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PENGANTAR MEKANIKA TANAH SI - 2222
Dosen: Erza Rismantojo
Jadwal Perkuliahan
Kamis atau Jumat ? Ujian Tengah Semester 9 – 13 Maret 2015 Akhir Perkuliahan Jumat 30 April 2015 Ujian Akhir Semester 4 – 20 Mei 2015
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Asisten: Christian Tirtawardhana Auberta Philanta
REFERENSI
Das, B.M., 1995, “Principles of Geotechnical Engineering”, PWS Engineering, Boston, USA
Holtz, R. D. and Kovacs, W. D., 1981, “An
Introduction to Geotechnical Enginering” Prentice-Hall
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MATERI KULIAH (sebelum UTS)
Minggu ke 1 – 7: Proses pembentukan tanah Pengenalan Geologi Teknik Weight-volume relationships, plasticity, soil structure Klasifikasi tanah menurut AASHTO dan USCS
(ASTM) Pemadatan tanah dan CBR (California Bearing Ratio) Permeability dan Seepage
Minggu ke 8 (10 – 14 Maret 2014): UTS
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MATERI KULIAH (setelah UTS)
Minggu ke 9 – 15: Permeability dan Seepage Tegangan dalam tanah Compressibility dan Consolidation
Minggu ke 16 (5 – 20 Mei 2014): UAS
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SISTEM PENILAIAN
Tugas: 20% Ujian Tengah Semester: 40% Ujian Akhir Semester: 40% Tugas dikumpulkan 1 minggu setelah diberikan.
Tugas yang terlambat tidak akan dinilai. Tidak ada Tugas/Ujian tambahan untuk
perbaikan nilai.
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PENDAHULUAN
Mekanika Tanah adalah cabang dari ilmu mekanika yang berurusan dengan gaya-gaya yang bekerja pada masa tanah.
Rekayasa Geoteknik adalah salah satu spesialisasi rekayasa yang menggunakan prinsip-prinsip Mekanika Tanah.
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Low viscosity, low shear strength
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Kerak Bumi
Kerak Bumi
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Pergerakan Kerak Bumi berdasarkan data Satelit GPS (NASA) tanggal 17 April 2008
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Jenis-jenis Pergerakan di Perbatasan antar Kerak Bumi
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Mineral
A mineral is a naturally occurring solid chemical substance that is formed through geological processes and that has a characteristic chemical composition, a highly ordered atomic structure, and specific physical properties. By comparison, a rock is an aggregate of minerals and does not have a specific chemical composition.
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Mineral Class
Silicate Class : terdiri dari silicon dan oxygen. Umumnya rocks ≥ 95% silicates Contoh: feldspars, quartz, olivines, pyroxenes, amphiboles, garnets,
and micas Carbonate Class: mengandung anion (CO3)2− . Contoh: calcite (CaCO3), dolomite CaMg(CO3)2
Sulfate Class (sulfate anion SO42- , contoh: gypsum)
Halide Class (halide anions: F-, Cl-, Br-, I-. Contoh: NaCl, salts) Oxide Class (contoh: hematite (iron oxide)) Sulfide Class (contoh: pyrite (iron sulfide, FeS2)) Phosphate Class (PO4
3-) Element Class (contoh: silver, gold, copper) Organic Class
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BATUAN (ROCKS)
DEFINISI BATUAN (ROCK) menurut Rekayasa Sipil (Teknik Sipil): Material yang keras (hard) dan tahan lama (durable) Material yang tidak dapat digali kecuali dengan menggunakan bahan
peledak (blasting)
JENIS BATUAN BERDASARKAN ASAL USUL PEMBENTUKANNYA: Batuan Beku (Igneous Rocks) Batuan Sedimen (Sedimentary Rocks) Batuan Metamorf (Metamorphic Rocks)
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SIKLUS PEMBENTUKAN BATUAN
Metamorphism
Transportation, Erosion,
weathering
Compaction, cementation, crystallization
Sedimentary Rock
Sediment
Igneous Rock
MagmaMetamorf Rock
melting
Transportation, Erosion, Weathering
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SIKLUS PEMBENTUKAN BATUAN
BATUAN BEKU (Igneous Rocks): Batuan yang berasal dari magma cair, lahar yang
membeku karena penurunan suhu. Intrusive igneous rocks: diorite, gabbro, granite and
pegmatite that solidify below Earth's surface; Extrusive igneous rocks such as andesite, basalt,
obsidian, pumice, rhyolite and scoria that solidify on or above Earth's surface.
