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Ahmad Zainuri

Fakultas Hukum, Universitas Kanjuruhan Malang

Author-ID : 427358

Religion Agriculture, Biological Sciences & Forestry Arts Humanities Automotive Engineering Biochemistry, Genetics & Molecular Biology Chemical Engineering, Chemistry & Bioengineering Chemistry Civil Engineering, Building, Construction & Architecture Computer Science & IT Control & Systems Engineering Decision Sciences, Operations Research & Management Earth & Planetary Sciences Economics, Econometrics & Finance Education Energy Engineering Environmental Science Health Professions Industrial & Manufacturing Engineering Languange, Linguistic, Communication & Media Law, Crime, Criminology & Criminal Justice Library & Information Science Materials Science & Nanotechnology Mathematics Mechanical Engineering Medicine & Pharmacology Nursing Physics Public Health Social Sciences Veterinary Other

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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

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.

Interpretasi Lapisan Bawah Permukaan Sebagai Perencanaan Tempat Penyimpanan Sampah Di Desa Talumelito, Kabupaten Gorontalo K Badaun, Nur Azizah; Zainuri, Ahmad; Akase, Noviar; Aris, Ayub Pratama
Journal of Applied Geoscience and Engineering Vol 1, No 2 : December 2022
Publisher : Universitas Negeri Gorontalo

The Talumelito waste storage area is located in Talumelito Village, Telaga Biru District, Gorontalo Regency which accommodates waste from various human activities. Organic and inorganic waste will become a breeding ground for diseases that are very dangerous for society and the environment. The purpose of this study was to determine the subsurface layer as an interpretation of the planning for the construction of a waste storage area and determine whether it is feasible or not. The resistivity geoelectric method of the Schlumberger configuration is one of the geophysical methods that is easy, inexpensive and efficient and does not damage the environment. The geoelectric method is a geophysical method used to identify the properties and physical conditions of the subsurface based on the resistivity values of the rock. This method utilizes variations in the resistivity values of the subsurface rocks to detect geological structures or subsurface rock formations. Based on an analysis of resistivity and geological electrical properties, the location of the planning for the construction of a waste storage area is at VES 2, VES 3, and VES 5 points. Where from the interpretation results the three VES points have bedrock rock layers with granite rock types. Meanwhile, at VES 1 and VES 4, there is a layer of sandstone under the top soil layer. VES 2, VES 3 and VES 5 points are suitable for waste storage because there are layers of waterproof rock. Whereas at VES 1 and VES 4 points it is not suitable for waste storage because the sandstone layer is a layer that has good permeability, so if there is liquid waste from garbage, the waste will contaminate groundwater.

Geologi Wilayah Tapaluluo dan Sekitarnya, Kabupaten Gorontalo Rasyid, Fajri Fitrah Fidianto A.; Zainuri, Ahmad; Kasim, Muhammad
Journal of Applied Geoscience and Engineering Vol 1, No 1 : Juni 2022
Publisher : Universitas Negeri Gorontalo

The research area is geographically located at coordinates 0041'30â€ â€“ 0045'00â€ North Latitude and 12300'30â€ â€“ 12303' 35â€ East Longitude with an area of ± 41 Km2. The method used in this research is scientific exploration by conducting a survey of surface geological mapping. It is carried out in the preparation of literature, tools and materials, the data collection stage is in the form of geomorphological data, stratigraphy, geological structure measurements and documentation. The data processing stage is in the form of laboratory analysis, namely conducting petrographic analysis and processing geological structure data in the form of joints and faults using the stereographic method. The geomorphology of the research area is divided into three geomorphological units, namely; lava flow ridge units, intrusion hills, and fault zone hill units. The study area is divided into three rock units informally in order from oldest to youngest, namely: andesite porphyry unit (early-middle Miocene), granodiorite unit (middle-late Miocene), and modified andesite porphyry unit (middle-late Miocene). The geological structure of the study area consists of joints, Tapaluluo Fault, and Botupololondalange Shear Fault. The geological potential of the research area is in the form of mineralization and rock mining.

