Ivan Taslim
Muhammadiyah University Of Gorontalo, Geography, Faculty Member
- Muhammadiyah University Of Gorontalo, Geografi-Fakultas Sains Dan Teknologi, Faculty MemberUniversitas Hasanudin, Geology, Alumnusadd
- Geology, Geophysics, Environmental Geology, Cave and Karst Studies, Karst Geomorphology, Geographic Information Systems (GIS), and 38 moreHydrology, Environmental Science, Remote Sensing, Earth Sciences, Environmental Sustainability, Geography, Climate Change, Environmental Engineering, Structural Geology, Social Sciences, Engineering, Culture, Biology, Philosophy, History, Computer Science, International Relations, Psychology, Karstology, Speleogenesis, Speleology, Karst hydrogeology, Speleothems, Geomorphology, Karst Environments, Karst and speleology, Karst and Caves, Fluvial Geomorphology, Hypogene Speleogenesis, Glacial Geomorphology, Morphotectonics, Disaster Management, Disaster risk management, Natural Disasters, Disaster Studies, Disaster risk reduction, Disaster Preparedness, and Crisis/disaster Managementedit
- I'm Lecturer at Geography Dept, Universitas Muhammadiyah Gorontaloedit
This study aims to identify the presence of karst groundwater reservoirs under the surface of the pious cave, Maros, South Sulawesi. This study will integrate with a mapping survey on a pious cave with the inversion of geoelectric... more
This study aims to identify the presence of karst groundwater reservoirs under the surface of the pious cave, Maros, South Sulawesi. This study will integrate with a mapping survey on a pious cave with the inversion of geoelectric measurements. the integration of these two methods can identify the presence of groundwater reservoirs of karst in the area so that it can be managed and utilized in the surrounding community.
Research Interests:
Abstrak: Pada wilayah rawan banjir, koordinasi antarpihak dalam kegiatan pengurangan risiko bencana sangat penting dilaksanakan. Hal ini dikarenakan bencana secara langsung akan berdampak pada gangguan kehidupan dan penghidupan... more
Abstrak: Pada wilayah rawan banjir, koordinasi antarpihak dalam kegiatan pengurangan risiko bencana sangat penting dilaksanakan. Hal ini dikarenakan bencana secara langsung akan berdampak pada gangguan kehidupan dan penghidupan masyarakat, juga menghambat proses pembangunan berkelanjutan. Penelitian ini bertujuan untuk menyusun skema koordinasi publik untuk kegiatan pengurangan risiko bencana (PRB) banjir berbasis sumber daya publik yang tersedia di Kabupaten Gorontalo. Sumber daya publik berasal dari instansi
pemerintah dan potensi masyarakat yang tersedia di Kabupaten Gorontalo dengan tugas masing-masing pada tahap sebelum, saat dan setelah bencana. Koordinasi publik diharapkan dapat mendukung pelaksanaan pembangunan berkelanjutan yang berbasis PRB di Kabupaten Gorontalo. Penyusunan skema koordinasi publik didahului penilaian bahaya banjir secara geospasial berdasarkan karakteristik Daerah Aliran Sungai (DAS) Limboto menggunakan perangkat Sistem Informasi Geografis (SIG). Hasil penilaian tersebut menjadi dasar
pelaksanaan penyusunan koordinasi publik untuk PRB. Kabupaten Gorontalo didominasi oleh satuan lahan pesisir yang berbatasan dengan Teluk Tomini, dataran hingga pegunungan. Curah hujan tinggi, tata guna lahan yang kritis serta permukiman yang berada di dataran rendah menyebabkan daerah penelitian termasuk pada zona risiko tinggi hingga sangat tinggi mengalami banjir. Pembangunan berkelanjutan dapat berjalan efektif apabila pelaksanaannya berbasiskan kebijakan PRB dengan koordinasi publik. Koordinasi publik dilakukan diantara instansi pemerintah dan masyarakat, yang bekerja sama sesuai peran dan tugas masing-masing pada tahap sebelum, saat hingga setelah bencana. Hasil penelitian menunjukkan bahwa dibutuhkan keterlibatan sektor yang lebih banyak pada tahap sebelum dan saat bencana. Hal ini mengindikasikan bahwa koordinasi publik sebelum terjadinya bencana merupakan kegiatan pencegahan dan pengurangan risiko yang harusnya lebih diutamakan dalam pelaksanaan pembangunan sebelum menghambat keberlanjutan pembangunan.
