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PERMFILE125186
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PERMFILE125186
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Entry Properties
Last modified
8/24/2016 10:22:38 PM
Creation date
11/25/2007 1:33:48 PM
Metadata
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Template:
DRMS Permit Index
Permit No
C1980007
IBM Index Class Name
Permit File
Doc Date
12/11/2001
Doc Name
Sylvester Gulch Facilities Area
Section_Exhibit Name
Exhibit 27A Baseline Soil Study (1996)
Media Type
D
Archive
No
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<br />Elemental <br />Plant <br />Macronutrient Within Plant <br />Concentration <br />(ppm) Culture Solution <br />Concentration <br />( m) SGFA Range <br />Concentration <br />(ppm) <br />Nitrogen (N) 12,000 2l0 2-171 <br />Phos horns (P) 2,500 30 1.2-23.7 <br />Potassium (K) 10,000 195 28-455 <br />With one notable exception, SGFA soils aze very low in the concentration of nitrogen <br />when compared to the satisfactory concentrations required for a plant growth solution <br />in the laboratory. In all but one sample, nitrate nitrogen concentrations were below 17 <br />ppm. The notable exception was the Beenom-Absazokee(1) A horizon. Noted prior, <br />this horizon also contained the highest concentration of organic matter (conifer <br />needles). Since nitrogen concentrations are correlated with plant growth activity and <br />decay, this is a logical correlation. <br />Phosphorus concentrations are more widely distributed than nitrogen concentrations. <br />The same horizon (Beenom-Absazokee(1) A) contains the highest concentration of <br />phosphorus. The lowest concentration is found within the Torriorthent(3) B/C horizon <br />found in the sedge meadow inclusion. Phosphorus concentrations are slightly to <br />moderately lower than the laboratory optimal requirements. <br />S Potassium concentrations in the SGFA soils were above the laboratory culture <br />concentration in 16 of the 23 samples. A significant trend of decreasing potassium <br />concentration with depth was observed in all of the soil types. <br />SODIUM ADSORPTION RATIO (SAR) <br />The Sodium Adsorption Ratio (SAR), with texture, clay mineralogy, soluble salt <br />concentration in rainwater, and other factors impacts the infiltration rate and hydraulic <br />conductivity of soils. With high SAR values, the structure of a soil may be <br />compromised, with accompanying decreases in hydraulic conductivity; leaving plants <br />unable to procure necessary nutrients from the soil, unable to penetrate cemented soils <br />with roots, or exposed to toxic concentrations of sodium. Soils within the SGFA <br />exhibit low SAR values, ranging from 0.3 to 6.3. The highest SAR value came from <br />the Tomorthent(3) sedge meadow inclusion, and the lowest value was found in the <br />Work loam A horizon and the Beenom-Absazokee(1) A horizon. <br />CATIONS (Ca, Ivig, Na, K, Zn, Fe, Mn, Cu, Se, Mo, B) <br />The majority of cations provide essential micronutrients to plants during their growth <br />and reproduction cycle. In general the concentrations of these cations required for <br />plant nutrition is very small, and they are not generally limiting. In the western United <br />• States, selenium, molybdenum, and boron may be found in concentrations, which <br />though not generally detrimental to plant growth, may affect livestock or other grazers <br />-11- <br />
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