道观河水库大银鱼移植生物学效应─Ⅰ.生长

本文根据大银鱼在道观河水库移植后的生长资料,计算出其生长指标,相对生长率和平均丰满度,对大银鱼在道观河水库的生长规律进行了分析,得出其体长体重关系为W＝1．2120×10-6L3．1820和VonBertalanffy生长方程的各项参数值：L∞＝193．03mm,W∞＝22．72g,K＝0．3328,由此得出大银鱼在该地区水域能移植驯化的科学依据．并据此为道现河水库大银鱼的最佳捕捞时间提出了初步的意见。     

湖北省水库与湖泊银鱼移植与增殖试验

在受试水库、湖泊中,移植与增殖二种银鱼,即近太湖新银鱼和太湖新银鱼。经三种人工采卵受精技术的比较试验,采用半干法人工受精最为理想。经多种受精卵运输方法的比较试验,采用塑料袋充氧运输最为理想。经散撒受精卵和网箱孵化的比较实验,采用网箱孵化最为理想。经不同放流鱼苗技术的比较实验,采用鱼苗平游后放流最为理想。经不同季节、不同开捕时间的比较实验,二种银鱼的合理捕捞时间为秋冬季,严禁在春季捕捞;最合理的开捕时间为国庆节前后。近太湖新银鱼和太湖新银鱼的人工采卵授精时间为3月上旬和4月上旬,严禁在非繁殖盛期采卵。银鱼的捕捞强度应控制在资源量的2/3或3/4范围内。     

近太湖新银鱼——银鱼移植新对象

近太湖新银鱼不仅在形态上与太湖新银鱼很相似,而且它们的个体大小、生长速度、食性等方面也十分相近。近几年在湖北地区的湖泊、水库相继发现了近太湖新银鱼,并在湖北省广水市徐家河水库成为优势种类,形成了较大生产规模。从目前研究的结果来看,近太湖新银鱼也是适宜我国湖泊、水库移植的银鱼种类。     

徐家河水库近太湖新银鱼(Neosalanx pseudotaihuensis Zhang)的性腺发育与产卵类型(英文)

银鱼生产的发展是通过银鱼的引种来实现的,银鱼的引种主要是采取向水体投放受精卵的方式来完成,受精卵又是通过人工繁殖而获得银鱼的人工繁殖不同于常规养殖鱼类,因其一经捕起很快就会死亡而不能进行人工催产因此银鱼人工繁殖的亲本是在银鱼的繁殖季节从天然水体中捕捞而获得,而大量的性成熟好的、可以立即进行人工受精的亲本只能在产卵高峰期才能捕获得到．所以了解并掌握银鱼的性腺发育规律和产卵时期对银鱼的人工繁殖十分重要 １９９２年４月至１９９６年５月在湖北省徐家河水库对近太湖新银鱼的性腺发育规律和产卵时期进行了长期的研究,并从１９９５年５月至１９９６年４月（银鱼的一生）周年标本中逐月进行了组织切片通过对近太湖新银鱼（Neosalanx pseudotaihuensis）卵细胞的组织学研究表明该鱼为分批产卵类型根据卵巢外部形态和内部组织结构,建议将近太湖新银鱼的卵巢划分为六个阶段;从卵巢每月发育期趋势和卵细胞大小以及卵的成熟度得出近太湖新银鱼的产卵期为３－５月,其中４月中旬至５月中旬为产卵高峰期;根据体长频率分布来看,近太湖新银鱼产完最后一批卵就死亡,因此,它的寿命仅一年从其周年体长和成熟系数分布并结合秋季大捕捞大量样本的检查,得出近太湖新银鱼只有春季产卵群     

太湖大银鱼生长特性的研究

本文根据太湖大银鱼(Protosalanx hyalocranius Abbott)周年生物学实测资料,并应用Von Bertalanffy生长方程进行计算,对大银鱼在太湖的生长规律及特点进行分析探讨,结果表明:1.体全长与体重呈幂函数关系:W=3.981×10~(-6)L~(2.9359);2.Von Bertalanffy生长方程的各项参数值为:L_∞=219.86(mm),W_∞=28.56(g),K=0.1469,t_0=0.33;3。生长拐点年龄为7、8月龄。     

