Loch Leven lies in a glacial depression 35 kilometres north of Edinburgh,Scotland. It has a large surface area, 13.3 km&sup2;, but is generally shallowwith a mean depth of 3.9 metres, although there are two deeper "holes"where the depth reaches 25 metres. Land use in the 145 km&sup2; catchmentdraining to the loch is predominantly arable farming, with some roughgrazing in the headwaters and with three small towns close to the loch.The physical characteristics of Loch Leven are fully described by Smith(1974); it is a National Nature Reserve, a Site of Special ScientificInterest, and is cited under the Ramsar Convention as a wetland site ofinternational importance

Ian R Fozzard

Janet A. Armstrong

Robert J. Sargent

FBA Journal System (Freshwater Biological Association)

OSOLLATORIA BLOOM IN LOCH LEVEN 203 
DEVELOPMENT AND COLLAPSE OF AN OSCILLATORIA BLOOM 
IN LOCH LEVEN DURING JULY 1994 
JANET A. ARMSTRONG, IAN R. FOZZARD AND ROBERT J. SARGENT 
(Dr J. A. Armstrong, I. R. Fozzard and R. J. Sargent, Forth River 
Purification Board, Clearwater House, Heriot Watt Research Park, 
Avenue North, Riccarton, Edinburgh EH 14 4AP, Scotland.) 
Introduction 
Loch Leven lies in a glacial depression 35 kilometres north of Edinburgh, 
Scotland. It has a large surface area, 13.3 km2, but is generally shallow 
with a mean depth of 3.9 metres, although there are two deeper "holes" 
where the depth reaches 25 metres. Land use in the 145 km2 catchment 
draining to the loch is predominantly arable farming, with some rough 
grazing in the headwaters and with three small towns close to the loch. 
The physical characteristics of Loch Leven are fully described by Smith 
(1974); it is a National Nature Reserve, a Site of Special Scientific 
Interest, and is cited under the Ramsar Convention as a wetland site of 
international importance. 
Because of its lowland situation the loch is naturally productive and 
algal blooms are common. Bailey-Watts et al. (1987) estimated the 
annual load of phosphorus entering the loch from diffuse sources in the 
catchment at 26 kilograms per day. Over the past ten years, point-source 
emissions of phosphorus have been steadily reduced from 32 kg per day 
to around 9 kg per day in 1994. However, there is a legacy of 
historically high phosphorus loadings held in the loch sediment, which 
can be released into the loch water under certain conditions. 
In 1992 a particularly severe bloom of the blue-green algae Anabaena 
and Microcystis caused much publicity and considerable damage to the 
world-famous fishery in Loch Leven. As a result of this the Forth River 
Purification Board (FRPB) decided to supplement its spot-sampling of the 
loch and its tributaries with a buoy, moored in the loch and able to 
continuously monitor basic water quality parameters. The buoy was 
deployed in May 1994 and produced detailed data on the condition of 
the loch through the development and subsequent collapse of a bloom 
of another blue-green alga, Oscillatoria. This article briefly describes 
some important features and gives our initial thoughts on events in the 
loch during this period. 
204 J. A. ARMSTRONG, I. R. FOZZARD AND R. J. SARGENT 
Sampling the loch 
Sampling has been carried out in conjunction with Scottish Natural 
Heritage and the NERC Institute of Freshwater Ecology. During 1994, 
weekly spot-sampling of open water sites on Loch Leven took place from 
16 March onwards, at the South Deep Hole (NCR NO 148 005), South 
of the Reed Bower (NO 138 012), and the Outlet at the Sluices (NT 168 
OSCILLATORIA BLOOM IN LOCH LEVEN 205 
995). When the weather prevented open water sampling, this was done 
on the shore at the Outlet at the Sluices and the Pier at Kinross (NO 127 
017). 
The samples from the South of Reed Bower and Sluices sites were 
taken from a 2-metre column of water whereas the South Deep Hole was 
sampled from a 15-metre column. From 12 July 1994, following thermal 
stratification, an additional site at the North Deep Hole (NT 141 031) 
206 J. A. ARMSTRONG, I. R. FOZZARD AND R. J. SARGENT 
was sampled. The Deep Hole sites were subsequently sampled using a 
2-metre column for a sub-surface sample and a displacement water-
sampler was used to take a grab sample at 20 metres depth. These spot-
samples were analysed for the variables shown in Figs 1 and 2, plus 
electrical conductivity. Temperature, dissolved oxygen and Secchi disc 
depth were recorded at each site. Depth profiles of temperature and 
dissolved oxygen were recorded at the South and North Deep Hole sites. 
The above water samples and recordings were all taken manually. 
Additional information on dissolved oxygen, temperature, pH, electrical 
conductivity and turbidity was recorded by a water quality monitoring 
buoy, comprised of a Hydrolab DataSonde 3, which performs the analy-
ses and logs the data at 15-minute intervals, and a buoy with a solar 
panel and telemetry link. The sonde was deployed on 24 May 1994 and 
initially located at the South Deep Hole without a solar panel, so it was 
