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Last modified
7/14/2009 5:02:31 PM
Creation date
5/20/2009 3:42:40 PM
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UCREFRP
UCREFRP Catalog Number
7798
Author
Richardson, S.
Title
Conceptual Management Plan for Razorback Sucker Habitat Enhancement in Flooded Bottomlands, Escalante Ranch, Jensen, Utah.
USFW Year
1994.
USFW - Doc Type
\
Copyright Material
NO
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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 />spring may be highest due to the effects of evaporation. The <br />conductivities measured at this site should not provide any major <br />constraints to development. High conductivity may actually prove <br />to be advantageous for razorback sucker habitat development as <br />invertebrate production is generally enhanced by high . <br />conductivities. <br /> <br />Patterns of sodium (Na+) concentrations are similar to <br />conductivity patterns, being highest in the north (Figure 15). <br />The gradients are strong with concentrations in the north thirty <br />times higher than the Green River and five to ten times higher <br />than the central wetland area. <br /> <br />2,6095 <br /> <br />2.609 <br /> <br />Sodium concentrations, mg/L. Escalante Ranch <br />o <br /> <br />~ = springs <br /> <br />2_6085 <br /> <br />2.608 <br /> <br />~N <br /> <br />167 <br /> <br /> <br />.2.6075 <br /> <br /> <br />320 <br /> <br />I 1.000 feel <br /> <br />200 <br /> <br />ft <br />c: <br />~ 2.607 <br />~ <br /> <br />Terrace <br /> <br />2.6065 <br /> <br />Escarpment <br /> <br />Wetland <br /> <br /> <br />2.606 <br /> <br />1860 <br /> <br />High <br /> <br />2.6055 <br /> <br /> 75,6 <br />60.5 Dike <br />~ Green River t- <br /> . <br />761.5 762.5 763.5 76.,5 <br />761 762 7E3 754 7e~ <br /> (Thcuscntbj <br /> <br />766 767 <br /> <br />2.605 <br /> <br /> <br />2.60.5 <br />760,5 <br /> <br />Figure 15. Sodium Ion Concentrations in the Escalante Wetlands <br />During 1993 (From Cooper And Severn 1994b) <br /> <br />Selenium concentrations followed a similar pattern to both <br />conductivity and sodium concentrations. Very high concentrations <br />of selenium were found in waters of the northern portion of the <br />study site (Figure 16). No detectable concentrations o! selenium <br />were found in the wetland area, but concentrations were-high on <br />the southern end of the site. Selenium most likely is moving in <br /> <br />25 <br />
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