A mixture of steam and geothermal brine is transported
from the wells to a central separation station. After being separated from
the brine, the steam is piped through moisture separators to steam heat exchangers inside the
plant building. The steam can be piped to steam turbines for co-generation
of electricity. Unutilized steam is released through a steam exhaust.
The heating process
Heat exchangers
Hitaveita Reykjavikur operated a pilot heating plant at Nesjavellir during
1974 - 1990. Various types of heat exchangers have been tested. Conventional
plate heat exchangers are used for the condensation of steam from the separators
and to cool the condensate. They are equipped with EPDM-gaskets and made
of titanium plates to avoid stress corrosion, as it is not possible to
guarantee problem free operation if stainless steel plates are used.
Conventional heat exchangers cannot be used for the separated water due
to the high content of dissolved solids (TDS 1200 PPM) which would cause
severe scaling of silica. A new type of heat exchanger, in the geothermal
context, has been tested successfully in the pilot plant. These are the
so-called "fluidized bed heat exchangers", or FBHX made by Eskla
Heat exchangers BV in the Netherlands. They are shell and tube heat exchangers
operating in a vertical position . Stainless steel balls, 1.5 mm in diameter,
circulate in the flowstream of the separated water. They impact continuously
against the pipe surfaces and remove any scaling that may form. A mechanical
device is fitted to the inlet and outlet of the heat exchangers to keep
the steel balls evenly distributed in the flow stream. The FBHX heat exchangers
make possible the direct utilization of the heat in the water from the
separators and contribute to the overall economy of the heating process.
Deaeration
The cold ground water is saturated with dissolved oxygen and becomes very
corrosive when heated. A conventional thermal deaeration method is used
where the ground water is boiled under vacuum after heating to remove the
oxygen. The cold ground water has a pH-value of 7.5-8.5. It is partially
degassed through boiling after heating. This raises the pH-value to 9.0-9.5
and the oxygen content is reduced down to about 50 ppb. The remaining dissolved
oxygen is removed through injection of small amounts of geothermal steam
that contains acid gases (H2S and CO2). Hydrogen sulfide gas reacts rapidly
with the dissolved oxygen. The final water product then has a pH-value
of 8.5-9.0. It is free of dissolved oxygen, and contains 0.5-2.0 PPM of
H2S. The remaining H2S gas reacts against any oxygen absorption in accumulators
and ensures that the "pleasant smell", which the users of geothermal
water in Iceland have become accustomed to, is retained.
Amorphous Mg-Si scaling was formed in the distribution system in Reykjavik
during the first months of operation of the plant, due to the high pH-value
of the mixture of the geothermal water from the low-temperature fields
and the heated ground water from Nesjavellir. Different ratios of these
two water types control the pH-value. Scaling can only be avoided by reducing
the amount of geothermal water in the mixture below 10-15%. Therefore the
original plan of mixing these two water types in the distribution network
has been abandoned. They will be used separately.
The waste geothermal
water
Geothermal heating plants in high-temperature fields only utilize the thermal
energy of the geothermal fluid, which, after use in heat exchangers. must
be disposed of with minimum risk to the environment. This disposal can
be performed in two different ways, i.e. at surface or into subsurface
aquifers. Surface disposal can be carried out in a similar way to the natural
disposal of flow from the hot springs, i.e. into the brook in the Nesjavellir
valley, which disappears into a lava field before reaching Lake Thingvallavatn.
Subsurface disposal requires that the waste water is pumped back into the
geothermal reservoir. This latter method is obviously more friendly to
the environment but more expensive. It can also be more difficult to operate
due to scaling in the reinfection wells and their aquifers.
There are two important features of the waste water from high-temperature
fields that may have a negative effect on the environment. These are the
raised temperature of surface waters and ground water aquifers and the
presence of hazardous chemicals in the waste water, i.e. arsenic, mercury,
boron, etc. Extensive research has been carried out at Nesjavellir with
respect to disposal of the waste water. Chemical and biological measurements
have been carried out at Lake Thingvallavatn since 1979 to define the pre-exploitation
value for future reference. All the wells at Nesjavellir were flow tested
in 1984-1987 as a part of the exploration program. Large amounts of geothermal
water were disposed of at the surface during these tests without any apparent
effects on water chemistry at the shoreline of the lake. This is in agreement
with the prediction of a ground water model that simulates fluid flow and
distribution of chemicals in the ground water system at Nesjavellir.
Chemical analysis of the geothermal fluid show that dangerous chemicals,
which may be expected from the condensate of the steam phase, are almost
absent.
All arguments seem to indicate that surface disposal of the waste water
can be used for the geothermal power plant at Nesjavellir.
THE GEOTHERMAL POWER PLANT
General outline
Due to scaling, the geothermal fluid from the Nesjavellir
field cannot be used directly in the space heating distribution network.
