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i <br /> ITable I-�.� H�•droloeic Soil Groups for Soils in the E�•erett Area <br /> ISoil Tv �droloeic���� <br /> I Aldenvood C <br /> Bellineham C <br /> Cathcart C <br /> ICuster C <br /> � A <br /> Everett <br /> � Indianola A <br /> Kivap C <br /> Lynnwood '� <br /> � McKenna � <br /> Mukilteo D <br /> Nomta D <br /> � Pastik � <br /> Puget C <br /> 1 Puyallup B <br /> Snohomish D <br /> Sumus C <br /> Tokul C � <br /> I Winston A ' <br /> IHvdrolocic Soil Grouo Classifications <br /> � A. Low runoff potential. Soils having high infiltration rates, even when thoroughly <br /> wetted, and consisting chiefly of deep,well-to-excessively drained sand�or <br /> ¢raveis. These soils have a high rate of�vater transmission. <br /> B, Moderately low runoff potential. Soils having moderate infiltration rates when <br /> I thorouehly wetted,and consisting chiefly of moderately fine to moderately <br /> coarse textures. These soils have a moderate rate of water transmission. <br /> I C. Moderately high runoff potential. Soils having slow infiltration rates when <br /> � thoroughly wetted,and consisting chiefy of soils with a layer that impedes <br /> downward movement of water or soils with moderately fine to fine textures. <br /> IThese soils have a slow rate of water transmission. <br /> D. High runoff potential. Soils having very slow infiltration rates wl�en thoroughiy <br /> I wetted and consisting chiefly of clay soils with a high swelling potential,soils <br /> with a pertnanent high water table, soils with a hardpan or clay layer at or near <br /> I the surface,and shallow soils over nearly impervious material. These soils � <br /> have a very slow rate of water transmission. <br /> 1-5-32 <br />