Article Per Year (5 Year)
p-Index From 2021 - 2026
4.689
P-Index
This Author published in this journals
All Journal Tunas Geografi Paduraksa : Jurnal Teknik Sipil Universitas Warmadewa Jurnal Pengelolaan Sumberdaya Alam dan Lingkungan (Journal of Natural Resources and Environmental Management) AKSIOLOGIYA : Jurnal Pengabdian Kepada Masyarakat UNM Geographic Journal SELAPARANG: Jurnal Pengabdian Masyarakat Berkemajuan Jambura Geoscience Review Lamahu: Jurnal Pengabdian Masyarakat Terintegrasi Sustainability (STPP) Theory, Practice and Policy Geosfera: Jurnal Penelitian Geografi JAGE Panrita Inovasi: Jurnal Pengabdian Kepada Masyarakat Jurnal Riset dan Pengabdian Interdisipliner
Noviar Akase
Universitas Negeri Gorontalo
Agriculture, Biological Sciences & Forestry Humanities Astronomy Civil Engineering, Building, Construction & Architecture Computer Science & IT Control & Systems Engineering Earth & Planetary Sciences Economics, Econometrics & Finance Education Energy Engineering Environmental Science Health Professions Languange, Linguistic, Communication & Media Law, Crime, Criminology & Criminal Justice Medicine & Pharmacology Nursing Physics Public Health Social Sciences Other

Published : 39 Documents Claim Missing Document
Claim Missing Document
Check
Articles

Found 39 Documents
Search

 1   2   3   4 
Penentuan Tipe Akuifer Daerah Bulontala Kabupaten Bone Bolango Menggunakan Metode Geolistrik Dai, Elan; Zainuri, Ahmad; Akase, Noviar
Journal of Applied Geoscience and Engineering Vol 1, No 1 : Juni 2022
Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1231.753 KB) | DOI: 10.34312/jage.v1i1.15533

Abstract

Research area Geographically, the location is at 0áµ’31'0''N - 0áµ’31'30'' North Latitude 123áµ’8'0'' - 123áµ’8'30'' East Longitude with an area of ± 22.02 km. The research location is an andesite lava hill unit. because the type of rock found at that location is andesite igneous rock. The purpose of this study is to determine the type or type of aquifer. The method used is in the form of collecting surface and subsurface geological data. The method used is the geoelectric method with the Schlumberger configuration. The results of the research for geological mapping of the research location have morphology in the form of volcanic plains and hills with an altitude of 200 meters above sea level. The statigraphic sequence at the research site is sorted from easy to leader, old unit in the form of Andesite and easy unit in the form of alluvial. As for the geological structure that plays a role in the study, the dominant direction is from the north to the south.Groundwater at the research site follows the topography of the research location which flows from south to north where the water flows from upstream to downstream, from high to low elevation points. based on the results of geoelectric research and well water data collection that the aquifer at that location is shallow with alluvial material types, sand and andesite igneous rocks.The type of aquifer at the research site obtained from geoelectric research is a free aquifer type (not compressed) and only has 1 boundary layer, namely andesite igneous rock.
Karakteristik Batugamping Dan Porositas Terhadap Potensi Reservoir Air Tanah Di Desa Buhudaa, Kabupaten Gorontalo Sino, Widya Indriani H.; Zainuri, Ahmad; Akase, Noviar
Journal of Applied Geoscience and Engineering Vol 4, No 1 : Juni 2025
Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.37905/jage.v4i1.33755

