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A CASE STUDY OF PRELOADING IN PEAT USING FINITE ELEMENT METHOD WITH PLAXIS SOFTWARE
AMANDA ANAK MANGAN
'fA 347 Bachelor of Engineering with Honors F5 (Civil Engineering) A484 2009/20102010
P.KHIDMAT MAKLUMAT AKADEMIK
111111111 IINfrnill 1111111 1000212981
UNIVERSITI MALAYSIA SARA WAK
RI3a
BORANG PENGESAHAN STATUS TESIS
ludul : A CASE STUDY OF PRELOADING IN PEAT USING FINITE ELEMENT METHOD WITH PLAXIS SOFTWARE
SESI PENGAJIAN: 2009/2010
Saya AMANDA ANAK MANGAN (HURUF BESAR)
mengaku membenarkan tesis • ini disimpan di Pusat Khidmat Maklumat Akademik, Universiti Malaysia Sarawak dengan syarat-syarat kegunaan seperti berikut:
I. Tesis adalah hakmilik Universiti Malaysia Sarawak. 2. Pusat Khidmat Maklumat Akademik, Universiti Malaysia Sarawak dibenarkan membuat salinan untuk
tujuan pengajian sahaja. 3. Membuat pendigitan untuk membangunkan Pangkalan Data Kandungan Tempatan. 4. Pusat Khidrnat Maklumat Akademik, Universiti Malaysia Sarawak dibenarkan membuat salinan tesis ini
sebagai bah an pertukaran antara institusi pengajian tinggi. 5. •• Sila tandakan ( ~ ) di kotak yang berkenaan
D SULIT (Mengandungi maklumat yang berdiujah keselamatan atau kepentingan Malaysia seperti yang termaktub di dalam AKT A RAHSIA RASMI 1972).
D TERHAD (Mengandungi mak1umat TERHAD yang telah ditentukan oleh organisasil badan di mana penyelidikan dijalankan).
o TIDAK TERHAD
Disahkan oleh
~. (TANDMANGAN PENULIS) (TANDATANGAN PENYELIA)
Alamat tetap: LOT 222 KAMPUNG
STAPOK, lLN BATU KAWA PROF. K. G. H. C. NIMAL SENEVIRATNE Nama Penyelia
93250, KUCHING
Tarikh: Tarikh:
CATATAN * Tesis dimaksudkan sebagai tesis bagi Ijazah Doktor Falsafah, Sarjana dan Sarjana Muda.
** lika tesis ini SULIT atau TERHAD, sila lampirkan surat daripada pihak berkuasalorganisasi berkenaan dengan menyatakan sekali sebab dan tempoh tesis ini perlu dikelaskan sebagai SULIT dan TERHAD.
APPROVAL SHEET
Final Year Project as follows:
Title: A Case Study Of Preloading In Peat Using Finite Element Analysis With
PLAXIS Software
Author: Amanda Anak Mangan
Matrics number: 13700
Read and approved by:
Proffesor Dr K. G. H. C. Nimal Seneviratne Date
Project Supervisor
-
A CASE STUDY OF PRELOADING IN PEAT USING FINITE ELEMENT
ANALYSIS WITH PLAXIS SOFTWARE
AMANDA ANAK MANGAN
This report is submitted to Faculty of Engineering, Universiti Malaysia Sarawak
(UNIMAS) as to fulfill the requirements of Bachelor Degree with Honours (Civil
Engineering) 2010
-~ -~-~-
...T 0 m~ love and special ones...
Famil~ - thanks for ~our
x
never end care, support, understand ing and concern.
Iwill a~wa~s love ~ou
,
ACKNOWLEDGEMENT
The author would like to thank Prof. Dr. K.G.H. C Nimal Seneviratne for the
constant supervision and guidance throughout the process of completing this
report.
The author would also like to thank all individuals whom have contributed to the
success of this project.
