_ __.�_.._..�_...__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 />
|