Abstract

Reservoir rocks are characterized by their ability to allow water to infiltrate beneath the surface, enabling them to store and transmit fluids due to their permeability. Porosity refers to the presence of pores or void spaces within rocks, which determines their capacity to store fluids. Therefore, the porosity of a rock plays a significant role in the volume of liquid or gas it can contain. The study area is located within the Ql Formation, and no prior research has been conducted on limestone reservoir rocks in Buhudaa Village, Batudaa Pantai Subdistrict, Gorontalo Regency. The research covers an area of approximately 3.3 km², including the villages of Buhudaa, Bongo, and Lopo. This study aims to map the geological conditions of the Buhudaa area and analyze the lithological characteristics and quality of limestone as a groundwater reservoir. The methods employed include petrographic analysis and specific gravity testing. The results indicate that the geomorphological conditions of the area consist of structural and low-structural hills. The limestone was classified into three lithofacies: Mudstone, Wackestone, and Packstone. Geological structures were identified using linear lineament analysis, which distinguished ridges and valleys. The dominant orientation of these features trends northeast–southwest. Based on Koesoemadinata’s (1980) classification, the quality of limestone as a reservoir rock in the study area ranges from fair to very good.
Identifikasi Kualitas Batugamping Berdasarkan Analisis Geokimia dan Petrografi Daerah Pilolodaa Provinsi Gorontalo Paputungan, Ulfanna; Permana, Aang Panji; Akase, Noviar
Journal of Applied Geoscience and Engineering Vol 4, No 1 : Juni 2025
Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.37905/jage.v4i1.33607

Abstract

Gorontalo is one of the provinces with significant limestone potential, particularly in the industrial sector. This study aims to identify the quality of limestone found in the Pilolodaa area and its surroundings. The methods used in this research include petrography to determine the limestone facies and XRF analysis to identify the mineral composition of the rocks. The study area consists of lithologies such as floatstone limestone facies, carbonate sandstone, and alluvial units. The floatstone limestone has a CaO composition greater than 50% and MgO less than 2%, making it highly potential for industrial applications.
Peningkatan Kapasitas Masyarakat Dalam Mengurangi Risiko Bencana Di Desa Bandung Rejo Kabupaten Gorontalo Koem, Syahrizal; Akase, Noviar; Muis, Irwan
Aksiologiya: Jurnal Pengabdian Kepada Masyarakat Vol 3 No 2 (2019): Agustus
Publisher : Universitas Muhammadiyah Surabaya

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.30651/aks.v3i2.1815

Abstract

The community capacity building program in reducing disaster risk aims to realize the Bandung Rejo village as a disaster resilient village. Efforts made to achieve community capacity building include: (1) institutional aspects through the establishment of Disaster Risk Management forums (DRR) and Community Disaster Preparedness Teams (CDPT), (2) aspects of capacity building through dissemination and training in the preparation of disaster management plans and contingency plans , (3) aspects of the implementation of disaster management through a program to create a threat map and create disaster warning signs. The establishment of DRR and CDPT forums has a strategic role in minimizing disaster risk. The results achieved from the socialization and training were the availability of Bandung Rejo village disaster risk analysis document. The document can be a reference in making development policies in the village. Based on the results of the analysis conducted by the forum that Bandung Rejo village had a flood hazard level in the medium category. The results of identification and analysis obtained two flood-prone points that were able to reach agricultural land and facilities and infrastructure facilities. The implementation of community capacity building programs in Bandung Rejo village can provide stimulus to local governments and the public about the importance of disaster anticipation.
Pemetaan Geologi Dalam Mengungkap Potensi Sumber Daya Alam Desa Bonedaa, Suwawa Selatan, Gorontalo Pade, Dwi Ziana Jamila; Akase, Noviar; Hutagalung, Ronal; Dachi, Mirdayanti; Mokodompit, I Gede Wahyu; Tangkudung, Latifa; Ente, Amargio Saputro; Rahman, Adisty S.; Puhi, Rian; Yani, Lisra; Putra, Moh. Bahrul Zaman Momidu; Nurahman, Ikwan
-
Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.37905/jrpi.v2i3.33435

Abstract

The community in Bonedaa Village and its surroundings possesses untapped natural resource potential. This community service aims to enhance public understanding of local geological conditions and natural resources through participatory geological mapping. The methods applied include field education, group discussions, and training on rock and geological structure identification. The results show an increased awareness among residents regarding local rock types, construction material potential, and geological hazards such as landslides and erosion. Participatory mapping produced a simplified geological map useful for village-level planning and decision-making. This activity demonstrates that geological approaches can contribute directly to sustainable resource management and disaster risk reduction. The outcomes are significant in promoting community resilience and independence based on local potential.
Karakteristik Batuan Piroklastik Berdasarkan Analisis Petrografi Daerah Molingkapoto dan Sekitarnya Kabupaten Gorontalo Utara Provinsi Gorontalo Matoka, Putri Aprilia; Kasim, Muhammad; Akase, Noviar
Geosfera: Jurnal Penelitian Geografi Vol 4, No 2 (2025): Geosfera : Jurnal Penelitian Geografi
Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.37905/geojpg.v4i2.32267

