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1.
空间数据引擎是实现空间数据高效访问和管理的关键技术之一.结合海洋地理信息系统应用需求,针对海洋底质数据特点,构建了海洋底质空间数据库引擎,介绍了其数据模型和数据访问结构,并通过工程实践实现了系统功能,为海洋底质空间数据组织和管理提供一个有效的解决方案,同时为海洋地理信息系统提供了强有力数据支持.  相似文献   

2.
2011年是十二五规划的开局之年,也是我国在新的历史起点上实现海洋事业发展新跨越的大干之年。2011年全国海洋厅局长暨党风廉政建设工作会议廓清了十二五海洋工作总体思路,明确了2011年的海洋工作任务。我们要根据会议精神,结合厦门海洋管理实际,不断开拓创新,全力抓好落实,为实现海洋事业发展新跨越而不懈努力。  相似文献   

3.
通过对海洋智能装备分类、国产化海洋智能装备发展现状和经典案例应用的描述,揭示了以技术创新为手段实现海洋智能装备国产化的必要性和紧迫性,并提出发展国产化海洋智能装备的一些思考和建议,为建立起我国自主知识产权的综合性、系统性、国产化的海洋智能装备研发和产业化体系,从而实现海洋智能装备国产化的目标提供了参考。  相似文献   

4.
海洋经济增长与海洋可持续发展统筹问题   总被引:1,自引:1,他引:0       下载免费PDF全文
结合海洋管理工作实践,分析海洋经济发展过程中海洋资源、环境和生态受损原因,探讨海洋经济增长与海洋可持续发展的统筹问题.统筹海洋产业布局,调整海洋产业结构,转变海洋经济发展方式是实现海洋可持续发展的根本出路:完善海洋经济发展政策法规与规划,建立海洋经济运行监测评估体系,创新海洋经济管理体制机制,是实现海洋可持续发展的重要保证.  相似文献   

5.
为促进我国海洋生态资源开发与保护的良性循环,保障海洋生态产品的可持续供给,文章基于海洋生态产品的定义和特征,分析海洋生态产品价值实现的演化逻辑,结合典型模式探索海洋生态产品价值实现路径,并针对我国海洋生态产品价值实现的现实困境提出机制设计。研究结果表明:海洋生态产品是海洋生态系统为满足人民日益增长的优美海洋生态环境需要...  相似文献   

6.
目前,许多大型的档案馆、资料室已经实现了计算机管理,但在海洋地质系统,很多单位还在沿用传统的手工管理模式,新形势下急需实现海洋地质档案资料的计算机管理。海洋地质资料室通常规模不大,档案资料专业性强,分类相对简单,这就使其在实现计算机管理时有着独特的优越性。结合工作实践,对海洋地质档案资料实现计算机管理的认识和可行性步骤进行探讨。  相似文献   

7.
对浙江发展海洋循环经济的思考   总被引:1,自引:1,他引:0       下载免费PDF全文
海洋经济的快速发展已成为浙江经济的新亮点.伴随着海洋经济的快速增长,海洋生态环境也面临危机.发展海洋循环经济是实现海洋经济可持续发展的有效路径,文章分析了目前浙江发展海洋循环经济面临的障碍,并对发展浙江海洋循环经济提出建议.  相似文献   

8.
融合海洋地质专题信息与海洋基础数据、遥感数据等,采用B/S架构实现基于Skyline的海洋地质Web三维GIS系统的组织、发布和应用技术,为海洋地质三维地理信息系统的实现奠定了基础,并从三维场景建模、B/S架构Web可视化和系统功能设计等方面详细地介绍了Skyline软件在海洋地质GIS中的集成应用。  相似文献   

9.
海洋生态产品价值实现对推进海洋生态文明建设与海洋经济高质量发展具有重要意义。目前,海洋生态产品价值实现存在市场化程度不高、公众参与度低、实现不充分等问题。本文通过构建海洋生态产品价值实现参与主体(企业、政府和社会公众)的演化博弈模型,探究各方主体的策略稳定性规律,探讨三方博弈系统的均衡点及其稳定性,并运用Matlab仿真分析不同参数变化对系统演化的影响,最后依据博弈分析结果为探索“政府+市场”的海洋生态产品价值实现路径提供对策建议。结果表明,政府是海洋生态产品价值实现的引导者与推动者,管控成本和社会收益是影响其策略选择的主要因素,加强政府的奖惩力度、增加企业提供海洋生态产品的潜在收益、降低供给成本对企业参与海洋生态产品价值实现具有正向作用,社会公众购买海洋生态产品所获效用的提升与监督成本的减少有利于促进社会公众参与海洋生态产品价值实现。  相似文献   

