9 Assuming that interconnected pores in a soil can be represented as a continuouscapillary tubes (Fig. 1), derive h as a function of dand then estimate how high the waterrise in the soil consisting of silt(with pore diameter (d) of 10 µm.)The surface tension ofwater = 72 mN/m. Explain whether this estimation is still valid for tortuous layer structures.p.g. I d→ Y. V=iRainfallܤ ܛ ܐunsaturated soil1i capillary waterWater tableSilth-$-Fig. 1. A structure of the soil consisting of porous silt layers above the water table.Saturated layer

Given values: Soil pore diameter, d = 10 μm Surface tension of water, Ts = 72 mN/m

Assuming that interconnected pores in a soil can be represented as a continuous capillary tubes (Fig. 1), derive h as a function of dand then estimate how high the wate rise in the soil consisting of silt(with pore diameter (d) of 10 μm.)The surface tension o water = 72 mN/m. Explain whether this estimation is still valid for tortuous layer structures Rainfall p.g. Id² h 1 T 1 14 unsaturated soil capillary water Water table Saturated layer Silt → Y. V = Fig. 1. A structure of the soil consisting of porous silt layers above the water table.

Assuming that interconnected pores in a soil can be represented as a continuous capillary tubes (Fig. 1), derive h as a function of dand then estimate how high the wate rise in the soil consisting of silt(with pore diameter (d) of 10 μm.)The surface tension o water = 72 mN/m. Explain whether this estimation is still valid for tortuous layer structures Rainfall p.g. Id² h 1 T 1 14 unsaturated soil capillary water Water table Saturated layer Silt → Y. V = Fig. 1. A structure of the soil consisting of porous silt layers above the water table.

Structural Analysis

6th Edition

ISBN:9781337630931

Author:KASSIMALI, Aslam.

Publisher:KASSIMALI, Aslam.

Chapter2: Loads On Structures

Section: Chapter Questions

Problem 1P

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