necessary to retrieve the sonde weekly and download data in the 
laboratory. From 28 June 1994 the complete buoy, including a solar 
panel, was installed at its permanent location, South of Reed Bower, and 
the sondes were changed fortnightly. 
Checks on the quality of field and laboratory data were performed 
routinely. In the laboratory, independently prepared standards of known 
concentration were analysed along with the samples, and the sample 
results were accepted if they fell within a pre-determined range. No 
problems were encountered. 
For field data the instrumentation was calibrated on a weekly or 
fortnightly basis. This included the field dissolved oxygen (DO) meter 
and the probes on the water quality sonde, which were calibrated prior 
to deployment; post-deployment calibration checks were made for 
calibration drift. The probe readings were also compared with the results 
for the spot-sample taken at about the same time. Winkler DO samples 
were taken at some sites as a check on the sonde DO readings. The 
sonde data were accepted if they passed these validation checks. 
Changes in chlorophyll-a and nutrients during the period 16 March to 
5 July 1994: development of the Oscillatoria bloom 
Very little difference between spot-sampling sites was observed during 
this first period of observations, and data from one site have been chosen 
as representative of conditions in the loch (Figs 1, 2). Throughout April 
and May there was a slow increase in levels of chlorophyll-a, followed 
FIG. 3. (On page 207) Plots of water temperature, dissolved oxygen and pH recorded by the 
water quality monitoring sonde on a buoy at the South of Reed Bower sampling site in Loch 
Leven, for the period 5 July to 22 July 1994. 
OSCILLATORIA BLOOM IN LOCH LEVEN 207 
208 J. A. ARMSTRONG, I. R. FOZZARD AND R. J. SARGENT 
by a rapid increase through June, reaching a maximum of 230 
micrograms per litre. This was mirrored to a considerable degree by the 
total phosphorus levels. A steady rise in the pH of the loch was also 
observed, with levels above pH 9 being recorded throughout June. 
The dissolved nutrient status of the loch showed little change over the 
spring period, except for total oxidised nitrogen. Ammonia was 
consistently less than 0.1 milligrams of nitrogen per litre whereas total 
oxidised nitrogen displayed a steady decline from 2.5 mg N per litre in 
March down to less than 0.1 mg N per litre from mid-June. In the period 
of rapidly increasing chlorophyll-a levels the total and dissolved silica 
displayed a steady increase. Soluble reactive phosphorus was less than 2 
micrograms P per litre on most sampling occasions from mid-May, whilst 
total dissolved phosphorus was between 10 and 20 micrograms per litre. 
As previously stated there was little difference in results from the three 
main sampling sites, suggesting that the water in the loch was well 
mixed. No marked difference in water temperature or dissolved oxygen 
was observed in the South Deep Hole profile prior to 12 July. 
Throughout this spring period the water quality monitoring sondes 
provided a valuable insight into the behaviour of the loch. There was a 
clear diurnal pattern in pH, dissolved oxygen and temperature. The level 
of change varied according to climatic conditions. The most marked 
changes in pH and dissolved oxygen occurred with the biggest 
fluctuations in temperature. These changes were indicative of algal 
photosynthesis, which increased the saturation levels of dissolved 
oxygen in the water, whilst carbon uptake by the algae caused a drop in 
carbon dioxide levels and thus a rise in water pH. 
Changes in chlorophyll-a and nutrients during the period 5 July to 16 
August 1994: collapse of the Oscillatoria bloom 
Through the telemetry link with the water quality monitoring buoy a 
marked decline in levels of dissolved oxygen was observed from 9 July 
onwards, heralding changing conditions in the loch. The events that took 
place in the summer of 1994, between 5 July and 16 August, are now 
described (Fig. 3). 
On 8 July there was a very rapid rise in water temperature, with a 
corresponding increase in dissolved oxygen and pH. Over a 30-minute 
period the temperature rose from 16.9°C to 18.8°C, the percentage 
saturation of dissolved oxygen rose by 48% to a maximum of 158 per 
cent saturation and the pH, which was already high, rose from 9.36 to 
9.68. These values appear to represent a peak in photosynthetic activity 
by algae. 
The peaks occurred around 1600 hours, the approximate time of the 
OSCILLATOR!A BLOOM IN LOCH LEVEN 209 
diurnal peaks observed on previous days, but were much more marked 
than previously. An overnight decline was observed and the rise in 
values on 9 July was limited, and from 0915 hours there was a drop in 
all three variables. Over the following three days a diurnal fluctuation 
was observed but with an overall downward drift until the afternoon of 
12 July, when dissolved oxygen was in the region of 20 to 30 per cent 
saturation and the pH was 7.35. 
