Variations in the water quality of a small urban tropical catchment: implications for load estimation and water quality monitoring

This paper presents findings on the quality of runoff draining a small urban tropical catchment in Singapore. Variations in runoff quality were studied by continuous, regular and storm event water sampling over a period of eleven months for suspended sediment, nutrient and inorganic variables. Storm events and anthropogenic activities exerted the most influence on runoff quality. Concentration-discharge rating relationships were derived to assess the rating curve method for calculating load of the variables monitored. The poor rating relationships obtained indicated that the method was not suitable for load estimation in this catchment. Instead, an interpolation method was used to calculate sediment loads. The preliminary results highlighted the importance of conducting small-scale, relatively short-term studies to identify and assess specific water quality problems facing each catchment. Such a sampling strategy might be more useful than either routine or continuous sampling in the context of planning more detailed monitoring strategies and management options suitable for disturbed catchments.     

Charophyte growth in small temperate water bodies: Extreme isotopic disequilibrium and implications for the palaeoecology of shallow marl lakes

A small pond containing the charophyte Chara hispida was monitored over a one-year period for changes in growth, water chemistry, water level and stable isotopic composition. Chara growth was found to be seasonal, with maximum growth occurring from late April to July. During this period, pH rose to > 10 while the dissolved inorganic carbon (DIC) and calcium fell as a result of photosynthesis and calcification. Large gradients in pH, water temperature and irradiance were found within the Chara sward and measurements showed that most growth and photosynthesis occurred within the upper 20 cm of the water column. Chara oospore formation was also found to be seasonal but dependent upon environmental conditions.

δ¹⁸O_w rose rapidly during summer as evaporation progressed and this was correlated with the δ¹⁸O_DIC, and to some extent with δ¹⁸O_c of the Chara encrusted calcite. However, extreme isotopic disequilibrium was observed between the δ¹⁸O_c and the δ¹⁸O_w and also between the δ¹³C_c and the δ¹³C_DIC. This arose from the high pH allowing atmospheric CO₂ to enter the water and combine directly with OH⁻.

It is concluded that, within shallow eutrophic lakes containing Chara swards, inferences of climate (e.g. air temperature) cannot be made from observations of the isotopic composition of Chara carbonates. However in combination with other geochemical data, disequilibrium events may be identifiable in ancient lake basins and taken as evidence for lake shallowing and/or eutrophication.     

Seasonal water quality of shallow and eutrophic Lake Pamvotis, Greece: implications for restoration

Lake Pamvotis is a moderately sized (22 km²) shallow (z _avg=4 m) lake with a polymictic stratification regime located in northwest Greece. The lake has undergone cultural eutrophication over the past 40 years and is currently eutrophic (annual averages of FRP=0.07 mg P l^-1, TP=0.11 mg P l^-1, NH₄ ⁺=0.25 mg N l^-1, NO₃ ^–=0.56 mg N l^-1). FRP and NH₄ ⁺ levels are correlated to external loading from streams during the winter and spring, and to internal loading during multi-day periods of summer stratification. Algal blooms occurred in summer (July–August green algae, August–September blue-green algae), autumn (October blue-green algae and diatoms), and winter (February diatoms), but not in the spring (March–June). The phytoplankton underwent brief periods of N- and P-limitation, though persistent low transparency (secchi depth of 60–80 cm) also suggests periods of light limitation. Rotifers counts were highest from mid-summer to early autumn whereas copepods were high in the spring and cladocerans were low in the summer. Removal of industrial and sewage point sources a decade ago resulted in a decrease in FRP. A phosphorus mass balance identified further reductions in external loading from the predominately agricultural catchment will decrease FRP levels further. The commercial fishery and lake hatchery also provides opportunities to control algal biomass through biomanipulation measures.     