10.
海洋环境以及资源的共享性决定了海洋公共管理的主体必须要扩展到整个公民社会。涉海公民不再是海洋政策的旁观者和被动接受者,而在海洋管理中承担着重要角色。目前,我国海洋公共管理中的公民参与还存在一定的现实困境,直接制约着其海洋管理功能的发挥和参与价值的实现。通过法律制度、协调机制、信息技术以及海洋文化的建设促使公民积极参与到海洋管理过程中,实现人海和谐及公共利益的维护。  相似文献   

11.
In order to assess the impact of deep-sea mining on the in situ benthic life, we measured the microbial standing stock and concentration of organic nutrients in the deep-sea sediments of the Central Indian Ocean Basin in the Indian pioneer area. Sediments were collected using box core and grab samples during September 1996. The total bacterial numbers ranged from 10 10 -10 11 cells per g -1 dry weight sediment. There was a marginal decrease in the number of bacteria from surface to 30 cm depth, though the subsurface section registered a higher number than did the surface. The highest numbers were encountered at depths of 4-8 cm. The retrievable number of bacteria were two orders less in comparison with the direct total counts of bacteria. An almost homogeneous distribution of bacteria, total organic carbon, living biomass, and lipids throughout the depth of cores indicates active microbial and benthic processes in the deep sea sediments. On the other hand, a uniform distribution of total counts of bacteria, carbohydrates, and total organic carbon in all the cores indicates their stable nature and suggests that they can serve as useful parameters for long-term monitoring of the area after the benthic disturbance. Further studies on temporal variability in this region would not only verify the observed norms of distribution of these variables but would also help to understand restabilization processes after the simulated benthic disturbance.  相似文献   

12.
The interdependence between the seismo-acoustic properties of a marine sediment and its geotechnical/physical parameters has been known for many years, and it has been postulated that this should allow the extraction of geotechnical information from seismic data. Though in the literature many correlations have been published for the surficial layer, there is a lack of information for greater sediment depths. In this article, a desktop study on a synthetic seafloor model illustrates how the application of published near-surface prediction equations to subsurface sediments (up to several tens of meters burial depth) can lead to spurious predictions. To test this further, acoustic and geotechnical properties were measured on a number of sediment core samples, some of which were subjected to loading in acoustically-equipped consolidation cells (oedometers) to simulate greater burial depth conditions. For low effective pressures (representing small burial depths extending to around 10 meters subsurface), the general applicability of established relationships was confirmed: the prediction of porosity, bulk density, and mean grain size from acoustic velocity and impedance appears generally possible for the investigated sedimentary environments. As effective pressure increases through, the observed relationships deviate more and more from the established ones for the near-surface area. For the samples tested in this study, in some instances increasing pressure even resulted in decreasing velocities. There are several possible explanations for this abnormal behavior, including the presence of gas, overconsolidation, or bimodal grain size distribution. The results indicate that an appropriate depth correction must be introduced into the published prediction equations in order to obtain reliable estimates of physical sediment properties for greater subsurface depths.  相似文献   

13.
An acoustic inversion method using a wide-band signal and two near field receivers is proposed and applied to multiple layered seabed models including a manganese sediment. The inversion problem can be formulated into a probabilistic model comprised of signals, a forward model, and additive noise. The forward model simulates wide-band signals, such as chirp signals, and is chosen to be the source-waveletconvolution plane wave modeling method. The wavelet matching technique, using weighted least-squares fitting, estimates the sediment sound-speed and thickness on which determination of the possible numerical ranges for a priori uniform distribution is based. The genetic algorithm is applied to a global optimization problem to find a maximum a posteriori solution for determined a priori search space. Here the object function is defined by an L 2 norm of the difference between measured and modeled signals. Not only the marginal pdf but also its statistics are calculated by numerical evaluation of integrals using the samples selected during importance sampling process of the genetic algorithm.  相似文献   

