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本文对在南海中部布设的两个层次(1191m和3696m)沉积物捕集器的沉降粒子进行了颗粒沉降通量和氨基酸组成的研究。南海的物质通量呈现季节性变化,深层样变动范围在69.6~141.7mg/(m2·d);但火山灰侵入后,其物质通量(按每月平均)高出1~2个数量级,氨基酸和氨基糖含量亦由原来的10×10-3和0.9×10-3减少为0.09×10-3和0.02×10-3。氨基酸组分中以天门冬氨酸占优势,其次为甘氨酸与谷氨酸。在火山灰影响下,其丰度顺序为:谷氨酸>天门冬氨酸>甘氨酸。 相似文献
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对红虾虾头和虾肉中的脂肪进行了提取和测定。脂肪甲酯化后,采用50m×0.35mmi.d.PEG-20M玻璃毛细管柱,FID检测器,并结合GCLMS进行了脂肪酸分析。结果表明,虾头中脂肪含量达10.8×10-2,其不饱和脂肪酸68.8×10-2,EPA+DHA占24.1×10-2;虾肉中脂肪仅为3.9×10-2,其不饱和脂肪酸69.8×10-2,EPA+DHA为27.3×10-2。 相似文献
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测定了南海东北部沉积物间隙水中NO3-N,NO2-N和SiO3-Si的含量。6个站位的5─10cm层的NO3-N,NO2-N和SiO3-Si的含量分别为0.47—1.70,0.84—2.60和10.17—11.69μmol/L。研究了上述物质含量在50号站的深度分布。估算了NO2-N和SiO3-Si从间隙水向上覆水扩散的通量分别为0.033和0.019mmol/m2·d。 相似文献
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南海东北部沉积物间隙水氮和硅的研究 总被引:9,自引:0,他引:9
测定了南海东北部沉积物间隙水中NO3-N,NO2-N和SiO3-Si的含量。6个站位的5-10cm层的NO3-N,NO2-N和SiO3-Si的含量分别为0.47-1.70,0.84-2.60和10.17-11.69μmol/L。研究了上术物质含量在50号站的深度分布。估算了NO3-N和SiO3-Si从间隙水向覆水扩散的通量分别为通量分别为0.033和0.019m mol/m^2.d。 相似文献
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杭州湾锋区浮游植物现存量和初级生产力 总被引:6,自引:0,他引:6
1987年12月和1988年7月,对杭州湾锋区附近海域的浮游植物细胞丰度、优势种类、叶绿素a浓度和初级生产力进行了现场测定。结果表明,夏季海域浮游植物细胞丰度(19.95×106个/m3)高于冬季(5.60×106个/m3)。主要为广温低盐河口性类群和近岸广温广盐性类群占优势。夏季表层平均叶绿素a浓度为2.74mg/m3,冬季为1.27mg/m3。其平面分布特征表现为,表层浓度高于中层和底层,小潮汛的浓度高于大潮汛,落潮时的浓度高于涨潮时,跟踪测站的浓度高于E断面。夏季平均初级生产力为150.27mgC/(m2·d)。杭州湾为高悬浮物浓度的海域,光强成为初级生产力的主要限制因素之一。 相似文献
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九龙江口本中1995年有机物的转移 总被引:1,自引:0,他引:1
1995年3个航次调查研究结果表明,九龙江口水体总有机物的含量受悬浮物含量控制。在S〈5的低盐度区,悬浮泥沙和有机物产生明显的絮凝;在S〉5的广阔海域,它们的行移接近于理想混合。估算得出九龙江河流的入海一约;悬浮泥沙为9.8*10^5t/a;总COD为3.2*10^t/a,其中溶解态COD为2.1*10^4t/a约占2/3,为水体有机物的主要开矿如换算为溶解有机碳,则DOC的平均通量为3.2*10 相似文献
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厦门西海域表层沉的重金属的分布特征及来源探讨 总被引:18,自引:1,他引:18
1994年10月调查研究了厦门西海域表层沉积物样品中Cu、Pb,Zn,Cd在不同粒度颗粒中不同结合态的含量。结果表明,该海域圾层沉积物中Cu,Pb,Zn,Cd在弱结合态中有一较稳定的分配比;Cu,Pb,Zn,Cd的平均浓度分别为30.2,77.2,144.2,0.7mg/kg;概据底质评价标准,Zn,Pb严重超标。 相似文献
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Arne Schnack-Friedrichsen Angela M. Davis Jim D. Bennell Dei G. Huws 《Marine Georesources & Geotechnology》2001,19(4):221-243
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
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Shigehisa Nakamura 《Marine Geodesy》2000,23(1):55-61
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
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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
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《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
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The relationship between the flux of exotic benthic foraminiferal tests (i.e. tests which are supplied from open-sea sources alone) in a tidal inlet and that of bulk sediment was analysed, which can be expressed as two first-order linear equations. According to this relationship, in order to determine net sediment transport directions in the entrance, the test concentration in surficial sediments of the tidal basin can be compared against a ‘ critical level ’. The critical level is determined for the conditions that no net transport of bulk sediment is present within the entrance. If the observed concentration (averaged over the tidal basin) is higher than the simulated critical level, then the net sediment transport is directed to landward. This method is applied to the analysis of net sand transport at Christchurch Harbour, a tidal inlet system located in southern England. In this investigation, concentrations of exotic foraminiferal tests in the surficial sediments of the tidal basin and ebb tidal delta area were obtained from the analysis of sea-bed sediment samples. A series of probable critical levels were calculated based upon the data sets with regard to: (1) sediment discharge from the rivers; (2) magnitude of sediment discharge within the entrance during the ebb; (3) the test concentration outside the harbour; (4) the thickness of the moving layer; and (5) two parameters associated with dispersive processes. The results show that the concentration in the tidal basin sediment is higher than a number of simulated critical concentrations for representative cases. Consequently, the high level of the concentration of exotic benthic foraminiferal tests within the harbour should be explained as a result of landward net transport of sands within the entrance. 相似文献
