Water surface profiles that are asymptotic at one end and terminated at the other end would include
M2andH2
From dydx=S0−Sf1−Q2TgA3=S01−(yny)10/31−(ycy)3
Using Manning's equation for wide rectangular channel.
(i) As y→y0;dydx→0; i.e. the water surface approaches normal depth line asymptotically
(ii) As y→yc;dydx→∞; i.e. the water surface meets the critical depth line vertically in region 2 and3
(iii) As y→∞;dydx→0; i.e. the water surface meets a very large depth as horizontal asymptote in region 1.
(iv) As y→0;dydx→∞; it means that the surface profile meets the channel bed vertically in region 3
Thus,
M1,M2,S2 and S3meet y0 line asymptotically
(ii) M1and S1 curve tend to horizontal as y→∞
(iii) M2,M3andS2 meet yc line normally
(iv) M3 and S3 meet channel bed normally.
The slope of:
C1 and C3 curve comes out to be equal to critical slope of the bed, if Chezy's equation is used. Otherwise they are slightly curved.