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Analysis of vertical vibration of earth dam in triangular canyons* X. Zhiying Department of Irrigation and Drainage Engineeering, Hohai University, Nanjing, China ABSTRACT In this paper, firstly, a partial differential equation of vertical motion for an earth dam with symmetrical cross-section in a triangular canyon is presented. Then by using the method of separation of variables and Bubnov-Galerkin ap- proach, an approximate eigenvalue solution for the fundamental natural fre- quency of vertical vibration of the dam isobtained. An approximate calculation formulas for vertical earthquake response of dam are given. These formulas are very simple and dynamic analysis may readily be made by hand calculation. At the end, a sample calculation has been presented. Some interesting and reason- abe results have been obtained. INTRODUCTION Designing an earth and rockfill dam to resist earthquake damage is probably one of the most difficult tasks to be faced by the geotechni- cal and earthquake engineer. Current methods for determining the seismic stability of an earth and rockfill dam usually involve a dy- namic response analysis of the dam for the maximum earthquake mo- tions to affect the structure. Generally, the assumption of plane strain condition for analyzing the dynamic response of dam is adopt- (D This research was supported by a grant from Science Foundation of State Education Commission, P. R. China. Transactions on the Built Environment vol 3, © 1993 WIT Press, www.witpress.com, ISSN 1743-3509
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Page 1: ABSTRACT -   · PDF fileEngineeering, Hohai University, Nanjing, China ABSTRACT ... formulas for vertical earthquake response of dam are given. These formulas are

Analysis of vertical vibration of

earth dam in triangular canyons*

X. Zhiying

Department of Irrigation and Drainage

Engineeering, Hohai University, Nanjing, China

ABSTRACT

In this paper, firstly, a partial differential equation of vertical motion for anearth dam with symmetrical cross-section in a triangular canyon is presented.Then by using the method of separation of variables and Bubnov-Galerkin ap-proach, an approximate eigenvalue solution for the fundamental natural fre-quency of vertical vibration of the dam is obtained. An approximate calculationformulas for vertical earthquake response of dam are given. These formulas arevery simple and dynamic analysis may readily be made by hand calculation. Atthe end, a sample calculation has been presented. Some interesting and reason-abe results have been obtained.

INTRODUCTION

Designing an earth and rockfill dam to resist earthquake damage is

probably one of the most difficult tasks to be faced by the geotechni-

cal and earthquake engineer. Current methods for determining the

seismic stability of an earth and rockfill dam usually involve a dy-

namic response analysis of the dam for the maximum earthquake mo-

tions to affect the structure. Generally, the assumption of plane

strain condition for analyzing the dynamic response of dam is adopt-

(D This research was supported by a grant from Science Foundation of State EducationCommission, P. R. China.

Transactions on the Built Environment vol 3, © 1993 WIT Press, www.witpress.com, ISSN 1743-3509

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516 Soil Dynamics and Earthquake Engineering

ed. If earth and rockf ill dam is built in a rectangular canyon where the

width of the canyon is large with respect to the height of dam, this as-

sumption is considered an adequate representation. However, for cas-

es of narrow rectangular canyons or triangular canyons, the response

of a dam is greatly affected by the proximity of the rigid boundaries,

and the validity of plane strain assumption becomes questionable. In

such cases, a three-dimensional solution is desirable to predict accu-

rately the dynamic response of an embankment. Probably the most

versatile tool currently available to perform such analyses is the 3-D

FEM [1-3], but it would be very costly.

Existing analytical techniques for earth and rockfill dam essen-

tially assume the response analysis restricted to horizontal shear defor-

mation in the upstream-downstream direction. Due to these restrictive

assumptions, the dynamic response analysis cannot be used to exam-

ine the nature of stress distribution within an earth dam due to verti-

cal ground motion. However, the strong ground motion in the verti-

cal direction is often observed at epicentral areas and their vicinites.

