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_ __.�_.._..�_...__y...Y. .._.�ti <br /> � � .. . <br /> ' sok exw.or�bon <br /> � ��w <br /> , ; . <br /> � <br /> ? � 662 CROMWELL AVENUc <br /> a ST. PAUL, MN 551�a <br /> S PHONE 6121E45�64ac, <br /> � May 18, 1983 <br /> . , <br /> + ,�',�vi �uipcir,��,on to TWIN CITY TESTING AND ENGINEERING LABORAT(�RY INC <br /> � <br /> � � ; <br /> Jann & Renee Olsten <br /> � 233 Glenmoor Lane ' ; <br /> I Long Lake, MN 55356 ; <br /> i , <br /> � Subject: Proposed Sewage Treatment System °�4-� <br /> Lot 1, Block 2 ; � � <br /> Farvi ew.Addi tion OFFICERS: <br /> Orono, Minnesota CHARLES W.BRITZIUS � � <br /> �1120-9990 chauman of the board I ; ' <br /> NORMAN E. HENfviNG ' <br /> �rbsident � +. <br /> Oear Ms Jann & Renee O1 sten ROBERT F.WITTMAN � <br /> exeCutivo vice Flosident <br /> CLINTON F. EUE <br /> On May 11 and 13, 1983� we put down three hand auger borings aecretary/treasurer <br /> and ran six percolation tests for a propused sewage treatment MOMEOFFICE: <br /> system. Two borings and four tests were made in the primary ST. PAUL, MN - <br /> treatment area, and one boring and two percolation tests - <br /> were made in the alternate (future) location. All the boring OFFICESIN: <br /> and test locations are shown on the attached sketch. MANKATO, nnn; <br /> FiOCHESTER, MN <br /> SOIL CONDITIONS <br /> �� The attached copies of the field boring logs show th: t the <br /> � soil profile is fairly similar throughout. About '-;' of dark <br /> � brown topsoil overlies sandy clay (CL), which classifies as <br /> � a clay loam according to the USDA Soil Textural Classification <br /> �t. System. The clayey soil changes in color from a fairly uni`orm <br /> �,� brown to a brown mottled as depth increases. The mottled brown <br /> �,� is not the typical multi-colored, mottled soil , which indicates <br /> ,� a fluct�ating ground water table, <br /> �� GROUND WATER <br /> �1 <br /> , � No wnter was noted in the borings at completian, although the <br /> soil was nearly saturated, which is typical of late sprinq <br /> cond:tions. Later, water was noted at depths of about 5' in borings <br /> 1 and 2. This may have been due to the heavy rains the pre- <br /> vious day and eveniny; or, it rnay be due to the temporary <br /> spring conditions. <br /> „ ��,�, �, ,�, ,� , ,�,; <br /> ,� .� . • , . , ' • . . � , .. �.. � .i .. ,, I•i I�,,r�l�,M,1 _,uHM��II l�i.l,1��1.l.Uhf iDl IvliAl V'NpVLHf r OF 1ME Clit NT <br /> ��^° ..��';�k'� ;g� 4 - ���"'�+',,��,��'.: <br /> J A6� t M1x4 .++� re r a 4Nzl�' 1 � �'�ipi4 a� � � ,7 S',� i i . <br /> .� . y r . i N . . , , ; . <br /> � <br /> w�4 _ � i� �' S q Z . . ' �i. <br /> �p , d }. <br /> I � <br /> �Q ,�, _ pb rt.t rE�.�,,.�"i�� .t '.�}� �,� . �d� � �N ��'�� �1y?�t,',. <br /> ,�` �y � x i � 6 � �,�,��;f �� �� �. <br /> ��i}-"`'��,�T"�� �'S��� �: e i i er�'*"r�"�`TA,���. . � <br /> a� y�� pt`�Tl a��a� Y � � �`�� ; ��` '�y {�� <br /> � ,k �1 �. <br /> �� <br /> �,�1,�Y���a#�: .�b ry.s�� #�:°���.,�},�... '�rh.� -4'Y <br /> ���,A��W��tfvw� L��:���FSai����aifd7� . . . _._.e�"�' <br />