SOIL SUCTION PROFILE DUE TO TREE INDUCED SUCTION FARAH FARHANA BINTI SULAIMAN
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1 SOIL SUCTION PROFILE DUE TO TREE INDUCED SUCTION FARAH FARHANA BINTI SULAIMAN A project report submitted in partial fulfilment of the requirements for the award of the degree of Master of Engineering (Civil - Geotechnic) Faculty of Civil Engineering Universiti Teknologi Malaysia AUGUST 2012
2 iii Special dedicated with love and affection To my beloved family members, Especially to my father and my mother, SULIMAN ABDULLAH & NORAINI CHATIB, & my entire friends. Who inspired me to do the best I can do and to share what we have learned together.
3 iv ACKNOWLEDGEMENT Alhamdulillah, I am very grateful to ALLAH all the Mighty; with the blessing to this project is completely and successfully done. First and foremost, I would like to express my sincere appreciation and deepest gratitude to Dr.Nazri Ali, my project supervisor who has given him technical expertise, undying patience, guidance and support throughout this project. A special thanks to all my friends who have been there for me, for giving me the support and comforts whenever is needed. Last but not least, my deepest gratitude to my family members, whose patience and encouragement played the greatest role in sustaining me through the challenge of completing this thesis.
4 v ABSTRACT Suction exerted by the roots water uptake of vegetation can have substantial effects on soil moisture, where it will influence the strength of the soil. However, rainfall pattern is one of the major factors that influence the changes of suction and lead to instability in unsaturated soils. This study discuss an exploration of soil suction is affected by water uptake by tree root at various condition from wet season (high rainfall) to dry season (prolonged no rainfall). The suction at study area are measured using Jet-fill tensiometers and Gypsum moisture block that placed at various depths and distances near vicinity of tree. A total of 18 Jet-fill tensiometers and Gypsum moisture blocks were installed in 6 stations, 3 stations at sloping ground and 3 stations at flat area. Each station consists of 3 Jet-fill tensiometers which at top, middle and bottom of the root zone to monitor the matric suction changes. The results of the soil suction obtained were used as an input data to develop soil suction contour using GID 7.2 software. From analysis of the pattern soil suction profile shown the suction rate is higher at near vicinity of tree and significant increase during dry period. However, a reduction in suction during high rainfall.the effect of tree induces suction will generate high suction in soil and can created dry condition to increase shear strength.
5 vi ABSTRAK Sedutan yang digunakan oleh penyerapan air akar tumbuh-tumbuhan boleh mempunyai kesan yang besar kepada kelembapan tanah, di mana ia akan mempengaruhi kekuatan tanah. Walau bagaimanapun, corak hujan adalah salah satu faktor utama yang mempengaruhi perubahan sedutan dan membawa kepada ketidakstabilan dalam tanah tak tepu. Kajian ini membincangkan eksplorasi sedutan tanah yang dipengaruhi oleh penyerapan air oleh akar pokok pada pelbagai keadaan dari musim basah (hujan yang tinggi) hingga ke musim kering (berpanjangan tiada air hujan). Sedutan di kawasan kajian diukur menggunakan Jet-fill tensiometer dan Gypsum moisture block yang diletakkan pada pelbagai kedalaman dan jarak berhampiran kawasan sekitar pokok. Sebanyak 18 Jet-fill tensiometer dan Gypsum moisture block telah dipasang di 6 stesen, 3 stesen di kawasan cerun dan 3 stesen di kawasan yang rata. Setiap stesen terdiri daripada 3 tensiometer iaitu di tengah-tengah atas, dan bawah zon akar untuk memantau perubahan sedutan matrik. Keputusan sedutan tanah yang diperolehi telah digunakan sebagai data input untuk membangunkan kontur sedutan tanah dengan menggunakan perisian GID 7.2. Daripada analisis profil corak sedutan tanah yang ditunjukkan kadar sedutan adalah lebih tinggi di kawasan sekitar berhampiran pokok dan peningkatan yang ketara semasa tempoh kering. Walau bagaimanapun, berlaku pengurangan dalam sedutan sewaktu hujan yang tinggi. Kesan sedutan pokok akan mendorong menjana sedutan yang tinggi dalam tanah dan akan mewujudkan keadaan kering untuk meningkatkan kekuatan ricih.
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