高矿化度沙漠湖泊水体的光学特性

沙漠湖泊水体和东部大型湖泊如太湖等存在较大差异.为深入研究沙漠湖泊水体的光学特性,利用腾格里沙漠月亮湖实测水面ASD高光谱数据和同步采集的水样,对水体矿化度与叶绿素a、DOC、悬浮物的含量进行相关性分析,比较沙漠湖泊水体和其它水体的黄色物质、浮游植物、非藻类悬浮物吸收特征光谱,探讨不同波段中水深和矿化度对水体反射率的影...     

低湿洼地鱼塘中异养细菌的矿化作用

对黄淮海平原低湿洼地鱼塘中异常细菌的矿化作用进行了初步研究,结果表明：（１）鱼塘水体中异养细菌的呼吸强度与鱼塘水体中的有机物质含量及温度密切相关;（２）鱼塘水体中异养细菌的生物量表现出明显的季节性变化;异养细菌的生物量在表层水及底层水之间的差异不明显。（３）鱼塘水体中异常细菌分解有机物质的动力学特点如下：开始时,鱼塘水体中有机物质的转化较少,随温度的增高及异养细菌生物量的增加,水体中的矿化作用逐渐     

Lee生物光学模型在不同水体组分特性下的适用性

辐射传输模型和生物光学模型均可用于模拟水体遥感反射率.前者模拟精度高,但计算复杂.不利于水质参数的反演;后者简便易反演,但在浑浊水体中的模拟精度还有待进一步检验.本文通过设计大量不同组分浓度组成的水体,以辐射传输模型(即Hydrolisht模型)模拟结果为真值,对生物光学模型(即Lee模型)模拟二类水体遥感反射率的精度...     

养殖污染水体-沉积物中磷的化学行为

通过受猪场污水影响的池塘和鱼塘水生生态系统中表层水。沉积物的磷含量、磷吸附能力比较,了解猪场污水、鱼塘养殖对表层水。沉积物系统磷行为的影响。结果表明,猪场污水排放和鱼塘养殖都会明显增加水体中溶解性反应磷（DRP）和溶解性有机磷（DOP）的含量,从DRP、DOP、PP3种形态磷在总磷中所占的比例来看,DRP是水体中主要增加的磷含量。猪场污水排放对水体中磷的增加作用比鱼塘养殖更剧烈一些,猪粪是水体中磷的主要来源。但是猪场污水排放对沉积物中不同形态磷含量的影响不明显。这可能与水体中磷的存在形态和转化时间有关。鱼塘养殖增加了沉积物中有机质、Fe-P、AI-P和总无机磷含量,增加了沉积物对磷的最大吸附容量,但是对磷的吸附能力却有所降低,进而增加了沉积物中磷向上覆水释放的可能。     

气候变暖和营养水平对洱海浮游植物的长期影响(1980-2009年)

气候变暖下湖泊富营养化进程是近年研究热点之一.本文对1980-2009年期间洱海富营养化进程研究发现,水体总磷、总氮与气温均呈升高趋势.气温、水体总磷和总氮均能显著促进浮游植物增长.统计分析表明,气温对浮游植物增长的促进作用不受水体总氮、总磷的影响;水体总磷对浮游植物增长的促进作用不受气温的影响,受水体总氮的影响;水体总氮对浮游植物增长的促进作用不受气温和水体总磷的单独影响,受它们共同的影响.因此,气候变暖与营养水平的增加共同促进了洱海的富营养化进程.     

渍涝洼地鱼塘中浮游动物的变化

1987—1989年对山东省禹城渍涝洼地新开鱼塘水体中浮游动物进行了调查。1987、1988、1989年成鱼养殖期间共检出浮游动物种类分别为29、34、52种,平均数量为11911、39366.1、77889.2个/L,平均生物量为5.145、5.7675、9.6285mg/L。1988、1989年,鱼塘水体中浮游动物的数量高峰在7月。新开鱼塘养鱼前,只检出5种。数量为600个/L,生物量为0.0585mg/L。养鱼后三年来,鱼塘水体中浮游动物种类、数量及生物量的逐年增加,表明了新开鱼塘富营养化的演变程度。鱼塘施肥前后,水体中原生动物与轮虫的数量均有明显变化,其中原生动物变化更为明显。     

