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1.
通过海水陆基围隔实验,研究了凡纳滨对虾(Litopenaeus vannamei)与青蛤(Cyclina senensis)、菊花心江蓠(Gracilaria lichevoides)投饵混养的适宜配比、经济效益和生态效益。实验结束时对虾的体重、成活率和净产量分别为5.30~6.12g,62.96%~78.21%和1 065.0~1 367.6kg.hm-2。青蛤体重和净产量分别为6.85~7.15g,和51~328kg.hm-2。菊花心江蓠净产量为3 900~9 380kg.hm-2。混养系统的经济效益和生态效益均优于对虾单养。在本实验条件下,混养系统的最佳结构为凡纳滨对虾30ind.m-2,青蛤30ind.m-2,菊花心江蓠200g.m-2;其N,P绝对利用率分别为52.94%和26.09%。 相似文献
2.
几种虾、贝、藻混养模式能量收支及转化效率的研究 总被引：1，自引：0，他引：1
实验采用围隔实验方法,对凡纳滨对虾(Litopenaeus vannamei)、青蛤(Cyclina sinesis)、菊花心江蓠(Gracilarialichevoides)和活菌净水剂的不同单、混养生态系统的能量收支和转化效率进行了研究。实验结果表明,实验期间系统接受的总太阳光辐射能为1 983.2 MJ/m2。浮游植物对光能的利用效率在各处理间无差异(0.147±0.007)%,混养江蓠显著地提高了总利用效率(0.308±0.019)%。总能量的转化效率,虾藻混养(28.36%)和江蓠单养(27.65%)最高,其次是虾贝藻混养(26.70%),对虾单养(12.24%)最低。单位净产量对饲料能的消耗,对虾单养(21.24 MJ/kg)最多,虾菌、虾贝混养(18.76~18.97 MJ/kg)次之,而虾藻、虾贝藻混养(2.64~3.24 MJ/kg)则显著地降低了饲料消耗量。实验中投喂组都有较多的能量沉积,对虾单养沉积量达到1.10 MJ/m2,虾贝混养(1.30 MJ/m2)稍高,而虾贝藻、虾菌、虾藻混养平均为0.53 MJ/m2,显著地低于对照。结果表明,混养青蛤和菊花心江蓠显著地提高了对虾养殖中的光能利用率和能量转化效率,减少了能量沉积,从而大大地提高了能量的利用效率。 相似文献
3.
两种虾、贝、藻综合养殖模式的初步比较 总被引：5，自引：0，他引：5
利用太平洋牡蛎(Crassostrea gigas)和孔石莼(Ulva pertusavar)与凡纳滨对虾(Litopenaeus vannamei)以2种方式搭配放养,旨在查明其各自的生态特征及养殖效果。实验中对虾设2个放养密度,分别为17尾/m2和34尾/m2;牡蛎、石莼各设1个放养密度,分别为1 700 g/m2,140 g/m2。实验结果表明,经过50 d的实验,2个密度下对虾的生长均是混养明显快于分养模式(高密度混养与分养对虾体重分别为(7.04±0.19)g,(5.20±0.22)g;低密度混养与分养对虾体重分别为(7.89±0.34)g,(5.66±0.30)g)。总产量也是混养模式稍高于分养模式[高密度混养与分养对虾产量分别为(330.92±8.91)g,(189.47±8.05)g;低密度混养与分养对虾产量分别为(264.97±11.46)g,(135.82±7.27)g]。混养模式水体中的浮游植物的含量高于分室循环水模式中的含量,其它水化学指标间没有明显差异。分养循环水模式下虾室中水体过清、透明度过高,从而导致水中光照强度和光色的变化可能是其中对虾生长较慢的主要原因。 相似文献
4.
