the effectiveness of coconut coik blanket in
TRANSCRIPT
THE EFFECTIVENESS OF COCONUT COik BLANKET IN CONTROLLING
SLOPE EROSION
AIZAT BIN MOHD TAIB @ TAlE
A thesis submitted in partial fulfillment of the requirements for the award of the
degree of Bachelor of Civil Engineering
Faculty of Civil Engineering & Earth Resources
Universiti Malaysia Pahang
DECEMBER 2010
ABSTRACT
A research to determine the effectiveness of coconut coir blanket in
controlling slope erosion was conducted. There were two major division of testing
made. One was the material analysis on the soil sample taken and the coconut coir
blanket used and another was the simulation of rainfall pouring on sloped surface soil
to analyze the erosion rate. Apparently, the division of material testing involved Soil
Mechanics Engineering and Light Structure Engineering. Soil Mechanics
Engineering assisted this research in soil analyzing in terms of the Soil
Classification, Atterberg Limit, Specific Gravity, Shear Strength, Standard Proctor
and Direct Shear testing. On the other hand, Light Structure Engineering focused on
Tensile Strength of the coconut coir blanket. Generally, the major testing was the
simulation of rainfall on the sloped surface soil. The soil sample which was taken
from construction site in Bukit Gambang,. Pahang was distributed into four cases.
The parameters manipulated were the degree of slope, type of vegetation and the
condition of the slope surface. The selected degree of slope were 0°, 100, 20°, 300,
400 and 500. The vegetations planted were based on the norm slopes grasses used
which were the Signal Grass and Japanese Millet. The conditions of the slope surface
were divided into two. They were bare controlled case and protected slope case using
coconut coir blanket. The main parameter which was the application of coconut coir
blanket as the protection to the slope was proven effective. By comparing the bare
controlled slope and the protected slope, the result showed that protected slope using
the coconut coir blanket decreases the erosion rate by the Total Suspended Solids
(TSS) test conducted. The bare controlled slope collected 0.014345 g/L amount of
TSS while protected slope using coconut coir blanket collected only 0.001368 g/L.
The difference of 0.0 12977 g/L TSS amount proved that coconut coir blanket was
effective in controlling slope erosion assisted by the vegetation of Signal Grass
which has longer leaves and gripping fibre roots in increasing the mode of slope
strength.
A
vii
ABSTRAK
Satu kajian untuk menentukan keberkesanan karpet sabut kelapa untuk
mengawal hakisan cerun telah dijalankan. Terdapat dua bahagian bagi ujikaji yang
dijalankan iaitu analisa ke atas sampel tanah diambil termasuklah sabut kelapa yang
digunakan dan simulasi proses hujan ke atas cerun tanah untuk menganalisa hakisan
cerun. Bahagian ujikaji untuk bahan yang digunakan merangkumi Kejuruteraan
Mekanik Tanah dan Kejuruteraan Struktur Ringan. Kejuruteraan Mekanik Tanah
membantu ujikaji mi dengan usaha menganalisa Pengelasan Tanah, Had Atterberg,
Graviti Tentu, Kekuatan Ricih, Proktor Piawai and ujikaji Ricih Terus. Sebaliknya,
Kejuruteraan Structur Ringan menumpukan kepada ujikaji Kekuatan Tegangan bagi
bahan karpet sabut kelapa yang digunakan. Secara amnya, ujikaji utama adalah
simulasi hujan ke atas cerun tanah. Sampel tanah yang diambil dari kawasan
pembinaan di Bukit Gambang, Pahang dibahagikan kepada empat kes.
