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IOP Conference Series: Earth and Environmental Science 2019年第1期273卷

作者： W L Nabigha B Setiawan D R Q Rabbani S M Alhabsyi SMP Negeri 1 Banda Aceh Jalan Prof. A. Majid Ibrahim 1 Banda Aceh 23116 INDONESIA Program Study of Geological Engineering Jalan Tgk. Syech Abdurrauf 7 Banda Aceh 23111 INDONESIA SMA Negeri 4 Banda Aceh Jalan T. Panglima Nyak Makam 19 Banda Aceh 23127 INDONESIA Dinas Pekerjaan Umum dan Penataan Ruang Kota Banda Aceh Jalan Prof. Ali Hasyimi Gp. Pango Raya Banda Aceh 23119 INDONESIA

A tsunami's tragedy happened at Banda Aceh 14 years ago, but most of the city dwellers don't grasp it clearly the hazardous of it. An un-adequate risk perception may be a contributing factor of this un-adequate preparedness. In general observation, we can make a hypothesis that many people in Banda Aceh are unprepared for the next strike. This study is to examine this hypothesis by studying the preparedness of students at SMP 1 Banda Aceh to the natural disaster of tsunami. An interview survey was carried out to randomly selected students to obtain data on their state of emergency preparedness and to ascertain their attitudes toward disaster. Thirty-one (31) students were interviewed. All the respondents know that the school is located at past tsunami's inundated area. About >75% respondents, who participated in the survey, have at least an emergency preparedness plan in place, and approximately 81% of these students believe that they know about contingency plan. However, based on the respondents' response to explain their action if any strong earthquakes strike, only 10% of the respondents have, truly, applied a contingency plan. It is recommended that a contingency plan campaign must be carried out in Banda Aceh.

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Regional tectonic and geochemical approach to distinguish bauxite characteristics in Pahang, Malaysia and West Kalimantan, Indonesia

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IOP Conference Series: Earth and Environmental Science 2018年第1期212卷

作者： R D Nugraheni D Sunjaya S Agustini Geological Engineering Study Program Faculty of Earth Technology and Energy Universitas Trisakti Jl. Kyai Tapa no.1 Grogol Jakarta Barat Indonesia PT Aneka Tambang Tbk Unit Geomin Jl. Letjen T.B. Simatupang no.1 Lingkar Selatan Tanjung Barat Jakarta Selatan

Indonesia and Malaysia are neighboring countries that situated in a tropical area and suitable for weathering, particularly favorable for lateritic deposit. One of laterite deposit is bauxite, where bauxite was formed as a chemical weathering product of metaluminous to peraluminous igneous rocks. The study area is located in the Kuantan area, Pahang State, Malaysia and West Kalimantan Province, Indonesia, which has contrasting tectonic origin and serve a different parent rock of bauxite. This study aims to distinguish the geochemical characteristics of bauxite in West Kalimantan against bauxite in Pahang Province. Method used in this study consists of pitting examination, where samples were collected from surface to maximum 10 m intervals and vertically logged. Samples were analyzed petrographically, XRD and XRF in order to observe the mineralogical composition and chemical compound. Result shows that magmatism in Pahang is dominated by basalt with oxide concentration of Al2O3, Fe2O3, SiO2 and TiO2 respectively ranges from 43.96 - 51.01%, 16.59 - 18.97%, 2.17 – 9.01% and 2.83 - 2.91%. In Indonesia, the parent rock of andesite and diorite (Al2O3 = 48.11 – 53.49%; Fe2O3 = 6.15 – 17.25%) shows higher amount of Al2O3 than that in granodiorit (Al2O3 = 30.10 – 48.68%). It can be inferred that andesite and diorite as bauxite's parent rock found in Kalimantan Barat generates abundant gibbsite and higher proportion of Al2O3 with lesser goethite and hematite (Fe2O3) relative to basalt as bauxite's parent rock in Pahang.

