l1 intro dan plate tectonics
TRANSCRIPT
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Geologi ialah suatu bidang tentang bumi
Kejuruteraan adalah suatu bidang berkaitandengan reka bentuk (design): selamat dan
ekonomi
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GEOLOGI KEJURUTERAN
AHLI GEOLOGI & JURUTERA
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Engineering geology is the application ofgeological data, techniques and principlesto the study of rock and soil surficial
materials, and ground water. This isessential for the proper location, planning,design, construction, operation and
maintenance of engineering structures.Engineering geology complementsenvironmental geology, orhydrogeology.
http://www.science.uwaterloo.ca/earth/geoscience/envi.htmlhttp://www.science.uwaterloo.ca/earth/geoscience/hydro.htmlhttp://www.science.uwaterloo.ca/earth/geoscience/hydro.htmlhttp://www.science.uwaterloo.ca/earth/geoscience/envi.html -
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Engineering geologists assess the natural foundations for buildings,bridges, dams, reservoirs, powerplants, pipelines, highways, canals,sewers, tunnels, mine adits and harbours. Design of thesestructures requires a thorough knowledge of the mechanicalproperties and stability of the rocks and sediments that will carrythese structures. Engineering geologists need to anticipate the
impact of subsidence, rains, floods, landslides, volcanoes andearthquakes on the foundations that bear these structures. Theyexplore the physical and chemical properties of structural materials(sand, gravel, cement, clay), and water in and around constructionsites. They advise on land use and on the planning and location ofnew urban and industrial development in cities. They examine andreport on waste disposal sites, and particularly those for the disposalof nuclear wastes.
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Engineering geologists must solve practical engineeringproblems. Basic university geology courses includephysical and historical geology, geomorphology, glacialgeology, mineralogy and petrology. Courses insedimentology, stratigraphy, structural geology, and
geophysics are also taken. Other topics include soil androck mechanics, hydrogeology, air photo interpretation,site investigation and urban geology. Canada is anorthern country with over half its land mass underlainby some type of perenially frozen ground so engineering
geologists are focussing increasing attention onpermafrost problems. Current global warming trends arelikely to intensify the melting of ice, causing sedimentstability problems for the foundations of structures
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Most engineering geologists work for consultingfirms in engineering geology, geotechnicalengineering or environmental assessment. Manyare employed in provincial and federal surveys.
Others are involved with large urban andindustrial development and construction firms.Still more are at universities or researchinstitutions. The petroleum industry also takes itsshare. The demand for engineering geologists is
high, and there are small numbers of graduates(about 100 each year) from Canadianuniversities
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Definition
Engineering geology is devoted to the
investigation, study and solution of the
engineering and enviromental problems
which may arise as the result of the
interaction between geology and the worksand activities of man as well as the
prediction and the development of measures
for prevention or remediation ofGeological hazards (IAEG Statutes, 1992)
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Engineering geology, as a science, is concernedwith the applications of the principles of
geology to civil (and to some extent, mining)
engineering, so that the engineer can take into
account these geological aspects which control
the economy, and safety of the structure which
is required to design and construct (Beavis,
1985)
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All civil engineering works are constructed
on, or in rock and soil masses. It is essential
therefore that the civil engineer be aware ofthe history, nature, and the properties of the
rocks and soils. Equally, it is essential for
the geologist, who is to work with theengineer, to have some knowledge of
engineering requirements.
sambung Beavis lagi
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Engineering geology embraces: the definition of the geomorphology, structure,
stratigraphy, lithology and ground water conditions ofgeological formations; the characterisation of the mineralogical, physico-
geomechanical, chemical and hydraulic properties of allearth materials involved in construction, resourcerecovery and environmental change;
the assessment of the mechanical and hydrologicalbehaviour of soil and rock masses;
the prediction of changes to the above properties withtime;
the determination of the parameters to be considered inthe stability analysis of engineering works and earthmasses;the improvement and maintenance of the environmentalcondition and properties of the terrain.