Estimasi Potensi Cadangan Air Tanah Dengan Metode Persamaan Darcy di Desa Pilomonu, Gorontalo Sugianti, Komang; Zainuri, Ahmad; Hutagalung, Ronal
Journal of Applied Geoscience and Engineering Vol 1, No 1 : Juni 2022
Publisher : Universitas Negeri Gorontalo

This research aims to know the prediction of potential for groundwater reserves. The research method applies surface geological mapping and subsurface data collection with the 200-span Schlumberger configuration geoelectric method. The stratigraphy of the research area is sorted from old to young, the first is the granodiorite unit, the sandstone unit, and alluvial units are deposited inconsistently. The geological structure working in the research area has a dominant northwest-southeast direction. The direction of. groundwater flow follows the topography of the research area, whicb is flowing from the north to the south, where the elevation of the norlh js higher than the eJevation of the south. The aquifer characteristics in the research area can be divided into two based on the mterpretation of geoelectric inversion, such as shallow aquifer with material in the form of sand and deep aquifer with sand and gravel material. Prediction of the potential for groundwater reserves is obtained from the interpretation of geoelectric data and data from the calculation of the groundwater level in the research area by observing the. conditions around the research area So, it is obtained a prediction of potential for shallow groundwater reserves is 360.444 m3/day or equivalent to 360,444 liters/day, and the prediction of poteptial deep groundwater reserves is 66,520.476 m3/day or equivalent to 66:,520,476 liters/day.

Analisis Resiko Longsor Di Desa Garapia Menggunakan Electrical Resistivity Tomography (ERT) Untuk Identifikasi Kedalaman Bidang Gelincir Katili, Gita Triyana Risti; Arifin, Yayu Indriati; Zainuri, Ahmad
Journal of Applied Geoscience and Engineering Vol 3, No 1 : Juni 2024
Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.37905/jage.v3i1.26910

This study explores the geological conditions and the depth of landslide slip surfaces in Garapia Village, North Gorontalo Regency, using Electrical Resistivity Tomography (ERT). By analyzing stratigraphy and geoelectrical data, the research aims to provide a comprehensive understanding of subsurface structures and their implications for landslide risks. Stratigraphic analysis reveals two primary geological units: weathered basalt, characterized by its grayish-black color, and alluvial deposits, indicating ongoing sedimentation. Structural analysis shows a Northeast-Southwest alignment, reflecting tectonic influences that may impact slope stability. ERT measurements identify three subsurface layers with varying resistivities: soil (10.6 â€“ 783 Î©m), basalt (783 â€“ 41,867 Î©m), and andesite (41,867 â€“ 244,307 Î©m). A significant slip surface detected at depths of 9.85 to 18.7 meters shows low resistivity (4.75 â€“ 48.1 Î©m), suggesting clay that is prone to landslides. The study highlights ERT's effectiveness in accurately identifying slip surface depths, offering valuable insights for landslide risk assessment and mitigation. This approach provides enhanced precision compared to traditional methods, thus improving disaster planning and risk management.

Karakteristik Geologi Daerah Dambalo dan Sekitarnya Kabupaten Gorontalo Utara, Provinsi Gorontalo Ismail, Zenza Harnold; Permana, Aang Panji; Zainuri, Ahmad
Journal of Applied Geoscience and Engineering Vol 3, No 2 : Desember 2024
Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.37905/jage.v3i2.30314

Dambalo is a village located in Tomilito sub-district, North Gorontalo Regency, Gorontalo Province. This study aims to identify and describe the geological characteristics of the Dambalo area and its surroundings. The study focuses on geomorphology, stratigraphy, geological structure, and geological potential. The methods used include field observation and laboratory analysis. Field observations include geological mapping, rock sampling, and measuring geological structures using a geological compass. Meanwhile, laboratory analysis was carried out to determine the mineral composition, rock texture and rock name through petrography and stratigraphic analysis. The results of the study indicate that the study area is stratigraphically composed of the oldest to the youngest lithological units, namely porphyry andesite units, volcanic breccias, and alluvial deposits. The dominant geological structure is tensile fractures (tension fractures) with three main orientations. The geological potential in this area includes C-type mining materials, which mainly consist of porphyry andesite rocks, which have economic value for the construction industry. However, this area also has the potential for landslide hazards, namely in areas with steep slopes. This research is expected to contribute to the management of natural resources and mitigation of geological landslide disasters in Dambalo and its surroundings.

