斜带髭鲷室外人工生态系育苗试验

本文系斜带髭鲷鱼苗室外水泥池不同生态系的育苗试验．在育苗前的“养水”期 间,1号池接入小球藻、微绿球藻、扁藻、金藻、轮虫、桡足类、枝角类等生物饵料;2号 池仅接入小球藻、轮虫生物饵料．在水温19．1～23℃、比重1．019、pH值8．5的条件 下．2池鱼苗经100d的培育后,平均全长各为31mm和29mm,平均体重各为0．90g 和0．75g,成活率18．5％和10．1％．试验表明:在育苗前期,生物饵料的多样性有利于 开口仔鱼的摄食和营养,也利于鱼苗的生长发育和成活率的提高．     

卵形鲳鯵人工育苗技术的研究

在卵形鲳鯵人工育苗技术的研究中，进行了不同饵料对仔鱼生长及成活率影响的试验，培育出体长3～5cm鱼苗23万尾．平均成活率为57．5％。结果表明用螺旋藻强化培育轮虫和采用二次培育方法进行卵形鲳鯵人工育苗．可提高鱼苗的成活率。     

利用单胞藻培养池进行真鲷育苗技术

１９９３年，于文登市小观海珍品育苗养殖场，在海湾扇贝和对虾育苗结束后，利用其配套的单胞藻培养地进行真鲷育苗，利用对虾育苗池和卤虫孵化池培养轮虫。在不增加任何设备的前提下，育成全长３．０１～６．５０ｃｍ，平均全长３．４４ｃｍ的真鲷商品鱼种１６１１１６尾，从仔鱼培育到商品苗种的成活率达到２４．７２％，平均单位水体出苗量达到２６８５尾，１９９３年７月１９日通过了文登市科委组织的验收。正材料和方法１．１育苗设施亲鱼产卵池（１个）和鱼苗培育池（６个）皆用单胞藻培养池（规格为３．８ｍ×３．７ｍ×０．８ｍ，水…     

南麂海区美国红鱼网箱养殖试验

1996年 1 0月底从青岛引进平均体长为 2 .1 cm、体重为 0 .5 g的美国红鱼苗 75 0 0尾在南麂海区进行网箱养殖试验 ,养至 1 997年 1 2月 2 5日止 ,其平均体长为 3 2 .8cm,尾均重达6 92 .8g,鱼苗期成活率为 5 5 .7% ,养成期成活率达 98.4% ,饵料系数为 7.2 2～ 9.5 9。此外 ,还对该鱼的放养时间、苗种培育、鱼病防治、人工增殖以及网箱抗风浪措施等问题进行了初步探讨     

红鳍笛鲷池塘人工育苗技术初步研究

本文报道了在海水池搪进行红鳍笛鲷人工育苗的实验结果．实验水温为26～32℃，盐度为25～31，经过33～35d的培育，3口池塘鱼的苗平均全长分别为35．3、32．3、28．5mm，成活率分别为16．7％、18．1％、7．8％．本文还对仔鱼的放养密度、生长状况、饵料系列以及池塘中主要生物饵料密度变化作了较为详细的阐述。     

花尾胡椒鲷的大规模生产性早繁育苗

2003年2月28日至4月15日于湛江东海岛进行了花尾胡椒鲷(Plectorhinchuscinctus)大规模生产性人工早繁育苗的研究。研究选取网箱养殖的成熟健壮亲鱼,强化培养一段时间后,采用LRH-A2,HCG进行人工催产,自然受精后放在30m3的育苗池中培养15d,再转移到室外高位池中培养。育苗获得平均体长40mm的鱼苗33.3万尾,育苗成活率为12.8%。     

