Information and Advisory Note Number 37 Back to menu
1.1 Scotland has some of the most favourable topography, geology and climate for
hydropower in Britain and the available resources have been well utilized over
the last 100 years. This note describes the main types of schemes and some of
the potential impacts on the physical, chemical and biological nature of
Scottish fresh waters. It will become clear that further research is required to
understand existing impacts and identify others. The note also discusses
mitigation measures and the roles relevant organisations have to play A glossary
of terms (words are highlighted in bold in the text) and suggested further
reading are provided at the end.
1.2 Hydropower is a form of energy generation which, unlike coal, oil and nuclear
power, does not normally involve the discharge of polluting chemicals into the
environment.
1.3 Hydropower is regarded as a renewable source of energy and existing Scottish
plant has a capacity to produce 1200 MW of electricity (excluding pumped storage
and independently owned plant). This accounts for about 10% of Scottish demand
and about 2% of the total UK generating capacity. A scheme with a capacity of
100 kW would typically supply enough electricity for about 60 homes.
1.4 Government policy is to stimulate the development and use of renewable sources
of energy (which includes tidal, wave, small-scale hydro and wind energy), and
to work towards 1500 MW of new renewable electricity generating capacity in the
UK by the year 2000. In Scotland, this policy will be implemented through the
Scottish Renewables Obligation by Orders made by the Secretary of State for
Scotland under the Electricity (Scotland) Act 1989
1.5 Although hydropower is regarded as a clean source of power generation, it
can have numerous ecological impacts In the past, the major concern in Scotland
has been for the survival of salmon stocks where hydropower dams have presented
barriers to migration. Additionally, small weirs and dams have partly or wholly
blocked off many small streams, and water transfers have reduced flows.
2.1 Storage
Most Scottish schemes are of the storage type in which water flowing from the
catchment is regulated by a reservoir Water levels in the reservoir and flows
from it are controlled to provide the driving energy for the turbines and to
maintain stream flow below the dam. A good example is the Rannoch power station
on the northern shore of Loch Rannoch (45 MW capacity). The amount of
electricity to be generated is proportional to the volume of water discharged
and the difference in height between the upper reservoir and the turbine
station. These schemes can be very different in size and power output depending
on the climate and terrain
2.2 Pumped
'Pumped storage' schemes have been developed in Scotland from the mid-1960s.
Water is stored at high altitude and is released to a lower loch or reservoir to
drive the turbines and provide power at times of peak demand or to control
frequency on the grid. When demand is light the water is pumped to the upper
reservoir for future use. There are two examples of pumped storage schemes in
Scotland' Cruachan by Loch Awe (400 MW) and Foyers by Loch Ness (300 MW).
2.3 Small-scale
Since the late 1970s the simpler small-scale schemes, generating up to 5 MW,
have become more common Typical small-scale schemes are of the 'run-of-river'
type, which rely on the natural flow of rivers to generate electricity by
utilizing the head of a number of small rivers in steep upland reaches They
generally consist of a small reservoir or head pond, an intake weir, a short
pipeline, and a small power station (Figure 1) They do not store water in wet
periods for use in dry spells, so the output is not constant and only occurs
when there is sufficient water in the river. Small-scale schemes are becoming
favoured over traditional schemes because they are more economical to construct
and maintain, and their impacts on the environment (though still requiring
research) are regarded as more localised than traditional schemes.

2.4 Different hydro power schemes are designed to serve various types of demand
in Scotland. Storage schemes occur throughout Scotland. They are designed for
peak demand and require modest reservoirs. Pumped storage schemes were developed
in the north for domestic and agricultural use, and often require reservoirs
storing about 30-40% of annual run-off to cater for seasonal variations of
rainfall. Small-scale schemes are constructed to supply remote areas in the
north-west and the islands of Scotland, and are the most likely type of hydro
scheme to be developed in the immediate future.
