A handy reference for use in geotechnical analysis and design Field Given Below :
1. 𝐼𝑓=𝑊1−𝑤2log10𝑁2/𝑁1
2. 𝐼𝑡=𝐼𝑝𝐼𝑓
3. 𝐶𝑢=𝐷60𝐷10
4. 𝐶𝑐=𝐷302𝐷60𝐷10
5. 𝐼𝑃=0.73 (𝑤𝐿−20)
6. 𝐼𝑃=𝑤𝐿−𝑤𝑃
7. 𝐼𝑠=𝑤𝑃−𝑤𝑆
8. 𝐼𝐿=𝑤−𝑤𝑃𝐼𝑃
9. 𝐼𝑐=𝑤𝐿−𝑤𝐼𝑃
10. 𝐴=𝐼𝑝𝐹 where 𝐹
is clay fraction (Activity)
11. 𝑅𝐷=𝑒𝑚𝑎𝑥−𝑒𝑒𝑚a𝑥−𝑒𝑚𝑖𝑛=1/𝛾𝑑,𝑚𝑖𝑛−1/𝛾𝑑1/𝛾𝑑,𝑚𝑖𝑛−1/𝛾𝑑,𝑚𝑎𝑥
12. 𝑘1𝑘2=tan𝛼1tan𝛼2 (non homogeneous)
13. 𝑘=𝐶𝛾𝑤𝜇𝑒31+𝑒
𝑑2
14. 𝐾=𝑘𝜇𝛾𝑤 (absolute permeability)
15. 𝑘=𝑞𝜋 ln(𝑟2/𝑟1)𝑧22−𝑧12
(Permeability in unconfined aquifer)
16. 𝑘=𝑞2𝜋𝑏 ln(𝑟2/𝑟1)𝑧2−𝑧1 (Permeability in confined aquifer)
17. 𝑘ℎ=𝑘1𝐻1+𝑘2𝐻2𝐻1+𝐻2 (effective horizontal permeability
in stratified soils)
18. 𝑘𝑣=𝐻1+𝐻2𝐻1𝑘1+𝐻2𝑘2 (effective vertical permeability in
stratified soils)
19. 𝑘𝑒=√𝑘ℎ𝑘𝑣 (effective permeability)
20. 𝑘=𝑎𝐿𝐴𝑡lnℎ1ℎ2 (falling head permeability test)
21. 𝑘=𝑞𝐿𝐴ℎ (constant head permeability test)
22. 𝑞=𝑘𝑒 ℎ𝑁𝑓𝑁𝑑 (seepage discharge)
23. 𝜎𝑧=3𝑄2𝜋1𝑧2 (11+(𝑟𝑧)2 )52 (Boussinesq’s formula)
24. 𝜎𝑧=𝑐𝑄2𝜋1𝑧2 (1𝑐2+(𝑟𝑧)2 )32 where 𝑐=√1−2𝜇2−2𝜇
(Wesrwegaard’s formula)
25. 𝜎𝑧=2𝑞𝜋𝑧 (11+(𝑥𝑧)2)2 (line load)
26. 𝜎𝑧=𝑞𝜋(2𝜃+sin2𝜃)
where 𝜃=tan−1𝑏𝑧 (stress under centre of strip load
of width 2𝑏 )
27. 𝜎𝑧=𝑞𝜋(2𝜃+sin2𝜃sin2∅) where 2𝜃=𝛽1−𝛽2 𝑎n𝑑 2∅=𝛽1+𝛽2 ( strip eccentric point)
28. 𝜎𝑧=𝑞(1−cos3𝜃)
where 𝜃=tan−1𝑅𝑧 (stress under centre of circular
