Posts

How to draw Isobar / Pressure Bulb

Image
Isobar/Presssure Bulb An imaginary line joining the points having same verticle stress i.e. same verticle pressure. Short Notes:- The isobar is symmetrical about verticle axis (shape is like an onion). The intensity of isobar goes on decreases from top to bottom and along radial distance. The significant depth is the depth upto which 10 percent of isobar (0.1Q) is exist. It is also called as Pressure Bulb and the shape is Spacial Curve/ Lemniscate.(⩉) Procedure To Draw Isobar . If 10% of isobar is to be drawn then (sigma) σz =0.1Q Let σz = Q÷Z ² × KB , putting the value of σz in this equation, Hence KB = 0.1×Z ² Assuming various values of depth (Z) and find out different KB. From Different KB Calculate various value of r/z and hence by knowing different Z find out 'r' Plot 10% of isobar by knowing different Z and r which is symmetric about verticle axis.   ✡Suppose 90% of isobar is to plot then σz = 0.9Q.

Rehbann's / Poncelets Theory

Image
Rebhann (1871) gave this graphical procedure for locating the slip plane and determining the total active earth pressure according to Coulomb’s wedge theory.   Procedure:- 1) Draw A retaining wall having height H i.e. AB 2) Draw three lines   Ground Line ( ß @ with horizontal)                                   Failure Line ∅                                     Earth pressure line  Ψ   3) Through point A Draw a line parallel to Ψ   line which cuts BD line at point C. 4) Through C draw perpendicular line CE which cuts an arc at E. 5) Join BE line consider BE as a radius and B as a center draw an arc through E       which cuts at point F on BD line. Through F draw a line parallel to  Ψ line which       cuts line AD at point G. 6) Consider GF as a radius and F is a centre. Draw an arc through G which cuts BD      at point H. Join GH to form a triangle GHF. 7) Consider GI is a height of triangle that is x. Through point B draw a line

Active earth pressure, passive earth pressure and at rest earth pressure

Image
Active earth pressure, passive earth pressure and at rest earth pressure  

Culmann's Graphical Method to find Active Earth Pressure

Image
Culmann's Graphical Method           Culmann's Curve is the curve use to find Active and Passive Earth Pressure in Retaning wall.  Culmann's curve is drawn using Culmann's Graphical Method. In this article we describe the step by step procedure how to draw culmann's curve and how to find Active Earth Pressure Using Culmann's curve. Procedure: 1) Draw Ground Line , Failure Line & Earth Pressure Line with β, 丫 , ψ angle respectively. 2) Consider any trial wedge ABC 1  and measure length AC 1  as a L 1 3) Calculate the weight of wedge ABC 1  and plot it at point E i.e. BE 1 =L 1 4) Consider all such lines BC2, BC3, BC4, and corresponding points E 1 , E 2 , E 3 , E 4 . 5) Through E 1  draw a line parallel to ψ line which cut's BC 1  at point F 1 . 6) Draw similar lines F 2 E 2 , F 3 E 3 , F 4 E 4 . 7) Draw a smooth curve which passes through B, F 1 , F 2 , F 3 , F 4 . This curve is called as     

Grading and classification of soil

Image
Well graded soil:- It shows good representation of diameter of each particles. Poorly graded soil / Uniformly graded soil:- Single diameter of particle exceed in a soil. eg. Aeoline soil. Gap graded soil :- Sum particles are more in quantity, where sum particles missing in soil.  Grain Soil Distribution Curve   Classification of soil  Diameter / size                                      Soil type   1) <2u                                                           clay 2) 2u - 75u                                                    Silt 3) 75u - 425u                                    Fine sand  4) 425u - 2mm                                   Mid sand 5) 2mm - 4.75 mm                        Fine Gravel 6) 4.75 mm - 20 mm                    Fine Gravel 7) 20mm - 80mm                     Coarse Gravel 8) 80mm - 300mm                               Cobble 9) >300mm                                         Boulder Symbols          Sr.                   Sym

To find Permeability in Stratified Soil deposits when direction of flow is parallel and perpendicular to strata.

Image
To determine equivalent permeability in stratified soil deposits.   (1)  When Direction of Flow is parallel (horizontal) to strata.   The Total discharge Q is the sum of discharge through individual layers (strata) hence Q=Q 1 +Q 2 +Q 3. Let Z 1 , Z 2 , Z 3  within thickness of each layer where as K 1 ,K 2 ,K 3  within coefficient of permeability for individual layers respectively as shown in figure. The piezometric head for each layer remains constant i.e. h=h 1 =h 2 =h 3   Hence equivalent permeability in horizontal direction i.e. 'x' is Kx or KH = K 1 Z 1 +K 2 Z 2 +K 3 Z 3                                                  ---------------------------------                                                              (Z 1 )(Z 2 ) ( Z 3 ) (2)  When Direction of Flow is perpendicular to strata The Total discharge Q remains same through each layers (strata) hence Q=Q 1= Q 2= Q 3. Let Z 1 , Z 2 , Z 3  within thickness