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1.
通过单因子实验,研究了短角异剑水蚤(Apocyclops royi)在不同温度、光照、pH 值、饵料密度以及单性条件下对盐生杜氏藻的滤水率(F)和滤食率(G),及其对3种常见饵料微藻(盐生杜氏藻、球等边金藻和海水小球藻)摄食的选择性,旨在为该物种的人工高效可控培养提供实验和技术基础.结果表明,实验温度范围内(20,25和30℃),短角异剑水蚤对盐生杜氏藻的滤水率和滤食率差异不显著,其中25℃时 F和 G 较高,分别为(0.049±0.014)mL/(个?h)和(1.393±0.369)×104个/(个?h);滤水率和滤食率随光照强度的增加而升高,光照强度为9800 lx 时 F 和 G 最高,分别为(0.053±0.012)mL/(个?h)和(1.295±0.303)×104个/(个?h); pH 值为9.0时,滤水率和滤食率显著高于其他实验组(7.0、8.0、10.0);滤水率随饵料密度的增加呈现先增加后降低的趋势,滤食率随饵料密度的增大而升高;滤水率和滤食率存在性别差异,雌性的 F 和 G 均比雄性约高16%.实验的3种微藻中,球等鞭金藻的选择性指数最高. 相似文献
2.
饵料密度、温度和体质量对大西洋浪蛤滤水率的影响 总被引：6，自引：0，他引：6
2004年4月～7月采用实验生态学方法对浙江引种养殖的大西洋浪蛤（Spisula solidissima）繁殖培育的一龄蛤进行滤水率的研究。结果表明：（1）以新月菱形藻为饵料，在适宜的饵料密度范围内大西洋浪蛤的滤水率随着饵料密度的增加而增大，它们之间呈函数关系；（2）体质量对滤水率的影响呈幂函数关系y=0．1622W^0.848（R^2=0．9988）；（3）在一定温度范围内，随温度升高滤水率增加；超过一定温度范围，随温度升高滤水率下降。当温度为21℃时滤水率达到最大值0．77L／h。 相似文献
3.
采用饵料浓度差减法,在实验条件下研究了不同细胞密度的中肋骨条藻和东海原甲藻对海月水母水螅体、碟状体和水母体摄食活动的影响。结果表明,不同种类和密度的微藻细胞密度对水螅体、碟状体和水母体的摄食有显著影响。在实验的藻细胞密度范围内,随藻细胞密度的增加,水螅体和碟状体对中肋骨条藻和东海原甲藻的摄食率一直升高。水螅体对中肋骨条藻和东海原甲藻的最大摄食率均发生在藻细胞密度最高处,分别为4623cells/(ind.h)和4118cells/(ind.h)。碟状体对中肋骨条藻和东海原甲藻的最大摄食率也是发生在藻细胞密度最高处,分别为174671cells/(ind.h)和47218cells/(ind.h)。清滤率随着藻细胞密度增加而降低。在相似细胞密度下,碟状体对中肋骨条藻的摄食率高于东海原甲藻。水螅体和碟状体对同种藻的摄食情况不同,在相似藻细胞密度下,碟状体的摄食率比水螅体高。经过藻类饵料适应处理的水螅体对藻类的摄食率会有显著增加,约为未经饵料适应处理的10倍。水母体对中肋骨条藻和东海原甲藻未发生摄食。 相似文献
4.
盐度对长江口3种滤食性贝类滤水率、摄食率、同化率的影响 总被引：4，自引：2，他引：2
采用实验生态学方法研究了盐度对长江口缢蛏(Sinonovacula constricta)、河蚬(Corbicula fluminea)和光滑河蓝蛤(Potamocorbula laevis)滤水率、摄食率、同化率的影响。缢蛏组设6个盐度梯度(5,10,15,20,25,30),光滑河蓝蛤组设6个盐度梯度(5,10,15,20,25,30),河蚬组设6个盐度梯度(0,5,10,15,20,25),并测定了此3种滤食性贝类的生物学参数。结果显示,3种滤食性贝类的滤水率、摄食率和同化率随着盐度的上升而增加,当上升到一定盐度时达到峰值,然后随着盐度的升高而降低。盐度20时,缢蛏滤水率、摄食率和同化率达到峰值,分别为0.57L/h、5.38mg POM/h和0.72%。盐度10时,光滑河蓝蛤滤水率和同化率达到峰值,分别为0.46L/h和0.53%,摄食率在盐度15时达到峰值3.80mg POM/h。盐度5时河蚬滤水率和摄食率都达到峰值,分别为0.39 L/h和2.48 mg POM/h,同化率在盐度0时已达到峰值0.51%,并随盐度上升而下降。上述结果表明,盐度对3种滤食性贝类的3个摄食生理指标均有显著影响。 相似文献
5.
