首页 | 本学科首页   官方微博 | 高级检索  
相似文献
 共查询到20条相似文献,搜索用时 46 毫秒
1.
海水养殖罗非鱼补偿生长的生物能量学机制   总被引:16,自引:4,他引:12  
王岩 《海洋与湖沼》2001,32(3):233-239
1998年4月28日—6月24日和5月20日—7月14日分别在汕头大学南澳海洋生物实验站研究了杂交罗非鱼停喂(简称绝食)或限量投喂(简称限食)后的补偿生长,探讨了杂交罗非鱼补偿生长的生物能量学机制。结果表明,海水养殖杂交罗非鱼在饱食状态下的能量收支为100C=32.8G+50.8R+15.3F+1.1U。在恢复生长期间,对照鱼的食物能和代谢能高于绝食鱼或限食鱼,但其单位体重的食物能、代谢能、生长能、粪能和排泄能均明显低于补偿生长的绝食鱼或限食鱼,绝食或限食后海水养殖杂交罗非鱼的能量收支模式未发生明显变化。  相似文献   

2.
温度对草鱼能量收支的影响   总被引:43,自引:0,他引:43  
于1992年4月-1992年5月在22,26及30℃,以莴苣叶为食物,不限量摄食,测定草鱼的能量收支。结果表明,草鱼摄食率及生长率均随温度上升而增加;最大摄食率与水温的关系温度对食物能分配于能量收支各组分的比例没有显著影响,在3个温度测定的平均能量收支式为:100c=29.89F+3.30U+52.48R+14.34G,式中C为食物能,F为排粪能,U为排泄能,R为代谢能,G为生长能。  相似文献   

3.
摄食水平和性别对稀有鮈鲫生长和能量收支的影响   总被引:7,自引:0,他引:7  
于1995年10月采集本所自繁有ju鲫(约1.03g/ind),在30℃水温下进行摄食-生长实验,研究了从饥饿到饱食5个摄食水平对不同性别稀有ju鲫的生长和能量收支的影响,结果表明,鱼体干物和能量含量不受摄食率和性别的影响,随着摄食率的增加,雌鱼的湿重,干重和能量特定生长率均呈双对数增加,雄鱼湿重特定生长率呈双对数增加,而干物质和能量特定生长率呈指增加,雄鱼生长速度及摄食率低于雌鱼,随着摄食率的增加,食物能损失于粪便中的比例均呈上升趋势,损失于排泄物中的比例变化不大,呈下降趋势,用于代谢的比例呈下降趋势,用于生长的比例呈上升趋势,除饥饿组外,在各个摄食水平,雌鱼食物能用于代谢的比例较雄鱼低,而用于生长的比例较雄鱼高。  相似文献   

4.
贝类生物能量学研究进展   总被引:12,自引:0,他引:12  
贝类生物能量学研究源于本世纪60年代,是研究能量在贝类体内转换的一门学科。其中心是研究贝类体内能量收支各组份之间的定量关系以及生态因子对这些关系的影响。贝类的能量收支模型可用如下模型表示[14,21]:其中,C为总摄取食物能,P为生长能,R为代谢耗能,U为排泄能,F为粪便能,单位均为焦耳(J)。目前,贝类能量研究主要集中于两个方面:(1)生态能量学,即种群水平的能量学;(2)生理能量学,即个体水平的能量学,即在实验室条件下以生物个体为对象,探讨生物体的摄食、生长、代谢等各能量组份之间的定量关系和…  相似文献   

5.
关于对虾池混养中的几个问题   总被引:5,自引:0,他引:5  
王岩 《台湾海峡》1999,18(1):106-112
在两年围隔实验的基础上讨论了对虾池混养中存在的几个问题,认为:(1)虾池混养能够提高养殖产量和池塘氮磷的利用率,有助于缓解养殖对环境的污染,但由于养殖种类在池塘氮磷收支所占的比例很小,仅靠混养还不能彻底解决养殖污染问题;(2)罗非鱼与海产贝类的食物灶存在一定的分化。二者对虾池水质的影响具有互补性,因此虾鱼贝混养较虾鱼混养或虾贝混养效果更好。(3)对多个池塘组成的养殖系统的总体优化应是今后虾池生态系统结构优化研究的重要内容。  相似文献   

