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1.
2001-2002年天目湖(沙河水库)浮游植物的生态学研究   总被引:7,自引:0,他引:7  
2001年6月~2002年5月,对天目湖进行的浮游植物周年调查表明,天目湖共有浮游植物7门75属,其中年平均丰度为5026.20×104个/L,以蓝藻为主,占总丰度的54.45%;而年平均生物量为(15.364±9.103)mg/L,其中硅藻居首位,为6.634 mg/L,占浮游植物年平均生物量的43.18%;其周年变化是丰度和生物量最高值均出现在5月,丰度在5月和9月出现2个峰值,而生物量则在5、7、10月出现3个峰值。浮游植物丰度从大坝处1#点到河流入湖口的9#、10#点变化不明显但略有增加,而生物量则呈明显增加。通过对水温、透明度、营养盐与浮游植物丰度和生物量的线性回归分析发现,浮游植物丰度、生物量与水温、TP存在显著的正相关,而与N/P比、透明度存在显著性负相关,与TN相关性不是很明显。  相似文献   

2.
利用2008年4月(春季)和8月(夏季)在杭州湾生态监测区调查海域获得的浮游植物样本,分析了浮游植物的种类组成、优势度、丰度及多样性、均匀度的变化趋势,并将分析结果与该海域2005~2007年春、夏季的浮游植物各数据资料进行了对比,结果表明,2008年春、夏季调查区鉴定出的浮游植物数量达61种,隶属于5个门29属,以硅藻门为最多,有21属49种;其次是甲藻门,4属7种;蓝藻门,2属2种;绿藻门,1属2种;金藻门,1属1种。中肋骨条藻Skeletonema costatum和琼氏圆筛藻Coscinodiscus jonesianus为调查区主要的浮游植物优势种。以S13和S36站位的连线为界,将调查海域划分为南、北两个观测区,2008年春季,南观测区内的浮游植物丰度高于北观测区,夏季情况则恰好相反,表明浮游植物的丰度分布受季节变化影响。该海域中浮游植物的多样性指数(H′)和均匀度指数(J′)均偏低,2008年4月和8月的多样性指数平均值分别为1.31和1.58,均匀度指数平均值分别为0.324和0.413。2005~2008年春、夏季,该海域浮游植物群落组成不稳定,单优藻类优势度呈明显上升趋势,生物多样性呈现下降趋势,生态风险有加大趋势。  相似文献   

3.
为了解崂山湾浮游植物群落年际变化特征,在该海域设置了14个监测站位,于2012年-2014年每年3,5,8,11月采用浅水Ⅲ型浮游生物网进行了12个航次调查,并同步监测其它环境因子。共鉴定浮游植物127种,隶属于硅藻、甲藻、金藻、蓝藻、绿藻5大门类25科47属,其中硅藻16科36属105种,占种类数的82.7%;甲藻6科8属19种,占种类数的15.0%;金藻、蓝藻、绿藻各1科1属1种。优势种季节更替明显,3月份主要优势种为冰河拟星杆藻、中肋骨条藻和加拉星杆藻等,5月优势种为夜光藻、尖刺拟菱形藻和密联角毛藻等,8月优势种为三角角藻、尖刺拟菱形藻和派格棍形藻等,11月份优势种为虹彩圆筛藻、派格棍形藻和冰河拟星杆藻,浮游植物群落年际相似性在42%水平聚类分为春夏秋冬四大类群。浮游植物丰度季节更替明显,上下半年均有一个高峰期,上半年高峰期出现在3月,平均丰度169.2×104cell/m3,下半年高峰期在8月,平均丰度51.8×104cell/m3。绝大部分时间浮游植物丰度由近岸向远海呈递减趋势,高值区出现在田横岛西侧和鳌山卫东北面的内湾处,低值区位于远离崂山湾的外侧海域。群落Shannon-Wiener多样性指数平均2.305(1.829—2.745),Margalef丰富度指数平均0.987(0.634—1.507),Pielou均匀度指数平均0.675(0.466—0.815)。浮游植物丰度很大程度上取决于硅藻丰度,二者均与盐度、铵盐、叶绿素a、N/P呈极显著正相关(P0.01),与p H和无机氮显著正相关(P0.05),而与水温呈显著负相关(P0.05)。甲藻丰度与无机氮和铵盐含量呈显著负相关(P0.05)。物种多样性指数与化学需氧量显著正相关(P0.05),与无机氮、总磷和活性磷酸盐显著负相关(P0.05)。  相似文献   