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Lihat kitar geologi(dari manusia dan geologi)
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science
To observe
To collect data
To plot data To evaluate and analyze data
To derive conclusion: hyphotheses or
theorizes, facts or illusion, truth or lies
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Jurutera merekabentuk untuk
Keselamatan
Keuntungan $$$$
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Sebuah madah
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Konsep2 asas geologi
1. Sistem solar dan kejadiannya
2. Bumi: struktur dalam, Tektonik Keping, proseskejadian di permukaan dan di dalam bumi
3. Batuan dan mineral, dan kejadiannya4. Batuan igneus dan kejadiannya, dan gunung
berapi
5. Luluhawa dan batuan mendak (stratigrafi)6. Batuan metamorfik
7. Masa geologi dan fosil
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1. Hidrologi: air tanah
2. Cangaan (struktur geologi)
3. Peta geologi, Peta Topografi, persekitaran geologi(enviromen kejadian dan pemendapan)
4. Sifat2 kejuruteraan tanah, batuan dan air5. Kajian tapak: geologi, geokimia, geofiziks
6. Kegunaan geologi dalam kejuruteraan: sumber alam(air, mineral, bijih, gas asli, petroleum, batuan, pasir,
tanahliat)7. Contoh2 kes penyelesaian masalah dalam
kejuruteraan: mekanik tanah dan batuan, tanah runtuh
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Tujuan kursus
Memperkenalkan konsep2 asas geologi
Menunjukkan bagaimana konsep2 asas geologidigunakan untuk menyelesaikan masalah dalam
bidang kejuruteraan (sama ada kejuruteraanawam, perlombongan, persekitaran, bahan, dll)
Hasilnyakita menjadi lebih peka dengan
sumber yang diberi oleh bumi (terhad) untukdimanafaat dengan baik oleh manusia sejagatuntuk mensejahtera kehidupan kita yang fanaini
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Sebuah madah
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Jurutera merekabentuk untuk
1 Keselamatan
2 Keuntungan $$$$
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Tujuan kursus
Memperkenalkan konsep2 asas geologi
Menunjukkan bagaimana konsep2 asas geologidigunakan untuk menyelesaikan masalah dalam
bidang kejuruteraan (sama ada kejuruteraanawam, perlombongan, persekitaran, bahan, dll)
Hasilnyakita menjadi lebih peka dengan
sumber yang diberi oleh bumi (terhad) untukdimanafaat dengan baik oleh manusia sejagatdemi kesejahteraan hidup kita yang fana in.
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Konsep2 asas geologi
Sistem solar dan kejadiannya
Batuan dan mineral, dan kejadiannya
Masa geologi
Proses kejadian permukaan bumi
Proses kejadian dalam bumi
Sumber alam (air, mineral, bijih, gas asli,
petrroleum, batuan, pasir, tanahliat) Persekitaran geologi
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Matlamat pembelajaran-pengajaran
Learn to know Learn to do
Learn to know and how to do
Matlamat ujian/peperiksaan?
??
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Somebody says
Knowledge is power!
What do you think?
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What do you think?
1
2
34
5
67
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Somebody also says
APPLIED knowledge is power
Do you agree?
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Earthquakes hits Hindu Kush,Afghanistan
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Anti-Atlas Mountains, Morocco
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Africa's Great Lakes
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Iceland
Iceland
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Snow in Northeast US
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Persian Gulf and Gulf of Oman
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Haro and Kas Hills, India
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Facts and figures
Bumi dilitupi 71% oleh air dan 29 % olehdaratan (landmass)
Didiami oleh manusia ..
Didiami oleh haiwan ..
Didiami oleh fauna dan flora ..
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seismology
P waves: surface waves,longitudinal/compressional/push-pull type
trasmitted parallel to the line of propagation;
moves faster than S waves at V = 6-8 km/s; firstto arrive
S waves: surface waves also, transverse/shear;particles moves sideways and wave motion is
transmitted in a shear fashion, transverse to theline of propagation; Vel = 3-4 km/s
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Cont-
S waves are not transmitted thru fluids;cause the earthquakes (principal shaking)
P waves moves thru solid and liquidphases
P & S waves: moves faster in dense rxthan in loose, low density materials: both
felt by people
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Facts and figures
Kerak
Mantel
Teras luar Teras dalam
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Pantulan gelombang
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isostacy
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Rakaman gelombang
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Kedudukan magma dalam bumi
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Pandangan dalam bumi
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Peringatan kpd tok guru
TEORI TEKTONIK KEPING (THEORIES OFPLATE TECTONICS) akan dibincangsemula sebagai konsep yg menyatukan
fahaman ahli sains tentang bumi dansistemnya (SOLAR?)
