Mineral Composition of Sapropelles of Lakes of the Right Bank of the Ob River (Middle Ob Region)

M. Sartakov, E. Osnitsky, K. Kudrin, N. S. Larina
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引用次数: 1

Abstract

The objective of this work is to study the mineral composition of bottom sediments of eight small lakes located on the right bank of the Ob River (Western Siberia) in the Surgut region of the Khanty-Mansiysk Autonomous Okrug - Yugra. The studies were carried out using wave dispersive X-ray fluorescence (WDFR) spectroscopy. The content of organic substances, ash, and oxides in the ash in the samples was determined. Based on these data, the studied bottom sediments were classified. The bottom sediments of Lake S-1 are siltstone sands, lakes Vach Lor and S-189 - weakly sapropelic siltstone sands, lakes S-5, S-6, S-3, S-89, and S-294 - typical sapropels. The article presents the content of the main elements in the ash of the studied samples.
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鄂毕河右岸(鄂毕中地区)湖泊锯末矿物组成
本工作的目的是研究鄂毕河(西西伯利亚)右岸的八个小湖的底部沉积物的矿物成分,这些小湖位于汉特-曼西耶斯克自治区的苏尔古特地区。这些研究是使用波散射X射线荧光(WDFR)光谱进行的。测定了样品中灰分中有机物、灰分和氧化物的含量。根据这些数据,对所研究的海底沉积物进行了分类。S-1湖的底部沉积物为粉砂岩,Vach Lor湖和S-189湖为弱腐泥质粉砂岩,S-5、S-6、S-3、S-89和S-294湖为典型腐泥。本文介绍了研究样品灰分中主要元素的含量。
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