Energy from the ocean occurs as
wind-driven waves, as wind-driven ocean currents and as lunar
activated ocean tidal changes. There are a range of methods
whereby the various forms of energy may be extracted from the
ocean. At several locations around the world, ocean currents pass
through narrow oceanic straits where submersible marine hydraulic
turbines may be installed to generate power. Water flow speed
invariably increases when ocean water flows from a wide and deep
channel into a narrow and shallow channel. Submersible turbines
operate at higher efficiency when the water passing through them
flows at a higher speed.
The combination of the West Wind Drift and Falkland Current
pushes ocean water through a narrowing channel called Falkland
Sound that separates West Falkland from East Falkland. The channel
is about 1-mile wide at its narrowest (and shallowest) point,
where an undersea hydraulic turbine may be installed. The West
Wind Drift flows through similar channels between islands located
to the south of Tierra del Fuego on the Chilean side of the border
with Argentina. At such locations, power may be generated from
ocean currents at high efficiency (over 25%) and the installations
would have the potential of becoming viable and cost effective.
This method of generate power from the ocean may be modified so as
to involve a tunnel dug under a short stretch of land that
separated 2-bodies of ocean water.
In Newfoundland, Canada, a 5-mile wide stretch of land
separates the northeast corner of Placentia Bay from the southeast
corner of Trinity Bay. A 5-mile long tunnel may be built below sea
level and under this stretch of land to connect the 2-bays. An
ocean current called the North Atlantic Drift along with winds
called the Westerlies push ocean water into Placentia Bay to a
greater height than which occurs in Trinity Bay. A turbine
installed in a tunnel that connects these 2-bays could generate
several hundred kilowatts of power for most of the day. Several
megawatts of power could be generated when the ocean tide rises
sooner in Placentia Bay and also to a greater height than it does
Trinity Bay. It is possible that the cost of building the tunnel
and installing turbines at that location may cost less than the
cost of installing bi-directional submersible water turbines
across the 40-mile wide entrance to Placentia Bay. Below is a
table of the typical times and heights of tides in Placentia Bay
and Trinity Bay.
At another Eastern Canadian location, a 16-mile stretch of land
separates the east-end of Chicnecto Bay which is located at the
east-end of the Bay of Fundy near Amherst, Nova Scotia from
Northumberland Strait. An underground tunnel could be built below
sea level and under the land that lies between these 2-bodies of
water. A hydraulic turbine driving electrical equipment may be
installed in the tunnel. The nature of the ocean currents and
prevailing winds causes water levels in the Bay of Fundy to be
slightly higher than water levels in Northumberland Strait. At
high tide, the difference in the height of water between these
2-bodies of water becomes very greatly pronounced. During low
tide, the tunnel turbine would produce very small amounts of
power. After the tide has risen, the power being generated by the
tunnel turbine would greatly increase.
The technology to build tunnels in the earth is well proven and
is continually being advanced and improved. The cost of building a
16-mile tunnel below sea level and under the land between
Chignecto Bay and Northumberland Strait may be competitive with
the cost of building a control dam and installing submersible
hydraulic turbines across the 40-mile wide entrance to the Bay of
Fundy. The turbine in the tunnel could operate at over 80% energy
conversion efficiency in faster flowing water while many
submersible turbine designs would operate at near 45% efficiency
in slower flowing water. Over time, the higher efficiency of the
tunnel turbine may be able to generate enough revenue from the
sale of electricity so as to be able to justify a higher initial
cost.
At present, a small tidal power generating station has been
built at the mouth of the Saint John River that flows south into
the Bay of Fundy. Another small tidal power station is being
installed at the entrance to the Minas Basin, an inlet located on
the south side of the Bay of Fundy. As high tide approaches, the
flow of ocean water from Chignecto Bay into the tunnel may be
reduced until water levels reach maximum tidal height at Saint
John and in the Minas Basin. At this point, ocean water would
resume flowing through the turbine in the tunnel between Chicnecto
Bay and Northumberland Strait and continue to generate power. The
operation of a turbine in an interconnecting tunnel would be quite
different to the operation of bi-directional submersible turbines.
The interconnecting tunnel would enable power to be generated
from ocean energy in the Bay of Fundy at times other than when the
tide changes. This energy would be the effect of the ocean current
and the Westerlies. The combination of the tunnel turbine(s)
operating in co-ordination with the tidal power stations at Saint
John and at the Minas Basin could make for viable and
cost-competitive ocean energy power conversion in the Bay of
Fundy. At an earlier time, the idea of connecting 2-bodies of
water via a tunnel may have been regarded as impractical. Advances
in tunnel building technology and hydraulic turbine technology
could make the tunnel approach competitive in locations like the
east-end of the Bay of Fundy and between Placentia Bay and Trinity
Bay. Below is a table of typical tidal heights and times in the
Bay of Fundy and Northumberland Strait.
On the other side of the world, New Zealand's West Coast has
2-sites that share similarities to those in Eastern Canada. The
East Australian Current flows parallel to New Zealand's West Coast
while the Nor'Wester winds blow directly toward it and pushes
ocean water into Kaipara Harbour and Manukau Harbour. The east-end
of the Kaipara Harbour is located some 12-miles from New Zealand's
East Coast while nn 8-mile wide stretch of land separates the
east-end of Manukau Harbour from Hauraki Gulf that is also on the
East Coast. Building tunnels under these stretches of land would
allow a base level of electric power to be generated from energy
in the ocean. The narrow entrances to both Kaipara Harbour and
Manukau Harbour can allow for less costly installation of control
gates to hold in the ocean water after the high tide ends. When
the tide is low, the control gates would remain open so as to
allow wind driven ocean currents to enter the harbours and
generate low levels of power.
The harbours at Auckland, New Zealand and Saint John, Canada
are frequented by commercial and recreational marine traffic. If
submersible bi-directional turbines were to be installed at the
entrances to Manukau Harbour and the Bay of Fundy, there would
need to be enough clearance to allow container ships with 45-feet
keels to pass over the turbines at low tide. This means that a
substantial cross section area of the flow of ocean water could
not be used to generate electric power. Under such circumstances,
the tunnel turbine system could compete against submersible
turbines in terms of total power output and also in terms of
energy conversion efficiency.
The tunnel turbine approach may also be able to compete against
submersible turbines in terms of cost at locations where the
entrances to suitable bays is very wide and the tunnel distances
are comparatively short, such as the example at Placentia Bay and
possibly at the Bay of Fundy. Researchers who study power
conversion from the ocean may need to undertake a comprehensive
technical and economic analysis of the respective merits and
drawbacks of each of these technologies. The findings of such
research will determine the optimal installations for Placentia
Bay and the Bay of Fundy in Canada and also Kaipara Harbour and
Manukau Harbour in New Zealand.
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