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Table 5 The characteristics of the upper stream network channel of Khanh waterfall

From: Torrent rainfall-induced large-scale karst limestone slope collapse at Khanh waterfall, Hoa Binh Province, Vietnam

Basic characteristics

Unit

Value

Calculated equation

Width of channel (B)

m

3.00

 

Height of channel (H)

m

2.00

Left slope of channel (1:m1)

 

0.50

 

Right slope of channel (1:m2)

 

0.50

 

Roughness coefficient (n)

 

0.10

 

Slope gradient (l)

%

0.18

 

Peak flow (Q)

m3/s

181.5

 

α

 

0.80

 

Cross-sectional area (A)

m2

8.00

A = H{2B + (m1 + m2)H}/2

Wetted perimeter (P)

m

7.47

P = B + H{(1 + m12)1/2 + (1 + m22)1/2}

Hydraulic radius (R)

m

1.07

R = A/P

Allowable flow (Qmax)

m3/s

3.55

Qmax = I1/2.R2/3.A/n

Peak flow/allowable flow

 

51

Q/ Qmax