Pembolehubah yang dimanipulasikan adalah darjah kecerunan, jenis tumbuhan dan
keadaan cerun itu. Darjah kecerunan yang dipilih adalah 0°, 100, 20°, 30°, 400 dan
50°. Tumbuhan yang ditanam merujuk kepada rumput yang biasa ditanam di
kawasan cerun iaitu Signal Grass dan Japanese Millet. Keadaan cerun telah
dibahagikan kepada dua iaitu kes tanah kosong yang dikawal dan kes cerun tanah
Yang dilindungi. Pembolehubah utama adalah aplikasi oleh karpet sabut kelapa
sebagai pelindung cerun dibuktikan berkesan. Dengan membandingkan cerun kosong
Yang dikawal dengan cerun yang dilindungi, keputusan ujikaji menunjukkan cerun
Yang dilindungi mengurangkan hakisan tanalmya melalui ujikaji Sisa Pepejal
Terampai yang telah dijalankan. Cerun yang kosong mengumpul 0.014345 g/L sisa
pepejal terampai sementana cerun yang dilindungi menggunakan karpet sabut kelapa
mengumpul hanya 0.001368 gIL. Perbezaannya adalah 0.012977 g/L yang
membuictikan karpet sabut kelapa lebih berkesan dalam mengawal hakisan cerun
yang ditanam dengan rumput Signal Grass dimana daunnya yang lebih panjang dan
akar serabutnya yang kuat bagi meningkatkan mod kekuatan cerun.
TABLE OF CONTENT
CHAPTER ITEM PAGE
TITLE
DECLARATION
DEDICATION iv
ACKNOWLEDGEMENT v
ABSTRACT vi
ABSTRAK vii
TABLE OF CONTENT viii
LIST OF FIGURES xiv
LIST OF TABLES xviii
LIST OF SYMBOLS AND ABBREVIATIONS xix
LIST OF APPENDICES xxi
INTRODUCTION
1.1 Background of Research 1
1.2 Problem Statement 3
1.3 Objectives 5
1.4 Scope of Study 6
1.5 Significant of Study 7
vu'
ix
2 LITERATURE REVIEW
2.1 Introduction 9
2.2 Causes of Erosion 10
2.3 Effects of Erosion 11
2.4 Erosion Control 14
2.5 Erosion Control Blanket 16
2.6 Coir Fibre 20
2.6.1 Coir Fibre Processing 21
2.7 Laboratory Testing 23
2.7.1 Particle Size Distribution 23
2.7.2 Moisture Content 24
2.7.3 Atterberg Limit 25
2.7.4 Direct Shear 26
2.7.5 Triaxial Compression 26
2.8 Case Study 27
3 METHODOLOGY
3.1 Introduction 31
3.2 Preparation of Soil Sample and Coconut Coir 33
Blanket
3.2.1 Soil Sample 34
3.2.1.1 Particle Size Analysis 34
3.2.1.2 Specific Gravity 37
3.2.1.3 Atterberg Limits 38
a. Liquid Limit 39
b. Plastic Limit 40
C. Shrinkage Limit 41
3.2.1.4 Standard Proctor Test 43
3.2.1.5 Unconsolidated Undrained Triaxial 45
Test
x
3.2.2 Coconut Coir Blanket 47
3.2.2.1 Tension Test 47
3.2.2.2 Direct Shear Test 48
3.3 Preparation of Slope and Rainfall Simulation Model 48
3.4 Testing 48
3.5 Result Analysis and Discussion 50
4 RESULTS AND DISCUSSION
4.1 Introduction 51
4.2 Soil Analysis 52
4.2.1 Soil Sampling 52
4.2.2 Particle Sieve Distribution 52
4.2.3 Particle Size Analyzer 53
4.2.4 Specific Gravity 54
4.2.5 Atterberg Limit 55
4.2.6 Standard Proctor Test 57
4.2.7 Shear Strength 58
4.3 Coconut Coir Blanket Analysis 61
4.3.1 Tensile Strength 61
4.3.2 Direct Shear 63
4.4. Rainfall on Slope Model Simulation Testing 65
4.4.1 Control Sample with Signal Grass Vegetation 65
for Slope of 00
4.4.2 Control Sample with Signal Grass Vegetation 66
for Slope of 100
4.4.3 Control Sample with Signal Grass Vegetation 67
for Slope of 201
4.4.4 Control Sample with Signal Grass Vegetation 68
for Slope of 30°
4.4.5 Control Sample with Signal Grass Vegetation 69
for Slope of 40°
xi
4.4.6 Control Sample with Signal Grass Vegetation 70
for Slope of 50°
4.4.7 Control Sample with Japanese Millet 71
Vegetation for Slope of 00
4.4.8 Control Sample with Japanese Millet 72
Vegetation for Slope of 100
4.4.9 Control Sample with Japanese Millet 73
Vegetation for Slope of 200
