特列博维奇湖的景观特征与资源潜力

V. Martyniuk, I. Zubkovych
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摘要

评估景观自然资源潜力的问题,特别是湖泊的自然-水生复合体(NAC)的问题得到更新。湖泊代表着水、生物、有机矿物和娱乐资源。湖底建有旅游设施、疗养院、游憩场所、养鱼场、采矿企业、自然公园和自然保护区。有鉴于此,有必要研究湖泊景观资源潜力,主要是湖泊资源,这将成为投资者和水资源综合管理的信息库。研究的目的是为了证实捷列博维奇湖的景观和地理特征及其资源潜力,以满足平衡自然管理的需要。在研究过程中,使用了湖泊的水深剖面、一般湖泊学方法、土壤地球化学剖面、景观湖泊学方法、湖泊和湖盆系统的gis制图建模等方法。研究的结果。建立了Terebovichi湖的数字测深图,水深间隔为0.25 m,局部深度最大为2.4 m,并计算了水库的主要形态和水文参数。通过解剖有机粘土、有机铁、褐铁矿三种类型的腐泥岩,绘制了湖泊沉积物地层剖面,建立了湖泊景观结构的制图模型,并进行了景观计量分析。结论。结果表明,捷列博维奇湖盆地中沉积率为79.34%。被冲积物覆盖的面积为50.0公顷,部分延伸到水库之外。平均厚度5.46 m,最大厚度11.3 m;推进器总容积为223.9万立方米。平衡地质储量- 49.8万吨,平衡地质储量- 6.1万吨。该湖泊具有良好的开发和提取前景。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
LANDSCAPE FEATURES AND RESOURCE POTENTIAL OF LAKE TEREBOVYCHI SAPROPEL
The problem of assessing the natural-resource potential of landscapes and natural-aquatic complexes (NAC) of lakes, in particular, is updated. Lakes represent water, biotic, organo-mineral, and recreational resources. Tourist facilities, sanatoriums, recreational shelters, fish farms, sapropel mining enterprises, natural parks, and nature reserves operate on the base of the lakes. Given the above, there is a need to study the landscape-resource potential of lakes, primarily sapropel resources, which will become an information base for investors and integrated management of water resources. The purpose of the research is to substantiate the landscape and geographical features of Terebovichi lake and the resource potential of sapropel for the needs of balanced nature management. In the research process, methods of bathymetric profiling of lakes, general limnological methods, soil-geochemical profiling, landscape-limnological methods, GIS-cartographic modeling of lakes and lake-basin systems have been used. Research results. A digital bathymetric map of the lake has been created Terebovichi, with a depth interval of 0.25 m and a local deepening with the greatest depth of 2.4 m, has been found, and the reservoir's main morphometric and hydrological parameters have been calculated. A stratigraphic section of lake sediments has been made with the dissection of three types of sapropel (organo-clay, organo-iron, limonite), and a cartographic model of the landscape structure of the NAC lake has been constructed, and its landscape metric analysis has been carried out. Conclusions. It was established that the basin of Terebovichi lake is 79.34% filled with sapropel deposits. The area covered by sapropel is 50.0 ha, partially extending beyond the reservoir. The average thickness of sapropel is 5.46 m, and the maximum is 11.3 m; the total volume of sapropel is 2239 thousand m3. Balance geological reserves of sapropel – 498 thousand tons, off-balance reserves – 61 thousand tons. The lake is promising for the development and extraction of sapropel.
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