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H,. V'-^r-» color is mediun blue.» soil was formed in ne soil is nearly lei'el ative vegetation'was wet periods of the <br />rface and ponding tnav <br />upper soil horizons <br />s a high potential <br />color is mediun blue, <br />in loam)' colluviun over <br />rainagewnys on foot slopes <br />and hills. The native <br />wed poplar trees. During <br />‘table within 1 foot of <br />lanic matter content in <br />earing values. There is <br />m <br />hat formed in cal- <br />*lls 1 to a feet <br />ire a few stones and <br />mixed hardwoods and <br />ope phase in Hennepin <br />h <br />v--\A V-- -v- :-Ki, <br />. V -vV^ :■' -;■■>:::;■! .-. ./a- <br />l-T .-v.' <br />F!-V * <br />mhm <br />light green. This <br />on low knolls. There <br />ring wet periods of <br />t walls. Since the <br />i?uirri. Soil stren- <br />Pll (volune change) <br />mmmmiM <br />ii»wmUMmA ‘. . V . <br />mm <br />mm:mk <br />s*^rOTKNTIAL or SOILS TOR OX-SITr KASTF: TRF.ATMF.XT <br />•iccording to the recommended <br />4*fcet below the bottom of the drain field trench . <br />This line of thinking has <^^*"**^ conducted^in^various areas <br />;;jrr“js: t.u <br />requirement <br />A. example of the innovative ’" <br />the mound system the seepage bed or seoaratlon dis- <br />the use of >0"? f“? '» ""('{S' 5Sp«{ ?{eSSS"Sd . bSJrlertance between the bottom or me scyHa^v <br />layer such as the watertable or bedrock. <br />:snr!S;\o,properi/t:.o ;.t!;..;opt^;d;;i,;r{;:;{;engi <br />Sri'S'A-itrtLSrf iiThS {SrSSSnS s^ris^sSir <br />populated. <br />?rr5ist^ss;!i:e^%irrafisrsr,?.vsui: p5 <br />i;Hcb-it'!:?crrr%'ma?LJJ%r;sjuJ ?aik%f?fSeSt':iu's.- <br />discussed. <br />-r> <br />'"A <br />' •■■■■■;.•.• y\;j <br />■ -:AM <br />mmmA- <br />ic-:kiV=' • • ' ■ .; V.^