The maximum accelerations of these motions frequently reach the lev-

els of maximum accelerations in the horizontal direction. Thus the

strong ground motion in the vertical direction will play an important

role in the stability of earth dams, and the problem of earthquake-in-

duced vertical vibration of earth dams is significant for the dam' s

safety but has received comparatively little attention. This paper de-

velops an approximate analytical method for evaluating the dynamic

responses of earth dams in the vertical direction.

EQUATION OF VERTICAL VIBRATION OF EARTH DAM

Fig. 1 shows a longitudinal section, a transversal section and a

transversal slice of dam, on which vertical forces are acting under

vertical motion. Assume longitudinal section and transversal section

are symmetrical triangle. The assumptions inherent to a shear wedge

analysis of a symmetrical earth dam are as follows; (1) The canyon

wall is perfectly rigid; (2) The direction of ground motion is verti-

cal and there is no displacement in other directions; (3) The dam is

homogeneous and the dam materials are linearly elastic; (4) Interac-

tion between water in the reservoir and the dam is negligible.

Transactions on the Built Environment vol 3, © 1993 WIT Press, www.witpress.com, ISSN 1743-3509

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Soil Dynamics and Earthquake Engineering 517

Forces acting on an element in the vertical direction as shown in

Fig. 1 (c) are.

1. Inertial force

2. Shear force on front

3. Shear force on back face

4. Normal force on bottom

f, =

5. Normal force on top

Where v is displacemennt in y direction, p density of material, / the widthof element in x direction, cr, normal stress in y direction, G shear modulus of thematerial, E the elastic modulus of the material and t time. #=2(l+/z)C=(0,in which |i is the Poisson's ratio of material and £=2 (l+/x).

As shown in Fig. 1 (c), under undamped condition, two shear forces, twonormal forces and one inertia force act on each element. Dynamic equilibrium of

element requires that.

Transactions on the Built Environment vol 3, © 1993 WIT Press, www.witpress.com, ISSN 1743-3509

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518 Soil Dynamics and Earthquake Engineering

:=l ^ X ,U

(c)

Figure 1: Analytical model of dam in triangular canyon for analysis.

From geometrical consideration it follows that;

/ dy y — H(2)

Substituting equation (2) into equation (1), the equation of motion gov-erning free vertical vibration of dam is obtained %

(3)

The following boundary conditions are applicable to the case of symmetrical dam

in a triangular canyon;

= 0dy

v = 0

|=0

a,

at y

at ,

= z = Kz (4)

Transactions on the Built Environment vol 3, © 1993 WIT Press, www.witpress.com, ISSN 1743-3509

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Soil Dynamics and Earthquake Engineering 519

where L is length of dam crest.

SOLUTION FOR FIRST NATURAL FREQUENCY

By the method of separation of variable [_v (y, ~, 0=#> (y, -) T (0],the following equations are obtained %

+ ofT = 0 (5)at

^ ^ _^_^ ^ (g)$ dy*^ M^ y- H 3y^ v*J

where CD is the natural frequency , Therefore j

T = dcosod + Ctsinot (7)

where C\ and Cg are arbitrary constants.Since the boundary conditions given by equation (4) have to be satisfied at

all times, the following boundary condition can be imposed on the function y%

= 0 at y = *

o rr= 0 at y = -z = K=

-O a, ,_.

(8)

Solution in closed form of equation (6) is difficult to obtain. However , anapproximate eigenvalue solution of equation (6) can easily be used to obtain arather accurate value for the first natural frequency of vibration of the system.

According to the Bubnov- Galerkin method, if a function y> which satisfiesthe boundary conditions given by equation (8) can be found, the following inte-

gral;

yields an algebraic equation from which the frequency of the system can be de-termined.

It can easily be shown that the function %

-(y + Kz)(y - Kz)(y - 2H + tf~Xy - 2H - Kz) (10)H.

