水下地貌学:选择、任务、需求

Pub Date : 2019-06-18 DOI:10.2478/bgeo-2019-0006
S. Rudowski, R. Wróblewski, J. Dworniczak, K. Szefler, B. Hac, Łukasz G. Gajewski
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引用次数: 1

摘要

摘要:本文的目的是介绍目前非侵入性海底测量方法的潜力,包括海洋和内陆水库的地形和结构的图解。本文介绍了Gdańsk海事研究所使用相同设备在海底、湖泊和河流进行调查时获得的结果示例:主要是用多波束回声测深仪(MBES)获得数字地形模型(DTM);侧面扫描声纳(SSS),以获得底部性质的一般图像(其“粗糙度”);以及地震剖面(海底剖面仪、沉积物回声测深仪[SES])来识别海底结构。所获得的结果构成了必要时开展进一步的专家调查(非侵入性或侵入性)的基础。目前使用MBES、SSS和SES的海底测量方案可能被视为使用LiDaR和GPR(地面穿透雷达)进行地面测量的水下等效。
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Subaqueous geomorphology: options, tasks, needs
Abstract The purpose of the paper is to present the potentialities of current non-invasive methods for bottom surveys, including cartometric presentation of its relief and structure in both marine and inland reservoirs. The paper presents examples of results obtained in the Maritime Institute in Gdańsk during surveys carried out at the bottom of seas, lakes and rivers with the use of the same apparatus: primarily, a multibeam echosounder (MBES) to obtain a digital terrain model (DTM); a side-scan sonar (SSS) to obtain a general image of the nature of the bottom (its “roughness”); and seismic profiling (sub-bottom profiler, sediment echo sounder [SES]) to recognise the structure of the bottom. The obtained results constitute a necessary basis for carrying out further specialist surveys (non-invasive or invasive) when needed. Current bottom survey options that use MBES, SSS and SES may be treated as subaqueous equivalents of the subaerial potentialities of a land surface survey using LiDaR and GPR (Ground Penetration Radar).
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