142 corresponding load decrements (P kPa) <strong>an</strong>d as obtained for black <strong>clays</strong> in this study are presented in Appendix (B). A summary <strong>of</strong> results <strong>of</strong> percentage swelling under various loading for tested samples is given in Table 7.20. The variation <strong>of</strong> percentage swelling (S) with pressure loads (P) is presented in Fig. (7.34). The variation is generally similar <strong>an</strong>d close for all tested samples, <strong>an</strong>d this once again reflects on the general homogeneity <strong>of</strong> black <strong>clays</strong>. Table 7.20. Percentage swelling <strong>of</strong> black <strong>clays</strong> under various load decrements (S% in relation to ultimate amount <strong>of</strong> swelling Smax). Sample No. S/Smax S (%) P (kPa) P/SP P (%) 0,01 1 82,46 1,00 100 0,1 10 41,23 0,50 50 SA2/70cm 0,24 24 19,99 0,24 24 0,31 31 10,00 0,12 12 0,52 52 5,00 0,06 6 0,7 70 2,50 0,03 3 1 100 0,01 0,00 0 0,01 1 37,48 1,00 100 0,13 13 18,74 0,50 50 SB1/70cm 0,3 30 10,00 0,27 27 0,46 46 5,00 0,13 13 0,66 66 2,50 0,07 7 1 100 0,01 0,00 0 0,01 1 36,23 1,00 100 0,14 14 17,49 0,48 48 SC25/50cm 0,34 34 8,75 0,24 24 0,55 55 5,00 0,14 14 0,73 73 2,50 0,07 7 1 100 0,01 0,00 0 0,01 1 44,98 1,00 100 0,12 12 22,49 0,50 50 SC29/50cm 0,3 30 11,24 0,25 25 0,54 54 5,00 0,11 11 0,72 72 2,50 0,06 6 1 100 0,01 0,00 0
143 Black <strong>clays</strong>: P (kPa) vs S (%) Pressure load P (kPa) 90,00 80,00 70,00 60,00 50,00 40,00 30,00 20,00 10,00 0,00 0 20 40 60 80 100 120 Swelling S (%) SA2/70cm SB1/70cm SC25/50cm SC29/50cm Figure 7.34. Variation <strong>of</strong> percentage swelling <strong>of</strong> black <strong>clays</strong> with loading pressures. A classification <strong>of</strong> the relative degree <strong>of</strong> swelling achieved under various loading pressure decrements for each <strong>of</strong> the soil samples tested is given in Table (7.21). As a result, a general classification for the black <strong>clays</strong> as a whole, has been derived <strong>an</strong>d presented in Table (7.22). It is observed that black <strong>clays</strong> would exhibit high percentage swelling when externally loaded to below 5 kPa; <strong>an</strong>d very low percentage swelling when loaded to over 80 kPa. This implies that external <strong>engineering</strong> structures imposing loads <strong>of</strong> up to 5 kPa <strong>an</strong>d less would still give way to maximum swelling <strong>of</strong> the <strong>clays</strong> on wetting, with a corresponding maximum destabilisation <strong>of</strong> the same structures. However, the structures would be relatively more stable when designed to impose loads <strong>of</strong> over 80 kPa. Table 7.21. Relative degree <strong>of</strong> swelling <strong>of</strong> black <strong>clays</strong> under various load decrements. Swelling degree Sample No. S (%) P (kPa) (after author, 2003) SA2/70cm 100-52 0-4,96 high 52-31 4,96-10 moderate 31-0 10,0-82,46 low SB1/70cm 100-85 0-1,18 high 85-30 1,18-10 moderate 30-0 10,0-37,48 low SC25/50cm 100-75 0-1,70 high 75-34 1,70-8,75 moderate 34-0 8,75-36,23 low SC29/50cm 100-85 0-1,58 high 85-30 1,58-11,24 moderate 30-0 11,24-44,98 low
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AN ENGINEERING GEOLOGICAL CHARACTER
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i Contents Page Acknowledgements Su
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iii Chapter 8. Distribution of inde
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v 7.29 - 7.33 Correlation between s
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vii 136 139 7.13 Compressibility cl
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ix Acknowledgements I would like to
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1 Chapter 1 Introduction 1.1 Scope
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Figure1.1 Map of Nairobi region sho
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5 Plates 1.2 (a) & (b) Strong shrin
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7 Available literature in the form
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9 slopes. The northern boundary bet
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11 1.6 Climate The Nairobi area and
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13 marked daily range of relative h
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15 Chapter 2 Previous works 2.1 Sum
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17 Table 2.1 Stratigraphic correlat
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19 Chapter 3 Geology 3.1 Introducti
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21 metamorphic minerals sillimanite
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25 and prismatic apatite occur as a
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27 Table 3.2 Chemical analyses of s
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29 caused by partial segregation of
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32 could otherwise lead to erroneou
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34 The red soils in this study occu
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36 17 16 15 14 13 12 11 10 9 8 7 6
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38 4.4 Vane test 4.4.1 Introduction
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40 Table 4.1 Classification of soft
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42 The variation of vane shear stre
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44 And thirdly, the field vane appa
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46 horizon, most probably a result
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49 The red friable clays on the who
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51 Results of chemical analyses of
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53 Results of previous soil classif
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55 neighbouring metamorphic areas a
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57 Table 5.10. Profile description
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59 The presence of BaO in the red a
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61 resulted most probably from supp