4.
在2011年10月(代表秋季)和2012年4月(代表春季)对大亚湾海域浮游植物的种类组成、优势种和丰度进行了观测,实测数据采用Surfer 8.0软件进行绘图和插图制作,用SPSS 17.0软件进行主成分因子分析(PCA),同时用多元逐步回归分析方法,以主成分得分为解释变量,研究环境因子对浮游植物丰度的影响,以筛选出影响该海区浮游植物丰度分布的重要环境因子,并讨论了浮游植物丰度分布特征与环境因子的相关性及影响浮游植物分布的主要因素。分析结果表明:2个航次观测获得的浮游植物有4门31属51种(包括变型与变种),其中硅藻门的占优势,甲藻门的次之,黄藻与着色鞭毛藻门的较少。秋季浮游植物优势种有赤潮异湾藻Heterosigma akashiwo、中肋骨条藻Skeletonemacostatum、刚毛根管藻Rhizosolenia setigera、尖刺菱形藻Nitzschia pungens和菱形海线藻Thalas-sionema nitzschioides;春季浮游植物优势种有叉状角藻Ceratium furca、微小原甲藻Prorocentrumminimum、梭角藻Ceratium fusus和三角角藻Ceratium tripos。秋季浮游植物丰度为1.56×104~8.03×104个/dm3,平均值为3.95×104个/dm3;春季浮游植物丰度为1.21×104~4.70×105个/dm3,平均值为7.84×104个/dm3。水温、pH值、磷酸盐和总磷是影响大亚湾海域浮游植物分布的主要因素。  相似文献   

5.
2006 年春季长江口及其邻近水域浮游植物   总被引:5,自引:0,他引:5  
赵冉  孙军  宋书群 《海洋通报》2013,32(4):421-428
根据2006 年5 月在长江口及其邻近水域(30毅30忆N-32毅30忆N,121毅E-123毅30忆E)39 个测站采集的浮游植物水样,应 用Uterm觟hl方法初步分析研究了该水域浮游植物群集特征,并针对浮游植物优势物种与相关环境因子进行典范对应分析。调 查区浮游植物以硅藻和甲藻为主,此外还有少量的金藻、蓝藻和绿藻。浮游植物细胞丰度介于0.76耀6123.78 cells/mL 之间, 平均为397.94 cells/mL,主要优势物种为具齿原甲藻(Prorocentrum dentatum),骨条藻(Skeletonema spp.) 和米氏凯伦藻 (Karenia mikimotoi),细胞丰度明显高于2006 年同航次网样分析结果,具齿原甲藻和米氏凯伦藻水采样品中为优势物种,网 样中则较少检出,水采结果甲藻丰度比例远高于硅藻,与网采结果相反。甲藻物种数和丰度比例较往年明显增加,群集结构 与其他季节有明显差异。浮游植物细胞丰度在5 m层出现最大值。两个典型断面的浮游植物分布特征受到具齿原甲藻、骨条 藻和米氏凯伦藻共同影响。南部水域浮游植物群集多样性程度和物种均一性高于浮游植物密集区。应用典范性对应分析表明 春季环境因子中盐度、溶解氧与甲藻相关性较大,硅藻与pH 值和营养盐浓度关系更为密切。  相似文献   