《海洋湖沼通报》2018,(5)
研究了珍珠龙胆石斑鱼(Epinephe lusfuscoguttatus♀×E.luslanceolatus♂)与3种不同海水植物工厂化原位混养系统的动植物生长及水质变化情况。实验设4个处理组,分别为珍珠龙胆与菊花江蓠(Gracilaria lichevoides)混养(FA),珍珠龙胆与长茎葡萄蕨藻混养(Caulerpa lentillifera)(FB),珍珠龙胆与海马齿(Sesuvium portulacastrum)混养(FC),以及珍珠龙胆单养(F)。结果表明,石斑鱼的特定生长率在0.69~0.82%之间,以实验组FC最高,显著高于FA和对照(P0.05),而与FB差异不显著(P0.05);饲料系数在1.02~1.11之间,以FC最高,显著高于FA和对照(P0.05),而与FB之间没有显著差异(P0.05)。三种混养植物的净产量方面,以海马齿最高,达(1730.26±117.01)g·m~(-2),显著高于菊花江蓠和长茎葡萄蕨藻(P0.05)。各混养处理的水质指标整体上均优于石斑鱼单养,其中以处理FC的整体水质条件最好,其PO_4~--P、COD、悬浮物浓度等指标均显著低于其他处理组(P0.05)。研究表明,工厂化养殖模式下珍珠龙胆石斑鱼与菊花江蓠、长茎葡萄蕨藻、海马齿3种海水植物原位混养的养殖效果均优于石斑鱼单养,其中以珍珠龙胆与海马齿的混养效果最佳。 相似文献
5.
发展虾池生态系统功能,采用围隔实验方法,研究了凡纳滨对虾(Litopenaenus vannamei)、青蛤(Cyclina sinensis)、江蓠(Gracilaria lichevoides)混养生态系统能量收支和能量转换效率。结果表明,实验期间所接受的总太阳辐射能为1 854.4MJ.m-2。各混养处理光合能显著高于对照。混养各处理光能利用率为0.23%~0.36%,随江蓠放养密度的增加而升高,显著高于对虾单养(0.14%)(p<0.05)。各混养处理与对虾单养相比,系统总能转化率分别提高了113.4%,94.2%,116.02%和41.91%,单位净产量耗总能则平均比对虾单养降低62.22%,但各处理饲料能转化率差异不明显(p>0.05)。各处理底泥沉积能量为0.71~1.38MJ,分别占总输出能的3.66%~8.61%,沉积量平均比对虾单养(1.65MJ)降低20.14%。可以看出,江蓠和青蛤混养可以显著提高对虾池光能利用率和投入系统总能的转化效率,降低虾池能量的沉积,进而大幅提高系统能量利用率。 相似文献
6.
三疣梭子蟹与凡纳滨对虾混养实验研究 总被引：1，自引：0，他引：1
采用海水陆基围隔实验方法探讨三疣梭子蟹和凡纳滨对虾混养的适宜配比和水环境的变化,并比较其养殖效果.实验中对虾6个放养密度分别为0,15,45,75,105,135 尾/m~2;三疣梭子蟹的密度为6尾/m~2.实验结果表明,经过60 d的养殖,混养组梭子蟹的成活率、规格和净产量均优于梭子蟹单养组,其中,混养对虾密度为45尾/m~2组(45.71%,43.22 g/ind,1 191 kg/hm~2)最高,其次是75尾/m~2组(44.58%,39.13 g/ind,1 050 kg/hm~2),梭子蟹单养组(35.13%,32.87 g/ind,693 kg/hm~2)最低.混养6尾/m~2密度梭子蟹条件下,对虾的养成规格和成活率与对虾密度呈负相关.实验后期各混养组水体中总氨氮、亚硝酸盐、硝酸盐和总氮含量均显著高于单养组,且随对虾放养密度增高显著上升.水体总氨氮含量各混养组在养殖50 d后均超过500 μg/L.本实验表明:三疣梭子蟹与凡纳滨对虾混养的最佳配比为三疣梭子蟹6尾/m~2,对虾45～75尾/m~2. 相似文献
7.
采用陆基围隔实验法,开展了草鱼(Ctenopharyngodon idellus)、鲢鱼(Hypophthalmichthys molitrix)和凡纳滨对虾(Litopenaeus vannamei)三元混养结构优化的初步研究。实验于2009年5～10月进行,每月定期采样,分别测定了各混养系统水质和底质的变化、养殖生物的成活率和养殖产量,分析了各混养系统的饲料转化效率、氮磷利用率及产出投入比。实验结果初步表明,草鱼放养密度为0.77尾/m2时,既可以保证出池规格(>1 100 g/尾)又不影响收获产量(>8 400 kg/hm2),同时饲料转化效率(>52%)及氮磷利用率(N>30%,P>14%)也较高;鲢鱼放养密度为0.23尾/m2或0.45尾/m2,可以起到调节水质的作用;对虾放养密度越大(48.9尾/m2),底质被污染程度越小。在本实验条件下,最佳的混养模式:草鱼与鲢鱼混养比例为草鱼0.77尾/m2鲢鱼0.45尾/m2;草鱼、鲢鱼和对虾混养比例为草鱼0.77尾/m2鲢鱼0.23尾/m2凡纳滨对虾16.3尾/m2。 相似文献
8.
