| For case of two dimensional flows under a straight floor  where:Thus for the first flow line AB which touches the outline of  the floor, the pressure can be obtained by putting different values of x in  equation. Fig shows the pressure distribution diameter both by equation 4 as  well as Bligh's Theory. From the fig the following conclusions can be drawn: Slope of Pressure diagram: At A and B in infinite, hence the  floor at A will be theoretically infinite acting downward and that at B will  also be infinite acting upward. This will cause sand boiling and hence the  floor should be depressed or cut off should be provided at the downstream end. Composite profile:The following specific causes of general form were  considered. 
               Straight horizontal flow of negligible thickness with pile  at either end, upstream or at downstream end.Straight horizontal floor of negligible thickness with pile  at some intermediate point.Straight horizontal floor, depressed below the bed, but with  no cut off. Method of independent variable:
               Most designs do not confirm to elementary profiles (specific  cases). In actual cases we may have a number of piles at upstream level,  downstream level and intermediate points and the floor also has some thickness.Khosla solved the actual problem by an empirical method  known as method of independent variables.This method consists of breaking up a complex profile into a  number of simple profiles, each of which is independently amiable to  mathematical treatment. Then apply corrections due to thickness of slope of  floor.As an example the complex profile shown in fig is broken up  to the following simple profile and the pressure at Key Points obtained.Straight floor of negligible thickness with pile at upstream  ends.Straight floor of negligible thickness with pile at  downstream end.Straight floor of negligible thickness with pile at  intermediate points.The pressure is obtained at the key points by considering  the simple profile. For the  determination of seepage below the foundation of hydraulic structure developed  the method of independent variable.In this  method, the actual profile of a weir which is complex, is divided into a number  simple profiles, each of which cab be solved mathematically without much  difficulty. 
The most  useful profile considered are:
 A  straight horizontal floor of negligible thickness provided with a sheet pile at  the upstream end or a sheet pile at the downstream end. 
 ii) A  straight horizontal floor depressed below the bed, but without any vertical cut-off. 
               A  straight horizontal floor of negligible thickness with a sheet pile at some Intermediate pointThe  mathematical solution of the flow-nets of the above profiles have been given in  the form of curves. From the curves, percentage pressures at various key points  E, C, E1, C1 etc) be determined. The important points to  note are: 
               Junctions  of pile with the floor on either side{E, C (bottom), E1, C1  (top) }Bottom  point of the pile (D), and Junction  of the bottom corners (D, D’) in case of depressed floor The  percentage pressures at the key points of a simple forms will become valid for  any complex profile, provided the following corrections are effected: 
 
               correction  for mutual interference of pilescorrection  for the thickness of floorcorrection  for slope of the floor. Correction  for Mutual Interference of PilesLet b1 = distance between the two  piles 1 and 2, and  D  = the depth of the pile line (2), the influence of which on the neighbouring  pile (1) of depth d must be determined  b = total length of the impervious  floor c = correction due to interference. The  correction is applied as a percentage of the head 
 This  correction is positive when the point is considered to be at the rear of the  interfering pile and negative for points considered in the forward or flow  direction with the interfering pile. Correction  for Floor Thickness Standard  profiles assuming the floors as having negligible thickness. Hence the values  of the percentage pressures computed from the curves corresponds to the top  levels (E1*, C1*) of the floor. However, the junction  points of the floor and pile are at the bottom of the floor (E1, C1) 
 The pressures  at the actual points E1 and C1 are interpolated by  assuming a straight line variation in pressures from the points E1*  to D1 and from D1 to C1 
 The corrected  pressures at E1 should be less than the computed pressure t E1*.  Therefore the correction for the pressure at E1 will be negative.  And so also is for pressure at C1.                  Correction  for Slope of FloorA correction  for a sloping impervious floor is positive for the down slope in the flow direction  and negative for the up slope in the direction of flow. 
               
                 | No. | Slope    = Ver:Horiz | Correction    as % of pressure |  
                 | 1 | 1:1 | 11.2 |  
                 | 2 | 1:2 | 6.5 |  
                 | 3 | 1:3 | 4.5 |  
                 | 4 | 1:4 | 3.3 |  
                 | 5 | 1:5 | 2.8 |  
                 | 6 | 1:6 | 2.5 |  
                 | 7 | 1:7 | 2.3 |  
                 | 8 | 1:8 | 2.0 |  The  correction factor must be multiplied by the horizontal length of the slope and  divided by the distance between the two poles between which the sloping floor  exists.  In the  diagram above, correction for slope can be applied only to point E2.  As the point E2 is terminating at the descending slope in the  direction of flow, the correction will be positive. The value of correction  will be:C.F. x bs/b1
  Where C.F. =correction factor  bs = horizontal length of sloping floor  b1 = horizontal distance  between the pile lines    Exit & Critical Gradient 
 Every  particle of water while seeping through the sub-soil, at any position will  exert a force f, which will be tangential to the streamline at  any point. As the streamlines bend upward, the tangential force f will  be having a vertical component f1. Also at that point,  there will be a downward force W due to the submerged weight of the soil  particle. Thus at that point there will be two forces on the particle; one  upward vertical component of f, and the other, the submerged  weight.  It is evident that if the soil  particle is not to be dislodged, then the submerged weight must be greater than  the upward vertical component of f.  The upward vertical component force at any  point is proportional to  the water  pressure gradient dp/dx.  Hence for  stability of the soil and for the prevention of erosion and piping, the seeping  water when it emerges at the downstream side, at the exit position, the force f1  should be less than the submerged weight W. In other words the exit gradient at  the downstream end must be safe.   If at the  exit point at the downstream side, the exit gradient is such that the force f1is  just equal to the submerged weight of the soil particle, then that gradient is  called critical gradient. Safe exit gradients = 0.2 to 0.25 of the  critical exit gradient. Values of  safe exit gradient may be taken as: 
	         0.14 to 0.17 for fine sand0.17 to 0.20 for coarse sand0.20 to 0.25 for shingle For the  standard form consisting of a floor of a length b, and a vertical cut-off of  depth d, the exit gradient at its downstream end is given by: Exit gradient GE = (H/d) x  |