圣十字山Suchedniów水库沉积物中反映的长期和灾难性过程(波兰)

IF 0.9 Q3 GEOLOGY
Geologos Pub Date : 2019-08-01 DOI:10.2478/logos-2019-0013
P. Przepióra, T. Kalicki, M. Aksamit, Piotr Biesaga, M. Fraczek, P. Grzeszczyk, Emanuela Malęga, M. Chrabąszcz, Edyta Kłusakiewicz, P. Kusztal
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引用次数: 3

摘要

摘要Suchedniów水库位于波兰中部圣十字山脉北部的卡米翁卡河中段。该地区曾属于波兰旧工业区,在中世纪,该工业区通过铁冶金得到了大力发展。河流沿岸的许多锻造厂和工厂使用水力,这导致了一个人为的小规模蓄水系统的建设。在二十世纪初,许多这样的水库在冶金活动崩溃后被抽干。现在的水库建于1974年,于2017年排水。对排水盆地的研究记录了各种形式和沉积物,其中一些记录了当今的沉积过程(防火粘土层、内陆扇三角洲),而另一些则代表了历史时期(较老水库的湖泊沉积物)。灾难性事件的痕迹也得到了保存;一系列巨大的波纹标志着1974年溃坝造成的突然排水。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Secular and catastrophic processes reflected in sediments of the Suchedniów water reservoir, Holy Cross Mountains (Poland)
Abstract The Suchedniów water reservoir is located in the central section of the River Kamionka in the northern part of the Holy Cross Mountains of central Poland. This area once belonged to the Old Polish Industrial District that, during the Middle Ages, was very intensively developed by iron metallurgy. Many forges and mills along the rivers used water power, which led to the construction of an anthropogenic, small-scale water retention system. At the beginning of the twentieth century many of these reservoirs were drained after the collapse of metallurgical activities. The present-day reservoir was built in 1974 and drained in 2017. Research into the drained basin has documented various forms and sediments, some of which record present-day depositional processes (fire proof clay layer, inland fan delta), while others represent the historical period (lacustrine sediments of older reservoirs). Traces of catastrophic events have been preserved as well; an assemblage of megaripples marks the sudden drainage caused by a dam break in 1974.
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来源期刊
Geologos
Geologos GEOLOGY-
CiteScore
1.70
自引率
0.00%
发文量
7
审稿时长
12 weeks
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