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All Journal Jurnal Ilmu Lingkungan Jurnal Pengelolaan Sumberdaya Alam dan Lingkungan (Journal of Natural Resources and Environmental Management) Bioeksperimen: Jurnal Penelitian Biologi Jurnal Ilmiah Dinamika Rekayasa (DINAREK) Jurnal Geomine EnviroScienteae Jukung (Jurnal Teknik Lingkungan) Jurnal GEOSAPTA Sainmatika: Jurnal Ilmiah Matematika dan Ilmu Pengetahuan Alam Jambura Geoscience Review J SIG (Jurnal Sains Informasi Geografi) Jurnal Sibermas (Sinergi Pemberdayaan Masyarakat) Jurnal Inovasi Pengabdian Masyarakat Pendidikan Lamahu: Jurnal Pengabdian Masyarakat Terintegrasi
Permana, Aang Panji
Universitas Negeri Gorontalo
Agriculture, Biological Sciences & Forestry Chemistry Civil Engineering, Building, Construction & Architecture Control & Systems Engineering Earth & Planetary Sciences Education Electrical & Electronics Engineering Energy Engineering Environmental Science Industrial & Manufacturing Engineering Languange, Linguistic, Communication & Media Mathematics Medicine & Pharmacology Physics Public Health Social Sciences Other

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ANALISIS KEDALAMAN LAUT PURBA BATU GAMPING GORONTALO BERDASARKAN KANDUNGAN FOSIL FORAMINIFERA BENTONIK Permana, Aang Panji; Eraku, Sunarty Suly
Bioeksperimen: Jurnal Penelitian Biologi Vol 6, No 1: Maret 2020
Publisher : Universitas Muhammadiyah Surakarta

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.23917/bioeksperimen.v6i1.10428

Abstract

The research location is in the form of highland morphology in the Gorontalo City. Research material in the form of limestone with research methods in the form of field surveys and micropaleontological analysis. The purpose of this research is to find out the bentonic foraminifera fossil species and to know paleobathymetry. The results of the analysis there are four fossil species namely Biloculinella depressa, Cornuspira foliacea, Pyrgo laevis and Rhabdammina discreta. Based on the content of bentonic foraminifera fossils, it can be determined that paleobathymetry is Middle Neritic - Outer Neritic (20-200 meters).
Lingkungan Purba Batubara Sorong (Provinsi Papua Barat) Berdasarkan Analisis Petrografi Permana, Aang Panji; M Imran, A; Widodo, Sri
Dinamika Rekayasa Vol 15, No 2 (2019): Jurnal Ilmiah Dinamika Rekayasa - Agustus 2019
Publisher : Jenderal Soedirman University

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.20884/1.dr.2019.15.2.262

Abstract

Batubara Sorong yang berada pada Cekungan Salawati memiliki potensi untuk dikembangkan. Penelitian detail mengenai batubara Sorong sangat dibutuhkan terutama penelitian mengenai lingkungan purba pada saat batubara diendapkan. Penelitian ini menjadi menarik karena posisi batubara Sorong yang secara stratigrafi regional masuk pada endapan aluvial dan litoral yang berumur kuarter. Untuk itu tujuan utama penelitian ini adalah mengetahui jenis maseral penyusun batubara dan menentukan lingkungan purba pengendapan batubara. Upaya dalam mencapai kedua tujuan tersebut maka digunakan dua metode penelitian yakni survei lapangan (pemboran cutting) dan analisis petrografi. Hasil analisis petrografi didominasi jenis grup maseral vitrinite (huminite) berkisar antara 76,5-87,8%. Lingkungan pengendapan batubara berdasarkan dua klasifikasi diinterprestasikan lingkungan limnic (terendapkan di rawa danau). Sedangkan untuk interprestasi lingkungan persediaan bahan makanan berdasarkan analisis menunjukkan rawa rheotrophic.
Tipe, Lingkungan Dan Sejarah Diagenesis Batugamping Buliide Gorontalo Berdasarkan Analisis Petrografi Aang Panji Permana
Jurnal Geomine Vol 7, No 2 (2019): Edisi Agustus 2019
Publisher : Universitas Muslim Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (992.39 KB) | DOI: 10.33536/jg.v7i2.327

