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r � . <br /> r Tahle I-5.5 Hydrologic Soil Groups for Soils in the Everctt Aroa <br /> � � ..� <br /> � Suii Tvce Hvdrolo¢ic Soil Groun <br /> r Alderwood � <br /> I Bellingham C <br /> Cathcart C <br /> � Custer � <br /> Everett '4 <br /> Indianola A <br /> r Kitsap C <br /> � Lynnwood P` <br /> McKenna D <br /> I, Mukilteo D <br /> Norma D <br /> Pastik C <br /> �- Puget � <br /> Puyallup B <br /> rSnohomish � <br /> � Sumus � <br /> Tokul � <br /> [ Winston A <br /> LHydmto�Soil Grou�Classifications <br /> L A. Low runoff potential. Soils having high infiltration rates,even when thoroughly <br /> wetted,and consisting chiefly of deep,well-to-excessively drained sands or <br /> gravels. These soils have a high rate of water transmission. <br /> tB. Moderai„ly low runoff potential. Soils having moderate infiltration r�tes when <br /> thoroughly wctted,and consisting chietiy of moderately fine to moderate{y <br /> 1 coarse textures. These soils have a moderate rate of water uansmission. <br /> � <br /> C. Moderately high runoff potential. Soils havi�g slow infiltration rates when <br /> � thoroughly vvetted,and consisting chiefly of soils with a layer that impedes <br /> downward movement of water or soils with moderately fine to fine textures. <br /> � These soils have a slow rate of water transmission. <br /> D. High runoff potential. Soils having very siow infiltration rates when thoroughly <br /> ` wetted and consisting chiefly ofclay soils with a high swelling porential,soiis <br /> 1 with a permanent high water table, soils with a hnrdpan or clay layer at or near <br /> the surface,and shallow soils over nearly impervious material. These soils <br /> t have a very slow rate of water transmission. <br /> l <br /> � 1-5-32 <br /> r <br />