ii
Abstrak
Tanah gambut dikategorikan sebagai tanah bennasalah kerana mempunyai
kekuatan ricih rendah dankebolehmampatan yang tinggi, yang ini tidak sesuai
untuk pembinaan. Tanah gambut merangkumi 13% dari tanah Sarawak di mana
jalan-jalan utama sebahagian besar dibina.Oleh kerana itu, adalah perIu untuk I
mencari altematif yang sesuai untuk meningkatkan kekuatan kerana tanah sangat
mahal dan sangat terhad. Pembebanan awal menggunakan pasir telah menjadi
teknik yang popular perbaikan tanah dasar gambut untuk sub jalan di
Sarawak. Penelitian ini menyajikan kesan dari preloading di gambut dengan
menggunakan kaedah elemen finit menggunakan software PLAXIS untuk
menunjukkan pembinaan berperingkat dengan pembebanan awal tambak dan
perkaitan penurunan konsolidasi dan karakteristik disipasi tekanan pori. Dua kes
dibuat dengan ada perbezaan dalam keadaan batas dan berbanding semasa
menggunakan material yang sarna, tahap pembinaan dan anal isis kadar konsolidasi
serta mesh kekasaran dalam model Regangan. Dari kes-kes yang dianalisis, jelas
bahawa penyebarari tekanan air pori dengan keadaan had terbuka di bahagian
bawah tanah gambut, dan penurunan konsolidasi yang lebih cepat berbanding
dengan kes di mana keadaan had tertutup di bahagian bawah
gambut. Kesimpulannya, tekanan pori akan membubarkan asalkan ada syarat batas
terbuka dan tidak menyebabkan perbezaan besar dalam penurunan konsolidasi, dan
kekasaran yang berbeza dalam generasi mesh subbase akan memberikan kegagalan
mekanisma yang berbeza. Oleh kerana itu, parameter sebenar sifat gambut harus
digunakan untuk kaj ian di masa depan.
111
Abstract
Peat is categorized as problematic soil because it has low shear strength and high
compressibility, which are not suitable for construction. Peat covers 13% of
Sarawak land where most major roads are constructed. Therefore, it is necessary to
find suitable alternatives to improve the strength since nowadays lands are very
expensive and very limited. Preloading using sand has been a popular technique of
peat ground improvement for road sub base in Sarawak. This study presents the
effect of pre loading in peat using finite element method using PLAXIS software to
model stage construction of a preloading embankment and associated
consolidation settlement and pore pressure dissipation characteristics. Two cases
are generated with differences in the boundary conditions and compared while
using the same material properties, stage of constructions and consolidation
analyses as well as coarseness mesh in a plain strain model. From the cases
analyzed, it is clear that the pore pressure disperses with open boundary condition
at the bottom of peat, and the rate consolidation settlement faster compared to the
case where closed boundary condition at the bottom of peat. In conclusion, the
pore pressure will disperse provided there is open boundary condition and it does
not lead to large difference in consolidation settlement, and different coarseness in
the sub base mesh generation will give different failure mechanism. Therefore, real
parametric of peat properties should be used for future research.
'11 at Kltiiliuat M Nl El<.S TJ ~A .. , ~ wnar MadclUik.
,yU\..W\¥SlA WI\¥.
Table of Content
Page
Dedication
Acknowledgement ii
Abstract iii
List of Tables vii
List of Figures viii
Chapter 1
Chapter 2
INTRODUCTION
1.1 Introduction
1.1.1 Peat Soil
1.1 .2 PLAXIS Software 3
1.2 Problem Statement 3
1.3 Purpose of Study 3
1.4 Objectives 4
1.5 Scope of study 4
LITERATURE REVIEW
2.1 Definition of Peat 5
2.2 Peat Classification 9
2.3 Peat Deposits in Malaysia 11
2.4 Preloading 13
2.4.1 Preloading Techniques 13
2.4.2 Principles of Pre loading 17
2.5 PLAXIS Software 20
v
212.5.1 Short Review of the Features
Chapter 3 METHODOLOGY
283.1 General
293.2 Problem Arise
333.3 Staged Construction
3.4 Geometric Preparation 35
373.5 Generation of Initial Stress
383.5.1 Case Study One
433.5.2 Case Study Two
443.6 Data Analysis
443.7 Result
Chapter 4 RESULTS AND ANALYSIS
454. I General
Chapter 5 CONCLUSION AND
RECOMMENDATION
595.1 General
595.2 Conclusions
605.3Recommendation
61References
63Attachment I
vi
List of Tables
Table Page
62.1 Standard Unified Soil Classification
2.2 Malaysian Soil Classification system for 8
engineering purposes and field identification
(Organic Soils and Peat Part Only)
2.3 Classification ofpeat on the basis of 11
decomposition on the von Post scale.
