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SR.LDK-01 / JP.DM.04-27 I 2012
LAPORAN PENYELIDIKAN TAN AH Proyek : Gl. Kalisari. Lokasi : Jl. MulyosariNo.185, Surabaya. Re/asi : Lumintu Dinar Konsorsium, Tangerang.
'\o sfl-{ f-GrND ++ &noBC, TESTANA ENGINEERING, INC. Soil Testings & Research Administration
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SR.LDK-01 / JP.DM.04-27 t 2012
LAPORAN PENYELI DIKAN TAN AH Proyek : Gl. Kalisari. Lokasi : Jl. Mulyosari No.185, Surabaya. Re/asi : Lumintu Dinar Konsorsium, Tangerang.
DAFTAR ISI l. lNFORL,lASl PROYEK
II. TANAH BAWAH III. KAJIAN TEKNIS LAMPIRAN A.1. Location of Testing Points. A.2. DutchCone Penetrometer Test. A.3. Soil Frofile in Cross Section 1. A.4. Bearing Capacity of Pile Foundation 1 1 3
Surabaya, 26 April 2012. Testana Engineering,
,r.( Dimas Anggraito, S.T., M.T. Geotechnical Engineer Jl. opak 66, surabaya. Telp-/fax. (031) s6TB329 (Hunting) Etnait.
[email protected]
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/ ..t a' :, it
I. INFORMASI PROYEK Narna proyek Lo.kasi Relasi
Tujuan penyelidikan Pekeryaan di
lapangan : Level muka tanah
Posisititik-titik uji Gl. Kalisari; Penyelidikan tanah. Jl. Mulyosari No.185, Surabaya.
Lumintu Dinar Konsorsium, Tangerang. Untuk mengungkapkan kekuatan dan k ondisi, serta struktur lapisanz tanah bawah lokasi setempat guna menunjang pererrcanaan pondasi gardu induk. sehingga dapat direrrcanakan pilihan pondasi yang aman, efisien, serta dimungkinkan daiam pelaksanaannya sedapat rnungkin dengan jasa lokal yang tersedia (tujuan ekonornis). 5 titik sondir (CPT, Cone penetration lesf), dengan menggunakan penetrometer mekanis model GfuiF, Holland, kapasitas alat 2.S ton sesuai ASTM D-3441 Elevasi muka tanah titik - titik uji sondir tebih tinggi
r 0.8 m terhadap permukaan jalan ybs.
(t 0.00 m). Lihat Lampiran A1.
II. TANAIi BAWAH Hasil-hasil pengujian sondir diberikan dalam LampiranA.2- Untuk memperkirakan stratifikasi tanah dasar, dapat digunakan sistem klasifikasi tanah yang diusuikan oleh Schmertmann OyTS) berikut ini.
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e -E ro -a ,ffb &€iat( -kdes E. trq. ki *k k.nr. h
,n ,d d L Hr Rreio Gesekm.
qo Gambar 7. Sisfem klasffikasitanah yang diusutkan oleh schmeftmann, lg7g.
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ffi_"4r..*f-?tr-
Sistem klasifikasi yang diusulkan oleh Schmertmann yang telah disajikan pada Gambar 1 diatas, relatif mudah diterapkan, dan diperkirakan merupakan sistem klasifikasi tanah yang diyakini lebih mendekati dengan kondisi dilapangan, terutama pada jenis-jenis pengujian sondir. Untuk mendapatkan stratifikasi tanah diperlukan dua parameter, yakni perlawanan uju ng sondir, yang menggambarkan pola perlawanan lapisanJapisan tanah dasar (q.), dan rasio gesekkannya (Fn). Selanjutnya pada Tahel
/ berikut ini menyajikan kedalaman akhir pengujian sondir termasuk nilai q" dikedalaman akhir penetrasi sondir. ffo. Titik sondir
@okg/cm?)''