4.4.10 Control Sample with Japanese Millet 74
Vegetation for Slope of 30°
4.4.11 Control Sample with Japanese Millet 75
Vegetation for Slope of 40°
4.4.12 Control Sample with Japanese Millet 76
Vegetation for Slope of 50°
4.4.13 Slope Model with Signal Grass Vegetation 77
and Coconut Coir Blanket for Slope of 00
4.4.14 Slope Model with Signal Grass Vegetation 78
and Coconut Coir Blanket for Slope of 100
4.4.15 Slope Model with Signal Grass Vegetation 79
and Coconut Coir Blanket for Slope of 20°
4.4.16 Slope Model with Signal Grass Vegetation 80
and Coconut Coir Blanket for Slope of 300
4.4.17 Slope Model with Signal Grass Vegetation 81
and Coconut Coir Blanket for Slope of 40°
4.4.18 Slope Model with Signal Grass Vegetation 82
and Coconut Coir Blanket for Slope of 50°
4.4.19 Slope Model with Japanese Millet 83
Vegetation and Coconut Coir Blanket for
Slope of 0°
xli
4.4.20 Slope Model with Japanese Millet 84
Vegetation and Coconut Coir Blanket for
Slope of 100
4.4.2 1 Slope Model with Japanese Millet 85
Vegetation and Coconut Coir Blanket for
Slope of 20°
4.4.22 Slope Model with Japanese Millet 86
Vegetation and Coconut Coir Blanket for
Slope of 30°
4.4.23 Slope Model with Japanese Millet 87
Vegetation and Coconut Coir Blanket for
Slope of 40°
4.4.24 Slope Model with Japanese Millet 90
Vegetation and Coconut Coir Blanket for
Slope of 500
4.4.25 Controlled Slope Model with Signal Grass 91
Vegetation against Controlled Slope Model
with Japanese Millet Vegetation
4.4.26 Protected Slope Model with Signal Grass 92
Vegetation against Protected Slope Model
with Japanese Millet Vegetation
4.4.27 Controlled Slope Model with Signal Grass 93
Vegetation against Protected Slope Model
with Signal Grass Vegetation
4.4.28 Controlled Slope Model with Japanese 94
Millet Vegetation against Protected Slope
Model with Japanese Millet Vegetation
4.5 Factors Affecting Results 96
4.5.1 Ambience Factor 96
4.5.2 Time Factor 96
4.5.3 Procedures Factor 96
XIII
5 CONCLUSION AND RECOMMENDATIONS
5.1 introduction 99
5.2 Conclusion 100
5.2 Recommendations 102
REFERENCES 104
APPENDIX A log
APPENDIX B 113
APPENDIX C 115
APPENDIX D 117
APPENDIX E 120
APPENDIX F 124
APPENDIX G 128
APPENDIX H 134
APPENDIX 1 143
LIST OF FIGURES
FIGURE NO. TITLE PAGE
2.1 Erosion control blankets for soil slope stabilization 19
2.2 Coconut layers 20
2.3 Original topography and design profiles 28
2.4 Front View of Failed Slope 28
2.5 Interpreted subsoil weathering profile 30
3.1 Flow chart for the sequences of methodology 32
3.2 Sieve set 35
3.3 Particle size analyzer 36
3.4 Density bottle and specific gravity apparatus 37
3.5 Atterberg limit stages diagram 42
3.6 Cone penetration apparatus 42
3.7 Standard proctor apparatus 44
3.8 Compression device 46
3.9 Coconut coir blanket 47
4.1 Particle size distribution curve 53
4.2 Particle size analyzer curve 54
4.3 Liquid limit determination 56
4.4 Graph of dry unit weight against moisture content 57 4.5 Triaxial compression test result for soil sample BHI 59
4.6 Triaxial compression test result for soil sample BHI2 60 4.7 Triaxial compression test result for soil sample B143 60 4.8 Coconut coir blanket was tested on tensile strength machine 61
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49 Tensile Strength graph 62
4.10 Soil sample with coconut coir blanket after shear test 63
4.11 Shear strength linear graph 64
4.12 Rate of Sedimentation for Control Sample with Signal 65
Grass Vegetation for Slope of 00
