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All Journal POSITRON Jurnal Penelitian Fisika dan Aplikasinya (JPFA) TELKOMNIKA (Telecommunication Computing Electronics and Control) Jurnal Fisika Unand Emerging Science Journal Jurnal Penelitian Pendidikan IPA (JPPIPA) Logista: Jurnal Ilmiah Pengabdian Kepada Masyarakat Jurnal Ilmu Fisika MONSU'ANI TANO Jurnal Pengabdian Masyarakat Riyadhoh : Jurnal Pendidikan Olahraga BERNAS: Jurnal Pengabdian Kepada Masyarakat Warta Pengabdian Andalas: Jurnal Ilmiah Pengembangan Dan Penerapan Ipteks

Marzuki Marzuki

Department Of Physics, Faculty Of Mathematics And Natural Sciences, Universitas Andalas, Padang 2516, West Sumatra, Indonesia

Author-ID : 1133611

Religion Agriculture, Biological Sciences & Forestry Humanities Astronomy Biochemistry, Genetics & Molecular Biology Chemical Engineering, Chemistry & Bioengineering Chemistry Civil Engineering, Building, Construction & Architecture Computer Science & IT Dentistry Earth & Planetary Sciences Education Electrical & Electronics Engineering Energy Environmental Science Languange, Linguistic, Communication & Media Materials Science & Nanotechnology Mathematics Medicine & Pharmacology Neuroscience Nursing Physics Public Health Social Sciences Veterinary Other

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Analysis of S-Wave Propagation and Resistivity Value in Porous Medium for Conjecture Potential of Groundwater in Lempuing Village, Bengkulu City Melly Angglena; Marzuki Marzuki; Arif Ismul Hadi
Jurnal Penelitian Pendidikan IPA Vol. 8 No. 2 (2022): April
Publisher : Postgraduate, University of Mataram

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.29303/jppipa.v8i2.1458

Bengkulu city is facing groundwater problems where some of the groundwater is brackish. The study aimed to determine the structure of the subsurface layer through the propagation velocity of secondary wave (Vs) in a layer of porous medium in estimating the potential for groundwater. This research supported by resistivity data and will be validated based on the depth of the well. MASW data was processed using WinMASW Professional 5.0 software to obtain a 1D profile of the Vs value, and Res2dinv software was used to obtain a 2D cross-section of the resistivity value. The results showed a decrease in the value of Vs in the porous medium layer from 133 to 358 m/s in the first path, and from 149 to 314 m/s for the second path. The decrease in the value of Vs is in the range of groundwater potential which is close to the depth of the resident's well, with the type of porous medium layer being sands and intact clays. The subsurface profile from the Vs measurement shows a good agreement with the resistivity value profile from the Geoelectric method. So, secondary wave propagation can be used in determining groundwater potential for a depth of < 10 m

Determination of Geothermal Fluid Characteristics in Pawan and Pendalian IV Koto Villages, Rokan Hulu Regency, Riau Province Using Geochemical Methods Rifa Lihayati; Muldarisnur Muldarisnur; Marzuki Marzuki
Jurnal Penelitian Pendidikan IPA Vol. 8 No. 2 (2022): April
Publisher : Postgraduate, University of Mataram

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.29303/jppipa.v8i2.1491

Geothermal in Pawan and Pendalian IV Koto Villages is one of the post-volcanic geothermal areas in the Rokan Hulu Regency. This study aims to determine the characteristics of geothermal fluids and estimate reservoir temperature based on geothermometer estimation. The research method used in the study consisted of several stages, namely field data collection and fluid geochemical analysis. The research results from 12 hot springs plotted on the Cl-Li-B triangle diagram show that all hot water samples are dominated by Cl, indicating that the hot springs are far from the geothermal reservoir. The Cl-SO4-HCO3triangle diagram shows that all of the hot springs are bicarbonate water types dominated by HCO3. The Na-K-Mg triangle diagram shows that all fluid samples are in the immature water area, which indicates that the fluid has undergone a reaction with other elements or the influence of meteoric water is quite dominant. The results of calculations with a geothermometer, the estimated reservoir temperature in the geothermal area is in the range of 160.69°-176.76°C, which is included in the medium-temperature reservoir system. Geothermal in this area can be used as the geothermal potential for developing geothermal power plants.