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CONTOH BATUAN BEKU Coarse-grained: Granite, Syenite, Gabbro,
Diorite
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Granite is a coarse-grained, light colored, intrusive igneous rock that contains mainly quartz and feldspar minerals.
CONTOH BATUAN BEKU Fine-grained: Rhyolite, Trachyte, Basalt,
Andesite
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Andesite is a fine-grained, extrusive igneous rock composed mainly of plagioclase with other minerals such as hornblende, pyroxene and biotite.
CONTOH BATUAN BEKU Obsidian (high-silica glass)
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Obsidian is a dark-colored volcanic glass that forms from the very rapid cooling of molten rock material. It cools so rapidly that crystals do not form.
CONTOH BATUAN BEKU
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Pumice is a light-colored vesicular igneous rock. It forms through very rapid solidification of a melt. The vesicular texture is a result of gas trapped in the melt at the time of solidification.
CONTOH BATUAN BEKU
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Welded Tuff is a rock that is composed of materials that were ejected from a volcano, fell to Earth, and then lithified into a rock. It is usually composed mainly of volcanic ash and sometimes contains larger size particles such as cinders (pyroclastic material similar to pumice).
Masalah-masalah yang berhubungan dengan penggunaan batuan beku
Beberapa jenis batuan beku dengan tekstur butiran halus (fine-grained) dan mengandung silika dapat bereaksi dengan kandungan alkali semen hasil reaksi alkali silika menyebabkan pertambahan volume sehingga merusak beton
Contoh: Andesite, Rhyolite, Volcanic Breccia, Obsidian, Pumice
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Alkali-Silica Reaction (ASR)
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Characteristic crack pattern associated with the alkali–silica reaction affecting a concrete step barrier on an US motorway (photograph courtesy of the Federal Highway Administration, US Department of Transportation).[1][2]
Ca(OH)2 + H4SiO4 → Ca2+ + H2SiO42− + 2 H2O → CaH2SiO4 · 2 H2O
Permasalahan Penggunaan Batuan Beku
Batuan beku berbutir kasar (coarse-grained) biasanya tidak baik untuk bahan konstruksi jalan, batu pelindung tanggul, karena tidak tahan terhadap abrasi
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Masalah-masalah yang berhubungan dengan penggunaan batuan beku
BATUAN SEDIMEN (SEDIMENTARY ROCKS)
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Sedimentary rocks are formed by the accumulation of sediments. Types of sedimentary rocks: 1) detrital sedimentary rocks such as breccia,
conglomerate, sandstone and shale, that are formed from solid particles derived from physical and chemical weathering of rock, transported, deposited, compacted, and cemented into rocks
2) chemical sedimentary rocks such as rock salt and some limestones, that form when dissolved materials precipitate from solution; and,
3) organic sedimentary rocks such as coal and some limestones which form from the accumulation of plant or animal debris.
BATUAN SEDIMEN (SEDIMENTARY ROCKS)
95% bagian terluar kerak bumi (16 km) adalah batuan beku dan batuan metamorf (5% adalah batuan sedimen)
75% batuan yang tersingkap di permukaan bumi adalah batuan sedimen
99% dari batuan sedimen adalah: shale (46%), sandstone (32%), dan limestone (22%)
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Detrital Sedimentary Rocks
Sedimen Ukuran Batuan Sedimen Gravel >2mm Conglomerate (partikel bulat)
Breccia (partikel angular) Sand 2 – 1/16 mm Sandstone
Silt 1/16 – 1/256 mm Siltstone (shale)
Clay < 1/256 mm Claystone (shale)
Silt and clay Shale
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Contoh Batuan Sedimen
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Breccia is a clastic sedimentary rock that is composed of large (over two millimeter diameter) angular fragments. The spaces between the large fragments can be filled with a matrix of smaller particles or a mineral cement which binds the rock together.
Contoh Batuan Sedimen
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Conglomerate is a clastic sedimentary rock that contains large (greater then two millimeters in diameter) rounded particles. The space between the pebbles is generally filled with smaller particles and/or a chemical cement that binds the rock together.
Contoh Batuan Sedimen
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Sandstone is a clastic sedimentary rock made up mainly of sand-size (1/16 to 2 millimeter diameter) weathering debris. Environments where large amounts of sand can accumulate include beaches, deserts, flood plains and deltas.
Contoh Batuan Sedimen
Contoh Batuan Sedimen
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Shale is a clastic sedimentary rock that is made up of clay-size (less then 1/256 millimeter in diameter) weathering debris. It typically breaks into thin flat pieces.