4.13 Rate of Sedimentation for Control Sample with Signal 66
Grass Vegetation for Slope of 101
4.14 Rate of Sedimentation for Control Sample with Signal 67
Grass Vegetation for Slope of 20°
4.15 Rate of Sedimentation for Control Sample with Signal 68
Grass Vegetation for Slope of 300
4.16 Rate of Sedimentation for Control Sample with Signal 69
Grass Vegetation for Slope of 40°
4.17 Rate of Sedimentation for Control Sample with Signal 70
Grass Vegetation for Slope of 50°
4.18 Rate of Sedimentation Graph for Control Sample with 71
Japanese Millet Vegetation for Slope of 0°
4.19 Rate of Sedimentation Graph for Control Sample with 72
Japanese Millet Vegetation for Slope of 100
4.20 Rate of Sedimentation Graph for Control Sample with 73
Japanese Millet Vegetation for Slope of 20°
4.21 Rate of Sedimentation Graph for Control Sample with 74
Japanese Millet Vegetation for Slope of 30°
4.22 Rate of Sedimentation Graph for Control Sample with 75
Japanese Millet Vegetation for Slope of 40°
4.23 Slope failure 76 4.24 Rate of Sedimentation Graph for Slope Model with Signal 77
Grass Vegetation and Coconut Coir Blanket for Slope of 00
4.25 Rate of Sedimentation Graph for Slope Model with Signal 78
Grass Vegetation and Coconut Coir Blanket for Slope of 100
4.26 Rate of Sedimentation Graph for Slope Model with Signal 79
Grass Vegetation and Coconut Coir Blanket for Slope of
200
4.27 Rate of Sedimentation Graph for Slope Model with Signal 80
Grass Vegetation and Coconut Coir Blanket for Slope of
300
4.28 Rate of Sedimentation Graph for Slope Model with Signal 81
Grass Vegetation and Coconut Coir Blanket for Slope of
40°
4.29 Rate of Sedimentation Graph for Slope Model with Signal 82
Grass Vegetation and Coconut Coir Blanket for Slope of
50°
4.30 Rate of Sedimentation Graph for Slope Model with 83
Japanese Millet Vegetation and Coconut Coir Blanket for
Slope of 0°
4.31 Rate of Sedimentation Graph for Slope Model with 84
Japanese Millet Vegetation and Coconut Coir Blanket for
Slope of 10°
4.32 Rate of Sedimentation Graph for Slope Model with 85
Japanese Millet Vegetation and Coconut Coir Blanket for
Slope of 20°
4.33 Rate of Sedimentation Graph for Slope Model with 86
Japanese Millet Vegetation and Coconut Coir Blanket for
Slope of 30°
4.34 Rate of Sedimentation Graph for Slope Model with 87
Japanese Millet Vegetation and Coconut Coir Blanket for
Slope of 40°
4.35 High amount of collection in TSS for every 10 minutes 88 4.36 The collection decreased for every 10 minutes 89 4.37 Rate of Sedimentation Graph for Slope Model with 90
Japanese Millet Vegetation and Coconut Coir Blanket for
xvi
xvii
Slope of 500
4.38 The comparison of Type of Grass in TSS for Controlled 91
Slope
439 The comparison of Type of Grass in TSS for Protected 92
Slope
4.40 The comparison of Type of Slope Protection using the same 93
Vegetation in TSS
4.41 The comparison of Type of Vegetation using the same 94
Slope Protection in TSS
5.1 Total Suspended Solids against Degree of Slope for all the 100
Slope Model
xv"
LIST OF TABLES
TABLE NO. TITLE PAGE
2.1 Physical properties of coir fibre 22
2.2 Fabric categories 22
2.3 Interpreted shear strength parameters 29
4.1 Data of specific gravity testing 55
4.2 Shear strength parameters 58
LIST OF SYMBOLS AND ABBREVIATIONS
A - Soil loss in tons/acre/year
R - Rain factor
K - Soil erodibility
LS - Topographic factor
C - Cover factor
P - Practice factor
c - Soil cohesion
E - Young's Modulus
v - Poisson's ratio
