Reconstruction of the primary bottom of a unique crater lake in the “Meteoryt Morasko Reserve” (Poland)

Pub Date : 2019-12-01 DOI:10.2478/bgeo-2019-0010
A. Choiński, A. Muszyński, M. Ptak, M. Słowik
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引用次数: 1

Abstract

Abstract There are a total of several million lakes in the world, which includes only approximately 30 crater lakes. Due to this extreme global rarity, they are the subject of research in many scientific disciplines. In spite of the widespread interest in them, however, many issues still require detailed investigation. In the case of the Morasko crater lake (Poland), hydrological research has been weakly developed so far. The undertaken analysis, which employed a complex research procedure involving the use of georadar, geological corings and bathymetric measurements, aimed to determine the primary bottom of the lake, and further to determine the scale and rate of its evolution. The modern water level suggests that the lake basin is currently approximately 55% filled in with organic matter, and the rate of its sedimentation in the deepest place can be estimated at approximately 0.8 mm·y−1.
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在“Meteoryt Morasko保护区”(波兰)重建一个独特的火山口湖的初级底部
世界上总共有数百万个湖泊,其中只有大约30个火山口湖。由于这种极端的全球稀缺性,它们是许多科学学科的研究对象。然而,尽管对它们有广泛的兴趣,许多问题仍需要详细调查。以莫拉斯科火山口湖(波兰)为例,迄今为止水文研究发展薄弱。所进行的分析采用了一种复杂的研究程序,包括使用地质雷达、地质取心和水深测量,目的是确定湖泊的初级底部,并进一步确定其演变的规模和速度。现代水位表明,湖盆目前约有55%被有机质填满,其最深处的沉积速率约为0.8 mm·y−1。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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