层次分析法在宁波港锚地选择中的应用

随着宁波港的快速发展,港口与锚地发展的矛盾日显突出,锚地规划及功能的划分也极不合理。本文通过AHP方法进行分析,得出锚地选择的合理性方案。     

CDMA在视频监视系统中的应用

简单介绍码分多址(CDMA)的基本原理及性能;然后利用CDMA传输技术,设计一个无线视频图像传输系统。最后,介绍该系统的结构、基本原理以及在试验视频监视系统中的应用。     

基于实时视景仿真技术的海上航标监管系统

海上航标系统是海上交通安全保障体系的重要组成部分。结合上海海事局厦门航标处的航标日常管理与实时监控的实际业务需求,开展了利用实时视景仿真技术与电子海图相结合构建海上航标监管系统的应用研究和系统实现等工作。该系统的实现,有利于航标设置方案的审定与选择,有利于监控者对现场环境的把握和应急决策。     

地铁屏蔽门系统构成分析

文章较详细地介绍了广州地铁使用的屏蔽门系统,重点是它的机械和电气部分的组成和作用.     

用高温超导线圈和常导线圈构成的混合式电磁悬浮系统

常导电磁吸力悬浮系统悬浮气隙小、悬浮功率大,电动斥力悬浮系统不能实现静止悬浮、磁场污染大。由于受电流变化率限制,单独采用高温超导线圈构成的电磁吸力悬浮系统不能实现稳定悬浮。经分析比较,提出了一种用高温超导线圈和常导线圈构成的混合式电磁吸力型悬浮系统方案。采用这种混合式悬浮方案可增大悬浮气隙、实现稳态"零"功率悬浮、减轻车体重量、降低制冷费用、且无磁场污染。     

船舶压载水不同处理方法的经济性分析

对船舶压载水不同处理方法所需费用和代价进行了简要评述。     

电力Modem在冷藏箱监控报警系统中的应用

文章从系统硬件、软件、通讯三方面介绍美国YORK公司开发的大型集装箱船舶冷藏集装箱集中监控系统REFCON,可供同行借鉴。     

成昆线红层地区泥石流沟侵蚀程度量化分析

以成昆铁路红层地区的3个小流域为研究区,计算3个年份的地面割裂度及其年平均变化率,分析用地面割裂度表征泥石流沟侵蚀程度的不足及其原因。基于泥石流沟发育的物理模型,以原来的地面割裂度定义为基础,引入表述沟谷分布零散程度的异型度因子,导出新侵蚀系数公式。以3个小流域固体物质的年平均流失量作为侵蚀程度强弱的标准,采用非参数统计推断方法,将侵蚀系数、地面割裂度的年变化值和固体物质的年平均流失量作秩统计和次序统计。对秩统计参数和次序统计参数比较结果表明:在表征泥石流沟侵蚀程度方面,侵蚀系数优于地面割裂度。     

国外核测井技术的发展状况

本文通过对近十年来国外核测井技术的状况和发展趋势的追踪,简要地介绍了几种我所有研发可能的测井仪器,以期能够为我所核测井仪器的研发提供一些参考。     

Distribution of suspended sediment in the coastal sea off the Ganges–Brahmaputra River mouth: observation from TM data

Remote sensing technique was applied to estimate suspended sediment concentration (SSC) and to understand transportation, distribution and deposition of suspended sediment in the estuary and throughout the coastal sea, off the Ganges–Brahmaputra River mouth. During low river discharge period, zone of turbidity maximum is inferred in the estuary near the shore. SSC map shows that maximum SSC reaches 1050 mg/l in this period. Magnitude of SSC is mainly owing to resuspension of the bottom surface sediments induced by tidal currents flowing over shallow water depths. The influence of depth on resuspension is farther revealed from the distribution and magnitude of SSC along the head of Swatch of No Ground (SNG) submarine canyon. During high river discharge period, huge river outflow pushed the salt wedge and flashes away the suspended sediments in the coastal sea off the river mouth. Zone of turbidity maximum is inferred in the coastal water approximately within 5–10 m depth of water, where the maximum SSC reaches 1700 mg/l. In this period, huge fluvial input of the suspended sediments including the resuspended bottom sediments and the particles remaining in suspension for longer period of time since their initial entry control mainly the magnitude of SSC. In the estuary near the shore, seasonal variation in the magnitude of SSC is not evident. In the coastal sea (>5 m water depth), seasonal influence in the magnitude of SSC could be concluded from the discrepancy between SSC values of two different seasons. Transportation and deposition of suspended sediments also experiences seasonal variations. At present, suspended sediments are being accumulated on the shallow shelf (between 5 and 10 m water depth) in low discharge period and on the mid-shelf (between 10 and 75 m water depth) during high discharge period. An empirical (exponential) relationship was found between gradual settle down of suspended sediments in the coastal sea and its lateral distance from the turbidity maximum.