Kata Kunci: banjir; koordinasi publik; pembangunan berkelanjutan; pengurangan risiko; SIG
Abstract: In flood-prone areas, coordination between parties in disaster risk reduction (DRR) activities is very important. This is because the consequences of disasters will directly affect the disruption of people's lives and livelihoods, and also hinder the process of sustainable development. The study aims to develop a public coordinating scheme for disaster risk reduction (DRR) activities based on public resources in Gorontalo Regency. Public resources from government agencies and society are available in Gorontalo Regency with their respective tasks at the stages before, during and after the disaster. Public coordination is expected to support the implementation of DRR-based sustainable development in Gorontalo Regency. The preparation of public coordination scheme begins with geospatial flood hazard assessment based on the characteristics of the Limboto Watershed using a Geographic Information System (GIS) tool. The result provides a basis for the implementation of public coordination arrangements for DRR. Gorontalo Regency is dominated by a coastal land parcel adjacent to Tomini Bay, stretching from lowland plains to hilly mountains. High rainfall, critical land use and settlements in the lowlands have caused the study area categorized into high- to very high-risk zones of flooding. To ensure sustainable development runs effectively, its implementation must be based on DRR policy with public coordination. Public coordination is carried out between government agencies and society, who cooperate in compliance with their respective roles and tasks at the stage before, during and after the disaster. The results show that the involvement of more sectoral parties is needed at the stage before and during the disaster. This indicates that public coordination before the disaster performs risk prevention and reduction activity that should be prioritized in the implementation of development before inhibiting its sustainability.
Keywords: floods; GIS; public coordination; risk reduction; sustainable development
pemerintah dan potensi masyarakat yang tersedia di Kabupaten Gorontalo dengan tugas masing-masing pada tahap sebelum, saat dan setelah bencana. Koordinasi publik diharapkan dapat mendukung pelaksanaan pembangunan berkelanjutan yang berbasis PRB di Kabupaten Gorontalo. Penyusunan skema koordinasi publik didahului penilaian bahaya banjir secara geospasial berdasarkan karakteristik Daerah Aliran Sungai (DAS) Limboto menggunakan perangkat Sistem Informasi Geografis (SIG). Hasil penilaian tersebut menjadi dasar
pelaksanaan penyusunan koordinasi publik untuk PRB. Kabupaten Gorontalo didominasi oleh satuan lahan pesisir yang berbatasan dengan Teluk Tomini, dataran hingga pegunungan. Curah hujan tinggi, tata guna lahan yang kritis serta permukiman yang berada di dataran rendah menyebabkan daerah penelitian termasuk pada zona risiko tinggi hingga sangat tinggi mengalami banjir. Pembangunan berkelanjutan dapat berjalan efektif apabila pelaksanaannya berbasiskan kebijakan PRB dengan koordinasi publik. Koordinasi publik dilakukan diantara instansi pemerintah dan masyarakat, yang bekerja sama sesuai peran dan tugas masing-masing pada tahap sebelum, saat hingga setelah bencana. Hasil penelitian menunjukkan bahwa dibutuhkan keterlibatan sektor yang lebih banyak pada tahap sebelum dan saat bencana. Hal ini mengindikasikan bahwa koordinasi publik sebelum terjadinya bencana merupakan kegiatan pencegahan dan pengurangan risiko yang harusnya lebih diutamakan dalam pelaksanaan pembangunan sebelum menghambat keberlanjutan pembangunan.