Influence of Weather Conditions on COVID-19 Case in Several Regions of Indonesia Bella Deswanti; Marzuki Marzuki; Robi Muharsyah; Helmi Yusnaini; Ravidho Ramadhan
Jurnal Penelitian Pendidikan IPA Vol. 8 No. 3 (2022): July
Publisher : Postgraduate, University of Mataram

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.29303/jppipa.v8i3.1851

This study investigates the relationship between COVID-19 and weather conditions in six regions in Indonesia, namely South Jakarta, East Jakarta, North Jakarta, Jember Regency, Semarang City, and West Pasaman Regency. The study uses the daily number of positive cases of COVID-19 and weather data. Weather parameters used in this study are the average, maximum, and minimum temperature, rainfall, and relative humidity. Weather data were obtained from surface observation of Agency for Meteorology, Climatology and Geophysics (BMKG) and reanalysis product (ERA-5) from European Centre for Medium-Range Weather Forecasts (ECMWF). The effect of weather conditions on the number of COVID-19 cases was evaluated using the Spearman and Kendall correlation. It was found that the number of positive cases of COVID-19 had a relationship with weather parameters. A negative correlation was found between the temperature and the number of positive COVID-19 cases. Thus, the number of positive COVID-19 cases increases when the temperature decreases. On the other hand, rainfall and relative humidity positively correlate to the number of positive cases of COVID-19, which means that when the rainfall and relative humidity increase, the number of positive cases of COVID-19 increases. The relationship between weather conditions and the number of COVID-19 cases is more apparent in areas with a higher population density, such as Jakarta. The results of this study can be valuable information in handling COVID-19 cases.

Comparison of Deformation Vectors Due to Earthquake in Subduction Zone and Sumatran Fault for Each Phase of Earthquake Cycle Fadilla Monica; Vira Friska; Deasy Arisa; Marzuki Marzuki
Jurnal Ilmu Fisika Vol 14 No 2 (2022): September 2022
Publisher : Universitas Andalas

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25077/jif.14.2.73-85.2022

This study compares the deformation in West Sumatra due to the earthquakes in the subduction zone and the Sumatran Fault. The Mw6.0 Mentawai earthquake 2019 with a thrust fault mechanism and the Mw5.4 South Solok earthquake 2019 with a strike-slip fault mechanism were used as case studies for the subduction zone and Sumatran Fault, respectively. The deformation was observed using 12 SuGAr (Sumatra GPS Array) and 8 InaCORS (Indonesian Continuously Operating Reference Station) stations, which were processed using GAMIT/GLOBK software. There are differences in the deformation vectors of the two earthquakes. The Mentawai earthquake experienced larger energy accumulation than the South Solok earthquake. The coseismic phase of the Mentawai earthquake experienced the largest horizontal shift at the SLBU station, which was 15.48 mm in the direction of S29.96W, while the South Solok earthquake is found to horizontally shift the CSDH station at the size of 5.75 mm towards S11.45E. The postseismic phase of the Mentawai earthquake lasted 60 days, longer than the South Solok earthquake (20 days). The difference in deformation characteristic between these two earthquakes found in this study will be valuable information in modeling earthquakes in Sumatra.

Analisis Sebaran Hiposenter Gempa Vulkanik Gunung Marapi Menggunakan Metode Geigerâ€™s with Adaptive Damping (GAD) Sri Hamdiyessi; Marzuki Marzuki; Ardian Putra; Novianti Indrastuti
Jurnal Fisika Unand Vol 11 No 4 (2022)
Publisher : Universitas Andalas

Telah dilakukan Telah dilakukan penelitian tentang klasifikasi gempa dan sebaran hiposenter gempa Gunung Marapi. Penentuan distribusi hiposenter menggunakan Geigerâ€™s method with Adaptive Damping (GAD). Prinsip yang digunakan dalam metode GAD adalah menghitung selisih antara waktu pengamatan dan waktu perhitungan Berdasarkan klasifikasi dan sebaran hiposenter gempa Gunung Marapi dapat disimpulkan bahwa pada bulan Januari-April gempa Vulkanik tidak dapat dianalisa. Gempa dominan terjadi pada bulan mei yang merupakanÂ kenaikan aktivitas dari Gunung Marapi. Sebaran Hiposenter berada pada kedalaman 2600 â€“ 4700 m. Episenter tersebar mengelilingi puncak Gunung Marapi dimana jarak antar episenternya mengelilingi puncak kawah, jarak episenter 1 â€“ 7 km dari puncak kawah. Hiposenter dan episenter memiliki sebaran yang tidak beraturan dan magma bergerak dari Barat Laut ke Tenggara. Sebaran hiposenter ini cukup dekat dari kawah Gunung sehingga ada kemungkinan untuk terjadi erupsi.Hal ini mengindikasi bahwa terjadi lonjakan aktivitas Gunung Marapi hanya saja tidak ada kenaikan level aktivitas gunung.