Transactions on the Built Environment vol 3, © 1993 WIT Press, www.witpress.com, ISSN 1743-3509

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520 Soil Dynamics and Earthquake Engineering

satisfies the equation (8). After substituting equation (10) into equation (9)and performing the integration the following algebraic equation is obtained %

32 o>> H* J_ _ 32ffTT 5ff* 45* ~"

Solving equation (11) for w, we get:

^ (12)

This expression gives the first natural frequency , i. e. a>i of a symmetricaldam in a triangular canyon under vertical vibration, the function ip in equation(10) is corresponded to the first mode shape of vibration , i. e. #>i.

EARTHQUAKE RESPONSE ANALYSIS OF DAM

It is easily proved that the equation governing vertical vibration of dam withdamping under earthquake can be written as.

Where v, (O is acceleration of rigid canyon in the y direction and c is coefficientof damping.

By the method of separation of variables [r(y,z,0=i

and based upon the orthogonality of mode shape , the following two equations forthe first mode shape are obtained %

ti . »i , g 3»i , o, A$ "TT i "TT H -- Tr "^ -- -- T^i = UV ^ y — H 3y vi *

(15)

where o>i is first natural frequency given by equation (12), AI is damping ratioof first mode, it is equal to c/2pco\ , /% is mode participate coefficient

rT%io/-__ J o J oVI — f//ff/A'

J o J o

Transactions on the Built Environment vol 3, © 1993 WIT Press, www.witpress.com, ISSN 1743-3509

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Soil Dynamics and Earthquake Engineering 521

("\"* _L(y + /feXy - KzHy -2H + KzHy - 2H - Ks)<H - tfdydz_ Jojo a'

PT" 4i(y + Kz)(y - Kz)(y - 2H + Kz)(y - 2H - Ks)(H - y)dydzJ o J o H

= 1. 839

The solution of equation (15) is

(16)O/i J 0 *

where 0/1=0)1 Vl —/,{, the Duhamal integral may be calculated by numerical

integration method.Because the higher modes have little effect on earthquake response of dam,

only a few lower modes (1 — 3 order) are adopted for practical requirement.Then the earthquake responses of dam in triangular canyons can be approximate-ly written as follows (In order to simplify, the subscripts "1" of symbol o>i,a/i, jji, AI , ipi and 7\ in the following formulas are omitted) %

1 Displacement response

TT y - #z)(y + Kz)(y - 2H + Kz)(y - 2H - Ks) XH

(17)o/

2 Velocity response

f'%4r(v-JM(y + Kz)(y- 2H + Kz)(y - 2H - Kz) X

(18)a/ Jo

3 Acceleration response

4 Shear stress response

Transactions on the Built Environment vol 3, © 1993 WIT Press, www.witpress.com, ISSN 1743-3509

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522 Soil Dynamics and Earthquake Engineering

BHK*yz - 8#Wz) X

- r)dr (20)

5 Vertical normal stress response

X

- T)<*T (21)

In engineering it is most interesting in the max. response of dam and so thefollowing formulas of max. response are useful for earthquake-resistant design

of dam;

(22)

(23)

(y- 2H + KzHy- W - Kz)\S. (24)•c*,,«*i G\y,i)\S,

G| J (4A:V - 4 /2 + %HK*yz - BH^K^~) \S< (25)

- 2H + Kz)(y - 2H - Kz)\S,

where &, & and £„ are displacement response spectrum, velocity response spec-trum and acceleration response spectrum respectively, as shown in Fig. 2 [4].

COMPUTED EXAMPLE

Suppose the symmetrical earth dam in the trianguar canyon is subjected avertical earthquake (EL Centro record in 1940), the max. height of dam # =50m, the dynamic properties of dam meterial are i>, = 200m/s, damping ratio A= 0.1, Poisson's ratio /z=0. 3, Determine the first natural frequencies and thevarious max. responses in the central and L/4 sections of dam with the charts on

Transactions on the Built Environment vol 3, © 1993 WIT Press, www.witpress.com, ISSN 1743-3509

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Soil Dynamics and Earthquake Engineering 523

-j—i—i—i—i—i i i i i . . i0.6 0.8 1.0 1.2 1.4 /.6 1.8 2JO 2.2 2.4 2.6 2.3 3.0

Period of vibration TD (a)

/800

I2OO

600

0.2 0.4 0.6 0.8 1.0 1.2 /.4 /.6 /-a 2.0 2.2 2.4 2.6 2.8 3.O

period of vibration TD (s)

(c)

" O.2 04 0.6 0.8 I.O t.2 /.4 i.f, 1.8 2.0 2.2 2.4 26 23 3.O

Period of vibration TD (a)

Figure 2: El Centro earthquake (1940) response spectrum(a) Velocity spectrum; (b) Acceleration spectrum;(c) Displacement spectrum.

