scholarly journals KETERDAPATAN HALOYSIT DAN IKUTANNYA DI PERAIRAN UTARA JAWA TIMUR

2016 ◽  
Vol 5 (1) ◽  
Author(s):  
Udaya Kamiludin ◽  
Noor C.D. Aryanto
Keyword(s):  
Aluminum Content ◽  
Major Element ◽  
Sediment Accumulation ◽  
X Ray Diffraction ◽  
The West ◽  
X Ray ◽  
North East ◽  
Investigation Area ◽  
Fine Grain ◽  
West Part

Perairan Utara Jawa Timur adalah perairan berenergi rendah yang berkaitan erat dengan akumulasi sedimen berbutir halus. Berdasarkan hasil pengolahan data granulometri menunjukkan sebagian besar percontohan sedimen diklasifikasikan kedalam lanau. Hasil Analisis “X-ray diffraction”, lanau yang secara megaskopis sebagai lempung mengandung mineral lempung jenis Haloysit; ikutannya yaitu kuarsa alfa, kalsit, feldspar, halit dan hematit. Hasil analisis mineral menunjukan haloysit ini mempunyai persentase antara 38,57-55,79 % dengan penyusunnya terlihat dari hasil analisis kimia unsur utama berupa aluminium dalam Al2O3 dan silikon dalam SiO2. Keterdapatan haloysit terbentuk secara mekanik dari pelapukan mineral aluminosilikat, seperti feldspar yang bersumber dari batuan volkanik di bagian barat dan bahan gunungapi di sebelah selatan daerah penelitian. Kata kunci : Lanau, haloysit, feldspar, perairan Utara Jawa Timur North East Java waters is a low energy waters in relation to fine grain sediment accumulation. Based on the processing results of granulometry data show the majority sample of sediment classified into silt. Results of X-ray diffraction analysis, silt megascopically described as clay which is consisted of clay mineral of halloysite type; its associations are quartz alpha, calcite, feldspar, halite and hematite. Mineral analyses results show the halloysite has percentage between 38,57 - 55,79 % with composition confirmed from major element chemical analysis which show aluminum content in Al2O3 and silicon in SiO2. The occurrence of halloysite formed through mechanical processes from surface weathering of aluminosilicate minerals, as feldspars which source from volcanic rock in the west part and from volcanic materials in the south side of the investigation area. Keywords : silt, halloysite, feldspar, Northeast Java waters.

Room Temperature Screw Form Rolling of AZ91D Magnesium Alloy through Processing by Extrusion-Torsion Simultaneous Working

2014 ◽  
Vol 783-786 ◽  
pp. 375-379
Author(s):  
Mitsuaki Furui ◽  
Shouyou Sakashita ◽  
Kazuya Shimojima ◽  
Tetsuo Aida ◽  
Kiyoshi Terayama ◽  
...  
Keyword(s):  
Magnesium Alloy ◽  
Room Temperature ◽  
Hardness Measurement ◽  
Rolling Process ◽  
X Ray Diffraction ◽  
X Ray ◽  
Az91d Magnesium Alloy ◽  
Microstructure Observation ◽  
Fine Grain ◽  
Simultaneous Processing

Extrusion-torsion simultaneous processing is a very attractive technique for fabricating a rod-shape material with fine grain and random texture. We have proposed a new screw form rolling process combined with preliminary extrusion-torsion simultaneous working. Microstructure evolution and mechanical property change of AZ91D magnesium alloy during extrusion-torsion simultaneous processing was examined through microstructure observation, X-ray diffraction analysis and micro-Vickers hardness measurement. By the addition of torsion, the crystal orientation of AZ91D magnesium alloy workpiece was drastically changed from basal crystalline orientation to the random orientation. Crystal grain occurred through the dynamic recrystallization and tended to coarsen with an increase of extrusion-torsion temperature. Grain refinement under 2 um was achieved at the lowest extrusion-torsion temperature of 523 K. M8 gauge AZ91D magnesium alloy screw was successfully formed at room temperature using the extrusion-twisted workpiece preliminary solution treating at 678 K for 345.6 ks. It was found that the extrusion-torsion temperature of 678 K must be selected to fabricate the good screw without any defects.