渍涝洼地鱼塘中浮游动物的变化

1987-1989年对山东省禹城渍涝洼地新开鱼塘水体中浮游动物进行了调查。1987、1988、1989年成鱼养殖期间共检出浮游动物种类分别为29、34、52种,平均数量为11911、39366.1、77889.2个/L,平均生物量为5.145、5.7675、9.6285mg/L。1988、1989年,鱼塘水体中浮游动物的数量高峰在7月。新开鱼塘养鱼前,只检出5种。数量为600个/L,生物量为0.0585mg/L。养鱼后三年来,鱼塘水体中浮游动物种类、数量及生物量的逐年增加,表明了新开鱼塘富营养化的演变程度。鱼塘施肥前后,水体中原生动物与轮虫的数量均有明显变化,其中原生动物变化更为明显。     

长春市石头口门水库颗粒物光谱吸收特性

针对东北地区水体,以长春市重要水源地石头口门水库为例,分别于2008年6月13日和9月23 日对该水库进行了水体颗牲物吸收特性研究.结果显示:2008年6月水库悬浮物含量高于9月,而叶绿素a含量低于9月:总颗粒物的吸收光谱曲线类似于非色素颗粒物,非色素颗粒物吸收对其的贡献明显大于浮游植物色素,9月份浮游植物吸收对其的贡献略有增加,吸收曲线在440nm左右能明显看到浮游植物引起的吸收峰;非色素颗粒物在440nm的吸收系数与悬浮物浓度存在较好的函数关系,而与叶绿素a浓度的相关性较弱;浮游植物色素吸收系数较低,色素组成中叶绿索a占主导地位,浮游植物在440nm和675nm的吸收系数与叶绿素a含量均存在较好的指数函数关系;6月浮游植物比吸收系数在440nm和750nm的均值分别为0.0483m2/mg和0.0263m2/mg,而9月份的均值分别为0.0337m2/mg和0.01 87m2/mg.     

云南高原湖泊有色可溶性有机物和颗粒物光谱吸收特性

云南高原湖泊是我国湖泊分布最密集的五大湖群之一,不但湖泊数量众多而且类型多样.由于湖泊所处位置海拔较高,容易受只益增强UV-B辐射影响.通过对云南高原34个湖泊有色可溶性有机物和颗粒物吸收测定,分析其光谱吸收特性及对总吸收的贡献,有利于深刻理解紫外辐射在高原湖泊内衰减.不同湖泊间CDOM吸收差异明显,其大小与水体营养盐状况相关,CDOM吸收系数与水体总氮存在显著正相关.增加背景项的指数函数模型能最好模拟CDOM光谱吸收.除在浮游植物浓度非常高的杞麓湖、听湖、星云湖,颗粒物吸收系数在675nm附近存在一个吸收蜂外,其它湖泊总颗粒物光谱吸收大致随波长的增加吸收系数逐渐降低,呈现非色素颗粒物光谱吸收特征,整体上颗粒物吸收以非色素颗粒物为主.CDOM对总吸收的贡献主要集中在600nm以下波长,尤其是400nm以下的紫外波段,其在紫外波段(350-400nm)的贡献明显要大于光合有效辐射波段(400-700nm)(ANOVA,P<0.001).特别对于透明度SD≥1.0的清澈型湖泊,CDOM吸收对紫外辐射衰减的贡献更大,其吸收很大程度上决定了紫外辐射的影响深度.     

基于浓缩法的浮游植物定量数据稳定性与可靠性分析

浮游植物是水生生态系统中重要的初级生产者,相对准确地定量它们的数量是进一步进行水质评价和生态功能分析的基础.通过采集处于不同营养状态的水库和不同处理的围隔中的浮游植物,研究影响浓缩法定量浮游植物的因素,了解如何通过浓缩法来合理地定量浮游植物.分析浓缩倍数、样品的显微镜计数量、水体营养状态对浮游植物丰度、生物量及群落多样性等定量参数稳定性的影响,同时比较单个不同水体中重复(或平行)样品之间浮游植物丰度的差别.结果表明,基于浮游植物的显微镜计数效率与定量数据稳定性的综合考虑,选择计数4片×10格/片即可基本保证定量数据的稳定性;在保证正常镜检的基础上,考虑水体营养状态适当增加浓缩倍数能够提高定量数据的可靠性;在特别依赖生物量或稀有种进行水质评价时,处于不同营养水平的水体均需要增加样品的平行数来提高定量数据的可靠性.     