Studi Geologi Daerah Titidu Kecamatan Kwandang Kabupaten Gorontalo Utara Wangi, Akrein Vender; Permana, Aang Panji; Zainuri, Ahmad
Journal of Applied Geoscience and Engineering Vol 3, No 2 : Desember 2024
Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.37905/jage.v3i2.30309

The research location is in the Titidu area, North Gorontalo Regency. This study aims to determine the distribution of volcanic igneous rocks in the Titidu area. The research method used in this study is surface geological mapping to determine the geology of the research area, and for data processing using petrographic analysis. The results of the study found that the geomorphology of the research area is volcanic hills, structural hills and alluvial plains, the stratigraphy of the research area is sorted from old to young is an altered andesite unit, andesite unit, pyroclastic breccia unit and fluvial sediment unit. The geological structure in the research area is in the form of a fracture (tension joint) with a general direction of northeast - southwest. Based on the results of petrography, the type of rock is basaltic andesite.

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

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.

Geologi Daerah Dulamayo Selatan, Kecamatan Telaga, Kabupaten Gorontalo Mahmud, Vani Akbarani Y.; Permana, Aang Panji; Zainuri, Ahmad
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.v4i1.33609

The purpose of this research is to examine and interpret the geological setting of the Dulamayo Selatan area in Telaga District, Gorontalo Regency. The research addresses aspects of geomorphology, stratigraphy, and structural geology to develop a thorough understanding of the geological framework of the region. The methodology includes field surveys such as surface geological mapping, outcrop observations, and laboratory analysis for petrology and petrography. The findings indicate that the study area can be classified into two distinct geomorphological units: Lava Flow Ridge and Intrusive Hills. The stratigraphy comprises two rock units: the andesite unit, consisting of andesite and altered andesite, and the granodiorite unit. Structurally, the area is dominated by tension joints with a primary northeast-southwest orientation. It is expected that the findings of this study will contribute to a better understanding of the geological conditions of the region and assist in efforts related to natural resource utilization and the mitigation of geological risks in Dulamayo Selatan.

Kajian Geologi Teknik dan Potensi Longsor pada Segmen IG1 dan IG2 Akses Tambang di Kabupaten Pohuwato, Gorontalo Ginting, Immanuel; Permana, Aang Panji; Zainuri, Ahmad
Journal of Applied Geoscience and Engineering Vol 4, No 2 : Desember 2025
Publisher : Universitas Negeri Gorontalo

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.37905/jage.v4i2.37128

This study examines the geological conditions and slope stability of segments IG1 and IG2 in the Magazine access area of the Pani Gold Project, Pohuwato Regency. The research methods include geological mapping, scanline analysis, kinematic evaluation using stereonet, and Rock Mass Rating (RMR) and Slope Mass Rating (SMR) assessments. Segment IG1 consists of volcanic breccia with an RMR value of 57 (Class III, Fair Rock) and an SMR value of 45–50 (Poor), indicating wedge failure potential. Segment IG2 is dominated by dacite with an RMR of 60 (Class III, Fair Rock) and an SMR of 55–60 (Fair–Good), showing a tendency toward toppling failure. The results suggest that IG2 is relatively more stable than IG1, although localized failures may occur. Technical recommendations include slope reinforcement with rock bolts, shotcrete, and drainage systems to minimize slope failure risks.