Kata Kunci: banjir; koordinasi publik; pembangunan berkelanjutan; pengurangan risiko; SIG
Abstract: In flood-prone areas, coordination between parties in disaster risk reduction (DRR) activities is very important. This is because the consequences of disasters will directly affect the disruption of people's lives and livelihoods, and also hinder the process of sustainable development. The study aims to develop a public coordinating scheme for disaster risk reduction (DRR) activities based on public resources in Gorontalo Regency. Public resources from government agencies and society are available in Gorontalo Regency with their respective tasks at the stages before, during and after the disaster. Public coordination is expected to support the implementation of DRR-based sustainable development in Gorontalo Regency. The preparation of public coordination scheme begins with geospatial flood hazard assessment based on the characteristics of the Limboto Watershed using a Geographic Information System (GIS) tool. The result provides a basis for the implementation of public coordination arrangements for DRR. Gorontalo Regency is dominated by a coastal land parcel adjacent to Tomini Bay, stretching from lowland plains to hilly mountains. High rainfall, critical land use and settlements in the lowlands have caused the study area categorized into high- to very high-risk zones of flooding. To ensure sustainable development runs effectively, its implementation must be based on DRR policy with public coordination. Public coordination is carried out between government agencies and society, who cooperate in compliance with their respective roles and tasks at the stage before, during and after the disaster. The results show that the involvement of more sectoral parties is needed at the stage before and during the disaster. This indicates that public coordination before the disaster performs risk prevention and reduction activity that should be prioritized in the implementation of development before inhibiting its sustainability.
Keywords: floods; GIS; public coordination; risk reduction; sustainable development
Research Interests:
Solar energy is renewable and environment friendly and has been widely used in electricity generation and thermal energy through photovoltaic thermal (PVT) system. This system is beneficial in terms of maximum energy generation and cost... more
Solar energy is renewable and environment friendly and has been widely used in electricity generation and thermal energy through photovoltaic thermal (PVT) system. This system is beneficial in terms of maximum energy generation and cost of usage. The growing concern on energy sources and their usage has increased the significance and demand for PVT collectors. A PVT air collector consists of a PV panel and a thermal collector system. In PVT air collector, electricity and thermal energy are generated simultaneously. This review focuses on efficiency and energy modelling for PVT air collector with extended heat transfer area. Findings of this review indicated that PVT air collector with extended heat transfer area produced PVT efficiency higher than conventional PVT air collector. The thermal efficiency of PVT air collector for with and without extended heat transfer area are 21-83% and 12-70%, respectively, which the improvement of thermal efficiency is 15.7-42.8%. 1. INTRODUCTION Energy is a key requirement for undergoing and performing work. Around the 20th century, the demand and energy consumption have increased, and the primary energy source is fossil fuels. At present, the world energy consumption is expected to continuously grow. However, fossil fuel reserves are limited and may not meet the energy demand in the future. In addition, the release of green gas resulting from excessive fossil fuel combustion releases greenhouse gases and causes global climate change. Hence, fossil fuel is an unsustainable energy source. At present, using energy from renewable resources is a key factor in improving and adding benefits to the society because it is sustainable. Solar energy is radiation produced by nuclear fusion and is radiated from the sun in all directions. Solar energy beamed onto the Earth for even an hour is sufficient to produce the global energy need for an entire year. Many technologies are available for harnessing energy from the sun, and such energy can be used in two forms, namely, thermal and electrical energy. Photovoltaic thermal (PVT) technology utilizes radiation from solar energy to produce electrical and thermal energy. This technology consists of a PVT collector, which is a hybrid system that deploys solar PV and solar heater. The solar cell temperature increases when the PV panel is irradiated with solar energy. The higher the difference between the ambient temperature and the temperature of the cell is, the lower the electrical efficiency and electrical output of the PV panel will be. The electrical efficiency can be enhanced through heat extraction by passing a heat-extracting fluid (air or water) under the module. This integrated method, where electrical and thermal energy are generated simultaneously, is the basis of PVT collectors [1-11]. Aste et al. [12] validated a simulation model proposed by Aste et al. [13] based mainly on three balance