Contoh Batuan Sedimen
Contoh Batuan Sedimen
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Coal is an organic sedimentary rock that forms mainly from plant debris. The plant debris usually accumulates in a swamp environment. Coal is combustible and is often mined for use as a fuel.
Contoh Batuan Sedimen
CHEMICAL SEDIMENTARY ROCKS
Carbonates: Limestone (Mineral calcite: CaCO3) Dolomite [Mineral dolomite: CaMg(CO3)2]
Evaporites: Gypsum (CaSO4.2H2O) Rock Salt (NaCl)
Fossil Rocks: Fossiliferous Limestone (Calcite fosil berukuran
pasir atau lebih besar)
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Limestone is a rock that is composed primarily of calcium carbonate. It can form organically from the accumulation of shell, coral, algal and fecal debris. It can also form chemically from the precipitation of calcium carbonate from lake or ocean water. Limestone is used in many ways. Some of the most common are: production of cement, crushed stone and acid neutralization.
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Rock Salt is a chemical sedimentary rock that forms from the evaporation of ocean or saline lake waters. It is also known by the mineral name "halite". It is rarely found at Earth's surface, except in areas of very arid climate. It is often mined for use in the chemical industry or for use as a winter highway treatment. Some halite is processed for use as a seasoning for food.
Detroit Salt Mine
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PENGGUNAAN BATUAN SEDIMEN
Reaksi alkali-carbonate pada beton Portland cement (High alkali cement > 0.6% Na2O) menyebabkan kerusakan pada beton
CaMg(CO3)2 + 2 NaOH —> CaCO3 + Na2CO3 + Mg(OH)2
Limestone dan Dolomite adalah material
yang baik untuk konstruksi Siltstone, shale, quartz sandstone biasanya
tidak baik sebagai material konstruksi
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Batuan Metamorf
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Metamorphic rocks have been modified by heat, pressure and chemical process usually while buried deep below Earth's surface. Exposure to these extreme conditions has altered the mineralogy, texture and chemical composition of the rocks. There are two basic types of metamorphic rocks: 1) foliated metamorphic rocks such as gneiss, phyllite, schist and slate which have a layered or banded appearance that is produced by exposure to heat and directed pressure; and, 2) non-foliated metamorphic rocks such as marble and quartzite which do not have a layered or banded appearance. (http://geology.com/rocks/metamorphic-rocks.shtml)
Batuan Metamorf
Terbentuk akibat berubahnya komposisi kimiawi dan tekstur dari batuan, perubahan ini disebabkan oleh panas dan tekanan
Selama proses batuan asal tidak mencair Terjadi kristalisasi mineral and perubahan
struktur komposisi mineral yang membentuk mineral baru
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Gneiss is foliated metamorphic rock that has a banded appearance and is made up of granular mineral grains. It typically contains abundant quartz or feldspar minerals.
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Quartzite is a non-foliated metamorphic rock that is produced by the metamorphism of sandstone. It is composed primarily of quartz.
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Slate is a foliated metamorphic rock that is formed through the metamorphism of shale. It is a low grade metamorphic rock that splits into thin pieces.
JENIS BATUAN METAMORF
Shale Slate (fine grained, slaty cleavage) Phyllite: memiliki komposisi yang hampir
sama dengan Slate dengan lebih banyak kandungan mineral muscovite (phyllosilicate mineral of aluminium and potassium)
Schist (metamorf lanjutan dari Slate) Gneiss (berasal dari coarse-grained igneous
rock granite & gabbro) Marble (marmer)
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MASALAH-MASALAH DENGAN BATUAN METAMORF
Foliated metamorphic rocks menghasilkan butiran yang pipih dan lonjong sewaktu dipecah mudah pecah pada waktu konstruksi pemadatan hot mixed asphalt
Coarse-grained gneiss mudah terabrasi Marble cavities (lubang akibat terlarutkan
oleh aliran air) masalah kebocoran bendungan, pondasi bangunan
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PROSES PELAPUKAN
Proses Pelapukan secara Mekanis (mechanical weathering) Kembang susut batuan akibat perubahan suhu panas dingin Tekanan yang diakibatkan membekunya air di dalam
rongga/retakan di batuan
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PROSES PELAPUKAN
Kehilangan tekanan di permukaan
Batuan yang semula berukuran besar pecah menjadi butiran kecil. Tidak terjadi perubahan komposisi kimia
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PROSES PELAPUKAN
Proses Pelapukan secara Kimiawi (chemical weathering) Reaksi kimia mengubah mineral yang terkandung dalam
batuan asal menjadi mineral baru H2O + CO2 H2CO3 (Carbonic Acid) 2K(AlSi3O8) + 2H+ + H2O 2K++ 4SiO2 + Al2Si2O5(OH)4
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Orthoclase (salah satu mineral di dalam batuan beku seperti granite)
Silica Kaolinite (clay mineral)
Hasil pelapukan di tempat batuan asal disebut Tanah Residual
Glacial soils (glaciers) Alluvial soils (transportasi oleh air) Lacustrine soils (pengendapan di danau) Marine soils (pengendapan di laut) Aeolian soils (transportasi oleh angin) Colluvial soils (transportasi oleh gravitasi)
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Transportasi Hasil Pelapukan Batuan
Transportasi Hasil Pelapukan Batuan
Residual Soil
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a) top soil and colluvium
c) young residual soil
b) mature residual soil
d) weathered rock.
