My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
7610
CWCB
>
UCREFRP
>
Public
>
7610
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/11/2009 11:32:56 AM
Creation date
8/10/2009 3:42:40 PM
Metadata
Fields
Template:
UCREFRP
UCREFRP Catalog Number
7610
Author
Wick, E. J. and J. A. Hawkins.
Title
Colorado Squawfish Winter Habitat Study, Yampa River, Colorado, 1986-1987
USFW Year
1987.
USFW - Doc Type
Final Report Year 1.
Copyright Material
NO
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
77
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
Show annotations
View images
View plain text
0 <br />6 <br />"active" if its location changed within e 5 meter diameter circle over its <br />original location, as long as the specific habitat used remained the same. <br />"Local" movement was designated if a fish moved to new location outside the <br />original 5 meter diameter circle about its original location but within the <br />same specific habitat. The "moving" designation was used if a fish was <br />observed in the process of moving to a new location or had moved to a <br />different specific habitat type regardless of distance (ie: fish moved from <br />eddy to run or from one eddy to another eddy). <br />Habitat measurements <br />At the conclusion of a monitoring period habitat.measurments were taken at all <br />site locations at which fish spent 30 or more minutes. Site locations were 49 <br />determined by triangulation from 2 to 5 transects which were previously marked <br />by survey flags placed along the bank during monitoring. Measurements taken <br />were water depth, velocity, substrate, cover, and water temperature. When fish <br />habitat was free of ice, measurements were taken from a boat or by wading. <br />When ice formed over the site location and was considered unsafe to walk upon, <br />access to the fish location was achieved by sitting in a small inflatable raft <br />at waters edge and pushing it over the surface of the ice using a wading rod. <br />Throughout most of the winter the ice was thick enough to walk upon safely. <br />However, as an added safety precaution a small inflatable raft was often taken <br />out on the ice and used to carry measurement equipment. Depth was measured <br />using a 10 foot wading rod (1\2 inch electrical conduit marked in 0.1 foot <br /> <br />increments). Velocity was measured using a Marsh- McBirney Model 201 current • <br />meter. Negative velocity was recorded if direction of current flow deviated <br />more than 90 degrees from that of the main channel current. Substrate was <br />categorized as a combination of primary and secondary components of clay, <br />silt, sand, gravel, coble or boulder by probing with a wading rod. Cover <br />designations included vegetation, brush, and boulder. <br /> <br />Three sets of measurements were taken at each site, one set was at the • <br />triangulated fish location (main site) with additional sets taken 1-2 meters <br />"in" toward shore and "out" away from shore. Velocity measurements at the main <br />site were taken at 0.2, 0.6, and 0.8 depth from the water surface when ice <br />free or from the bottom of the ice during ice cover. At the "in" and "out" <br />measurement sites velocity was measured at 0.6 depth. During ice cover, <br /> <br />habitat measurements were taken through holes drilled in the ice. Holes were • <br />drilled using either an 8 inch Strikemaster hand auger or 7 inch Strikemaster <br />gasoline power auger. Additional measurements were then taken to determine <br />ice-free water depth. These included solid ice thickness (ice below the water <br />surface in the hole), frazil ice thickness, and total depth (water depth in <br />the hole). Water depth below the surface of the ice was then calculated by <br /> <br />subtracting ice thickness from total water depth (Figure 2a). When frazil ice • <br />was present under the hard ice cover its thickness was determined by lowering <br />the velocity probe to the bottom, getting a positive velocity reading, and <br />then slowly raising the probe until the frazil could be felt touching the <br />probe and velocity decreased to 0.0 feet per second. The compact, non-moving, <br />frazil ice deposits were treated as solid ice in making water depth and <br /> <br />velocity measurements (Figure 2b). • <br />40
The URL can be used to link to this page
Your browser does not support the video tag.