![Curve Number Method
• Calculates runoff on the retention capacity of
soil, which is predicted by wetness status
(Antecedent Moisture Conditions [AMC]) and
physical features of watershed
• AMC - relative wetness or dryness of
a watershed, preceding wetness conditions
• This method assumes that initial losses are
satisfied before runoff is generated
)8.0(
)2.0( 2
SP
SP
Q
)4.25(
2540
S
CN
](https://image.slidesharecdn.com/hydrunoff-191113103706/85/Hyd-runoff-29-320.jpg)
Hyd runoff
- 2. • At the end of this section, students will be able to – Explain different types of runoff – Explain the factors affecting runoff – Apply rational method to estimate peak rate of runoff – Estimate the runoff coefficient for a heterogeneous watershed – Estimate time of concentration for a watershed
- 3. • Runoff is the portion of rainfall which flows through the rivers, streams etc. Total Precipitation Precipitation Excess Surface Runoff Infiltration Subsurface Runoff Prompt SSR Delayed SSR Deep Percolation Groundwater Runoff Abstractions Base flowDirect Runoff Total Runoff
- 4. Types of Runoff • Surface runoff – Portion of rainfall (after all losses such as interception, infiltration, depression storage etc. are met) that enters streams immediately after occurring rainfall – After laps of few time, overland flow joins streams – Sometime termed prompt runoff (as very quickly enters streams) • Subsurface runoff – Amount of rainfall first enter into soil and then flows laterally towards stream without joining water table – Also take little time to reach stream
- 5. • Base flow – Delayed flow – Water that meets the groundwater table and join the stream or ocean – Very slow movement and take months or years to reach streams
- 6. Factors affecting runoff • Climatic factors – Type of precipitation • Rain and snow fall – Rainfall intensity • High intensity rainfall causes more rainfall – Duration of rainfall • When duration increases, infiltration capacity decreases resulting more runoff – Rainfall distribution • Distribution of rainfall in a catchment may vary and runoff also vary • More rainfalls closer to the outlet, peak flow occurs quickly
- 7. • Direction of prevailing wind – If the wind direction is towards the flow direction, peak flow will occur quickly • Other climatic factors – Temperature, wind velocity, relative humidity, annual rainfall etc. affect initial loss of precipitation and thereby affecting runoff
- 8. • Physiographic factors – Physiographic characteristics of watershed and channel both – Size of watershed • Larger the watershed, longer time needed to deliver runoff to the outlet • Small watersheds dominated by overland flow and larger watersheds by runoff – Shape of watershed • Fan shaped, fan shaped (elongated) and broad shaped
- 10. • Fan shaped – runoff from the nearest tributaries drained out before the floods of farthest tributaries. Peak runoff is less • Broad shaped – all tributaries contribute runoff almost at the same time so that peak flow is more – Orientation of watershed • Windward side of mountains get more rainfall than leeward side – Landuse • Forest – thick layer of organic matter and undercover – huge amounts absorbed to soil – less runoff and high resistance to flow • barren lands – high runoff
- 11. – Soil moisture • Runoff generated depend on soil moisture – more moisture means less infiltration and more runoff • Dry soil – more water absorbed to soil and less runoff – Soil type • Light soil (sandy) – large pores and more infiltration • Heavy textured soils – less infiltration and more runoff – Topographic characteristics • Higher the slope, faster the runoff • Channel characters such as length, shape, slope, roughness, storage, density of channel influence runoff
- 12. – Drainage density • More the drainage density, runoff yield is more watershedofareaTotal lengthchannelTotal densityDrainage
- 13. Runoff Computation • Computation of runoff depend on several factors • Several methods available – Rational method – Cook’s method – Curve number method – Hydrograph method – Many more
- 14. Rational Method • Computes peak rate of runoff • Peak runoff should be known to design hydraulic structures that must carry it. QPeak = Peak runoff rate (m3/s) C = runoff coefficient I = rainfall intensity (mm/h) for the duration equal to the time of concentration A = Area of watershed (ha) 360 CIA QPeak
- 15. • Runoff coefficient – Ratio of peak runoff rate to the rainfall intensity – No units, 0 to 1 – Depend on landuse and soil type – When watershed has many land uses and soil types, weighted average runoff coefficient is calculated A aC Cw aaa aCaCaC C n i ii w 1 321 332211
- 16. Runoff coefficient for Rational Method
- 17. • Time of concentration (Tc) – Time required to reach the surface runoff from remotest point of watershed to its outlet – At Tc all the parts of watershed contribute to the runoff at outlet – Have to compute the rainfall intensity for the duration equal to time of concentration – Several methods to calculate Tc – Kirpich equation
- 18. • Computation of rainfall intensity for the duration of Tc 385.077.0 02.0 SLTc Tc = time of concentration (min) L = Length of channel reach (m) S = Average channel slope (m/m) h mmorcm T I c DepthRainfall
- 19. • Assumptions of Rational Method – Rainfall occur with uniform intensity at least to the Tc – Rainfall intensity is uniform throughout catchment • Limitations of Rational Method – Uniform rainfall throughout the watershed never satisfied – Initial losses (interception, depression storage, etc). are not considered
- 20. Cook’s Method • Computes runoff based on 4 characteristics (relief, infiltration rate, vegetal cover and surface depression) • Numerical values are assigned to each Steps in calculation • Step 1 – Evaluate degree of watershed characteristics by comparing with similar conditions
- 22. • Step 2 – Assign numerical value (W) to each of the characteristics • Step 3 – Find sum of numerical values assigned ΣW = total numerical value R, I, V, and D are marks given to relief character, initial infiltration, vegetal cover and surface depression respectively DVIRW
- 23. • Step 4 – Determine runoff rate against ΣW using runoff curve (valid for specified geographical region and 10 year recurrence interval) • Step 5 – Compute adjusted runoff rate for desired recurrence interval and watershed location SFRPQPeak ...