不同养殖类型池塘浮游生物群落结构的初步分析

1988年在山东省禹城县渍涝洼地中选择四口鱼塘以不同放养类型进行试验,4—10月测定其浮游生物数量、生物量的变化。根据浮游生物各主要大类(如原生动物、轮虫以及蓝藻、绿藻、硅藻、隐藻和裸藻等)的变化,分析不同养殖类型池塘浮游生物群落结构变化的稳定性和同步性,同时分析了环境因子特别是生物营养物质的变化对浮游生物的影响。结果指出,肥水性鱼类在养殖池塘中因搭配比例的差异而导致池塘中浮游生物变化。     

渍涝洼地不同类型高产鱼池的浮游动物

根据渍涝洼地没深度,不同主养鱼于池浮游动物群落的动态变化特征,探讨了高产精养鱼池中原生动物在池塘生态系统中的作用及鲢镛鱼摄食对浮游动物的影响,并就池塘水体中游游动物的供养能力及看水养鱼水质标准作了评价。     

Nutrient Behavior and Productivity in a River System Affected by Fishpond Effluents

The expanding culture of fish in coastal areas has raised issues concerning resource use conflicts and water quality problems. A major concern is pollution resulting from nitrogen and phosphorus lost to the environment from feed wastage and fish excretion. The purpose of the study was to assess the environmental conditions in a river system affected by fishponds. Nutrient fluxes and productivity measurements were obtained from Sta. Rita River, a river estuary used as a discharge and an irrigation area of approximately 316 ha of fishponds. During the dry season, when freshwater influence is absent, salinity values inside the river were higher than outside (in the bay). Nutrient trends during ebb and flood periods were similar except for some lag in the profiles that indicate tidal oscillation. The absence of river flow during the dry period resulted in a negligible flux of nutrients along the river. During the wet season, the increase in nitrate concentrations indicates river inputs while the decrease in phosphate values imply less of freshwater influence but more from ponds and domestic wastes. Similarity in productivity estimates signifies good agreement between direct and indirect methods. The absence of flushing during the dry season translates to trapping of nutrients discharged from the ponds in the drainage canals.     

三江平原沼泽地主养鲤鱼塘能量转换效率研究

对1988～1992年三江平原沼泽地泥炭池主养鲤鱼生态系统的能量转换效率进行了研究分析。结果表明,一个生长期浮游植物毛初级生产力对太阳辐射能的转换效率为0.204～0.308％;鲢鳙净产量对浮游植物净产量的转换效率为1.195～4.815％;太阳能转换为鱼类总净产量的生态学效率为0.067～0.123％。总辅助能、总生物能和饲料辅助能转换为鱼类总净产量的效率分别为8.91～14.05％、10.96～17.20％和11.06～17.57％.在2500kg/hm~2、3500kg/hm~2及5000kg/hm~2三个净产量级型池塘中,以5000kg/hm~2产量级的能量转换效率为最佳型。     

Varied impact of land use on water and sediment parameters in fish ponds of the Dombes agro-ecosystem,France

Abstract

Agricultural land use in the area of water bodies is generally considered to increase the nutrient status of the water body water and sediments, but is this also the case for already nutrient-rich fish ponds? We studied 83 fish ponds in the Dombes region, France, where 1100 ponds are located in a heterogeneous agricultural landscape. Different water and sediment parameters were analysed for ponds and in ditches after rainfall events. Land use was studied in the primary catchment of ponds and in a 100-m zone around ponds. Soil parameters of different land-use types were analysed and farmers interviewed about agricultural practices. Increasing cropping area in the catchment of the ponds is significantly correlated to higher PO₄ ^3- concentration of pond water and to a lower degree, also to NO₃ ^?, but only in certain years with higher rainfall and with a more uneven distribution in spring. Sediment parameters were not significantly influenced. High NO₃- concentration in the water of a ditch during significant rainfall events was found for a cropland dominated catchment.

Citation Wezel, A., Arthaud, F., Dufloux, C., Renoud, F., Vallod, D., Robin, J., and Sarrazin, B., 2013. Varied impact of land use on water and sediment parameters in fish ponds of the Dombes agro-ecosystem, France. Hydrological Sciences Journal, 58 (4), 854–871.     

盐碱池塘浮游动物的群落演替和多样性

于1997年4月5日至1998年9月1日对山东高青赵店乡渔场34个盐碱池浮游动物群落演替及其多样性进行了研究,采集了389个浮游动物定量水样。结果表明,轮虫主要是在夏秋高温季节占主导地位,桡足类在春季和秋末冬初在大部分养鱼池和所有无鱼对照池中占绝对优势,原生动物在养鱼池浮游动物中占相当比重,浮游动物生物量的冬季变动一般都有放养早期的春季生物量峰值和盛夏至初秋的生物量高峰,浮游动物多样性指数的季节变动形式与浮游动物生物量的季节变动不尽相同,其季节变动的总趋势是,冬季最低,春季开始上扬,夏季最高,秋季又开始下降;浮游动物多样性指数在浮游动物生物量峰值时多是低谷,而生物量下降时多样性指数又上升,无鱼对照池和新挖池塘的浮游动物多样性指数和生物量均较一般养鱼池塘的高。     

Application of food waste based diets in polyculture of low trophic level fish: Effects on fish growth,water quality and plankton density

