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CORRELATION BETWEEN CONE PENETRATION TEST AND BEARING CAPACITY FOR SHALLOW FOUNDATION MAZLAN AHMAD A project report submitted in partial fulfillment of the requirements for the award of the degree of Master of Engineering (Civil – Geotechnics) Faculty of Civil Engineering Universiti Teknologi Malaysia APRIL 2007

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Page 1: MAZLAN AHMAD A project report submitted in partial

CORRELATION BETWEEN CONE PENETRATION TEST AND BEARING

CAPACITY FOR SHALLOW FOUNDATION

MAZLAN AHMAD

A project report submitted in partial fulfillment of the requirements for the

award of the degree of Master of Engineering (Civil – Geotechnics)

Faculty of Civil Engineering

Universiti Teknologi Malaysia

APRIL 2007

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DEDICATION

To my beloved mother, wife and daughters,

Thank you very much for your love, patience and support.

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ACKNOWLEDGEMENT

I am very grateful for the support and help of numerous individuals whom have lent

me support and advice in completing my Master Degree.

I would like to thank Associate Professor Ir. Dr. Ramli Nazir whom has guided me in

completing this study.

My sincere appreciation to Associate Professor Dr. Nurly Gofar for her advice.

Special words of thanks to Ir Ismail Abd. Rahman for making available the data for

the study.

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ABSTRACT

The Cone Penetration Test (CPT) is a simple and versatile test that is becoming more

popular in Malaysia for soft clay and fine to medium coarse sand. It can be used as a

direct method to determine the soil bearing capacity for a foundation. Analyses were

carried out on the CPT data from local project site based on the published correlation

and. Data were grouped into cohesive and non cohesive. Based on the results, it is

observed that the current published correlations are not suitable to be used in

Malaysia. Meyerhof’s Bearing Capacity and Schmertmann’s equations were used to

obtain the estimated bearing capacity. These figures were then plotted on the graphs

and the best fit lines are obtained. Two correlations had been evaluated and

presented. These correlations represent cohesive and non cohesive soil respectively.

From the two correlations, it can be concluded that Schmertmann’s correlation gives

a much higher value compared with bearing capacity calculated using Meyerhof’s.

However it shall be noted that the lack of data prevents a better correlation from

being produced. A correlation had been proposed in the study to predict the soil

bearing capacity value based on the tip resistance. However these correlations are not

to be used in practice due to its limitation of data. The published correlations are not

suitable to estimate the soil bearing capacity for shallow foundation for soil under

study Bearing Capacity correlation for cohesive and non cohesive soils proposed by

Schmertmann is likely to overestimate the actual bearing capacity values. The

correlation is not appropriate to be used in Malaysia.

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ABSTRAK

Ujian Penusukan Kon (CPT) merupakan ujian yang mudah dan seba boleh di mana ia

lebih popular di Malaysia bagi tanah liat lembut dan pasir halus hingga sederhana. Ia

boleh digunakan sebagai kaedah langsung untuk memperolehi keupayaan galas tanah

bagi rekabentuk asas. Analisis dilakukan daripada data CPT daripada tapak projek

tempatan berdasarkan hubungan terbitan. Data diketegorikan kepada jelekit dan tidak

jeleket. Berdasarkan kepada keputusan yang diperolehi, dapat dilihat bahawa

hubungan terbitan sekarang tidak sesuai digunakan di Malaysia. Persamaan

keupayaan galas Meyerhof dan Schmertmann digunakan untuk mendapatkan

anggaran keupayaan galas. Nilai yang diperolehi kemudiannya diplot ke dalam graf

dan seterusnya untuk garis terbaik diperolehi. Dua hubungan akan dinilai dan

dipaparkan. Hubungan yang diperolehi ini mewakili tanah jeleket dan tidak jeleket.

