scholarly journals Petrochemical Features of Manganese Nodules in Madaka (Sheet 142) SE and Part of Kwana - Bala (Sheet 142) NE, Nigeria

Author(s):  
Akintola Ojo Adeoye ◽  
Najime Tavershima ◽  
Danladi Bello Abubakar ◽  
Ogunleye Paul Olusegun ◽  
Abubakar Ismail Yusuf

Manganese nodule occurs in Madaka (Sheet 142) SE and part of Kwana - Bala (Sheet 142) NE, Nigeria. Four (4) samples of manganese nodules were analyzed petrochemical using X-ray diffractometry (XRD), reflected light microscopy, Electron probe micro analysis (EPMA), Atomic absorption spectrophotometer (AAS). XRD reveals sphalerite, manganates and ilmenite as major minerals in the nodules. Accessory minerals are siderite and rutile. Chemical study of the manganese nodules from Madaka and Kwana - Bala reveals that Mn-, Fe-, Co-, Ni-, and Cu-, minerals (including native elements and sulfides) commonly occur in the samples. Also, the results indicate that increased in Mn relative to the manganite content (10AO- plus 7AO), led to increase in Ni and Cu recovery. However, slightly greater amounts by weight of Ni and Cu were dissolved from the manganites than from Mn. This followed from the much higher Ni and Cu contents of manganites relative to Mn. The exploration for Ni and Cu from nodules on assay criterion was inadequate; the sphalerite Mn02 phase structure would also be a necessary criterion. It was suggested that nodules could be processed upon beneficiation for Ni and Cu contents for a future time relative to the original processing. It was thus proposed that Ni and Cu could be produced from manganese nodules in the study area.

2008 ◽  
Vol 63 (6) ◽  
pp. 739-741 ◽  
Author(s):  
Alain Largeteau ◽  
Stéphane Darracq ◽  
Graziella Goglio

Experimental investigations concerning the synthesis of Si1−xGexO2 solid solutions with quartz structure have been carried out under solvothermal conditions from sol-gel preparations. The cell parameters of the powders have been determined by X-ray powder diffraction. The amount of germanium inside the SiO2 structure was measured also by electron probe micro-analysis (EPMA).


2018 ◽  
Vol 925 ◽  
pp. 520-523
Author(s):  
Gunilla Runnsjö ◽  
Kaj Grönlund

In material science, there is an increased demand for mapping of microstructural components and their composition. EPMA (Electron Probe Micro Analysis) with WDS (Wavelength Dispersive Spectrometry) is known as having high spectral resolution and sensitivity, but in practice considered to be slow in mapping applications. The present work describes a development of EPMA including design of both instrumental hardware and software related to electronics and calibration.


Biomaterials ◽  
2001 ◽  
Vol 22 (13) ◽  
pp. 1787-1794 ◽  
Author(s):  
Motohiro Uo ◽  
Fumio Watari ◽  
Atsuro Yokoyama ◽  
Hironobu Matsuno ◽  
Takao Kawasaki

JOM ◽  
2020 ◽  
Vol 73 (1) ◽  
pp. 345-355
Author(s):  
Tobin Harvey ◽  
Mark I. Pownceby ◽  
Jeff Chen ◽  
Nathan A. S. Webster ◽  
Thi Bang Tuyen Nguyen ◽  
...  

AbstractAnalogue sinter tablets were produced at temperatures between 1250°C and 1320°C, with a range of hold times and cooling rates. Platy silico-ferrite of calcium and aluminum (SFCA) morphology was identified in samples produced at 1250°C using reflected light microscopy; however, quantitative x-ray diffraction (XRD) identified the presence of the SFCA phase, with no SFCA-I detected. This proves that the platy SFCA morphology common in analysis by reflected light microscopy cannot be attributed to the SFCA-I mineral without further analysis. Micro-XRD and electron probe micro-analysis (EPMA) were carried out on an area of platy SFCA confirming this result. The sinter analogue tablets were reduced in a 30% CO, 70% N2 gas mixture at 900°C in a tube furnace thermo-gravimetric analyzer. The degree of reduction of the tablets in this study was found to be controlled by the porosity of the samples, rather than by the morphology or mineralogy of the bonding phase.


2021 ◽  
Vol 7 ◽  
pp. 78-89
Author(s):  
O.Ya. Chervyatsova ◽  
A.V. Kasatkin ◽  
N.V. Chukanov ◽  
F. Nestola

The paper reports on the results of studies of supergene sulfate mineralization found in a tunnel of the Pyatigorskiy Proval cave. The sulfate minerals include humberstonite K3Na7Mg2(SO4)6(NO3)2·6H2O, sid-eronatrite Na2Fe(SO4)2(OH)·3H2O, metasideronatrite Na2Fe(SO4)2(OH)·H2O, natrojarosite NaFe3(SO4)2(OH)6, tamarugite NaAl(SO4)2·6H2O, and epsomite MgSO4·7H2O, which were identifed by electron probe micro-analysis, powder X-ray difraction and infrared spectroscopy. The presence sulfate sulfur can be related to both the oxidation of sulfde grains, which were found in some samples, and the oxidation of gaseous H2S air oxygen. Humberstonite and metasideronatrite are found for the frst time in Russia.


2020 ◽  
Vol 26 (S2) ◽  
pp. 874-874
Author(s):  
Philipp Poeml ◽  
Karen Wright ◽  
Hirokazu Ohta ◽  
Luca Capriotti ◽  
Jason Harp

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