6.
摄食水平对异育银鲫生长及能量收支的影响   总被引:31,自引:3,他引:28  
于 1 995年 6月在中国科学院水生生物研究所关桥繁殖场采集异育银鲫自繁鱼种(体重为 1 .2 6± 0 .0 5g) ,采用生长实验的方法 ,在 30℃水温下 ,测定其从饥饿到饱食 6个摄食水平下的生长和能量收支。结果表明 ,随着摄食水平的增加 ,鱼体干物质和能量含量、表观消化率呈上升趋势 ;湿重特定生长率随摄食水平的增加呈线性上升 ,干重和能量特定生长率呈对数增加 ;饲料转化效率随摄食水平增加而增加 ,达到最大值后维持不变。排泄能和总代谢耗能占摄入食物能的比例不受摄食水平的影响。最大摄食水平下的能量收支式为 :1 0 0C =1 2 .32F 3.2 1U 63.74R 2 0 .72G ,式中 ,C为食物能 ,F为粪便能 ,U为排泄能 ,R为代谢能 ,G为生长能。  相似文献   

7.
使用2种不同蛋白源配方的饲料投喂卵形鲳Chan。结果表明:投喂豆粕型饲料与投喂鱼粉型饲料在平均尾重,平均日增重、平均饲料系系等生长指标上无显著差异(P>0.05),两者的成活率,鱼获得量则存在显著差异(P<0.05)。说明海水网箱养殖卵形鲳Chan饲料的蛋白来源可利用植物蛋白代替动物蛋白。  相似文献   

8.
低温对条纹锯鮨生长及能量收支的影响   总被引:1,自引:0,他引:1  
在实验室条件下研究条纹锯鮨(Centropristis striata)在9,13,17,21℃条件下的摄食生长和能量收支。结果表明,9℃时鱼体表现为负增长,生长能为-1 124.1 kJ±20.8 kJ,13℃时鱼体生长能为510.3 kJ±8.1 kJ,在实验温度的范围内,随着温度的升高,生长逐渐加快,21℃仍为生长的适宜温度。条纹锯鮨生长的补偿温度在9~13℃之间。生长能和呼吸能的变化主导实验鱼的能量收支模式。温度对鱼体的蛋白质质量分数影响显著(P<0.05),脂肪的质量分数在9℃时最高,13℃时最低,然后随着温度升高而逐渐加大,水分和灰分的质量分数随温度的变化没有呈现出明显的规律。  相似文献   