2.4 Areas under peat in the various administrative 12
divisions in Sarawak (km2)
3.1 Material properties of the road embankment and 36
subsoil
vii
List of Figures
Figure Page
1.1 Peatswamp land forest in Sarawak (Department of 2
Irrigation and Drainage Sarawak, 2009)
2.1 An excavator sunk into the soft soil 5
2.2 Principles of preloading 14
2.3 Settlement vs time 15
2.4 Vacuum system 16
2.5 Vertical stress profile (a) initial in situ condition, 18
(b)conventional surcharge and (c) vacuum-induced
surcharge
3.1 Flow to conduct the project 31
3.2 Flow of conducting the staged construction using 32
PLAXIS
3.3 Situation of typical road embankment on soft soil 34
3.4 Geometry model in the Input window (PLAXIS) 35
3.5 Generated mesh 37
3.6 Closed consolidation condition on left and right 39
3.7 Initial stress generation 40
3.8 Construction of first layer of embankment 41
3.9 Phase input data 42
3.10 Point of selection for curve generation 43
4.1 Plot ofdeformed mesh 45
Vlll
4.2 Plot ofhorizontal displacements (arrows) 46
4.3 Plot of horizontal displacements (contour lines) 47
4.4 Plot ofvertical displacements (arrows) 47
4.5 Plot of vertical displacements (contour lines) 48
4.6 Plot ofhorizontal increments (arrows) 48
4.7 Plot ofvertical increments (arrows) 49
4.8 Plot of effective stresses (principal directions) 49
4.9 Plot of horizontal displacements (arrows) 50
4.10 Plot ofvertical displacements (arrows) 50
4.11 Plot of horizontal increments (arrows) 51
4.12 Plot ofvertical increments (arrows) 51
4.13 Plot of excess pore pressures (shadings) 52
4.14 Plot of effective stress (principal directions) 53
4.15 Plot ofgroundwater head (contour lines) 53
4.16 Active pore pressure vs time 54
4.17 Increment of steps in meter vs time 55
4.18 Steps increment vs time 56
4.19 Case 2 Closed consolidation condition 57
CHAPTER!
INTRODUCTION
1.1 Introduction
Land development is constantly growing, in line with the increasing demand
and population of the country. Construction of infrastructure over soft soil such as
peat is a need to solve the increasing demand and decreasing land availability.
Since peat soil is categorized as problematic soil, it is essential to study the
settlement of soil prior to construction. Therefore, this project will concentrate on
the effect preloading, especially road constructed on peat soil.
In the past few years, there is increasing number of researches been done to
model the constructions over soft soils. These modelling and case study will be
elaborated further in Chapter 2.
1.1.1 Peat soil
Peat is categorized under soft soil and organic soil. According to Huat et. al
(2004), this type of soil covered about 3.0 million hectares or 8.0% of the
Malaysian land. Although problematic, engineers believed that there are ways to
improve the soft soil condition, appropriate for construction. The peat soil
properties will be discussed further in Chapter 2 as well.
Figure 1.1 shows the distribution of roads constructed on peaty area. Most
major cities in Sarawak are located by the river bank, areas where soft soil such as
sandy and peat swamp is the main ground. History tells that the riverside
economic growth is much better due to the ease in transportation . Nowadays,
people prefer to travel either on land or by air. Therefore, it is important to
improve the road facilities in Sarawak.
t SOJTH CHI~lA SEA
KAllMANnN
E3 EXISTING ROAD
• PEATSOlS
Figure 1.1 Peatswamp land forest in Sarawak (Department of Irrigation and Drainage Sarawak, 2009)
2
1.1.2 PLAXIS software
PLAXIS is a geotechnical software, developed to assist in analyzing the
deformation and stability in geotechnical engineering problems. Geotechnical
applications require advanced structured models for the simulation of the non
linear and time-dependent behaviour of soils. Furthermore, since soil is a multi
strata material, special procedures are required to deal with hydrostatic and non
hydrostatic pore pressures in the soil. Although the modelling of the soil itself is
an important issue, many geotechnical engineering projects mix up the modelling
of structures and the interaction between the structures and the soil. PLAXIS is
equipped with special features to deal with the numerous aspects of complex
geotechnical structures. These features will be elaborated further in Chapter 2.
1.2 Problem statement
Preloading, also known as precompression is a method involving placement
and removal of dead load (Bell, 1993). The problem arise from this method is time
dependent. PLAXIS is designed to overcome this method by analyzing the soil
behaviour prior to construction.
1.3 Purpose of study
The study aims to use PLAXIS to demonstrate the effect of preloading to
improve the road construction method over sub grade that consists of peat soil.