Daripada dua perhubungan ini, ia boleh disimpulkan bahawa hubungan

Schmertmann memberi nilai yang lebih tinggi berbanding nilai keupayaan galas yang

dikira menggunakan hubungan Meyerhof. Walau bagaimanapun, perlu diketahui

bahawa kekurangan data menghalang hubungan yang lebih baik dihasilkan. Suatu

hubungan akan dicadangkan dalam kajian ini bagi meramalkan nilai keupayaan galas

tanah berdasarkan rintangan yang diberi. Bagaimanpun, tidak digunakan sebagai

a,alan disebabkan data yang terhad. Hubungan terbitan tidak sesuai untuk

menganggar keupayaan galas tanah bagi asas cetek. Untuk tanah di bawah kajian

hubungan keupayaan galas untuk tanah jeleket dan tidak jeleket yang dicadangkan

oleh Schmertmann seperti terlebih anggaran daripada nilai keupayaan galas sebenar.

Hubungan ini tidak sesuai untuk digunakan di Malaysia.

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TABLE OF CONTENTS

CHAPTER TITLE PAGE

DECLARATION ii

DEDICATION iii

ACKNOWLEDGEMENT iv

ABSTRACT v

ABSTRAK vi

TABLE OF CONTENTS vii

LIST OF TABLES

LIST OF FIGURES

LIST OF SYMBOLS

LIST OF APPENDICES

1 INTRODUCTION

1.1 Introduction 1

1.2 The History of CPT 3

1.2.1 Mechanical Cone Penetrometers 3

1.2.2 Electric Cone Penetrometers 6

1.2.3 The Piezocone 7

1.3 Problem Statement 8

1.4 Aim and Objective of Studies 9

1.5 Scope of Studies 9

1.6 Expected Finding 10

2 LITERATURE REVIEW

2.1 Introduction 11

2.2 Cone Penetrometer and Piezocone 11

2.3 Pushing Equipment 13

2.4 Test Procedures 14

2.4.1 Continuous test 14

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2.4.2 Verticality 14

2.4.3 Rate of Penetration 15

2.4.4 Interval of Readings 15

2.4.5 Measurement of the depth 15

2.5 Data Acquisition 15

2.6 Calibration of Sensors 16

2.7 Maintenance 17

2.8 Precision and Accuracy 17

2.9 Application of Cone Penetration Test 17

2.10 Correlation between CPT and Soil Bearing Capacity 19

2.10.1 Schmertmann’s Method 21

2.10.2 Meyerhof’s Method 22

3 METHODOLOGY

3.1 Introduction 25

3.2 Source of Data 28

3.2.1 Data Selection 28

3.3. Data Analysis 28

4 RESULTS AND DISCUSSION

4.1 Introduction 30

4.2 Discussion 76

5 CONCLUSIONS AND RECOMMENDATIONS 77

REFERENCES 79

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LIST OF TABLES

TABLE NO. TITLE PAGE

2.1 SPT-N vs qc correlations 20

2.2 Meyerhof’s Bearing Capacity, Shape and Depth Factors 23

3.1 Flowchart of the study 26

4.1 Raw data for CPT 38 31

4.2 Raw data for CPT 40 33

4.3 Raw data for CPT 41 35

4.4 Raw data for CPT 42 37

4.5 Raw data for CPT 43 39

4.6 Raw data for CPT 44 41

4.7 Raw data for CPT 107 43

4.8 Raw data for CPT 108 45

4.9 Raw data for CPT 260 47

4.10 Raw data for CPT 261 49

4.11 Raw data for CPT 263 51

4.12 Raw data for CPT 264 53

4.13 Raw data for CPT 265 55

4.14 Raw data for CPT 266 57

4.15 Raw data for CPT 268 59

4.16 Raw data for CPT 39 61

4.17 Raw data for CPT 105 63

4.18 Raw data for CPT 106 65

4.19 Raw data for CPT 262 67

4.20 Tabulation of average cone resistance and N values at 1.5m

deep

69

4.21 Summary of soil parameters at 1.5m deep 72

4.22 Summary of qu 73

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LIST OF FIGURES

FIGURE NO. TITLE PAGE

1.1 Terminology for cone penetrometers 2

1.2 Dutch cne with conical mantle (Sanglerat 1972) 4

1.3 Begemann type cone with friction sleeve (Sanglerat

1972)

