Table 8.1 Types of weirType
ShapeKnRemarksSharp-crested weirRectangular (Fig. 8.6(a))2/3CdC(2vg)1/2
b3/2beffective width of notch; to measure moderate to
large dischargesCd
(h/
P), where
0.602 and
0.075 forb/B
1
0.592 and
0.011 forb/B
1/2
Triangular (Fig. 8.6(b))8/15CdC(2vg)1/2tan/25/2
included angle; to measure small flowsCdf(h/P,P/B,)0.580.61 (see BSI, 1969a, b, 1986)Compound weirs (Fig. 8.6(c))To measure wide range of flows; sensitive toapproach conditions and submergenceBroad-crested weirRectangular0.544CCdgv
1/2
b3/2To measure large flows; less sensitive to approachconditions and submergenceCdf(h, crest lengthL
,h/b, roughness of the(Table 9.2 and Worked example 9.1)crest)0.850.99 (for recent studies, see Ranga Raju (1993))Spillways:Kandn
values are the same as those of sharp-crested rectangular weirs butCmay vary (Chapter 4)dCrump weirSharp crestedCCdgv
1/2
b3/2Fairly constant value ofC; tod(Water Resourceswith 1:2 upstreammeasure moderate flows; lessBoard, 1970)and 1:5 downstreamsensitive to approachslopesconditions; good prediction(Fig. 8.21)of submerged (non-modular)flows (Worked example 8.3)FlumesVenturi0.544CCdgv
1/2
b3/2bthroat width; to measure wideCdf(L/b
,h/L)0.95–0.99 (see BSI, 1969a, b, 1986)range of flows; copes with sediment andParshall (Fig. 8.7)Kandnvary withdebris-laden flows; increased non-modularsize of flume; designflow range with reasonable estimatestables available(see Bos, 1976)(Bos, 1976)Throatless flume:Kandnvalues are theTo measure moderate flows (seeraised bed (hump) insame as those of broad-Featherstone and Nalluri, 1995)streamcrested weirs; cheapSteep slope streamflume: supercriticalapproach flow: specialflume (Harrison andOwen, 1967)Cvnh
nH
;Hh(^2) Va
/2g
;V
a
Q
/B
(h
P), where
H
is the energy head and
Va
is the approach velocity;
Cv
(
1.0) is a function of the discharge coefficient
Cd
,b
/B
and
h/(
h
P),
where
B
is the channel width and
P
is the height of the sill. Solutions for
Cv
(graphical or analytical) are available (e.g. see BSI, 1969a, b, 1986; Ackers
et al.
, 1978)