The impacts of hydro schemes are only predictable in general terms Hydro dams
vary
in size and operation, and impounded water may be released from the reservoir
surface, near the bottom, or both These differences influence the impact on the
river The impacts of dams are not exclusively associated with hydropower and can
apply to other schemes involving river regulation, e.g. water supply. For
large-scale hydro schemes assessment should concentrate on the impacts of scheme
operation and maintenance, since it is unlikely that there will be future
development of these schemes in Scotland For small-scale schemes it is also
important to consider impacts during the construction phase, such as siltation
(see paragraphs 3 1.8 and 3.2 4).
3.1.1 Flow changes
Many large-scale dams have transformed shallow, free-flowing rivers into wide,
deep reservoirs which may be several kilometres in length Reservoirs attenuate
flood peaks, so that flow magnitude is reduced and natural river flow variability
downstream is moderated (Figure 2) If flows are reduced from their normal summer
levels, large areas of river bed can become exposed and spray from waterfalls can
be reduced Water transfer between rivers can result in the donor river
periodically drying out, e.g. River Garry, Perthshire

3.1.2 Hydropower releases can result in repetitive and rapid changes in
river
levels (Figure 3), e g the River Tummel below Rannoch power station. Changes in
river flow pattern can be observed across daily, monthly, seasonal and annual
timescales In Scotland, hydropower releases usually enter lochs where water
level fluctuation is small.
On the River Tay, however, hydropower releases have resulted in stage changes 60
km downstream at the tidal limit.

3.1.3 During operation of some small-scale schemes the natural flow regime is
altered by water intake, resulting in locally reduced flood peaks and reduced
flows over waterfalls.
3.1.4 Compensation flows
The compensation water released from a dam is set so that the river flow
downstream does not drop below its natural (unregulated) minimum However, this
does not necessarily mean that it is set to benefit or maintain ecological
interest. Compensation releases do not always reflect natural fluctuations in
river flow, and can result in higher flows during dry periods than would
naturally occur.
3.1.5 Compensation flows are often expressed as a 'Q' value. The 'Q' value is a
percentage which equates to the natural flow exceeded 'Q'% of the time. Hence, a
Q95 release is equal to the natural flow which is exceeded 95% of the time
Compensation flows can vary seasonally. 'Q' values are usually based on
long-term annual flow figures, which can be provided by SEPA (Scottish
Environment Protection Agency).
3.1.6 Freshets
Where flood flows are considered important, particularly in rivers with
migratory fish, artificial flood flows known as 'freshets' may be released at
the request of local DSFBs (District Salmon Fishery Boards) Freshets help to
encourage movement of fish upstream and mitigate ecological damage caused by
artificially prolonged low flows, such as drying out of spawning grounds
Freshets can also be
requested by SEPA to dilute and flush out pollution.
3.1.7 Sedimentation and erosion
Reservoirs act as major sediment traps which
interrupt the natural transport of sediment Rarely has sedimentation led to a
loss of reservoir storage capacity, though some reservoirs infill with sediments
behind dams and have to be purged (e g Fort William scheme). As a result of
sediments being trapped in the reservoir, sediment-free water is released
downstream of the dam at high velocity. This leads to altered patterns of local
and downstream erosion and sedimentation. Scouring of fine sediments from the
river beds and banks is intensified in the reach immediately below a dam, and
high discharge releases can lead to armouring of the stream bed.
3.1.8 In small-scale schemes, the risk of increased sedimentation downstream is
usually greatest during the construction phase. Siltation is not an immediate
problem in steep upland reaches, as silt deposits are likely to be quickly
washed away, but silts can collect lower downstream and alter river morphology.
3.1.9 Temperature
Dams can affect water temperatures both in the reservoirs and in the downstream
channels, especially if the water in the reservoir is stratified or layered In
Scotland the magnitude of temperature modification is suppressed by the
prevailing uniform climate and stratification is unlikely to be a common
occurrence. Some deep Scottish lochs only stratify intermittently in summer,
exhibiting gradual gradients in oxygen and temperature profiles. This can result
in water temperature differences between the reservoir and river. For instance,
small streams may fluctuate by 6-8°C on sunny summer days, but larger water
bodies may vary less than 2-3°C. Such temperature differences in the reservoir
will affect the river downstream when water is released from the dam.
3.1.10 Water chemistry
Hydro schemes involving water transfer may bring about a change in the water
chemistry of the recipient river.