Central European water quality indices applied to long-term data from peri-alpine lakes: test and possible improvements

We tested the applicability of two available Water Framework Directive (WFD) compliant phytoplankton indices on three large peri-alpine lakes to analyze their suitability for trophic classification. We show that the indices vary in their final resulting Ecological Quality Ratios (EQRs) and are only appropriate to roughly distinguish lakes of different water quality according to OECD criteria (OECD, 1982). Annual mean TP concentration in Lake Geneva was 0.03 mg l^?1 in 2006 (Lazzarotto &; Rapin, 2007), which marks mesotrophic conditions. According to the tested indices, the lake is of ‘good’ (0.60–0.80) quality after the German WFD method (PSI) and of ‘moderate’ quality according to the Austrian WFD method (BI). We prove that the way how to derive the per annum value of the metric ‘Brettum Index’ (BI) in the Austrian WFD method significantly influences the resulting index and the scatter of long-term data. We focused on improvement strategies for this index in terms of calculation and sampling frequency. Contrary to the tested bin, the modified index presents no significant differences between four and six sampling dates per year. In order to improve the significance of the available indices, we propose to modify the way of per annum index calculation for the Austrian WFD method as well as to focus on species composition to achieve a high relative proportion of indicator species. A phytoplankton index alone may not be sensitive enough to track the changes that occur within a lake. The results confirm the need to take into account other biological elements such as fish, macrophytes, attached diatoms and macrozoobenthos as suggested by the WFD.     

The ice cover on small and large lakes: scaling analysis and mathematical modelling

Lake ice cover is described by its thickness, temperature, stratigraphy and overlying snow layer. When the ratio of ice thickness to lake size is above ～10^?5, the ice cover is stable; otherwise, mechanical forcing breaks the ice cover, and ice drifting takes place with lead-opening and ridging. This transition enables a convenient distinction to be made between small and large lakes. The evolution of the ice cover on small lakes is solved by a wholly thermodynamic model, but a coupled mechanical–thermodynamic model is needed for large lakes. The latter indicates a wide distribution of ice thickness, and frazil ice may be formed in openings. Ecological conditions in large lakes differ markedly from those in small lakes because vertical mixing and oxygen renewal may take place during the ice season, and the euphotic zone penetrates well into the water column in thin ice regions. Mesoscale sea ice models are applicable to large lakes with only minor tuning of the key parameters. These model systems are presented and analysed using Lake Peipsi as an example. As the climate changes, the transition size between small and large lake ice cover will change.     

UV damage in shallow lakes: the implications of water mixing

The plankton of shallow lakes is expected to experience increasingexposure to ultraviolet radiation (UVR) within the next decades.In addition to stratospheric ozone depletion, decreases in dissolvedorganic carbon (DOC), caused by climate warming or acidification,will result in greater UVR penetration in many lakes. Circulationpatterns induced by moderate winds force the plankton of shallowlakes to be cycled through the whole water column. This translatesinto higher doses and fluctuating dosage rates. Here, we reportthe results of a series of ‘in situ’ UV exposureexperiments in which two zooplankton crustaceans (one capableof photorecovery and the other not) were incubated either atfixed depths or under simulated mixing. Our main goal was toassess the extent to which the results from static incubationscould be extrapolated to vertically moving zooplankton. Staticincubations accurately predicted the survival of moving individualsfor the species without photorecovery, but failed to do so forthe species capable of photorecovery. The fluctuations in dosagerate for high doses tended to increase the survival of the specieswith photorecovery. We contend that neglecting the effects ofvertical mixing may result in a biased perception of UVR effectsin shallow lakes.     

Density structure of the fine surface water layer of large lakes and remote measurement of the temperature

Remote sensing of surface temperatures in large lakes differs in some critical respects from that in marine conditions. Firstly, the atmospheric structure over large lakes has some continental features, which makes the calculation of its influence more complicated. Secondly, the vertical temperature structure in the fine surface layer of a lake is more complex than in marine waters. A prominent feature of the thermal structure of spring heating of large lakes (e.g. in Lake Ladoga from May to July) is the existence of a thermal front, which is manifested on the lake surface as a fine strip with steep horizontal temperature gradient. The existence of a thermal front makes it possible to calibrate infra-red space survey data without using in situ surface temperature measurements. The calibration of arbitrary heat brightness values for +4 °C can be obtained by plotting a frequency distribution histogram of the heat brightness values obtained for the IR-image pixels. While the thermal front is in existence, the heat brightness frequency distribution appears bimodal, and the brightness value at the minimum between the peaks is assigned the temperature of +4 °C. Laboratory and field experiments have enabled us to separate two types of near-surface density structures. Under conditions of density instability in the fine surface layer, microconvection limits the magnitude of vertical temperature difference in this layer to a constant range of 0.6–0.8 °C. However, when a stable density structure prevails during calm conditions, much greater vertical temperature differences may exist.     

