排序方式: 共有162条查询结果,搜索用时 15 毫秒
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瓯江下游河段污染物质滞留时间数值模拟研究 总被引:1,自引:1,他引:0
利用平面二维数学模型对瓯江下游守恒性污染物质滞留时间的空间变化及其对于径流、潮差、初始排放时刻的响应进行了研究.研究将瓯江梅岙至口门河段分为8个子区域分别进行数值试验.数学模型上、下游边界分别采用径流量和潮位控制.上游径流量选取5个代表性流量,下游选取大、中、小潮及混合潮型进行组合研究滞留时间的基本变化规律.研究认为,... 相似文献
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Mohammad Rezwanul Islam Syeda Fahliza Begum Yasushi Yamaguchi Katsuro Ogawa 《Journal of Marine Systems》2002,32(4):73
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. 相似文献
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采用"有无对比"方法,分析长江口深水航道从水深7 m整治到12.5 m所带来的直接经济效益。利用进出长江口深水航道的船舶数据、长江口及沿江港口吞吐量等基础数据,分3个整治阶段,按集装箱船、散货船、油船分别测算深水航道整治所带来的直接经济效益。提出长江口深水航道整治工程实施对于加快上海国际航运中心建设、带动沿江地区经济的快速增长和产业结构的优化调整均起到重要作用。 相似文献
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针对兆河入湖口门附近存在拦门沙碍航问题,采用实测资料分析和三维水沙数模计算相结合的研究方法,研究风生浪流动力作用下湖区泥沙输运特征,探讨口门航道整治方案布置。研究结果表明,巢湖底沙粒径较小,大风天风浪在近岸浅水区发生变形破碎,使水体含沙量增大,在风生湖流作用下,近岸泥沙表现为"波浪掀沙、湖流输沙"的运动特征。结合以往航道治理实践经验,提出整治与疏浚相结合的思路,多方案比选计算结果表明,筑堤方案可明显减小航槽淤积量,其中双侧筑堤方案整治效果更优。综合比选推荐采用双侧筑堤高坝缓坡方案。研究成果可为类似湖区口门航道整治提供借鉴。 相似文献
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汉江河口段属典型的"两堤一江"河段,河道微弯,河槽单一。根据《湖北省内河航运发展规划(修编)》,本河段将在十三五期间将航道等级提升到Ⅱ级。根据河道地形资料,从河道平面、深泓纵剖面、深槽变化等方面着手,对该河段的河床演变规律、影响因素及碍航特性进行研究,并针对碍航浅区段提出相应的治理思路,为该河段的航道治理提供依据。 相似文献
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阐述珠江口有代表性的土层结构和特征,确定了珠江口地区的标志性土层,参考区域性的研究资料对土层的时代成因进行探讨。根据黏性土固结程度的研究和结论,对珠江口重要黏性土层的固结程度进行了分析和探讨。 相似文献
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合理开发北港航道可缓解目前长江口主航道在南港段面临的巨大通航压力、畅通长江黄金水道、拓宽上海港在长江口的岸线利用范围。通过分析北港航道的开发条件,对北港航道的可开发规模及开发时序作出探讨。分析认为:现阶段可通过规范北港通航,利用自然水深建设5 000吨级航道,部分缓解南港的通航压力;近期可开辟8 m航道,通航2万吨级及以下船舶;中远期则需全面整治北港,开辟10 m航道,满足3万吨级船舶的通航需求。 相似文献