SINTESIS DAN KARAKTERISASI NANOPARTIKEL Fe2O3 DARI PASIR ALAM DESA LOGAS KABUPATEN KUANTAN SINGINGI

M. Sihombing, Erwin Amiruddin
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引用次数: 2

Abstract

Determination of magnetic and structural properties of natural sand from Logas Village, Kuantan Singingi have been carried out using a magnetic Probe Pasco PS-2162 and X-Ray Diffraction methode. Samples were synthesized using multi step ball milling methode for 90 and 90+30 hours. Results show that the magneticsuceptibility increased with increasing of ball milling time, from 90 hours to 90+30 hours. This magnetic suceptibility within the interval (46-80000) x 10-8 m3/kg which is the interval of Ilminite mineral (FeTiO3; Antiferromagnetic). X-Ray Fluorescence result showed that the composition of Fe and Ti increased after milled for 90+30 hours, while other element like Si decreased. The XRD result confirmed that the phase of the sample structure is Hematite (α-Fe2O3). However, some other phases including SiO2 and FeTiO3 are observed in diffraction pattern. This indicates that the sample is not purely hematite.
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采用Pasco PS-2162磁性探针和x射线衍射法对广西关丹省Logas村天然砂的磁性和结构性质进行了测定。样品采用多级球磨法合成90和90+30小时。结果表明:随着球磨时间的增加,磁化率从90 h增加到90+30 h;磁化率在(46-80000)× 10-8 m3/kg区间内,这是钛矿矿物(FeTiO3;反铁磁性的)。x射线荧光结果显示,经过90+30小时的碾磨后,Fe和Ti的成分增加,而Si等其他元素的成分减少。XRD结果证实样品结构物相为赤铁矿(α-Fe2O3)。然而,在衍射图中观察到一些其他相,包括SiO2和FeTiO3。这表明样品不是纯赤铁矿。
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