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The behaviour of an axially pre-loaded cylindrical member of an offshore structure, hit by a supply ship, has been investigated. The effects of axial pre-loading on the dynamic properties of members, the extent of damage and propagation of dynamic instability in the tubular members have also been investigated. Numerical models have been validated using available experimental data from the literature although these are mostly static with no pre-loading. Axial pre-loading was found to change the dynamic characteristics of some cylindrical members quite dramatically while it had no significant effect on others. The study examined whether there was any change in the behaviour between local and global modes when the loading was dynamic rather than static. The effect of damping on the dynamic instability of axially pre-loaded tubes under lateral dynamic loads was also studied. It was observed that for some geometries the quasi-static response can be used to define the boundary between bounded and unbounded dynamic responses. The main contribution of this study, compared with previous investigations reported in the literature, is that both pre-loading and dynamic effects have been included. 相似文献
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Rahul Sharma 《Marine Georesources & Geotechnology》2000,18(3):237-250
Observations on seafloor features from subbottom profiling and seabed photography data show that the undisturbed and natural conditions before the benthic disturbance undergo a substantial change after operation of the disturber. The effects can be seen in the form of deep trenches and grooves, formed by the action of the sleds and the pumping of the sediment along its path, as well as sediment piles on either side of the track. Biological traces such as fecal coils, casts, tubes, burrows, and trails get obliterated in the areas of disturbance and resedimentation. The smooth, uniform nature of the seafloor observed in predisturbance phase shows microtopographic changes in and around the disturbed area as a result of sediment excavation and resettlement. Vertical mixing as well as lateral transport of sediment alter the geological, biological, physical, and chemical conditions on the seafloor, which need to be monitored over time to assess the process and the time taken for restoration of environmental conditions. 相似文献
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Vance P. Vicente 《Marine Ecology》1989,10(2):179-191
Abstract. Long-term changes in the distributional patterns of commercial sponges ( Spongia spp. and Hippospongia spp.) within the West Indian Region indicates that: 1) commercial sponges had a widespread distribution throughout the whole West Indian Region and were ubiquitous in very shallow water until about the first half of the present century; 2) they were fished commercially not only in the traditional northern Caribbean sites (Florida, Gulf of Mexico, Bahamas) but also in the Greater ( e. g. , Hispaniola, Jamaica) and Lesser Antilles; and 3) they became extinct throughout most of the Lesser Antilles ( e. g. , Puerto Rico, Vieques, St. Thomas) sometime during the first half of this century. Mortalities of spongiids within the Antilles were found to differ from other marine mortalities in that: 1) species disappeared from a large region; 2) species vanished from different habitats and depths; and 3) natural populations never recovered. Species richness patterns suggest that commercial sponge genera ( Spongia and Hippospongia ) evolved under slightly cooler elimatic conditions than those found at present, and that these extinctions occurred as a direct or indirect effect of positive thermal anomalies in sea surface and atmospheric temperatures between 1900–1950. The concept that species diversity is stable on a regional scale is questioned. 相似文献