Geotechnical Engineering Circular No. 9 Design, Analysis, and Testing of Laterally Loaded Deep Foundations that Support Transportation Facilities



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hif18031
Soldier Rev B
Condition
Relative Density
Loose
k (pci)
Relative Density
Medium
k (pci)
Relative Density
Dense
k (pci)
Submerged
20 60 125 Above Water
25 90 225 9. Establish the parabolic section of the p-y curve as follows
𝑝𝑝 = 𝐢𝐢𝑦𝑦
1 Equation A-28)
Μ…
Where:
𝐢𝐢 =
𝑝𝑝
π‘šπ‘š
𝑦𝑦
π‘šπ‘š
1 Equation A)
Μ…
π‘šπ‘š Equation A)
π‘šπ‘š =
𝑝𝑝
𝑒𝑒
βˆ’ 𝑝𝑝
π‘šπ‘š
𝑦𝑦
𝑒𝑒
βˆ’ Equation A-31)
Point β€œk” in Figure A signals the end of the linear segment of the p-y curve. Its y-coordinate is determined as follows
𝑦𝑦
π‘˜π‘˜
= Equation A)
Μ…
10. For y>= D, pis equal to the ultimate resistance per unit length of pile/shaft calculated in Step 3. If Equations A and A have no intersection, Equation A defines the p-y curve until there is an intersection with the p-y curve branch defined in Step 10.


229
Figure A Values of coefficients
and
(after Reese et alb


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 ≀ q
u
≀ 5 MPa (5.2 tsf ≀ q
u
≀ 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, p
u
(F/L), of rock was given by for 0 ≀ z r
≀ D
𝑝𝑝
𝑒𝑒
= 𝛼𝛼
𝑐𝑐
𝜎𝜎
𝑐𝑐𝑖𝑖
𝐷𝐷 �1 + 1.4
π‘˜π‘˜
𝑐𝑐
𝐷𝐷� Equation A) for z r D
𝑝𝑝
𝑒𝑒
= 5.2𝛼𝛼
𝑐𝑐
𝜎𝜎
𝑐𝑐𝑖𝑖
𝐷𝐷 Equation A) where Οƒ
ci
is the uniaxial unconfined compressive strength of intact rock Ξ±
r
is the strength reduction factor, which is used to account for fracturing of rock mass D is the diameter of the drilled shaft and z
r
is the depth below rock surface. Ξ±
r
is 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
𝐾𝐾
𝑖𝑖𝑐𝑐
= Equation A) where K
ir
= initial tangent to p-y curve E
m
= deformation modulus of rock masses, which could be obtained from a pressuremeter or dilatometer test and k
ir
= dimensionless constant. The expressions for k
ir
, derived by correlation with experimental data, areas follows
π‘˜π‘˜
𝑖𝑖𝑐𝑐
= οΏ½100 +
400π‘˜π‘˜
𝑐𝑐
3𝐷𝐷
οΏ½ for 0 ≀ z r
≀ D Equation A)
π‘˜π‘˜
𝑖𝑖𝑐𝑐
= 500 Equation AA complete description of the interim p-y criteria maybe summarized as follows First segment


232
𝒑𝒑 = π’Œπ’Œ
π’Šπ’Šπ’Šπ’Š
π’šπ’š; π’šπ’š ≀ Equation A) Second segment:
𝒑𝒑 =
𝒑𝒑
𝒖𝒖
𝟐𝟐 �
π’šπ’š
π’šπ’š
π’Šπ’Šπ’“π’“
οΏ½
𝟎𝟎.𝟐𝟐𝟐𝟐
; π’šπ’š β‰₯ π’šπ’š
𝑨𝑨
𝒂𝒂𝒂𝒂𝒔𝒔 𝒑𝒑 ≀ Equation A) Third segment:
𝒑𝒑 = 𝒑𝒑
𝒖𝒖
; 𝒑𝒑 β‰₯ Equation A) Where
𝑦𝑦
π‘šπ‘š
= π‘˜π‘˜
π‘π‘π‘šπ‘š
𝐷𝐷 Equation A)
𝑦𝑦
𝐴𝐴
= Equation A) in which, k
rm
is the strain at 50 percent of the ultimate load, which ranges from 0.0005 to 0.00005.

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