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<br />. <br /> <br />~ <br /> <br />I <br />I <br />; I ' <br />I <br />f <br />I <br />. <br />i <br />! <br />f <br />. <br />~ <br />t <br />i <br />~ <br />r <br />r <br />, <br />i <br />t <br />i <br />e <br />I <br />I <br />f <br />i <br />r <br />~ <br />I <br />f <br />, <br /> <br />Fish with transmitters were found in water as deep as 15 m while <br />those without transmitters were found in a maximum depth of 12.5 m <br />(Figure 3). Data from fish without transmitters indicates a selection <br />for water less than 5 m deep. Data from the radio-tagged fish shows the <br />same general pattern, but indicates a greater use of water deeper than <br />about 7 m. This phenomenon is probably an artifact of sampling; electro- <br />fishing is most effective in shallow water or with fish close to the <br />surface in deep water. Radiotelemetry was most effective in water less <br />than 6 m, but enabled monitoring of those fish that positioned themselves <br />in midwater of a deep area. At no time in this investigation, except <br />with fish caught in entanglement nets, could the position of a fish in <br />the water column be determined. Thus, all measurements were taken of <br />total water depth at the capture or monitor site. <br /> <br />The velocity occupied by fish without modules was 0-3.8 fps and that <br />by radio-tagged fish was 0.2-1. 3 fps. The distribution of these two data <br />sets is similar with apparent selection by the species for less than 1 <br />fps velocity (Figure 3). Water velocity measured in a deep area like <br />Black Rocks can be tenuous. There appears to be much tl sheet ing" and <br />"1ayering"of velocities when measured in vertical profile, especially <br />during runoff. A fish may thus be situated in a layered region of quiet <br />. .water but velocity recorded at six-tenths of the water depth may indicatj! <br />a moderate to strong velocity. High turbidity precludes accurate <br />measurement of these microhabitats. <br /> <br />Swimming performance tests in the laboratory (Bulkley et ale 1981) <br />showed that humpback chub were capable of sustained swimming speeds of <br />2.2 ft/sec for a matter of minutes at 20oC, compared to speeds of 1.6 <br />ft/sec for Colorado squawfish, 1.47 ft/sec for razorback sucker, and 1.9 <br />ft/sec for bony tail chub.. These results and the field observation of <br />this study indicate that humpback chub are capable swimmers in swift <br />water but prefer to spend most of their time in the. quiet areas. <br /> <br />The same four substrates were used by radio-tagged fish as by non- <br />tagged fish (Figure 3). Sand and bedrock were most often used by the <br />former and sand and boulder were most often associated with the latter. <br />These substrates appear to reflect those available in the study area, <br />Black Rocks. <br /> <br />Spawning <br /> <br />Radiotelemetry with humpback chub was initiated primarily to aid in <br />locating spawning sites and assessing spawning conditions for the <br />species. Water temperatures and flows in 1981 were affected by below- <br />normal snow fall, and the chubs spawned earlier than expected. <br /> <br />The spawning period in 1981 was 15-27 May at water temperatures of <br />l6.0-16.50C and flow of 3000-5000 cfs. Spawning in 1980 occurred 2 weeks <br />later, about 2-15 June, at water temperatures of 11.5-16.0.C and flows of <br />21,500-26,000 cfs. <br /> <br />36 <br />