Research Interests:
The service system of clean water network in Pontianak provided by the state water company (PDAM Tirta Jaya) in average has high coverage across the city. Yet, some parts of the community are still left behind and require attention. This... more
The service system of clean water network in Pontianak provided
by the state water company (PDAM Tirta Jaya) in average has high
coverage across the city. Yet, some parts of the community are
still left behind and require attention. This study aims to reveal
which part of the community receive the least service, their current
coping mechanism. It also aims to identify the potential solutions
that PDAM or local community might be able to consider at an
affordable cost. We utilise various datasets related to water, PDAM
customer database, socio-economic background, and spatially related
information. Based on those, we identify that the majority of low-income
households in sub-district Pontianak Utara do not have formal
access to water provision by PDAM. Our Finding on the behavior
of non-piped water households confirms that these are the most
vulnerable community and we propose an alternative solution to
expand the water supply network by building a water bank using
rainwater and runoff especially accessible in the northern area of
Pontianak City
KEYWORDS
Water supply company, water access, clean water, water bank
by the state water company (PDAM Tirta Jaya) in average has high
coverage across the city. Yet, some parts of the community are
still left behind and require attention. This study aims to reveal
which part of the community receive the least service, their current
coping mechanism. It also aims to identify the potential solutions
that PDAM or local community might be able to consider at an
affordable cost. We utilise various datasets related to water, PDAM
customer database, socio-economic background, and spatially related
information. Based on those, we identify that the majority of low-income
households in sub-district Pontianak Utara do not have formal
access to water provision by PDAM. Our Finding on the behavior
of non-piped water households confirms that these are the most
vulnerable community and we propose an alternative solution to
expand the water supply network by building a water bank using
rainwater and runoff especially accessible in the northern area of
Pontianak City
KEYWORDS
Water supply company, water access, clean water, water bank
Research Interests:
Spatial and temporal data and information are very useful in reducing the number of dengue maladies in each region. Including in Kabupaten Gorontalo that does not yet have spatial and temporal information about DHF incidence. The purpose... more
Spatial and temporal data and information are very useful in reducing the number of dengue maladies in each region. Including in Kabupaten Gorontalo that does not yet have spatial and temporal information about DHF incidence. The purpose of this research is to analyze data and information of DHF incidence in Gorontalo Regency spasiotemporal. The study was conducted in Gorontalo. An ArcGIS 10.1 software was applied in this study to view descriptive epidemiology present ed in the form of maps, and the tables are then described in an overlap with DHF incidence data through geographic information systems (GIS). The results of this study indicate that in the last six years, from 2010 to 2016 Gorontalo District has DHF outbreak in Limboto sub-district, then in 2013-2016 there are 9 districts that have DHF outbreak of Telaga District, Telaga Jaya, Telaga Biru, West Limboto , Tilango, Tibawa, Bilato and Tabongo marked by an increase in cases every year in the Eastern Region of Gorontalo Regency precisely located in the area of Lake Limboto Area. if diverivikasi use Rainfall data, Dengue incidence in Gorontalo District in 2011 until 2015 is not affected by the amount of rainfall but will be different from the incidence of dengue in 2016 which is actually influenced by the amount of rainfall is high.
