东湖放养鱼类时空分布的水声学研究

2000年,用鱼探仪逐月对东湖鱼类的空间分布进行探测的结果表明：东湖鱼类主要分布在1．5m以下的水层,1．5m以上与1．5m以下的水层的鱼类密度分布存在显差异,此外,东湖中不同区域的鱼类密度分布亦有显性差异,统计分析显示,这种水平分布差异与水深,离岸距离等因素没有明显的相关,可能主要由群聚行为引起,由不同月份群聚程度不一致,推测水温的变化可能会影响鱼类的群聚行为,污水排放对鱼类空间分布也可能有一定的影响。     

基于水声学方法的天目湖鱼类资源捕捞与放流的生态监测

本文在天目湖捕捞赶鱼前（2011年12月）、赶鱼后（2012年1月）、捕捞与放流后（2012年3月）3个渔业阶段,结合渔业捕捞统计,采用水声学方法对天目湖鱼类资源（赶鱼后为不包括集鱼网箱的湖区鱼类资源）的捕捞与放流进行了生态监测,并构建GIS模型,得到鱼类种群结构、大小组成、鱼类密度、鱼类集群、鱼类资源量及其分布,为天目湖保水渔业的实施和渔业生产提供科学依据。天目湖鱼类种群以鲤科鱼类为主,鲢鳙2011年捕捞统计重量占比为98.07%,单网簖采样尾数占比为68.72%,鱼类资源受放流种类和规格影响较大;赶鱼前后和捕捞与放流后3个渔业阶段的鱼类平均目标强度（TS）分别为（-47.84?4.79）dB、（-48.58?4.98）dB、（-47.24?5.10）dB,且差异性显著（P<0.05）,捕捞与放流后TS在-45—-40 dB的鱼类明显升高到24.40%;3个渔业阶段的鱼类密度（FPCM）分别为（0.0124?0.0292）ind/m3、（0.0062?0.0227）ind/m3、（0.0098?0.0185）ind/m3,捕捞赶鱼作业显著（P<0.05）降低了鱼类密度,而捕捞与放流后鱼类密度显著（P<0.05）低于赶鱼前则是由于水深上升所致;在冬季的中下层水体出现典型的鱼类聚群,且随温度降低团聚程度提高;通过构建GIS模型评估鱼类资源量,赶鱼前约61万尾、赶鱼后约38万尾、捕捞与放流后约67万尾,资源量在中下游分布较高。     

三峡库区香溪河鱼类资源水声学探测效果的昼夜差异研究

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基于水声学探测的香溪河鱼类资源时空分布特征评估

为了掌握三峡水库香溪河鱼类资源时空分布特征, 2013 年5 月和11 月运用Simrad EY60 型分裂波束回声探测仪在香溪河进行了水声学探测, 辅以常规渔获物分析方法。渔获物调查共发现鱼类7 科41 种, 其中似鳊、贝氏、、银和蛇等小型鱼类在数量上占据优势地位。水声学探测结果表明, 香溪河春季鱼类密度显著高于秋季, 采用加权平均法求得2013 年5 月和11 月探测的鱼类密度分别为53.4 和15.4 ind./1000 m3。鱼类资源在空间上不均匀分布, 从高岚河至香溪河口鱼类密度逐渐降低;在垂直方向上, 春季和秋季水声学探测的鱼类密度显示出相同的趋势, 即表层 中层 底层。在运用鱼类生物操纵改善水质途径方面, 建议通过壮大肉食性鱼类种群来控制小型鱼类资源量, 同时通过增殖放流鲢、鳙以加强对浮游植物的滤食作用。       

三峡库区澎溪河鱼类时空分布特征的水声学研究

为了解三峡库区支流澎溪河鱼类时空分布变化,2009—2010年的秋季、冬季和春季,使用Simrad EY60鱼探仪对澎溪河的鱼类资源量及其时空分布特征进行3次声学调查。结果表明:3个季节鱼类水平分布不均匀,鱼类最大密度分别为67.07尾/1000 m3,19.66尾/1000m3,17.25尾/1000m3且不同季节上层、中层鱼类密度水平分布有显著性差异(P≤0.01,P=0.03);各季节鱼类密度垂直分布也有一定差异,冬季上层鱼类密度和下层鱼类密度差异较为显著(P=0.05);另外鱼类密度昼夜分布有显著性差异(P<0.05),造成该现象的原因主要是由于鱼类的昼夜垂直节律(Diel Vertical Migration,DVM)引起;3个季节的鱼类目标强度(TS值)的差异极其显著(P<0.01),其中秋季鱼类TS最高((-57.0±5.6)dB),春季TS值最低((-58.6±4.9)dB),造成该差异的原因是4—6月是长江上游鱼类繁殖季节,仔稚鱼居多。鱼类空间分布及其位点的水深关系分析显示,鱼类密度水平分布秋季、冬季与水深不相关(︱r︱<0.2),春季与水深中度负相关(r=-0.5,P≤0.05)。     

