三峡水库香溪河库湾夏季水华调查

以三峡水库支流香溪河为研究对象,以2011年夏季的采样数据为基础,比较分析了水华前后支流库湾营养盐和叶绿素a的时空分布规律及其相关性。结果表明,2011年6月21—29日,香溪河暴发了显著的藻类水华,叶绿素a峰值达到125.8 mg·m-3。相关分析表明,水华过程显著影响可溶性无机N、P的空间分布,营养盐空间分布从中游高、河口低,转变为从河口至上游递减,并且在水华区域锐减;长江干流较高的营养盐本底值增大了支流库湾水华的风险;高营养盐背景值的长江干流水体在香溪河库湾的潜出位置是水华最严重的区域;干流水体对库湾表层的营养盐补给作用是影响库湾水华生消的关键因素。     

香溪河库湾春季叶绿素a 浓度动态及其影响因子分析

2005年3月至4月,对三峡水库香溪河库湾的叶绿素a动态及其与TN、TP等环境因子的关系进行了研究。结果表明,从香溪河库湾下游到上游,叶绿素a存在明显的水平分布。在时间分布上,3月17日暴发一次大规模的水华,4月份水华的暴发有一个明显的平面推移的过程。叶绿素a浓度与TN、TP之间存在着一定的负相关关系,TN与叶绿素a浓度的相关性较显著。香溪河库湾极可能是N限制型水体,而不受P限制。叶绿素a与透明度存在反双曲线关系,与溶解氧呈显著正相关关系。     

香溪河水系附石藻类的时空动态

香溪河系长江三峡水库湖北库区内第一大支流.对香溪河2005年7月—2006年6月干流及主要支流上12个样点的附石藻类进行调查,共观察到藻类218种,其中硅藻183种、绿藻24种、蓝藻10种、黄藻1种,硅藻门的线形曲壳藻为绝对优势种.其物种丰富度和Shannon-Wiener多样性指数时空动态差异显著（或接近显著）,总平均值分别为32和154.附石藻类密度和叶绿素a含量年总平均值分别为8.75×10.9 cells·m^-2和14.62 mg·m^-2.不同样点的藻类密度和叶绿素a含量差异显著,其中古夫河支流最高,九冲河支流最低,两者相差一个数量级; 不同季节附石藻类密度和叶绿素a含量差异不显著(P>0.05),但均表现出冬春季高、夏秋季低的趋势.附石藻类密度及叶绿素a含量与海拔及水流流速呈显著负相关,而与总氮呈正相关.     

在不同蓄水位下三峡库区春季水华特征及趋势分析

基于2004—2015年三峡库区支流春季水华的监测数据,开展了三峡库区不同蓄水位下春季水华特征及趋势分析。结果表明:总共有26条支流发生春季水华,香溪河为水华发生概率最高的支流。水华藻类优势种主要是硅藻和甲藻,甲藻水华出现的概率随着蓄水位的增加而增加,但是在持续几年175 m蓄水之后,甲藻水华出现的频率下降,硅藻水华出现的频率增加。在175 m蓄水之前,水华发生期藻类密度、叶绿素a含量及水体营养盐水平相对较低,此后都有了较高的提升,但是在持续几年175 m蓄水之后,藻类密度、叶绿素a浓度以及营养盐浓度都有下降趋势。对藻密度及叶绿素a含量与主要环境因子进行主成分分析(Principal components analysis)发现,藻密度和叶绿素a与总磷、总氮、高锰酸盐指数聚类一簇,藻密度、叶绿素a浓度与总磷、溶解氧、高锰酸盐指数显著正相关。在蓄水之后,三峡库区支流营养水平有所增加,随着蓄水位的增加,三峡库区支流断面的平均流速降低,在合适的温度下,三峡库区支流水华易发生。     

香溪河流域水体环境因子研究

基于香溪河及其三大支流古夫河、高岚河与九冲河的8年监测数据,对该流域水体的环境因子及其时空动态进行了比较分析。结果显示,香溪河流域的水体呈中性偏弱碱性,属于中等硬度水,水体溶解氧丰富,还原性物质以及氯化物水平不高,具有较强的缓冲能力。多数环境因子具有明显的季节变化,而年际变化规律不显著。香溪河流域水体的主要营养元素氮含量较高,并以有城镇影响的古夫河为最;高岚河由于受到生活污水与农业活动的影响,水质相对较差;香溪河的磷污染严重;森林覆盖率较高的九冲河的水质最佳。在香溪河流域,氮主要以面源污染的方式进入河道,而香溪河的磷则主要以点源污染的方式进入河道。水土流失是香溪河流域面源污染的主要途径,磷矿和磷化工厂的排污则是磷点源污染的主要途径。从保护三峡水库香溪河库湾的生态学角度考虑,应重点控制香溪河磷的点源污染。     