6.
东海低氧区及邻近海域固氮蓝藻丰度与分布   总被引:1,自引:0,他引:1  
分别对2006年6月、8月和10月东海低氧区及邻近海域(26°N~34°N,120°E~126°E)进行综合调查,探讨了东海低氧区及邻近海域固氮蓝藻物种、丰度与分布变化特征。调查区蓝藻主要物种有铁氏束毛藻(Trichodesmium thiebautii)、汉氏束毛藻(Trichodesmium erythraeum)和红海束毛藻(Trichodesmium hildebrandtii),在个别区域检测到胞内植生藻(Richelia intracellu-laris),铁氏束毛藻为优势物种。8月蓝藻细胞丰度最大,藻丝体和细胞平均丰度为12.58×103和954.67×105cells/L,其次是10月,藻丝体和细胞平均丰度为44.08×103fikaments/L和68.37×105cells/L,最低为6月,藻丝体和细胞平均丰度为1.07×103/L和1.53×105cells/L。蓝藻主要分布在靠近外海受台湾暖流影响的海区,在靠近长江河口透明度较低的区域蓝藻丰度很低,甚至在河口门区未检测到蓝藻,垂直分布特征为主要分布在水深50m以上,丰度高值区域为表层和10m。环境因子中温度对蓝藻生长具有明显的影响,6月时温度与蓝藻丰度呈显著正相关。盐度与蓝藻丰度没有相关性。  相似文献   

7.
2006年秋季长江口及其邻近水域浮游植物群集   总被引:1,自引:0,他引:1  
赵冉  孙军  白洁 《海洋科学》2010,34(4):32-39
根据2006年11月在长江口及其邻近水域(30°30′N~32°30′N,121°E~123°30′E)39个测站采集的浮游植物水样研究了该水域浮游植物群集特征。调查区浮游植物以硅藻和甲藻为主,此外还有少量的金藻、蓝藻和绿藻。浮游植物细胞丰度介于0.13~59.69个/mL之间,平均为4.39个/mL,主要优势物种为圆海链藻Thalassiosira rotula和骨条藻Skeletonema spp.,调查区两个细胞丰度密集区分别出现在靠近口门以及外海水域。浮游植物细胞在20m层出现最大值。调查区两个典型断面的浮游植物分布特征分别由骨条藻和圆海链藻所刻画。固氮蓝藻铁氏束毛藻Trichodesmium thiebautii主要出现在调查区东部水域表层。根据浮游植物物种和细胞丰度进行聚类分析后,发现存在调查区东部与近岸2个浮游植物分区。  相似文献   

8.
作者基于2011年9月(丰水期)和2012年1月(枯水期)粤西近岸30米以浅海域的调查资料,分析该海域浮游植物的种类组成、优势种、丰度及其群落结构多样性。结果表明,调查海域共鉴定浮游植物4门41属116种,硅藻为最主要优势类群。丰水期与枯水期共有种类40种,物种相似性指数为34.48%,表明2个调查季节种类组成变化较大,存在明显的季节性差异。枯水期优势种仅1种,为金藻门(Chrysophyta)的球形棕囊藻(Phaeoecystis globosa),优势度高达0.496;丰水期优势种有4种,其中以硅藻门的旋链角毛藻(Chaetoceros curvisetus)优势度较高(0.249)。浮游植物丰度表现出时间和空间异质性,丰度总体呈现近岸站位高于离岸站位,此外,丰水期浮游植物丰度湛江沿岸站位高于其他调查站位,枯水期浮游植物丰度则由西南部向东北部递减,总体而言,枯水期浮游植物丰度比丰水期高。群落结构多样性为枯水期西南部海域明显低于东北部海域,丰水期站位间多样性无明显变化规律,相比之下,丰水期群落物种多样性水平相对较高。相关分析表明:浮游植物丰度与p H、悬浮物呈正相关,与丰水期水温和枯水期盐度呈负相关。  相似文献   

9.
根据2010年10月的调查数据,对衢山岛海域浮游植物的种类组成、优势种、丰度、多样性及其环境因子进行了分析。在本次调查期间,共采集到浮游植物7门181种,其中硅藻133种,占总种数的73.9%,为调查海域浮游植物群落的主要类群,且中肋骨条藻为绝对优势种;甲藻38种,占总种数的21.1%。该海域浮游植物的种类组成和细胞丰度具有明显的潮周期特性,体现为大潮期浮游植物种类数和细胞丰度明显高于小潮期;大、小潮期间浮游植物平均H′分别为0.65和1.10;由聚类分析发现,浮游植物不同群落间组成差异显著。衢山岛海域富营养化现象较为严重,大潮期间,无机氮及活性磷酸盐的平均浓度分别为0.81 mg/L和0.04 mg/L;小潮期间,无机氮及活性磷酸盐的平均浓度分别为1.04 mg/L和0.04 mg/L。  相似文献   