Analisis Kecepatan Pergeseran Seismik Sesar Palu Koro Akibat Gempa Palu 2018 Menggunakan Data Global Navigation Satellite System Nurdin Nurdin; Dwi Pujiastuti; Marzuki Marzuki
Jurnal Fisika Unand Vol 11 No 4 (2022)
Publisher : Universitas Andalas

Kecepatan pergeseran seismik horizontal dari Sesar Palu koro akibat gempa Palu 28 September 2018 dengan kekuatan 7,4 SR telah dianalis menggunakan 10 stasiun InaCORS (Indonesian Continuously Operating Reference Stations) untuk melihat pergeseran yang terjadi sebelum gempa/praseismik, saat gempa/koseismik, dan setelah gempa/pascaseismik. Stasiun yang digunakan adalah CBAL, CRAU, PALP, CKEN, CTOL, CPRE, CMLI, CPAL, CMAK, dan CBIT. Penelitian ini menggunakan software GAMIT, GLBOK, dan GMT. Data pengamatan yaitu sebanyak 100 DoY (Day of Years) dimulai dari 6 Agustus sampai 28 November 2018 (DoY 218-317). Pada fase praseismik (DoY 218-270), stasiun InaCORS mengalami kecepatan pergeseran 0,245819 mm/hari-0,026816 mm/hari dengan arah pergerakan dipengaruhi oleh manifestasi tektoknik yang ada di Sulawesi. Kecepatan Pergeseran meningkat pada fase koseismik (DoY 271-272) dimana stasiun InaCORS kecepatan pergeseran 1151,790819 mm/hari sampai 0,592832 mm/hari dengan arah yang berlawanan dengan fase praseismik. Stasiun yang bagian utara bergerak dominan ke utara dan yang selatan dominan ke selatan. Pada fase pascaseismik (DoY 273-318), Kecepatan pergerakan stasiun InaCORS mengikuti arah pergerakan pada fase koseismik, dengan besar kecepatanÂ sebesar 0,023154 mm/hari 0,283536 m.

Identification of Fault Structure in the Vicinity of Bukik Gadang Hot Spring Mount Talang Subdistrict Using Geomagnetic Method Ikhwan Fikri Maulidan; Marzuki Marzuki; Ardian Putra
Jurnal Penelitian Pendidikan IPA Vol. 8 No. 4 (2022): October
Publisher : Postgraduate, University of Mataram

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.29303/jppipa.v8i4.1962

Geological structures in the Bukit Gadang geothermal area have been identified using the geomagnetic method to determine the type of fault. Data was measured using a magnetometer in the area with dimensions of 1200 m × 1200 m consisting of 144 points at 12 tracks, and the spacing between points was 100 m. Magnetic anomaly data performed diurnal and IGRF (International Geomagnetic Reference Field) corrections. Furthermore, reduced to poles and continuous upwards processes were carried out to remove noise and separate local and regional anomalies. The magnetic field anomaly in the study area ranges from -1771.8 nT to 1089.9 nT, dominated by negative values, indicating the presence of heat sources and the influence of demagnetization of subsurface rocks. The 2D modeling results show that two primary rocks dominate the study area; pyroclastic flow units and andesite lava rock, which come from the Jantan and Batino volcanic formations. The caprock rock layer was identified in the upper layer with a depth of 850 meters. The reservoir rock layer with low susceptibility values was below the caprock layer. The 3D modeling results show a normal fault with a depth of 300-800 meters or at the border of the Jantan volcanic formation with the Batino volcanic formation. The fault line leads to the southeast-northwest (N160°E). The faults obtained from the 2D and 3D models are suspected to be the outflow of geothermal fluid from the reservoir rock layer and form a manifestation in the form of a hot spring at Bukik Gadang.

Effects of Land Cover Change and Deforestation on Rainfall and Surface Temperature in New Capital City of Indonesia Ramadani Safitri; Marzuki Marzuki; Mohammad Ali Shafii; Helmi Yusnaini; Ravidho Ramadhan
Jurnal Penelitian Pendidikan IPA Vol. 8 No. 6 (2022): December
Publisher : Postgraduate, University of Mataram

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.29303/jppipa.v8i6.2182

Land cover change and deforestation have a significant impact on climate change. This study investigates the effect of land cover change and deforestation on surface temperatures and extreme rainfall in the New Capital City of Indonesia (IKN), particularly in Samboja and Sepaku Subdistricts, East Kalimantan Province. Land cover change and deforestation were analyzed from Landsat 5 TM, 7 ETM+, and 8 OLI satellite data during 2001-2020. Land cover is divided into four classes: built-up land, water bodies, vegetation, and agricultural area. Rainfall data were obtained from the Integrated Multi-satellite Retrievals for GPM (IMERG) version 6 satellite, and extreme temperatures were taken from fifth-generation ECMWF reanalysis (ERA5) data. A significant decrease in vegetated land area is observed every year, followed by an increase in residential land and buildings (built-up area) and agricultural land. The highest rate of increase was observed in the area of agricultural land. Such change is correlated with an increase in surface temperature in the IKN. The strongest correlation is shown by increased built-up area and agricultural land. The relationship between rainfall and land cover is weak, and the body of water shows a relatively strong relationship. The extreme number of very wet days (R95p), consecutive dry days (CDD), and max 1-day precipitation (RX1day) rain index showed a decreasing trend during 2001-2020. However, the consecutive wet days (CWDs) index showed an increase. This needs to be a concern because consecutive precipitation extremes may cause more catastrophability than occasional extreme events.