3
1.4 Objectives
To achieve the mentioned alms stated above, it is essential to fulfill the
objectives as follows:
i) To understand the effect of preloading on peat soil as the sub
grade.
ii) To demonstrate the effect of preloading in peat using PLAXIS
software.
iii) To use PLAXIS and finite element method to determine
deformation and failure due to preloading and relate them to soil
properties.
1.5 Scope of study
The scope ofthis project is to study the behaviour of peat upon preloading,
and the application of finite element method in solving peat deformation. The
analysis is based on research and reports obtained, from publish literature and also
from relevant party and authority.
This study will focus on the analysis of effect of preloading on peat using
finite element code, PLAXIS. The software used will be PLAXIS 2D-Version 8.
4
CHAPTER 2
LITERATURE REVIEW
2.1 Definition of peat
In the engineering point of view, peat is recognized as highly compressible
type of soil. Engineers are reluctant to construct on peat lands because of the
difficulty to access the site and other problems related to unique characteristics of
peat. Peat poses high moisture content, other than very high and long term
settlement. These characteristics usually raise problems from preconstruction to
the post construction. One such problem is shown in Figure 2.1.
Figure 2.1: An excavator sunk into the soft soil
5
Geologist identifies the peat soil as a separate soil entity and the Unified Soil
Classification System (USC), which is adopted by the American Society for
Testing and Materials (ASTM) as the standard classification of soils for
engineering purposes and has been described as having been accepted in
international geotechnical communication. It has a major division called Highly
Organic Soils (pt) which refers to peat, muck and other highly organic soils
(ASTM, 2007).
Table 2.1: Standard Unified Soil Classification
Group Group nameMajor divisions symbol
clean gravel GW
well graded gravel,
gravel <5% smaller fine to coarse gravel
> 50% ofcoarse than no. 200 Coarse GP poorly graded gravel
fraction retained Sieve grained
soils on No.4 (4.75 gravel with GM silty gravel ·
more than mm) sieve >12% fines GC clayey gravel 50%
well graded sand, fine retained on SW No.200 sand clean sand to coarse sand
(0.075 mm) 2: 50% ofcoarse SP I
poorly-graded sand sieve fraction passes sand with SM silty sand
No.4 sieve >12% fines SC clayey sand
ML silt. . morgamc
CL claysilt and clay
Fine grained liquid limit < 50 organic OL
I
organic silt, organic clay
soils more than MH
silt of high plasticity,
50010 passes elastic silt
No.200 inorgahic
clay of high plasticity, sieve silt and clay I CH
fat clay liquid limit 2: 50
orgamc I
OH organic clay, organic silt
HighJy organic soils Pt Peat
Malaysia termed her own soil classification, suitable for the local use, a
proposed from the Public Works Department, Malaysia together with (Jarret,
1991). According to Jarret, peat soil in Malaysia can be subdivided into three
categories, which differs in their organic content respectively. This organic
content is three-point scale classification based on fiber content resulting from
decomposition and humidification according to the U.S Department of Agriculture
(USDA). A fiber is defined as > 0.15mm. The organic fiber content has been
referred to as the fabric of the organic soil. An appreciation of the constituent
matter and its attributes like orientation aids in the constitutive modelling of this
soil type for basic understanding of the mechanical behaviour.
7
00
'able 2.2: Malaysian Soil Classification system for engineering purposes and field identification (Organic Soils and Peat Part Only)....... .....II I...-........ ~... I) 57 rd.
~o~.,... ~II'MP----... ...........~=.. ,......,ILIOHTLYORGANIC 140 9OU.S .... ORGANIC Noa...-SlLT P&ATS 00
Sli",Orpnic SOILS
<JjFo ao ,,.,.CLAY Clioar.eyo-.3. 50-70
2Oko Co CEo 10-90 :090
ORGASIC OROA."JC SOILS 0
SOILS Qrsaftje CGmcnt 3)%...75%
II......,. ar...- SIL(........ 1iIce Co)
~ 0rpNe CLAY of1_ plMticky SliIhdJ Or.,- CLAY of ................dclty lIilhdY o.anlc CLAY or...... ..iQo II....,. Or.wc CLAY ofwry hip plMlicil)' ~!rJ'..~ CLAY or ........Iyiii tiCilY
Subdivision ofOrpnic Soih is cil&cuk•• ntidler die humirlCalion _u _ rdlUlo Ix IboIlL "'weh a "'ties. Ale,," is die proa.w. 0IM0me of IUbdivision l.mna 10 dMa'iplion aac:h .. -Fillrous ORCiA!'IlIC SOIL" Or"~ ORGA.'f1C SOILoflntermedJale PlastEitv.
