基于Bibexcel和Pajek的海洋生态环境保护领域科学计量与知识图谱分析

利用文献处理工具Bibexcel和网络分析工具Pajek对SCIE和SSCI文献数据库1990—2020年全球海洋生态环境保护文献数据进行统计与可视化分析,以期揭示该领域的科研产出情况、领域知识基础、研究热点分布及前瞻发展态势。研究结果表明：海洋生态环境保护领域文献产出近30年来持续增长;美国、澳大利亚、加拿大、法国等国家在该领域内有着较强的科研竞争力和学术影响力,其中美国处于研究合作核心地位,美国加利福尼亚大学、法国国家科研中心等机构为主要发文机构;海洋生态环境保护研究的热点方向主要为海洋生态环境修复与管控、气候变化、生态系统服务、海洋保护区等;该领域研究学科交融趋势明显,研究者应充分借鉴、吸收其他学科理念和方法,加强海洋生态环境与气候变化、人为活动及生态物种等因素的制衡与协同。     

冷泉系统研究国际发展态势分析

以Web of Science信息平台的SCIE数据库为数据源,利用文献计量方法,分析国际冷泉系统研究的年度变化、期刊分布、主要研究国家、机构的影响力及合作情况以及国际研究热点领域。研究结果发现:国际冷泉系统研究论文产量一直呈增长趋势;美国论文产出数量最多、合作中心性最强。德国亥姆霍兹国家研究中心联合会发文最多。中国近三年发文比例和第一国家发文比例均排名第一,其中发文最多的机构为中国科学院。微生物甲烷厌氧氧化、冷泉区生物多样性以及冷泉碳酸盐岩的矿物学和地球化学是研究热点。     

2015年第5期整期打包下载

统计了1982-2014年国家海洋局被美国Web of Science核心合集数据库收录的4466 篇SCI科技论文, 通过分析SCI论文产出数量和被引次数, 了解国家海洋局与全球科研机构合作情况、热点学科分布和国际学术影响力状况。结果显示:国家海洋局的科研合作伙伴遍布全球大约60个国家和地区, 1560所大学和研究机构;在基础研究领域和应用研究领域都取得了许多国内外较高水平的成果;其优势学科向国际前沿延伸的态势较为明显, 影响和辐射作用越来越大。这说明以国家海洋局为代表的我国海洋科学学术国际影响力呈现增长的态势。     

从SCI科技论文分析国家海洋局科技成果的国际影响力

统计了1982-2014年国家海洋局被美国Web of Science核心合集数据库收录的4 466篇SCI科技论文,通过分析SCI论文产出数量和被引次数,了解国家海洋局与全球科研机构合作情况、热点学科分布和国际学术影响力状况。结果显示:国家海洋局的科研合作伙伴遍布全球大约60个国家和地区,1 560所大学和研究机构;在基础研究领域和应用研究领域都取得了许多国内外较高水平的成果;其优势学科向国际前沿延伸的态势较为明显,影响和辐射作用越来越大。这说明以国家海洋局为代表的我国海洋科学学术国际影响力呈现增长的态势。     

基于文献计量的中美红树林与气候变化耦合关系研究现状与热点对比分析

红树林与气候变化耦合关系研究既是气候变化领域的研究热点,同时也是红树林领域的研究热点。本研究采用文献计量分析方法对中美红树林与气候变化耦合关系的研究现状和热点进行对比分析,探讨两国在该领域研究特征的异同。研究结果表明：(1)美国作为文献发表数量最高的国家,同样具有最强的学术影响力;中国拥有世界排名第三的发文数量,但在学术影响力方面与美国存在一定的差距。中美两国在该领域的发文量均呈现持续增长的趋势。(2)中美在该领域保持着较强的合作关系,且各自形成了较为广泛的国际合作网络。(3)中美两国的科学家均对气候变化背景下红树林生态系统的脆弱性以及红树林作为基于自然的解决方案在应对气候变化方面起到的作用等问题表现出浓厚的兴趣。但是,由于起步较晚,中国在红树林与气候变化领域相关研究的广度和深度较美国还存在一定的差距,需要进一步扩大国际合作,加强科研产出,提升学术影响力。本研究的相关成果将为我国红树林与气候变化领域的科研工作开展、政策制定及管理实践等提供信息参考。     

