Location of pits The pits are placed at the lowest point or corners of intersection of every sub-catchment area in order to collect runoff water. Runoff water would flow to the pits due to gravitational force. Also wales and gutters are connected to those pits accordingly. The runoff water would travel from high contour profile to low contour profile through swales and gutters. Runoff coefficient estimation The runoff coefficient is the coefficient that represents the ratio of runoff against rainfall amount. In the design of an urban area, proportion of impervious area needs to be taken into account. Rainfall could not infiltration into impervious area and rainfall would immediately become runoff if rainfall water fall on those area. Therefore, …show more content…
The discharge or runoff of every sub-catchments are calculated with the equation as shown below. Q=fCIA Where Q = Flow (m3/sec), f = Unit conversion factor = 1/3.6, C= Runoff coefficient, I= Rainfall intensity (mm/hr), A = Area (km2) The rainfall intensity I is determined by the IFD data of Melbourne extracted from the Bureau of Meteorology department. Only the 5 year ARI is considered in our design as the pipe system is designed for 5 year ARI events. Applying the Melbourne IFD equation I=-26.91 ln(t)+128.31 for 5 years ARI, the intensity could then be determined. Time of Concentration Time of concentration represents the time taken for the pits to reach maximum discharge. By knowing the maximum discharge, we could determine the required size of pits. And the time of concentration is determined as the sum of time of overland flow and time of gutter flow. Tc=To+Tg or Tc=To+Ts Where, Tc = Time of concentration, To = Time of overland flow, Tg = Time of gutter flow, Ts= Time of swale …show more content…
After that, the velocity of gutter flow is calculated from the cross-section area found and, then is used to determine the gutter flow time for each sub-catchment. Equations used in calculation are shown as below: Depth of gutter flow, d= ((Q n)/(0.375 F S_o^(1/2) Z))^(3/8) Velocity of gutter flow, v=Q/A (m2/s) Time of gutter flow, T_g=L_g/v (s) The cross section of the gutter is illustrated in Figure 5.1 below. In the design, an assumption on reciprocal cross slope is made which the value of for reciprocal of cross slope is set to be 4 for all gutters in all sub-catchments. Time of swale flow, t_s Manning’s equation is applied for the design of vegetated swales. Q=(AR^(2/3) S^(1/2))/n Where A=area of the sub catchment area (m^2), R=(Cross section of swale)/(Wet perimeter of swale), S=longitudinal slope of swale and n=roughness coefficient of swale The following fixed design perimeters are set in order to facilitate the calculation. Manning's Roughness Coefficient 0.3 Design Width of swale (m) 2.5 m Design Depth of swale (m) 0.3 m Slop of trapezoid
The results shows us that the hypothesis between the river Loughton brook and the erosion shows that it gets wider and deeper due to many reasons such as vertical erosion, lateral erosion, hydraulic action and abrasion of rocks.
How does the bare soil surface type affect the amount of runoff? Speculate why this
There are six different types of water erosion: splash erosion, sheet erosion, rill erosion, gully erosion, valley or stream erosion, and bank erosion. Splash erosion is when raindrops hit soil and small soil particles are displaced. Sheet erosion is when raindrops remove soil in thin layers. During rill erosion, small concentrated flow paths are created. “These paths create a sediment source and delivery system for hillslope erosion. Areas where precipitation rates exceed soil infiltration rates are more prone to this type of erosion. During gully erosion, water flows in narrow channels during or after heavy rains or melting snow. The gullies can erode to considerable depths. Valley or stream erosion is created by water flowing alongside land. It extends downward, deepening a valley, and extending the valley into the hillside. This occurs more frequently
Next, it is necessary to identify the land that is possibly flooded and this can be calculated as:
3. Statements (1) and (2) refer to water amounts. Are these Net or Gross amounts? (1) Crop water
(1) TIME ALLOWED – 3 Hours (2) TOTAL NUMBER OF QUESTIONS – 6 (3) ANSWER ALL QUESTIONS (4) THE QUESTIONS ARE OF EQUAL VALUE (5) THIS PAPER MAY NOT BE RETAINED BY THE CANDIDATE (6) ONLY CALCULATORS WITH AN AFFIXED “UNSW APPROVED” STICKER MAY BE USED (7) STATISTICAL FORMULAE ARE ATTACHED AT END OF PAPER STATISTICAL TABLES ARE ATTACHED AT END OF
Civica will first create the model for future conditions based on the calibrated model. This will involve adding proposed ponds and changing parameter values to reflect the future developments (e.g. imperviousness and curve number).
Another part of it is Sud, which is within the ‘Dargile Formation’ that is formed in the Silurian period(Figure 3). Therefore, the parent materials of both pits are sedimentary and basalt rocks(Figure
Another reason for this scientific assumption is that the Downtown area, which is inundated with impervious covered surfaces, will produce runoff, especially in the event of a flash flood, and will meet in this same area along Clearwater River near Ralston (Keller, 2008, p. 269).
8. From the flow net in Figure 3, the flow rate is calculated as shown
The inflow into the tank was then graphed to show the Inflow vs. Time, the results obtained had some outliers in the initial negative trend so a linear interpolation of the part of the data set
Flow unit = 1 order of 1 dozen the theoretical flow time is 26 minutes. This is
The relevance is given as we need an adequate material to build the dam as well as enough water to achieve a water level and finally to maintain that level. It also should be thought about a solution for the silt coming down the river in order to keep on getting a clear flush.
If injection rates during the latter part of the flood are relatively stable, then 1/Wid function can be approximated by a straight line, which can be fitted by equation of the form:
The engineers who built the barrier need to be able to calculate the maximum force that the water could produce on to each floodgate because it is important