3.1.11 Pollution incidents during construction
and maintenance of different schemes, such
as oil spills from transformers and ancillary
equipment, can have potentially adverse
effects on rivers Oil spills are toxic to biota,
and cause a reduction in light penetration and
increase in biological oxygen demand.
3.2 Potential biological impacts of hydro schemes
3.2.1 The magnitude and type of effects are dependent on the kind of scheme Some
effects may be permanent, and may occur at various distances from an impoundment.
3.2.2 Macrophytes
Some storage reservoirs have resulted in the permanent loss of terrestrial,
wetland and riverine habitat through upstream inundation. Where a fast-flowing
river has been impounded the reduction of light penetration, sedimentation, and
chemical changes in deep water have caused a loss of macrophytes adapted to the
original riverine habitat.
3.2.3 Changes in riparian plant populations may occur downstream as a result of less
frequent and reduced flooding and spray/humidity Water discharged from dams
attenuates natural peak flows which may result in stranding and desiccation of
aquatic flora that require moist conditions Periodic flooding is a vital
component of wetland ecosystems, and the removal or altered timing of natural
flooding can change these highly productive areas into less productive
terrestrial habitats. Generally, colonization by macrophytes below a dam is
dependent on the frequency and magnitude of discharge fluctuations The less
extreme the artificial flow regime, the more successful the retention or
establishment of macrophytes
3.2.4 During construction of small-scale schemes, river-bank engineering,
e.g. digging
trenches for pipelines, may result in the disturbance and permanent loss of
riparian vegetation. In upland reaches removal of bankside vegetation reduces
leaf fall, shading and ambient humidity, and may lead to a reduction in
important bryophyte communities.
3.2.5 Invertebrates
A major problem in reservoirs is drawdown. The rate at which the water level
drops depends on the storage capacity of the reservoir in relation to generation
requirements. In extreme situations most of the stored water is used for power
generation at one time and the drawdown zone of the reservoir is wide. Invertebrates may then become stranded or cannot colonize these areas
permanently, though re-colonization by chironomids and amphipods may be rapid.
3.2.6 Daily flow variation caused by power
station operation can reduce available habitat
and be lethal for species which only survive within specific flow limits. This
can cause a decline in species diversity and abundance. Flow fluctuations also
affect the natural cycle of invertebrate drift. Artificially high flows can
increase invertebrate drift, whereas lower flows may reduce drift.
3.2.7 Altered flows downstream of small-scale schemes can result in reduced habitat
diversity and lead to changes in instream biota which are highly adapted to
local flow conditions. For example, low flows can cause a change from lotic
mayfly species (e.g. Baetis and Rhithrogena) to lentic mayflies, such as Cloeon
and Paraleptophlebia species.
3.2.8 Fish
Alterations to invertebrate and macrophyte communities, caused by hydropower
schemes, can lead to reduced shading and food availability for fish
3.2.9 Dams clearly present a formidable
physical barrier to the movement of migratory
fish, such as salmon, sea trout, eels, and
lampreys, both upstream and downstream.
The Atlantic salmon has an ability to leap
about 3.3 metres which is not nearly enough
to surmount most major hydro dams in
Scotland. Fish passes for such dams are
therefore essential for fish to reach their
spawning grounds and nursery areas.
3.2.10 Migrating fish can become trapped or delayed in pools when a power station
stops operating and may be killed in summer by overheating or become more
susceptible to predation by, e.g. pike, goosanders, and mink. Small-scale schemes
also present restrictions to the movement of fish where there are longer periods
of low flow, or where small weirs and intake pipes block upstream migration.
3.2.11 When a power station is in operation strong currents occur which can draw
downstream migrating fish into the turbine intakes, rather than safely passing
through turbine outlets and fish passes Approximately 10-40% of salmon smolts
may be killed or injured after passing through turbines, depending on the type
and size of turbine blades, and difference between upstream and downstream water
level Smolt screens are used to prevent migratory fish entering the turbines.
However, smolt mortalities may occasionally occur if fish are trapped against
the screens by the force of water being drawn off at the intake.