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63 800 Impulse 700 600 500 SC 17 -5
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65 sericite and chlorite (see next
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67 Q: Quartz (1%) H: Haematite K: K
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69 Plate 6.3. K-feldspar phenocryst
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71 The trachytes generally show a r
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73 Plate 6.16. Organic matter (rema
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75 Plate 6.24. Solution pores/ cavi
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77 Plate 6.29. Iron concretion with
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79 The CS-225 is a micro-processor
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81 The red soils generally exhibit
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83 Chapter 7 Laboratory soils index
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85 According to Johnson and Degraff
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87 Table 7.2. Results of index test
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89 Plate 7.2a. Apparatus for liquid
- Page 103 and 104: 91 Activity chart Plasticity index
- Page 105 and 106: 93 Table 7.3 (continued). Atterberg
- Page 107 and 108: 95 where 7.1.4.4 Results V = volume
- Page 109 and 110: 97 A standard classification of soi
- Page 111 and 112: 99 Table 7.6. Viscosity and density
- Page 113 and 114: 101 Table 7.7, continued. Results o
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- Page 117 and 118: 105 Plate 7.7a. Shear testing showi
- Page 119 and 120: 107 Shear stress / Displacement Cur
- Page 121 and 122: 109 Table 7.10. Distribution and/ o
- Page 123 and 124: 111 illustrated in Figures 7.6, 7.7
- Page 125 and 126: 113 Black clays Cohesion c´ (kN/m
- Page 127 and 128: 115 7.4 Oedometer consolidation tes
- Page 129 and 130: 117 The compound coefficient, K/ρw
- Page 131 and 132: 119 Primary consolidation is a time
- Page 133 and 134: 121 where w (%) = moisture content
- Page 135 and 136: 123 Relationships between values of
- Page 137 and 138: 125 Plate 7.8. Oedometer consolidat
- Page 139 and 140: 127 Cumulative log-time/settlement
- Page 141 and 142: 129 Ranges of values of coefficient
- Page 143 and 144: 131 is most probably due to the ten
- Page 145 and 146: 133 The results of correlation show
- Page 147 and 148: 135 by differences in lithology, mi
- Page 149 and 150: 137 Black clays and red soils Swell
- Page 151 and 152: 139 Testing procedure involved cutt
- Page 153: 141 Black clays Swelling pressure S
- Page 157 and 158: 145 The same relationship is repres
- Page 159 and 160: 147 Alternatively, percentage swell
- Page 161 and 162: 149 Combined sample results: S % vs
- Page 163 and 164: 151 Black clays: Greek method P% =
- Page 165 and 166: 153 partly produced by effects of w
- Page 167 and 168: 155 Chapter 8 Distribution of index
- Page 169 and 170: 157 the study area, respectively. R
- Page 171 and 172: 159 Liquid limit variation; 0,50m a
- Page 173 and 174: 161 Liquid limit (LL) variation (>
- Page 175 and 176: 163 (8.6). The few isolated patches
- Page 177 and 178: 165 Similarly, soil thicknesses of
- Page 179 and 180: 167 Free swell variation; 0,50m dep
- Page 181 and 182: 169 fraction at the two depth inter
- Page 183 and 184: 171 Variation of fines (%), < 0,50m
- Page 185 and 186: 173 %coarse % coarse fraction varia
- Page 187 and 188: 175 1°19´S 22 Shear angle variati
- Page 189 and 190: 177 9.2 Grain size distribution The
- Page 191 and 192: 179 rapid dissipation of pore water
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- Page 197 and 198: 185 On the other hand, laboratory m
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193 Table 10.5, continued. Calculat
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195 Table 10.6. Calculated and labo
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197 The swelling capability in term
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199 Free swell/ clay fraction Free
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201 There has also been a decrease
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203 PI = 1,88*LS A comparison of pl
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205 cc = 0,0099(122-LL) for black c
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207 Chapter 12 Recommendations Anal
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209 cc = 0,0099(122-LL) for black c
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211 References Abebe, S. T., 2002.
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213 Galster, R.W., 1977. A system o
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215 Mitchell, J.K., 1993. Fundament
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217 ------,1964. Long term stabilit
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Appendix A: Oedometer consolidation
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Table A7. Consolidation parameters
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Results of swelling tests on black
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Appendix D Distribution/ variation
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4000 3000 2000 Distance (m) 1000 We
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4000 3000 2000 1000 Distance (m) We
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4000 3000 2000 Distance (m) 1000 We
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4000 3000 2000 Distance (m) 1000 We
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4000 3000 2000 Distance (m) 1000 We
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4000 3000 2000 Distance (m) 1000 We
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4000 3000 2000 Distance (m) 1000 We
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4000 3000 2000 Distance (m) 1000 We
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4000 3000 2000 Distance (m) 1000 We
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4000 3000 2000 Distance (m) 1000 We
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Appendix E Geotechnical soil map of