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PUEBLO AREA, COLORADO <br />properties of the soils-Continued <br />65 <br /> Percentage less than 3 inches <br /> passing sieve- Available Hydro- <br /> Perms- water Reaction Salinity Shrink-s ell potential logic <br /> __ ahility capacity soil <br /> No. 4 No. ]0 No. 40 No. 200 <br />group <br /> (4.7 mm) (2.0 mm) (0.42 mm) (0.074 mm! <br /> !n yn in dfmhayrnn <br /> In pn hr o/roil yN of 95°C <br /> RO-95 75-90 6.5-85 45-f,5 0.6-"_.U 0 OS 0 07 6 6-7.R <? Low.. .._.. -. <br />~ - C <br /> 50-GO 35 45 3U-40 '_5 40 0 0G 0 -^ 0 (17 0.09 7A S.4 C >'ludcrnte. <br /> 100 :r0 100 O.i -7.i <br />I a..-;:, U 0 ~ 0 U.16 U J9 G. 1.7.4 G7 Low -.-- .-- ----- B <br /> 100 90 100 .5-100 6U :III (1 (i ': 0 0 1G-0 "1 6 6 S 4 C: Ln u', <br /> RS-l0U 75-90 40-65 25-35 <br />----- 0.6 ?.0 <br />- 0.03-0.13 7.3-8.0 <" Low_____ ____________ D <br /> <br />100 <br />100 <br />65-85 <br />15-35 - <br />>20 <br />0.07-0.12 <br />6 6-7.3 <br /><2 <br />Low_ _ ___ <br />____________ <br />A <br /> 100 95-100 65-80 5-'LO > 20 0.05-0.10 6.6-7.8 G2 Low. <br /> 55-65 45-55 40-50 3515 0.06-0.2 0.11-0.18 6.6-7.3 <2 High_____ ____________ D <br /> 100 90-]00 60-85 30-45 2 0-6.0 0 I1-0.13 6.6-7.3 <2 Low______ ___________ B <br /> 100 90-100 65-90 30-50 6.0 °0 0.12-0,14 6.6-8.4 <'L Low. <br /> 100 90-100 50-70 15-30 > 20 0.06-0.11 7 4-8.4 <2 Low. <br /> 100 90-100 50-75 15-30 >''?0 U.09-0.11 6.6-7.3 <2 Low______ ___________ B <br /> 100 90-100 65-90 30-50 6.0-''?0 0.12-0,14 6.6-R 4 <2 Low. <br /> ]00 90-100 50-10 15-30 ''?0 0 OS-0.11 7.4-8.4 <2 Low. <br /> 60-80 60-75 355 20-30 6.0 ~0 0.07-0.09 6.1-7.3 <2 Low______ ___________ D <br /> 60-70 55-65 30-40 25-35 6 D-20 0.07-0.09 6 1-7.3 <2 Low. <br /> 100 100 90-100 70-90 0.6-2.0 0.19-0.21 7.4-7.8 <2 Low ______ ___________ B <br /> 100 100 90-100 70-95 0.2-0.6 0.19-0.2] 7.9-8 4 <2 Low. <br /> 100 100 90-100 70-90 0.2-0.6 0.16-0.21 7.9-8.4 <2 Low. <br /> 95-]00 95-100 90-100 70-90 0.2-0.6 O.19-0.21 6.6-7.3 2-8 Low_______ ___________ D <br /> 95-100 95-100 90-100 70-95 0,06-0.2 0 19-0.21 6.6-8.4 2-8 High. <br />saturation extract, in millimhos per centimeter at <br />25° C. Salinity affects the suitability of a soil for crops, <br />its stability when used as construction material, and <br />corrosiveness to metals and concrete. <br />Shrink-swell potential is the relative change in vol- <br />me of soil material to be expected with changes in <br />moisture content, that is, the extent to which the soil <br />shrinks as it dries out or swells when it gets wet. Ex- <br />tent of shrinking and swelling is influenced by the <br />amount and kind of clay in the soil. Shrinking and <br />swelling of soils cause much damage to building <br />foundations, roads, and other structures. A higla <br />shl•ink-smell potential indicates a hazard to the mainte- <br />nance of structures built in, on, or with material that <br />has this rating. <br />Hydrologic soil group classifies the soils into four <br />groups according to their infiltration and transmission <br />1•ates. The groups are designated (low 1•unoff poten- <br />tial), B, C, and D (high runoff po ential) (11 ). <br />Interpretations for the corrosivi y to uncoated steel <br />and concrete are not shown in table 5. Most soils in the <br />survey area have a high corrosivi to uncoated steel <br />pipe and a medium Corrosivity to c ncrete. Corrosivity <br />pertains to potential soil-induced c emical action that <br />dissolves or weakens uncoated ste or concrete. Rate <br />of corrosion of uncoated steel is ]ated to such soil <br />properties as drainage, texture, ota] acidity, and <br />electrical conductivity of the soil m terial. Corrosivity <br />to concrete is influenced mainly y the content of <br />sodium or magnesium sulfate, but Iso by sail texture <br />and acidity. Installations of uncoat d steel that inter- <br />sect soil boundaries or soil horizon are more suscep- <br />tible to corrosion than installation made entirely in <br />one kind of soil or in one soil horizo . <br />