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MCQ
4821. A cylindrical specimen of saturated soil failed under an axial vertical stress of 100kN/m² when it was laterally unconfmed. The failure plane was inclined to the horizontal plane at an angle of 45". The values of cohesion and angle of internal friction for the soil are respectively
0.5 N/mm² and 30°
0.05 N/mm² and 0"
0.2 N/mm² and 0"
0.05 N/mm² and 45"
4822. The ratio of the weight of water to the weight of solids in a given mass of soil, is known
Porosity
Specific gravity
Void ratio
Water content
4823. The shear resistance of a soil is constituted basically of the following component.
The frictional resistance to translocation between the individual soil particles at their contact point
To the structural relation to displacement of the soil because of the interlocking of the particles
Cohesion and adhesion between the surfaces of the soil particles
All the above
4824. A foundation consisting of thick reinforced concrete slab covering area to the bottom of the structure is known as (কাঠামোর নীচে পুরু রিইনফোর্স কংক্রিট প্ল্যাব আচ্ছাদন এলাকা নিয়ে গঠিত একটি ভিত্তিকে বলে)
Combine footing.
Grillage footing
Strap footing .
Raft footing
4825. The consolidation time for soils
Increases with increasing compressibility.
Decreases with increasing permeability
Increases rapidly with increasing size of soil mass
All the above
4826. নিচের কোনটি স্প্রেড ফুটিং এর উদাহরণ ?
অফসেট
ওয়াল ফুটিং
আর সি সি ফুটিং
সব গুলোই
4828. The quantity of seepage of water through soils is proportional to
Coefficient of permeability of soil
Total head loss through the soil
Neither (a) nor (b)
Both (a) and (b)
4829. Select the incorrect statement.
Effective cohesion of a soil can never have a negative value.
Effective angle of internal friction for coarse grained soils is rarely below 30".
Effective angle of internal friction for a soil increases as state of compactness increases.
Effective angle of internal friction is a complicated function of mineralogy and clay size content.
4830. In a purely cohesive soil, the critical centre lies at the intersection of
Perpendicular bisector of slope and the locus of the centre
Perpendicular drawn at 1/3rd slope from toe and the locus of the centre
Perpendicular drawn at 2/3rd slope from toe and the locus of the centre
Directional angles
4831. The weight of a container is and that of container with soil simple, is. If the weight of the container and oven dried soil sample is W3, the moisture content of the soil, is
[(-W3)/(W3-)) x 100
[(W3-)/(-)] × 100
[(-)/(-W3)) x 100
[(-)/(-W3)) x 100
4832. The pressure that builds up in pore water due to load increment on the soil, is termed
Excess pore pressure
Excess hydrostatic pressure
Hydrodynamic pressure
All the above
4834. Coefficient of compressibility is
Constant for any type of soil
Different for different types of soils and also different for a soil under different states of consolidation
Different for different types of soils but same for a soil under different states of consolidation
Independent of type of soil but depends on the stress history of soil
4836. When the measured length is less than the actual length, the error is known as a-
Positive error
Negative error
Instrumental error
Compensating error
4837. If is specific gravity of sand particles, is porosity, the critically hydraulic gradient
ic (G+1)/(1-e)
ic (G+1)/(1+e)
ic(G-1)/(1+e)
ic = (G-1)/(1-e)
4840. In a liquid limit test, the moisture content at 10 blows was 70% and that at 100 blows was 20%. The liquid limit of the soil, is
35%
50%
65%
None of these