Real Time Kinematic (RTK) heave as a replacement of Motion Reference Unit (MRU) heave in hydrographic surveying works

Mohammed Elmeligy, Saad Mesbah, Mohamed Mohasseb
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Abstract

Heave is one of the major contributors to errors in water depth measurements. Motion Reference Unit (MRU) measures the heave signal with high-level accuracy as well as other ship motions. Unfortunately, MRU has been reported to have some of drawbacks such as; heave drift error, influence of ship motion dynamic, In addition to its very expensive price Real-Time Kinematic (RTK) GPS uses dual frequency receiver and carrier phase differential technique under kinematic solution and provides very accurate position in all three components in real time. In addition, RTK GPS also calculates the low frequency changes in water level such as tidal oscillation. This research is an attempt to investigate the possibility of using the RTK GPS data to deduce the heave signal from the GPS height (tides - heave) instead of heave from MRU to correct the water depth. Moreover, to examine to what extent, RTK heave can be used as a backup to satisfy the International Hydrographic Organization (IHO) survey order standards. A comparison between the extracted RTK heave and MRU heave signals revealed a good agreement with a strong direct correlation of 0.96. As shown in figure 1 RTK heave as a replacement for MRU heave in hydrographic surveying was statistically validated with the use of a lot of methods of analysis such as Test of the Normality, Paired Samples T Test, Wilcoxon Signed Ranks Test, Heave Signals Frequency Adjustment , Descriptive Statistics for the Two Heave Signals , Descriptive Statistics for Each Signal Individually , Correlation and Trend, Analysis Between the Two Signals, Scatter Diagram and Trend, Standard Deviation and Uncertainty for Soundings, Characteristics of the Difference between Two Signals , Comparing the Surfaces by TIN Model. The results of this analysis provided the possibility of using RTK heave as a replacement for MRU heave in hydrographic surveying. Therefore, RTK GPS is not only used to provide precise position or tidal oscillations but also based on this study, can be used to measure heave accurately to correct the depth satisfying IHO survey standards. Received: 28 January 2023 Accepted: 26 April 2023 Published: 22 May 2023
在水文测量工作中,实时运动学(RTK)升沉取代了运动参考单元(MRU)升沉
起伏是造成水深测量误差的主要原因之一。运动参考单元(MRU)以高精确度测量升沉信号以及其他船舶运动。不幸的是,据报道MRU有一些缺点,例如;实时运动学GPS (RTK)采用双频接收机和载波相位差分技术,在运动学解下,实时提供三个部件非常精确的位置。此外,RTK GPS还计算了潮汐振荡等水位的低频变化。本研究试图探讨利用RTK GPS数据从GPS高度(潮汐-升沉)推导升沉信号的可能性,而不是从MRU升沉来校正水深。此外,还考察了RTK升沉在多大程度上可以作为后备,以满足国际海道测量组织(IHO)的测量顺序标准。将提取的RTK起伏信号与MRU起伏信号进行比较,结果表明两者具有较好的一致性,直接相关系数为0.96。如图1所示,RTK升沉替代MRU升沉在水文测量中得到了统计验证,使用了多种分析方法,如正态性检验、配对样本T检验、Wilcoxon符号秩检验、升沉信号频率调整、两个升沉信号描述性统计、每个信号单独描述性统计、相关性和趋势、两个信号之间的分析、散点图和趋势、测深的标准差和不确定性,两种信号的差异特征,用TIN模型比较表面。分析结果为在水文测量中使用RTK升沉代替MRU升沉提供了可能性。因此,RTK GPS不仅可以提供精确的位置或潮汐振荡,而且基于本研究,可以精确测量升沉,以校正满足IHO测量标准的深度。收稿日期:2023年1月28日收稿日期:2023年4月26日发布日期:2023年5月22日
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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