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  • 1
    ISSN: 1365-2427
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: SUMMARY. 1. The pattern of fluctuations in the total biomass and species composition of phytoplankton in the shallow, eutrophic Loch Leven exhibits considerable inter-annual and within-year variability. Nevertheless, studies over the 18-year period reviewed here (1968–85) show that many of the observed changes can be explained in -terms of light regimes and the concentrations and fluxes of nutrients. On occasion, the incidence of fungal parasitism and of protozoan, rotiferan and crustacean grazing is also important.2. Changes in annual mean algal biomass from very high levels in the late 1960s and early 1970s to somewhat lower levels in the late 1970s, followed by occasional high peaks in the present decade, are attributed to shifts in phosphorus loading-particularly from a P-rich industrial source.3. In spite of complex and erratic sequences of algal species, seasonal patterns in the size distribution of the phytoplankton assemblage have been identified. However, these also changed. During the 4 years prior to 1971, Daphnia hyalina was not recorded in the plankton, and small algae have been abundant only in late winter or early spring.4. The potential importance of the weather is highlighted as one of the possible causes of the irregular appearance of algal species. The effect of the characteristically variable, oceanicclimate of Northern Britain on this large (13.3 km2), shallow (z̄= 3.9 m) loch is thought to be of particular importance.5. The influence of the weather on phytoplankton sequences is explored by comparing records of monthly flushing rate values with time-series data on aspects of the aquatic environment and plankton populations. The preliminary assessment suggests that variation in flushing rate (p) has a considerable effect on temperature regimes and the supplies and in-loch dynamics of nutrients; through such changes, p controls major features of phytoplankton succession such as the temporal abundance of diatoms, as well as detailed sequences of events relating to the development and collapse of particular algal species - and. as a consequence, in some cases, of the animals preying on them.6. Concluding remarks emphasize how little would have been understood about the functioning of shallow lakes, had the long-term commitment to Loch Leven research been abandoned. The view is also expressed that the findings are of considerably greater relevance to research on ‘classic’ stratifying lake systems, than the focus on the shallow waterbody might hitherto have suggested.
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  • 2
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Freshwater biology 17 (1987), S. 0 
    ISSN: 1365-2427
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: SUMMARY. 1. Coidingham Loch (Berwickshire. Scotland) (area. 8.4 ha, mean depth 2.9 m, max. depth 12.3 m) belongs to Hakansson's convex shape category. It lies in a basin of Silurian Greywackes rock within 0.25 km of coastal sea cliffs (c. 133 m a.s.l.). The theoretical hydraulic replacement time is 3.17 years.2. The loch stratifies intermittently in summer. Fluctuations in oxygen concentration generally correspond to spells of mixing and stratification; low values of 10% saturation occur at the bottom.3. The sum of the concentrations of major cations (Na+, K+, Ca2+, Mg2+) is in accordance with measured conductivities ranging between 380 μS cm−1 and 420 μS cm−1 (k.25). The ratios (by equivalents) of Na+/Cl− (0.04) are similar to those in sea-water, whilst values for Ca+2+/Cl− (0.85–1.01) and Mg2+/Cl− (0.79–0.88) reflect the bedrock.4. Nitrate concentrations were lowest (〈0.05 mg N1−1) in summer following losses from the column of 107 mg N m−2 1−1, a rate corresponding well with published figures on microbial nitrate reduction. Nitrate increased at a rate of 8μg N I−1 d−1 to a winter maximum of 1.55 mg N I−1. Mass balance calculations show that if this rise is attributed to run-off from surrounding land, a loss rate of 11.1 kg N ha−1 yr−1 would be required; this value is also commensurate with published figures.5. Changes in phosphorus and factors controlling them contrast markedly with those of nitrate. The minimum concentration of 55 μg total P l−1 (mainly in soluble reactive form) occurs in spring. An increase to the maximum ofc. 300 μg l−1 in summer is sustained mainly by release from the sediments at a regular rate of 3 μg P l−1 d−1 (8.7 mg m−2 d−1). Adsorption by the sediments is considered to be the major process accounting for autumnal losses of phosphorus of 2.6 mg P M−2d−1.6. Silica showed a less regular seasonal pattern, but varied some 45-fold with a maximum of 2.25 mg SiO2, l−1 in August.
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  • 3
    ISSN: 1365-2109
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract. A sharp rise in the concentration of soluble reactive phosphorus antl a marked decrease in the level of nitrate were associated with intermittent thermal stratification and localized de-oxygenation in Coldingham Loch (Berwickshire, Scotland) in summer. These conditions apparently favoured plunktonic blue-green ‘algae’ (Cyanobacteria) such asAphani-zomenon, which grew to bloom proportions and threatened the trout angling fishery for which the loch is managed. Various measures for ameliorating the situation are discussed and two bubble-gun units were installed in the deepest part of the loch (ca 12m), to distribute compressed air and mix the column. The installation was operated continuously during the periods May-September of 1984 and 1985. Temperature and chlorophyll measurements indicated good vertical and horizontal mixing.In spite of virtually no effect on rates of release of phosphorus from the sediments, mixing prevented surface bloom formations of Aphanizomenon and reduced its biomass; maxima of 17 and 52m filament 1−1 in 1984 and 1985 respectively contrast markedly with peaks of 130 and 630m 1−1 recorded in 1983. Total phytoplankton abundance was also lower. In 1984, the main difference occurred at the ‘critical’ late-summer period with chlorophyll concentrations of ca 20 μg 1−1 being only one-half of those measured at the same time in 1983, and Secchi disc transparencies of ca 3·0 m compared to values of ≤ l·5min 1983. An even greater response was recorded in 1985; throughout May to September, chlorophyll levels rarely exceeded 13μg 1−1 while water transparency usually exceeded 3·0m.