Data dan informasi spasial dan temporal sangat berguna dalam upaya mengurangi jumlah kejadain DBD di setiap daerah. Termasuk di Kabupaten Gorontalo yang belum memiliki informasi secara spasial dan temporal mengenai kejadian DBD. Tujuan dari penelitian ini adalah untuk menganalisis data dan informasi kejadian DBD di Kabupaten Gorontalo secara spasio-temporal. Penelitian ini dilakukan di Kabupaten Gorontalo.Sebuah perangkat lunak ArcGIS 10.1 diaplikasikan dalam penelitian ini untuk melihat secara epidemiologi deskriptif yang disajikan dalam bentuk peta, dan tabel yang kemudian digambarkan secara tumpang susun dengan data kejadian DBD melalui sistem informasi geografis (SIG). Hasil penelitian ini menunjukkan bahwa dalam enam tahun terakhir, sejak Tahun 2010 hingga Tahun 2016 Kabupaten Gorontalo mengalami KLB DBD di Kecamatan Limboto, kemudian pada tahun 2013-2016 terdapat 9 Kecamatan yang mengalami KLB DBD yakni Kecamatan Telaga, Telaga Jaya, Telaga Biru, Limboto Barat, Tilango, Tibawa, Bilato dan Tabongo yang ditandai oleh peningkatan kasus pada setiap tahun di Wilayah bagian Timur Kabupaten Gorontalo tepatnya berada di area Kawasan Danau Limboto. jika diverivikasi menggunakan data curah hujan, Kejadian DBD di Kabupaten Gorontalo pada tahun 2011 hingga tahun 2015 tidak dipengaruhi oleh jumlah curah hujan akan tetapi berbeda dengan kejadian DBD pada tahun 2016 yang justru dipengaruhi oleh jumlah curah hujan yang tinggi.
Data dan informasi spasial dan temporal sangat berguna dalam upaya mengurangi jumlah kejadain DBD di setiap daerah. Termasuk di Kabupaten Gorontalo yang belum memiliki informasi secara spasial dan temporal mengenai kejadian DBD. Tujuan dari penelitian ini adalah untuk menganalisis data dan informasi kejadian DBD di Kabupaten Gorontalo secara spasio-temporal. Penelitian ini dilakukan di Kabupaten Gorontalo.Sebuah perangkat lunak ArcGIS 10.1 diaplikasikan dalam penelitian ini untuk melihat secara epidemiologi deskriptif yang disajikan dalam bentuk peta, dan tabel yang kemudian digambarkan secara tumpang susun dengan data kejadian DBD melalui sistem informasi geografis (SIG). Hasil penelitian ini menunjukkan bahwa dalam enam tahun terakhir, sejak Tahun 2010 hingga Tahun 2016 Kabupaten Gorontalo mengalami KLB DBD di Kecamatan Limboto, kemudian pada tahun 2013-2016 terdapat 9 Kecamatan yang mengalami KLB DBD yakni Kecamatan Telaga, Telaga Jaya, Telaga Biru, Limboto Barat, Tilango, Tibawa, Bilato dan Tabongo yang ditandai oleh peningkatan kasus pada setiap tahun di Wilayah bagian Timur Kabupaten Gorontalo tepatnya berada di area Kawasan Danau Limboto. jika diverivikasi menggunakan data curah hujan, Kejadian DBD di Kabupaten Gorontalo pada tahun 2011 hingga tahun 2015 tidak dipengaruhi oleh jumlah curah hujan akan tetapi berbeda dengan kejadian DBD pada tahun 2016 yang justru dipengaruhi oleh jumlah curah hujan yang tinggi.
Research Interests:
This study aimed to identify potential subsurface water resources (underground river in Saleh Cave) on the Maros karst morphology. Identification of an underground river channel at Saleh Cave using resistivity measurements geoelectric... more
This study aimed to identify potential subsurface water resources (underground river in Saleh Cave) on the Maros karst morphology. Identification of an underground river channel at Saleh Cave using resistivity measurements geoelectric method Wenner-Schlumberger configuration compiled with Saleh Cave dimensional mapping data, as well as muscular and topographical measurements. Geoelectric measurement consists of 9 tracks, acquired 2D and 3D resistivity cross-section shows the flow of the cave identified through the high resistivity range ρ> 2000 Ωm. Goa Saleh has a long corridor about 200m, where an underground river channel identified at a depth of 84-110 meters above sea level trending N320oE or leads from the Southeast to the Northwest. This is consist with the results of measurements of the fracture pattern (strike / dip) in the study site showing the same pattern of dominant fractures trending with underground streams in Saleh Cave. Compilation method used in this research can identify potential water resources that located beneath the surface karst morphology.
