The Effect of Stabilizing Piles on a Self-Supported Earth-Retaining Wall     

Jaeuk Sim  Kyoungchul Kim 《Marine Georesources & Geotechnology》2016,34(3):265-279

The behavior of a self-supported earth-retaining wall with stabilizing piles was investigated using a numerical study and field tests in urban excavations. Special attention is given to the reduction of lateral earth pressures acting on a retaining wall with stabilizing piles. Field tests at two sites were performed to verify the performance of the instrumented retaining wall with stabilizing piles. A number of 3D numerical analyses were carried out on the self-supported earth-retaining wall with stabilizing piles to assess the results stemming from wide variations of influencing parameters such as the soil condition, the pile spacing, the distance between the front pile and the rear pile, and the embedded depth. Based on the results of the parametric study, the maximum horizontal displacement and the maximum bending moment are significantly decreased when the retaining wall with stabilizing piles is used. In engineering practice, reducing the pile spacing and increasing the distance between the front pile and the rear pile can effectively improve the stability of the self-supported earth-retaining wall with stabilizing piles.  相似文献   

正规矩阵选取半参数灰色模型改进的预测建模     

周敏  周世健  王奉伟 《测绘科学》2016,41(8):152-155,164

正规矩阵是对模型误差补偿性的直接表达,时间序列法用一阶差分方程和二阶差分方程计算得到不同的正规矩阵。针对传统GM(1,1)模型没有考虑模型误差,而数据处理过程中所建立的数学模型与客观现实并不一致的问题,该文提出建立顾及模型误差的半参数模型的GM(1,1)模型。对由传统半参数模型得到的正规矩阵采取一阶差分法进行改进,并通过算例证实了改进正规矩阵的半参数模型的GM(1,1)预测精度更高。  相似文献   

侧扫声呐图像分割的中性集合与量子粒子群算法   总被引：1，自引：1，他引：0  

赵建虎  王晓  张红梅  胡俊  简晓敏 《测绘学报》2016,45(8):935-942

针对现有的侧扫声呐图像分割方法存在分割准确率不高和效率偏低的问题,提出了一种基于中性集合和量子粒子群算法的侧扫声呐图像阈值分割方法。通过基于中性集合计算图像灰度共生矩阵,实现了侧扫声呐图像精细纹理的表达,提高了分割精度;基于二维最大熵理论,采用量子粒子群算法计算二维最优分割阈值向量,实现了分割阈值向量的快速准确获取,提高了分割效率和精度。最终实现了高噪声侧扫声呐图像目标的准确、高效分割。通过对含有不同目标的侧扫声呐图像的分割试验,验证了该算法的有效性。  相似文献   

A fisheries application of a dual-frequency identification sonar acoustic camera   总被引：2，自引：2，他引：2  

Moursund  Russell A; Carlson  Thomas J; Peters  Rock D 《ICES Journal of Marine Science》2003,60(3):678-683

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侧扫声纳声线反射和折射干扰的实验分析     

邓志军  魏建江  葛健  丰启明 《海洋测绘》2006,26(6):45-47

介绍了侧扫声纳由自身声源反射和折射衍生的两种干扰波的形成机理,提出以绘制声线图进行分析的研究方法,着重通过海上实作验证了温度跃层产生的声线弯曲对声纳的影响特点,为外业工作的设计和施测提供了几点建议。  相似文献   

A consistent approach to definitions and symbols in fisheries acoustics   总被引：7，自引：17，他引：7  

Maclennan  David N.; Fernandes  Paul G.; Dalen  John 《ICES Journal of Marine Science》2002,59(2):365-369

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Evidence for a clustered spatial distribution of clupeid fish schools in the Norwegian Sea and off the coast of southwest Africa   总被引：1，自引：0，他引：1  

Haugland  Eli Kyrkjebo; Misund  Ole Arve 《ICES Journal of Marine Science》2004,61(7):1088-1092

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Strike-slip tectonic processes in the northern Caribbean between Cuba and Hispaniola (Windward Passage)     

Eric Calais  Bernard Mercier De Lépinay 《Marine Geophysical Researches》1995,17(1):63-95