14.
海上大直径钢管桩打桩过程中,桩周土体受到强烈扰动而发生强度弱化,掌握桩周土体强度弱化规律对于准确预测打桩过程、保证工程安全具有重要意义。为研究土体强度弱化规律,开展了环剪试验模拟打桩对桩周土体的扰动,测试土体强度随剪切速率的变化规律,建立了描述土体强度弱化规律的拟合公式,引入到打桩分析软件中。研究结果表明:土体的强度折减程度不仅与土体本身的性质有关还受到土体的埋深和剪切速率的影响,埋深越深土体强度折减程度越低,剪切速率越高土体强度折减越高,在打桩分析中可采用这里推荐的线性折减方法来模拟不同深度处土体强度的折减规律。  相似文献   

15.
Specific properties of the interannual sea level variations and annual tides in the Northwestern Pacific were studied. Several tide stations were monitored. The monthly mean sea level for the year of 1995 was analyzed at each tide station. A seismic event in 1995, some tectonic activity around the subject area, and the Kuroshio (the oceanic western boundary current) may possibly contaminate results which would have occurred from the astronomical annual tide alone.  相似文献   

16.
The effect of different fixation and storage protocols on the flow cytometric (FCM) simultaneous analysis of bacterioplankton and phytoplankton in coastal seawater samples (Mediterranean coastal lagoons) was investigated. FCM measurements (cell number, fluorescence and scatter characteristics) were obtained through DAPI staining. Three fixatives [glutaraldehyde (GA), formaldehyde (FA) and paraformaldehyde (PFA)] and two storage (3 months duration) methods (5 °C and −196 °C) were tested. Two dominant populations were detected in studied samples: bacteria and eukaryotic picophytoplankton. Adding fixatives (2% final concentration) appears necessary to obtain FCM exhaustive counts of all the bacteria and phytoplanktonic cells. This was related to the permeation effect of fixatives which allowed a better DAPI staining of the cells. Maximum fluorescence, i.e. optimal staining of the cells was obtained with FA or PFA, and significant lower fluorescences with GA. Fixed samples stored at 5 °C induced rapid cell loss. Only storage in liquid nitrogen of samples fixed with FA or PFA, allows mid-term (≥4 months) preservation of bacteria or picophytoplankton cell numbers, and limited evolution of DAPI-induced fluorescence and scatter characteristics.  相似文献   

17.
18.
《海洋学报(英文版)》2014,(9):F0003-F0003
<正>Acta Oceanologica Sinica(AOS)is a comprehensive academic journal edited by the Editorial Committee of Acta Oceanologica Sinica and is designed to provide a forum for important research papers of the marine scientific community which reflect the information on a worldwide basis.The journal publishes scholarly papers on marine science and technology,including physics,chemistry,biology,  相似文献   

19.
20.
Oedometer tests have been carried out on 70 undisturbed surficial clays (at approximately 250 mm below the mudline), mostly collected by free-fall corers from sites widely scattered throughout the deep-sea North Atlantic. Acoustic measurements were also made, initially on contiguous samples and ultimately on the same sample using a geophysically instrumented oedometer which also collected electrical resistivity data. Apart from those quiescent areas below the carbonate compensation depth, such as north of the West Indies where very fine clays exist, most of the samples are silty clays whose geotechnical-geophysical properties are dependent on the type of clay minerals present (and their ability to take in moisture), the sand-size fraction, and the quantity of carbonate present. Thus the pure clays have high compressibilities which decrease on the addition of coarse particles, while the converse is true for the acoustic parameters, these increasing with the sand fraction. Using the notion of the intrinsic compression line for all samples, and comparison to it of the measured compression curves, it is clear that, contrary to some previously held ideas, most deep-sea clays are normally consolidated; the addition of carbonate has the effect of creating an open, stronger sediment skeleton. Interestingly, where information is available, the variation with depth of a sample's acoustic velocity follows the void ratio pressure relationship of the compression curve. This allows the construction of an in-situ sediment compression curve using the in-situ geophysical observations.  相似文献   

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