logging in or signing up Constructed Wetlands Bioswales and More Jeremiah Download Post to : URL : Related Presentations : Share Add to Flag Embed Email Send to Blogs and Networks Add to Channel Uploaded from authorPOINTLite Insert YouTube videos in PowerPont slides with aS Desktop Copy embed code: (To copy code, click on the text box) Embed: URL: Thumbnail: WordPress Embed Customize Embed The presentation is successfully added In Your Favorites. Views: 281 Category: Entertainment License: All Rights Reserved Like it (0) Dislike it (0) Added: January 03, 2008 This Presentation is Public Favorites: 0 Presentation Description No description available. Comments Posting comment... Premium member Presentation Transcript Constructed Wetlands, Bioswales, and More, Oh my!: Constructed Wetlands, Bioswales, and More, Oh my! Hydraulic Zones: Hydraulic Zones Vegetative Zones: Vegetative Zones Water Quality Considerations: Water Quality Considerations Example: Example Pre-development: 40 acres of ag row crop Post-development 40 acres of commercialSizing for Water Quality: Sizing for Water Quality Rv = 0.05 + 0.009(0.85) = 0.05765 WQv = (1.2*0.05765*40)/12 = 0.2306 ac-ftStorage Volume: Storage Volume For small drainage areas, a preliminary estimate of the storage volume required for peak flow attenuation may be obtained from a simplified design procedure that replaces the actual inflow and outflow hydrographs with the standard triangular shapes shown in Figure 2.2.4-1. The required storage volume may be estimated from the area above the outflow hydrograph and inside the inflow hydrograph, expressed as: VS = 0.5TI (Qi - QO) (2.2.6) Where: VS = storage volume estimate (ft3) Qi = peak inflow rate (cfs) QO = peak outflow rate (cfs) Ti = duration of basin inflow (s) Storage Volume Example: Storage Volume Example VS(1 yr) = 0.5Ti (Qi - QO) 0.5(.4hr*3600sec/hr)(24.7cfs -6 cfs) 13,464 cu ft (.31 ac-ft) Alternate Method: Alternate Method An alternative preliminary estimate of the storage volume required for a specified peak flow reduction can be obtained by the following regression equation procedure (Wycoff and Singh, 1976). (Step 1) Determine input data, including the allowable peak outflow rate, QO, the peak flow rate of the inflow hydrograph, Qi, the time base of the inflow hydrograph, tb, and the time to peak of the inflow hydrograph, tp. (Step 2) Calculate a preliminary estimate of the ratio VS/Vr using the input data from Step 1 and the following equation: (2.2.7) Where: VS = volume of storage (in) Vr = volume of runoff (in) QO = outflow peak flow (cfs) Qi = inflow peak flow (cfs) Tb = time base of the inflow hydrograph (hr) [Determined as the time from the beginning of rise to a point on the recession limb where the flow is 5% of the peak] Tp = time to peak of the inflow hydrograph (hr) (Step 3) Multiply the volume of runoff, Vr, times the ratio VS/Vr, calculated in Step 2 to obtain the estimated storage volume VS. Water Quality Volume: Water Quality VolumeTR-55 (for Detention Storage): TR-55 (for Detention Storage)Slide26: Ag Devel. Commercial Devel.Storage Volume: Storage Volume Examples: Examples Robert Murase – Treatment Plant: Robert Murase – Treatment Plant Murase – Willamette Treatment: Murase – Willamette Treatment You do not have the permission to view this presentation. In order to view it, please contact the author of the presentation.
Constructed Wetlands Bioswales and More Jeremiah Download Post to : URL : Related Presentations : Share Add to Flag Embed Email Send to Blogs and Networks Add to Channel Uploaded from authorPOINTLite Insert YouTube videos in PowerPont slides with aS Desktop Copy embed code: (To copy code, click on the text box) Embed: URL: Thumbnail: WordPress Embed Customize Embed The presentation is successfully added In Your Favorites. Views: 281 Category: Entertainment License: All Rights Reserved Like it (0) Dislike it (0) Added: January 03, 2008 This Presentation is Public Favorites: 0 Presentation Description No description available. Comments Posting comment... Premium member Presentation Transcript Constructed Wetlands, Bioswales, and More, Oh my!: Constructed Wetlands, Bioswales, and More, Oh my! Hydraulic Zones: Hydraulic Zones Vegetative Zones: Vegetative Zones Water Quality Considerations: Water Quality Considerations Example: Example Pre-development: 40 acres of ag row crop Post-development 40 acres of commercialSizing for Water Quality: Sizing for Water Quality Rv = 0.05 + 0.009(0.85) = 0.05765 WQv = (1.2*0.05765*40)/12 = 0.2306 ac-ftStorage Volume: Storage Volume For small drainage areas, a preliminary estimate of the storage volume required for peak flow attenuation may be obtained from a simplified design procedure that replaces the actual inflow and outflow hydrographs with the standard triangular shapes shown in Figure 2.2.4-1. The required storage volume may be estimated from the area above the outflow hydrograph and inside the inflow hydrograph, expressed as: VS = 0.5TI (Qi - QO) (2.2.6) Where: VS = storage volume estimate (ft3) Qi = peak inflow rate (cfs) QO = peak outflow rate (cfs) Ti = duration of basin inflow (s) Storage Volume Example: Storage Volume Example VS(1 yr) = 0.5Ti (Qi - QO) 0.5(.4hr*3600sec/hr)(24.7cfs -6 cfs) 13,464 cu ft (.31 ac-ft) Alternate Method: Alternate Method An alternative preliminary estimate of the storage volume required for a specified peak flow reduction can be obtained by the following regression equation procedure (Wycoff and Singh, 1976). (Step 1) Determine input data, including the allowable peak outflow rate, QO, the peak flow rate of the inflow hydrograph, Qi, the time base of the inflow hydrograph, tb, and the time to peak of the inflow hydrograph, tp. (Step 2) Calculate a preliminary estimate of the ratio VS/Vr using the input data from Step 1 and the following equation: (2.2.7) Where: VS = volume of storage (in) Vr = volume of runoff (in) QO = outflow peak flow (cfs) Qi = inflow peak flow (cfs) Tb = time base of the inflow hydrograph (hr) [Determined as the time from the beginning of rise to a point on the recession limb where the flow is 5% of the peak] Tp = time to peak of the inflow hydrograph (hr) (Step 3) Multiply the volume of runoff, Vr, times the ratio VS/Vr, calculated in Step 2 to obtain the estimated storage volume VS. Water Quality Volume: Water Quality VolumeTR-55 (for Detention Storage): TR-55 (for Detention Storage)Slide26: Ag Devel. Commercial Devel.Storage Volume: Storage Volume Examples: Examples Robert Murase – Treatment Plant: Robert Murase – Treatment Plant Murase – Willamette Treatment: Murase – Willamette Treatment