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WSP07348
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Last modified
1/26/2010 2:26:52 PM
Creation date
10/12/2006 2:16:08 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8220.101.09A
Description
Glen Canyon Dam/Lake Powell
State
AZ
Basin
Colorado Mainstem
Date
10/4/1989
Title
GCES Research Plan for the Steady Stream Flow Test
Water Supply Pro - Doc Type
EIS
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<br />. <br /> <br />. <br /> <br />Sampling timing will approximate the movement or a <br />water mass through the system, i.e., staggered <br />downstream at the rour gaging stations used ror <br />discharge measurements. Water samples will be taken <br />rour times per 2~ hrs at each site on days when <br />sampled. <br /> <br />Requirements: <br />Permission rrom NPS to install data collection platrorm <br />at gaging sites (see Stream Discharge section). <br /> <br />Permission rrom NPS to take water samples. <br /> <br />Placement or personnel at gag~ng sites. <br /> <br />~vailability Or cold storage and rapid transport <br />equipment to get samples to analytical laboratory. <br /> <br />~vailability Or qualiried analytical labs to do <br />analyses. <br /> <br />Possible placement or hydrolab on one or more <br />platrorms. <br /> <br />Water Mass Movement <br /> <br />Objectives: <br />Determine the rate at which a particular mass or water <br />moves through the system rrom Glen Canyon Dam to <br />Diamond Creek or Lake Mead. <br /> <br />Justirication: <br />The movement Or peaks and troughs through the system <br />during rluctuating rlows does not correspond with the <br />movement or a particular mass Or water, thus use Or <br />stage discharge measurements are only estimates Or <br />water movement through the system. Nutrient and <br />sediment dynamics Or the system are closely aligned <br />with water mass movement as well as discharge whether <br />fluctuating or constant. Knowing the rate or movement <br />Or a mass or water through the Canyon will make <br />evaluation Or nutrient and sediment dynamics more <br />accurate. Initial measurements or mass movement should <br />be based on constant flows to allow for future <br />comparisons with dirferent fluctuating flows. <br /> <br />Methods: <br />Use of an appropriate inert tracer (e.g., Rhodamine <br />WT). <br /> <br />Tracer will be placed at gage sites on the same day <br />after the system has reached equilibrium (or closest <br /> <br />6 <br />
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