Studying Baikal region sand properties

A. A. Yakovleva, E. A. Guseva, M. Konstantinova
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引用次数: 1

Abstract

The study is aimed at a more detailed determination of the thermal properties of Baikal region sands and establishment of their dependence on geological and mineralogical characteristics in order to assess the possibility of using this raw material in the food industry. The objects of the study are sands sampled on the southwestern coast of Lake Baikal. The subject of the study is the mineralogical composition of sand, its grain size composition and heat capacity. The mineral composition of sand samples and their crystal structure were studied using the method of X-ray phase analysis. A standard sieve analysis method was used for granulometric estimation of sands. The average heat capacity of sand samples was determined by the mixing method. Based on the analysis of the obtained X-ray diffraction patterns, the mineralogical composition of the studied samples was determined. It was found that quartz predominates in their composition since its percentage in samples amounts to 40–60 %. The proportion of such minerals as albite and anorthoclase is 15–30 % in different samples. Less than 5 % in each sample accounts for dickite and indialite. The presence of the mineral of anthophyllite has been found only in one sample in the amount of about 9 %. The results of granulometric composition determination show that a fraction, which accounts for 70–90 %, can be isolated in most samples. The sample from the town of Slyudyanka was the only one where the fractions of different sizes were present in approximately equal amounts. For this sample, the dependence of heat capacity on the grain size was determined. In other samples, the difference in certain heat capacity values correlated well with their mineralogical composition. The results of the conducted studies and their analysis  allow to conclude that Slyudyanka and Baikalsk sands are the most attractive sands in terms of high heat capacity. The sand with the grain size from 0.125 to 0.25 mm is found to be the most suitable for the use as a thermal storage medium. This fraction is predominant in the sand of the town of Baikalsk.
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研究贝加尔湖地区砂的性质
这项研究的目的是更详细地确定贝加尔湖地区沙子的热特性,并确定它们对地质和矿物学特征的依赖性,以便评估在食品工业中使用这种原料的可能性。研究对象是贝加尔湖西南海岸取样的沙子。研究的主题是砂的矿物组成,其粒度组成和热容。用x射线相分析方法研究了砂样的矿物组成和晶体结构。采用标准筛法对砂粒进行粒度测定。采用混合法测定了砂样的平均热容。根据所获得的x射线衍射图的分析,确定了所研究样品的矿物组成。样品中石英含量为40 ~ 60%,以石英为主。钠长石、斜长石等矿物在不同样品中的比例为15 ~ 30%。每个样品中不超过5%是dickite和indiite。仅在一个样品中发现了约9%的花青石矿物的存在。颗粒组成测定结果表明,在大多数样品中可分离出占70 - 90%的组分。来自斯柳京卡镇的样本是唯一一个不同大小的分数大致相等的样本。对于该样品,确定了热容与晶粒尺寸的关系。在其他样品中,某些热容值的差异与它们的矿物组成密切相关。所进行的研究和分析的结果表明,就高热容量而言,斯柳扬卡和贝加尔斯克的沙子是最具吸引力的沙子。粒度为0.125 ~ 0.25 mm的砂最适合作为储热介质。这个部分在贝加尔斯克镇的沙子中占主导地位。
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