Alluvial soils (transportasi oleh air)
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ALLUVIAL soil is formed when a soil carrying stream gradually loses its carrying capacity with decreasing velocity. In slowing down, a river does not have sufficient power to keep the large particles of soil suspended; these particles settle to the riverbed. Further decrease in velocity causes smaller particles to settle. As the river becomes slow and sluggish (as in the lowlands where its gradient becomes small), it holds only the extremely fine particles in suspension. These particles are deposited, finally, at the mouth of the river, where they form DELTAS of fine-grained soil
Transportasi Hasil Pelapukan Batuan
Lacustrine soils (pengendapan di danau)
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Freshwater lake deposits are called LACUSTRINE soils. They are fine grained soils resulting from material brought into freshwater lakes by streams or rivers.
Transportasi Hasil Pelapukan Batuan
Aeolian soils (transportasi oleh angin)
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Transportasi Hasil Pelapukan Batuan
Colluvial soils (transportasi oleh gravitasi)
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COLLUVIAL soil consists of mixed deposits of rock fragments and soil materials accumulated at the bases of steep slopes through the influence of gravity.
Transportasi Hasil Pelapukan Batuan
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Clay Mineral
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Clay Mineral Aluminum silicates Terdiri dari 2 unit dasar:
Silica Tetrahedron Alumina Octahedron
Silica Tetrahedron Silica sheet
Clay Mineral
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Alumina octahedron Octahedral sheet (Gibbsite sheet) Disebut Brucite sheet jika atom Aluminum diganti Magnesium
Clay Mineral
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Silica-gibbsite sheet
Clay Mineral
Kaolinite Illite Montmorillonite Chlorite Halloysite Vermiculite Attapulgite
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Clay Mineral
Kaolinite Gabungan lembaran “silica-gibbsite sheet” Tebal lembaran = 7.2 Angstrom (1 Angstrom = 10-10 m) Berbentuk “platelets” berdimensi lebar atau
panjang 1000 – 20000 Angstrom, tebal 100 – 1000 Angstrom
Specific surface = 15 m2/g
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Kaolinite
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Kaolinite
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Kaolinite
CLAY MINERAL
ILLITE Gibbsite sheet + 2 Silica sheet (di atas dan bawah) Lembaran illite diikat oleh ion potassium (K) Ion K menetralkan muatan negatif yang
disebabkan oleh penggantian atom silicon dengan aluminum di “tetrahedral sheet”
Dimensi lateral 1000 – 5000 Angstrom, tebal 50 – 500 Angstrom
Specific surface = 80 m2/g
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ILLITE
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CLAY MINERAL
Montmorillonite Struktur hampir sama dengan Illite Atom aluminum di dalam octahedral sheet diganti
oleh magnesium dan iron (besi) Tidak ada ion potassium diantara lembaran Dapat menarik banyak molekul air ke dalam
ruangan yang di antara lembaran Dimensi lateral = 1000 – 5000 Angstrom Tebal = 10 – 50 Angstrom
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Montmorillonite
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Montmorillonite
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Clay Mineral
Permukaannya memiliki muatan negatif karena: Isomorphous substitution
Al Si (tetrahedral sheet) Mg Al (octahedral sheet)
Ketidaksempurnaan pada ujung-ujung/sisi-sisi lembaran clay yang putus
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Clay Mineral
Muatan negatif pada permukaan clay dinetralkan oleh kation (ion positif) yang ada disekitarnya Ca2+, Mg2+, Na+, K+
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Diffuse Double Layer
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Diffuse Double Layer
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