首页> 外文期刊>Rasayan Journal of Chemistry >INVESTIGATION ON THE MINERALOGICAL PHASE OF ANCIENT BRICK SAMPLES OF KATHMANDU VALLEY (NEPAL) USING XRD AND FTIR ANALYSIS
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INVESTIGATION ON THE MINERALOGICAL PHASE OF ANCIENT BRICK SAMPLES OF KATHMANDU VALLEY (NEPAL) USING XRD AND FTIR ANALYSIS

机译:XRD和FTIR分析加德满都谷地古砖样品的矿物相

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The total eight clay brick samples including five archaeologically importance samples from different historical sites and three samples from more than a century old buildings of Kathmandu valley were collected and their mineralogical phases were characterized using X-ray diffraction and Fourier transform infrared spectroscopic methods in this study. Mineralogical phases existed in these archaeological and ancient clay bricks are identified as quartz, feldspars, spinel, muscovite, margarite and hematite in accordance with the powder diffraction standard files. The degree of the disappearance of feldspars phase and appearance of the spinel phase in all the brick samples is found to be different indicating that the firing temperature applied to produce these brick specimens should not be same. The firing temperature applied for the production of the eight clay brick samples should be in the range of 900°-1000° C. Most of the archaeological clay brick samples used in this study should be produced by firing at the high-temperature comparison with those brick samples used in old buildings of Kathmandu valley.
机译:本研究共收集了八种粘土砖样品,包括来自不同历史遗址的五个具有考古学意义的样品和来自加德满都谷地一个百年以上历史建筑物的三个样品,并使用X射线衍射和傅里叶变换红外光谱法对其矿物学相进行了表征。 。根据粉末衍射标准文件,这些考古和古代粘土砖中存在的矿物学相被鉴定为石英,长石,尖晶石,白云母,玛格石和赤铁矿。发现所有砖样品中长石相的消失程度和尖晶石相的出现程度均不同,这表明用于生产这些砖样品的烧成温度不应相同。用于生产八个黏土砖样品的烧成温度应在900°-1000°C的范围内。本研究中使用的大多数考古黏土砖样品应通过在高温下进行烧成来生产。加德满都山谷的老建筑中使用的砖样品。

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