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Petrological and geochemical characteristics of pumiceous tephra deposit from Slamet stratovolcano, Central Java, Indonesia: Explosive period of the most differentiated magma of a basaltic stratovolcano

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AIP Conference Proceedings 2018年第1期1987卷

作者： A. Harijoko R. A. Noor S. A. Sari H. E. Wibowo N. I. Setiawan E. Handini W. Suryanto E. T. W. Mei 1Department of Geological Engineering Faculty of Engineering Universitas Gadjah Mada Yogyakarta Indonesia 2Volcanology Research Group LPPT Universitas Gadjah Mada Indonesia 3GAMA-InaTEK Universitas Gadjah Mada Indonesia 4Study Program of Geophysic Faculty of Mathematic and Natural Science Universitas Gadjah Mada Indonesia 5Faculty of Geography Universitas Gadjah Mada Indonesia

We reported detailed investigation of the pumiceous deposits reside in the western part of Slamet Volcano that are found as both primary and secondary product. Pyroclastic fall, flow and surge deposits represent those of the primary products, whereas lahar and fluvial deposits represent those of the secondary products. The tephra fall deposits are separated by pyroclastic flow and surge deposits as typical of sub-plinian to plinian eruption type. The secondary deposits of fluvial deposits occurred in between the primary deposits indicating repose time of the explosive events, whereas lahar deposits occurred as the youngest deposits concluding these pumiceous events. Petrographic observation show that pumice deposit is extremely vesicular with various bubble sizes, vitrophyric in texture, and contains subhedral phenocryst of plagioclase, orthopyroxene, clinopyroxene, opaque mineral and minor biotite. Chemical compositions of major and trace elements were obtained using ICP-MS-AES. SiO2 range from 58,7 to 63,9 wt.% and classified as andesite to dacite with LOI number range from -0,04 to 3,06. Ratios of incompatible elements (e.g. Ba/Zr, Rb/Zr, Zr/Nb, and Hf/Nb) consistently separate rocks of Old and Young Slamet. In these ratios, pumiceous samples are plotted within the range of Young Slamet implying for genetic relationship. These explosive events are “unique” considering typical recent basaltic activities of Slamet volcano and need to be carefully considered in the volcanic hazard mitigation.

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Laboratory scale of rainfall’s pattern and threshold in volcanic soil slope failure

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AIP Conference Proceedings 2016年第1期1730卷

作者： R. D. Kartiko I. A. Sadisun A. Tohari P. Sumintadiredja 1Geological Engineering Study Program Faculty of Earth Sciences and Technology Bandung Institute of Technology West Java Indonesia 2Research Center for Geotechnology Indonesian Institute of Sciences West Java Indonesia

Relationship between rainfall pattern, threshold and landslide process have widely developed. However, real-time observation in real landslide event is time consuming and has high degree of uncertainty. Therefore more analysis is usually developed in regional data scale with correlation between regional rainfall dataset and landslide inventory mapping. In this study, another approach is developed with a physical laboratory scale model. This research developed correlation between simulated rainfall pattern with mechanism and process of landslide. Rainfall with specific intensity and duration are given in residual volcanic soil in laboratory scale. Rainfall threshold observed between laboratory and regional model is highly correlated. There also occurred clear relationships between intensity, duration, antecedent rainfall, with rainfall’s initiation and morphology.

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A METHOD FOR ASSESSING RESIDUAL NAPL BASED ON ORGANIC-CHEMICAL CONCENTRATIONS IN SOIL SAMPLES

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GROUND WATER MONITORING AND REMEDIATION 1991年第2期11卷 128-136页