云南蒙自五里冲水库区F1,F2断层新活动年代研究

五里冲水库地处侵蚀山区,缺乏第四纪地层作为研究断层新活动年代的对比标志。本文以F_1、F_2断层带内发育的多期方解石脉和断层泥为研究对象,采用显微构造分析,热释光(TL)测年法和扫描电镜(SEM)分析,石英溶蚀速率测年法,对库区F_1、F_2断层新活动的年代进行综合判定。确认:F_1、F_2断层最后一次明显活动的年代分别为(2.93±0.31)×10~5年和(2.33±0.26)×10~5年以前,为评估五里冲水库构造稳定性,提供了可靠的数据。     

鄱阳湖产银鱼的繁殖生物学

本文记述了鄱阳湖产太湖短吻银鱼(Neosalanx tangkahkeii taihuensis)、乔氏短吻银鱼(Neosalanx jordani)、雷氏银鱼(Reganisalanx brachyrostralis)等三种银鱼的成熟年龄、繁殖时期、生殖群体的体长、性比、生殖力、卵的特征等繁殖生物学资料,并记述了太湖短吻银鱼性腺成熟系数的周年变化、太湖短吻银鱼和乔氏短吻银鱼的产卵生态条件等。近二十年来鄱阳湖银鱼产量急剧下降的主要原因是产卵场遭到了严重破坏。银鱼生命周期仅一年,繁殖力强,认为加强繁殖保护、合理安排捕捞时间是恢复鄱阳湖银鱼资源的关键措施。     

太湖的泥沙与演变

历史时期,太湖是不断扩展的,其平均扩展速率为0.37km~2/a。据沙量平衡分析与计算表明。因湖岸崩塌和太湖水系的输沙作用,近期太湖的泥沙淤积量为9.28×10~5t/a.泥沙数量虽然不大,但经过长期的积累,对太湖演变具有深刻影响。就自然演变趋势而言,近期太湖面积仍以0.168km~2/a的速率扩大,容积则以3.95×10~5m~3/a的速率减小,太湖正进一步向浅平方向演变。然而,因围湖造田,建国以来,太湖的面积则以4.58km~2/a的速率在减小。     

丹江口水库的饵料生物资源及水体营养状态评价

根据1992年12月至1993年9月的调查,丹江口水库的饵料生物资源量为1．845×10~6t．其产鱼潜力为1．615×10~4t．是现有鱼产量（包括捕捞产量和不投饵网箱产量）的5倍左右．就水体营养状态而言,汉江库区为中营养型,丹江库区属贫一中营养型．文中还对丹江口水库的渔业发展和水质保护进行了讨论．     

生态环境需水量评估方法与例证

首先评价了生态环境需水量概念内涵, 包括概念的界定、生态环境水的组成结构和需水特点. 在此基础上, 提出了生态环境需水量分级和计算方法. 以黄淮海地区为研究实例, 估算了研究区生态环境现状用水量、最小需水量、适宜需水量, 并计算了相应的缺水量. 然后根据相关的规划, 对未来的水平年2010年, 2030年和2050年生态环境需水量进行了预测. 结果显示, 随着功能设定的不同, 水资源参照平台的差异, 最小和适宜生态环境需水量不同, 相应的缺水量也会产生差异. 研究表明, 黄淮海地区最小生态环境需水范围在2.84×10¹⁰~1.02×10¹¹ m³, 适宜需水量范围在6.45×10¹⁰~1.78×10¹¹ m³, 最小需水时的缺水量范围为9.1×10⁹~2.16×10¹⁰ m³之间, 适宜需水时的缺水量范围为3.07×10¹⁰~7.53×10¹⁰ m³之间. 通过不同的缺水量数值, 可以安排配水的优先性. 三个预测年的生态环境需水量范围分别为4.49×10¹⁰~1.73×10¹¹ m³, 5.99×10¹⁰~2.09×10¹¹ m³和7.44×10¹⁰~2.52×10¹¹ m³.     

