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PERMFILE124206
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PERMFILE124206
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Last modified
8/24/2016 10:21:49 PM
Creation date
11/25/2007 12:23:16 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1982056
IBM Index Class Name
Permit File
Doc Date
12/11/2001
Section_Exhibit Name
Exhibit 04e-2 AVF Evaluation Fish Creek Mine
Media Type
D
Archive
No
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red renectances on the color infrared photography were indications of shallow groundwater <br />• conditions (as opposed to reflectances indicative of vegetation type, topographic position, <br />relation to nearby reservoirs, etc.) In addition, alluvial water levels were evaluated for seasonal <br />variation during [he growing season as well as [he elevation of the capillary fringe in relation [o <br />tl~e terrace surfaces and expected rooting depths for agriculturally useful species of plants (i.e., to <br />allow subirrigation). Soil test pits had been previously described by Walslr (1980) and all <br />pertinent data concerning observations of moisture, soil mottling, rooting depth, and soil textures <br />was reviewed. These data are provided in Appendix Il. All of these data were compared <br />upstream and downstream to determine if patterns were apparent regarding potentially <br />subirrigated areas that would later guide more detailed field studies. <br />based on [he conclusions arrived at from review and evaluation of the previously collected <br />information, test pits were installed on the valley Floor to further verify the presence of <br />srbirrigation of agriculturally useful species (see Map 4). <br />During the test pi[ investigations, records were kept of the presence of vegetative species which <br />are representative of the terrace surface being evaluated. In addition, data were collected with <br />respect [o subsurface observations of soil moisture (including subsequent laboratory analyses), <br />soil mottling, rooting depth of agriculturally useful species, and field soil textures (Appendix I). <br />Whenever possible the test pit elevations were also related to nearby alluvial water table <br />elevations. 1~he following narrative presents the detailed analyses of subirrigation conducted in <br />the drainages of Fish Creek. <br />risk Creek <br />• Tlie limit of the subirrigation investigation in the Fish Creek valley was based on the extent of <br />valley bottom deposits along Fish Creek meeting the geomorphic criteria for an AVF (as <br />described in Section II and delineated on Map 2). With respect to these areas, all available data <br />were reviewed and additional field investigations were undertaken (where needed) in order to <br />delineate areas where subirrigations agricultural activities are occurring. subirrigation <br />investigations were limited to include only the lower Ti, T2, and T} terrace deposits along Fislr <br />Creek (Map I). <br />Evaluation of Infrared Photoeraahy <br />Tlie Fish Creek drainage was initially checked to see where enhanced moisture conditions were <br />suggested for agriculturally useful species on the color infrared photography. The initial review <br />of the photography revealed several areas with red reflectance, with several shades of red. In the <br />field, several areas were verified as having enhanced moisture conditions associated with various <br />types of vegetation. •For example on upper Fish Creek in Section 16, TSN, R86W the moderate <br />red shades along the Fish Creek Ti terrace are primarily associated with the concentrations of <br />shrubs such as shrubby cinquefoil, silver sage, rubber rabbit brush, and willow (see vegetation <br />description for TI terrace, Appendix i, AVF Test Pit Fish-}). In the same vicinity a light red <br />blush was observed on the T2 terrace which includes smooth brome hayfield, while T} terrace <br />landfornis, also in smooth brome, had little if any red tinge on the photos. <br />Downstream, areas of native vegetation indicate varying reflectances based on fence lines, <br />indicating agricultural utilization differences. ignoring the changes in hue caused by the <br />variability in utilization, native vegetation is obviously supplied with additional moisture on the <br />• alluvial fill below three reservoirs in Section 15, TSN, R86W. Moderate shades of red are also <br />noted in an area of native vegetation on the valley bottom below a spring (SEI/4, NEI/4, Section <br />I:environ\tncy\documendExhibTA G 01/16/98 <br />A~pRf'$/'i~ J:J~I 2 8 2CL'D <br />
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