Microstructure Evolution of a Fine Grain Al-50wt%Si Alloy Fabricated by High Energy Milling

2011 ◽  
Vol 479 ◽  
pp. 54-61 ◽  
Author(s):  
Fei Wang ◽  
Ya Ping Wang
Keyword(s):  
Grain Growth ◽  
Microstructure Evolution ◽  
Room Temperature ◽  
Milling Time ◽  
High Energy ◽  
X Ray Diffraction ◽  
Scanning Calorimetry ◽  
Laser Method ◽  
X Ray ◽  
Fine Grain

Microstructure evolution of high energy milled Al-50wt%Si alloy during heat treatment at different temperature was studied. Scanning electron microscope (SEM) and X-ray diffraction (XRD) results show that the size of the alloy powders decreased with increasing milling time. The observable coarsening of Si particles was not seen below 730°C in the high energy milled alloy, whereas, for the alloy prepared by mixed Al and Si powders, the grain growth occurred at 660°C. The activation energy for the grain growth of Si particles in the high energy milled alloy was determined as about 244 kJ/mol by the differential scanning calorimetry (DSC) data analysis. The size of Si particles in the hot pressed Al-50wt%Si alloy prepared by high energy milled powders was 5-30 m at 700°C, which was significantly reduced compared to that of the original Si powders. Thermal diffusivity of the hot pressed Al-50wt%Si alloy was 55 mm2/s at room temperature which was obtained by laser method.

scholarly journals PHYSICOCHEMICAL STUDY AND QUANTITATIVE ANALYSIS SWARNA MAKSHIKA BHASMA.

2021 ◽  
Vol 9 (1) ◽  
Author(s):  
Rajni Bhardwaj ◽  
Smita Johar ◽  
Amit Kapila ◽  
Amandeep Sharma
Keyword(s):  
Particle Size ◽  
Quantitative Analysis ◽  
Iron Oxide ◽  
Major Element ◽  
X Ray Diffraction ◽  
X Ray ◽  
Minor Elements ◽  
Rhombohedral Crystal ◽  
Main Component ◽  
Reddish Brown Color

Swarnamakshika is grouped under Updhatu of Swarna and is composed of Copper, Iron and Sulphur. In this study Swarnamakshika was subjected to Shodhana by Bharjana with Nimbuka swarasa and Shudha Swarnamakshika was given Bhavana with Nimbuka swarasa and subjected to Varahaputa. With ten Varahaputa Bhasma Siddhi Lakshanas were attained swarnamakshika Marana was done by using Nimbuka swarasa until bhasma siddi lakshanas found and it took 10 puta till it attained reddish brown color. The X-ray diffraction analysis showed that d-identified peaks after 10th puta Swarnamakshika bhasma composition is of Iron oxide with rhombohedral crystal system as main component. EDX analysis of Swarna makshika bhasma shows that it contains Iron and Oxygen, as major element and Copper, Sulphur, Carbon, Aluminium, Calcium etc. as minor elements. FESEM study revealed that the particle size of Ashudha and Shudha Swarnamakshika was in the range of 500 nm-3nm. Keywords: Swarnamakshika Bhasma, Nimbuka swarasa, puta

Halloysite in some soils from north-east Scotland

Clay Minerals ◽  
1977 ◽  
Vol 12 (1) ◽  
pp. 59-66 ◽  
Author(s):  
M. J. Wilson ◽  
J. M. Tait
Keyword(s):  
Electron Microscopy ◽  
Electron Diffraction ◽  
Soil Samples ◽  
X Ray Diffraction ◽  
X Ray ◽  
Drainage Class ◽  
North East ◽  
Parent Rocks ◽  
Diffraction Patterns

AbstractX-ray diffraction and electron microscopy show that halloysite occurs widely in soils derived from a variety of parent rocks (granite, gabbro, schist and slate) in north-east Scotland. Both tubular and non-tubular forms are observed, the latter being characterized by electron diffraction patterns with 001 reflection either absent or very weak and diffuse. Clay fractions from a poorly drained profile separated without prior drying of the soil samples contain essentially dehydrated halloysite at the surface, this becoming progressively more hydrated with depth. Since halloysite occurs extensively in soils of widely varying drainage class the mineral is probably not the result of recent soilforming processes but may have originated during Tertiary or interglacial weathering.

