共查询到20条相似文献，搜索用时 62 毫秒
1.
漠斑牙鲆早期发育阶段的摄食与生长特性 总被引：1，自引：0，他引：1
2006年12月至2007年2月,在漳州市东山县华涛水产综合养殖场,采用生态学方法对人工培育的漠斑牙鲆仔、稚、幼鱼的摄食习性与生长特性进行了分析.结果表明,在水温为18.1～23℃时,仔鱼在孵出第6天开口摄食,开口饵料为褶皱臂尾轮虫(Bruchionus plicatilis),以后随着鱼体的生长,开始投喂卤虫无节幼体.对288尾仔、稚、幼鱼观察结果表明,其摄食率达83.0%,消化道饱满系数波动在0.9%～6.6%之间,日摄食指数在6.8%～29.6%;摄食具有明显的昼夜节律,一昼夜中仔鱼出现两个摄食高峰,分别出现在12:00和翌日08:00,稚鱼摄食高峰出现在10:00～14:00,幼鱼摄食高峰出现在12:00,但12:00～20:00均保持较高的摄食水平.仔、稚鱼夜间基本不摄食,幼鱼夜间有少量摄食.摄食量(y)与体重(W)的关系式为y=0.030 7W 0.050 5,全长(LT)与日龄(D)的关系式为LT=2.666 1e0.043 3D,体重(W)与日龄(D)的关系式为W=0.065e0.169 3D,全长(LT)与体重(W)的回归方程为W=0.001 8LT3.689 4. 相似文献
2.
鮸状黄姑鱼早期发育阶段的摄食与生长特性 总被引：9，自引：0，他引：9
1997年4－5月,在集美大学水产学院海水育苗试验场,采用生态学方法对人工培育的状黄姑鱼仔、稚、幼鱼的援食和生长特性进行分析。结果表明,在人工培育条件下,仔、稚、幼鱼的摄食率达97.9％,摄食量占体重的1．4％－23．4％,日摄食量占体重的36．47％－6519％;摄食具明显的昼夜节律,黄昏和早晨为摄食高峰;对较大个体的饵料生物有明显的选择性;饵料密度对摄食量有一定影响。摄食量与体重的关系式为y=0.1327x＋0．5613,全长与日龄的关系式为LT=2.5799eg.g516D,体重与日龄的回归方程为W=0．0537e‘.1786D,全长与体重的回归方程为W＝0．0042L。 相似文献
3.
《应用海洋学学报》2015,(3)
于2013年5~7月对人工培育的云纹石斑鱼(Epinephelus moara)仔、稚鱼的摄食习性与生长特性进行了研究.在水温为(26.7±1.3)℃的培育条件下,云纹石斑鱼仔、稚鱼摄食能力强;仔鱼4日龄开口,摄食率为40.00%;仔、稚鱼平均摄食率为97.63%,且13日龄之后的平均饱食个体比例为92.25%,摄食量(y)与体重(W)的关系可用二项式方程y=0.000 1W2+0.055 9W-0.629 8表达;云纹石斑鱼仔鱼、稚鱼在白天均出现两个摄食高峰,夜间基本不摄食,为白天摄食类型,并可以初步确定以鱼体重的10%~20%和8%~10%分别作为云纹石斑鱼仔鱼和稚鱼的日投喂量.全长(Lt)与日龄(D)的回归方程为Lt=0.008 8D2+0.162 2D+1.114 5,体重(Wt)与日龄(D)的回归方程为Wt=0.366 0D2-11.361D+59.022 3,全长(Lt)与体重(Wt)的回归方程为Wt=0.011 7Lt3.017 8,b=3.017 8约等于3,表明云纹石斑鱼仔、稚鱼为均匀生长类型. 相似文献
4.
2002年5~6月,在集美大学水产学院水产试验场,采用生态学方法对人工培育的双棘黄姑鱼(Nibeadiacanthus(Lacpde))仔、稚、幼鱼的摄食习性与生长特性进行分析。结果表明,在人工培育条件下,双刺黄姑鱼仔、稚、幼鱼的摄食率达93.1%,摄食量占体质量的4.09%~21.07%,日摄食量占体质量的23.67%~57.24%;摄食具明显的昼夜节律,黄昏为摄食高峰。摄食量与体质量的关系式为y=0.1267x0.7878,全长与日龄的关系式为L=1.8603e0.0723D,体质量与日龄的回归方程为M=0.0203e0.2484D。全长与体质量的回归方程为M=0.0024L3.4633。 相似文献
5.
