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1.
九龙江河口区磷的转移和入海通量   总被引:1,自引:3,他引:1  
1992~1993年4个航次的调查研究结果表明,九龙江河口区总磷的分布和转移受悬浮物含量明显控制。当SPM含量低时,其迁移过程接近理想行为;SPM含量高时则为非理想行为。估算得出,九龙江水体总磷的平均人海通量为1.47×103t/a。其中,溶解态磷为0.43×103t/a,约占29%;颗粒态磷占71%,九龙江水磷的输入以颗粒态为主。溶解态磷的分布,基本上在某一水平上了波动,其入海通量受环境影响很小,可能意味着颗粒磷的缓冲作用。  相似文献   

2.
九龙江口水体中1995年磷的转移   总被引:1,自引:0,他引:1  
1995年3个航次的调查研究结果表明,九龙江口水体总磷含量受悬浮物含量控制,在S<5的低盐度区,悬浮泥沙和磷产生明显的絮凝沉降,在S>5时,它们的迁移接近于理想混合。溶解磷的河口转移与其在河流端的浓度密切相关。当河端浓度低时,磷略呈溶出现象;而河端浓度高时则接近于理想混合过程。估算得出九龙江河流总磷的平均入海通量为2.9×103t/a,其中溶解磷和颗粒磷各占一半左右。  相似文献   

3.
九龙江口磷的界面分配和转移   总被引:5,自引:0,他引:5  
陈松  廖文卓 《台湾海峡》1997,16(3):293-298
1992年8月航次调查结果表明,九龙江口水体中磷的迁移呈保守行为,TP和PP含量随着海水盐度的降低呈增加趋势,DP含量刚好相反;S〈15的低盐区,盐度对磷迁移的影响比较显著。  相似文献   

4.
对海南岛南岸古珊瑚后报海温研究的几点看法   总被引:1,自引:0,他引:1  
海南岛南是研究古珊瑚后报古海温的理想场所之一。根据近海现今海温与珊瑚生长率季节变化的特点,指出开展古珊瑚地化指标后报海面温度(SST)研究时,应尽可能采用先进取样技术进行小样品取样,应开展珊瑚生长模式研究,注意SST变化中数年平均值与气候平均值的差值范围,建议重视近数在年冬季SST后报工作。  相似文献   

5.
河口及近岸海区营养盐含量较丰富,是海洋生物繁殖的良好环境,因此调查研究这些区域水体中的营养盐有重要的现实意义。AsTon指出,近年来河口区磷酸盐、硅酸盐、硝酸盐及其它无机形式氮行为的研究已引起了许多研究人员的注意。一方面是由于这些物质对生物过程包括对控制生产力的过程具有重要作用;另一方面是由于对排入河口富营养污水(例如生活污水等)影响的关注。 关于河口及近岸区营养盐含量变化及行为的研究情况曾进行了大量的研究工作。当河水与海水混合时,河流带入营养盐的行为,如活性磷酸盐、活性硅酸盐及硝酸盐是否有转移,保守性如何,是近年来较为关心的问题之一,也是一个十分复杂的过程。且影响  相似文献   

6.
本研究采用学习记忆行为训练和生化测定的方法,观察了我国4种常见海蛇的乙醇浸出物(AlcoholicExtractsofBodiesofSea Snake.AEBSS)对小鼠的正常学习记忆、东莨菪碱(Scopolamine,Scop)所致记忆障碍、脑不同部位蛋白质含量的影响。结果表明,AEBSS(剂量500mg浸出蛋白/kg体重以上)对正常小鼠的学习记忆能力及脑内蛋白质合成有明显的促进作用;AEBSS还能极显著地改善Scop所致的学习记忆障碍,使Scop组大脑皮层和小脑的蛋白质含量显著增加,海马脑区的蛋白质含量增加极显著。结果提示,AEBSS对小鼠学习记忆的作用机制可能与中枢胆碱能递质系统的蛋白质合成有关。  相似文献   

7.
海蛇乙醇浸出物对小鼠学习记忆的影响   总被引:2,自引:0,他引:2  
本研究采用学习记忆行为训练和生化测定的方法,观察了我国4种常见海蛇的乙醇浸出物(AEBSS)对小鼠的正常学习记忆、东莨菪碱(Scop)所致记忆障碍、脑不同部位蛋白质含量的影响。结果表明,AEBSS(剂量5.00mg浸出蛋白/kg体重以上)对正常小鼠的学习记忆能力及脑内蛋白质合成有明显的促进作用;AEBSS还能极显著地改善Scop所致的学习记忆障碍,使Scop组大脑皮层和小脑的蛋白质含量显著增加,海  相似文献   

8.
125Ma后陆-陆碰撞造成的碳储存的讨论DerrillKerrick等评论:Selverstone和Gutzler(1993)认为,在特提斯陆-陆碰撞期间,碳从大气转移到深成变质储集层可能导致了125Ma后的全球变冷。但是,由于大气CO_2含量长期由...  相似文献   

9.
粉煤灰海上倾倒中几种因素对Se^4+溶出的影响   总被引:1,自引:0,他引:1  
傅云娜  于涛 《海洋通报》1994,13(6):48-52
探讨了粉煤灰中的Se^4+在海水中的溶出现象,找出了几种因素对Se^4+从煤灰中溶出浓度的影响规律。结论是如果粉煤灰中硒的溶出率在10%-20%之间,将粉煤灰投入一个封闭海域,只要固液比达到1:1000,海水中的硒含量就可达到2-3μg/L,即远远超过海水中硒含量的本底值0.03μg/L。PH=7时,盐度越高,温度越高越有利于粉煤灰中Se^4+的溶出,从而使硒在封闭海域溶出值远高于海水硒含量的本底  相似文献   

10.
从长江口1990年6月的一次中肋骨条藻赤潮发生过程中营养盐含量变化可见,由于潮汐的作用,观测水域各营养盐要素都在不同程度上存在周日波动特征,其中,NO3-N在一个潮周期内变化幅度可达1倍以上。赤潮发生时表层水体NO3-N,PO4-P和SiO3-Si值都呈下降趋势,降幅最大的PO4-P达3倍上;N/P值则急剧上升,峰值为450。随着赤潮肖亡,NO3-N,NO2-N和SiO3-Si浓度很快恢复正常,N  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.
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   

14.
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   

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   

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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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