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Lecture tambahan
Apa yang berlaku di luar bumikehebatan
dan kepentingan astronomi
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Mt Everest
29 035 kaki
8.84 km
(1 kaki = 0.0003 km)
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Renungan kpd soalan
Adakah komposisi kimia kerak bumi,mantel bumi dan teras bumi mempunyaipersamaan dgn planet2 lain dan meteorit?
Kalau ada persamaan, apa rumusan yangboleh di buat?
Kalau berbeza, apa rumusan yang boleh
dibuat?
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persoalan
Conceptual learning vs realities
Mental learning vs physical learning
Context vs content
Relative truth vs absolute truth
Science vs religion
Syariat vs hakikat
PERSOALAN 2 YG LEBIH BESAR
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PERSOALAN 2 YG LEBIH BESARDAN HEBAT
Bagaimana alam semesta terjadi? Bagaimana permulaannya dan bagaimana
kesudahannya?
Adakah bumi sahaja yang boleh dihunioleh manusia?
Bagaimana dengan planet2 lain? Ada
kehidupan lain? Kalau ada kehidupan, apa maknanya?
Kalau tak ada kehidupan, apa maknanya?
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persoalannya
Adakah kita ada jawapannya?
Pastikah kita tentang jawapannya?
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In retropect
Kita dah banyak tahu tentang permukaan bumi,dalam perut bumi, di luar permukaan bumihingga ke angkasa lepas, ada apa untuk kita?
Sebagai manusia, itu soalan yg jauh yg sukarnak ditelusuri
Sebagai jurutera, kita hadkan kegiatan kita padapermukaan bumi, sedikit di dalam permukaan
bumi, dan sedikit di luar permukaan bumi=kita kaitkan dgn kerja kita (sudah cukup!!!)
KENAPA TERHAD DI
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KENAPA TERHAD DIPERMUKAAN?
KITA AKAN MEREKABENTUK APA JUASTRUKTUR DI PERMUKAAN BUMI, DANSEDIKIT DI DALAM PERMUKAAN BUMI
DAN SEDIKIT DI LUAR PERMUKAANBUMI YANG DI DALAM KAWALAN KITA,BUKAN DI LUAR KAWALAN KITA
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J is im (bum i =
1)
Jejari
(km)
ketumpata
n Kompos is i
Matahari 332000 695000 1.41 H2, He
Utarid 0.055 24440 5.44
Kejora 0.815 6050 5.27 CO2,N2, H2O, Ar, SO2
Bumi 1 6371 5.52 N2, O2, CO2, H2O
Marikh 0.11 3397 3.95 H2, He, CH4, NH3
Musytari 318 71600 1.31 H2, He, CH4, NH3
Zuhal 95.2 60000 0.7 H2, He, CH4, NH3
Uranus 14.6 25900 1.21 H2, He, CH4, NH3
Neptun 17.2 24750 1.66 H2, He, CH4, NH3
Pluto 0.0017 1300 1?
Ciri2 fizikal dan kimia sistem solar
Relative abundance of elements by wt
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Relative abundance of elements by wt
crust whole earth meteorites sun Moon
O Fe O H O
Si O Fe He SiAl Si Si O Mg
Fe Mg Mg C Fe
Ca Ni S N Ca
Na S Ni Si AlK Ca Ca Mg Ni
Mg Al Al Fe S
Ti Na Na Si Ti
H Cr Cr Al Cr
P Mn Mn Ca Na
Mn Co P Ni P
Fe P Co Na Mn
Ba K K Cr V
Kandungan unsur dalam kerak bumi
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g
SiO2 60.18
Al2O3 15.61
Fe2O3 3.14
FeO 3.88
MgO 3.56
CaO 5.17
Na2O 3.91K2O 3.19
TiO2 1.06
P2O5 0.3
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Look at lect31 pamela