花鲈仔、稚、幼鱼摄食习性与生长的研究 总被引：39，自引：3，他引：36
分析了花鲈仔、稚、幼鱼的摄食习性与生长.结果表明,在水温为15.5～16.5℃时,花妒仔鱼孵出约140h左右开口摄食,开口饵料为小型臂尾轮虫.全长10mm左右的仔鱼可摄食卤虫幼体,全长11mm左右的个体可摄食枝角类.对431尾仔、稚、幼鱼观察结果,在实验条件下其摄食率高达99.1%,胃饱满系数波动于2.38%～16.48%之间,日摄食指数在45%～60%.其摄食强度具明显的昼夜节律,以16:00～20:00胃饱满度最高.仔、稚鱼夜间基本不摄食,部分幼鱼个体少量摄食.仔、稚、幼鱼个体间生长速度具有一定的差异性.其体重与摄食量的关系符合直线方程y=0.1018+8.3261×10-2x;全长与体重的相关关系可用ω=1.6473×10-3L3.4743表示,全长与日龄的关系式为Lt=5.5242e1.9681×10-2D;体重与日龄的回归方程为ω=0.5836e6.9208×10-2D. 相似文献
6.
斜带石斑鱼仔、稚鱼的摄食与生长特性 总被引：1，自引：0，他引：1
据2005年10～12月，在集美大学水产学院海水育苗试验场的试验数据，采用生态学方法对人工培育的斜带石斑鱼仔、稚鱼的摄食习性与生长特性进行了分析．结果表明，在水温为26．5～28．5℃时，仔鱼在孵出第4天开口摄食，开口饵料为牡蛎受精卵和担轮幼虫．以后随着鱼体的生长，依次投喂臂尾轮虫、卤虫无节幼体、桡足类、鱼糜．对422尾仔、稚鱼观察结果表明，其摄食率达95．1％，消化道饱满系数波动在0．96％～34．15％之间，日摄食指数在45．83％～82．08％之间，其摄食具有明显的昼夜节律，仔鱼摄食高峰出现在11：00和15：00，稚鱼摄食高峰出现在13：00和17：00，仔、稚鱼夜间基本不摄食．对较大个体的饵料生物有明显的选择性．摄食量（Y）与体重（形）的关系式为Y=0．017W＋0．198，全长（LT）与日龄（D）的关系式为Lr=2．229e^0.038D，体重（形）与日龄（D）的关系式为形=0．063e^0.130D，全长（LT）与体重（形）的回归方程为W=0．0047LT^3.319． 相似文献
7.
研究了花尾胡椒鲷幼鱼的最大摄食量与温度和体重的关系。花尾胡椒鲷幼鱼的最大摄食量与体重呈正相关 ,二者的关系为 :Cmax=1 5 95 .3W0 .6 87(Cmax:最大摄食量 ,J/d ;W :体重 ,g)。最大摄食量随温度的变化情况为 :在实验温度为 2 2～ 2 8℃范围内 ,二者呈正相关 ,超过 2 8℃之后呈负相关。最大摄食率与体重的相关关系为 :Rmax=1 5 0 7.6W-0 .313[(Rmax:最大摄食率 ,J/(d·g) ]。采用回归分析 ,建立了由温度和体重预测该种鱼的最大摄食量和最大摄食率的模型 :Cmax=2 86 790e-0 .90 4ln(T3-77.738T2 1985 .185T -16 42 9.710 ) W0 .6 16 n =1 6 ,r =0 .994Rmax=0 .887e1.2 6 4ln(-T3 78.0 6 1T2 -2 0 0 3.397T 172 36 .5 2 0 ) W-0 .2 83 n =1 6 ,r=0 .978 相似文献
8.
9.
人工养殖条件下达氏鳇杂交种幼鱼生长特性的初步研究 总被引：6，自引：0，他引：6
为了解在人工养殖条件下达氏鳇(Huso dauricus)杂交种(达氏鳇♂×天然杂交种♀(达氏鳇♀×史氏鲟♂) )的生长特性,在水温11～22 ℃时,对达氏鳇杂交种体长和体重的生长进行实验研究.应用计算机软件Excel和SPSS对测量的数据进行处理分析,结果表明:平均全长为33.32 cm、平均体重为145.83 g的139日龄幼鱼经75 d的人工饲养长成平均全长为48.79 cm、平均体重为437.36 g的个体,全长与日龄之间呈线性关系L=3.292 7t 30.517,R2=0.959 4,其全长日均增长量为2.06 mm、平均瞬时增长率为 0.076 3,体重与日龄呈指数函数关系,Wgc=119.74e0.234 6t,R2=0.956;体重日均增长量为3.887 1 g、平均瞬时生长率为0.219 7;体重与全长的回归曲线为WwL=0.005 6L2.892 9,R2=0.998 2,幂指数接近于3,表明该鱼体重与全长的立方呈正相关系,属于等比生长类型. 相似文献
10.
实验室条件下测定花鲈 ( L ateolabrax japonicus C & V)的代谢率 ,温度为 ( 2 5.2± 0 .5)℃ ,鱼体湿重范围 :4 .64～ 52 .2 8g(平均体重 17.81g± 0 .33g)。饥饿鱼的正常代谢相关于体重的关系式 :Rr=15.37W0 .74 4。( r=0 .934 )。摄食代谢与摄食量呈线性正相关关系 ,摄食代谢水平为正常代谢的 1.8～ 2 .4倍。 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
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
17.
18.
《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
19.
20.
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