Food quality for Daphnia in humic and clear water lakes

1. Growth and reproduction of Daphnia fed lake seston were measured in two categories of meso‐ to eutrophic lakes differing with respect to terrestrial organic matter influence (humic and clear water lakes). The content of highly unsaturated fatty acids (HUFA), P and N, as well as the taxonomical composition of seston were analysed. 2. Seston HUFA and C : P ratios were similar between lake categories, whereas C : N ratios were lower in the clear water lakes in both spring and summer. Despite the similarity in HUFA and P content of seston, Daphnia growth rate, clutch size and the proportion of gravid females were, respectively, about 1.5, 3 and 6 times higher in the clear water lakes. 3. Differences in growth and reproduction were related to a combination of higher N content and good fatty acid quality of the seston in the clear water lakes. Relatively high biomass of edible algae, such as Rhodomonas sp. and Cryptomonas sp., in the clear water lakes, and differences in water pH likely contributed to the observed differences in Daphnia growth and reproduction between lake categories. Additionally, it is possible that Daphnia was energy limited in the humic lakes despite high particulate organic carbon (POC) concentrations, as the contribution of non‐algal and detrital C to the POC pool was high. 4. Our results suggest that dietary HUFA content has the potential to improve herbivore growth and reproduction if N and P are not limiting. N merits more attention in studies of zooplankton nutrition.     

Cyprinid assemblages,and the physical and chemical characteristics of small northern Ontario lakes

Synopsis The cyprinid species, and physical and chemical characteristics were recorded from 58 small lakes in the Algoma district of northern Ontario. A group of typical stream-dwelling lithophilous species, which included common shiner, Notropis cornutus, creek chub, Semotilus atromaculatus, and blacknose dace, Rhinichthys atratulus, tended to occupy lakes of larger than average drainage areas. Phoxinus spp., pearl dace, Semotilus margarita, and fathead minnow, Pimephales promelas, occurred commonly in lakes with small drainage areas, and the average drainage area of lakes they occupied was near or below the overall average. Lakes without stream cyprinids were discriminated from lakes with them on a combination of chemical variables, including pH, alkalinity and calcium, which indicated that they were more susceptible to anthropogenic acidification.     

武汉东湖鱼产量时间序列模型及回归分析

随着城市人口的增长和经济的快速发展,武汉东湖的水体富营养化日益严重。80年代以来,东湖通过实施滤食性鱼类治理水华取得了一定成效。利用统计学软件SPSS,应用时间序列模型和回归分析对东湖44年鱼产量数据进行运算,对东湖鱼产量变化进行了分析和预测:东湖最高鱼产量在1700～1850t之间,比较合理的鱼产量应维持在1150t左右。     

Statistical analysis of algal and water quality data

Data on cyanobacteria (blue-green algae) are generallycollected on a reactive basis, frequently in responseto bloom events. Such data presents a biased andincomplete snapshot of water quality. This paper looksat two typical data sets for UK waters showing thatwhile statistics may be used to describe the data theyare of limited use in forecasting. Suggestions ofappropriate tests for small and sparse data sets aremade.     

