Laserfiche WebLink
The SAR value from the Pyeatt wells has generally been • <br />between 1 and 3. 'Che SAR values from alluvial wells J1 and COY <br />have been approximately 1 and 2, respectively. <br />Values between'13 and 15 were measured for the SAR from well <br />GLUX-1 water in 199,x. Water from wells 81-4~3a and GMP-1 had SAR <br />values of 66 and 16.1, respectively, for 199?. <br />A SAR of greater than <br />most soils and. therefore <br />source. Some ground avatar <br />systems at Trapper mine <br />irrigation and, therefore. <br />a potential sourr_e. <br />15 will result in ar. alkali build-up on <br />will not be an acceptable irrigation <br />naturall,v has a high SAR. Ground water <br />do not yield an arieauate rate £or <br />are not very lively to be considered as <br />• <br />3.5 OTHER CONSTITUENTS <br />The ma,ior constituents other than the carbonates are presented <br />on pages B-77 throu~;Yi B-95. The heavy metals with a "t" subscript <br />by their symbol represent total measurements, while the others are <br />dissolved concentrations. Dissolved and total concentrations are <br />similar for most of the heavy metals, except for iron <br />concentrations in some wells cahere the total values are <br />significantly greater in some wells. <br />• <br />3-1~ <br />