High-pressure, high-temperature sintering of diamond–SiC composites by ball-milled diamond–Si mixtures

2002 ◽  
Vol 17 (8) ◽  
pp. 2153-2160 ◽  
Author(s):  
J. Qian ◽  
G. Voronin ◽  
T. W. Zerda ◽  
D. He ◽  
Y. Zhao
Keyword(s):  
Ball Milling ◽  
Amorphous State ◽  
Silicon Powder ◽  
X Ray Diffraction ◽  
X Ray ◽  
Fine Grain ◽  
High Pressure High Temperature ◽  
Micron Size ◽  
Infiltration Technique ◽  
Sic Composites

A new method of sintering diamond-silicon carbide composites is proposed. This method is an alternate to the liquid silicon infiltration technique and is based on simultaneous ball milling of diamond and silicon powder mixtures. Composites with fine-grain diamonds embedded in a diamond–SiC nanocrystalline matrix were sintered from these mixtures. Scanning electron microscopy, x-ray diffraction, and Raman scattering were used to characterize the ball-milled precursors and the sintered composites. It was found that the presence of diamond micron-size particles in the initial powder mixture promotes milling of silicone particles and their transformation into the amorphous state. Mechanical properties of the composites, sintered from mixtures of different ball-milling history at different pressure–temperature conditions, (6 GPa/1400 °C and 8 GPa/2000 °C) were studied.

scholarly journals Structural Characterization of Heteroepitaxial Growth of AlxGa1-xSb/GaSb by LPE

2014 ◽  
Vol 70 (a1) ◽  
pp. C1795-C1795
Author(s):  
Primavera Lopez ◽  
Javier Martinez ◽  
Gabriel Juarez ◽  
Joel Diaz
Keyword(s):  
Liquid Phase ◽  
Aluminum Content ◽  
Reciprocal Space ◽  
Diffraction Maximum ◽  
Heteroepitaxial Growth ◽  
X Ray Diffraction ◽  
Reciprocal Space Mapping ◽  
X Ray ◽  
Crystallographic Tilt

The heteroepitaxial AlxGa1-xSb/GaSb (001) growth with different x aluminum content, from 0.05 to 0.2 prepared by Liquid Phase Epitaxy (LPE) is presented. The interest in this study is due to the layers of AlxGa1-xSb systems should be well matched for fabrication of sources and detectors operating in the 1.3-1.6 micron range. The layered structure obtained was characterized mainly by high-resolution X-ray diffraction and reciprocal space mapping. In the case of x = 0.05 aluminum content, the relaxation is minimal, and almost without deviation respect to GaSb. As the aluminum content increases above 0.05, the relaxation is larger and deviation from GaSb substrate too. Crystallographic tilt is detected by a shift of layer diffraction maximum on reciprocal space maps. Deviation changes the intensity of layer respect to substrate peak in rocking curves and hence the estimation of thickness of layer obtained from them. A correction for estimated thickness of layers is obtained from mapping.

scholarly journals Characterisation of Natural and HDTMA-Br Modified Dijah-Monkin Bentonite Clay: FTIR, XRF, XRD and SEM

2021 ◽  
Vol 7 (5) ◽  
pp. 2010-2018
Author(s):  
Olukayode Gideon Oloyede ◽  
◽  
Umar Omeiza Aroke ◽  
Saidat Olanipekun Giwa ◽  
Alexander Asanja Jock ◽  
...  
Keyword(s):  
Cation Exchange Capacity ◽  
Bentonite Clay ◽  
Exchange Capacity ◽  
Basal Spacing ◽  
Hexadecyltrimethylammonium Bromide ◽  
Acid Activation ◽  
X Ray Diffraction ◽  
X Ray ◽  
North East ◽  
Scanning Electron

In this study, Dijah-Monkin bentonite clay was modified with a cationic surfactant hexadecyltrimethylammonium bromide (HDTMA-Br) at the level of twice the cation exchange capacity (CEC). This process results in the development of hydrophobic organoclay with an improved adsorption capacity. The clay obtained from Zing LGA Taraba State, North-East Nigeria, was beneficiated and pulverised to a particle size of 125 µm. The modification was performed without acid activation to prevent damages to the clay’s crystal structure. The organoclay was characterised for chemical composition, functional groups, mineralogical and surface morphology using X-ray fluorescence (XRF), Fourier Transform Infrared (FTIR) spectroscopy, X-ray diffraction (XRD) and scanning electron microscopy (SEM), respectively. The XRD showed an increase in the basal spacing from 15.681Å to 17.758 Å, while the XRF revealed a 5.35% concentration of Br on the modified clay, indicating successful intercalation. The FTIR spectra also revealed the appearance of symmetric and asymmetric stretching bands at 2847.7cm-1 and 2914.8cm-1, respectively, as a consequence of the modification, resulting in more sites for adsorption.

