GEO-6 Regional Assessment for Africa
phosphorus for future years (2000-2050) (Yasin et al. 2010) . This increases the risk of eutrophication in rivers, which can pose a threat to environmental and human health, affect tourism and lead to loss of livelihoods.
In addition to threats to water quality such as sedimentation, eutrophication and acidification of surface waters, climate change, the decommissioning and removal of dams from waterways, the discharge of chemicals into surface waters, and the identification of new and emerging pathogens pose challenges to maintaining water quality (UNEP/GEMS 2008). Few dams have been decommissioned in Africa, including the Wiken Weeg in the Kruger National Park in South Africa (Wray 2016). The removal of dams, which act as sinks for pollutants and silt, increases pollution loads downstream. However, the increase of dams in Africa both for water supply and energy is beneficial. The quality of freshwater from rivers is also affected by mine-water discharges containing toxic chemicals, though in the West Rand gold field of South Africa, for example, the discharge of acid mine water can, after expensive treatment, help to ensure the return of relatively clean water to the environment. At the same time, the direct flow of untreated mine water through the streams and rivers into the Hartbeespoort Dam may be having a negative impact on irrigation water owing to the concentration of toxic chemicals (Abiye 2014; Abiye et al. 2015). Environmental
contaminants such as the highly persistent organochlorine pesticides (OCPs) which are used in industry and agriculture, especially have deleterious effects on aquatic ecosystems and organisms, as well as bio-accumulate in the fatty tissues of organisms. In Zimbabwe, for example, the use of DDT (dichlorodiphenyltrichloroethane) for control of malaria mosquitoes and tsetse flies was responsible for the high levels found in the Lake Kariba ecosystem (Berg 1995) and accumulated levels in human breast milk (Chikuni et al. 1997)
Due to its hidden nature within rock interstices and fractures, groundwater is less known to consumers, making uncontrolled land-use activities more likely to deteriorate its quality. Shallow groundwater is compromised by poor sanitation through the use of pit latrines. In the Sorou Valley in Burkina Faso, for example, shallow wells that are important local sources of drinking water are highly polluted with coliform levels of 1 x 104 cfu/100 ml, compared to WHO standards of 0 cfu/100 ml (Boubacar et al. 2013). In south- east Botswana, the government is working on the water quality, which deteriorated due to poor sanitation, to make it potable. Naturally high fluoride content, such as in the East African Rift �alley groundwater, makes the water unfit for consumption. In addition, large-scale irrigation and industrial and mining pollution also play a significant role in making groundwater unfit for use by consumers. For example,
West Rand acid mine discharge, South Africa Credit: Tamiru Abiye
60
Mine water treatment facility, West Rand, South Africa Credit: Tamiru Abiye
Page 1 |
Page 2 |
Page 3 |
Page 4 |
Page 5 |
Page 6 |
Page 7 |
Page 8 |
Page 9 |
Page 10 |
Page 11 |
Page 12 |
Page 13 |
Page 14 |
Page 15 |
Page 16 |
Page 17 |
Page 18 |
Page 19 |
Page 20 |
Page 21 |
Page 22 |
Page 23 |
Page 24 |
Page 25 |
Page 26 |
Page 27 |
Page 28 |
Page 29 |
Page 30 |
Page 31 |
Page 32 |
Page 33 |
Page 34 |
Page 35 |
Page 36 |
Page 37 |
Page 38 |
Page 39 |
Page 40 |
Page 41 |
Page 42 |
Page 43 |
Page 44 |
Page 45 |
Page 46 |
Page 47 |
Page 48 |
Page 49 |
Page 50 |
Page 51 |
Page 52 |
Page 53 |
Page 54 |
Page 55 |
Page 56 |
Page 57 |
Page 58 |
Page 59 |
Page 60 |
Page 61 |
Page 62 |
Page 63 |
Page 64 |
Page 65 |
Page 66 |
Page 67 |
Page 68 |
Page 69 |
Page 70 |
Page 71 |
Page 72 |
Page 73 |
Page 74 |
Page 75 |
Page 76 |
Page 77 |
Page 78 |
Page 79 |
Page 80 |
Page 81 |
Page 82 |
Page 83 |
Page 84 |
Page 85 |
Page 86 |
Page 87 |
Page 88 |
Page 89 |
Page 90 |
Page 91 |
Page 92 |
Page 93 |
Page 94 |
Page 95 |
Page 96 |
Page 97 |
Page 98 |
Page 99 |
Page 100 |
Page 101 |
Page 102 |
Page 103 |
Page 104 |
Page 105 |
Page 106 |
Page 107 |
Page 108 |
Page 109 |
Page 110 |
Page 111 |
Page 112 |
Page 113 |
Page 114 |
Page 115 |
Page 116 |
Page 117 |
Page 118 |
Page 119 |
Page 120 |
Page 121 |
Page 122 |
Page 123 |
Page 124 |
Page 125 |
Page 126 |
Page 127 |
Page 128 |
Page 129 |
Page 130 |
Page 131 |
Page 132 |
Page 133 |
Page 134 |
Page 135 |
Page 136 |
Page 137 |
Page 138 |
Page 139 |
Page 140 |
Page 141 |
Page 142 |
Page 143 |
Page 144 |
Page 145 |
Page 146 |
Page 147 |
Page 148 |
Page 149 |
Page 150 |
Page 151 |
Page 152 |
Page 153 |
Page 154 |
Page 155 |
Page 156 |
Page 157 |
Page 158 |
Page 159 |
Page 160 |
Page 161 |
Page 162 |
Page 163 |
Page 164 |
Page 165 |
Page 166 |
Page 167 |
Page 168 |
Page 169 |
Page 170 |
Page 171 |
Page 172 |
Page 173 |
Page 174 |
Page 175 |
Page 176 |
Page 177 |
Page 178 |
Page 179 |
Page 180 |
Page 181 |
Page 182 |
Page 183 |
Page 184 |
Page 185 |
Page 186 |
Page 187 |
Page 188 |
Page 189 |
Page 190 |
Page 191 |
Page 192 |
Page 193 |
Page 194 |
Page 195 |
Page 196 |
Page 197 |
Page 198 |
Page 199 |
Page 200 |
Page 201 |
Page 202 |
Page 203 |
Page 204 |
Page 205 |
Page 206 |
Page 207 |
Page 208 |
Page 209 |
Page 210 |
Page 211 |
Page 212 |
Page 213 |
Page 214 |
Page 215