comparison of environmental aspects of geothermal ... - Orkustofnun
comparison of environmental aspects of geothermal ... - Orkustofnun
comparison of environmental aspects of geothermal ... - Orkustofnun
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Report 17<br />
During implementation <strong>of</strong> this project,<br />
there was no <strong>environmental</strong> law for<br />
guidance and no mandatory Environmental<br />
Impact Assessment process<br />
project proposals. The project activities<br />
were however bound by and undertaken<br />
in line with a memorandum <strong>of</strong><br />
understanding signed between KenGen<br />
and the Kenya Wildlife Service (KWS),<br />
who are custodians <strong>of</strong> all national parks<br />
and nature reserves in Kenya. However,<br />
from the early 1990s, most power<br />
projects were subject to the EIA process<br />
which are a mandatory condition by<br />
financiers such as World Bank,<br />
International Monitory Fund (IMF) and<br />
regional financial institutions.<br />
417<br />
Mwawughanga<br />
4.2.2 Nesjavellir <strong>geothermal</strong> electric<br />
power project in Iceland<br />
Nesjavellir power plant is located within<br />
the Nesjavellir <strong>geothermal</strong> field, which<br />
is along the northern margin <strong>of</strong> the hightemperature<br />
thermal anomaly associated<br />
with the Hengil central volcano in SW-<br />
Iceland, as shown in Figure 4. The<br />
power plant is operated by Orkuveita<br />
Reykjavíkur (Reykjavík Energy).<br />
Annual precipitation averages 2,780<br />
mm/year and mean annual temperature<br />
is 2.9°C. The project is located FIGURE 3: Location <strong>of</strong> the Olkaria 1 power plant<br />
southwest <strong>of</strong> Lake Thingvallavatn<br />
in the East African Rift valley<br />
which is under protection, and activities<br />
<strong>of</strong> the power project may affect the lake since waste brine is disposed <strong>of</strong> in an open stream which<br />
disappears underground and emerges as springs at the lake. The vegetation in the area is characterised<br />
by mosses, grasses, shrubs, and woodland in some areas. The vegetation is poor due to over-utilization<br />
in the past and soil erosion rampant in the upper areas due to the sensitivity <strong>of</strong> the soils.<br />
The depth <strong>of</strong> production wells for electricity production ranges from 1000 to 2200 m and the temperature<br />
in the production wells is in the range 320-360°C. The electric power plant has an installed capacity <strong>of</strong><br />
90 MWe. Prior to the commissioning <strong>of</strong> the electric power plant in 1998, Nesjavellir produced 200 MWt<br />
<strong>of</strong> hot water for district heating purposes only for Reykjavík. In 1998, two 30 MWe turbine generators<br />
were installed and modifications made to the thermal plant (Gíslason, 2000). Another 30 MWe turbine<br />
generator was installed in 2000.<br />
The concept <strong>of</strong> the plant was to co-generate electricity for the national grid, and water for district heating.<br />
Exhaust steam is used to preheat fresh water in condensers. The separated <strong>geothermal</strong> water is used in<br />
heat exchangers to heat preheated water to the required temperatures. The heated water is then treated in<br />
de-aerators to suit requirements <strong>of</strong> the distribution system. Thus, water and steam are used in the most<br />
economic way while lowering the temperatures <strong>of</strong> waste water considerably, reducing thermal impacts<br />
on the environment.