利用潮汐效应测量河流深度

N. Hirata, Krisana Punayangkool, K. Kose, K. Hasegawa
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引用次数: 0

摘要

东南亚有许多适合高速铁路运输的河流。然而,在雨季结束时,大量的沉积物积聚在河流中,导致频繁的事故,如搁浅。因此,这些河流需要疏浚,以确保安全航行。为此,及时、方便地测量水深是非常重要的。然而,在大范围内测量水深仍然很困难,作者提出了一种简单的方法。研究了动态GPS (K−GPS)测深仪在河流水深测量中的应用。然而,在进行精确测量时,潮汐效应应该被考虑在内。用线性插值法从潮汐表中估计各测点的潮位。将K−GPS测得的河面高度(飴)代入估算的河面高度(①),估算出各点的河图基准面。结果表明,下界海图基准面与上界海图基准面重合,验证了所提出的消潮方法。因此,可以将潮汐信息与测深数据相结合,得到河流水深。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Survey the River Depth with Tidal Effect
In South East Asi4 there are many rivers that are suitable fbr transportatio η. However , at the end of rainy season , a large amount of sedimentatbn afises in the river 」t causes frequent accidents such as groundings. Therefbre, thosc rivers need to be dredged fbr the safety navigation . For this purpose, 置t is very important to measure the water depth timeiy and easily . However , it is still difficult to measure water depth in wide are 乱 The authors have proposed a simple method . Tlle m 巳asurement of water depth ef the river using Kinematic GPS (K −GPS ) sounder is investigated . However , the tidal effect should be taking into an account fbr the precise measurement . The tide level of each measurement point estimated by linear interpolation f}om tide tables. Substituting 血 us est1mated t量de level仕om the measured surface altitude ofthe river sur 飴ce by K−GPS , river chart datum of each polnt was estimated. Thus estimated chart datum on downstre 一bound and 叩 stream −bound coincide weU , and the proposed method of eliminating tide was verified . Therefore it{s able to obtain the river water depth combirling the tide{nf()rmation and measured sounder data.
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