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Total Economic Value of Maasai Mau, Trans Mara and Eastern Mau ...

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the river. Because we did not obtain data on the capacity <strong>of</strong> the water project underconstruction, we assumed that the Sigor water project would provide water to apopulation equal to that <strong>of</strong> Narok town. The water supply to Narok town was thusused as a proxy for measuring the water dem<strong>and</strong> in the Nyangores River. The twomajor urban centres <strong>of</strong> Narok <strong>and</strong> Bomet respectively consume about 18,000m 3 <strong>and</strong>6000m 3 <strong>of</strong> water per day. Thus, the annual dem<strong>and</strong> for water by the population is8,760,000m 3 . With a price <strong>of</strong> KES 200 for the first 6m 3 or KES 33.3 per cubic metre, theurban centres will accumulate KES 291,708,000 (US$ 3,889,440) as gross annual revenue.The total cost <strong>of</strong> running a borehole for a year is given in Table 6.Table 6: <strong>Total</strong> annual cost <strong>of</strong> running a boreholeHouseholds Livestock Irrigation MiningProportion <strong>of</strong> the total dem<strong>and</strong> 20 17 51 3dem<strong>and</strong> for water (m 3 ) 4,800,000 4,080,000 12,240,000 720,000Number <strong>of</strong> boreholes 1,753 1,490 4,470 263Cost <strong>of</strong> constructing a borehole 21,185 21,185 21,185 21,185<strong>Total</strong> cost <strong>of</strong> boreholes 37,139,518 31,568,590 94,705,771 5,570,928Annual cost <strong>of</strong> boreholes (US$) 1,237,984 1,052,286 3,156,859 185,698Annual cost <strong>of</strong> borehole maintenance 1,994 1,994 1,994 1,994<strong>Total</strong> annual cost <strong>of</strong> running a borehole 1,239,978 1,054,280 3,158,853 187,6923.4 Forest Functions for Soil Conservation <strong>and</strong> Water RegulationForests play a major role in soil <strong>and</strong> water conservation, particularly regulation <strong>of</strong> waterflows <strong>and</strong> control <strong>of</strong> floods <strong>and</strong> erosion. Currently, there is scanty information <strong>and</strong> datato enable quantification <strong>of</strong> the contribution <strong>of</strong> forests to soil stabilization <strong>and</strong> waterregulation in the upper catchment areas <strong>of</strong> Kenya. Soil erosion is affected by manyfactors including rain intensity <strong>and</strong> periodicity, soil type, slope, vegetation cover <strong>and</strong>agricultural practices prevailing in the site. It was not possible to estimate the soilconservation functions <strong>of</strong> the forests due to lack <strong>of</strong> quantitative data <strong>and</strong> hence the usebenefit transfer method. Langat <strong>and</strong> Cheboiwo (2010) used data <strong>and</strong> information fromFAO/IISA (1991) to evaluate the potential protective cover <strong>of</strong> Tindiret Forest ascompared to l<strong>and</strong> under maize crop using the yield loss method. Tindiret Forest is part<strong>of</strong> <strong>Mau</strong> Forest Complex so similarity is assumed that justified the use the method toestimate values for the forest blocks.Key assumptions for estimation <strong>of</strong> soil conservation values were the natural forestshave at least 50mm <strong>of</strong> litter layer <strong>and</strong> canopy <strong>of</strong> 75% with 90% <strong>of</strong> the area covered by at35

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