5

1.4 The Fugro electrical friction cone 6

1.5 The Wissa Pizometer Probe (Wissa et al. 1974) 7

2.1 Cone Penetrometer 12

2.2 Self propelled crawler 13

2.3 Data Acquisition Equipment 16

2.4 qc vs N for African residual soil (from Ajayi and

Balogun, 1988)

19

2.5 qc vs N for Singapore residual soils (from Chang, 1988) 20

2.6 Correlation between bearing capacity of footing on

cohesionless soils and average cone resistance

(Eslaamizaad and Robertson, 1996)

22

3.1 Flowchart of the study 26

3.2 Typical test data 27

4.1 Depth vs Cone Resistance for CPT 38 32

4.2 Depth vs Cone Resistance for CPT 40 34

4.3 Depth vs Cone Resistance for CPT 41 36

4.4 Depth vs Cone Resistance for CPT 42 38

4.5 Depth vs Cone Resistance for CPT 43 40

4.6 Depth vs Cone Resistance for CPT 44 42

4.7 Depth vs Cone Resistance for CPT 107 44

4.8 Depth vs Cone Resistance for CPT 108 46

4.9 Depth vs Cone Resistance for CPT 260 48

4.10 Depth vs Cone Resistance for CPT 261 50

4.11 Depth vs Cone Resistance for CPT 263 52

4.12 Depth vs Cone Resistance for CPT 264 54

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4.13 Depth vs Cone Resistance for CPT 265 56

4.14 Depth vs Cone Resistance for CPT 266 58

4.15 Depth vs Cone Resistance for CPT 268 60

4.16 Depth vs Cone Resistance for CPT 39 62

4.17 Depth vs Cone Resistance for CPT 105 64

4.18 Depth vs Cone Resistance for CPT 106 66

4.19 Depth vs Cone Resistance for CPT 262 68

4.20 Correlation between qc and qu for non cohesive soil 70

4.21 Correlation between qc and qu for cohesive soil 71

4.22 Best fit line for non cohesive soil 74

4.23 Best fit line for cohesive soil 75

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LIST OF SYMBOLS

CPT - Cone Penetration Test

SPT - Standard Penetration Test

EFCS - Extended Field Computer System

Qc - The total force acting on the cone

Ac - Projected area of then cone

qc - Cone resistance

Fs - Total force acting on the friction sleeve

fs - Sleeve friction

qu - Ultimate Bearing Capacity

n.a. - not applicable

o.m. - organic material

o.r. - out of range

s.f.g - sensitive fine grained

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CHAPTER 1

INTRODUCTION

1.1 Introduction

The design and construction of foundations require a good knowledge of the

mechanical behaviour of soils and of their spatial variability. Such information can be

best obtained from a properly planned programme of both laboratory and in situ tests.

Among the vast number of in situ devices, the static penetrometer or Cone Penetration

Test (CPT) represents the most versatile tool currently available for soil exploration.

In the Cone Penetration Test, a cone on the end of a series of rod is pushed into

the ground at a constant rate and continuous or intermittent measurements are made of

the resistance (cone / tip resistance and sleeve friction) to penetration of the cone. The

penetration resistance which is digitized permits detail inferences about sratigraphy and

lithology. CPT is a reliable and efficient method of obtaining soil-engineering

parameters for geotechnical design.

Cone Penetration Tests are conducted to obtain the cone resistance, the side

friction and, if there is a piezocone, the pore pressure. The soil type can be determined

by analyzing these results, the values can also be used in the design of shallow

foundations through the estimation of stiffness and shear strength of cohesive soils.

The total force acting on the cone, Qc, divided by the projected area of the cone,

Ac, produces the cone resistance, qc. The total force acting on the friction sleeve, Fs,

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divided by the surface area of the friction sleeve As, produces the sleeve friction, fs. In

the piezocone penetrometer, pore pressure is measured typically at one, two or three

locations as shown in Figure 1.1. These pore pressures are known as: on the cone (u1),

behind the cone (u2) and behind the friction sleeve (u3).

