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Adi Susilo
Jurusan Fisika Fakultas MIPA Universitas Brawijaya Malang
Environmental Science

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Microtremor and Geolistrik Resistivity Study Around the Trans Timor Primary Arterial Road for Disaster Mitigation Harti Umbu Mala; Adi Susilo; Sunaryo Sunaryo
Natural B, Journal of Health and Environmental Sciences Vol 3, No 1 (2015)
Publisher : Natural B, Journal of Health and Environmental Sciences

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (781.399 KB) | DOI: 10.21776/ub.natural-b.2015.003.01.4

Abstract

The research on microtremor and geoelectric resistivity around Trans Timor Primary Artery Road to disaster mitigation, has been done. The aims of this research were to obtain the Peak Ground Acceleration (PGA) value, the soil dominant frequency, seismic vulnerability index and to estimate the thickness of sediment layer. Microtremor data collection was done by using a three-component seismometer, DS-4A feedback short-period, at 52 points with 250 m interval. Dominant frequency and amplification factors were obtained by using curve analysis method, horizontal to vertical spectral ratio (HVSR). The PGA value was calculated using Kanai empirical equations, where the data of dominant period were obtained from the inversion of frequency values while the parameters of the earthquake were based on seismic events in the last 50 years, from 1963 to 2013 with magnitude of ≥ 3. Geoelectric measurements were conducted using a Resistivity-meter OYO, based on Wenner Schlumberger configuration and it was divided into two lines, with length of 400 m each.  From the results obtained by PGA value is ranged between 80 and 500 gal with level of risk moderate two to very large one. The distribution value of the soil dominant frequency was 0.62 Hz-18.27 Hz, while the distribution of the seismic vulnerability index ranged from 0.21 to 21.83. The type of soil is dominated by clay and alluvium as top soil and its thickness varies from 10 m to 50 m, strengthened by limestone as bedrock. 
Spread Indication of Underwater Surface Contaminants Using Magnetic Method (Case Study: TPA Supit Urang, Malang) Arif Rahman Hakim; Adi Susilo; Sukir Maryanto
Natural B, Journal of Health and Environmental Sciences Vol 2, No 3 (2014)
Publisher : Natural B, Journal of Health and Environmental Sciences

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (799.884 KB) | DOI: 10.21776/ub.natural-b.2014.002.03.13

Abstract

Research has been done on the spread of contaminants in the Supit Urang landfill, the city of Malang. The research was done in April 2013 - January 2014 in the area around Supit Urang landfill. The research purpose to determine the presence of contaminants in the Supit Urang landfill and distribution patterns. This research was begun by doing a data correction, consists of diurnal correction and IGRF correction so that got the total magnetic anomaly. Then, did reduction to the pole and upward continuation so that got the residual magnetic anomaly value ranging from -800 nT to 1100 nT. The results of data processing showed that contaminants in Supit Urang landfill accumulated on the inside of the landfill and then spreads in all directions with a depth of seepage reaches 25 meters. The spread of these contaminants are more inclined to the south because there is a river which is the discharge path of leachate from landfill to the river in the area. The results also showed the structure of the subsurface Supit Urang landfill dominated by sedimentary rocks such as sandstone, clay, tuff, tuff breccia and breccia. Based on the chemical test results, it showed contaminants in landfill is suspected to be leachate with susceptibility value between 0.0001 Wb/Am to 0.001 Wb/Am. Leachate from landfill contains some heavy metals with different concentrations, such as Cobalt (Co) 0.38 mg/L, Copper (Cu) 0.58 mg/L, Iron (Fe) 6.5 mg/L, Lead (Pb) 5.4 mg/L and Zinc (Zn) 4.8 mg/L.
Estimation of Seepage Zone at Bajulmati Dam, Banyuwangi Regency Based on Litology Analysis Using Magnetic Data Hanna Azizah Rahmah; Adi Susilo; Arief Rachmansyah
Natural B, Journal of Health and Environmental Sciences Vol 3, No 1 (2015)
Publisher : Natural B, Journal of Health and Environmental Sciences

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1209.079 KB) | DOI: 10.21776/ub.natural-b.2015.003.01.6

Abstract

A research regarding seeping in Bajulmati Dam of Banyuwangi Regency based on lithology analysis by geomagnetic data has been done to discover the location of zone with seeping potential. This research is done by analyzing lithology from magnetic data (primary data) that was acquired from the field that covers the area of Bajulmati Dam. The research began with the acquisition of magnetic data using PPM (proton procession Magnetometer). Acquired data is then corrected by diurnal and IGRF correction, reduction in to even surface, upward continuation as well as reduction to the pole. Local anomaly contour is acquired with the value ranging from -1000 nT up to 700 nT at loop 1 and ranging from -2800 nT up to 1600 nT at loop 2. Based on the result of data processing by magnetic method, the subsurface layers beneath the said dam consist of the layer of clay (tuff), sandstone, gravel, and volcanic lava. By analyzing the mentioned results, some cracks are located in AA’ line with the measurement point of 20 m and 90 m, and in the 120 m and 160 m, 80 m and 100 m measurement point of BB’, and CC’ line respectively. Those cracks can be expected to cause seepage in Bajulmati Dam. 
Co-Authors Arief Rachmansyah Arif Rahman Hakim Hanna Azizah Rahmah Harti Umbu Mala Sukir Maryanto Sunaryo Sunaryo