29
Laboratory Teaching Exercises
Index to Exercises
Exercise A - Rainfall-Runoff Relationships (Storm Hydrographs)
Exercise B - Generation of Overland Flow
Exercise C - Initiation and Characteristics of Bedload Motion
Exercise D - Effect of Changing Stream Power on Channel Morphology
Exercise E - Effect of Base Level Change
Exercise F - Scour in Open Channel Flow
Exercise G - Water Abstraction from a Well in a Confined Aquifer
Exercise H - Water Abstraction from a Well in an Unconfined Aquifer
Exercise I - Water Abstraction from a Number of Neighbouring Wells
Exercise J - Rainfall on a Circular Island with a Central Well
Exercise K - Ground Water Flow between Two Canals With and Without Rainfall
CAUTION:
Although the sand tank cannot move suddenly when adjusting the
elevation, extreme care should be taken when operating the jacks to prevent
crushing of fingers, hands or other objects between the upper and lower frames.
General Equations and Constants
Equations
Discharge (m³/s) = Discharge (l/min) x (50/3)
Average channel depth (or width) (m) = Sum of depths (or widths) (m)
number of
depth (or width) measurements taken
Rainfall Intensity (mm/hr) = ((Rainfall Flow Rate (l/min) x (50/3
Catchment Area
(m²)) x (5/18)
Sediment Transport Rate (kg/ms) = (Sediment Yield (kg)
Time taken (s))
Average width (m)
or
Sediment Transport Rate (kg/s) = Sediment yield (kg)
Time taken (s)
Valley Slope (%) = Reading from scale on end of simulator
Darcy’s Equation =
Thiem’s Equation =
Содержание S12-MKII
Страница 1: ...Advanced Environmental Hydrology System Instruction Manual S12 MKII ISSUE 21 February 2014...
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Страница 8: ...4 Equipment Diagrams Figure 1 Front View of S12 MKII Hydrology System...
Страница 9: ...Equipment Diagrams 5 Figure 2 Plan View of S12 MKII Hydrology System...
Страница 10: ...Armfield Instruction Manual 6 Figure 3 End View of S12 MKII Hydrology System...