A 60o cone with face area 10cm

2 and 150cm

2 'friction sleeve' is hydraulically

pushed into the ground at a constant speed (ranging form 1.5 to 2.5 cm/s). The force

required in maintaining this penetration rate and the shear force acting on the friction

sleeve are recorded. The friction ratio (cone resistance / side friction) gives an indication

of the soil type.

Figure 1.1: Terminology for cone penetrometers.

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Probing with rods through weak ground to locate a firmer stratum has been

presented since 1917. It was in the Netherlands in 1932 that CPT was introduced in a

form recognizable today.

A cone penetrometer with a 10cm2 base area cone with an apex angle of 60

o is

accepted as the reference and has been specified in the International Reference Test

Procedure (ISSMFE, 1989)

The cone penetration tests provide continuous sounding capability and good

repeatability. The CPT has three main applications in the site investigation process:

i. to determine sub-surface stratigraphy and identify materials present

ii. to estimate geotechnical parameters

iii. to provide results for direct geotechnical design

1.2 The History of CPT

Comprehensive reviews of the history of penetration testing in general have been

given by Sanglerat (1972) and Broms and Flodin (1988).

1.2.1 Mechanical Cone Penetrometers

The first Dutch cone penetrometer test were made in 1932 by P. Barentsen, an

engineer at the Rijkwaterstaat (Department of Public Works) in Holland. A gas pipe of

19 mm inner diameter was used; inside this is a 15 mm steel rod could move freely up

and down. A cone tip was attached to the steel rod. Both the outer pipe and the inner rod

with the 10 cm2 cone with a 60

o apex angle were pushed down by hand (Barentsen,

1936). Barentsen corrected the measured cone resistance by subtracting the weight of the

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inner rod. The maximum penetration depth was 10-12 meters and the penetration

resistance was read on the manometer.

Several Dutch and Belgian engineers used the early version of the cone

penetration test for evaluating pile bearing capacity (e.g. Buisman, 1935; Huizinga,

1942; de Beer, 1945; Plantema, 1948)

Figure 1.2: Dutch cone with conical mantle (Sanglerat 1972)

Begemann (1953, 1969) significantly improved the Dutch static cone penetration

test by adding an “adhesion jacket” behind the cone. Using this new device the local

skin friction could be measured in addition to the cone resistance. Measurements were

made every 0.2 m and for special purposes the interval could be decreased to 0.1 m.

Begemann (1965) was also the first to propose that the friction ratio (sleeve friction/cone

resistance) could be used to classify soil layers in terms of soil type.

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Figure 1.3: Begemann type cone with friction sleeve (Sanglerat 1972)

Most mechanical cone penetrometers measure the force needed to press down the

inner rod with a manometer at ground level. Mechanical cone penetrometers are still

widely used because of their low cost, simplicity and robustness. In rather homogeneous

competent soil, without sharp variations in cone resistance, mechanical cone data can be

adequate, provided the equipment is properly maintained and the operator has the

required experience. Nevertheless, the quality of the data remains somewhat operator

dependent. In soft soils, the accuracy of the results can sometimes be inadequate for a

quantitative analysis of the soil properties. In highly stratified materials even a

satisfactory qualitative interpretation may be impossible.

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1.2.2 Electric Cone Penetrometers

According to Broms and Flodin (1988) the very first electric cone penetrometer

was probably developed in Berlin during the Second World War.

Figure 1.4: The Fugro electrical friction cone

The signals were transmitted to the ground surface through a cable inside the hollow

penetrometer rods. Muhs (1978) reviewed the main improvements of the new

penetrometer relative to mechanical cone penetrometer namely:

1. The elimination of possible erroneous interpretation test results due to friction

between inner rods and outer tubes.

2. A continuous testing with a continuous rate of penetration without the need for

alternative movements of different parts of the penetrometer tip and no possibility

for undesireable soil movements influencing the cone resistance.

3. The simpler and more reliable electrical measurement of the cone resistance with the

possibility for continuous readings and easy recording of the results.

Another reason for using electrical measurement systems is that very sensitive load

cells can be used and thereby much more accurate readings can be obtained in very soft

sols.

