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PUEBLO AREA, COLORADO <br />properties of the soils--Continued <br />i <br /> <br />65 <br />Percentage less than 9 inches <br />paining sieve- <br /> <br />Perme- <br />Available <br />water <br /> <br />Reaction <br /> <br />Salinity <br /> <br />Shrink•ewell potential <br />H dro- <br />lo <br />i <br /> <br />ability <br />capacity g <br />c <br />soil <br />No.4 No. 10 No. 40 No. 200 <br />group <br />(4.7 mm) (2.0 mm) (O.d2 mm) (0.074 mmj <br /> <br /> !n yn hr °7 ~[ nH at is°C <br />80-95 75-90 65-8b 45-65 0.6-2.0 0.05-0.07 6.6-7.8 <2 Low__________________ C <br />50.60 96-45 3010 25-40 0.06-0.2 0.07-0.09 7.4-8.4 <2 Moderate. <br />100. 90-100 65-95 95-75 0.6-2.0 0.16-0.19 6.1-7.4 <2 Low__________________ B <br />100 90-100 75-L00 60-90 0.6-2.0 0.16-0.21 6.6-8.4 <2 Low. <br />x'86-i00 .`,,.76A6 IQ-66 `26-35r 0.6-2.4 :.OAB-0.l$ 7.2-8:0 <2 law------------------ D , <br />100 100 65-85 15-35 > 20 0.07-0.12 6.6-7.3 <2 Low__________________ A <br />100 96-100 65-80 6-20 > 20 0.06-0.10 6.6-7.8 <2 Imw. <br />66-65 46-66 40-50 35-45 0.06-0.2 0.11-0.18 6.6-7.3 <2 High_________________ D <br />100 90-100 60-86 30-45 2.0-6.0 0.11-0.13 6.6-7.3 <2 Low_______________ ___ H <br />100 90-100 65-90 30-50 6.0-20 0.12-0.14 6.6-8.4 <2 Low. <br />100 90-100 60-70 15-30 > 20 0.06-0.11 7.4-8.d <2 Low. <br />100 90-100 50-75 15-30 >20 0.09-0.11 6.6-7.3 <2 Low__________________ B <br />100 90-100 65-90 30-50 6.0-20 0.12-0.14 6.6-8.4 <2 Low. <br />100 90-100 60-70 15-30 20 0.08-0.11 7.4-8.4 <2 Low. <br />80-80 60-75 35-45 20-30 6.0-20 0.07-0.09 6.1-7.3 <2 Low__________________ D <br />60-70 55-66 90-40 25-35 6.0-20 0.07-0.09 6.1-7.3 <2 Low. <br />100 100 90-]00 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 0.19-0.21 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 />I <br />D <br /> <br />95-100 <br />i <br />96-100 <br />90-100 <br />70-95 <br />0 06-0.2 <br />0.19-0.21 <br />6.6-8.4 <br />2 8 <br />High. <br />saturation extract, in millimhos per centimeter at <br />26° C. Salinity affects the suitability of a soil for crops, <br />its stability when used as construction material, and <br />its corrosiveness to metals and concrete. <br />Shrink-swell potential is the relative change in vol- <br />ume 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 high <br />shrink-swell 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 />oups according to their infiltration and transmission <br />rates. The groups are designated A (low runoff poten- <br />tial), B, C, and D (high runoff potential) (11 ). <br />Interpretations for the corrosivity to uncoated steel <br />and concrete are not shown in table 5. Most soils in the <br />survey area have a high corrosivity to uncoated steel <br />pipe and a medium corrosivity to concrete. corrosivity <br />pertains to potential soil-induced chemical action that <br />dissolves or weakens uncoated steel or concrete. Rate <br />of corrosion of uncoated steel is related to such soil <br />properties as drainage, texture, total acidity, and <br />electrical conductivity of the soil material. corrosivity <br />to concrete is influenced mainly by the content of <br />sodium or magnesium sulfate, but also by soil texture <br />and acidity. Installations of uncoated steel that inter- <br />sect soil boundaries or soil horizons are more suscep- <br />tib]e to corrosion than installations made entirely in <br />one kind of soil or in one soil horizon. <br />