International Seminar 2013 Faculty of Mathematics and Sciences No 1 2 Name Adi Susilo,Ph.D Prof.Dra. Fatchiyah, M.Kes.,Ph.D Destination Seminar Title Schedule Istanbul, Turkey 2013 2nd International Conference on Traffic and Logistic Engineering (ICTLE 2013) Subsurface structure prediction of railroad tunnel in Malang, Indonesia based on dipole-dipole geoelectrical method 15-17 March 2013 Tokyo Japan The 8th Asia Pacific Conference on Clinical Nutrition New Approach of Nutritional Genomic of System Biology on Target Cells 9-12 June 2013 Abstract A study on a railway tunnel in the area of Karangkates, Sumberpucung Subdistrict, Malang District, Indonesia, had been undertaken. This study aims to detect cracks that may have been filled with water from rain that can be fatal to the power of the tunnel. This research was conducted with the active geophysical methods, namely resistivity geoelectrical dipole-dipole configuration (pseudodepth section). Interpretation of the data acquisitions was made after further processing. With the merge for each pseudodepth section, it will be obtained a physical description of the target (tunnel). The results showed that, rock solid structure (red) is located at the bottom of the tunnel (rail), while at the top and sides of the tunnel, which is lithologic structure, is relatively less dense (blue). It is estimated that the are cracks as well as the distribution of the lens on the ground subsidence above the tunnel. Another thing is the carrying capacity of the tunnel is dominated by the presence of cast concrete that is located on the side walls and top of the tunnel. But the cracks in the top and sides must be taken into account to avoid the danger of a more fatal in the future, because it was pretty crowded tunnel, as trains passed from Malang to Blitar cities, and in one of the top of the tunnel is the path Malang – Blitar buses. Index Terms— Railway Tunnel, geophysical resistivity, dipole-dipole, pseudodepth section, Malang, Indonesia. 3 4 5 Prof.Dr.drh. Aulianni'am, DESS Dr.Sc. Lukman Hakim, M.Sc Dr. Sukir Maryanto Tokyo Japan The 8th Asia Pacific Conference on Clinical Nutrition Anti diabetic activity of Temu Giring (Curcuma heyneana) extract in diabetic rats induced by multi low dose streptozotocin (MLDSTZ) 9-12 June 2013 Singapore The 15th Asian Chemical Congress The Inclusion of guest molecule inside ice and its influence to the host structure 19-23 August 2013 Kagoshima Japan IAVCEI Forecasting Volcanic Activity 2013 Observation of seismity and eruptive activity at Semeru Volcano, East Java, Indonesia 20-24 July 2013 A hybrid type of grand-canonical Monte Carlo simulation is carried out to investigate the accommodation of guest molecules inside ice and its influence to the host structure. The simulation shows that the presence of guest molecules inside the interstitial space of ice structures can enhance their stability, which in turn push the envelope of phase boundaries of those ices to higher temperature and pressure. The quantification of hydrate stability in term of chemical potential of water, calculated based on extension of van der Waals-Platteuw theory, lead to the global phase diagram. The influence of guest molecules inside ice structures also bring unique mechanical properties, such as positive gradient in compressibility with the increase of pressure applied to ice II filled with hydrogen. The effect of Lennard-Jones (LJ) parameter εwg, which mainly determines the strength of van der Waals interaction, in stabilizing the host structure is also clarified by varying its magnitude in a series of simulation. KEYWORDS: Water, Ice, Gas hydrate, Non-bonded interaction, Monte Carlo simulation Semeru volcano (3676m above sea level) is an andesitic stratovolcano located in East Java, Indonesia. Summit explosions have occurred continuously since 1967. During this period strombolian and vulcanian type explosions have occurred, producing explosion plumes rising 400–1000 m above the summit. We observed some of volcano earthquakes recorded at Semeru volcano in 2009. We analyzed the deep volcano earthquakes known as VA and also investigated the explosion earthquakes in relation with the different of it’s visual appearances. The hypocenters of VA with frequency ranged from 3-7Hz distributed into two clusters. First cluster is distributed at a depth of 3-4km and the second is about 6-8km which is associated with rising magma to the surface. The frequency of eruption earthquakes ranged from 0,78 to 4,09 Hz. Correlation between visual appearances and frequency are as follow; the eruption earthquakes that is manifested by visual grayish white eruption in January-February has 0,87 to 3,8 Hz; the eruption earthquakes that is manifested by the eruption of white visual show ,87-2,64 Hz. Whereas lava dome growth at the end of 2009, the eruption of earthquake frequency content of 1.06 to 2.73 Hz. Eruption earthquake hypocenter is located at a depth of less than 1km below the crater. Keywords: Semeru volcano, volcanic earthquakes, explosion earthquake, hypocenter 6 7 8 9 Akhmad Sabarudin, M.Sc, Dr.Sc Dr.Eng. Masruroh, M.Si Dr.Ir. Estri Laras Arumingtyas, M.Sc.St Dr.Eng. 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