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排序方式: 共有480条查询结果,搜索用时 15 毫秒
61.
用对称反投影及递归迭代实现扇束CT快速重建 总被引:5,自引:1,他引:4
为提高扇束滤波反投影(FBP)算法重建CT图像的速度,本文提出了一种利用对称反投影并结合递归迭代的方法来减少反投影的运算量.研究表明该方法可使重建速度提高约23倍,且不会带来新的重建误差. 相似文献
62.
Charles W. Finkl Jr. Syed M. Khalil Jeffrey L. Andrews 《Marine Georesources & Geotechnology》2013,31(2):155-173
Erosion of sandy beaches is a worldwide problem that elicits innovative geoengineer‐ing techniques to reduce adverse impacts of shoreline retreat. Beach replenishment has emerged as the “soft”; shore‐stabilization technique of choice for mitigating beach erosion. This method of shore protection involves the addition of sand to the littoral sediment budget for sacrificial purposes. Because inland sand sources are often uneconomical or impractical to use, and known nearshore sources are limited, finding adequate quantities of suitable sand on the inner continental shelf is often vital to beach replenishment projects. The technical studies of survey and materials analysis that identify and delineate usable sand sources are sometimes almost as expensive as small‐project dredging, pumping, and placing the sand on the beach as fill. Inadequate quantity or substandard quality of shelf sand, as well as often‐prohibitive overhead expenses, thus compel shoreline managers to seek suitable sand sources offshore. In the study area off the central‐west coast of Florida, offshore potential borrow areas (PBAs) were identified on the basis of studies conducted in reconnoitory and detailed phases. Sophisticated state‐of‐the‐art equipment used in this investigation provided more detailed subbottom mapping information than is normally obtained with conventional seismic equipment. An example of sand exploration studies was incorporated in a 215‐km2 survey of offshore areas by conducting bathymetric surveys and subbottom seismic profiling, collecting jet probes, grab samples, and vibrocores, and analyzing sediment grading in subsamples from vibrocores. These combined analyses indicated that at least 8.8 ×106 m3 of sand is available in potential borrow areas from 7.0 to 12 km offshore in water depths of 8.0 to 11.5 m. In the PBAs, mean grain size of sand falls into the range 0.13–0.53 mm, sorting averages 0.65–1.31ø, and the overall silt content varies from 3.9–8.5%. High silt contents (13–19%) mapped in some areas make these sedimentary deposits unsuitable as fill for artificial beach renourishment. 相似文献
63.
Michael J. Dunnington Richard A. Wahle Michael C. Bell Nathan R. Geraldi 《新西兰海洋与淡水研究杂志》2013,47(6):1253-1276
Seabed mapping, spatially referenced trapping, and mark‐recapture methods have all been useful tools in ecological studies of lobsters and other benthic animals. Here we integrate the three methods to evaluate local population dynamics and movements of American lobsters, Homarus americanus, in coastal fishing grounds in Maine, United States. The study was conducted on five study areas of different size, and used two different sampling protocols. At one site (1 km2 in area) we used a monthly mark‐recapture sampling interval over a 6‐month period, only tagging a subsample of the catch. At four smaller sites (0.3 km2) we used a shorter‐term approach, sampling at 3–4‐day intervals for a 2‐week duration, tagging the entire catch. Tagging data were analysed with a modified Jolly‐Seber model adapted for continuous sampling to estimate population abundance, gains (immigration), and losses (emigration and mortality). Side‐scan sonar surveys of the seabed combined with diver‐based population surveys, stratified by substrate type, provided an independent comparison to mark‐recapture‐based estimates of abundance over the same areas. Spatial referencing of trap catch also allowed us to relate catch rates and lobster movements directly to seabed features. The longer‐term tagging data on the larger study area provided abundance estimates that were more consistent with the diver observations, and estimates of gains and losses statistically more robust, than those derived from the shorter‐term effort on the smaller sites. The flux of lobsters followed the well known seasonal movements on these fishing grounds, with gains and losses from the larger study area ranging over 1000 individuals per day, and an estimated mid‐summer peak density of >65 000 lobsters per km2 (individuals >50 mm carapace length). This approach may lend itself to broader application with the American lobster. 相似文献
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65.