3.2.12 Salmon and sea trout require clean, fast-flowing water through clean gravel
or small stones to spawn successfully. Reservoirs in upstream areas may have
inundated spawning areas and created silted, static conditions. It is therefore
essential that below a dam compensation flows are adequate to maintain spawning
reaches.
3.2.13 Reservoirs can provide an opportunity for brown trout fisheries to expand and
become more available for exploitation. On the other hand, coarse fish such as
perch or pike may colonize these new and then prey on or compete with trout and
salmon.
3.2.14 Birds, mammals and amphibians
Water level fluctuations in reservoirs can have indirect impacts by removing
habitat and reducing invertebrate and fish food sources for birds such as
black-throated divers Drawdown can have direct effects on wildfowl breeding,
through nests being stranded and possibly abandoned by adults, or the incubating
adult being more susceptible to predation.
3.2.15 Otters are predominantly piscivorous
and changes to fish populations could affect
the carrying capacity of the habitat for this
species. However, there is relatively little
information on the impacts of hydropower
schemes on amphibians or riparian mammals,
though reduced food supply, changes to
natural water level fluctuations and reduced
cover will influence their distribution and
abundance.
4.1 Contingency and management plans can significantly reduce the impacts of
pollution events or prevent accidental release/spillage of pollutants. Sediment
traps can be used to prevent and remove unwanted silt and debris, and oil
interceptors prevent machinery oil from entering drainage systems.
4.2 Most research into mitigating the impacts of hydropower schemes on fresh
waters has concentrated on the important Scottish fishery and fish stock aspects
There has been less effort to investigate practical conservation measures for
mammals, amphibians or birds (though floating islands or nesting rafts for some
bird species have been used to reduce the impacts of water level changes on
their breeding behaviour and success).
4.3 Fish passes and other solutions for migrating fish
There are many designs of fish pass and several methods for deflecting fish from
turbine intakes, all of which have limited success The 'fish ladder1 is a series
of small watery steps which the fish actively surmount when migrating upstream.
A good example can be seen at the Pitlochry Dam.

Borland 'fish lifts' carry the fish upwards as the lift is filled with water,
and the fish continue their upstream journey from the top of the lift. Examples
are at Torr Achilty Dam in the Conon catchment, and Aigas Dam on the River
Beauly

4.3.1 Encouraging fish migrating downstream to enter a fish pass can be a problem if
currents are stronger from turbine intakes, as fish are attracted to faster
currents. One design solution is to locate the fish pass so that downstream
migrating fish encounter it before the intakes' immediate influence become
apparent.
4.3.2 Many power station intakes are fitted with deflector screens or very fine mesh
screens to prevent entry by smolts In extreme cases, migrating fish are caught
and transported by road around some dams, in the Conon River system smolts
migrating downstream were at one time trapped and transported for 32 km by road
to a downstream release point; 99.8% of the smolts survived transport. Recent
developments in turbine design and slower starting-up procedures have minimised
fish damage at many sites. On small streams, downstream migration causes fewer
problems because damage is generally less frequent and escape over spillways or
passes is easier. Some research has involved the possible use of noise screens,
loud underwater noises or even sounds of fish themselves to deter fish from
entering turbine intakes Other research has concentrated on visually attracting
fish to passes and lifts.
5.1 Planning permission
New hydro developments below 1 MW , capacity require local authority planning
permission Schemes above 1 MW capacity require consent from the Secretary of
State (Electricity Act 1989). An environmental assessment may be required for
schemes up to 10 MW (Environmental Assessment (Scotland) Regulations 1988) The
Government has also produced planning guidance and advice for renewable energy
developments. The planning consultation process provides SNH with an opportunity
to comment on impacts affecting the natural heritage.
5.2 Discharge consents
SEPA provides information regarding the setting of compensation flows and sets
discharge conditions (under the terms of the Control of Pollution Act 1974,
amended by the Water Act 1989), and should be consulted for all proposed hydro
developments. The discharge consultation process again allows SNH to comment on
likely impacts on nature conservation interests.