双斑东方Tun人工繁殖及育苗技术

本文报道了福建省水产研究所2001年双斑东方Tun人工繁殖及育苗过程与结果。在春季当海水水温达到16℃以上时，用DOM、LRH－A3或HCG进行催产，混和或单一使用，剂量视亲鱼性腺成熟度而定。受精卵在水温18．0－22．4℃、盐度22．2－28．6条件下，经117－156h孵化。用250万尾开口仔鱼培育出平均全长为37mm，平均体重为1．3g的鱼苗52．35万尾，成活率25．5％。此外，对亲鱼的暂养、催产、受精卵的孵化、仔鱼的前期培育和后期培育等关键环节进行了探讨。     

酸碱度、盐度对方斑东风螺卵囊孵化率和不同饵料对幼虫生长发育、存活的影响

分别用pH6．32～9．76和盐度16．7～40．9共8个梯度的海水进行方斑东风螺(Babyloniaare Lamarck)卵囊的孵化试验。结果表明,卵囊孵化最适pH范围在8．23～9．35之间,孵化率均在80％以上,pH8．81时高达93．7％;卵囊孵化适宜盐度范围为30．3～37．0,盐度40．9时仍有67．0％的孵化率,表现出耐高盐的特性,盐度低于27．6,孵化率明显下降。幼虫在15d的培育过程中,通过投喂不同的饵料,结果显示投喂单胞藻比投喂人工配合饵料、酵母效果好,单独投喂扁藻(Platymonas subcondiformis (Wille)Hazen)幼虫生长发育最快,体长增长倍数达1．90倍;投喂扁藻、小球藻(Chdorella spp．)、扁藻 金藻(Isochrysis galbana Palbana)、扁藻 小球藻幼虫的成活率相差不明显,分别为58．5％、54．3％、63．3％和50．3％,而投喂人工配合饵料虾片、螺旋藻粉幼虫成活率则较低,只有3．6％和12．8％,投喂酵母第9天全部死亡。     

小刀蛏室内人工育苗技术研究

本文研究了小刀蛏(Cultellus attenuatus)室内人工育苗技术。在繁殖季节选择壳长7.5 cm亲贝,采用铺泥沙蓄养培育,以阴干+维生素浸泡刺激法获得精、卵,幼虫培育中人工控制幼虫密度,D形幼虫到壳顶幼虫前期为5～6个/mL,壳顶幼虫后期为1～2个/mL。进行了不同运输方式和不同底质亲贝蓄养比较试验、不同底质附着基采苗方法试验以及稚贝无底质上升流培育和不同盐度培育试验。研究表明,采用铺细沙加冰的运输方法亲贝成活率最高,干露9 h成活率可达90%;以纯海泥底质蓄养的亲贝肥满度和成活率最高;无底质采苗和铺泥采苗对幼虫变态率的影响没有差异;无底质采苗的稚贝,其生长速度明显慢于铺泥采苗;小刀蛏稚贝不宜用上升流进行培育,宜采用铺泥培育的方法;盐度为15时,稚贝培养效果最好,生长速度快、成活率高,盐度为35时培养效果最差。采用上述技术,成功培育出3 mm以上的商品苗2 000万粒,育苗效果显著。     

贻贝幼体在对虾育苗中的应用

应用卤虫幼体育苗成本相对较高,占育苗成本费用４０％［１］。而用蛋糕、蛋黄等代用饵料营养不足,且对水质污染较重。寻找合适的代用饵料,已成为降低育苗成本的一条可行途径。作者于１９９７年应用贻贝幼体进行对虾育苗试验,取得良好的经济效益,现将情况报告如下。１　材料与方法１．１试验条件试验点设在岚山对虾育苗场,育苗水体１０００ｍ~３,均为室内水泥池。培育池为长方形,每池４０ｍ~３,共用４个。卤虫培育他２个,贻贝幼体培育池２个。育苗池采用小型室内对虾孵化池。孵化池为２ｍ×２ｍ×４ｍ,有效水体为１５ｍ３,共用５…     

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.     

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.     

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.     

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.     

Flow Cytometric Analysis of Coastal Lagoon Bacterioplankton and Picophytoplankton: Fixation and Storage Effects

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.