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'_' 1 ;1 <br />• <br />lien <br />IIN <br />i <br />to <br />o = .l;- <br />{il° <br />°o° an° cn^ <br />a <br />lal <br />u=1 <br /> <br /> <br />ti li l'. n.ll ti L11~ .1 \.\ 1. 1' 411 ~ '~~1 <br />r,llculatiuns made with logarithmic spiral and circular arc :li failure iurfaccs <br />give very close results. Extensive suuhes by Swedioh engineers of slope lailures <br />in clay during the rely p;ut of this cenuu~y ;Ilse revcllal th:u the lailure <br />surface closely approaches the circular arc. The ^nalysis of slope stability <br />using a circular slip surface was developed by Fclleniw (19}ti) ;uul others <br />and is often referred to :IS the Sredieh cindr nlrrhod. Figurt S.?? shows the <br />displacement of the soil nws's produced by a s'lupe failure. <br />F, <br />II <br />r• <br />(nl <br /> <br />e <br />!. <br />r <br />o dt'. <br />~tl <br />n/' <br />11 <br />, ~ ```` <br />.rl all <br />Fip. hal. Circuhlr-ale ntelhod of olope analysis. <br />an° au° liu- <br />0 <br />,6) <br />Pig. ts.?n. l3a:u ing capacity numhen litr found,l- <br />liom with inclined loads. [After Ateyerho0~(19i3).] <br />1•t.s.'rll' tart t.tuntl at. ru. <br /> <br /> <br /> <br /> -n.rrr = n <br /> ~~ ---u/rr = l <br /> ` <br /> . <br /> <br /> <br /> ~ ~ <br /> <br /> <br /> an° ~~ . <br />~ <br /> , <br /> <br /> <br /> <br /> <br /> au° m = as° <br /> <br />Cirrulur arc merGod. Figurt 8.? I(u) shows a soil mass bounded by the <br />slip surface abet/. Since the circular arc is nn assumed ;lip surface, iti position <br />is not determinate. The arc obcd is therefore an arbitrarily assumed arc. The <br />furcts acting un the soil m;us obcd arc the weight of the soil muss II' and the <br />force on the failure surface. The farce un any element Lc of the slip surface <br />is composed of a normal component dF„ and shear or tangemiul component <br />r/F, parallal to it. At failure, dF, must be equal to the shear strength of the <br />soil as expressed by Eq. (7.?), which in this case can be written as <br />rlF,=cdf+dF„ulna <br />