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The first electrical cone penetrometer in Holland, called the Rotterdam cone, was

developed and patented, in 1948 by the municipal engineer Bakker. A large number of

different electric cone penetrometers have been developed in many countries all over the

world. However, the mechanical cone penetrometer is still used in some countries.

1.2.3 The Piezocone

A conventional electric piezometer, developed by the Norwegian Geotechnical

Institute (NGI), was used by Janbu and Senneset (1974) to measure pore pressures

during penetration adjacent to CPT profiles. Schmertmann (1974) also pushed in a

piezometer probe and measured penetration pore pressures.

Figure 1.5: The Wissa Pizometer Probe (Wissa et al. 1974)

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Schmertmann recognized the importance of pore water pressure measurement for

the interpretation of CPT data. Both Janbu and Senneset and Schmertmann showed the

results of the changes in pore pressures during a pause in the penetration.

Schmertmann (1978) used the Wissa type piezometer probe and a 60o cone with

filter at the tip in a study of the evaluation of liquefaction potential of sands. Baligh et al.

(1980) also did test with the Wissa probe in addition to tests with 60o cones with various

filter locations. However, each cone recorded only pore water pressure and from only

one sensing filter elements. Parallel tests were performed with the electric cone

penetrometers. Baligh et al. suggested that the pore water pressure data, when combined

with the CPT data, could provide a promising method for soil identification and an

estimate of overconsolidation in a clay deposit.

A large number of piezocones have been developed in recent years. For practical

projects pore pressures are not normally measured at one location; most frequently

behind the cone. For research and special projects, piezocone with two or three filter

positions have been developed. Bayne and Tjelta (1987) and Zuidberg et al. (1987)

reported the development of the triple element piezocones.

With the measurement of pore water pressures it became apparent that it was

necessary to correct cone resistance for pore water pressure effects.

1.3 Problem Statement

CPT is gaining popularity in Malaysia and the data obtained has been used for

the design of foundation through empirical correlation. However the correlation used in

the design of foundation is based on the foreign soil and still yet to be established for

Malaysian soil condition. Thus the application of these correlations for Malaysian soil

will lead to an erroneous conclusion.

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1.4 Aim and Objectives of Studies

The aim of the study is to find the correlation between CPT values and Soil

Bearing Capacity that best suit the type of soils in Malaysia. In order to achieve this aim,

three objectives have been identified for the study:

i. To evaluate published correlation for CPT values and the soil bearing capacity.

ii. To tabulate the CPT values obtained from collected soil sample and propose the

best fit line with respect to the soil bearing capacity.

iii. To obtain a correlation between CPT values with soil bearing capacity that is

best suited for the type of soil in Malaysia. Two (2) correlations will be produced

to differentiate cohesive and non cohesive soil.

1.5 Scope of Study

Ninteen (19) numbers of peizocone and eight (8) numbers of boreholes were

carried out at the proposed site of “Cadangan Pembinaan Pusat Angkasa Negara Di Atas

Lot 2233 Mukim Kelanang, Daerah Kuala Langat, Selangor Darul Ehsan”.

Two sets of equation will be used through out the study;

i. Interpretation of data for soil bearing capacity will be applied through

Meyerhof’s (1951) General Bearing Capacity equation. The values for cohesion,

soil unit weight and angle of friction are obtained from the lab test carried out to

the undisturbed sample of soil retrieved during the deep boring works.

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ii. Interpretation of data for soil bearing capacity with respect to the cone resistance

will be applied through equation developed by Schmertmann (1978). The values

of cone resistance are obtained from the Cone Penetration Test.

iii. Correlation between cone resistance and N values is produced as a matter of

comparison to the works which have been carried by other researchers.

1.6 Expected Findings

Cone Penetration Test is one of the available methods apart from SPT to

determine the soil strength. It can be directly used in design of foundation but usually is

incorporated with correlation based on local conditions. However since they are

generalized, the empirical relationship used may not be applicable locally. An empirical

correlation for local condition is expected to be derived from the collected data. This

correlation will help geotechnical designers to improve the reliable interpretation

methods used to estimate the bearing capacity of Malaysian soil using CPT.