Effects of hypolimnetic oxygenation on water quality: results from five Danish lakes

Stratified eutrophic lakes often suffer from hypolimnetic oxygen depletion during summer. This may lead to low redox conditions and accumulation of phosphate and ammonia in the hypolimnion. Hypolimnetic oxygenation has been used as a lake management strategy to improve the water quality in five eutrophic dimictic Danish lakes where oxygenation was conducted for 4–20 years. In one lake, the hypolimnetic oxygen concentration clearly improved by oxygenation, whereas the other four lakes still exhibited low mean summer levels (<2.2 mg O₂ l⁻¹). Oxygenation generally increased the hypolimnetic water temperature by 0.5–2°C, but in one lake it increased by 4–6°C. In all lakes, oxygenation significantly reduced the hypolimnetic concentrations of phosphorus and ammonia during stratification. The accumulation of phosphorus and ammonia typically decreased by 40–88%. In two lakes oxygenation was stopped for 1–2 years and here hypolimnion concentrations of both phosphorus and ammonia increased again. Surface water quality only improved in one lake, but was likely also influenced by simultaneously occurring changes in external nutrient loading. Overall, it is concluded that hypolimnetic oxygenation reduces the hypolimnetic accumulation of phosphorus and ammonia and may prevent anoxia in the deeper parts of the lake. However, long-term oxygenation is required and it is uncertain whether the overall lake water quality can be improved by oxygenation. Reduction of the external nutrient loading is still essential to improve lake water quality. Handling editor: Luigi Naselli-Flores     

Gill anomalies of perch and roach from four lakes differing in water quality

This study examined gill anomalies of two common freshwater fish species, roach Rutilus rutilus and perch Perca fluviatilis , collected over five seasons in 1989–1990 from four lakes in central Finland. The lakes differed both in water quality and in fish parasite species composition. Particular attention was paid to the differences in chloride cell proliferation. Gill anomalies were generally more common and abundant in roach than in perch. Chloride cell proliferation was the most frequent histological change in roach but was that least often found in perch. Most of the changes were systemic and light in severity. In perch an unidentified lesion of noncellular eosinophilic inclusions in an enlarged epithelium was also recorded. There was a marked pattern in the severity of histological changes in perch when comparing those from the natural Lake Peurunka to those from three 'altered' lakes. Gills of perch from Lake Peurunka possessed more alterations in all the recorded parameters. In roach, a significant differences were detected in chloride cell and epithelial proliferation: these were greater in Lake Peurunka and 'polluted' Lake Vatia. In perch, all histological changes were significantly more frequent at the end of autumn 1989 when compared to other seasons. In roach, increased frequencies of all gill changes were noted in winter and spring samples. Tissue reactions to parasites were either only localized or absent. The systemic gill alterations in freshwater fish may reflect the soft nature and low winter temperature of Finnish fresh waters, in which chemical imbalances, such as acid peaks, may induce more dramatic changes in fish tissues than in harder waters.     

Interspecific habitat associations of juvenile salmonids in Lake Ontario tributaries: implications for Atlantic salmon restoration

Diel variation in habitat use of subyearling Chinook salmon (Oncorhynchus tshawytscha), subyearling coho salmon (O. kisutch), yearling steelhead (O. mykiss), and yearling Atlantic salmon (Salmo salar) was examined during the spring in two tributaries of Lake Ontario. A total of 1318 habitat observations were made on juvenile salmonids including 367 on steelhead, 351 on Chinook salmon, 333 on Atlantic salmon, and 261 on coho salmon. Steelhead exhibited the most diel variation in habitat use and Chinook the least. Juvenile salmonids were generally associated with more cover and larger substrate during the day in both streams. Interspecific differences in habitat use in both streams occurred with Atlantic salmon (fast velocities) and coho salmon (pools) using the least similar habitat. Chinook salmon and Atlantic salmon used similar habitat in both streams. These findings should help guide future management actions specific to habitat protection and restoration of Atlantic salmon in Lake Ontario tributaries.     

Contribution of ciliated protozoa to the planktonic biomass in a series of Ontario lakes: quantitative estimates and dynamical relationships