在封闭循环水高密度养殖条件下(平均密度14.1 kg/m2±0.51 kg/m2), 设置4 个流速梯度(200, 400,600, 800 L/h,分别以A～D 组表示), 挑选相近体质量(200.3g±7.6 g)的大菱鲆进行42 d 养殖试验, 每个梯度设置3 个重复, 每个重复55 尾鱼, 研究流速对封闭循环水养殖大菱鲆生长、摄食以及水质氮素的影响。试验结果表明: (1) 大菱鲆(Scophthatmus maximus L)特定生长率、增质量率、摄食量随流速增大先快速上升后缓升趋稳, 饲料系数则相反。B、C、D 3 组特定生长率、摄食量分别显著高于A 组30.77%～52.31%、17.30%～22.05%; 饲料系数则显著低于A 组13.83%～22.34%; (2) 养殖水体中总氨氮、非离子氨及亚硝酸氮浓度随流速的增大先快速下降后缓降趋稳。B、C、D 3 组水质总氨氮氨浓度均显著低于A 组53.70%～79.07%; (3) 根据流速对特定生长率、水体总氨氮二者的影响, 得出养殖的生态适宜流速为625 L/h。再结合流速对水循环动力的影响, 得出养殖的生态经济适宜流速为480 L/h。 相似文献
6.
UV-B辐射增强对壶状臂尾轮虫摄食的影响 总被引：4，自引：0，他引：4
研究了UV-B辐射条件下壶状臂尾轮虫(Brachionusurceus)对6株海洋微藻:小球藻(Chlorellasp.)、绿色巴夫藻(Pavlovauiridis)、扁藻(Tetraselmischuii)、球等鞭金藻8701(IsochrysisgalbanaPark8701)、牟氏角毛藻(Chaetocerosmuelleri)和小新月菱形藻(Nitzschiaclostertum)的室内摄食实验。结果表明,UV-B辐射增强对壶状臂尾轮虫的摄食有显著的抑制作用。与对照组相比,壶状臂尾轮虫对给定饵料单胞藻的滤水率和摄食率都随UV-B辐射剂量的增大而显著减小(P<0.05)。而且壶状臂尾轮虫对每一种饵料单胞藻的滤水率和摄食率是不相同的,这说明壶状臂尾轮虫对饵料单胞藻是有选择性的。 相似文献
7.
本文以硬壳蛤(Mercenariamercenaria)为研究对象,开展了两种类型改性粘土(聚合氯化铝改性粘土MCⅠ,硫酸铝改性粘土MCⅡ)对其急性、亚急性毒性实验。96h急性毒性实验结果显示,MCⅠ和MCⅡ对小规格硬壳蛤[壳长(1.98±0.05)mm,壳高(1.75±0.04)mm]的半致死浓度(LC_(50))分别为4.91和1.85g/L,对大规格硬壳蛤[壳长(5.70±0.15)mm,壳高(5.09±0.13)mm]的LC_(50)分别为5.77和3.40g/L。亚急性毒性实验结果表明:浓度低于1.0g/L的MCⅠ和MCⅡ未对两种规格硬壳蛤的存活产生影响;硬壳蛤滤水率随改性粘土用量增加而降低,其中0.1g/L的MCⅠ和MCⅡ对两种规格硬壳蛤滤水率无影响, 0.5g/L的MCⅡ对两种规格硬壳蛤滤水率均有显著影响(P0.05),而MCⅠ仅对小规格硬壳蛤滤水率有影响;当改性粘土浓度升高至1.0g/L,两种规格硬壳蛤的滤水率均显著低于对照(P0.05)。生长率的结果显示,仅1.0g/L的MCⅠ和MCⅡ显著影响小规格硬壳蛤生长。多年的应用结果表明,现场能有效消除有害赤潮藻华的改性粘土用量为4—10t/km~2,低于本实验中对硬壳蛤产生影响的改性粘土浓度。另外,我国近海实际养殖过程中投放的硬壳蛤通常为1cm左右,大于本研究中的硬壳蛤规格。据此可以推断,改性粘土在现场治理藻华的同时不会对其存活和生长产生不良影响。本研究结果将为改性粘土在近海养殖水域的应用提供科学依据。 相似文献
8.