Keywords: Karst Maros morphology, Underground river, Geoelectricity, Saleh Cave
Keywords: Karst Maros morphology, Underground river, Geoelectricity, Saleh Cave
Research Interests:
Indonesia's sustainable development system should be disaster-based mitigation. This research aims to analyze spatial geomorphology aspects, that identifies the potential and vulnerability of disaster that can be caused in Leato area... more
Indonesia's sustainable development system should be disaster-based mitigation. This research aims to analyze spatial geomorphology aspects, that identifies the potential and vulnerability of disaster that can be caused in Leato area (North Leato and southern Leato) at District Dumbo Raya of Gorontalo. Geomorphologically studied aspects using Geographic Information System (GIS) Global Mapper v12 and ArcGIS v10.3. Geomorphological analysis at the location of the research found that the area has coastal morphography up to the steep hills with an average height of 200-500 mdpl and morphometry of 8o to > 55o. Active morphostructure of tectonic activity which lasted relatively continuously since the Eocene - Early Miocene to Quarter, thus making it prone to high earthquake disaster that could become the trigger factor of a landslide. These influences resulted in the formation of geological structures including lithology breakthrough units Diorite Bone (Tmb) and Volcanic rocks Pinogu (TQpv) with a sturdy system that makes the weathering process run intensively on the body of the rock. Rock weathering conditions is a passive morphostructure of a landscape that can affect the cohesiveness of rocks so that some of them become rock fall type material avalanches. In terms of the morphology of the research area, the closure and use of land such as dryland and shrub farming to land and residential land transportation routes make the area not only vulnerable to landslides but also becomes vulnerable to a particularly adverse disaster on sustainable development in Gorontalo.
Keyword: geomorphology, gis, sustainable development, leato, rock fall landslides
Keyword: geomorphology, gis, sustainable development, leato, rock fall landslides
Research Interests:
ABSTRAK Penelitian ini bertujuan untuk menganalisis kesesuaian iklim pada daerah penelitian yaitu Kabupaten Bone Bolango di Provinsi Gorontalo dengan beberapa komoditi tanaman perkebunan. Data iklim yang digunakan dalam penelitian ini... more
ABSTRAK Penelitian ini bertujuan untuk menganalisis kesesuaian iklim pada daerah penelitian yaitu Kabupaten Bone Bolango di Provinsi Gorontalo dengan beberapa komoditi tanaman perkebunan. Data iklim yang digunakan dalam penelitian ini merupakan data sekunder yang bersumber dari TRMM, NASA dan BMKG yang diakses secara daring (online). Adapun data yang diakses diantaranya adalah data curah hujan, suhu (temperatur udara), kecepatan angin, dan kelembaban nisbi. Hasil pengolahan dari data-data tersebut selanjutnya dianalisis dan mendapatkan hasil rata-rata curah hujan tahunan (mm/tahun) di lokasi penelitian diketahui berkisar antara 1.301 mm/tahun hingga 1.758 mm/tahun. Suhu (temperatur udara o C) rata-rata sebesar 24,04 o C, kecepatan angin (knot) rata-rata adalah sebesar 2 knot atau 3,704 km/jam, dan kelembaban nisbi (%) rata-rata hingga 79,8%. Hasil tersebut disesuaikan (matching) dengan beberapa tanaman perkebunan perihal syarat tumbuhnya dengan menggunakan kriteria diantaranya S1: Paling sesuai; S2: Cukup sesuai; S3: Sesuai marginal dan N: Tidak sesuai. Diketahui bahwa beberapa tanaman perkebunan yang cocok dibudidayakan pada daerah penelitian
Research Interests:
Maros karst area known has a morphology similar to a tower form, valley (doline, uvala) along cave with an underground river. This research aims to analyze the hydrogeology behavior of Maros karst area so it will reveal the existence of... more
Maros karst area known has a morphology similar to a tower form, valley
(doline, uvala) along cave with an underground river. This research aims to analyze the hydrogeology behavior of Maros karst area so it will reveal the existence of water potential. The method used in this research is geology survey there is fracture system measure for getting joint dominant direction related to a cave system development and underground river, along with morphology identification to know the function as catchment area, aquifer, and infiltration zone.