深海多金属硫化物采矿研究进展及其前景探讨

随着陆地金属矿产资源的日渐枯竭,深海多金属硫化物逐渐成为海洋矿产资源勘探的新趋势。文章介绍了全球主要海底多金属硫化物矿床的成因及分布特点,阐述了多个国际矿业公司和国际海洋组织对西南太平洋、大西洋和印度洋海底块状多金属硫化物勘探活动的最新进展。从海底多金属硫化物的金属品质、深海采矿的法律政策和环境保护等方面对海底多金属硫化物的开发前景进行探讨,并提出积极投身国际海底资源开发规章制定,进一步细化国内法律制度,为深海采矿提供良好的法律制度环境;提升深海治理能力,增强我国在深海领域的话语权;完善深海技术装备体系,提高深海开发创新能力等建议。     

国际海底矿产资源勘查与研究进展

随着调查和研究的深入,世界各国对国际海底区域分布的多金属结核、富钴结壳、多金属硫化物和深海稀土几种深海固体矿产资源的关注程度日益增高,越来越多的国家为占有国际海底资源,加快了资源调查和评价的步伐,国际海底区域矿产资源的竞争形势愈加紧迫。通过调研的方式收集了大量资料,对国际海底区域多金属结核、富钴结壳、多金属硫化物和深海稀土几种深海矿产资源的分布和勘察现状进行评述,从而对国际海底矿产资源的研究趋势有所了解和把握。     

关于中国国际海底区域矿区采矿的思考

文章结合国际深海采矿的现状和中国现有国际海底区域矿区的情况,分析中国国际海底区域矿区采矿存在缺少法律依据、尚未完成矿区资源评价和"区域"放弃、深海采矿技术发展相对滞后、海洋环境影响评估尚有不足等问题;在此基础上提出未来发展建议,即开展与国际海底管理局的深度合作,在制定"区域"内矿产资源开发规章中有所作为;加快对中国国际海底区域的勘探工作,尽快完成矿区资源评价和"区域"放弃;跟踪国际深海采矿行业进展,加快推进中国深海采矿系统的建造并尽快试开采;继续加大深海采矿对海洋环境的影响研究,尽快形成深海采矿环境影响预测评价技术指南。     

21世纪全球海洋经济研究热点及前沿 ——基于Citespace和Web of science数据库的分析

21世纪是海洋的世纪。为探究进入21世纪后全球在海洋经济方面的研究演进路径和未来可能的研究热点,文章选取Web of Science核心数据库中主题为“Marine Economy”或“Marine Economics”的1 444篇期刊论文,利用Citespace软件分别进行科学合作网络分析、关键词共现分析和文献共被引分析。结果发现：进入21世纪以来,全球对海洋经济研究的关注度普遍提升。①美国、中国和英国构成了海洋经济领域研究的核心力量,但欧美国家之间机构合作较为密切,我国海洋研究机构国内外合作仍需加强,国际影响力仍需进一步提升;②现有海洋经济研究除聚焦渔业管理、海洋经济增长以及相关影响因素问题,还注重生态系统服务、环境保护等可持续性发展的问题;③近年来海洋经济研究相关热点开始转向小规模渔业管理、海洋生态环境保护、海洋产业空间布局和海洋休闲渔业,尤其是小规模渔业管理和海洋生态环境保护,是未来海洋经济研究需要重点关注的方向。     

国际海洋药物研究动态与发展趋势

文章用文献计量与科学知识图谱方法呈现海洋药物研究态势与热点,旨在为海洋药物研究提供参考。本文以SCIE(Science Citation Index Expanded)为数据源,以1980～2017年海洋药物领域论文为研究对象,采用文献计量与知识图谱可视化分析方法,结合Excel、VOSviewer软件,对论文年代分布、研究机构、期刊、作者、高被引论文及研究热点进行分析。结果表明,海洋药物研究的热点方向为海洋天然产物、抗菌活性、细胞毒性、海绵等,应重点关注海洋天然产物及其抗菌药理作用的研究。世界范围内关于海洋药物研究的论文数量呈逐年上升趋势,美国在该领域研究占据绝对优势,其发文量、总被引和H指数均占绝对地位。该领域主要发文期刊为《Marine Drugs》、《Journalof Natural Products》。发文机构中中国科学院位列世界第一,但整体论文质量欠佳,中国在该领域研究水平有待加强,论文影响力仍需提高。     

Microbial Biomass and Organic Nutrients in the Deep-Sea Sediments of the Central Indian Ocean Basin

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.     