c' - Effective cohesion
(1)0 - Effective friction angle
LL - Liquid limit
PL - Plastic limit
SL - Shrinkage limit
Su - Undrained shear strength
AL - Length deformation
L0 - Initial length
- Strain
Gs - Specific gravity
7 - Dry unit weight
Cu - Shear strength
% - Percentage
Rm - Micrometer
- Degree
mic - Micron
xix
w% - Water content
M0 - Initial mass
G - Stress
MD - Machine direction
CD - Cross direction
lbs - Pounds
in - Inch
ac - Acre
tan - Tangent
f - Internal friction
kPa - Kilo Pascal
- Degree Celcius
ASTM - American Society for Testing and Materials
AASHTO - American Association of State Highway and Transportation
Officials
LIST OF APPENDICES
APPENDIX TITLE PAGE
A Soil Classification 108
B Specific Gravity 113
C Atterberg Limit 115
D Standard Proctor 117
E Shear Strength 120
F Tensile Test 124
G Direct Shear 128
H Total Suspended Solids 134
I Comparison of Results 143
wi
CHAPTER 1
INTRODUCTION
1.1 Background of Research
The surface of planet earth consists of mountains, flat grounds and water
filled sea. Each of these places needs to play roles in locating developments as the
world has limited ground areas for all mankind to live in. As these places are built up
to meet advanced civilization, the nature on their own is changing. The ground
surface of earth basically is having crust movement as the planet rotates on its axis.
The ambience which lives in the atmosphere too becomes the factors which lead to
the adjustment of nature physically. Thereafter, the geological cycle of earth may be
classified as disturbed.
Geologically, Malaysia is greatly disturbed by one of the major natural
disaster which is landslide. Landslide occurs mostly at the surface of mountainous
slopes that engaging danger to the residents. This alarming phenomenon can be
predicted by geologists but on many cases, it happens unexpectedly leaving the
residents in chaos. Lives are taken away and private properties are damaged which
concurrently affect the residents spiritually and the country's economic sustainment.
Many cases involved in the previous years and now seems like there is very minor
improvement has been implemented in slope reinforcement due to the numerous agendas.
2
In Peninsular Malaysia, the states located in the region of north, west and
south are having the gradual and evenly distributed rainfall season throughout the
month of April to May and September to December,. These States comprising of
Kedah, Perak, Selangor and Johor are slightly affected to the landslide occurrence as
a result from heavy rainfall. Based On climatology, these places basically have a dry
season starting from January. Due to this, they are least in the dilemma of landslide.
Out of jurisdiction, flooding may occur from time to time in the raining season.
Apparently, landslide which takes place due to human activities is normally
because of major construction on the existing site. Construction works such as the
cuts and excavations, removal of retaining wall or sheet piles and drawdown of water
bodies can easily take leads to slope failure. Certain construction uses high
technologies in order to cut hill slopes. Explosive are one of the major practice and
most expensive method which being carried out. Any misleading of the explosion
could simply produce unnecessary vibrations to the slope area.
Another example of human activities effects will be mining and quarrying
process for the purpose of construction materials trading and entrepreneurship.