Abstract

Daerah penelitian berlokasi di Molingkapoto dan sekitarnya, Kabupaten Gorontalo Utara, Provinsi Gorontalo. Secara fisiografi, daerah penelitian berada pada zona pegunugan utara di formasi Batuan Gunung Api Bilungala dan Breksi Wobudu. Secara stratigrafi, daerah penelitian terdiri dari batuan berumur tersier hingga kuarter. Tujuan dari penelitian ini adalah untuk mengetahui karakteristik batuan piroklastik daerah penelitian berdasarkan analisis petrografi, dengan menggunakan metode pemetaan lapangan yang merupakan bagian dari pengumpulan data untuk pengolahan data studio, dan metode analisis petrografi yang digunakan untuk pengolahan data laboratorium. Hasil penelitian menunjukkan bahwa daerah penelitian terdiri dari perbukitan aliran piroklastik dan dataran aluvial dengan litologi breksi piroklastik dan tuff yang dimana merupakan produk hasil vulkanisme. Analisis petrografi menunjukkan bahwa matriks dari batuan breksi piroklastik daerah penelitian berjenis tufa kristal  (PA 04) yaitu batuan yang didominasi pecahan -pecahan kristal dan tufa litik (PA 24) yang didominasi pecahan -pecahan atau fragmen batuan sementara batuan tufa berjenis litik tufa (PA 18) yaitu batuan yang didominasi pecahan -pecahan atau fragmen batuan.
Stratigrafi Daerah Sumalata Timur, Kabupaten Gorontalo Utara Rivai, Alya Sri Andini; Maryati, Sri; Akase, Noviar
-
Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.37905/jrpi.v2i3.33928

Abstract

The research area was located at coordinates 122°28’0’’- 122ᵒ36’0’ N - 0ᵒ52’0’’ - 1ᵒ2’0’ E with an area of 157 km2. Administratively, it is located in Sumalata Timur Subdistrict, North Gorontalo Regency, Gorontalo Province. The methods used in this research were surface geological surveys and laboratory analysis. Surface geological surveys included direct lithological observations at outcrops. Laboratory analysis included petrographic analysis using thin sections. The geologycal mapping aims to knowing the geological condition in East Sumalata. The lithology of the research area consists of 5 units, namely andesite unit, diorite unit, breccia unit, sandstone unit, and coastal sediment unit. The geomorphology of the research area is divided into 3 morphological units, namely the Volcanic Hills Unit, the Denudational Hills Unit, and the Marine Plains Unit.
Analysis of Microfaces and Depositional Environment of Limestone in North Isimu Area, Gorontaolo Regency Robot, Ladya Cheryl; Permana, Aang Panji; Akase, Noviar
Tunas Geografi Vol. 13 No. 1 (2024): JURNAL TUNAS GEOGRAFI
Publisher : Department of Geography Education, Faculty of Social Sciences, Universitas Negeri Medan

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.24114/tgeo.v13i1.41981

Abstract

The geological conditions in the northern part of Lake Limboto vary greatly from the constituent rocks to the working geological structures. Lithological variations consist of volcanic and plutonic rocks to limestone. The area where limestone is widely distributed is in the North Isimu Region, Gorontalo Regency. This research aims to analyze the geological conditions, microfacies and depositional environment of limestone in the North Isimu Region, Gorontalo Regency. The research methods used to achieve this goal consist of field surveys and petrographic laboratory analysis. Field surveys include taking rock samples, taking coordinate points, taking elevation, geomorphological observations, observing geological structures and taking field documentation. Meanwhile, petrographic analysis of rocks uses a polarizing microscope as a tool to follow up megascopic observations. Observation of rock incisions under a microscope using cross nicol and parallel nicol. Based on the results and discussion, it shows that the geomorphology of the research area includes structural hills with sub-parallel river flow patterns. The geological structure of the research area is a descending fault trending northwest-southeast. The research area is divided into four facies, namely foraminifera wackestone, crystalline limestone, foraminifera algae packstone and coralline floatstone. Standard microfacies (SMF) in the North Isimu Region consists of three SMF namely SMF-3, SMF-4 and SMF-5 with two limestone depositional environmental zones namely toe of slope (FZ-3) and slope (FZ-4). FZ-3 was deposited at the end of the foreslope zone and FZ-4 was deposited seaward of the foreslope from the edge of the carbonate debris platform.Keywords: Limestone; Microfacies; Depositional Environment; North Isimu
Analisis tipe gerakan tanah pada lereng Bendungan Bulango Ulu Kabupaten Bone Bolango menggunakan metode kinematika Moehammad Jasim Agi Saputra; Aang Panji Permana; Noviar Akase
PADURAKSA: Jurnal Teknik Sipil Universitas Warmadewa 244-249
Publisher : Program Studi Teknik Sipil, Fakultas Teknik dan Perencanaan, Universitas Warmadewa