- 25. QPeak = Peak runoff for specified geographical location and recurrence interval (m3/s) P = Uncorrected runoff obtained from step 4 R = Geographic rainfall factor (Figures for Sri Lanka) F = Recurrence interval factor (Figures for Sri Lanka) S = Shape factor
- 26. Shape factor for Cook’s method • Table 5.4 Suresh
- 27. Rainfall Factor
- 28. Frequency Factor
- 29. Curve Number Method • Calculates runoff on the retention capacity of soil, which is predicted by wetness status (Antecedent Moisture Conditions [AMC]) and physical features of watershed • AMC - relative wetness or dryness of a watershed, preceding wetness conditions • This method assumes that initial losses are satisfied before runoff is generated )8.0( )2.0( 2 SP SP Q )4.25( 2540 S CN
- 30. Q = Direct runoff P = Rainfall depth S = Retention capacity of soil CN = Curve Number • CN depends on landuse pattern, soil conservation type, hydrologic condition, hydrologic soil group
- 31. • Curve Numbers
- 32. Procedure • Step 1 – Find value of CN using table – Calculate S using equation – Use equation and calculate Q (AMC II) – Use correction factor if necessary to convert to other AMCs) • Three AMC conditions
- 33. Factors for converting AMC II to AMC I or AMR III CN – AMC II Conversion Factor AMC I AMC III 10 0.40 2.22 20 0.45 1.85 30 0.50 1.67 40 0.55 1.50 50 0.62 1.40 60 0.67 1.30 70 0.73 1.21 80 0.79 1.14 90 0.87 1.07 100 1.00 1.00
- 34. • AMC I – Lowest runoff generating potential – dry soil • AMC II – Average moisture status • AMC III – Highest runoff generating potential – saturated soil • Soil A – low runoff generating potential, sand or gravel soils with high infiltration rates • Soil B – Moderate infiltration rate, moderately fine to moderately coarse particles • Soil C – Low infiltration rate, thin hard layer prevents downward water movement, moderately fine to fine particles • Soil D – High runoff potential due to very low infiltration rate, clay soils
- 35. Classification of Streams • Based on flow duration, streams are classified into – Perennial • Streams carry flow throughout the year • Appreciable groundwater contribution throughout the year – Intermittent • Limited groundwater contribution • In rainy season, groundwater table rises above stream bed • Dry season stream get dried – Ephemeral • In arid areas • Flow due to rainwater only • No base flow contribution
- 37. Flow Duration Curve • Gives the variability of stream flow in a year – Arrange stream flow data in descending order – Assign rank number – Calculate plotting position (Probability) – Plot plotting position and discharge 100 1 n m P
- 38. 0 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1 0 20 40 60 80 100 AverageStreamFlow(m3/s) Probability (%)
- 39. • Characteristics of flow duration curve – Steep slope – highly variable flow – Flat slope – little variation in the flow – Flat portion at top of curve – stream has large flood plain – Flat portion at lower end – considerable baseflow
- 40. • Uses of flow duration curve – Discharge for any probability can be known – Variation of flow within a year can be known – Plan water resources projects – Design of drainage structures – Decide on flood control structures to be used – Evaluate hydropower potential – Determine sediment load carried by stream