9.
研究了不同饵料种类(小沙丁鱼肉-NSF,鳗鱼配合饲料-CEFF,海水鱼配合饲料-CMFF)和摄食水平(从饥饿至饱食)对军曹鱼 Rachycentron canadum 幼鱼(平均初始体重约28g)生长和氮收支的影响,并建立了不同饵料种类时的生长-摄食关系和氮排泄-摄食关系.结果表明,投喂3种不同饵料的军曹鱼幼鱼湿重、干重和氮特定生长率均随摄食水平的增加呈显著增长趋势,其中,投喂NSF和CEFF组的特定生长率与摄食水平之间表现为减速增长曲线,投喂CMFF组的表现为直线;饱食时,投喂NSF和CEFF组的特定生长率接近而明显高于投喂CMFF组.投喂NSF和CEFF组的食物转化效率随摄食水平的增加而增长或呈先增长后下降的趋势,在饱食或次饱食(约为饱食量的70%)摄食水平组有最大值,而投喂CMFF组的食物转化效率随摄食水平的增加而持续增长,在饱食摄食水平时有最大值;除食物湿重转化效率外,投喂NSF组的食物转化效率最高,其次为投喂CEFF组,而两者均明显高于投喂CMFF组.3个饵料组的军曹鱼幼鱼摄食氮、排粪氮、生长氮和排泄氮均随摄食水平的增加呈显著增长趋势;投喂NSF和CEFF组的摄食氮、生长氮和排泄氮明显高于投喂CMFF组,而投喂CMFF组的排粪氮最高,其次为投喂CEFF组,且两者明显高于投喂NSF组.军曹鱼幼鱼投喂NSF、CEFF和CMFF时饱食和次饱食摄食水平的氮收支方程分别为:100CN=1.1(0.9)FN+27.0(29.3)GN+71.9(69.8)UN、100CN=5.2(4.3)FN+27.0(28.7)GN+67.8(67.0)UN和100CN=9.9(8.4)FN+21.6(10.1)GN+68.5(81.5)UN(氮收支方程括号中的为次饱食数据);3个饵料组军曹鱼幼鱼饱时和次饱食时摄食氮中用于排粪的比例较小且变化不大,投喂NSF和CEFF组次饱食时摄食氮中用于生长的比例较饱食时略大而用于排泄的比例较饱食时略小,但投喂CMFF组饱食时摄食氮中用于生长的比例明显高于而用于排泄的比例明显低于次饱食摄食水平时.因此,军曹鱼幼鱼的氮排泄和氮收支方程受摄食水平和饵料种类双重因素的影响,但不管投喂何种饵料,摄食氮增大是导致鱼类氮排泄增加的主要原因.综合考虑生长、食物转化效率、氮排泄和氮收支方程各因素,军曹鱼由幼鱼优先选择投喂的饵料为NSF,其次为CEFF,在本实验的生长阶段,两者的适宜投喂水平以占饱食量的70%-100%为佳.  相似文献   

10.
海水仔稚鱼对于n—3高度不饱和脂肪酸需求量的研究现状   总被引:3,自引:0,他引:3  
提供能量和必需脂肪酸(EFA)对于鱼类营养有着重要的作用。n-3高度不饱和脂肪酸(n-3HUFA)是海水仔稚色的必需脂肪酸,它主要包括二十碳五烯酸(EPA:205n-3)和二十二碳六烯酸(DHA:22:6n-3)。这些脂肪酸对于确保细胞膜渗透性和可塑性、前列腺素的产生和其它功能是必要的。Yone和Fujii报导:补充亚麻酸(18:3n-3)(淡水鱼的必需脂肪酸),对于改善真绸仔稚鱼的生长状况并没有效用,而只有n-3YIUFA作为EFA(必需脂肪酸),对于这种鱼的生长才有用。现在对许多种海水仔稚鱼的研究普遍认为:具有n-3HUFA的饵料对海水…  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.
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   

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.
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   

15.
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   

16.
《海洋学报(英文版)》2014,(8):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   

17.
18.
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.  相似文献   

19.
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.  相似文献   

20.
This article presents a methodology developed to evaluate the instability of submarine slopes that extend over a large area. Special attention was paid to (1) the complex geometry (bathymetry) and the expanse of the slope, (2) the heterogeneity of the sediment, and (3) the distribution of the pore pressure. The safety factor was considered as a spatially varying quantity. The General Formulation (GLE, Fredlund and Krahn 1977), which fully satisfies equilibrium conditions, was used for evaluating the stability of the marine slope. The submarine slope failure, which occurred on 16 October 1979 during the construction of the new Nice airport, was studied in order to test the developed model. Geotechnical parameters were taken from experimental tests carried out by IFREMER on 19 cores extracted at different depths (from 27 m to 1300 m) (Cochonat, Bourillet, and Savoye, 1993; Mulder et al., 1994). Many scenarios were proposed in order to explain the cause of the Nice slope failure (Habib, 1994). In this article, two of those scenarios were tested. Simulation results are presented and discussed.  相似文献   

设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号