A Review of Some Environmental Issues Affecting Marine Mining

This article reviews information recently available from existing marine and coastal mining for responses to environmental issues affecting marine mining at different depths. It is particularly but not exclusively concerned with those issues affecting seabed biodiversity impact and recovery. Much information has been gathered in the past 10 years from shallow mining operations for construction aggregate, diamonds, and gold, from coastal mines discharging tailings to shallow and deep water, and from experimental deep mining tests. The responses to issues identified are summarized in a series of eight tables intended to facilitate site-specific consideration. Since impacts can spread widely in the surface mixing layer SML, and can affect the biologically productive euphotic zone, the main issues considered arise from the depth of mining relative to the SML of the sea. Where mining is below the SML, the issue is whether it is environmentally better to bring the extraction products to the surface vessel for processing (and waste discharge), or to process the extraction products as much as possible on the seabed. Responses to the issues need to be sitespecific, and dependent on adequate preoperational environmental impact and recovery prediction. For deep tailings disposal from a surface vessel, there are four important environmental unknowns: (1) the possible growth of "marine snow" (bacterial flocs) utilizing the enormous quantities of fine tailings particles (hundreds or thousands of metric tons per day) as nuclei for growth, (2) the possibility that local keystone plankton and nekton species may migrate diurnally down to and beyond the depth of deep discharge and hence be subjected to tailings impact at depth, (3) the burrow-up capability of deep benthos and their ability to survive high rates of tailings deposition, and (4) the pattern and rate of dispersion of a tailings density current through the deep water column from discharge point to seabed. Actions to obtain relevant information in general and site-specifically are suggested.     

Increased Particle Fluxes at the INDEX Site Attributable to Simulated Benthic Disturbance

Particle fluxes were measured 7 m above the sea bottom during the predisturbance, disturbance, and postdisturbance periods by using time series sediment traps attached to seven deep-sea moorings deployed in the INDEX experiment site in the Central Indian Basin. The predisturbance particle fluxes varied between 22.3 to 55.1 mg m -2 day -1 . Increased and variable particle fluxes were recorded by the sediment traps during the disturbance period. The increase observed was 0.5 to 4 times more than the background predisturbance fluxes. The increases in particle fluxes (~4 times) recorded by the sediment trap located in the southwestern direction (DMS-1) were the greatest, which could be the result of preferential movement of resuspended particles generated during the deep-sea benthic disturbance along the general current direction prevailing in this area during the experimental period. Also, the traps located closer to the disturbance area recorded greater fluxes than did the traps far away, across the Deep Sea Sediment Resuspension System path. This variability in recorded particle fluxes by the traps around the disturbance area clearly indicates that physical characteristics such as grain size and density of the resuspended particles produced during the disturbance had an important effect on particle movement. The postdisturbance measurements during ~5 days showed a reduction in particle fluxes of ~50%, indicating rapid particle settlement.     

Assessing the Validity of Seismo-Acoustic Predictor Equations for Obtaining Seabed and Sub-Surface Sediment Physical Properties

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.     

Geoacoustic Inversion via Genetic Algorithm and Its Application to Manganese Sediment Identification

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.     

海上大直径钢管桩打桩过程中桩周土强度弱化研究

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。     

Determination of In Situ Sediment Shear Strength from Advanced Piston Corer Pullout Forces

The advanced piston corer (APC) has been used by the Ocean Drilling Program since 1985 for recovering soft sediments from the ocean floor. The pullout force measured on extracting the core barrel from the sediment is shown to correlate with the average shear strength of the sediment core measured in the ship's laboratory. A simple rule of thumb is derived relating the shear strength of the sediment to the pullout force. Multiple APC holes at individual sites allow the consistency of the pullout measurements to be assessed. The effects of different operational procedures during APC coring are also explored. Although generally applicable, the correlation between pullout force and laboratory measurements of shear strength breaks down for some APC holes, possibly because of the disturbance of some sediment types during the APC coring process. A better understanding of the physical process of APC coring, and its effect on the properties of the sediment both inside and immediately outside the core barrel, would indicate what confidence can be put on the measurement of pullout force as a way of evaluating the in situ shear strength of deep sea sediments.     

Interannual Sea Level Variations and Annual Tides in the Northwestern Pacific

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.     

《Acta Oceanologica Sinica》Vol. 33(2014) contents

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