三峡库区古夫河着生藻类分布与水质因子的关系

于2010年12月至2011年12月,对位于长江三峡库区内的湖北省兴山县古夫河着生的藻类和水体共采样10次,共鉴定出着生藻类28属,检测水质指标12项。对水质变量进行因子分析,根据特征值大于1的原则选取4个主成分,第一主成分主要代表总氮（TN）和硝酸盐氮（NO3--N）,第二主成分主要代表pH和化学需氧量（CODCr）,第三主成分主要代表磷酸盐磷（PO34--P）、总磷（TP）和氨氮（NH4＋-N）,第四主成分主要代表电导率（Cond）和总有机碳（TOC）。将提取的9项主要水质因子与着生藻类重要属进行典型对应分析（CCA）,结果可见,古夫河主要水质因子与着生藻类类群分布相关性大小为：CODCr〉pH〉TN〉NO3--N〉TOC〉TP〉PO34--P〉Cond〉NH4＋-N。Monte Carlo显著性检验表明,CODCr和pH对古夫河着生藻类物种组成及空间分布的影响最大,其次为TN、NO3--N和TOC。pH与CODCr呈极强的负相关关系,古夫河着生藻类大多数类群均与CODCr表现出正相关关系,仅胶毛藻属（Chaetophora）倾向低CODcr和偏碱性的环境。TN和NO3--N有很强正相关性,而两者均与TOC有强负相关,它们将古夫河着生藻类大体上分为两类,即亲碳元素的类群和亲氮元素的类群。TP通常是河流生态系统中的限制性营养因子,但在古夫河流域中并不是影响着生藻类物种分布的主要水质因子。     

香溪河大型底栖无脊椎动物空间分布

2005年7月至2006年6月,通过对大型底栖无脊椎动物的量化检测,对三峡水库湖北库区最大河流香溪河的大型底栖无脊椎动物空间分布进行了研究.结果表明：四节蜉、高翔蜉、短尾石蝇为香溪河水系大型底栖动物优势类群;香溪河各支流间生境特征及大型底栖无脊椎动物群落结构差异较大;功能摄食类群密度相对丰度的变化能够反映不同的栖境特征.对生物多样性指数及优势类群耐污值的比较表明,大型底栖动物栖境为九冲河最好,香溪河干流次之,高岚河和古夫河较差.典型对应分析表明：铵态氮对香溪河大型底栖动物群落结构影响显著;pH值、浊度、水深、二氧化硅、电导和碱度对九冲河大型底栖动物群落结构影响显著;浊度对高岚河大型底栖动物群落结构影响显著;铵态氮和硝酸盐氮对古夫河大型底栖动物群落结构影响显著.     

钱塘江干流杭州段水体叶绿素a浓度及与环境因子的关系

2006年1月至2007年12月,对钱塘江干流杭州段水体的叶绿素a时空分布及其与环境因子的关系进行研究.结果表明钱塘江干流杭州段的叶绿素a浓度时间差异显著,空间差异不显著.叶绿素a浓度呈现夏秋季节高、冬春季节低的规律.叶绿素a浓度与温度呈显著正相关,叶绿素a与透明度在不同范围内表现出不同的相关关系,叶绿素a与TN、TP之间的相关关系在不同江段有所差异.钱塘江干流杭州段总氮和总磷浓度均很高,足够满足藻类生长需要;氮磷比较低,基本在8～30之间,说明氮磷含量可能不是钱塘江藻类生长的限制因子.     