10.
2006年夏季长江口及其邻近水域浮游植物群集   总被引:5,自引:0,他引:5  
根据2006年8月在长江口及其邻近水域(30°30′N~32°30′N,121°E~123°E)39个观测站采集的浮游植物水样,研究了该水域浮游植物群集特征.调查区浮游植物以硅藻和甲藻为主,此外还有少量的金藻、蓝藻和绿藻.浮游植物主要优势物种为脆指管藻(Dactyliosolen fragilissima)和中肋骨条藻(Skeletonema costatum).浮游植物细胞丰度介于0.27~4830.09 cells·mL-1,平均为290.92 cells·mL-1,高值出现在调查区122°30′E~123°E水域,近岸细胞丰度较低.浮游植物细胞丰度的垂直分布特征是随水深增加先增大后减小,最大值出现在10m层.调查区两个断面细胞丰度由沿岸至冲淡水域呈增加趋势,但在调查区靠近外海一侧出现细胞丰度最低值.  相似文献   

11.
对辽宁省大伙房水库(1980-1987)和柴河水库(1981-1987)的水文、理化和生物数据,与这两座库同时间的不投饵网箱养殖的鲢、鳙鱼种的生长和产量进行回归分析。结果表明,7-8月的入库水量和出库水量、9月与6月间的水位差等参数同鲢,鳙均重及产量相关显著,用它们来估测大体鲢、鳙的生长与产量是可行的。  相似文献   

12.
基于BP神经网络的湖南镇水库叶绿素a浓度预测模型的研究   总被引:1,自引:0,他引:1  
以湖南镇水库2006-2007年间的监测资料为基础,利用插值和主成分分析法,运用BP人工神经网络方法构建预测模型,探求叶绿素a浓度与总氮、总磷、溶解氧等5项环境因子之间的关系,选出最佳预测模型,并对模型进行敏感度分析.结果显示:(1)BP神经网络模型对叶绿素a浓度预测值与实测值之间拟合程度良好,相关系数达到了0.95,...  相似文献   

13.
以1960~2001年共41 a的7月和8月西行进入南海海域的热带气旋样本为基础,采用遗传算法与神经网络相结合的方法,进行了热带气旋强度预报模型的预报建模研究.并根据相同的热带气旋个例,将这种遗传-神经网络热带气旋强度预报模型与气候持续法热带气旋强度预报方法进行对比分析,试验预报结果表明,遗传-神经网络方法具有更好的预报能力.  相似文献   

14.
The Luzon Strait is the main impact pathway of the Kuroshio on the circulation in South China Sea (SCS). Based on the analysis of the 1997–2007 altimeter data and 2005–2006 output data from a high resolution global HYCOM model, the total Luzon Strait Transport (LST) has remarkable subseasonal oscillations with a typical period of 90 to 120 days, and an average value of 1.9 Sv into SCS. Further spectrum analysis shows that the temporal variability of the LST at different depth is remarkable different. In the upper layer (0–300 m), westward inflow has significant seasonal and subseasonal variability. In the bottom layer (below 1 200 m), eastward outflow exhibits remarkable seasonal variability, while subseasonal variability is also clear. In the intermediate layer, the westward inflow is slightly bigger than the eastward outflow, and both of them have obvious seasonal and subseasonal variability. Because the seasonal variation of westward inflow and eastward outflow is opposite, the total transport of intermediate layer exhibits significant 50–150 days variation, without obvious seasonal signals. The westward Rossby waves with a period of 90 to 120 days in the Western Pacific have very clear correlationship with the Luzon Strait Transport, this indicates that the interaction between these westward Rossby waves and Kuroshio might be the possible mechanism of the subseasonal variation of the LST.  相似文献   