The
power plant therefore uses the geothermal energy to heat
cold ground water indirectly in heat exchangers. The heated water is treated
so that it can be used directly in the network.
The geothermal power plant at Nesjavellir consists of the following five
sub-systems all of which have separate functions:
The cold water supply
Cold ground water (4°C) is pumped from 30 m deep wells, at Gramelur,
6.2. km north of the power house, in a lava field at the shore of Lake
Thingvallavatn. The nominal capacity of each pump is 278 kg/s, but larger
pumps can be installed. Four wells have been drilled so far with only 5
m spacing.
Pumping tests of up to 600 kg/s have confirmed a very high permeability
of the lava formation. The pumping station is designed so that it can be
enlarged for future developments and house additional wells.
The cold water is piped 6.2 km through a DN 900Æ mm pipe from Gramelur
to the power house. The pipe is made of ductile iron and has the same capacity
as the transmission pipeline to Reykjavik, i.e. about 1900 kg/s. The water
is piped to an 1000 m3 storage tank by the power house, before entering
the heat exchangers and deaerators.
The geothermal
fluid supply
The geothermal fluid supply system gathers the fluid from the production
wells, separates water and steam and then pipes them individually to the
power house.
Figure 15 shows a schematic flow diagram of the system. It includes two
phase pipes from the production wells, separators, pressure control valves
and the mist eliminators by the power house.
The wells discharge a mixture of water and steam, which is transported
along the two-phase pipes to a central separator station close to the power
house instead of a number of separators nearer to the wells. The two-phase
pipes are therefore relatively long, which is made possible by the high
enthalpy of the well fluid and favorable topography.
The dissolved solids are largely confined to the separated water phase,
as steam and water are almost completely (over 99.9%)
separated in the separators. The separator station is situated
400 m away from the power house. The separated steam pipeline is constructed
so that some condensation occurs in the pipe. The condensate washes out
remaining dissolved solids in the steam. It is drained through control
valves on the pipe and the remaining droplets are removed in the mist eliminators.
Three wells (no. NJ-11, 13 and 16) are connected to the separator station
for the first phase, with well NG-6 as a reserve. These wells have a very
high steam fraction (enthalpy 2000 kJ/kg). It was therefore decided to
operate the steam separators at 15 bara, which is an unusually high pressure
for a geothermal power plant. The advantages are smaller pipes and more
efficient electricity generation. Power station II will utilize wells with
lower fluid enthalpy and a lower separator pressure will be more practical,
probably 8 bara.
Vertical separators have hitherto been chosen for steam separation in geothermal
power plants. Nesjavellir is the first one to operate conventional horizontal
separators with Chevron-filters, their main advantages being less height,
hence lower cost for separator building and much easier water level control.
The capacity of each separator equals 35 kg/s or about 50 MWt (at 15 bara).
The mist eliminators are in principle of the same size and type (horizontal)
as the main separators but are fitted with "wire-mesh" filters.
No steam turbine is installed in the first phase of the power plant. The
steam pressure must therefore be lowered in control valves from 15 to 2
bara before entering the heat exchangers. This causes superheating of the
steam and very high noise level due to sonic flow. The control valves are
therefore placed in a separate building. Here, condensate is injected into
the superheated steam to cool it to saturation conditions to protect the
gaskets in the plate heat exchangers.
Electricity generation is planned in phases 2 and 3. The high pressure
steam will then expand in back pressure turbines, down to 2 bara, relieving
the control valves of the high flow load. The exhaust steam from the turbine
will be piped directly to the heat exchangers.
The heat exchangers
The indirect heating of the cold ground water takes place in the heat exchangers.
About 82% of the heat is transferred in the steam heat exchangers. The
condensate heat exchangers cool the condensate from the steam heat exchangers
down to 20°C and add about 14% to the heating process, whereas the
heat exchanger for the separated geothermal water finally contributes only
4% to the heating in the first phase of the power plant.
Steam heat exchangers. Three out of four of the installed steam heat exchangers
have titanium plates, but one of the heat exchangers has plates of ANSI
316 stainless steel for testing the long-term corrosive resistance of this
material. The steam temperature is kept below
120°C (2 bara), the maximum temperature that the EPDM material in the
gaskets can withstand for a longer period. They are manufactured by REHEAT
in Sweden. Each titanium heat exchanger is composed of 329 plates with
a total heat exchange surface area of 280 m2, whereas the stainless steel
heat exchanger has 367 plates and heating surface of 312 m2. The heat transfer
coefficient is stated to be 4300 W/(m2K) for clean plates.