密度和温度对萼花臂尾轮虫产卵量和混交雌体的影响

用小球藻(Chlorella sp.)为食培养萼花臂尾轮虫(Brachionus calyciflorus),食物浓度约1×10~6cells/mL,温度25℃,光照强度约40001x,昼长比LD=18:6。在1.0mL、0.5mL和0.25mL培养液中同时进行单个体和群体培养。结果发现:1)单个体培养时每个母体平均产卵量分别为12.0,13.8和7.8个;后代个体中混交雌体的百分比分别是46.38％,53.49％和55.83％。2)群体培养时,每个母体平均产卵量分别为8.7、3.1和2.65个,随密度增加而减少;后代个体中混交雌体百分比分别为41.70％,53.59％和54.26％,群体培养的密度为4.0ind./mL与2.0ind./mL,2.0ind./mL与1.0ind./mL混交雌体的百分比差异不明显。母体密度高低与后代混交雌体百分比间具有明显相关性。在上述培养条件下,轮虫为1.0ind./mL时,进行单个体培养,分别用急剧冷休克(SS)、逐渐冷休克(GS)和恒温对照(C)进行处理,结果表明:个体平均产卵量分别为10.8、9.2和12.6个。后代混交雌体百分比分别为32.85、20.7和16.87,SS和C处间后其混交雌体比例具显著差异,而SS和GS,GS和C处理间没有显著差异。     

The whitefish (Coregonus lavaretus (L.)) of the Wahnbach reservoir and their assessment by hydroacoustic methods

In 1957 whitefish were successfully introduced into Wahnbach reservoir, a drinking water storage near Bonn (FRG). Since excessive predation on the herbivorous zooplankton by fish could have negative effects on water quality, the size of the pelagic fish stock had to be known. For this purpose, and for establishing management guidelines for the whitefish population, a stock assessment involving hydroacoustics, trawling and gillnetting was performed in October 1984. The results indicate that the whitefish stock is self-sustaining today. Growth of individual fish is moderate. The total pelagic fish population was estimated to 11,130 fish, comprising some 2600 whitefish larger than 25 cm. Stock density was found to be low. An annual catch of about 900 adult whitefish (300 or 1.4 kg ha⁻¹) is recommended in order to control population size and to limit predation pressure on the herbivorous zooplankton.     

Water Quality,Phytoplankton Diversity and Production in G. B. Pant Sagar at Rihand Dam,Pipri

The man made reservoir, G. B. Pant Sagar at the dam site (24° 15′ N Lat) in the South Mirzapur district of eastern U. P. was investigated in terms of water quality, phytoplankton diversity and production at monthly intervals between January 1987 and December 1987. The reservoir water showed low to moderate dissolved oxygen (4.3 … 7.5 mg/l) and quite low nutrient contents (0.01-0.2 mg l^?1). Phytoplankton diversity narrowly fluctuated (3.17-3.74) and mean annual production (149.7 g/m³ · aC) showed a meso- to eutrophic condition. A significant positive correlation was obtained between gross production and phytoplankton density (r = 0.79; P < 0.001) Multiple regression equation (GPP = 11.292 + 0.043 BAC + 0.075 CHL + 0.073 CYN) indicates that Chlorophyta contributed more to gross production due to the presence of a higher number of individuals.     

Maßnahmen zur Sanierung und Restaurierung des Elsterstausees bei Leipzig

Redevelopment and Restoration Measures for Lake Elsterstausee (Leipzig) Lake Elsterstausee is an artificial lake in the south of the town Leipzig. It was built in 1933, has an actual area of 50 ha, and an average depth of 2 m. Between 1970 and 1991, the lake was used for intensive fishery. Because of fish feeding and supplying the lake with highly nutrient loaded water from river Elster the waterbody was in a polytrophic state during this time. Secchi depth seldom exceeded 0.4 m, but pHvalues often exceeded 9. Therefore and because of ammonia concentrations between 1.5 and 4.0 mg/L fish kills often occured. Lake Elsterstausee had no usability as bath waterbody although it was orginally built for this purpose. In 1991, a complete programme for redevelopment and res-toration of the lake started. The main measures were the total exchange of trophic loaded water and the only supply with treated groundwater, the drastic decrease of fish populations – in 1991 140 tons of fish (90% carps) were removed from the lake, – the development of healthy wild fish populations and of a eutrophication diminishing food chain, and the development of a reed zone almost around the lake. The groundwater treatment was steadily improved between 1992 and 1996. Actually, the following optimized system works: Drained groundwater from the surface lignite mine Zwenkau (pH = 6.95) and percolating water from the heaps (pH = 3.01) are mixed in the proportion 1:1 after intensive aeration. The water flows through a ditch that is 1 600 m long and has a performance up to 300 m³/h. In the well-diversified ditch, up to 90% of the iron is removed by precipitation and filtration effect of submerged macrophytes and filamentous algae. In the same time, deacidification occurs primarily by sulfate reduction in the sediment. Meanwhile, the water has a pH of 4.64 immediately after mixing, this value enhances up to the end of the flowing distance to 7.3. Internal restoration of the lake started in November 1991 with the total removal of loaded water and of almost all carps and white fishes. In 1993, 4 000 carnivore fishes (zanders, pikes, welses) were given into the lake to keep white fish popu-lations on a low level. Additionally, every year between 5 and 7 kg of water fleas (Daphnia sp.) were added. By means of this initial biomanipulation, food chain in lake Elsterstausee was stabilized. As results of the above mentioned measures, nutrient content in the waterbody decreased and secchi depth increased steadily. Between 1991 and 1997, trophy degree according to Klapper developed from 5 (hypertrophic) to 3 (eutrophic).     