Abstract

Penyebaran batugamping secara geologi yang berada di bagian tengah Cekungan Limboto menjadi daya tarik untuk penelitian mengenai tipe, lingkungan dan sejarah proses diagenesis batugamping. Penelitian difokuskan di Daerah Buliide Kota Gorontalo  yang berada di bagian selatan Danau Limboto. Penelitian ini menjadi menarik karena baru pertama kali dilakukan. Tujuan penelitian ini ada tiga yakni mengetahui tipe diagenesis, lingkungan diagenesis dan sejarah proses diagenesis batugamping Buliide. Ketiga tujuan penelitian tersebut akan dicapai melalui dua metode penelitian yakni survei lapangan berupa analisis petrologi dan analisis laboratorium berupa analisis petrografi. Hasil penelitian menunjukan nama batugamping Buliide adalah coralline floatstone. Tipe proses diagenesis yang terjadi ada lima yakni sementasi, pelarutan, penggantian, mikritisasi dan rekristalisasi. Lingkungan diagenesa batugamping Buliide terdiri dari zona marine phreatic, zona vadose dan zona freshwater  phreatic. Sejarah proses diagenesis batugamping Buliide dapat dibagi menjadi tiga tahapan yakni tahapan pertama terjadi di zona marine phreatic, tahapan kedua zona freshwater phreatic dan tahapan ketiga zona vadose dengan tipe diagenesis berbeda-beda.
ANALISIS KEMAMPUAN DAN KESESUAIAN LAHAN DI DAERAH ALIRAN SUNGAI ALO, PROVINSI GORONTALO Sunarty Suly Eraku; Aang Panji Permana
Jukung (Jurnal Teknik Lingkungan) Vol 6, No 1 (2020): MARET 2020
Publisher : Program Studi Teknik Lingkungan Fakultas Teknik Universitas Lambung Mangkurat

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (502.651 KB) | DOI: 10.20527/jukung.v6i1.8243