scholarly journals PHASE COMPOSITION OF OXIDE FILMS FORMED ON THE SURFACE OF THE FE-CR-AL SYSTEM COATINGS

2020 ◽  
pp. 14-18
Author(s):  
V. G. Shmorgun ◽  
A. I. Bogdanov ◽  
O. V. Slautin ◽  
V. P. Kulevich
Keyword(s):  
Phase Composition ◽  
Aluminum Content ◽  
Oxide Films ◽  
X Ray Diffraction ◽  
Surface Layers ◽  
X Ray ◽  
Glancing Angle ◽  
Stable Growth ◽  
Metastable Alumina

The phase composition of the oxide films on the surface of the Fe-Cr-Al system coatings is studied using glancing angle X-ray diffraction. It is shown that at 900 °С the formed oxide films consist of αAlO and (FeCr)O, to which FeAlO oxide is added during long-term exposure. An increase in temperature to 1100 °C intensifies the growth of oxide films, and an increase in the aluminum content ensures a stable growth of αAlO and FeAlO oxides. When the aluminum content in the coating is more than 10 at. % at large exposure times, metastable alumina δAlO is formed, the formation of which is associated with a decrease in the concentration of chromium in thin surface layers.

scholarly journals Occurrence of Sesquioxide in a Mid-Low Grade Collophane-Sedimentary Apatite Ore from Guizhou, China

Minerals ◽  
2020 ◽  
Vol 10 (11) ◽  
pp. 1038
Author(s):  
Jie Deng ◽  
Kecheng Zhang ◽  
Dongsheng He ◽  
Hengqin Zhao ◽  
Rachid Hakkou ◽  
...  
Keyword(s):  
Electron Microscope ◽  
Scanning Electron Microscope ◽  
Low Grade ◽  
Carbonate Apatite ◽  
X Ray Diffraction ◽  
X Ray ◽  
Fine Grained ◽  
Mineral Liberation ◽  
Fine Grain ◽  
Scanning Electron

Checking the presence of sesquioxide (Fe2O3, Al2O3) is helpful for its removal in advance. Therefore, the occurrence of sesquioxide in a mid-low grade calcareous-siliceous collophane ore (massive carbonate-apatite, also known as francolite) from Guizhou, China was determined by X-ray fluorescence spectroscopy (XRF), X-ray diffraction (XRD), field emission scanning electron microscope-energy dispersive X-ray spectrometry (FESEM-EDX) and Mineral Liberation Analyzer (MLA). The results show that iron mainly occurs as pyrite FeS2, goethite FeO(OH) and as substitution within dolomite Ca(Mg,Fe)(CO3)2, while aluminum is enriched in muscovite KAl2(AlSi3O10)(OH)2 and also found in apatite (F,CO3)CaPO4 and calcite CaCO3 due to isomorphism or adsorption. All these minerals are fine-grained, among which pyrite and goethite tend to be enriched in larger particles. Intergrowth is predominant in the six minerals’ locking. Pyrite is mainly intergrown with calcite, biotite and also included in apatite and muscovite, while the monomer pyrite appears as semi-automorphic fine grain with the liberation of 56.1%. Apatite particles are mainly intergrown with quartz and calcite. Most of goethite, dolomite, muscovite and calcite form intergrowth with apatite, with contents of 21.7%, 11.1%, 19.5% and 41%, respectively. The removal of pyrite, goethite, dolomite, muscovite and calcite in the ore is the key to reduce the contents of Fe2O3 and Al2O3. In the subsequent beneficiation, the ore must be fully ground. In addition to flotation, magnetic separation can also be considered to remove part of iron in ore. For the removal of aluminum from apatite, leaching method can be considered.

Clay mineral provinces in the tertiary sediments of the Hampshire Basin

Clay Minerals ◽  
1968 ◽  
Vol 7 (3) ◽  
pp. 351-361 ◽  
Author(s):  
R. J. Gilkes
Keyword(s):  
Diffraction Study ◽  
Clay Mineral ◽  
X Ray Diffraction ◽  
The West ◽  
Eastern Province ◽  
X Ray ◽  
Western Province ◽  
Tropical Weathering

AbstractAn X-ray diffraction study of over 600 specimens has shown that the Tertiary sediments of the Hampshire Basin are divided into two clay mineral provinces. The western province is characterized by kaolin from the West Country granites whilst the highly montmorillonitic sediments of the eastern province were partially derived from the dissolution of Chalk by tropical weathering.

Sign in / Sign up

Export Citation Format

Share Document