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Last modified
1/26/2010 11:38:47 AM
Creation date
10/9/2006 4:32:51 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8062.100
Description
Federal Reserved Water Rights - Division 1
State
1
Basin
Statewide
Water Division
1
Date
6/14/1989
Author
Unknown
Title
Water Information Management System Handbook - Chapter 30 - Procedure for Quantifying Channel Maintenance Flows
Water Supply Pro - Doc Type
Report/Study
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<br />32.8--3 <br /> <br />WATER INFORMATION MANAGEMENT SYSTEM HANDBOOK <br /> <br />5. ~~~ssion~~: For ease of construction, to <br />approximately mimic the natural hydrograph, and to reasonably <br />construct the rise and recession segments of the channel mainte- <br />nance flow hydrograph, this common step incorporates the <br />follow~ng assumptions. <br /> <br />a. Most sediment transport will occur during the period of <br />flow which begins with the occurrence of mean annual discharge <br />and continues through bankfull discharge. <br /> <br />b. Sediment transport will be' provided for in the channel <br />maintenance flow hydrograph if the constructed hydrograph <br />includes bankfull discharge and one-half of the calculated <br />rise-recession flow with most of this flow being distributed to <br />the rising segment of the constructed hydrograph. <br /> <br />c. A recession segment composed of a series of single day <br />decrements in flow will generally prevent adverse streambank <br />effects from rapid drawdown. <br /> <br />If local data and professional judgement indicate the need, the <br />hydrologist should modify this step to make allowance for <br />situations which do not fit the above assumptions. <br /> <br />Considering the segment of the flow-duration curve <br />between the bankfull discharge (QB/QB) ratio point <br />QA/QR ratio point (ex. 2), locate graphically the <br />r~sing-recession flow steps as follows. <br /> <br />that lies <br />and the <br /> <br />(1) Beginning at the Q /Q ratio point on the flow- <br />duration curve, extend a ve~ti~al line down to intersect the <br />0.90 catio level. From this intersection, extend a horizontal <br />line to intersect the flow-duration curve. This becomes the <br />first step of the rise-recession flow component. The duration <br />of this component is determined by converting to days and <br />subtracting the percent time increment limits, in days, of the <br />step (that is, the difference between the bankfull discharge <br />time increment and the 0.90 flow-duration curve intersection <br />point time increment). <br /> <br />___=___u___J2t~:~uc-c-eedin_g--rise-rece-ss~on steps,frid their durations are <br />u"_, u.-uu---determined in If'similar fashion. For example, extend a vertical <br />line from the 0.90 curve intersection point down to intersect <br />. the 0.80 ratio lev~l, then extend a line horizontally to <br />intersect the flow-duration curve. This becomes the second <br />rise-recession flow step. <br /> <br />(3) Proceed in the above manner, using 0.1 decrements in <br />the y-axis ratio levels, until a decrement value falls below the <br />QA/QB ratio. At the QA/QB ratio extend a horizontal <br /> <br />*-FSH 4/89 AMEND 3-* <br />
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