香溪河库湾枝角类的种类组成及垂直分布

枝角类在水库生态系统的物质循环和能量流动过程中具有重要的作用, 有关水库枝角类的研究在水库水生生物研究中历来备受重视。枝角类在深水水体中具有垂直分布的特性, 生物和非生物因素影响着包括枝角类在内的浮游动物垂直分布及垂直分布的时空变化。香溪河河口至兴山峡口段在2003 年6 月三峡水库蓄水后被没,形成香溪河库湾。因受干流库区的水体顶托, 库湾水体流速缓, 更新时间长, 容易产生富营养化现象, 香溪河库湾2004 年春季就有藻类异常繁殖现象发生。       

香溪河大型底栖无脊椎动物群落结构季节动态研究

研究香溪河大型底栖无脊椎动物群落结构和季节动态特征情况,发现高翔蜉、萝卜螺、河蚬、湖沼股蛤、四节蜉为香溪河水系优势分类单元,各季节底栖动物优势种的组成存在显著差异。冬季的生物密度、生物量、生物多样性指数显著高于其他季节,说明冬季的河流生境最适宜大型底栖无脊椎动物生存。香溪河刮食者丰度最高,撕食者最低,表明香溪河着生藻类丰富;固着型底栖动物在香溪河底栖类群中丰度最高,说明香溪河河流流速较快,生境更适宜固着型动物栖居。不同季节环境因子对大型底栖动物群落结构有显著影响。     

Seasonal changes in composition and biomass of epilithic algal floras of a chalk stream and a soft water stream with estimates of production

Microscopic epilithic algae in the River Itchen at Otterbourne near Southampton and in the Ober Water in the New Forest were studied during 1984 and 1985. The River Itchen rises from chalk springs and has a steady pH near 8.2 and a mean alkalinity of 236 mg HCO₃ 1^–1; at the study site the river is about 16 m wide and 20 cm deep, with a mean flow rate of 0.33 m s^–1 and a discharge ranging through the year between 0.34 and 2.46 m³ s^–1. The Ober Water, which drains sands and gravels, has a pH between 6.9 and 7.2 and a mean alkalinity of about 50 mg HCO₃ 1^–1; at the study site it is about 6 m wide, with a mean flow rate of 0.27 m s^–1 and a discharge ranging through the year between 0.08 and 1.0 m³ s^–1.Epilithic algae removed from the pebbles that form the major part of the beds of both streams show seasonal changes in abundance and composition. Diatoms peaked in April/May and dominate the epilithic flora in both streams, comprising 70–95% of all algal cells; highest numbers of chlorophytes occurred in summer and cyanophytes increased in autumn. The species composition of the epilithic flora in the two streams was different, as was the population density; algal cell numbers ranged between 500 and 7000 cells mm^–2 of stream floor in the River Itchen and between 8 and 320 cells mm^–2 of stream floor in the Ober Water. The chlorophyll a content of epilithic algae in the River Itchen ranged between 115 and 415 mg m^–2 of stream floor, representing an annual mean biomass of about 8 g m^–2, whereas in the Ober Water a chlorophyll a content of 2.2 to 44 mg m^–2 of stream floor was found, representing an annual mean biomass of about 1 g m^–2. Cautious estimates of the annual production of epilithic algae in these streams suggest a value of about 600 g organic dry weight m^–2 in the River Itchen and about 75 g m^–2 in the Ober Water.     

Exotic crayfish in a brown water stream: effects on juvenile trout, invertebrates and algae

SUMMARY 1. The impact of the introduced omnivorous signal crayfish (Pacifastacus leniusculus) on trout fry, macroinvertebrates and algae was evaluated in a brown water stream in southern Sweden using in situ enclosures. We also examined the gut content of all surviving crayfish in the enclosures. Two crayfish densities in addition to a control without crayfish were used in replicate enclosures (1.26 m²) in a 1‐month experiment. Additionally, 20 trout fry (Salmo trutta) were stocked in each enclosure to assess the effects of crayfish on trout survival and growth. 2. Detritus was the most common food item in crayfish guts. Animal fragments were also frequent while algae and macrophytes were scarcer. Crayfish exuviae were found in crayfish guts, but the frequency of cannibalism was low. 3. Trout survival in enclosures was positively related to water velocity but was unaffected by crayfish. 4. Total invertebrate biomass and taxon richness were lower in crayfish treatments. The biomass of all predatory invertebrate taxa was reduced but only three of six non‐predatory taxa were reduced in the crayfish treatments. 5. Epiphytic algal biomass (measured as chlorophyll a, on plastic strips) was not related to crayfish density, whereas the biomass of epilithic algae (measured as chlorophyll a) was enhanced by high water velocity and high crayfish density. The latter was possibly mediated via improved light and nutrient conditions, as active crayfish re‐suspend and/or remove detritus and senescent algal cells during periods of low water velocity. 6. We conclude that the introduced signal crayfish may affect stream communities directly and indirectly. Invaded communities will have reduced macroinvertebrate taxon richness and the signal crayfish will replace vulnerable invertebrate predators such as leeches. In streams that transport large amounts of sediment or organic matter, a high density of crayfish is likely to enhance benthic algal production through physical activity rather than via trophic effects.     