Transactions on the Built Environment vol 3, © 1993 WIT Press, www.witpress.com, ISSN 1743-3509

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524 Soil Dynamics and Earthquake Engineering

(e)

o

10-

20-

50

lO-

20-

30-

O

10-

20-

30-

v (cro/s)/? 20 _££_

(g)

v (an/s*)200 400 600

(h)

(Jfcftl)60

(0

20

50-

4O

so-i(j)

Figure 3: Distribution of various max. responses(a) ~ (e) — central section; (f) ~ (j) — L/4 section1, 2, 3, 4, 5 — case in Table 1

Transactions on the Built Environment vol 3, © 1993 WIT Press, www.witpress.com, ISSN 1743-3509

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Soil Dynamics and Earthquake Engineering 525

Fig. 2, for the cases of L = 50m, 100m, 200m and 300m (i. e. L/#=l, 2,4, 6) respectively.

Solution. For the case of L= 50m, K=2H/L= 2X50/50 = 2. Substititing the val-ues of i>.,H and K into equation (12), we get the first natural frequency u> and first naturalperiod TD as follows.

X 2(1 4- 0.3) 4-5 X 2' = 28. 08/a4

x

According to this value of TO and from the charts of response spectrum we get %S. = 15cm, S< = 0. 6cm, S. = 350cm/s*

Substituting the value of &, &, £., r) and G into equations (22) — (26), the variousmax. response distributions with depth are obtained. For the case of L=100m, 200m and300m, an analogous computation has been performed. The computed results are summarizedas in Table 1 and Fig. 3.

Table 1 Computed Results

case No.

L (m)

L/H

w (1/s)

r, (s)

1

50

1

28. 08

0.22

2

100

2

23.4

0.27

3

200

1

22. 1

0.28

4

300

6

21.8

0.29

CONCLUSION

The approximately analytical formulas developed in this paper are verysimple and they can be used for analysis of vertical vibration of earth and rock-fill dam in triangular canyons under earthquake notion, by corresponding simpli-fied method, such as response spectrum technique. Generally, analyses mayreadily be made by hand calculation even without a computer. A detailed examplecompution has shown that the analytical model presented here will provide infor-mation of practical as well as academic significance. The spatial distributions ofvarious max. response are conforming with general law.

REFERENCES

1. Mejia, L. H. and Seed, H. B. Three Dimensional Dynamic Response Anal-ysis of Earth Dams, Report No. EERC 81 — 51, University of California,Berkeley, 208-237, 1981.

Transactions on the Built Environment vol 3, © 1993 WIT Press, www.witpress.com, ISSN 1743-3509

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526 Soil Dynamics and Earthquake Engineering

2. Mejia, L. H. and Seed, H. B. Comparison of 2 —D and 3-D DynamicAnalysis of Earth Dam, J. Geotechnical Engng Div. ASCE 109, 11 '•

1383-1398.3. Xu Zhiying and Zhou Jian. Generation, Diffusion and Disspation of Seismic

Pore Water Pressure in Earth Dam by 3-D Dynamic Analysis, EarthquakeEngng and Engng Vibration, 5,4: 57 —72, 1985 (in Chinese).

4. Wiegel, R. L. Earthquake Engineering, Prentice-Hall, Inc. , London, 319

-320, 1970.

Transactions on the Built Environment vol 3, © 1993 WIT Press, www.witpress.com, ISSN 1743-3509


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