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Development of mud layer detecting device and its application to the measurement of vertical slices of density profile in Kushiro Port

机译:Ku路口泥层探测装置的研制及其在密度剖面垂直切片测量中的应用

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The vertical slices of density profile along the surveying lines provide important information for establishing a countermeasure for the deterioration of coastal marine environments and for the shoaling of waterway or anchorage with a drift of soft mud such as low consistency clay or silt. To detect the density profiles of the mud layer from the surface ship, a mud layer detecting device using wide-band and narrow beam underwater acoustic pulses has been developed for the detection in the sea areas of several tens of meters deep. The device has 3 acoustic transducers that transmit and receive 25, 71 and 250 kHz signals respectively. The beam angle of these transducers is 2 degrees and their band width is equal to the half of the central frequency. The device receives the acoustic signals reflected from the sea bottom, digitizes them, stores them in the hard disk of a computer located on the ship and analyzes them off-line using a wave-form analyzing technique. This device was used to obtain over 10 vertical slices of the density profile in Kushiro Port (Hokkaido, Japan). The density profiles that were obtained by using this device agree well with those of the core-sample. The surface density distribution was low, less than 1.3 g/cm/sup 3/, at the east side of the port, but over 1.4 g/cm/sup 3/ at the west side of the port which is open to the waterway. According to results of sounding before and after the "Offshore of Tokachi Earthquake in 2003" (Sep. 26, 2003), the depth after the earthquake was about 50 cm deeper than the one before the earthquake. This depth change is considered caused from the movement of the surface sediment by Tsunami from the earthquake. The higher density area over 1.4 g/cm/sup 3/ at the west side of the port is deemed caused as the result of the movement of the surface sediments. The change of sedimentation can be known easily with this device as described above. It is expected that this device is applicable to the maintenance and control of ports and harbors.
机译:沿着测量线的密度剖面的垂直切片可提供重要的信息,以便为对付沿海海洋环境恶化,淡化水道或利用软泥(例如低稠度黏土或淤泥)流失的锚地提供对策。为了检测水面舰船上的泥浆层的密度分布,已经开发了一种使用宽带和窄束水下声脉冲的泥浆层检测装置,用于在几十米深的海域中进行检测。该设备具有3个声换能器,分别发送和接收25、71和250 kHz信号。这些换能器的束角为2度,其带宽等于中心频率的一半。该设备接收从海底反射的声信号,将其数字化,将其存储在船上计算机的硬盘中,并使用波形分析技术进行离线分析。该设备用于获取Ku路港口(日本北海道)的密度分布的10多个垂直切片。通过使用该设备获得的密度曲线与岩心样品的密度曲线非常吻合。表面密度分布很低,在港口的东侧小于1.3 g / cm / sup 3 /,但在通向水路的港口西侧的表面密度分布超过1.4 g / cm / sup 3 /。根据“ 2003年十胜海上地震”(2003年9月26日)前后的测深结果,地震后的深度比地震前的深度约50厘米。这种深度变化被认为是地震引起的海啸造成的地表沉积物运动的结果。认为在港口西侧的密度较高的区域超过1.4 g / cm / sup 3 /是表面沉积物运动的结果。如上所述,利用该装置可以容易地知道沉降的变化。期望该设备适用于港口的维护和控制。

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