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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />study of endangered razorback suckers being done by the U.S. Geological Survey, the National <br />Park Service, and the U.S. Fish and Wildlife Service under the auspices of the Upper Colorado <br />River Endangered Fish Recovery Program. The load-cell sensor weighs the sediment, water, and <br />air above it, and an accompanying pore-pressure sensor weighs the water and air above it. The <br />difference between the two weights is the weight of the sediment overlying the sensor pair. <br />Combined sensitivity and repeatability are:tO.Ol foot of sediment thickness or less. A temperature <br />sensor in the pressure-sensor housing provides useful information about the spawning-bed and <br />sensor environment and enables calibration of the pressure sensors to :to.02 percent offull-scale <br />output. During August 1998, seven sensor pairs were buried in an array across the bar and the <br />adjacent channel and have provided hourly data to a datalogger (Figure 1). The sensors <br />documented (1) deposition of as much as 0.7 foot of sediment on the spawning bar during the <br />historically determined spawning period and within the historically determined spawning- <br />temperature range, (2) subsequent erosion of the deposited sediment, (3) the migration of dunes <br />0.2 foot in height or less in the channel, (4) passage ofa cobble (or other debris) in the bed load <br />with a scour hole in front of and behind the cobble or debris, and (5) ice-dam buildup with <br />ponding of as much as 5 feet over the bar and subsequent erosion of the ice dam. During October <br />2001, the sensors were replaced with four pairs that were strategically located using recent data <br />from radio tracking offish. In addition, the cables to the datalogger were enclosed in conduit, and <br />the datalogger, which had been vandalized, was replaced. <br /> <br />12,000 <br /> <br />~...~""':'" <br /> <br />o <br />is <br />u <br />w <br />., <br />II: <br />W <br />G. 6.000 <br />m 4,000 <br /> <br />fi1 2.000 <br />:> <br />o <br /> <br /> <br />-0.- <br /> <br />'0,000 <br />8.000 <br /> <br />FlamIng -..- <br /> <br />2 <br />Iii 3.0 <br />~ <br />;!; <br />uS 2,5 <br />g <br />Z <br />~ 2.0 <br />w <br />g S8ns5lj' t; <br />-< ..5 <br />., <br />., <br />W <br />~ 1.0 <br />o <br />I <br />I- <br />!Z 0.5 <br />w <br />:::! <br />is Sensor E <br />:Jl 0 <br /> <br />~.. fobbIe passing over Sensor D: <br /> <br />~~ ==:us::: <br />bui ffl.'/ allsricfllnakup8l : <br />rL ,,' \.. ,-~\" ,......-... ' <br />'_'i. ..... I <br />,iIlf "Il <br />,f"'\ ' 'A, <br />",' ., <br />. , <br /> <br />I- 12 <br />w <br />~ 10 <br />;!; <br />ui <br />" <br />I! <br />., <br />II: <br />w <br />> <br />ii: <br /> <br /> <br /> <br />Sensor G <br /> <br />~ Sensur F <br />- <br /> <br />-- <br /> <br />Figure 1. Streambed deposition Bnd erosion, river stage, and substrate temperature at the razorback <br />sucker spawning bar compared with discharge from Aaming Gorge Dam and river stage and water <br />temperature al the Jensen, Utah. streamftow-gaging station. <br /> <br />7 <br />