不同渔业方式水库鱼类资源的水声学评估

采用Biosonics DT-X回声探测仪(208 kHz)在2011年的秋末冬初对大溪、沙河、金牛山3个不同渔业方式的中等营养化水库进行了水声学调查,并构建了水库中鱼类资源分布的GIS模型.结果表明： 3个水库间鱼类平均大小无显著性差异,但鱼类目标强度(TS)分布曲线表明鱼类大小分布比例并不一致,受渔业方式影响明显.大溪水库鱼类密度(平均0.0183 ind·m^-3)与沙河水库鱼类密度(平均0.0124 ind·m^-3)差异不显著,金牛山水库鱼类密度(平均0.0085 ind·m^-3)显著小于大溪水库和沙河水库,3个水库中鱼类密度水平分布与水深没有显著的相关关系.3个水库中鱼类均成群分布,对大溪水库和沙河水库调查时还发现鱼类聚群行为.3个水库的鱼类资源量分布均在下游最高,除沙河水库受赶鱼作业影响外,其他2个水库大坝前鱼类资源量分布明显偏高.基于鱼类分布GIS建模的栅格化数据、各个栅格的水面面积,对TS>-60 dB鱼类资源总量进行估算,大溪水库约为48万尾,沙河水库约为61万尾,金牛山水库约为52万尾;对TS>-40 dB的鱼类进行统计评估,大溪水库约为5.04万尾,沙河水库约为5.29万尾,金牛山水库约为9.07万尾.     

三峡库首鱼类分布格局的水声学探测评估

2007年4月19-24日,应用EY60回声探测仪三峡水库库首区域的鱼类分布格局进行了水声学探测。研究发现:三峡大坝坝前至巫山干流江段鱼类分布不均匀,密度范围为0.718～37.46ind./1000m³,均值为3.117ind./1000m³;鱼类主要分布的区域为支流河口及码头等位置,其中船闸通道位置密度最高;垂直分布上鱼类主要分布在30～60m的水层。分析认为,三峡库首区域鱼类的分布可能与浮游生物的丰富度有关。另外本文分析了三峡库区探测中鱼类个体目标强度的分布及信号过滤,以便下一步水声学探测研究的深入。     

水坝拆除对黑水河鱼类群落结构和空间分布的影响

水坝拆除引起河流连通性、水动力、河流地貌等一系列变化,直接影响了鱼类群落结构和空间分布。黑水河为金沙江左岸一级支流,其上共建四级电站,出于支流生境恢复需求,第四级水坝老木河水坝于2018年12月实行拆除。为探明低水头坝拆除对鱼类群落的影响,结合2018年6月和2019年6月黑水河下游60.4km河段10个点位的渔获物调查,对拆坝前后鱼类群落结构和生态类型变化、优势物种与单位捕捞努力量以及不同河段间的群落相似性进行了分析。结果表明,水坝拆除半年后优势物种仍以鲤科和鳅科为主,但物种数和丰度整体上增加;生态类型上以杂食、喜急流和产微粘性卵鱼为主;拆坝后鱼类群落空间分布变化明显,靠近河口的自然河段鱼类上溯洄游到原坝址的上下游,部分长江上游特有鱼类在原坝址附近发生定殖行为,且拆坝后各河段的鱼类组成结构有同质化趋势。总体上,老木河水坝的拆除对黑水河下游的鱼类群落结构和空间分布产生了积极的影响。     

