Mines and Technology of Potassium Ore Processing. CrossRefView Record in ScopusGoogle Scholar.
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