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I <br /> W-4940-01 <br /> Aun: Mr.Tony Vivolo, P.G. <br /> � Junc 1G, 198R <br /> c�a "0 Page 4 <br /> � �a <br /> c r. i <br /> y � N <br /> H <br /> .t r� f1 <br /> O C� O <br /> � N H <br /> o r�. � At-re�t oanh pressures due to the soil c-� both side: of the ringw all are shown on Figure 10. If I <br /> the soil along the outside of the wall uill not be remova�during the life of the swcturc, such <br /> � � ns for maintenan�e o(pipes,the ai mst pressure along the c,utsidc of the wall can be used to � <br /> M , teduce the pressures un the inside of tne wall. <br /> � H � Two values for:.he at-rest earth pressure ccefficient,Ko,are given on Figure 10. I(the <br /> y � rin�+�all is conswcted such tnat its faas are poured against a very dense venical, undisturtxd, <br /> � o y glacial ull surface, a Ko value of Q4 can be used to calculate the lateral pressures on the wall. <br /> � � � If the ringwall is forraed on both sides and then bacldilled with compacted smicmral fill, a Ko <br /> � value of 0.5 shnald Ix uscd. <br /> N <br /> The passive nressure illustrated along the outside of the u all on Figure 10 is not to be used in <br /> thc hoop tension design of the µa1L The passive pressure shown should be used to resist <br /> horizonwl forces during seismic or wind loading. <br /> The passive tanh pressure ccxificient, Kp= 3.6, gi�'en o�i Figure ]0, is based on the <br /> assumption that the outside of the wall µ�ill be bacY.t-illed w�th swctural fill or drainage materia] <br /> (see folloµ�ing secrion). ' <br /> I�in�nr an�1 f3ackfill� .e I <br /> Ground wster seepage was observecl in the test pit explorarions m�de at the sitt on April I 1, <br /> 198R. This watcr appeared to by perched aior the very dense glacial till. We recommend that a <br /> � �� a dt emoveathis u ier.�aTha groundhaz u d the re�ervoir sholuld tx:sloped�go promotelsurface� <br /> � „ <br /> drainage away (rom ihe tank. <br /> � ��� Backfill on both sides of ihe ringwall, including the drainage sand and gravel,should bc <br /> a�� Strucwr:� Fill,compacted to at least 95 perceN of its 1�1odified Procror maximum dry densit�•. <br /> Native soil th�t is essentially free of roots and organic material could be used as Svuctural Fill <br /> provided that its moisture content at the time of compactian is ncar the optimum. Soil generally� <br /> '� encountered below a depth of about 2 feet in the iest pits could be used as Swctural Fill; <br /> ��I hoµ�e��cr,dn�ing woul� oe necessary to :ower i�s moisrore content(appmximately 12 to 29 <br /> percent in TP-1 through lP•a)to nearer optimum for compacuon. H'e estimate the optimum <br /> moismre conient of these native soils�o be between R and 12 percent. Grain size distribuuon� � <br /> and compaction tat results for the native soils cncoumere�f in the test pits below a depth of= <br /> �,� feet are shoµn in Figures 7, 8 and 9. <br /> lf sufficient native matenal is not a��ailable for use as Stn:cwral Pill, u'ell-graded sand and <br /> , � gravel should be imponed. The imported sand and gra��el should ha��e a maximum paniclr size <br /> ��� of 3 inchea, should be free of orFanics, and its moisture content should not be above the <br /> optimurn for compaction. <br /> Fer fill placed in non-structural areas, such as for landscaping, the compacuon requiremen[ <br /> iI���) may be re�±uced to 42 percent. <br /> � ]f backfilling is auempted during wet, rainy weaihcr,the native soil w�ll not be usable as <br /> Strucr�ral Fill, and die fines contem (percentage of minus 3/4-inch material passing the No. <br /> SHANNUN 6 V`'ILSON INC <br />