Original source · versioned page text
24647 Seaview Tce Enviro Mgmt Plan
Attached to the e-mail MCU14/0084 Environmental Management Plan (71 Seaview Tce).
The original of this document is very large (18.0 MB). Opening the original or downloading it may take a few minutes. Please be patient and don't click again. The page text is quick to read. If you are on mobile data, it is best to wait until you are on Wi-Fi.
This document appears to be plans or drawings. Its page text below holds only the words printed on the drawings, without the drawings themselves, so it may be jumbled or hard to follow. To see the plans as drawn, choose Original above or download the file (both need you to log in).
Log in to see the plans as drawnSediment Basin Spillway Design Information Peak Flow Qy = (Cy x Itc,y x A)/360 Equation 1 (IECA 2008) Where: Qy= Peak flow rate (m3/s) of average recurrence interval (ARI) of Y years Cy= runoff coefficient (dimensionless) for ARI of Y years Job No. 17SUN-0024 Itc,y= Average rainfall intensity (mm/hr) for design duration of tc hours and ARI of Y years. Client HUTCHINSON A= Area of catchments (ha) Job 71 SEAVIEW TERRACE 360= Conversion Factor Date 3/8/2016 Wier (Minor friction loss over spillway crest and approach channel) Refer to Figure 1 Water level in sediment basin solved using equation below using trail and error. Q = 1.7bH1.5 + 1.26mH2.5 Equation 2 (IECA 2008) H 1 Where Q= Peak flow rate (m3/s) of average recurrence interval (ARI) of Y years (calculated using Equation 1) b= Base width of wier m H= Water level within Sediment Basin relative to spillway (weir) crest (m) b Figure 1 Wier Profile Chute Refer to Figure 2 Flow height is solved by trial and error using the three equations below as per IECA 2008. Q = 1/n x A x R2/3 x S1/2 Equation 3 (IECA 2008) Where Q= Peak flow rate (m3/s) of average recurrence interval (ARI) of Y years n= Mannings coefficieint (unitless) A= Cross sectional area of flow (m2), refer to Eqaution 4 R= Hydraulic Radius (m), refer to Equation 5 S= Slope of energy line, equal to slope of chanel bed (m/m) A = (b + xy)y Equation 4 (IECA 2008) Where A= Cross sectional area of flow (m2) b= Base width of channel (m) x= side slope of channel y= depth of flow in channel (m) + required 0.30m freeboard R = ((b + xy)y) / (b+2y(1+x2)1/2) Equation 5 (IECA 2008) Where R= Hydraulic radius of flow (m) Figure 2 Cross-section of Chute b= Base width of channel (m) x= side slope of channel y= depth of flow in channel (m) + required 0.30m freeboard Energy Dissipator Refer to Figure 3 d50 Median Rock Diametre (mm) Table 5 of IECA 2008 Fact Sheet "Chutes Part 1" Figure 3 Energy Dissipator W1= Width 1 (m)=(b+2xy)+0.6 W2= Width 2 (m)=(b+2xy)+0.4L L= Length of dissipator (m) Table 6 of IECA 2008 Fact Sheet "Chutes Part 1" R calculation & Velocity Check Base Batter Depth Area (m²) P (m) R D50 Velocity Max V Total Site (compacted) 5 2 0.021 0.105882 5.09391486 0.02 200 1.78 2.23 0 0 2 #N/A #N/A #N/A #N/A 200 #N/A 2.23 0 0 2 #N/A #N/A #N/A #N/A 200 #N/A 2.23 0 0 0 0.000 0 0 #DIV/0! 200 0.00 2.23 Peak Flow (Entering Basin) Wier Chute Energy Disipator Minimum Required Upstream Chute Maximum Horizontal Height with Base width water level Channel Channel Depth with Permissable Sediment Basin Slope of 0.30m (m) relative to Label C50 Itc,y Tc A Q20 Wier Freeboard Base Width Side Slope Slope Flow 300mm Velocity Velocity Mean rock size, d50 Wier (m) (m) Length (m/m) Proposed Lining Mannings Peak Flow Depth (m) Feeboard (m/s) (m/s) (mm) Width 1 (m) Width 2 (m) Length (m) (m) H+ b m H freeboard b x So n Q y y+0.3m Vmax V d50 W1 W2 L Total Site (compacted) 1.012 291 5 0.23 0.19 5.00 2.00 0.07 0.37 5.00 2 0.2500 Coir Mat TMC7 0.0220 0.188 0.021 0.321 3.30 1.78 100.000 5.684 5.484 1.000 - #VALUE! 0.00 2 0.2500 Rock R200, D100 (0.5) 0.0600 0.000 #N/A #N/A 1.58 #N/A #N/A #N/A #N/A #N/A
See the original
The page text is free to read. Viewing or downloading an original file needs an account.
Log in to see the originalVery large file: the download may take a few minutes. If you are on mobile data, it is best to wait until you are on Wi-Fi.
Searchable page text hides email addresses. Original files are unchanged and may show email addresses.