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.22225/pd.12.2.7343.244-249

Abstract

The Bulango Ulu Dam is one of the strategic projects built in Tuloa Village, North Bulango District, Bone Bolango Regency, Gorontalo Province. In building a dam, geological analysis and slope stability are very important to avoid the risk of collapse or structural failure. This research aims to conduct geological analysis and slope stability at the Bulango Ulu Dam using kinematics methods. The kinematics method is used to determine the type of ground movement on the dam slope and identify the probability value of failure. Geological data related to lithology, petrography, geological structure and geomorphology are collected through direct observations and in the laboratory. Then, this data is used to determine geological conditions, geological structure and geomorphology which are then interpreted in relation to slope stability. The research results show that the geomorphological units are alluvial plains and low structural hills. The lithology that makes up the slopes of the Bulango Ulu Dam is composed of alluvial units and granodiorite units. The geological structure that develops is in the form of tensile joints in a general direction east-west (E-W) and cut by tension joints in a general direction north-south (N-S). The type and probability of ground movement that occurs based on segment, namely on segment A-B slopes in the form of Wedges (21.65%), segment B-C slopes in the form of Wedges (12.27%), segment E-F slopes in the form of Wedges (15.12%), and segment slopes G-H is a Wedge (21.8%). Based on the results of kinematic and boundary equilibrium analysis, the slopes on the Bulango Ulu dam are in the stable category. This research recommends that there is no need to make changes to the geometry of the dam slope because the slope is in a stable condition.
Co-Authors Abd Kadir Mubarak A Amin Abduh, Alan Gani Ahmad Iryanto Rompo Ahmad Zainuri Ahmad Zainuri Antoni, Isan Aris, Ayub Pratama Cindi Claudia Male Dachi, Mirdayanti Dai, Elan Daud Yusuf Deden, Mokoagow Deden Ente, Amargio Saputro Fandji Marfian Fitryane Lihawa Hidayansya, Taufik Hutagalung, Ronal Indriati Arifin, Yayu Intan Noviantari Manyoe Irene Ester Wowiling Irmawati Irmawati Irwan Muis K Badaun, Nur Azizah M. Iqbal Liayong Pratama Male, Cindi Claudia Mamonto, Fajri Kurniawan Matoka, Putri Aprilia Moehammad Jasim Agi Saputra Moh. Nazer Ismail Mokodompit, I Gede Wahyu Muh Kasim Muhammad Iqbal Asiki Muhammad Kasim Muis, Irwan Mutiara Nonsi Nonsi, Mutiara Nurahman, Ikwan Nurmuhniyanti M. Hubaib Pade, Dwi Ziana Jamila Pakaya, Siti Aqdawiya Paputungan, Ulfanna Permana, Aang Panji Ponto, Nadia Fransisca Puhi, Rian Putra, Moh. Bahrul Zaman Momidu Rachman, Arianzah Rizki Rahman, Adisty S. Rauf, Jayanti Rivai, Alya Sri Andini Rizky Hizrah Wumu Robot, Ladya Cheryl Ronal Hutagalung Rusdi, Infithar Hi Sino, Widya Indriani H. Siti Fatimah Sri Maryati Sri Maryati Suma, Muhamad Danial Sumarjis, Suly Ayu Supriadi Supriadi Syahrizal Koem Tangkudung, Latifa Umar Zulkarnain Bakkar Yani, Lisra Yayu Indriati Arifin