brzozÓwka河流域(波兰东北部)的地质雷达勘测

Krzysztof Żurek, T. Kalicki
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引用次数: 0

摘要

蜿蜒的Brzozówka河是Biebrza河的左支流,位于波兰东北部的Podlasie Voivodeship。河流在Goniądz和Suchowola-Janów高地之间的一个宽的北向的隧道谷(冰川洼地)中流动。山谷底部覆盖着泥炭。地质雷达研究的目的是识别坳陷底部的地质构造,确定泥炭厚度及其矿物基础。首先,在GIS环境下定义了河流两岸的两个主要研究剖面。然后它们被分成若干部分,每一部分都有已知的空间坐标。在现场,使用带有500 MHz屏蔽天线的Mala ProEx地质雷达进行GPR分析。在Ground Vision程序中对得到的数据进行处理。研究区共获得21张超声图,总长度3525 m。结果是在东西向建立了一条穿过Brzozówka河谷的探地雷达剖面。超声图上记录了许多不同层次的异常。这可以解释为覆盖着一层有机层的不规则矿物基。这些异常可能是更新世辫状河系统遗迹的证据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
GEORADAR SURVEY OF THE BRZOZÓWKA RIVER VALLEY (NE POLAND)
The investigated meandering Brzozówka River, a left tributary of the Biebrza river, is located in NE Poland in Podlasie Voivodeship. The river flow in a wide N-S orientated tunnel valley (glacial depression) between the Goniądz and Suchowola-Janów Uplands. The valley bottom is covered by peats. The aim of geo-radar research (GPR) was to identify the geological structure of the depression bottom, determine the peat thickness and its mineral base. First, two main research profiles on both sides of the river have been defined in the GIS environment. Then they have been divided into a number of sections, each of which has known spatial coordinates. The field, where GPR profiling was performed using the Mala ProEx geo-radar with a 500 MHz shielded antenna. The obtained data was processed in the program Ground Vision. In total, 21 echograms were obtained in the research area, with a total length of 3525 m. The result was the creation of a GPR profile crossing the Brzozówka River Valley in the W-E orientation. A number of anomalies at different levels have been recorded on echograms. There can be interpreted as an irregular mineral base covered with an organic layer. These anomalies may be evidence of a remnant of the Pleistocene braided river system.
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