Marine geophysical data including Seabeam, seismic reflection, magnetics, gravimetry and side-scan sonar have been recently collected along the northern Caribbean strike-slip plate boundary between Cuba and Hispaniola, in the Windward Passage area. The analysis of this comprehensive data set allows us to illustrate active strike-slip tectonic processes in relation to the kinematics of the Caribbean Plate. We show that the transcurrent plate boundary trace runs straight across the Windward Passage, from the southern Cuban Margin in the west (Oriente Fault) to the Tortue Channel in the east. The Windward Passage Deep is thus not an active pull-apart basin, as previously suggested. The plate boundary geometry implies that the motion of the Caribbean Plate relative to the North American Plate is partitioned between a strike-slip component, accommodated by the Windward Passage active fault zone, and a convergence component, accommodated by compression at the bottom of the Northern Hispaniola Margin. On the basis of a correlation with onland geological data, an age is given to the stratigraphic sequences identified on seismic profiles. A kinematic reconstruction is proposed that follows the tectonic unconformities recognized at sea and on land (Late Eocene, Early Miocene, Middle Miocene and Late Pliocene). Each one of these tectonic events corresponds to a drastic reorganization of the plate boundary geometry. We propose to correlate these events with successive collisions of the northern Caribbean mobile terranes against the Bahamas Bank. During each event, the plate boundary trace is shifted to the south and a part of the Caribbean Plate is accreted to North America.  相似文献   

基于小波变换的声纳图像边缘特征检测研究   总被引：1，自引：0，他引：1  

贾伟广  李希玲 《海洋技术学报》2006,25(3):103-105

声纳图像的边缘特征检测是其目标识别技术的重要技术基础。声纳图像背景复杂、噪声污染严重,而传统的边缘检测方法对图像噪声非常敏感,所以针对这一特点,利用小波变换易于消除噪声、运算方便的数学特征,提出了一种基于小波变换的声纳图像边缘特征检测算法。由计算机仿真结果可以得到,与传统的边缘检测算法相比,此算法在有效地抑制噪声的同时,还可以得到较高的边缘定位精度,能够很好地检测到原始声纳图像的边缘。  相似文献   

Structure and Stability of Non-Transform Discontinuities on the Mid-Atlantic Ridge between 24° N and 30° N     

Sara Spencer  Deborah K. Smith  Johnson R. Cann  Jian Lin  Edward McAllister 《Marine Geophysical Researches》1997,19(4):339-362

Observations of the median valley within the 24–30° N area ofthe Mid-Atlantic Ridge (MAR), using the IOSDL high resolutionside-scan sonar instrument TOBI, image four separate areas of themedian valley, containing part or all of nine spreading segments, and fivenon-transform discontinuities between spreading segments (NTDs).These high resolution side scan images were interpreted in parallel withmultibeam bathymetry (Purdy et al., 1990), giving a greater degree ofstructural precision than is possible with the multibeam data alone. Threedistinct types of NTD were identified, corresponding in part to typespreviously identified from the multibeam bathymetric survey of the area.Type 1 NTDs are termed septal offsets, and are marked by a topographic ridgeseparating the two spreading segments. The offset between the spreadingsegments ranges from 9 to 14 km. These can be further subdivided into Type1A in which the septa run parallel to the overall trend of the MAR and Type1B in which the septa lie at a high angle to the bulk ridge trend. Type 1ANTDs are characterised by overlap of the neovolcanic zones of the segmentson each side, and strong offaxis traces, while Type 1B NTDs show no overlapof neovolcanic zones, and weak offaxis traces. Type 2 NTDs arebrittle/ductile extensional shear zones, marked by oblique extensionalfractures, and associated with rotation of tectonic and volcanic structuresaway from the overall trend of the MAR. Type 3 NTDs are associated withoffsets of less than 5 km, and show no sign of any accommodating structure.In this type of NTD, the offset zone is covered with undeformed volcanics.The type of NTD developed at any locality along the ridge axis appears todepend on the amount of segment offset and segment overlap, the overalltrend of the mid-ocean ridge, the width of the zone of discontinuity, themedian valley offset and the longevity of the offset. These factorsinfluence the mechanical properties of the lithosphere across thediscontinuity, and ultimately the tectonic style of the NTD that can besupported. Thus brittle/ductile extensional shear zones are long-livedstructures favoured by large segment offsets, and small or negative segmentoverlaps. Septa can be short or long lived, and are associated with largesegment offsets. Segment overlaps vary from negative (an along axis gap) tozero, for Type 1B septal offsets, or positive to zero for Type 1A septaloffsets. Non-tectonised NTDs are generally short lived structures,characterised by small segment offsets and zero or positive overlaps.  相似文献