Condensate heat exchangers. The condensate heat exchangers are of the conventional
plate type. They extract the heat of the condensate from the steam heat
exchangers through cooling from about 90 to 20°C. Two heat exchangers
connected in parallel were installed in the first phase of the power plant,
one acts as a reserve. They are manufactured by REHEAT of Sweden. The plates
are made of the ANSI 316 stainless steel and have a heat exchange surface
area of 190 m2
Heat exchangers for the separated water. There are two fluidized bed heat
exchangers (FBHX) connected in series, which transfer heat from the separated
water to the cold ground water. Each FBHX is equipped with 19 steel pipes
(ID 50 mm, length 9 m). These heat exchangers contribute only 4% to the
heating process of the first phase, as stated earlier. They are therefore
installed mainly to obtain operational experience, as they will play an
important role in power station II when the low enthalpy wells will be
connected. The separated water is cooled down to 20-35°C before entering
the waste water system.
Deaeration
of the heated water
The main role of the two deaerators installed in the plant is to remove
oxygen from the heated fresh water. It enters the vessel at the temperature
of 85-88°C and is deaerated through boiling by vacuum pressure down
to 83°C. The main flow enters the central part of the deaerators. The
water boils vigorously as it sprays over the filling material. Steam and
gas rise to the top. There the steam is condensed through injection of
cold water before the gas is ejected. At the bottom of the vessel a small
amount of geothermal steam is injected into the deaerated water to dissolve
hydrogen sulfide. This lowers the pH, rids the water of any remaining oxygen
and acts against oxygen absorption.
The deaerators are made of stainless steel. They are 2.5 m in diameter
and 11 m high. The nominal capacity of each is 278 kg/s of heated water
or 50% of the first phase.
The control system
The computerized control system for the geothermal power plant at Nesjavellir
is identical to the one that is used to supervise and control the pumping
stations for the low-temperature fields and the distribution network in
Reykjavik. This control system was tailor-made for Hitaveita Reykjavikur
[Magnusson and Gunnarsson, 1989]. The advantage of using the same type
of control system is to reduce the investment, training and maintenance
costs.
The data processors. The control system is built around process computers
of the Texas Instruments 565 PC type. They take care of sequence and closed
loop controls. They are situated in the cold water pumping station, in
the transformer station and in the power house. Two process computers are
connected together in the power house in a hot back-up configuration, as
they control the most critical part of the heating process.
The SCADA System. The process computers are connected to a SCADA system
(Supervision Control and Data Acquisition). The SCADA system is based on
a PDP 11/83 computer in the control building at Nesjavellir . Peripherals
such as color screens and printers are located in the control rooms at
Nesjavellir and in Reykjavik . The power plant is operated round the clock
from Reykjavik as the control room at Nesjavellir is usually unmanned.
The peripherals in Reykjavik are connected to the PDP 11/83 computer through
a 64 kbit/s data multiplex and a fiber-optical data link.
The color VDU display system used is of the ABB Tesselator type. One of
the advantages of this system is that it can be connected to the SCADA
computer by modem. The Tesselator system can therefore easily be moved
around, which facilitates all process tests and remote monitoring.
Should the SCADA system fail, the power plant can be controlled from switch
boards that are connected directly to the PC's processors.
The operation of the power plant is fully automated. It can run all day
without any manual intervention, except during breakdowns. A closed loop
control is used at all stages and reserve pumps take over automatically
in case of pump failure. Restarting of the plant after shut-down is at
present done manually but automation will be gradually increased as experience
is gained in the operation.
The process simulator. A computer model has been developed for the dynamic
behavior of the plant. It runs on a PC computer and the whole process is
incorporated into the model. A lot of effort was made to make the program
code as effective as possible for real time simulation.
The simulator consists of a PC computer that simulates the process, a process
computer with the same software as is used for the control system of the
plant and a SCADA system similar to the one used in the power plant. The
process computer program had to be modified to communicate with the PC
computer instead of the sensors and control system of the power plant.
The main advantages of the simulator are expected to be:
· The designers and operators can optimize regulation and control
strategies in a simple way. Tests that are either too risky or time consuming
can be simulated.
· Training of personnel can be carried out without disturbing the
operation of the plant. Both normal operation and various types of breakdowns
can be simulated.
· Development of an expert system for operation and maintenance
of various parts of the system.
Ventilation of
buildings
The atmosphere at Nesjavellir is contaminated with H2S gas from the geothermal
field. Its concentration varies depending on weather conditions, but is
estimated to be around 100 ppb on average. H2S is especially corrosive
for copper and silver, materials that are common in electrical and electronic
equipment. Instruments are therefore largely situated in air-tight buildings
. These buildings are fitted with airlocks and an independent ventilation
system where the hydrogen sulfide gas is absorbed in active carbon filters.
The requirements for the indoor conditions are that the H2S content is
below 3 ppb and relative humidity around 40%.
This is expected to be achieved with the ventilation system by pressurizing
the building up to 100 kPa, recirculating about 85% of the air inside the
building and placing the fresh air intake about 6 m above the roof of the
power house (20 m above ground level).
The power plant buildings have two additional ventilation systems installed.
One is for the visitors' reception hall and the other for the process halls.
Both of these are conventional systems without gas purification but they
use the same fresh air intake.