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Last modified
7/14/2009 5:02:37 PM
Creation date
6/1/2009 11:34:35 AM
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UCREFRP
UCREFRP Catalog Number
9667
Author
Brouder, M. J. and T. L. Hoffnagle.
Title
Paria River Native Fish Monitoring - 1996-1997 Annual Report.
USFW Year
1997.
USFW - Doc Type
Flagstaff, AZ.
Copyright Material
NO
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<br />Patia River Fish Monitoring Annual Report <br />day. The daily range of temperatures among trips ranged from 16.2° C in July to 4.6° C in <br />November (Trip 98-6). <br />The wide, shallow character of the Paris and the open canyon in which it flows are <br />conducive to wide fluctuations in water temperature. In the summer, the Paris River warms <br />rapidly during the day, as evidenced by a 16.2° C temperature change over the approximately <br />four hours that it took to sample all sites. Since we conclude our sampling by 15:00, the <br />maximum temperature and temperature range of the Paris River is undoubtedly higher. The <br />~ converse is true during winter, when the stream cools rapidly at night. During the December <br />sample, there was ice (2-3 mm thick) along shore and surrounding exposed rocks and frazil ice <br />floating downstream. However, the ice melted by approximately 11:30 and water temperature <br />increased from 0.2° C at 10:40 to 4.9° C at 13:50. Warmer temperatures (5.4° C) were later <br />recorded in the mouth as water from the Paris and Colorado rivers mixed <br />Turbidity <br />In 1998, turbidity in the Paris River ranged from 22.9 NTU in June to 105,500 NTU in <br />July (Table 3). Turbidity tends to be less in the ponded mouth of the Paris River, where the <br />clear water of the Colorado River dilutes the sediment in the Paris and reduced velocity causes <br />the fine sediment to precipitate. <br />Turbidity in the Paris River is mostly dependent upon flooding. At base flow, the Paris <br />is a slightly turbid river, measuring approximately 30 NTU. The Paris River is an alluvial <br />~ stream and drains 3730 kmZ of southern Utah and northern Arizona (Topping 1997). The Paris <br />River is the second largest contributor of sediment to the Colorado River, delivering 23,000 tons <br />of sediment /year (Andrews 1991). Turbidity appears to be used by native fishes as a form of <br />cover -fish are more likely to be captured in shallow water at a turbidity of >30 NTU (Valdez <br />and Rye11995; Arizona Game and Fish Department 1996a). Its characteristic high turbidity and <br />high summer temperature may be a laxge factor in limiting the species diversity of the Paris <br />River. , <br />velocity <br />Velocity was only measured during November. Mean velocity for the 12 sites samples <br />• <br />Hoffnagle 1999, Paris Rivet 1998 Annual Report Arizona Game dt Fish Departrnent 7 <br />
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