Food waste was collected from local hotels and fish feed pellets were produced for a 6 months long field feeding trial. Three types of fish feed pellets (control diet: Jinfeng® 613 formulated feed, contains mainly fish meal, plant product and fish oil; Diet A: food waste based diet without meat and 53% cereal; Diet B: food waste based diet with 25% meat and 28% cereal) were used in polyculture fish ponds to investigate the growth of fish (grass carp, bighead and mud carp), changes in water quality and plankton density. No significant differences in the levels of nitrogen and phosphorous compounds of water body were observed between 3 fish ponds after the half-year feeding trial, while pond receiving Diet A had the highest density of plankton. The food waste combination of Diet B seems to be a better formulation in terms of the overall performance on fish growth.     

Nutrient dynamics in water and sediment of Mediterranean ponds across a wide hydroperiod gradient

In Mediterranean ponds, summer drought enhances seasonality whose intensity varies along topographic and climatic gradients. The alternation of wet and dry periods in rain dependent ponds affects their biogeochemistry and differentiates them from ponds fed by more stable water sources, such as groundwater springs. Superimposed onto this, land use is also a very strong factor of variability. In this study we compared nutrients and organic matter concentrations, in water and in sediment, among different types of Mediterranean ponds based on the source of water, hydroperiod and land use. Forty-three ponds were sampled in Eastern Spain corresponding to five pond types: (1) permanent spring ponds in lowlands, (2) permanent spring ponds in mountains, (3) semi-permanent rain ponds, (4) temporary rain ponds with long hydroperiod and (5) temporary rain ponds with short hydroperiod.The results of this study indicate relevant differences among these pond types. The temporary rain ponds with short hydroperiod are characterized by high turbidity due to suspension of sediment particles rich in phosphorous adsorbed onto them (argillotrophic aquatic systems). They are used for watering domestic sheep that enhance sediment suspension by trampling. Total phosphorous (TP) concentrations in the water are high (like those of hypertrophic lakes), but planktonic chlorophyll a is very low and not correlated with TP, because of the low P-bioavailavility in the water. At the other extreme, we have permanent ponds in lowlands fed by groundwater springs. They are heavily loaded with nitrates due to the surrounding intensive agriculture. In these and other permanent/semipermanent ponds chlorophyll is highly correlated with TP. Sediment characteristics provide a good indication of the hydroperiod, since desiccation has important effects on biogeochemical transformations. A threshold of 5% organic matter (OM) in the sediment separates temporary ponds with a short hydroperiod from those with a long hydroperiod, and a threshold of 8% separates the later from the semi-permanent and permanent ponds. Besides OM reduction, important loss of N occurs during desiccation through mineralization, ammonia volatization and the sequential nitrification/denitrification pathway. On the other hand, the increase of organic P mineralization in dry sediments does not represent a loss of P from the system, since o-P remains adsorbed or bound onto the soil. This leads to a low TN/TP ratio in sediments in temporary ponds with short hydroperiod. These characteristics have to be taken into account when establishing pond typologies and ecological thresholds to assess water quality in these unique aquatic habitats.     

Seasonal dynamics in shallow freshwater pond‐peatland hydrochemical interactions in a subarctic permafrost environment

Terrestrial and aquatic ecological productivity are often nutrient limited in subarctic permafrost environments. High latitude regions are experiencing significant climatic change, including rapid warming and changing precipitation patterns, which may result in changes in nutrient dynamics within terrestrial and aquatic systems and hydrochemical transport between them. The objective of this research was to characterize changes in runoff quantity and quality within, and between peatlands and ponds throughout the snow‐free summer season. Two ponds and their catchments were monitored over the snow‐free season to measure changes in hydrologic storage, and to determine how water chemistry changed with the evolution of the frost table depth. Thresholds in hydrologic storage combined with frost table position (which inhibited infiltration and storage) produced nonlinear responses for runoff generation through highly conductive shallow peat layers while deeper, less conductive layers retarded flow. Greater inputs were required to exceed hydrologic storage (fill and spill) as a deepening frost table increased the hydrologically active portion of the soil, leading to seasonal variability in runoff pathways between peatlands and ponds. Runoff contributions to ponds were an integral component of the snow‐free water balance during the study period, contributing up to 60% of all snow‐free inputs. Groundwater chemistry (and pond chemistry following runoff events when ponds were connected with peatlands) reflected the different depths of peat and mineral soil accessed throughout the season. This work has improved scientific understanding of the combined controls of hydrologic inputs and ground frost on runoff and nutrient transport between peatlands and ponds, and sheds insight into how nutrient dynamics in cold regions may evolve under a changing climate.