load)
29. sin∅=𝜎1−𝜎3𝜎1+𝜎3 (for cohesion less soils)
30. sin∅=(𝜎1−𝜎3)/2𝑐cot∅+(𝜎1+𝜎3)/2 (for cohesive soils)
31. 𝜎1=2𝑐tan𝛼+𝜎3tan2𝛼 where 𝛼=45+∅2
32. tan∅=𝜏𝜎 (shear box test for cohesion less
soils)
33. 𝑇=𝑐 𝜋𝐷2(𝐻2+𝐷6) (if both top and bottom surfaces
contributes)
34. 𝑇=𝑐 𝜋𝐷2(𝐻2+𝐷12) (if only bottom surface
contribute)
35. 𝑆𝑖=𝑞 𝐵 1−𝜇2𝐸 𝐼𝑓 (immediate settlement )
36. 𝑆𝑓=𝑆𝑝(𝐵𝑓𝐵𝑝 𝐵𝑝+0.3𝐵𝑓+0.3)2 (settlement of footing based on plate settlement)
37. Δ𝑢=𝐵(Δ𝜎𝑐)+𝐴𝐵 (Δ𝜎𝑑) (Skempton’s pore pressure parameters)
38. 𝑞=𝑚𝑃+𝑘 is stress path equation where ∅=tan−1𝑚 and 𝑐=𝑘/cos∅
39. 𝐶𝑐=Δ𝑒log10𝜎0+Δ𝜎𝜎0
40. 𝐶𝑐=0.009 (𝑤𝐿−10) (for normally consolidated soil)
41. 𝐶𝑐=0.007 (𝑤𝐿−10) (for over consolidated soil)
42. Δ𝑒1+𝑒0=Δ𝐻𝐻
43. 𝑚𝑣=Δ𝐻/𝐻Δ𝜎0
44. 𝑐𝑣=𝑘𝛾𝑤𝑚𝑣
45. 𝑇𝑣=𝑐𝑣𝑡𝑑2
46. 𝑇𝑣=𝜋4𝑈2 when 𝑈≤0.6
47. 𝑇𝑣=−0.933 log10(1−𝑈)−0.085 when 𝑈>0.6
48. 𝑆𝑓=𝐶𝑐𝐻1+𝑒0 log10𝜎0+Δ𝜎𝜎0
49. 𝑆𝑓=𝐶𝑟𝐻1+𝑒0 log10𝜎𝑐𝜎0+𝐶𝑐𝐻1+𝑒0 log10𝜎0+Δ𝜎𝜎𝑐
50. 𝐴𝑟=𝐷02−𝐷𝑖2𝐷𝑖2
51. 𝑆𝑛=𝑐𝑢𝐹𝛾𝐻
52. 𝑞𝑢=𝑐𝑁𝑐+𝑞 𝑁𝑞+0.5 𝛾
𝐵 𝑁𝛾 (Terzaghi’s strip)
53. 𝑞𝑢=1.3 𝑐𝑁𝑐+𝑞 𝑁𝑞+0.4 𝛾
𝐵 𝑁𝛾 (Terzaghi’s square)
54. 𝑞𝑢=1.3 𝑐𝑁𝑐+𝑞 𝑁𝑞+0.3 𝛾
𝐵 𝑁𝛾 (Terzaghi’s circle)
55. 𝑞𝑢=(1+0.3𝐵𝐿) 𝑐𝑁𝑐+𝑞 𝑁𝑞+(1−0.2𝐵𝐿)0.5 𝛾 𝐵 𝑁𝛾 (Terzaghi’s rectangle)
56. 𝑞𝑢=𝑐𝑁𝑐𝑆𝑐𝑑𝑐𝑖𝑐+𝑞 𝑁𝑞𝑆𝑞𝑑𝑞𝑖𝑞+0.5 𝛾
𝐵′ 𝑁𝛾 𝑆𝛾𝑑𝛾𝑖𝛾 (Meyerhof)
𝐵′=𝐵−2𝑒𝑥 and 𝐿′=𝐿−2 𝑒𝑦