15.
The wintertime ratio of inorganic dissolved nitrogen to phosphorus (DIN/DIP) in the surface waters of the Baltic Sea is typically below the molar Redfield ratio of 16, which expresses the presence of an excess inorganic dissolved phosphorus (eDIP) reserve compared to DIN. We assessed the role of the vernal phytoplankton bloom period (VPBP) in the consumption of the potential wintertime eDIP reserve, and the role of eDIP after the VPBP as a nutritional agent for the summertime growth of the cyanobacteria in the Baltic Sea. We employed a high-frequency dataset collected by the unattended monitoring systems on board merchant ships. The dataset encompasses the Baltic basins from the Arkona Basin to the Western Gulf of Finland and the time period from 1993 to 2009. All the observed values of the wintertime DIN/DIP ratio were below the molar Redfield ratio; the ratio showed a declining trend during the study, suggesting that there is a pronounced wintertime stock of the potential eDIP in the waters of the Baltic Sea, and that this stock has lately increased in magnitude. The VPBP took up excessively DIP to DIN than calculated according to the uptake in the molar Redfield ratio, thus reducing the potential eDIP reserve. On average, 59% of the potential eDIP reserve was left in the water after the VPBP as eDIP. eDIP was typically exhausted in the time frame early June–early July, matching well the timing of the appearance of cyanobacteria in substantial numbers in the water-column. eDIP clearly fueled the cyanobacterial growth in every instance in which it was possible to clarify their relationship. The cyanobacteria must still have another DIP source than eDIP to form extensive late-summer blooms, except in the western Gulf of Finland, where eDIP remained detectable up to early August. The annual role of eDIP for cyanobacterial growth depends greatly on the weather of late spring and early summer: this may sometimes launch the cyanobacterial growth much earlier than is usually expected.  相似文献   

16.
The dynamics in the transition zone between the North Sea and Baltic Sea are analyzed here using data from a 22-year-long climatic simulation with a focus on the periods 1992–1994 and 2001–2003 when two recent major inflow events occurred. Observations from gauges and in situ measurements are used to validate the model. Parameters, which cannot be easily measured, such as water and salt transports through straits, have been compared against similar previous estimates. The good performance of simulations is attributed to the finer resolution of the model compared to earlier set ups. The outflow in the Kattegat, which is an analogue of the tidal outflows, tends to propagate to the North over the shallows without showing a substantial deflection to the right due to the Earth's rotation. The inflow follows the topography. The different inflow and outflow pathways are explained as a consequence of the specific combination of bathymetry, axial and lateral processes. The circulation in Kattegat is persistently clockwise with an eastern intensification during inflow and a western one during outflow regimes. The tidal wave there propagates as Kelvin wave, keeping the coast on its right. The flows in the two main straits reveal very different responses to tides, which are also highly asymmetric during inflow and outflow conditions. The circulation has a typical two-layer structure, the correlation between salinity and velocity tends to increase the salt transport in the salinity conveyor belt. The transversal circulation in the entrance of the Sound enhances the vertical mixing of the saltier North Sea water. The long-term averaged ratio of the water transports through the Great Belt and the Sound is ∼2.6-2.7 but this number changes reaching lower values during the major inflow in 1993. The transports in the straits are asymmetric. During inflow events the repartition of water penetrating the Baltic Sea is strongly in favor of the pathway through the Sound, which provides a shorter connection between the Kattegat and Baltic proper. The wider Great Belt has a relatively larger role in exporting water from the Baltic into the North Sea. A demonstration is given that the ventilation of the Baltic Sea deep water is not only governed by the dynamics in the straits and the strong westerly winds enhancing the eastward propagation of North Sea water (a case in 1993), but also by the clockwise circulation in the Kattegat acting as a preconditioning factor for the flow-partitioning.  相似文献   