陆水水库的浮游生物及营养类型

报道了１９９１￣１９９５年对面积为１６９３ｈｍ＾２的黑龙滩水库渔业利用优化模式研究的结果,主要内容有：水生生物种类组成和现存量调查、浮游植物初级生产力测定、渔获物统计和鱼产力估算;水体理化性状和水位变化对鱼产量和浮游生物群落结构的影响,网箱养殖鲤、草鱼的高产试验结果;多功能水库生态系统的渔业利用优化模式初步探讨。经三年努力,水库鱼产量由６２２ｔ上升到１２５５．１ｔ,平均单产７５０ｋｇ／ｈｍ＾２。为     

于桥水库的水质保护与渔业生产

大水面增养殖将水体中的氮、磷、有机物转化成鱼产品,并以渔获物的形式输出水体,从而加大水体氮、磷、有机物的输出量,有减缓水体富营养化、净化饮水水质的作用;同时鱼类的摄食、消化、排泄等新陈代谢活动可加速水中氮、磷等物质循环,使藻类繁衍,如果大量放养草鱼还会导致水草资源破坏、生态失衡,对饮水卫生、安全不利;网箱养鱼投入饲料,直接增加了水源有机污染。围网养殖对局部水域生态平衡有破坏作用,放养密度过大,投入     

1987—2022年新安江水库（千岛湖）水面面积时空变化及其与水位、蓄水量的响应关系

水面面积、水位、蓄水量是水库水资源管理的重要基础数据,遥感是湖库水体提取、水位和蓄水量估算的重要技术手段。由于不同水体提取方法的适用性差异、测高卫星数据的有限时间覆盖度和开源数据集的时空分辨率不足等原因,湖库水面面积、水位、蓄水量的长时序、高频率时空变化监测仍存在一定挑战。本研究以新安江水库为研究区,结合多源遥感、气象、水文和土地利用等数据,基于Google Earth Engine云平台,运用水体指数法,分析1987—2022年新安江水库水面面积时空变化特征,构建水位—水面面积、水位—蓄水量和水面面积—蓄水量响应关系,探究水面面积时空变化成因。结果表明:(1)Landsat 5、Landsat 8和哨兵2号数据的最佳水体提取指数分别为AWEI_sh和GNDWI,F1-score分别为91.93%、91.03%和93.14%。相比于开放数据集GSWED(32.61%)、JRC GSW(76.17%)和ReaLSAT(69.76%),基于最优水体指数的水体提取结果具有最高的F1-score(91.26%);(2)时间上,1987—2022年新安江水库水面面积呈显著上升...     