Abstract

DAS Alo terletak di Kecamatan Tibawa Kabupaten Gorontalo Provinsi Gorontalo. DAS Alo memiliki ketinggian antara 50 m di atas permukaan laut di bagian hilir dan 475 m di atas permukaan laut di bagian hulu. Hulu DAS Alo merupakan perbukitan – pegunungan struktural di bagian utara dan barat laut dengan kemiringan lereng yang berkisar antara 15 - 40 persen.  Di bagian selatan (hilir) di dominasi oleh bentuklahan asal solusional yaitu perbukitan karst. Karakteristik DAS Alo terdiri dari luas DAS mencapai  69.736.900 m2, panjang sungai utama 21.160.422 meter dan kemiringan sungai 2,21%. Tujuan utama penelitian ini adalah menganalisis kemampuan dan kesesuaian lahan di DAS Alo Provinsi Gorontalo. Untuk mencapai tujuan tersebut digunakan metode survei lapangan dan analisis laboratorium sampel tanah. Hasil penelitian menunjukan bahwa kemampuan lahan dan kesesuaian lahan dipengaruhi oleh karakteristik Biogeofisik lahan di DAS Alo. Satuan bentuklahan perbukitan denudasional berbatu breksi memiliki kelas kemampuan lahan I, III, IV dan VI. Perbukitan struktural berbatuan breksi memiliki kelas kemampuan lahan I, II, III, IV, V dan VI. Perbukitan struktural berbatuan diorit, kelas kemampuan lahannya II, III, IV, V dan VI. Perbukitan karst kelas kemampuan lahannya III dan VIII dengan faktor pembatas lereng permukaan sedangkan kelas kemampuan lahan VII tidak dijumpai. Kelas kesesuaian lahan pertanian jagung pada kelas kesesuaian lahan S3, kelas kesesuaian lahan N1 (tidak sesuai saat ini) dan kelas kesesuaian lahan N2 (tidak sesuai selamanya). Sedangkan untuk kelas kesesuaian lahan S1 (sangat sesuai) dan kelas kesesuaian lahan S2 (cukup sesuai) tidak dijumpai di DAS Alo. Kata kunci: DAS Alo, Kemampuan Lahan, Kesesuaian Lahan.  Alo Watershed is located in Tibawa Sub-District, Gorontalo Regency, Gorontalo Province. The Alo watershed has a height of between 50 m above sea level in the downstream and 475 m above the sea level in the upper reaches. The upper Alo watershed is a structural hill - mountain range in the north and northwest with a slope ranging from 15 - 40 percent. In the south (downstream) is dominated by the form of land from the original solution, the karst hills. The characteristics of the Alo Watershed consist of an area of 69,736,900 m2, a main river length of 21,160,422 meters and a river slope of 2.21%. The main objective of this study is to analyze the ability and suitability of land in the Gorontalo Province Alo Watershed. To achieve this goal field survey methods and laboratory analysis of soil samples are used. The results showed that land capability and land suitability were affected by biogeophysical characteristics of land in the Alo watershed. Unit shape den denational hills breccia rocky has a land capability class I, III, IV and VI. The rocky structural breccias hills have land capability classes I, II, III, IV, V and VI. Diorite rocky structural hills, land capability classes II, III, IV, V and VI. Karst hills are land capability classes III and VIII with surface slope limiting factors while land capability class VII is not found. Corn land suitability class in S3 land suitability class, land suitability class N1 (not suitable at present) and land suitability class N2 (not suitable forever). As for the S1 land suitability class (very suitable) and S2 land suitability class (quite suitable) not found in the Alo watershed. Keywords: Alo Watershed, Land Capability, Land Suitability.
Analisis Kedalaman Laut Purba Batu Gamping Gorontalo Berdasarkan Kandungan Fosil Foraminifera Bentonik Aang Panji Permana; Sunarty Suly Eraku
Bioeksperimen: Jurnal Penelitian Biologi Vol 6, No 1: Maret 2020
Publisher : Universitas Muhammadiyah Surakarta

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.23917/bioeksperimen.v6i1.10428

Abstract

POTENSI BATUGAMPING TERUMBU GORONTALO SEBAGAI BAHAN GALIAN INDUSTRI BERDASARKAN ANALISIS GEOKIMIA XRF Aang Panji Permana
EnviroScienteae Vol 14, No 3 (2018): EnviroScienteae Volume 14 Nomor 3, November 2018
Publisher : Universitas Lambung Mangkurat

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (320.946 KB) | DOI: 10.20527/es.v14i3.5688

Abstract

The potential of reef limestone in Gorontalo Province is very large. The proof is in two research stations in Kelurhan Buli'ide and Tanjung Kramat Village. Research on the potential of reef limestone using two methods of analysis petrology and geochemistry of XRF. Based on the results of the research both stations have the name of the rock and the composition of the chemical compounds is different. The results of the study differ from previous studies. Differences are found in the composition of CaO compounds higher than 80%. The chemical composition of compounds in two research stations has the potential to be developed into industrial material. Use of reef limestone can be used as building stones, road stabilizers, agricultural lime, ceramic materials, water purification and the process of deposition of non-ferrous metal ores.
Kualitas Batugamping Gorontalo Sebagai Reservoir Air Tanah Berdasarkan Analisis Jenis Porositas Aang Panji Permana; Sunarty Suly Eraku
EnviroScienteae Vol 16, No 1 (2020): EnviroScienteae Volume 16 Nomor 1, April 2020
Publisher : Universitas Lambung Mangkurat

