Gulf of Jakarta is an area of active sedimentation. There exist a wide sediment deposition area on the north coast of Jakarta. Generally, these sediments have not been consolidated, so that the conditions in these area is an important factor to determining liquefaction in these area. Liquefaction may occur because of earthquake that cause loss of strength and stiffness in soils. Analysis of liquefaction potential based from SPT data taken at gulf of Jakarta, include susceptibility rate and the factors that triggering. Liquefaction analysis methods compared with each other to get the factor of safety against liquefaction according to the characteristics of the soil. Liquefaction analysis at surface using susceptibility rating factor (SRF). SRF method controled by factors: history, geology, composition, and groundwater. Each factors have parameters that determine the value of SRF.From the analysis, Gulf of Jakarta has susceptibility rating from liquefaction with SRF value 12 – 35. The value shows that Gulf of Jakarta dominated by area that have susceptibility rating from medium to high. High susceptibility rating from liquefaction concentrated at coast area.

1.
Kramer
,
Steve L.
.
2008
.
Evaluation of Liquefaction Hazards in Washington State
.
Washington State Departement of Transportation
.
2.
Idriss
I. M.
and
Boulanger
,
R.W.
.
2008
.
Soil Liquefaction During Earthquake
.
Oakland
:
Earthquake Engineer Research Institute (EERI
).
3.
Irsyam
,
M.
,
Sengara
W.
,
Hendriyawan
,
Asrurifak
,
M.
,
Prakoso
,
W. A.
,
Juniansyah
,
U.
,
Sumiartha
,
P.
, dan
Jayasaputra
,
U.
.
2010
.
Laporan Akhir Pendayagunaan Peta Mikrozonasi Gempa di DKI Jakarta
.
Kementrian Riset dan Teknologi
.
4.
Das
,
Braja M.
.
2007
.
Fundamentals of Geotechnical Engineering
3rd ed.
Madrid
:
Chris Carson
.
This content is only available via PDF.
You do not currently have access to this content.