These changes were coincident with a marked reduction in 
chlorophyll-a values, which had climbed to 230 micrograms per litre by 
5 July, falling to approximately 70 micrograms per litre on 12 July (Fig. 
2). The low levels of dissolved oxygen and pH were maintained until 16 
July, with dissolved oxygen levels as low as 10 per cent saturation 
occurring in the early morning (0500-0600 hours). The pH remained 
fairly constant at around pH 7.35 (Fig. 3). 
On 16 July, after about a week with low levels of dissolved oxygen 
saturation and circumneutral pH values, evidence of a resurgence of 
photosynthesis was observed. Dissolved oxygen rose from 47 per cent 
saturation at 1200 hours to 132 per cent by 2000 hours, with a 
corresponding rise in pH from 7.55 to 9.05. This effectively marked the 
end of the perturbations caused by the crash of the Oscillatoria bloom. 
Possible causes of the collapse of the algal bloom 
The rising trend of chlorophyll-a values (Fig. 2) began to slow around 21 
June, shortly after total oxidised nitrogen effectively became exhausted in 
the loch (Fig. 1). Like most phytoplankters, Oscillatoria is unable to fix 
atmospheric nitrogen (Steinberg & Hartmann 1988). The collapse of the 
algal bloom appears likely to have been caused by this factor, perhaps 
triggered by the peak of photosynthesis noted on 8 July. The conjunction 
of these two events appears to be similar to conditions in the summers of 
1968 to 1971 when Oscillatoria was last present as a major component 
of the phytoplankton (Bindloss 1974; Holden & Caines 1974). The 
removal, from the water column, of a substantial biomass of Oscillatoria 
(and the other phytoplankters present - green algae and diatoms) was 
associated with order of magnitude increases in the concentrations of 
soluble reactive phosphorus, total dissolved phosphorus, and ammonia. 
Dissolved silica, in contrast, declined steeply from 12 July to 2 August. 
Whether this was due to uptake by rapidly growing diatoms or a 
chemical effect is not yet clear. 
Following the crash of the algal bloom, both of the deep "holes" in 
Loch Leven displayed a sharp dissolved oxygen gradient, down to less 
than 5 per cent saturation at 20-metres depth. This persisted into early 
August. Under such conditions further increases in the dissolved 
210 J. A. ARMSTRONG, I. R. FOZZARD AND R. J. SARGENT 
phosphorus concentration might be expected, and samples from 20-
metres depth did confirm significantly raised concentrations compared 
with surface samples. 
The nutrients at the sluices have shown raised levels compared to 
other surface samples on some occasions since the algal crash; it may be 
that water flows from the South Deep Hole site directly to the sluices 
without much mixing. This may also explain the only noted fish kill that 
took place throughout this interesting period, in the afternoon of 13 July. 
This fish kill occurred downstream of the sluices after they had been 
raised, allowing a greater volume of water to flow out of the loch. Brown 
trout (Salmo trutta) and rainbow trout {Oncorhynchus mykiss) were killed 
in the long canal-like "cut" downstream from the loch; the actual 
number of mortalities is not known because some were carried away by 
the high volume of released water, but the total killed was probably less 
than a hundred fish. Brown trout within the loch presumably 
accommodated to the situation by seeking out areas with higher oxygen 
levels, e.g. near inlets or in turbulent areas, and by restricting their 
oxygen consumption for example, by reduced feeding and swimming. 
Acknowledgements 
The authors would like to thank Mr W. Halcrow, Director of the Forth 
River Purification Board, for permission to publish this article and 
colleagues at the Board for their work in collecting and analysing water 
quality samples. Sincere thanks are also due to Dr Tony Bailey-Watts for 
identification of algal species and staff at Scottish Natural Heritage for 
assistance during sampling. 
References 
Bailey-Watts, A. E., Sargent, R J., Kirka, A. & Smith, M. (1987). Loch 
Leven Phosphorus Loading. Institute of Terrestrial Ecology, Edinburgh. 
85 pp. 
Bindloss, M. E. (1974). Primary productivity of phytoplankton in Loch 
Leven, Kinross. Proceedings of the Royal Society of Edinburgh, B74, 
157-181. 
Holden, A. V. & Caines, L. A. (1974). Nutrient chemistry in Loch Leven, 
Kinross. Proceedings of the Royal Society of Edinburgh, B74, 101-121. 
Smith, I. R. (1974). The structure and physical environment of Loch 
Leven, Scotland. Proceedings of the Royal Society of Edinburgh, B74, 
81-100. 
Steinberg, C. E. W. & Hartmann, H. M. (1988). Planktonic bloom-
forming cyanobacteria and the eutrophication of lakes and rivers. 
Freshwater Biology, 20, 279-287. 


Development and collapse of an Oscillatoria bloom in Loch Leven during July 1994

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Development and collapse of an Oscillatoria bloom in Loch Leven during July 1994

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