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.20527/es.v16i1.8993

Abstract

The potential of limestone in Gorontalo City is not only the use of industrial minerals but also its availability as a reservoir of groundwater reservoirs. The availability of groundwater is the main focus in preserving the environment. For this reason, this research focuses on the quality of limestone reservoirs by analyzing limestone porosity. The purpose of this study was to determine the average porosity percentage, porosity type and porosity quality both semi-quantitative and qualitative. In order to achieve these objectives, two methods are used namely the field survey method and petrographic analysis. The results showed the average percentage of porosity quality of limestone as a reservoir of groundwater in the excellent category with the type of porosity is fracturing and growing (vugular).
ANALISIS LINGKUNGAN PURBA BATUGAMPING DAERAH LIMBOTO BARAT KABUPATEN GORONTALO Aang Panji Permana; Muhammad Kasim; Fajri Kurniawan Mamonto
Geosapta Vol 7, No 2 (2021): Juli 2021
Publisher : Universitas Lambung Mangkurat

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.20527/jg.v7i2.10681

Abstract

Penelitian batugamping di Cekungan Limboto tepatnya di daerah Limboto Barat Kabupaten Gorontalo sangat menarik diteliti. Penyebaran batugamping di bagian tengah danau jelas menunjukkan kompleksitasi geologi daerah penelitian. Limboto Barat yang saat ini merupakan bagian dari danau air tawar jelas menarik diteliti mengingat keberadaan batugamping yang mengandung fosil foraminifera merupakan makluk hidup yang berasal dari laut. Untuk itu tujuan penelitian ini membuktikan sekaligus menganalisis lingkungan purba batugamping daerah Limboto Barat pada jutaan tahun lalu. Tujuan penelitian tersebut akan dicapai menggunakan dua metode yakni survei lapangan dan analisis laboratorium berupa analisis biostratigrafi. Berdasarkan hasil dan diskusi dari penelitian ini menunjukan bahwa terdapat tujuh spesies fosil foraminifera bentonik dengan lingkungan purbanya adalah brackish lagoons and estuaries.
Analisis Kedalaman dan Kualitas Air Tanah di Kecamatan Hulonthalangi Kota Gorontalo Aang Panji Permana
Jurnal Ilmu Lingkungan Vol 17, No 1 (2019): April 2019
Publisher : School of Postgraduate Studies, Diponegoro Univer

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1493.709 KB) | DOI: 10.14710/jil.17.1.15-22