Underprivileged monitoring of these activities might cause the area of site to be
exposed for landslide. Additionally, the construction for tunnel without proper soil
investigation and effective work may contribute in slope failure too. The hill that has
been drilled may be subjected to undesired settlement. More to this construction
industry, the building of a damn have a major risk in developing a landslide. Water
which run underneath the ground level and water pressure against the wall of the
dam may create a downfall.
Due to poor site investigation, a critical landslide may sweep off the entire
construction area. This may happen too to completed projects for example in
Malaysia itself, Jalan Semantan and Bukit Antarabangsa had landslide particularly in
2008 which killed a number of residents. Both projects are residential areas which
stand aside to a retaining wall that protects the slope from settling down. These two
cases were most likely the repetition of previous Highland Tower collapse back in 1985. It was a massive destruction as the whole tower fell to the side leaving few
3
survivors. It is learnt that, construction within slope areas is Still unsecured due to
natural effects not human errors.
Though high technology and recognized philosophies had been practiced into
the matter of slope protection, flaws seemed to rise and slowly engaging total
disaster. Effort on improving of the reinforcement to slope have to be revised
continuously as the analogy changes because of the transition made to the
environment naturally or man-made. As the deformation keeps going on, slope
erosion occurs because of the soil which eroded by water and wind factor. The slope
erosion is one major reason why landslide phenomenon exists. The landslide proved
that better technology is highly recommended for slope embankment and more
protection is seriously needful in order to have a promising Factor of Safety.
1.2 Problem Statement
Soil erosion is one factor why landslide occurs. The erosion involved the
human activities which development is engaged over the existing area. Due to
uncontrollable scenario, the soil surface is exposed to wind and water. As the soil is
being eroded, the changes made to the originality of the soil. Numerous elements are
taken into discussion for the basic properties of the soil are altered. The soil will be
losing nutrients and moisture, change in its structure and vegetation, and running
through a salirnzation. Hence, the behaviour of the soil is deformed form its original
state leaving it ineligible for many purposes.
Once an area of soil becomes degraded and eroded, the particular area shall
be put up for sale as it cannot be used for farmland anymore. The elements of the soil
which are altered made the soil become unsuitable for plantation to grow especially
at highland grounds. The maintenance fee may go higher as the soil has to be
modified in order to regain its natural behaviour. Unfortunately, the value of the soil
too will decrease therefore the people fanning it would be harvesting lesser or
4
reducing stock and eventually end up poorer. Regarding to this, it can be assumed
that erosion causes social, economic and political consequences to farm industries.
Whenever there is any presence of soil erosion, the existing ground is no
longer safe for construction unless remedial measures are implemented. In residential
divisions, high value residential nowadays favours the location of highland grounds
that overlook scenic environment. However, the safety measures promised are
vulnerable as any changes made by Mother Nature are unpredictable. Most eases that
relates to residential happens when the slopes holding the houses overturn and slide
resulting the houses to collapse. Lives were taken at stake. A home which is the
safest area for people to live in becomes dangerous unexpectedly.
Other than residential area, high rise building such as offices, academic
institutions, private organizations are too exposed to landslide caused by soil erosion.
These multi-storeys building faces higher risk of destruction if the foundation of the
structure is disrupted by the soil erosion scenario. The foundation which holds the
main structure of the building may fail and bring down the whole building. Many
cases have been highlighted in previous years as soil erosion keep on occurring after
intense improvement on the slope reinforcement.
Most importantly, roadways which have been the network to human
connections too seemed to be invaded by the severity of slope erosion. Highways
which cut through a hill will be facing the dilemma of soil erosion by both sides of
the excavated hill. The soil erosion which affects the roadway condition will be
hazardous to the road users. Rocks, dust, and soil particles deposited by water
certainly blocks the sight for the drivers. In a worsened scenario, the slope may fail
thoroughly and engaging into landslide. Vehicles on the road during that particular
moment may be having fatal accidents. If the destruction continues and the roadway
itself collapses into lower ground, the structure of the main road is impaired. Road
network is barred and transport connection is limited.