PEATS PEAT PI Plf HI.H3 Flbric: or FlbtooI Pclu. ~ K4-H6 Hemic or Mocter.ely lJieeompoled
Orpnic lUI H7-HIO P-. Concent SIpric or AmoqJhout ,. more ..... n 7$%
u.uaII)< Vft)' .-Ie 10 .,... i. 1IOIour ...... _of .........,. Ibc YiIibIc. Oftea_ .....dwe GIpIIic s_IL
~ _""" 10black il'I eolour. ~"halow ....iIy.. -.. • .... MljoIily of~.il Grpnic SO if ~dIc whole ~I will Ibc reoopi.ble"'.1 ICmir1e.More likely 10 IUN."II IIrOapy if hilihlV humiRed
Note: The mcthodoiosy for estimatins the Orsanic Content and Degree of Humific:ation UBin, the Van Post
In the world of forestry, peat swamp forests are waterlogged forests growing
on a layer of dead leaves and plant material up to 20 meters thick. They comprise
an ancient and unique ecosystem characterized by water logging, with low
nutrients and dissolved oxygen levels in acidic water regimes. Their continued
survival depends on a naturally high water level that prevents the soil from drying
out to expose combustible peat matter. This harsh waterlogged environment has
led to the evolution of many species of flora uniquely adapted to these conditions.
Unlike engineers and geologist, the people in the forestry field appreciate the water
logging condition in peat.
Peat properties enables it to accommodate the need of peat swamp forest to
produce a dynamic link between land and water, a transition zone where the flow
of water, the cycling of nutrients and the energy of the sun combine to produce a
unique ecosystem of hydrology, soils and vegetation (United Nations Development
Programme (UNDP) & Ministry of Natural Resources and Environment Malaysia,
2008). These swamps provide a variety of goods and services, both directly and
iDdirectly, in the form of forestry and fisheries products, energy, flood mitigation,
water supply and groundwater recharge.
U Peat classification
In engineering practice, the peat classification and division is based on visual
inspection of the structure and consistency and on the squeezing test according to
von Post (1924), (see Table 2.3). The following is a distinctive description of the
caaegorized peat:
9
• Fibrous peat is low-humified and has a distinct plant structure. It is brown
to brownish-yellow in colour. If a sample is squeezed in the hand, it gives
brown to colourless, cloudy to clear water, but without any peat matter.
The material remaining in the hand has a fibrous structure. (Degree of
decomposition on the von Post scale; H I-H4.)
Pseudo-fibrous peat is moderately humified and has an indistinct to
relatively distinct plant structure. It is usually brown. If a sample is
squeezed in the hand, less than half of the peat mass passes between the
fingers. The material remaining in the hand has a more or less mushy
consistency, but with a distinct plant structure (H5- H7).
• Amorphous peat is highly humified. The plant structure is very indistinct
or invisible. It is brown to brown-black in colour. If a sample is
squeezed in the hand, more than half of the peat mass passes between the
fingers without any free water running out. When squeezing, only a few
more solid components, such as root fibres and wood remnants can be felt.
These constitute any material remaining in the hand, (H8-HIO).
10
Table 2.3: Classification of peat based on the decomposition of fibre content according to the von Post scale.
Dllipation Group Description
Fibrous peat HI-H4 Low degree of decomposition. Fibrous
structure. Easily recognizable plant
structure, primarily of white mosses.
Psc:udo-fibrous peat H5-H7 Intennediate degree of decomposition.
Recognizable plant structure.
Amorphous peat H8-HIO High degree of decomposition. No
visible plant structure. Mushy
consistency.
Peat deposits in Malaysia
Peat as mentioned earlier is classified as one of the major problematic soils
found in Malaysia. Over 3.0 million hectares of Malaysia is covered with peat
(Huat et al. 2004). The areas covered with peat deposits are found where the
conditions are favourable for their fonnation (Duraisamy, Bujang, & Azlan, 2007).
For example on the west coast of Malaysian Peninsular, the deposits are fonned in
depressions consistin~ predominantly of marine clay deposits or a mixture of
marine and river deposits especially in areas along river courses. In Figure 1.1 the
bmation are found near the coastal area. There are two types of peat deposit, the
Ihallow deposit usually less than 3 m thick while the thickness of deep peat deposit
in Malaysia exceeds 5 m.
In the past decade the development of peat land in Malaysia is almost
avoidable although construction on marginal land such as peat has become
11