Abstract

ABSTRAKAir tanah merupakan sumber utama cadangan air tawar yang bekerja dalam siklus hidrostatik. Air tanah disediakan untuk konsumsi manusia, pertanian, industri dan banyak ekosistem yang bergantung pada air tanah, terutama selama musim kemarau. Kecamatan Hulonthalangi secara geografis terletak bagian selatan Kota Gorontalo berbatasan langsung dengan Teluk Tomini terdiri dari 5 kelurahan yakni Donggala, Pohe, Siendeng, Tenda dan Tanjung Kramat. Jumlah penduduknya 16.304 yang dilalui tiga sungai yakni Sungai Bone, Bolango dan Tamalate. Penelitian ini bertujuan mengetahui kedalaman muka air tanah dangkal secara pasti dengan mengukur langsung sumur warga. Selain itu penelitian ini juga bertujuan mengetahui kualitas air tanah dengan analisis parameter fisika dan kimia. Metode yang digunakan adalah analisis secara kualitatif dan kuantitatif. Analisis kualitatif mengamati kualias air tanah berdasarkan parameter fisika seperti warna, bau, rasa dan keterdapatan endapan serta mewawancara warga. Untuk analisis kuantitatif mengukur dan memplot koordinat, elevasi, kedalaman air tanah dan kandungan kimia. Hasil dan pembahasan penelitian menunjukan kedalaman muka air tanah rata-rata 2,87 - 4,04 meter. Pola aliran air tanah terbagi dua yakni dari tenggara ke barat laut dan dari timur ke barat. Analisis kualitas air, untuk warna 16% sampel terindikasi perlu tindaklanjut analisis laboratorium. Parameter bau 12% sampel tidak memenuhi syarat, untuk rasa 24% sampel tidak memenuhi syarat dan untuk endapan 14% sampel terindikasi tindaklanjut analisis laboratorium. Pemanfaatan air tanah 24% untuk kebutuhan pokok temasuk air minum. Analisis kimia di Stasiun 46 Kelurahan Pohe merupakan depot air minum mengandung besi 0,02 mg/l, nitrat 1,2 mg/l dan arsen 0 mg/l memenuhi standar kesehatan. ABSTRACT Ground water is the main source of freshwater reserves that work in the hydrostatic cycle. Groundwater is provided for human consumption, agriculture, industry and many ecosystems that depend on ground water, especially during dry seasons. Hulonthalangi Subdistrict is geographically located south of Gorontalo City adjacent to Tomini Bay consists of 5 villages namely Donggala, Pohe, Siendeng, Tenda and Tanjung Kramat. The population of 16,304 passes through three rivers namely Bone, Bolango and Tamalate Rivers. This study aims to determine the depth of shallow groundwater face with certainty by directly measuring the residents' wells. In addition, this study also aims to determine the quality of groundwater with the analysis of physical and chemical parameters. The method used is qualitative and quantitative analysis. Qualitative analysis observes the quality of groundwater based on physical parameters such as color, odor, taste and sediment deposit and interviewing citizens. For quantitative analysis measures and ploting the coordinates, elevation, depth of ground water and chemical content. Results and discussion of the study showed the depth of groundwater averaging 2.87 - 4.04 meters. The pattern of groundwater flow is divided into two, namely from southeast to northwest and east to west. Analysis of water quality, for the color of 16% samples indicated need follow-up laboratory analysis. The odor parameter of 12% samples was not eligible, for a taste of 24% unqualified samples and for precipitation 14% samples indicated follow-up laboratory analysis. Utilization of ground water 24% for basic needs including drinking water. Chemical analysis at Station 46 Pohe Village is drinking water depot contain 0.02 mg/l iron, 1.2 mg/l nitrate and 0 mg/l arsen meets health standards. 
KAJIAN PELAPUKAN GRANIT DAERAH LEATO BERDASARKAN ANALISIS XRD DAN SEM Ronal Hutagalung; Aang Panji Permana; Dewi Rahmawaty Isa
EnviroScienteae Vol 18, No 1 (2022): ENVIROSCIENTEAE VOLUME 18 NOMOR 1, APRIL 2022
Publisher : Universitas Lambung Mangkurat

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.20527/es.v18i1.12977

Abstract

Weathering is a natural process due to the work of exogenous forces both physically and chemically which results in the breakdown of rocks and constituent minerals into loose materials. Weathering can cause compact and resistant granite to move easily, causing rock fall in the Leato area, Gorontalo City. This study aims to assess the level of weathering of granite based on X-Ray Diffraction (XRD) and Scanning Electron Microscope Analysis (SEM) analysis. The research objectives will be achieved using two methods consisting of field surveys and laboratory analysis in the form of XRD and SEM analysis. Based on the results and discussion that granite rocks have undergone weathering. Evidence of weathering is clearly shown in SEM photos, namely weathering occurs at the edges of granite rocks.
Co-Authors Aisyah Alya H Panai Angki Suaib Asmoro Widagdo Ayub Pratama Aris Dewi Rahmawaty Isa Dewi Rahmawaty Isa Djamal Adi Nugroho Uno Evi Hulukati Fajri Kurniawan Mamonto Hendra Hendra Ivan Taslim M Imran, A Masruroh Masruroh Moch Rio Pambudi Mohamad Karmin Baruadi Muh Kasim Muh Nasrullah Al Fauzan Muhammad Kasim Ninasafitri, Ninasafitri Novariani Payuyu Nurdin Mohamad Ronal Hutagalung Sri Widodo Sunarty Suly Eraku Sunarty Suly Eraku