Seasonal variation in biomass and photosynthetic activity of epilithic algae on a rock at the upper littoral area in the north basin of Lake Biwa, Japan

Vertical distributions of biomass and the photosynthetic activity of epilithic algae were observed seasonally with regard to their physical and chemical parameters along a rocky shoreline of the upper littoral area in the north basin of Lake Biwa. Chlorophyll a amounts in epilithic algae showed a marked change with depth from spring to early summer. The algal biomass showed higher values on the lower part of a large rock in early spring, and gradually increased on the upper part as a result of the growth of Spirogyra sp., a filamentous Chlorophyceae. This growth seems to be associated with a rise in water temperature, with the biomass at the upper depths seeming to be affected by a hydraulic disturbance. The standing crop of epilithic algae showed a maximum value in June and declined to a minimum in August because of the corresponding proliferation or disappearance of Spirogyra as well as changes in the water level. The maximum value of the assimilation number calculated from the potential photosynthetic rate of epilithic algae was obtained at the lower depths in June when Spirogyra grew vigorously. Appreciably high assimilation numbers were also observed in summer and fall, although chlorophyll a amounts were low. The present study is the first in a series to clarify the contribution of epilithic algae on rocky areas to productivity throughout the entire littoral ecosystem.     

长江口冬季和春季浮游植物的粒级生物量

根据2005年2月28日—3月10日和5月30日—6月4日在长江口及其邻近水域进行的多学科综合外业调查,报道了冬季和春季浮游植物粒级生物量的空间分布和组成特征,并探讨了影响浮游植物粒级生物量的环境因子.结果表明：冬季长江口及其邻近水域表层叶绿素a平均浓度为1.28 mg·m^-3,高值区集中在口门附近;小粒径浮游植物（<20 μm）对浮游植物生物量的贡献率为66.7%,但在冲淡水区大粒径浮游植物（>20 μm）占据优势.春季长江口及其邻近水域表层叶绿素a浓度大幅增加,口门内、外的平均值分别为0.67和6.03 mg·m^-3,122.5°—123.0° E间水域因水华爆发出现显著的叶绿素a高值区;小粒径浮游植物对浮游植物生物量的贡献高达83.5%,其优势在水华区尤为明显.典型站位浮游植物粒级生物量的垂向分布显示,2种粒径浮游植物叶绿素a浓度的差异随水深增加而减小,至底层二者浓度相当.根据所获的环境因子资料,盐度和营养盐是影响长江口及其邻近水域浮游植物粒级生物量分布和组成的重要环境因子.     

Epilithic Algae Distribution Along a Chemical Gradient in a Naturally Acidic River, Río Agrio (Patagonia, Argentina)

The epilithic algae distribution along a pH gradient and the relationship between the chemical gradient and biomass development were studied in Río Agrio, a naturally acidic river located in Patagonia (Argentina). The epilithic community was monitored during the summer of three consecutive years in sites located above and below the entrance of tributaries. The epilithic community showed differences between sites based on the chemical composition of the water and the precipitates that appear on the streambed of the river. The lowest biomass, diversity, and number of species were found at the most extreme part of the river in terms of pH (ca. 2) and element concentrations. Euglena mutabilis was the dominant species in this section of the river. As pH increased (ca. 3), the community changed to be dominated by filamentous green algae (Ulothrix spp., Mougeotia sp., Klebsormidium sp.) showing luxuriant growths in terms of biomass. With the inflow of a neutral tributary, the pH of Río Agrio increased above 3, and the precipitates of orange-red iron hydroxides appeared. The algal community was not affected by these precipitates or the low P concentrations, along the next 30 km of river downstream from this site. The apparent physical stress that the precipitates impose on algae is in fact a dynamic reservoir of P because diel cycle of Fe could be promoting precipitation and redissolution processes that binds and releases P from these precipitates. Where the pH increased above 6, precipitates of aluminum hydroxides appeared. At this site, the epilithic biomass and density decreased, some algae species changed, but the diversity and the number of species in general remained consistent with the upstream values. The physical stress of the Al precipitates on the algae is added to the chemical stress that represents the sequestering of P in these precipitates that are not redissolved, resulting P a limiting nutrient for algae growth.     

