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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.

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