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Last modified
7/14/2009 5:02:36 PM
Creation date
5/22/2009 5:08:36 PM
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UCREFRP
UCREFRP Catalog Number
9592
Author
Mueller, G. A., J. Carpenter and P. C. Marsh.
Title
Cibola High Levee Pond Annual Report 2004.
USFW Year
2004.
USFW - Doc Type
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<br />INTRODUCTION <br /> <br />The Cibola High Levee Pond (CHLP) study is a cooperative project with the goal of describing <br />the early life history and habitat requirements of the bonytail (Gila elegans) and razorback <br />sucker (Xyrauchen texanus). CHLP represents the only location where both species are <br />successfully producing young. The resulting information will be used to duplicate CHLP on a <br />larger scale to benefit these species elsewhere. <br /> <br />This report is organized into six sections. They include: <br />· Physical water quality parameters, <br />· Preliminary analysis of recapture data, <br />· Cover utilization of bony tail, <br />· Predator tank tests, <br />· Miscellaneous studies, <br />· And management recommendations. <br /> <br />1. PHYSICAL WATER QUALITY MEASUREMENTS <br /> <br />Physical water quality parameters were measured at 0.5 m depth intervals through the vertical <br />water column during most field trips. Measurements were taken at the pond's deepest location <br />which was approximately 15 m west of the river levee. Parameters were measured using a <br />Hydrolab@ and included: temperature, dissolved oxygen, pH and conductance. A Peabody/Ryan <br />paper chart recorder was placed near the southern shoreline to record surface temperatures. <br /> <br />~onductance - Salinity at CHLP fluctuates seasonally in response to river flow. Conductance <br />peaked at 11 06 ~S/cm in January and gradually declined to 980 ~S/cm in June (Figure 1). Pond <br />conductance is directly linked to evaporation and water exchange rates from the river. Its cyclic <br />nature demonstrates the hydraulic connectivity of these two bodies of water. It is speculated that <br />higher spring flows may increase the hydraulic pressure and volume of groundwater entering the <br />pond from the river and exiting toward Pretty Water. Pronounced evaporation by mid-summer <br />(July) combined with decreasing flows in late fall causes salinity to rise. This water exchange <br />maintains lower pond salinity than what would be expected if the site was hydraulically isolated <br />(BR 2004). <br /> <br />Conductance IJS/cm <br /> <br />. <br />c.. <br /> <br />1150 <br />1100 <br />1050 <br />1000 <br />950 <br /> <br />.... <br />~ <br />........ <br />.............. <br />......... <br />.... <br /> <br />1/27 2/24 3/10 4/26 5/4 5/19 6/23 7/27 <br /> <br />Figure 1. Surface conductance (~S/cm) taken at Cibola High Levee Pond during 2004. <br /> <br />2 <br />
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