The plankton of nine Ontario lakes spanning several physiographicregions was sampled every two weeks during the ice-free periodof 1981, and one lake was studied in the three previous years.Phytoplankton, zooplankton, and ciliated protozoa were sampled,counted and sized. The size data were converted to biomass estimatesto yield quantitative comparisons of the relative allocationof biomass among different functional compartments. This isthe first study to look simultaneously and quantitatively atthe total plankton system of lakes (including ciliates, pbytoplanktonand net zooplankton) over a broad physiographic region. Ciliatesconstitute –10% of the non-algal biomass and 5% of thetotal planktonic biomass of these lakes. Ciliate standing cropsamong lakes are significantly corrrelated with total organicand total inorganic carbon concentrations in the water column,while the dynamics of ciliate biomass fluctuations are significantlycorrelated with variations in total phosphorus concentration,in conductivity, in Kjeldahl nitrogen concentration, and ininorganic carbon content. There appears to be a significantdynamical relationship between ciliates as a proportion of thetotal planktonic biomass, exclusive of filamentous and large(>30 µm) spherical algae, and the relative biomassof small algae (2–5 µm) as a fraction of total algalbiomass, again exclusive of filaments and large (>30 µm)algae. The hypothesis is advanced that ciliates primarily functionas bacterial grazers in planktonic ecosystems and that theirprimary competitors in this role are rotifers.     

Larval chaoborid mandibles in surface sediments of small shallow lakes in Finland: implications for palaeolimnology

The aim of this study was to assess the value of phantom midge Chaoborus (Diptera: Chaoboridae) larvae as a palaeoenvironmental proxy in northern Europe. The presence of Chaoborus was examined in 80 small shallow lakes across Finland (60–70°N), based on their subfossil mandibles preserved in lake sediments. Chaoborus flavicans was present in 33 lakes, but was the most abundant midge taxon in only one of the lakes. Chaoborus crystallinus/obscurripes mandibles were present in two lakes. Statistical analyses showed that the distribution of Chaoborus was significantly correlated with lake depth and mean July air temperature. Chaoborus was absent in the northern study lakes, whereas the results indicated that C. flavicans was frequently found in small shallow lakes in southern Finland. Chaoborus flavicans was particularly abundant in fish-free, macrophyte-rich, dystrophic lakes, but absent in oligotrophic clear-water lakes having fish. The results of this study indicate that the subfossil mandibles of Chaoborus can provide valuable information in multiproxy palaeolimnological studies, especially when investigating past changes in water level and temperature in small shallow lakes in northern Europe. Guest editors: K. Buczkó, J. Korponai, J. Padisák & S. W. Starratt Palaeolimnological Proxies as Tools of Environmental Reconstruction in Fresh Water     

Time series analysis of hybrid neurophysiological data and application of mutual information

Multivariate time series data of which some components are continuous time series and the rest are point processes are called hybrid data. Such data sets routinely arise while working with neuroscience data, EEG and spike trains would perhaps be the most obvious example. In this paper, we discuss the modeling of a hybrid time series, with the continuous component being the physiological tremors in the distal phalanx of the middle finger, and motor unit firings in the middle finger portion of the extensor digitorum communis (EDC) muscle. We employ a model for the two components based on Auto-regressive Moving Average (ARMA) type models. Another major issue to arise in the modeling of such data is to assess the goodness of fit. We suggest a visual procedure based on mutual information towards assessing the dependence pattern of hybrid data. The goodness of fit is also verified by standard model fitting diagnostic techniques for univariate data.     

青岛市秋季空气微生物群落多样性

采用KC-6120空气综合采样器采集空气微生物样品,通过构建16S/18SrDNA克隆文库方法分析青岛市市区街道秋季空气微生物群落结构特征.结果表明： 空气细菌分布在6大类,分别为变形菌门(78.8%)、厚壁菌门(14.6%)、放线菌门(4.0%)、浮霉菌门(1.3%)、蓝藻门(0.7%)和栖热菌门(0.6%),优势菌属为不动杆菌属(39.7%)、葡萄球菌属(11.3%)、鞘脂单胞菌属(8.6%)和副球菌属(6.0%).空气真菌分布在子囊菌门(97.5%)和担子菌门(2.5%),优势菌属为核腔菌属(76.5%)、炭角菌属(13.6%)和外瓶霉属(2.5%).空气微生物中存在不动杆菌属、鞘脂单胞菌、葡萄球菌等致病菌或条件致病菌,以及引发多种农作物枯萎死亡的麦类核腔菌、团炭角菌和角状平脐疣孢等真菌.