Geoelectricity method used to presume limestone structure and cave system base on the value of resistivity. The result revealed that the morphological of the research location implied in karst hill with macro type (eksokarst) positive form that is tower karst and negative form that is ponor, also many speleothems (endokarst). Analysis of fissure system orientation found two (2) common direction at Saleh Cave that is northeast to southwest direction it’s about 65oNE–245oSW where the joint direction relatively having the same direction with dry channel and southeast to northwest direction it’s about 140oSE -320oNW where the underground cave system has the same way. Geoelectricity interpretation indicates the cave system and underground river reside in about 18-45 meter below surface.
Hydrogeology behavior of Maros karst at Saleh Cave very dependent by
morphology condition, also the development of fissure structure.
Keywords: karst, hydrogeology, morphology, geoelectric method.
Kawasan karst Kabupaten Maros dikenal memiliki morfologi dengan
bukit-bukit menyerupai bentuk menara, lekuk-lekuk lembah (dolina, uvala), serta gua-gua yang di bawahnya mengalir sungai bawah tanah. Penelitian ini bertujuan untuk mempelajari tentang perilaku hidrogeologi pada kawasan karst Maros sehingga dapat mengungkap keberadaan potensi sumberdaya air.
Metode yang digunakan dalam penelitian ini adalah survei geologi yaitu
pengukuran sistem rekahan untuk mendapatkan arah dominan kekar
hubungannya dengan perkembangan sistem perguaan dan sungai bawah tanah, serta identifikasi morfologi untuk melihat fungsinya sebagai daerah tangkapan hujan, akuifer dan sebagai daerah resapan air ke bawah permukaan. Pengukuran geolistrik digunakan untuk menduga struktur batugamping dan sistem perguaaan berdasarkan analisis nilai resistivitasnya.
Hasil penelitian menunjukkan bahwa lokasi penelitian masuk dalam
morfologi perbukitan karst yang memiliki morfologi karst makro (eksokarst) dengan bentuk positif yaitu menara karst dan bentuk negatif yaitu ponor, dan berbagai bentuk speleothem (endokarst). Analisis orientasi pola rekahan didapatkan dua (2) arah umum rekahan Gua Saleh yaitu berarah Timur laut- Barat daya sekitar 65oNE–245oSW dimana arah kekar relatif searah dengan lorong gua kering dan berarah Tenggara-Baratlaut sekitar 140oSE-320oNW dimana arah kekar relatif searah dengan lorong aliran sungai bawah tanah.
Interpretasi data pengukuran geolistrik menunjukkan sistem perguaan berada pada kedalaman sekitar 18-45 meter di bawah permukaan.
Perilaku hidrogeologi karst Maros di Gua Saleh sangat bergantung pada
keadaan morfologi, dan perkembangan struktur rekahan.
Kata kunci: karst, hidrogeologi, morfologi, metode geolistrik.
(doline, uvala) along cave with an underground river. This research aims to analyze the hydrogeology behavior of Maros karst area so it will reveal the existence of water potential. The method used in this research is geology survey there is fracture system measure for getting joint dominant direction related to a cave system development and underground river, along with morphology identification to know the function as catchment area, aquifer, and infiltration zone.
Geoelectricity method used to presume limestone structure and cave system base on the value of resistivity. The result revealed that the morphological of the research location implied in karst hill with macro type (eksokarst) positive form that is tower karst and negative form that is ponor, also many speleothems (endokarst). Analysis of fissure system orientation found two (2) common direction at Saleh Cave that is northeast to southwest direction it’s about 65oNE–245oSW where the joint direction relatively having the same direction with dry channel and southeast to northwest direction it’s about 140oSE -320oNW where the underground cave system has the same way. Geoelectricity interpretation indicates the cave system and underground river reside in about 18-45 meter below surface.
Hydrogeology behavior of Maros karst at Saleh Cave very dependent by
morphology condition, also the development of fissure structure.
