230
Figure A Values of coefficients B for soil resistance vs. depth (after Reese et al. 1974). A.5 P-Y CURVES FOR WEAK ROCK (REESE 1997) Reese (1997) proposed a p-y criterion for drilled
shafts socketed in weak rock, defined as having an unconfined compressive strength 0.5 MPa β€
quβ€ 5 MPa (5.2 tsf β€
quβ€ 52 tsf). In this criterion, the ultimate resistance of the weak rock is a function of the uniaxial unconfined compressive strength of intact rock,
the drilled shaft diameter, rock quality designation (RQD), and depth.
231
Figure A Basic shape of p-y curve for weak rock (Reese 1997). The shape of the Reese (1997) p-y curve is shown in Figure A. The ultimate reaction,
pu(F/L), of rock was given by for 0 β€ z r
β€ D
ππ
π’π’
= πΌπΌ
ππ
ππ
ππππ
π·π· οΏ½1 + 1.4
ππ
ππ
π·π·οΏ½ Equation A) for z r D
ππ
π’π’
= 5.2πΌπΌ
ππ
ππ
ππππ
π·π· Equation A) where
Οciis the uniaxial unconfined compressive
strength of intact rock Ξ±ris the strength reduction factor, which is used to account for fracturing of rock mass
D is the diameter
of the drilled shaft and zris the depth below rock surface.
Ξ±ris assumed to be 0.33 for RQD = 100 percent and to increase linearly up to 1.0 for RQD = 0. The slope of the initial portion of the p-y curve was given by
πΎπΎ
ππππ
= Equation A) where
Kir= initial tangent to p-y curve
Em= deformation
modulus of rock masses, which could be obtained from a pressuremeter or dilatometer test and
kir= dimensionless constant. The expressions for
kir, derived by correlation
with experimental data, areas follows
ππ
ππππ
= οΏ½100 +
400ππ
ππ
3π·π·
οΏ½ for 0 β€ z r
β€ D Equation A)
ππ
ππππ
= 500 Equation AA complete description of the interim p-y criteria maybe summarized as follows First segment
232
ππ = ππ
ππππ
ππ; ππ β€ Equation A) Second segment:
ππ =
ππ
ππ
ππ οΏ½
ππ
ππ
ππππ
οΏ½
ππ.ππππ
; ππ β₯ ππ
π¨π¨
ππππππ ππ β€ Equation A) Third segment:
ππ = ππ
ππ
; ππ β₯ Equation A) Where
π¦π¦
ππ
= ππ
ππππ
π·π· Equation A)
π¦π¦
π΄π΄
= Equation A) in which,
krmis the strain at 50
percent of the ultimate load, which ranges from 0.0005 to 0.00005.
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