太湖贡湖湾鲚(Coilia ectenes taihuensis Yen et Lin)食物组成的季节变化

鲚(Coilia ectenes taihuensis Yen et Lin)是太湖主要的鱼类之一,其产量随水体富营养化程度的加重呈上升趋势.本研究于2009年4-12月用刺网(a=10 mm)在太湖贡湖湾采集了鲚,分析了其胃含物中食物组成的季节变化以及鲚对食物种类的选择性.结果表明,鲚在各月中主要以浮游动物为食,同时也摄食幼鱼、幼虾和水生昆虫等.鲚的食物组成具有明显季节变化,4月份以桡足类为食,其中桡足幼体、汤匙华哲水蚤(Sinocalanus dorrii Brehm)和剑水蚤(Cyclops spp.)所占的平均个数百分比相当;6、8和10月份主要以枝角类为食,其中6月以裸腹溞(Moina spp.)为主,而8和10月以象鼻溞(Bosmina spp.)为主.食物选择性方面,鲚对大型浮游动物表现出主动选择;当环境中出现溞(Daphnia spp.)和透明薄皮溞(Leptodora kindti Focke)时,鲚对它们表现出很强的选择性摄食,但透明薄皮溞只出现在6月鱼类食物中;个体较小的裸腹溞也是鲚主动选择的重要食物,在整个调查期间鲚对裸腹溞都表现出较高的主动选择性;象鼻溞虽然在各月份食物中的出现率最高,但除10月份鲚对其表现出主动选择外,其它月份表现为主动回避或随机选择.本研究结果有助于我们了解鲚对浮游动物群落影响的季节变化,为制定合理的湖泊与渔业管理方案提供依据.     

Using of the Ornamental Fish in Wastewater Biological Treatment

Breeding ornamental fish in wastewater was a successful solution not only to decrease sanitary risks but also to encourage fish growth. In fact, the secondary treated effluent was used to grow a walking catfish (Clarias batrachus), a western mosquitofish (Gambusia affinis; Poeciliidae), and a leopard pleco (Glyptoperichthys gibbiceps). The growth rate of fish reared in final treated wastewater was significantly higher than of treated effluent (25 and 50%) and the relative growth rate during 2 months reached 2, 4, and 2.5, respectively. Bacterial loads were important in the gills compared to other fish organs (intestine, skin, and edible muscles). However, the total aerobic germs ranged between 2 × 10³ and 3.4 × 10³ cfu/g in the edible fish species cultured in secondary treated effluent. The pathogenic bacteria Aeromonas hydrophila was absent in all examined fish muscles. However, the presence of tested fishes did not prevent the reduction of the treatment biological parameter (BOD and COD) at half, in the three treated wastewater proportions (25, 50, and 100%) and thereafter, they clearly participated to the tertiary biological treatment of used water. Further bacteriological and physico‐chemical analyses indicated that the use of treated wastewater in aquaculture is safe and risks to human health are reduced.     

Modification of halocline source waters during freezing on the Beaufort Sea shelf: evidence from oxygen isotopes and dissolved nutrients

During some, but not all winters, waters on the Mackenzie shelf of the Beaufort Sea become sufficiently saline to ventilate the halocline of the adjacent Canada Basin. This occurred in March 1988, at which time a survey of the temperature, salinity, dissolved nutrient and ¹⁸O properties of the ventilating waters was completed. The regional hydrography of 1988 was very similar to that of 1981, when ventilation also occurred in this area. The δ¹⁸O-salinity properties of the cold, saline shelf waters revealed that in the winter of 1987–1988, ice was grown from water initially more saline by about 1.5 [psu] than is typical for the area. The higher initial salinity appears to have been a consequence of a two-stage conditioning of shelf waters by storms in the autumn of 1987. Since the amount of ice growth, and consequent salt rejection, over the winter of 1987–1988 was abnormally low, this conditioning played a crucial role in the formation of the ventilating water mass. Nutrient concentrations in ventilating waters were the same as those of waters unaffected by freezing. Thus significant regeneration of nutrients within the cold saline shelf waters did not occur during their 6-month period of formation. In consequence, the nutrient signatures carried into the arctic halocline by winter shelf waters from this area tended to erode, rather than to reinforce the nutrient maxima. For this reason they are not the dominant source of supply to the arctic halocline. Waters in the Chukchi and northern Bering Seas during the same period had δ¹⁸O values intermediate between those on the Mackenzie shelf and those in the arctic halocline. Thus winter shelf waters are supplied to the arctic halocline with a range of nutrient, temperature, salinity and δ¹⁸O properties. On average, the southern Canada Basin is an impressive net producer of sea ice. The net rate of production from waters in the upper 350 m in this area is about 2 m y⁻¹, approximately twice the net rate of production in the central Arctic Ocean.