hydrology and IRR Flashcards
Gumbel’s extreme value distribution applied on design flood discharge
Xt = Xm + (Yt -Yn) / Sn Yt = -ln(ln(T / (T-1))) Yn = 0.577 Sn = 1.2825
Slope area method
- find average conveyance K= (k1.k2)^.5
- Hf = h1 -h2 - (velocity head2- velocity head1) *(1- contraction_loss_coeff)
- V1.A1 = K* sqrt( Hf / L)
- Q =V1 * A1
different type of precepetation
-Rain, 0.5mm < d < 6mm, den>2.5mm/hr
-snowfall, combined flakes of ice crystals
average density = 0.1 g /cm^2
-drizzle, d < 0.5mm, density < 1mm/hr
-glaze, sheet on ground
-sleet, frozen rain drops at sub freezing-temp
-Hail, large lumps of size > 8mm
first and last section average width in river discharge calculation when dept and distance to bank is given
W= (W1 +.5*W2)^2 / 2W1
finding discharge without sediment movement
According to SHEILDS equation -critical tractive stress at bottom tau.c = 0.056* γw *d* (S-1) = γw.d/11 for S=2.5 -equate with applied stress tau = γw *R*S -find R
-critical tractive stess on side slopes Tauc' = α *tau.c α = sqrt [ 1- (sinθ /sinΦ)^2 ] -equate with reduced applied stress tau' = 0.75*γw *R*S
canal outlets
non modular
semi modular
rigid moduler
non modular - discharge depends upon dH btween distributary and water course
semi modular- indipendent on water course level, but depends on distributary level
rigid moduler- constant discharge, irrespective of fluctuations either side
flexibility of outlet
flexibility = dQ(of outlet) / dQ (of distributing channel)
proportionality of outlet
when flexibility ==1
senitivity of outlet
sensitivity = dQ / dH (in distributing channel)
efficiency of outlet
ratio = head recovered / Head put in
Setting of outlet
= depth below FSL / depth of FSL
adjustability of outlet
capacity for modification to take into account changed conditions such as silting and scouring of distributing channel
type of floods
standard project flood(SPF) = flood of severe conditions
maximum probable flood(MPF) = catastrophic flood
design flood = flood of desired re-occurrence interval
Maximum flood = peak flow obtained from data
triangular hydrograph depth- discharge relation shortcut
0.18 T*Q = A*d Q= cu.m T = base period in hours A = area Km^2 d = depth in cm
Height of wave depending on Fetch and wind speed
Pressure force generated by wind
hw = 0.032 sqrt(VF) + 0.673 - 0.271 f^0.75
hw = 0.032 sqrt(VF) for F> 32 km
Pw = 2 (water unit weight) .hw^2