几种环境因子对墨氏胸刺水蚤摄食的影响 总被引：6，自引：0，他引：6
研究了不同藻类、藻细胞密度、温度、盐度、容器容积、昼夜变化等环境因子对浮游桡足类墨氏胸刺水蚤(Centropagesmcmurrichi)的摄食关系。结果表明:1)藻种类、藻细胞密度对墨氏胸刺水蚤的清滤率和滤食率都有显著影响;2)墨氏胸刺水蚤对4种藻的摄食顺序为球等鞭金藻(摄食率I=12.418μgC/ind穐)>角毛藻(I=9.824μgC/ind穐)>异胶藻(I=6.683μgC/ind穐)>小球藻(I=5.229μgC/ind穐);3)温度在6~20℃范围内变化对墨氏胸刺水蚤的清滤率和滤食率无显著影响,但以10~15℃为佳。盐度对墨氏胸刺水蚤的清滤率和滤食率有显著影响,最适摄食盐度为20~27;4)容器容积和昼夜变化对墨氏胸刺水蚤的摄食影响不显著。 相似文献
9.
盐度、pH对波纹巴非蛤(Paphia undulate)滤水率的影响 总被引：6，自引：0，他引：6
在实验室条件下,用流水系统分别测定了盐度和pH对波纹巴非蛤(Paphia undulata)滤水率的影响.对盐度梯度分别为24,28,32,36和pH值分别为7.0,7.5,8.0,8.5,9.0 梯度下波纹巴非蛤的滤水率进行了测定.结果表明:盐度和pH对波纹巴非蛤的滤水率有显著影响.在盐度24～32范围内滤水率随着盐度的升高而增大,在盐度32～36范围内随着盐度的升高而减小,盐度28和32时滤水率明显高于其它盐度组.在pH值7.0～9.0范围内,波纹巴非蛤的滤水率变化迅速,呈现一个峰值变化,pH值为8时达到最大值. 相似文献
10.
水温、盐度和饵料密度对橄榄蚶滤水率的影响 总被引：1，自引：0，他引：1
用实验生态学的方法研究了不同水温(15、20、25、30℃)、盐度(16、21、26、31、36)和饵料密度(0.5×104、1.5×104、2.5×104、3.5×104、5×104个/m L)对橄榄蚶(Estellarca olivacea)滤水率的影响。实验结果表明,以金藻作为饵料,水温、盐度、饵料密度对橄榄蚶的滤水率有显著影响(P0.05)。水温15~30℃、盐度16~36、饵料密度为0.5~5×104个/m L时,橄榄蚶的滤水率都呈峰值变化。水温25℃、盐度26、饵料密度3.5×104个/m L时,其滤水率分别达到最大值。在所研究的范围内,水温、盐度、饵料密度与滤水率之间分别满足函数关系:FRT=–0.3396T2+1.8937T+0.2728(R2=0.9857,P0.05);FRS=–0.3424S2+1.9626S+0.7112(R2=0.9683,P0.05);FRC=1.7395 C 0.4607,(R2=0.9062,P0.05)。 相似文献
11.
Chandralata Raghukumar G. Sheelu P. A. Loka Bharathi Shanta Nair C. Mohandass 《Marine Georesources & Geotechnology》2001,19(1):1-16
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.
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
13.
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. 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.
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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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
18.
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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20.
Phylogenetic diversity and phenotypic characterization of cultivable bacterioplankton isolated from polar oceans 总被引：1，自引：0，他引：1
A set of 27 marine planktonic bacteria isolated from the polar regions was characterized by 16S rDNA sequencing and physiological and biochemical testing. More than half of these bacteria were positive for caseinase, gelatinase and 13-glucosidase, and could utilize glucose, maltose or malic acid as carbon source for cell growth. Twelve isolates expressed nitrate reduction activities. Except for one antarctic isolate BSwlO175 belonging to Actinobacteria phylum, these isolates were classified as γ-Proteobacteria, suggesting that γ-Proteobacteria dominated in cultivable marine bacterioplankton at both poles. Genus Pseudoalteromonas was the predominant group in the Chukchi Sea and the Bering Sea, and genus ShewaneUa dominated in cultivable bacterioplankton in the Prydz Bay. With sequence similarities above 97%, genus Psychrobacter was found at both poles. These 27 isolates were psychrotolerant, and significant 16S rDNA sequence similarities were found not only between arctic and antarctic marine bacteria （ 〉 99% ）, but also between polar marine bacteria and bacteria from other aquatic environments （ ≥ 98.8% ）, including temperate ocean, deep sea, pond and lake, suggesting that in the polar oceans less temperature-sensitive bacteria may be cosmopolitan and have a bipolar, even global, distribution at the species level. 相似文献