r 1. 2. 3. 4. 5. Kedal.aman akhir penetrasi sondir
n! i (m) Pe rl awa n a n uj
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17.8 21A i ,.+
Pengujian titik-titik sondir terhenti yang tersaji pada Tabel / menginformasikan bahwa penetrasi sondir terhenti pada kedalaman yang bervariasi dari
+ 17 hingga 25 m dengan nilai :e' t-::
perlawanan ujung konus dikedalaman akhir bervariasi mulai dari 75 hingga 210 kg/cm2. Lebih lanjut .!-..3 ?ii
pola perlawanan ujung sondir (q", kg/cmz ), dan rasio gesekkannya (Fn, %) yang disajikan vs kedalaman, diberikan berikut ini. q" ftglcm2) F* (9/o)
0 5{, 100 t50 m0 80 0
246810 I f
s-1 - -s4
t -s-I D -s3 a
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7 a ED i Ft-
-s4 -s6 .T tt
(t-
i gE 1l ..,: F bF
=>i a > Gambar 2. Profil perlawanan ujung sondir dan rasio geseknya.
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l€ I:::il1::,:i:.TL Il; lI
" Hasil-hasil pengujian sondir, berupa kompilasi data bacaan manometer di lapangan tersaji berupa grafik'? sondir, diberikan dalam Lampiran A.2. Berdasarkan hubungan antara q" (kglcm?1 dan rasio gesekkannya (%), mulai dari permukaan (dalam hal ini dibawah urugan sirtu) hingga kedalaman maks. + 17 m, stratifikasi lapisan tanah dasar tersusun oleh lanau berlempung, berkonsistensi sanga_t lunak hingga lunak, dengan dijumpai lensa kepasiran dengan ketebalan maks.
t 2 m. Lapisan tanah selanjutnya diperkirakan tersusun oleh pasir berlanau dengan variasi tingkat kepadatan mulai
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> beban keria, di bawah setiap kemungkinan beban yang dipikulnya, dan kestabllannva (a.1. terhadap pengaruh pengembangan, penurunan konsolidasi, geser, guling, dll) harus aman dan terjamin, deformasinya masih dalam batas-batas yang dapat diterima.
Penggunan pondasi dangkal untuk mendukung struktur utama kurang disarankan, mengingat kondisi lapisan tanah dasar yang tersusun oleh lanau berlempung berkonsistensi sangat lunak hingga lunak mencapai kedalaman
t 17 m, menyimpan potensi untuk mengalami pemampatan akibat isobar tegangan yang berasal dari sistem pembebanan gardu induk. Oleh karenanya diberikan alternatif pondasi tiang yang tertancap pada lapisan tanah pendukung @earing layer) yang stabil dan kokoh jauh dari permukaan untuk mengeliminir pemampatan t anah dasar.
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Kapasitas dukung pondasi tiang dihitung berdasarkan pendekatan yang disampaikan oleh Schmeftmaan-Nottingham (1978) menggunakan data sondir S-1. Mempertimbangkan terbatasnya data{ata penyelidikan tanah, dalam melakukan kajian kapasitas dukung pondasitiang menggunakan batasan2 sebagai input di dalam perhitungan, a.l. nilai perlawanan bikonus (q") maks.
+6 MPa dan perlawanan selimut konus (f,) maksimum sebesar 0.1 MPa (Hasil-hasilselengkapnya dapat dilihat pada lampiran A.3): Dab,Sondir. Kedalamgn: (m),, s-1
a25x25 18 20 20 27 Pracetak 18 25 o 30x3C 20 34 Bor
440 18 20 27 35
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untuk menlantisipasi pecah/ retaknya dindingi lantai bangunan yang berimpitan, Penyambunoan elemeq+lemen tiano dan cara penqelasannya harus dilakukan sebaik mungkin agar tiang tidak menyimpan potensi retak dan patah yang mengundang iegagalan pondasi, Disarankan untuk dilakukan trial pile. ouna memastikan tiang oracetak teroenetrasi sesuaidenqan kedalaman vano direncanakan,.
Tianq Bor bor di temoatl : Diameter dan panjang tiang bor dapat divariasikan sesuai beban kerja maupun kedalaman lapisanlapisan tanah keras (Tiang bor iniluga ditunjang dengan kemungkinan instalasi tiang yang
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A"""! 'b ?,ryue67-oh Ae'+on, UAIA,' l/\^Ut^b)iUA"^ t^^.L""1 **""A^fL^ W
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nnl-,"15.r,*^
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fy\u*"{ LP'\o^ !'*a^t-"o
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