针对海底侧扫声纳图像对比度低、纹理弱、噪声严重等问题,提出了一种基于第二代Curvelet变换的声纳图像增强算法。首先对原始声纳图像进行多尺度、多方向的Curvelet变换分解,得到低频子带和高频子带;然后引入非线性S型函数对低频系数进行处理,提高图像整体的对比度;采用一种可以避免过度增强的新型非线性函数对各尺度的高频子带系数进行处理,提高图像整体的对比度,增强图像边缘和纹理细节,并通过估计噪声水平设定阈值进行阈值降噪。最后经Curvelet逆变换得到增强图像。实验表明,该方法不仅改善了海底侧扫声纳图像对比度低的问题,而且降低了噪声,突出了声纳图像的边缘和纹理细节。 相似文献
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68.
目的:探讨腹部能谱CT血管成像双低扫描方案的可行性和应用价值。方法:前瞻性收集疑腹部病变需行全腹血管CT成像BMI≤25的患者367例。首先按照首诊时间分实验组和对照组,再根据体质指数(BMI)分成两个亚组,BMI≤22为实验1组或对照1组,22vol,对比剂碘含量及肾动脉图像质量评分。结果:腹主动脉CT值:实验1组、实验2组分别为(601.75±67.11)HU和(459.87±49.17)HU,对照1组、对照2组分别为(436.55±84.12)HU和(432.15±87.68)HU,实验1组>对照1组,差异具有统计学意义(P值<0.05)。CNR:实验1组、实验2组分别为(19.01±2.66)和(15.24±2.52),对照1组、对照2组分别为(12.42±2.68)和(10.24±2.22),实验1组>对照1组,实验2组>对照2组,差异均有统计学意义(P<0.05)。FOM:实验1组、实验2组分别为(69.72±29.75)和(33.44±8.87),对照1组、对照2组分别为(20.08±8.05)和(15.21±10.12),实验1组>对照1组,实验2组>对照2组,差异均有统计学意义(P值<0.05)。CTDIvol:实验1组、实验2组为(5.41±1.38)mGy和(6.98±1.49)mGy,对照1组、对照2组为(9.87±2.97)mGy和(12.02±5.21)mGy,实验1组较对照1组降低45.19%(4.46/9.87)、实验2组较对照2组降低41.93%(5.04/12.02)。实验组、对照组的碘对比剂浓度分别为270mgI/mL和350mgI/mL,实验组降低22.86%(80/350)。肾动脉血管评分:实验1组、实验2组分别为(4.61±0.47)和(4.22±0.59),对照1组、对照2组分别为(3.73±0.72)和(3.93±0.66),实验1组>对照1组,差异具有统计学意义(P<0.05);实验2组与对照2组间差异无统计学意义(P值>0.05)。结论:针对中小体质指数患者,双低扫描方案腹部能谱CT血管成像在保证图像质量的同时可以大幅度地降低辐射剂量和碘对比剂含量,适于推广临床应用。 相似文献
69.
断裂带变形分析方法研究 总被引:1,自引:0,他引:1
结合地质、地球物理和小震精定位结果,对小江断裂带3条断层参数地质分段进行合理选取,并设定一定的差异范围,利用GPS区域网资料分析各断层段的变形状态。结果表明,断层参数的设定对反演结果影响很大(导致断层的位错量差异高达3 mm)。在断层参数难以确定的情况下,扫描线段法在一定程度上能反映断层的变形状态。 相似文献
70.
Michael Wiedenbeck Dina Schulze Ilya Veksler 《Geostandards and Geoanalytical Research》2009,33(1):111-114
This short technical note describes a simple technique for synthesising an optimised binary glass for performing coarse mass table calibrations of secondary ion mass spectrometers. A Ge-Bi glass doped with five selected trace elements was used to anchor the entire mass table up to m/z ≥ 209 at an accuracy of < 0.5 dalton. Using this material it has been possible to calibrate coarsely the mass table of a Cameca ims 6f instrument in less than five minutes, thereby greatly simplifying the switch from low mass range to high mass range measurements. Although not suitable for the quantification of geological materials, the ease of synthesis and its utility for rapidly performing what is an otherwise time consuming process makes this material a useful tool for SIMS instruments which offer a multiple mass range capability. 相似文献