Local disturbance history affects patchiness of benthic river algae

1. Recent research has shown that high‐flow events in streams leave a small‐scale mosaic of bed patches that have experienced scouring, sediment deposition (fill), or remained stable. Few studies have investigated if this ‘local disturbance history’ contributes to the patchy distribution of benthic organisms in streams and rivers. 2. In the present research, we demonstrate that local disturbance history in a mid‐sized river can have both short‐ and long‐term effects on epilithic algae. Chains buried vertically in the substratum of the river bed (236 in a 800‐m reach) indicated that two floods (return periods ≤1 year) caused a mosaic of bed patches with different disturbance histories. Once after the first and twice after the second flood, we sampled epilithic algae (mainly diatoms) in replicate patches that had been scoured, filled, or remained stable during the respective event. Algal biomass and cell density per substratum area were determined. 3. Three months after the first flood, algal biomass, total diatom density, diatom taxon richness, and densities of six of nine most common taxa were highest in fill patches. Six days after the second flood, biomass was highest in stable patches, indicating a refugium function of these patches. The refugium patches consisted of average‐sized stones, in contrast to previous studies of flood refugia for benthic algae in which these refugia were always large and/or immobile substrata. Four weeks after the second flood, diatoms tended to be most abundant in scour patches. With one exception, these differences between patch types could not be attributed to differences in local near‐bed current velocity or water depth. 4. The effects of disturbance history were more complex than a simple refugium function of stable patches because algal patterns changed with time since the last disturbance, possibly depending on the successional state of the algal mats.     

The influence of floodplain habitat on the quantity and quality of riverine phytoplankton carbon produced during the flood season in San Francisco Estuary

Primary productivity, community respiration, chlorophyll a concentration, phytoplankton species composition, and environmental factors were compared in the Yolo Bypass floodplain and adjacent Sacramento River in order to determine if passage of Sacramento River through floodplain habitat enhanced the quantity and quality of phytoplankton carbon available to the aquatic food web and how primary productivity and phytoplankton species composition in these habitats were affected by environmental conditions during the flood season. Greater net primary productivity of Sacramento River water in the floodplain than the main river channel was associated with more frequent autotrophy and a higher P:R ratio, chlorophyll a concentration, and phytoplankton growth efficiency (α^B). Total irradiance and water temperature in the euphotic zone were positively correlated with net primary productivity in winter and early spring but negatively correlated with net primary productivity in the late spring and early summer in the floodplain. In contrast, net primary productivity was correlated with chlorophyll a concentration and streamflow in the Sacramento River. The flood pulse cycle was important for floodplain production because it facilitated the accumulation of chlorophyll a and wide diameter diatom and green algal cells during the drain phase. High chlorophyll a concentration and diatom and green algal biomass enabled the floodplain to export 14–37% of the combined floodplain plus river load of total, diatom and green algal biomass and wide diameter cells to the estuary downstream, even though it had only 3% of the river streamflow. The study suggested the quantity and quality of riverine phytoplankton biomass available to the aquatic food web could be enhanced by passing river water through a floodplain during the flood season.     

基于附石藻类生物完整性指数对汝溪河水生态系统健康的评价

以三峡库区支流-汝溪河自然河段为研究区域,调查了自然河段内9个样点的附石藻类群落和水环境理化特征,并在此基础上应用生物完整性评价指数（Index of Biotic Integrity,IBI）,对汝溪河水生态系统进行健康评价。结果表明,汝溪河自然河段附石藻类群落结构具有明显的空间和时间异质性,驱动附石藻类群落结构形成的水环境因子为电导率、浊度、硝态氮和溶解氧。IBI结果表明,上游生物完整性较高;中下游和下游生物完整性较差;枯水期生物完整性较高,而平水期和丰水期生物完整性较低。由此可见,汝溪河自然河段生物完整性一般,表明汝溪河水生态系统已处于亚健康程度。