5
Seemingly, slope erosion by means of soil erosion leads to many difficulties
to the nature and its surroundings. Most of the factor is withstood by the human
activities themselves. The failure that damaging farmland, residential areas, high rise
buildings and roadways are the major places involved. Lives are taken and properties
are swept off each time a landslide occurs. As protecting slope is very important, this
study leads to one of the many preventive measures by reinforcing the slope literally.
1.3 Objectives
The objectives of the study are:
1. To determine the strength and durability of coconut coir matting.
2. To determine the effectiveness of the coir blanket in controlling slope
erosion.
6
1.4 Scope of Study
In the real world, the phenomenon of landslide cannot be forecasted of its
time of occurring and how bad it is going to be. Many factors affected the movement
of particles in the soil layers which were clearly subjective. The safety protections
suggested and applied too were occasionally vulnerable due to the changes made by
the Mother Nature. To gain such safety protections, many measures were taken into
consideration. Due to this, testing was carried out based on the objectives of this
study. The effectiveness of coconut coir in controlling slope erosion was determined
by several testing.
The related laboratory testing in this study covers in two specific engineering
division. It included both Geotechnical Engineering testing and Structural
Engineering testing. These two majors were mainly for the soil sample analysis and
the coconut coir properties assessment respectively. For Geotechnical Engineering
testing, there were Soil Classification, Atterberg Limit, Specific Gravity, Standard
Proctor, Shear Strength and Direct Shear tests. While Structural Engineering
highlighted on the coconut coir blanket properties assessment based on the Tensile
test.
In this study, a rainfall simulation model was built which contain a sloped
surface of soil sample. An artificial rainfall was spurred all over the soil sample area,
filtered into the layer of soil and the deposited amount of water was collected at the
edge of the model. The rainfall water supplied came from a direct water supply from
a water tab. The rainfall was designed to distribute the water uniformly over the soil
sample area. Sprinklers were installed as to contribute in the distribution of the
artificial rainfall thoroughly. Pressure gauge was connected to the main pipeline of
the water supply for monitoring the water pressure so to alter the intensity of the
rainfall as favoured in the testing. Each testing was gone for a one-hour raining
session. The data accumulated were averaged out over 60 minutes.
7
One controlled condition of slope was to be tested with bare surface. The
other condition was the sloped surfaces covered With coconut coir blanket. Both of
the conditions were varied by the vegetations used which were the Signal Grass and
Japanese Millet. The angles for the slope tested were 0 0, 100, 200, 30°, 40° and 500.
Therefore, the total number of cases was 144. The soil sample was collected from a
coflstrUCtlOfl site in Bukit Gambang, Pahang. Soil which was altered extremely is
most likely being disapproved as the originality of the soil content will be needed to
assure the properties of natural soil.
1.5 Significant of Study
The phenomenon of landslide can be factored by many aspects. There are
ground conditions, geomorphological processes, physical processes and man-made
processes. One of the main factors is erosion that belongs in the category of
geomorphological processes as it is a norm occurrence in Malaysia. Out of the many
factors, erosion is chosen to be discussed in this study in a way that excessive rainfall
season in Malaysia generates the soil particles movement settled in the slope area. It
is without a doubt that the well-known relationship between heavy rainfall and
landslides is the major contributions to slope erosion.
Remediation processes are highly important to slope failures. But practising
such operation is not recognizable as prevention save lives and the human properties
at the first place. Hence, remedial measures are the ones that need to be stressed out
In controlling slope erosion. Geotextile proves that it is effective to reduce erosion in
slopes. However, geosynthetic fibre is a new material which has better advantages
than the polymerized geotextile already has. Coconut coir is the base material
Selected to be used in this study as it certainly belongs in eco-friendly element. A
coconut coir based blanket is fully produced naturally. The raw material used is the
coconut coir alone without any additives.