作者： FEENSTRA, S MACKAY, DM CHERRY, JA Stan Feenstra is a hydrogeochemist and president of Applied Groundwater Research Ltd. in Mississauga Ontario He received a B.Sc. in earth sciences and an M.Sc. in hydrogeology from the University of Waterloo in 1978 and 1980 respectively and was designated a Certified Ground Water Professional by AGWSE in 1989. Since 1980 he has been a ground water consultant with Golder Associates in Mississauga Ontario and Zenon Environmental in Burlington Ontario and founded Applied Groundwater Research Ltd. in 1987. Feenstra specializes in the hydrogeochemical evaluation of ground water contamination at waste disposal facilities and chemical spill sites. He is currently a Ph.D. candidate in hydrogeology and research associate in the Waterloo Centre for Ground Water Research at the University of Waterloo (Waterloo Ontario N2L 3G1) and is involved in research related to the behavior of dense organic solvents in ground water. Douglas M. Mackay is an adjunct professor at the Waterloo Centre for Groundwater Research at the University of Waterloo Waterloo Ontario (N2L3G1). Dr. Mackay received a B.S. in engineering and M.S. and Ph.D. in civil engineering from Stanford University in 1970 1973 and 1981 respectively. From 1986 to 1990 he was a faculty member of the Environmental Science and Engineering Program of the UCLA School of Public Health. His research focuses on field studies of transport and fate of organic chemicals in ground water various scale studies of decontamination of soil and ground water and ground water monitoring technologies. John A. Cherry is a professor at the Waterloo Centre for Groundwater Research at the University of Waterloo Waterloo Ontario (N2L 3G1). He received his B.S. in geological engineering from the University of Saskatchewan in 1962. He received his M.S. from the University of California at Berkeley in 1964 and his Ph.D. from the Department of Geology at the University of Illinois in 1966. His research interests include the field study and modeling of contaminants in ground wat

Ground water contamination by non-aqueous phase liquid (NAPL) chemicals is a serious concern at many industrial facilities and waste disposal sites. NAPL in the form of immobile residual contamination, or pools of mobile or potentially mobile NAPL, can represent continuing sources of ground water contamination. In order to develop rational and cost-effective plans for remediation of soil and ground water contamination at such sites, it is essential to determine if non-aqueous phase liquid (NAPL) chemicals are present in the subsurface and delineate the zones of NAPL contamination. The presence of NAPL pools may be evident as a floating or sinking phase in monitoring wells. The residual NAPL contamination may be identified in soil samples if residual contents are high and contaminated zones in the soil cores are thick. However, visual identification may not be effective if residual contents ar elow or if the NAPL residual is distributed heterogeneously in the samples. The chemical analysis of soil samples provides a measure of the total chemical concentration in the soil but cannot determine directly whether NAPL is present in the samples. Qualitatively, soil analyses that exhibit chemical concentrations in the percent range or > 10,000 mg/kg would generally be considered to indicate the presence of NAPL. However, the results of soil analyses are seldom used in a quantitative manner to assess the possible presence of residual NAPL contamination when chemical concentrations are lower and the presence of NAPL is not obvious. The assessment of the presence of NAPL in soil samples is possible using the results of chemical and physical analyses of the soil, and the fundamental principles of chemical partitioning in unsaturated or saturated soil. The method requires information on the soil of the type typically considered in ground water contamination studies and provides a simple tool for the investigators of chemical spill and waste disposal sites to assess whether soil

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Abstracts

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Environmental Management 1977年第1期1卷 67-96页

