Pengaruh Variasi H2SO4 Pada Pembentukan Nanosilika Berbasis Batu Apung | Zendy

Riska Trisuraini | Zendy; Posman Manurung | Zendy; Suprihatin Suprihatin | Zendy

AI Assistant Blog Pricing

Home ZAIA Blog

Open Access

Pengaruh Variasi H2SO4 Pada Pembentukan Nanosilika Berbasis Batu Apung

Author(s) -

Riska Trisuraini,

Posman Manurung,

Suprihatin Suprihatin

Publication year - 2019

Publication title -

jurnal teori dan aplikasi fisika

Language(s) - English

Resource type - Journals

eISSN - 2549-1156

pISSN - 2303-016X

DOI - 10.23960/jtaf.v7i2.1954

Subject(s) - pumice , diffractometer , calcination , materials science , nuclear chemistry , anorthite , mineralogy , analytical chemistry (journal) , amorphous solid , albite , particle size , scanning electron microscope , chemistry , metallurgy , crystallography , chromatography , composite material , geology , biochemistry , quartz , volcano , seismology , catalysis

Nanosilica was extracted by using NaOH, H2SO4 and HCl. The amounth of NaOH and HCl are 3,0 M and 1,0 M respectively. The titration using H2SO4 was varied of 4,0 M; 4,5 M; 5,0 M; 5,5 M; 6,0 M. The pumice powder was calcined for 4 hours at 500 ºC and the nanosilica powder was calcined for 5,5 hours at 800 ºC. The results of X-Ray Flouresence (XRF) showed nanosilica with the highest purity in variation of H2SO4 5,0 M at 95,32%. The results of the X-Ray Diffractometer (XRD) showed that pumice consistent the anorthite and albite phase. The variation of H2SO4 5,0 M produced an amorphous phase. The results of Transmission Electron Microscopy (TEM) show nanosilica particle size with variations of H2SO4 5,0 M in the range 4,8-11,3 nm with an average (7,62 ± 2,15) nm.

The content you want is available to Zendy users.

Already have an account? Click here to sign in.

Having issues? You can contact us here

Accelerating Research