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  • 4
    ISSN: 1573-5117
    Keywords: lake ; phosphorus ; loading ; restoration ; Loch Leven ; Scotland
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Eight tonnes of phosphorus in all forms (total phosphorus, TP) entered Loch Leven from its catchment in 1995, compared to 20 t in 1985. Diffuse run-off from the land, and waste from over-wintering geese contributed 59% of the total loading in 1995 cf. 42% in 1985. Point-sources of sewage, and waste-water from fish-rearing ponds, produced the rest. Inputs of phosphorus in soluble reactive form (SRP) totalled 5 t, i.e. 63% of the TP loading in 1995, as compared with 1985 values of 11.8 t and 59%. Point-sources of SRP contributed 54% of the total SRP input in 1995 cf. 69% in 1985. Loadings from three sewage treatment works (STW) totalled 3.1 t TP in 1995 as compared with 5.3 t in 1985; this included 2.6 t SRP (cf. 3.6 t). Daily per capita outputs of the upgraded Kinross North and Milnathort STWs were 0.68 g and 0.81 g TP, respectively, compared with pre-upgrade values of 1.77 g and 2.03 g. Nett reductions in TP and SRP loadings between 1985 and 1995, are 55% and 59% respectively. These values are attributable as much to the lower rainfall of 890 mm over the period of study in 1995, compared to 1250 mm in 1985, as to ‘managed’ elimination of P usage at a major industrial source, and upgrades of STWs. In spite of these cutbacks, a combination of the lower rainfall and an extraordinarily hot summer in 1995 negated the expected reduction in lake phosphorus and chlorophyll levels. The lowered specific areal loading of ca. 0.7 g P m−2 estimated for 1995 still considerably exceeds the ideal maximum for the loch. These statistics nevertheless ignore the significance of a reduction of ca. 7 t in P entering the system in bio-available form, a recently completed upgrade of a major STW and channelling of effluent from a small works out of the catchment.
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Hydrobiologia 255-256 (1993), S. 305-315 
    ISSN: 1573-5117
    Keywords: Rotifera ; Synchaeta ; Loch Leven ; population dynamics ; interference competition ; embryo development time
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Synchaeta kitina Rousselet reached population densities of up to 5000 ind.l−1 in Loch Leven, between January 1977 and December 1982. The species was found over the entire range of temperatures recorded (0.4–21.4 °C), but was most abundant at temperatures above 7 °C. Embryo development times, determined under laboratory conditions, ranged from 122 h at 2 °C to 12.5 h at 20 °C. There was a marked inverse relationship between populations of S. kitina and Daphnia hyalina var. lacustris in the loch. It seems unlikely that this was due to interference competition from Daphnia. S. kitina can be cultured on Rhodomonas minuta var. lacustris and there is some evidence that this rotifer also feeds on small flagellates in its natural environment.
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  • 6
    ISSN: 1573-2983
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Medicine
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Russian chemical bulletin 18 (1969), S. 1325-1328 
    ISSN: 1573-9171
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology
    Notes: Conclusions 1. The possibility of the extraction of scandium by the thiocyanate ion and a chloroform solution of α- and β-picolines, 2-methyl-5-ethylpyridine, and collidine was demonstrated. 2. The extraction of scandium by collidine was investigated at various concentrations of the reagents and scandium, acidities of the solution, times of contact of the phases, and in the presence of NaCl, NaNO3, and NaClO4. The composition of the complex of scandium thiocyanate with collidine corresponds to the formula ColH+[Sc(SCN)4(Col)2]. The extraction of Fe(III), Y, Zr, and Th was studied under the optimum conditions for the extraction of scandium.
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  • 8
    ISSN: 1573-9171
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology
    Notes: Conclusions 1. Second-order regression equations, characterizing the extraction of scandium thiocyanate by chloroform solutions of 1,10-phenanthroline and collidine, were obtained by the method of mathematical planning of experiments. 2. The optimum conditions of extraction of scandium were found.
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  • 9
    ISSN: 1573-9171
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology
    Notes: Conclusions 1. The mechanism of the extraction of scandium thiocyanate with 1,10-phenanthroline and collidine against a background of NaCl and NaNO3 was studied by the method of mathematical planning of experiments (the method of two-dimensional cross sections). 2. In the case of the 1,10-phenanthroline-thiocyanate complex, the background electrolyte NO 3 − is inserted into the complex; in the case of the collidine-thiocyanate complex, the background electrolytes NO 3 − and Cl− are not inserted into the complexes.
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  • 10
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