MONQAR EL SANAB-MONQAR EL RAML SILICA SAND, QARAT SOMARAH REGION, EGYPT: ECONOMIC POTENTIAL AND SOME FORM OF PROCESSING TECHNIQUES

Hassaan
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Abstract

Monqar El-Sanab Monqar El-Raml area is located 50 km SSW El-Hammam city, Northern Western Desert between latitudes 30°26'30" and 30°20'00"N. and longitudes 29°09"00" and 29°22"30" E. The composite stratigraphic succession of the Early Miocene Moghra Formation includes exposed very compact and consolidated ferruginous sandstones, calcareous silica sand and silica sand beds 19.5m thick and greyish black clay and shale bed 1.5m thick at its top. Silica sand is essential raw materials for glassmaking, industrial, horticultural, leisure and foundry casting applications. The study aims at undertaking investigations on the silica sand geologic features, grain size, chemical composition, easy remove of deleterious impurities, together with the level of friable sand some required form of processing technique to conform very closely to the standard specifications, and consistency in quality suitable for economic applications. The silica sand beds are sited at the top of southwards moderate sloping to the base of the succession. The consolidated and very compact ferruginous sandstones comprise calcareous quartz arenite and ferruginous calcareous quartz arenite. Both consist chiefly of >90% quartz, fine to coarse, rounded to sub-angular occasionally fractured grains (>95wt. % silica). The SiO2 discriminates three Grades I, II, III: > 98, < 98 > 97, < 97> 95 wt. % and as well, Al2O3 and Fe2O3 contents: 0.35 0.14, 1.710.3; 0.80.2, 2.3-1.71; and 1.840.4, 2.3 1.71 wt. % respectively. The 3 grades record highest wt. % of the size <600 μm >106 μm to be considered suitable for upgrading the sand. Exceptional samples of Grades I, II exist where the sizes >600 μm possess high wt. % to recommend combination of these size classes > 600 μm of the sand from the sites of such samples on exploitation. The washing of the sizes <600 μm >106 μm produced sharp decrease of Fe2O3, CaO content of the three grades (times 0.39, 0.32, 0.18 and 0.46, 0.35, 0.016). Loss on washing with water is 6.4, 1.8, 16.0 kg/ton and with 2 and 5% HCl solution 6.4, 1.8, 16.0 kg/ton to be considered an approach of suitable upgrading.
埃及卡拉索马拉地区的Monqar el sanab-monqar el ramel硅砂:经济潜力和某种形式的加工技术
Monqar El-Raml地区位于北纬30°26′30”至30°20′00”之间的西部沙漠,El-Hammam市西南偏南50公里。东经29°09”00”和29°22”30”e,早中新世Moghra组复合地层序列包括出露的非常致密固结的含铁砂岩、19.5m厚的钙质硅砂和硅砂层,顶部为1.5m厚的灰黑色粘土和页岩层。硅砂是玻璃制造,工业,园艺,休闲和铸造铸造应用的重要原料。本研究旨在调查硅砂的地质特征、粒度大小、化学成分、易去除有害杂质、易碎程度以及砂的某些加工工艺形式,使其非常符合标准规范,且质量一致性适合经济应用。硅质砂层位于向南缓坡的顶部至序列底部。固结且非常致密的含铁砂岩包括钙质石英砂岩和含铁钙质石英砂岩。两者主要由>90%的石英组成,细到粗,圆形到次角状,偶尔断裂的晶粒(>95wt)。%硅)。SiO2区分I、II、III三个等级:> 98、< 98 > 97、< 97> 95 wt. %, Al2O3和Fe2O3含量分别为0.35、0.14、1.710.3;0.80.2, 2.3 - -1.71;1.840.4%、2.3 1.71 wt. %。3个等级的106 μm尺寸的wt %最高,被认为适合升级砂。粒径>600 μm的I级和II级特殊样品具有较高的wt. %,建议在开采时使用这些粒径>600 μm的样品组合。106 μm尺寸的洗涤使3个等级的Fe2O3、CaO含量急剧下降(分别为0.39、0.32、0.18和0.46、0.35、0.016次)。水洗损失分别为6.4、1.8、16.0 kg/吨,2%和5% HCl溶液水洗损失分别为6.4、1.8、16.0 kg/吨。
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