柠条细根的空间分布特征及其季节动态

以晋西北黄土区30年生柠条(Caragana korshinskii Kom.)人工林为研究对象,2007年应用Minirhizotron技术,分别在距茎干水平距离0、50、100 cm处设点,对林地0-100 cm土层深度范围内的柠条细根空间分布及其生长季的动态进行了研究。结果表明:(1)生长季柠条细根根长密度(RLD)总平均值为1.3423 mm/cm²。在水平方向上,距茎干水平距离50 cm处分布最多(1.5369 mm/cm²),其次为0 cm处(1.3855 mm/cm²), 100cm处分布最少(1.1044 mm/cm²)。在垂直深度上,各土层RLD平均值大小顺序为40-60 cm>60-80 cm>20-40 cm>0-20 cm>80-100 cm;(2)在0-100 cm土层范围内,月平均RLD在生长季的波动范围为0.4405 2.1040 mm/cm²,其中9月份最多,4月份最少;RLD在5个土层深度3个水平距离处随季节变化均表现先增加后减少的趋势,且不同空间位置RLD峰值变化均在秋季(8 10月份)波动。细根的这种时空分布差异,可能主要受林下土壤资源空间异质性及其季节性变化的影响,但也不排除其它因素的影响(如真菌,植食性昆虫)。     

Seasonal and spatial distribution pattern of nitrogen fixing bacteria in fish ponds under different management systems

Enumeration of nitrogen fixing bacterial population in water and sediment samples of six fish farming ponds (polyculture, monoculture and traditional systems) over a period of two and a half years revealed significant differences between the culture systems with maximal and lowest counts in the monoculture and traditional systems, respectively. Polynomial equations of the 2nd to 4th degree were used to represent the observed seasonal data in these ponds. The bacterial populations peaked in summer, while the lowest count was observed in winter. The environmental factors such as pH, different species of nitrogen, dissolved organic carbon were responsible for the seasonal changes in nitrogen fixing bacteria.     

The results of hydroacoustic observations on roach in Lake Glubokoe in winter

This paper describes under-ice observations on the diurnal dynamics of the distribution and behaviour of roach in Lake Glubokoe in March, 1983, and in March, 1984. It presents data on the reactions of fish to external stimuli. Some factors influencing the distribution of fish in the winter period are discussed.     

三峡库区大宁河鱼类的时空分布特征

为了解大宁河鱼类资源量及其分布特点,于2006年12月和2007年4月利用HTI Model 241鱼探仪对三峡库区大宁河进行了声学调查。结果表明：冬季鱼类密度显著高于春季,这与鱼类自身的繁殖越冬行为有关。统计分析显示,鱼类水平分布的差异与水深没有明显的相关性,可能主要由群聚行为引起。另外,冬季大宁河鱼类主要分布在中下层,上层和中下层的鱼类密度分布存在极显著性差异(p <0.01);春季鱼类主要分布在中上层,中层和下层的鱼类密度分布差异显著(p <0.05)。大宁河鱼类在冬季和春季均属于成群分布,并且春季各层鱼类密度的变异系数高于冬季,这与水温和鱼类的防御机制有关。     

Temporal and spatial distribution of biogenic silica and its significance in the Wuliangsuhai Lake and Daihai Lake

In this work, the concentrations, temporal and spatial distributions and the relationship between biogenic silica (BSi) and primary productivity are discussed on the basis of the geochemistry character of BSi in the water–sediment system of the Wuliangsuhai Lake and Daihai Lake. The results show that the average concentrations of SiO₃^2- and BSi are 3.0 mg/L and 3.5 mg/g in the overlying water and sediments from the Wuliangsuhai Lake, respectively, while they are 1.0 mg/L and 7.5 mg/g, respectively, in the Daihai Lake. It is the uptake and assimilation of diatom phytoplankton which results in the significant difference of the SiO₃^2- concentrations between the two lakes, and the inputs of surface runoff is one of the important factors in impacting the spatial distributions of SiO₃^2- in the overlying water. The spatial distributions of BSi suggest the Si source of the two lakes and indicate the differences of eutrophication types and ancient primary producer between the two lakes. The eutrophication precesses and ancient primary productivity of diatom phytoplankton are reconstructed by applying the geochemistry information of BSi archived in the vertical concentration profiles in the two lake sediments. The geochemistry information of BSi well responds to the paleoenvironment and paleoclimate of the Daihai drainage basin indicating silicate limitation of primary productivity by diatoms phytoplankton in the Daihai Lake.     