Co-Authors Abduh, Alan Gani Abdul Hadi Abdul Malik Abidin, Miftahul Agissa, Aina Warda Agus Dwi Catur Ahmad Ahmad Ahmad Sururi Ahmad Sururi Ahmawati, Fitri Dewi Aisa, Aisa Al-Hakim, Luqman Amir Hamzah Amrullah, M. Kholis Annisa Astrid Annisa Fitri, Rizqi Ardana Ardiansyah, Keisha Elvaretta Arimurti, Ilham Aripin, Ahmad Saiful Aris, Ayub Pratama Arni Arni Arni Arwani, Ragil As'ari, Muh Hasym Asmuni Asmuni Audina, Novia Az Zahrah, Fathanah Azzahra, Nafa Baskoro Setioputro Basori, Ruchman Bastomi, Bastomi Berthanila, Rethorika Berthanilla, Rethorika Daeng Permana, Mujiantara Dai, Elan Daniel Happy Putra Daud Yusuf Dewa Gede Eka Setiawan Dewi Wahyuni K. Baderan Dewi, Marisa Santi Dinawati Trapsilasiwi Doni Susanto, Doni Dwi Catur, Agus Dwi Saputri, Mar'atul Latifah Eka Saputra, Darwin Emiliya, Emiliya Epilia, Epilia Fadilah, Rika Julianti Fadli Arafah, Ahmad Farhani, Deswita Fatimah Zahra, Frika Fauzan, Ali febriyanti febriyanti Fitriani, Geti Fitryane Lihawa Gani, Muslim Gani, Yasir Muslim Ginting, Immanuel Hamimu, Moh Febrianto Hamzah, Tajuddin Hasim Hasim Hasim Hermawan, Hosnan Hidayat Hidayat Hidayat, Dede Hiola, Tya Ivanka HR, Mahmutarom Hutagalung, Ronal I Made Suartika Ibrahim Ibrahim Ibrahim Sota IGNK Yudhyadi Ismail, Zenza Harnold Juita, Fiksi K Badaun, Nur Azizah Katili, Gita Triyana Risti Kholid, Nur Kiwo, Anince Kurnia, Riza Kusuma, Nur Hadi Lahay, Muamart Gimnastiar Lasahido, Moh. Syach L. Leni Marlina lidia oktavia, lidia M. Fajar, M. M. Khusna Amal Maharani, Amanda Mahendra, Arivan Mahmud, Fitria Mahmud, Vani Akbarani Y. Male, Cindi Claudia Mamonto, Naya Fanisa Mamonto, Yusril Mahendra Marike Mahmud Marlina Masay, Muhammad Syawal Ardiansyah Maulidia, Firda Mbuinga, Ansyar Meidji, Icha Untari Mia Audina, Mia Miftahul Jannah Mohamad, Nurdin Muchtar, Aflatun Muh. Kasim Muhammad Fakhriza, Muhammad Muhammad Kasim Mukti, Mukti Mursalin . Nabila, Salsa Natua, Moh Rizky A R Ninasafitri, Ninasafitri Nofiani, Julia Noviar Akase Nugraha, Lukman Nugraha, Praja Nugrahi, Putri Inayah Nurfaika Nurfaika Nurjanah, Diana Nurul Mahmudah, Nurul Oktarina, Wulan Padmiatmi, Pandri Pahrun, Aliim Risky Paladan, Rayhand Batara Paladan, Reynhard Batara Panai, Irdiansyah Paputungan, Qurota Ayuni Paryanto Dwi Setiawan, Paryanto Dwi Permana, Aang Panji Pramudita, Ratri Putri, Selia Seftiani Rabial Kanada, Rabial Rahmi Mulyasih Rakhmat Jaya Lahay Rama Adji Prasetya, M Rasyid, Fajri Fitrah Fidianto A. Rismawan Adi Yunanto Rizki, Arif Robi Yanto Rohliyati, Rohliyati Rois, Choirur Romdoniyah, Siti Ruru, Susanti S. Sinarep, S. S. Supriyadi, S. Sabera Adib, Helen Sahidah, Aril A.H Saipul Annur Salim, Amil Sandi, Ari Saprullah, Saprullah Saputra, Ade Akhmad Saputri, Arliani Sari Hernawati Sari, Via Anjela Sarwah, Putri Hana Sayid Habiburrahman, Sayid Sibron, A Simbala, Susilo Bintang Sinarep Sino, Widya Indriani H. SM, Farid Sri Mulyani Sugianti, Komang Suharjono, Gilang Eko Setyo Sujita, Sujita Surya, Sandy Syaifuddin Fahmi Syam S. Kumaji Tutut Handayani Tyas, Dyte Meining Umurohmi, Ulfa Umurohmi, Ulfah Utari, Desy Wangi, Akrein Vender Waspodo, Waspodo Wiwik Handayani Yana, Leli Yasir, Muslim Gani Yayu Indriati Arifin Yulianti, Rachmi Yulianti, Rachmi Yuniarti, Ira Yunita Yunita Zahra, Frika Fatimah Zahro , Mukminatuz Zainal Berlian

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