Perlit

Perlit yang membesar

Perlit adalah kaca vulkanis nirbentuk yang relatif banyak mengandung air. Perlit umumnya terbentuk dari hidrasi batuan obsidian. Perlit tercipta secara alamiah dan memiliki sifat dapat membesar ketika dipanaskan secukupnya. Bahan ini merupakan mineral industri dan produk yang diperjualbelikan dengan keutamaan kepadatannya yang rendah setelah diolah.[1]

Telaah kandungan

Catatan kaki

  1. ^ Reka, Arianit A.; Pavlovski, Blagoj; Lisichkov, Kiril; Jashari, Ahmed; Boev, Blažo; Boev, Ivan; Lazarova, Maja; Eskizeybek, Volkan; Oral, Ayhan; Makreski, Petre (24 October 2019). "Chemical, mineralogical and structural features of native and expanded perlite from Macedonia". Geologia Croatica (dalam bahasa Inggris). 72 (3): 215–221–215–221. doi:10.4154/gc.2019.18. ISSN 1333-4875. Diakses tanggal 4 January 2020.
  2. ^ Md Arifuzzaman and H. S. Kim, "Prediction and evaluation of density and volume fractions for the novel perlite composite affected by internal structure formation", Construction and Building Materials, Vol 141, 2017, 201–215.

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