Temporal and spatial distribution of biogenic silica and its significance in the Wuliangsuhai Lake and Daihai Lake

In this work, the concentrations, temporal and spatial distributions and the relationship between biogenic silica (BSi) and primary productivity are discussed on the basis of the geochemistry character of BSi in the water–sediment system of the Wuliangsuhai Lake and Daihai Lake. The results show that the average concentrations of SiO₃^2- and BSi are 3.0 mg/L and 3.5 mg/g in the overlying water and sediments from the Wuliangsuhai Lake, respectively, while they are 1.0 mg/L and 7.5 mg/g, respectively, in the Daihai Lake. It is the uptake and assimilation of diatom phytoplankton which results in the significant difference of the SiO₃^2- concentrations between the two lakes, and the inputs of surface runoff is one of the important factors in impacting the spatial distributions of SiO₃^2- in the overlying water. The spatial distributions of BSi suggest the Si source of the two lakes and indicate the differences of eutrophication types and ancient primary producer between the two lakes. The eutrophication precesses and ancient primary productivity of diatom phytoplankton are reconstructed by applying the geochemistry information of BSi archived in the vertical concentration profiles in the two lake sediments. The geochemistry information of BSi well responds to the paleoenvironment and paleoclimate of the Daihai drainage basin indicating silicate limitation of primary productivity by diatoms phytoplankton in the Daihai Lake.     

布哈河青海湖裸鲤鱼苗鱼卵的时空分布研究

2008年7月1日到10月7日,使用水文过河缆道及圆锥网接滤过式集苗器进行采样,对青海湖布哈河鱼类早期资源的时空分布进行了研究,以期了解青海湖裸鲤的自然繁殖状况,为其资源监测及生态保护提供基础性资料。结果表明:布哈河中鱼类早期资源种类单一,主要为青海湖裸鲤,采样期间有多次苗汛,主要苗汛出现于7月份,9月上旬仅有小规模苗汛;鱼苗平均密度3.17ind.·m^-3,最高达54ind.·m^-3;晚上鱼苗密度(22:00-22:10)与下午鱼苗密度(14:00-14:10)有显著性差异(df=98,P<0.05);青海湖裸鲤的鱼卵在上层平均密度为0.075ind.·m^-3,下层平均密度0.175ind.·m^-3,两者亦存在显著性差异(df=10,P<0.05);鱼苗的漂流运动主要集中在晚上;总体上看,鱼苗主要分布在河流上层,有近岸分布的趋势,而鱼卵则主要分布在河流下层,接近河流中央位置;鱼苗断面系数为0.43,鱼卵断面系数为2.32。     

抚仙湖底栖软体动物的种类组成与空间分布

2005年6-7月在抚仙湖采集到底栖软体动物7科8属9种,其出现率为70%,分布的最大水深为118 m,平均水深为31 m,分布区内的平均密度为614 ind·m-2,平均生物量为80.64 g·m-2.软体动物主要分布在湖湾,在密度方面,长角涵螺和环棱螺占优势,在生物量方面,河蚬和环棱螺占优势.现存量分布北区大于南区,沿岸区大于湖心区,水草区大于无草区.软体动物密度分布主要受湖底理化性质影响,与表层水体营养水平相关关系不显著.     

Factors influencing the spatial distribution of zooplankton and fish in Loch Ness, UK

• 1 The vertical and horizontal distribution of phytoplankton, zooplankton and fish in Loch Ness, Scotland, were monitored during one day‐time and one night‐time survey in July 1992. The vertical samples were collected at a site located at the northern end of the loch and the horizontal samples along a longitudinal transect.
• 2 The vertical distribution surveys demonstrated that the phytoplankton, the zooplankton and the fish were concentrated in the top 30 m of water above the seasonal thermocline. Within this layer, Cyclops stayed much closer to the surface than Eudiaptomus but both species moved towards the surface at night.
• 3 The most important factor influencing the horizontal distribution of the phytoplankton was the north‐ south gradient in productivity. The sub‐catchments surrounding the north basin contain a greater proportion of arable land than those to the south and the concentrations of nitrate‐nitrogen and phytoplankton chlorophyll increased systematically from south to north.
• 4 Zooplankton distribution patterns were influenced by wind‐induced water movements and the dispersion of allochthonous material from the main inflows. The highest concentrations of Cyclops were recorded in the north, where there was more phytoplankton, and the highest concentrations of Eudiaptomus in the south, where there were higher concentrations of non‐algal particulates.
• 5 There was no spatial correlation between total zooplankton and total fish abundance but the highest concentrations of small (1–5 cm) fish were recorded in the south where there was a large patch of Eudiaptomus. The number of Eudiaptomus at specific locations within this patch were, however, negatively correlated with the numbers of small fish. These results suggest that the fish were actively foraging within the patch and were depleting their zooplankton prey in the areas where they were most abundant.