Keywords: karst, hydrogeology, morphology, geoelectric method.
Kawasan karst Kabupaten Maros dikenal memiliki morfologi dengan
bukit-bukit menyerupai bentuk menara, lekuk-lekuk lembah (dolina, uvala), serta gua-gua yang di bawahnya mengalir sungai bawah tanah. Penelitian ini bertujuan untuk mempelajari tentang perilaku hidrogeologi pada kawasan karst Maros sehingga dapat mengungkap keberadaan potensi sumberdaya air.
Metode yang digunakan dalam penelitian ini adalah survei geologi yaitu
pengukuran sistem rekahan untuk mendapatkan arah dominan kekar
hubungannya dengan perkembangan sistem perguaan dan sungai bawah tanah, serta identifikasi morfologi untuk melihat fungsinya sebagai daerah tangkapan hujan, akuifer dan sebagai daerah resapan air ke bawah permukaan. Pengukuran geolistrik digunakan untuk menduga struktur batugamping dan sistem perguaaan berdasarkan analisis nilai resistivitasnya.
Hasil penelitian menunjukkan bahwa lokasi penelitian masuk dalam
morfologi perbukitan karst yang memiliki morfologi karst makro (eksokarst) dengan bentuk positif yaitu menara karst dan bentuk negatif yaitu ponor, dan berbagai bentuk speleothem (endokarst). Analisis orientasi pola rekahan didapatkan dua (2) arah umum rekahan Gua Saleh yaitu berarah Timur laut- Barat daya sekitar 65oNE–245oSW dimana arah kekar relatif searah dengan lorong gua kering dan berarah Tenggara-Baratlaut sekitar 140oSE-320oNW dimana arah kekar relatif searah dengan lorong aliran sungai bawah tanah.
Interpretasi data pengukuran geolistrik menunjukkan sistem perguaan berada pada kedalaman sekitar 18-45 meter di bawah permukaan.
Perilaku hidrogeologi karst Maros di Gua Saleh sangat bergantung pada
keadaan morfologi, dan perkembangan struktur rekahan.
Kata kunci: karst, hidrogeologi, morfologi, metode geolistrik.
Research Interests:
Maros karst area known have a morphology similar a tower form, valley (doline, uvala) along cave with underground river. This research aims to analyse the hydrogeology behavior of Maros karst area so it will reveal existence of water... more
Maros karst area known have a morphology similar a tower form, valley (doline, uvala) along cave with underground river. This research aims to analyse the hydrogeology behavior of Maros karst area so it will reveal existence of water potential. Method used in this research is geology survey there is fracture system measure for getting joint dominant direction related to cave system development and underground river, along with morphology identification to know the function as catchment area, aquifer and infiltration zone. Geoelectricity method used to presume limestone structure and cave system base on value of resistivity. The result reveal that the morphological of the research location implied in karst hill with macro type (eksokarst) positive form that is tower karst and negative form that is ponor, also many speleothem (endokarst). Analysis of fissure system orientation found two (2) common direction at Saleh Cave that is northeast to southwest direction it's about 65 o NE–245 o SW where the joint direction relatively having the same direction with dry channel and southeast to northwest direction it's about 140 o SE-320 o NW where the underground cave system have the same way. Geoelectricity interpretation indicate the cave system and underground river reside in about 18-45 meter below surface. Hydrogeology behavior of karst Maros at Saleh Cave very dependent by morphology condition, also development of fissure structure.
Research Interests:
This study aims to identify the presence of karst groundwater reservoirs under the surface of the pious cave, Maros, South Sulawesi. This study will integrate with a mapping survey on a pious cave with the inversion of geoelectric... more
This study aims to identify the presence of karst groundwater reservoirs under the surface of the pious cave, Maros, South Sulawesi. This study will integrate with a mapping survey on a pious cave with the inversion of geoelectric measurements. the integration of these two methods can identify the presence of groundwater reservoirs of karst in the area so that it can be managed and utilized in the surrounding community.