17.
吕宋海峡纬向海流及质量输送   总被引:30,自引:6,他引:24  
分析和计算了吕宋海峡PR21断面最近海洋调查的部分CTD资料和ADCP资料,再一次证明吕宋海峡常年存在纬向流。但对于天气尺度而言,该流型是多变的。根据高分辨率的海洋环流数值模式4a(1992~1996年)海平面高度(SSH)的输出值,运用地转关系估计了吕宋海峡纬向流的月平均值。研究表明;通过海峡流入、流出南海纬向流的深度一般达到500m左右,200m以上流速较大,平均流速为50cm/s,最大时达80cm/s以上。500m以下的纬向地转流流速较小,通常小于10cm/s.由大洋进入海峡的入流位置位于海峡的中部和南部,月平均入流最大值出现在11月,为50cm/s.位于海峡的北部和南部上层海洋的月平均出流,最大流速亦出现在11月,也为50cm/s,这与秋季北赤道流分叉位置最北(15°N),春季分叉位置最南(14°N)有关。上层流入、流出海峡的流量的月平均值分别约为10×106m3/s和5×106m3/s.当东北季风盛行时(从10月到翌年2月),流入海峡的流量远大于流出海峡的流量,两者的差可达8×106m3/s,而在其他季节两者的差仅为3×106m3/s.这说明东北季风盛行时,会有较多的水从南海南?  相似文献   

18.
The Bras d'Or Lakes are a system of interconnecting basins open through two narrow channels to the Sydney Bight at the mouth of the Gulf of St Lawrence. Hydrographic surveys between 1972 and 1974 showed that surface waters can warm by more than 10 °C from May to July and that horizontal salinity differences of up to 10 psu can exist between Sydney Bight (30 psu) and the innermost regions of the Lakes. Using the data from May and June 1974 to derive horizontal and vertical exchanges, a simple budget model has been set up consisting of two or three layers in each of nine separate regions. The model has a bottom inflow from Sydney Bight, deep inflow through the narrow channels to other basins and a surface outflow. The exchanges agree reasonably well with estimates derived from available current meter data. The model's predicted temperatures and salinities for July 1974 had rms errors of about 1·5 °C and 0·82 psu, respectively. The dissolved oxygen concentrations in four of the more isolated basins are similar to those calculated from the model, giving support to the derived circulation.  相似文献   

19.
东海与邻近海域水、热、盐通量的季节变化研究   总被引:1,自引:0,他引:1  
本文基于高分辨率的区域海洋数值模式对东海及邻近海域进行温、盐、流的数值模拟,模拟结果与实测结果拟合较好。结果表明:东海与邻近海域的水交换过程具有显著的季节变化特征。从流量的角度看,台湾海峡、台湾-西表岛之间水道和西表岛-冲绳岛之间水道是外海水流入东海的3个主要水道,而冲绳岛-奄美大岛、吐噶喇海峡、大隅海峡、济州岛东部和黄东海断面是海水流出东海的水道;其年平均体积输运值分别为1.06×106 m3/s、20.49×106 m3/s、3.20×106 m3/s、-0.92×106 m3/s、-20.59×106 m3/s、-0.30×106 m3/s、-2.37×106 m3/s和-0.37×106 m3/s(向内为正)。对比发现,东海与邻近海域之间各水道的体积、热量和盐量输运均具有相似的季节变化趋势,其最大值往往出现在夏季(7月或8月),最小值往往出现在冬季(1月或2月)。从7月到11月整个东海是流量净流出的过程,而从12月到翌年6月是流量净流入的过程,全年流量基本上保持平衡状态。东海终年存在向黄海的净输入,其体积、热量和盐量的年平均输运值分别为0.37×106 m3/s,0.027×1015 W和12.7×106 kg/s。  相似文献   

20.
东海混浊海域悬沙浓度的三维数值模拟及与观测的比较   总被引:1,自引:1,他引:0  
借助ECOMSED模式进行了东海混浊水海域三维悬浮泥沙输运的数值模拟,其中水动力模拟中考虑了潮汐,海流(包括黑潮,长江径流等)及风场的作用,输运模型中考虑了粘性泥沙的絮凝、粘性和非粘性泥沙的再悬浮等过程。另外,在沉积输运模式中,增加了波浪的作用,使沉积输运模拟更完善,并与2006年8月份在长江口外海域获得的走航断面及定...  相似文献   

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