57. 𝑞𝑛𝑢=𝑐𝑁𝑐 (Skempton
𝑁𝑐=5(1+0.2𝐷𝑓𝐵)(1+0.2𝐵𝐿)
Limiting
value of 𝐷𝑓/𝐵 𝑖𝑠 2.5
58. 𝑄𝑢=𝑊ℎ 𝜂ℎ𝑆+𝐶 (ENR) where 𝐶=2.54 𝑐𝑚 𝑓𝑜𝑟 𝑑𝑟𝑜𝑝 ℎ𝑎𝑚𝑚𝑒𝑟 𝑎n𝑑 0.254 𝑐𝑚 𝑓𝑜𝑟 𝑠𝑡𝑒𝑎𝑚 ℎ𝑎𝑚𝑚𝑒𝑟
| Geotechnical engineering basic formulas |
59. 𝑄𝑢=𝑊ℎ𝜂ℎ𝜂𝑏𝑆+𝐶2 (Hiley)
where 𝐶=𝐶1+𝐶2+𝐶3
𝐶1=9.05𝑅𝐴 with dolley and 𝐶1=1.77𝑅𝐴 without dolley and 𝐶2=0.657𝑅𝐿𝐴 𝐶3=3.55𝑅𝐴 𝐿=𝐿𝑒𝑛𝑔𝑡ℎ 𝑜𝑓 𝑃𝑖𝑙𝑒 𝑖𝑛 𝑚 𝑅=𝑃𝑖𝑙𝑒 𝑐𝑎𝑝𝑎𝑐𝑖t𝑦 𝑖𝑛 𝑡𝑜𝑛𝑛𝑒𝑠=0.1𝑄
𝐴=𝑐𝑟𝑜𝑠𝑠 𝑠𝑒𝑐𝑡𝑖𝑜𝑛 𝑎𝑟𝑒𝑎 𝑜𝑓 𝑝𝑖𝑙𝑒 𝑖𝑛 𝑐𝑚2
𝜂𝑏=𝑊+𝑒2𝑃𝑊+𝑃 when 𝑊>𝑃
𝜂𝑏=𝑊+𝑒2𝑃𝑊+𝑃−(𝑊−𝑒𝑃𝐸+𝑃)2 when 𝑊<𝑃𝑒
60. 𝑄𝑢=𝑊ℎ𝜂ℎ𝑆+𝑆02 (Danish) 𝑆0=√2𝜂ℎ𝑊ℎ𝐿𝐴𝐸
61. 𝑄𝑢=𝐴𝑝𝑐𝑁𝑐+𝐴𝑠𝛼 𝑐 (clays)
62. 𝑄𝑢=𝐴𝑝𝑐𝑁𝑐+𝐴𝑠 𝜆(𝜎̅+2𝑐) (clays)
63. 𝑄𝑢=𝐴𝑝𝜎̅ 𝑁𝑞+𝐴𝑠𝜎̅ 𝑘tan𝛿
(sands) 𝜎̅ 𝑖𝑛𝑐𝑟𝑒𝑎𝑠𝑒 𝑢𝑝𝑡𝑜 15 𝑑
𝑑𝑒𝑝𝑡ℎ
64. 𝑄𝑢=𝑁(𝐴𝑝𝑐𝑁𝑐+𝐴𝑠𝛼 𝑐) or 𝑄𝑢=(𝐴𝑔𝑝𝑐𝑁𝑐+𝐴𝑔𝑠 𝑐) (Group)
65. 𝑝𝑎=𝑘𝑎𝜎̅−2𝑐√𝑘𝑎+𝑢
66. 𝑝𝑝=𝑘𝑝𝜎̅+2𝑐√𝑘𝑝+𝑢
67. 𝑘𝑎=1−sin∅1+sin∅ and 𝑘𝑝=1+sin∅1−sin∅
69. 𝑘𝑎=sin2(𝛽+∅)sin2𝛽sin(𝛽−𝛿) (1+√sin(∅+𝛿)sin(∅−𝑖)sin(𝛽−𝛿)sin(𝛽+𝑖))2 (Coulomb’s active )
70. 𝑘𝑝=sin2(𝛽−∅)sin2𝛽sin(𝛽+𝛿) (1−√sin(∅+𝛿)sin(∅+𝑖)sin(𝛽+𝛿)sin(𝛽+𝑖))2 (Coulomb’s passive )
71. 𝑘𝑎=cos𝛽−√cos2𝛽−cos2∅cos𝛽+√cos2𝛽−cos2∅ and 𝑃𝑎=𝑘𝑎𝛾ℎ22cos𝛽
(Inclined backfill)
72. 𝑘𝑝=cos𝛽+√cos2𝛽−cos2∅cos𝛽−√cos2𝛽−cos2∅ and 𝑃𝑝=𝑘𝑝𝛾ℎ22cos𝛽
(Inclined backfill)
73. 𝑁𝑐=15+12(𝑁−15)
𝑤ℎ𝑒𝑛 𝑁>15 𝑎𝑛𝑑 𝑁𝑐=𝑁 𝑤ℎ𝑒𝑛 𝑁≤15 (dilatancy)
74. 𝑖𝑐=𝐺−11+𝑒
(Quick sand condition)
0 Comments
For more Information Please Comment