5.3 Nature conservation
SNH is a statutory consultee for hydro development proposals at sites of
international conservation importance (Special Areas of Conservation and Special
Protection Areas), under the Conservation (Natural Habitats, etc.) Regulations
1994 Where a proposal may affect a nationally important site (e.g. Site of
Special Scientific Interest) SNH
should be notified and consulted For proposals likely to affect these sites an
environmental assessment will normally be required SNH policy regarding
renewable energy developments is set out in an SNH Policy Guidance Note (see
further reading)
5.4 Fisheries
Careful planning is required for the protection of all species of fish,
particularly migratory salmon and sea trout Throughout the planning process the
local DSFB (or in its absence, the Scottish Office Inspector of Salmon and
Freshwater Fisheries) should be consulted, especially in the design and location
of fish passes and exclusion devices, such as intake screens The Scottish Office
has published a guidance note on the construction and maintenance of fish passes
and screens for the safe passage of salmon and sea trout This guidance is
provided to aid those who have to implement the Salmon (Fish Passes and Screens)
(Scotland) Regulations 1994. Fish passes may require planning permission from
the local authority, and advice should be sought from SEPA in avoidance of
pollution risks during construction
6.1 One of the major areas for research is the effects of reduced flows on
invertebrates, marginal plants, fish production, and distribution of birds,
amphibians and mammals (especially in the light of possible re-introduction
programmes, e g European beaver)
6.2 As the UK electricity industry continues to evolve, it is possible that some
existing schemes may, in the future, be decommissioned. The potential ecological
effects of any such proposals should be investigated, and this may require
additional research before any decommissioning plans are implemented.
Ancillary equipment - transformers, storage tanks, etc
Amphipods - members of an order of marine and freshwater crustaceans, e g
freshwater shrimp (Gammarus sp)
Armouring tight compaction of the stream bed substrate by high dam discharges
Biological oxygen demand (BOD) -
measurement of the amount of organic pollution in water (high BOD indicates
heavy pollution)
Bryophytes - mosses and liverworts
Carrying capacity - the maximum number of individuals that can be supported
indefinitely by a given part of the environment
Chironomids - family of true flies whose larvae develop in fresh waters
Drawdown - the fall of water in a reservoir, which can lead to a sterile
reservoir margin
Invertebrate drift - the downstream movement of invertebrates in running waters,
which shows natural daily patterns
Lentic - standing water, e.g. a loch or pond
Lotic - running water, e.g. a river or bum Macrophytes - freshwater plants
visible to the naked eye
Piscivorous - fish-eating
Riparian - anything pertaining to the banks of a watercourse
Spawn - to deposit eggs and sperm in prepared gravels (redds)
Spawning grounds - the riverine gravels used for spawning
Stage changes - flow changes recorded on hydrograph
Gilvear, D. J. 1994. River flow regulation. In The Fresh Waters of Scotland. A
National Resource of International Significance. Maitland, P S., Boon, PJ. and
McLusky, D.S. (Eds), 463-487. John Wiley, Chichester.
Johnston, F. G. 1988. Hydropower development on rivers in Scotland Regulated
Rivers: Research and Management. 2, 277-292.
Langford, T.E. 1983. Electricity Generation and the Ecology of Natural Waters.
Liverpool University Press, Liverpool.
Petts, G. E. 1988 (2nd ed). Impounded Rivers: Perspectives for Ecological
Management John Wiley, Chichester. Petts, G.E., and Wood, R. (Eds) 1988.
Regulated Rivers Research and Management. 2
SNH 1996. Policy Guidance Note: Renewable Energy. Edinburgh.
SOAFD 1995. Notes for Guidance on the Provision of Fish Passes and Screens for
the Safe Passage of Salmon. Edinburgh.
SOEnD 1994. National Planning Policy Guideline No.6 Renewable Energy. Edinburgh
SOEnD 1994. Planning Advice Note No.45: Renewable Energy Technologies.
Edinburgh.
Nikki Wood, Scottish Natural Heritage
Dr Terry Langford, Hopehead Ecological Services, Milford-on-Sea, Hampshire.
Nikki Wood
Freshwater Conservation Officer
Dr Philip Boon
Head of Aquatic Environments Branch
Located at
Scottish Natural Heritage
Research and Advisory Services Directorate
2 Anderson Place
Edinburgh EH6 5NP
Telephone: 0131-447 4784