作者： Frankenfeld, John W. Schulz, Wolfgang McMurty, George J. Petersen, Gary W. May, G. A. Hering, F. S. Schwartz, J. I. Heywood, J. B. Chigier, N. A. Grohse, E. W. Walker, J. D. Colwell, R. R. Petrakis, L. Pergament, H. S. Thorpe, R. D. Schoepf, Richard W. Krzyczkowski, Roman Henneman, Suzanne S. Hudson, Charles L. Putnam, Evelyn S. Thiesen, Donna J. Parks, G. A. McCarty, Perry L. Leckie, J. O. Schrumpf, Barry J. Simonson, G. H. Paine, D. P. Lawrence, R. D. Pyott, W. T. Leh, M. Elders, W. Combs, J. Caplen, T. Harrison, F. L. Wong, K. M. Heft., R. E. Charnell, Robert L. Lehmann, Edward J. Mallon, Lawrence G. Hatfield, Cecile Adams, Gerald H. Johanning, James Talvitie, Antti Noll, Kenneth E. Miller, Terry Smiarowski, Joseph F. Willis, Cleve E. Foster, John H. Schlesinger, Benjamin Daetz, Douglas Lear, Donald U. Smith, Mona F. Hundemann, Audrey S. Crockett, Pernell W. Werner, Kirk G. Carroll, Thomas E. Maase, David L. Genco, Joseph E. Ifeadi, Christopher N. Lowman, F. G. Christensen, S. W. Van Winkle, W. Mattice, J. S. Harrison, Elizabeth A. Barker, James C. Chesness, Jerry L. Smith, Ralph E. Shaheeen, Donald G. Raney, R. Keith Borton, T. Wezernak, C. T. Raney, R. K. Sherwani, Jabbor K. Moreau, David H. Eisenberg, Norman A. Lynch, Cornelius J. Breeding, Roger J. Johnson, J. D. Foster, K. E. Mouat, D. A. Clark, R. Hyden, John William Owen, Wilfred Bayfield, Neil G. Barrow, Graham C. Stolz, Stephanie B. Wienckowski, Louis A. Brown, Betram S. Keyfitz, Nathan Wilson, W. L. Newman, Peter W. G. Bammi, Deepak Bammi, Dalip Goddard, James E. Chisholm, Tony Walsh, Cliff Brennan, Geoffrey Thompson, K. S. Richardson, R. Jensen, Clayton E. Brown, Dail W. Mirabito, John A. Cowing, Thomas G. Binghamton, Suny Siehl, George H. Albrecht, O. W. Alexander, Ariel Barde, Jean -Philippe Darby, William P. McMichael, Francis Clay Dunlap, Robert W. Muckleston, Keith W. Frankenhoff, Charles A. Giulini, Lorenzo T. Wyatt, T. Black, Peter E. Keating, William Thomas Leonard, M. E. Fisher, E. L. Brunelle, M. F. Dickinson, J. E. Pethig, Rudiger Clapham Exxon Research & Engineering Co. Linden Government Research Lab Coast Guard Washington D.C. Department of Transportation Washington D.C. Office For Remote Sensing of Earth Resources. NASA Earth Resources Survey Program Pennsylvania State University Washington D.C. Department of the Navy Washington D.C. Cambridge. Dept. of Mechanical Engineering Massachusetts Inst. of Technology USA Huntsville. School of Graduate Studies and Research Alabama Univ. USA Dept. of Microbiology. Office of Naval Research Maryland Univ. Arlington Research and Development Co. Pittsburgh AeroChem Research Labs. Inc. Princeton Dept. of the Interior Office of Library Services. Bibliographic Series (Final) Washington D.C. Interplan Corp. Santa Barbara Urban Mass Transportation Adm. Washington D.C. Naval Underwater Systems Center Newport Calif. Mercury Project. National Science Found Stanford Univ Washington D.C. Div. of Advanced Environmental Research & Tech. USA Corvallis. NASA Earth Resources Survey Program Oregon State Univ. Washington D.C. Riverside. Inst. of Geophysics and Planetary Physics National Science Foundation California Univ. Washington D.C. Livermore Lawrence Livermore Lab. California Univ. USA Atlantic Oceanographic and Meteorological Labs. National Oceanic and Atmospheric Administration Miami National Technical Information Service Springfield Miami Univ. Coral Gables School of Law National Oceanic and Atmospheric Administration Rockville National Academy of Sciences Office of Sea Grant Washington D. C. School of Law National Oceanic and Atmospheric Administration Office of Sea Grant. Rockville Norman. Dept. of Civil Engineering and Environmental Science. Urban Mass Transportation Administration Oklahoma Univ. Washington D. C. Knoxville.Dept. of Civil Engineering. Federal Highway Administration Tennessee Univ. Washington D. C. Amherst.Water Resources Research Center. Office of Water Research and Technology Massachusetts Univ. Washington D. C. Calif. Dept. of Industria

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