采用陆基围隔实验法,开展了草鱼(Ctenopharyngodon idellus)、鲢鱼(Hypophthalmichth ys molitrix)和凡纳滨对虾(Lito penaeus vannamei)三元混养结构优化的初步研究.实验于2009年5～10月进行,每月定期采样,分别测定了各混养系统水质和底质的变化、养殖生物的成活率和养殖产量,分析了各混养系统的饲料转化效率、氮磷利用率及产出投入比.实验结果初步表明,草鱼放养密度为0.77尾/m2时,既可以保证出池规格(＞1 100 g/尾)又不影响收获产量(＞8 400 kg/hm2),同时饲料转化效率(＞52％)及氮磷利用率(N＞30％,P＞14％)也较高;鲢鱼放养密度为0.23尾/m2或0.45尾/m2,可以起到调节水质的作用;对虾放养密度越大(48.9尾/m2),底质被污染程度越小.在本实验条件下,最佳的混养模式:草鱼与鲢鱼混养比例为草鱼0.77尾/m2鲢鱼0.45尾/m2;草鱼、鲢鱼和对虾混养比例为草鱼0.77尾/m2鲢鱼0.23尾/m2凡纳滨对虾16.3尾/m2. 相似文献
9.
对虾、青蛤和江蓠混养系统氮磷收支的实验研究 总被引：8，自引：0，他引：8
为减少养殖污水中营养盐的排放量,降低对近海水质的污染,采用海水陆基围隔实验法,对凡纳滨对虾(Litope-naeus vannamei)、青蛤(Cyclina sinesis)和菊花心江蓠(Gracilaria lichevoides)不同混养系统的氮(N)、磷(P)收支状况进行了实验研究。结果表明:实验中的单养组投放的饵料占N总输入的75.5%,占P总输入的93.6%,混养组投放的饵料占N总输入的54.7%~64.8%,占P总输入的81.6%~88.7%;在支出项目中,单养组和混养组收获的养殖生物分别占N总输入的25.0%和44.4%~51.5%,占P总收入的11.2%和25.1%~31.8%;底泥沉积N,P为其主要支出项目,单养组和混养组分别占总输入的45.1%和30.0~32.5%,68.3%和50.3%~57.1%,其中混养组N,P的底泥沉积量低于单养组。 相似文献
10.
测定不同光强下菊花心江蓠(Gracilaria lichevoides)的产氧率和耗氧率.结果表明,20 000 lx以内菊花心江蓠的产氧率和光强的相关曲线的回归方程为y=0. 000 144 3x-0. 122 1,R2=0. 993 8,实验条件下菊花心江蓠的耗氧率为0. 121±0. 010 mg/(g·h),光补偿点为825 lx,光饱和点在20 000～22 000 lx之间,光饱和时的产氧率为2. 723±0. 329 mg/(g·h).光饱和以后菊花心江蓠的产氧率基本保持不变,45 000 lx以后出现轻微光抑制现象.测量水下光强随水深变化情况,发现水深达到水体透明度深度时,光强约14 000～15 000 lx,与菊花心江蓠的最大生长率的光强接近.测量不同养殖模式的溶解氧浓度昼夜变化,发现养殖密度过大可能在凌晨出现缺氧状态.根据菊花心江蓠的光合特性,提出江蓠养殖、江蓠用于生态修复的水深调控方法以及江蓠用于生态养殖的密度调控方法,以保持不同需求条件下较高的经济或生态效益. 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.
Derek V. Ellis 《Marine Georesources & Geotechnology》2001,19(1):51-63
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
14.
G. Parthiban 《Marine Georesources & Geotechnology》2000,18(3):223-235
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
15.
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
16.
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. 相似文献
17.
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
18.
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
19.
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
20.