DHARM
N-GEO\OBJ.PM5 897
OBJECTIVE QUESTIONS 897
- Dupuit, Thiem
- (b)
- k = 100 D 102
- laminar, circular pipe (cylindrical conduit)
- False
- decreases
- False
- False
- the zone above the water–table saturated
by Capillary moisture - False
- (c)
- nf /nd (nf = number of flow channels, nd =
number of equipotential drops); permeabil-
ity. - Unconfined
- Laplace’s
- (a)
- (c)
- j = i.γw (i = hydraulic gradient, γw = unit
weight of water) - decreased
- normally consolidated
- Unity
- (b)
- Cc = 0.009 (wL – 10)
- (a)
- Secondary consolidation
- (b)
- infinite
- (a)
- (d)
- T = (π/4) U^2
- (a)
- (c)
- False
- (i) Interlocking
(ii) friction between individual grains
(iii) Cohesion - Mohr-Coulomb
- (a)
- Hvorselv’s true
- (b)
87. Direct shear test (shear box test)
88. (c)
89. (σ 1 + σ 3 )/2, (σ 1 + σ 3 )/2
90. unconfined compression test
91. (b)
92. (c)
93. dense
94. Critical void ratio
95. overconsolidated or undisturbed sensitive
96. (a)
97. rapid drawdown
98. (b)
99. decrease - central angle
- σz = 3Q/2πz^2
- stress isobar or pressure bulb
- Westergaard’s theory
- False
- q/π
- N.M. Newmark
- Newmark’s chart
- equivalent point load method or (2:1
method) - smaller
- time-rate of settlement and total settlement
- infinite
- centre of the footing
- (b)
- dry density
- smaller
- True
- Higher
- True
- Vibration
- the ratio of dry density obtained in the field
to the Proctor maximum dry density. - (c)
- True
- A little, relatively larger
- Ko = ν
()1−ν
, ν being the Poisson’s ratio of
the soil.