Deformation Analysis of 2012 Mw8.6 Indian Ocean Earthquake Based on GPS Data in Preseismic, Coseismic, and Postseismic Phases Marzuki Marzuki; Zul Ikram; Vira Friska
Jurnal Penelitian Pendidikan IPA Vol. 8 No. 6 (2022): December
Publisher : Postgraduate, University of Mataram

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.29303/jppipa.v8i6.2419

The earthquake was one of the biggest natural disasters in Sumatra and dramatically affected this region and the surrounding area. Determination of surface deformation due to the earthquake is essential for disaster mitigation. The Global Navigation Satellite System (GNSS) is a commonly used method for determining surface deformation due to earthquakes. This study analyzes surface deformation during the preseismic, coseismic, and postseismic phases due to the 2012 Mw8.6 Indian Ocean earthquake. The study used Global Positioning System (GPS) data from the Sumatran GPS Array (SuGAr) network. The most significant horizontal deformation was observed at the LEWK station, which was 280.554 mm towards the northeast and experienced a subsidence of 40.830 mm in vertical deformation. Horizontal deformation is still felt by 22.453 mm to the northeast and vertical deformation of 8.810 mm (uplift) at stations that are farther (580 km) from the earthquake's epicenter. However, in the observation period of 60 days (postseismic phase), stations closer to the epicenter are still experiencing a postseismic phase. In contrast, stations far from the epicenter show that the postseismic phase is almost complete. In the preseismic phase, all stations experience almost the same horizontal deformation, ranging from 2.210 mm-3.639 mm, but with a different direction of movement, which may be caused by previous intense earthquake activity, which is still releasing energy (postseismic phase). On the other hand, the vertical deformation during the preseismic phase generally experiences an uplift except at the LEWK station. The results of this study can be additional information for earthquake mitigation in the Sumatra region

Pengelolaan Laboratorium Bagi Guru-Guru Fisika dan Perancangan Laboratorium Percontohan di SMAN 2 Harau Dedi Mardiansyah; Afdhal Muttaqin; Ramacos Fardela; Feriska Handayani Irka; Astuti; Sri Handani; Harmadi; Dahyunir Dahlan; Zulfi; Rahmad Rasyid; Marzuki; Mohammad Ali Shafii; Arif Budiman; Elvaswer; Mora; Wildian
BERNAS: Jurnal Pengabdian Kepada Masyarakat Vol. 4 No. 1 (2023)
Publisher : Universitas Majalengka

Laboratorium merupakan salah satu sarana dan prasarana pembelajaran fisika di sekolah untuk menarik pembelajaran dan mendorong motivasi siswa dalam belajar fisika. Kegiatan yang dilaksanakan di laboratorium biasanya dalam bentuk praktikum atau demonstrasi. Laboratorium harus dikelola dan direncanakan dengan baik agar fungsinya optimal sebagai sarana pembelajaran fisika. Hasil observasi di beberapa SMA yang ada di Kabupaten Lima Puluh Kota ditemukan permasalahan bahwa laboratorium tidak dikelola dengan baik sehingga keberadaanya tidak efektif. Siswa jarang diajak praktikum di laboratorium. Alat-alat praktikum yang sudah diperoleh dari Dinas Pendidikan jarang digunakan untuk kegiatan praktikum, sehingga banyak alat yang sudah rusak karena jarang dipakai. Penataan alat dan fasilitas di laboratorium cukup memprihatinkan, tidak tertata dengan rapi dan tidak di inventaris dengan baik. Guru fisika kesulitan dalam mengadakan praktikum karena tidak adanya modul praktikum/buku petunjuk praktikum. Oleh karena itu kegiatan praktikum yang biasanya dilaksanakan di laboratorium kini dilaksanakan di ruang kelas dengan peralatan yang seadanya. Ini menyebabkan keberadaan laboratorium fisika tidak dimanfaatkan dengan baik. Atas dasar permasalahan-permasalahan tersebut, maka kami tim Pengabdian Kepada Masyarakat mengadakan pembinaan pengelolaan laboratorium fisika bagi guru-guru MGMP fisika yang ada di Kabupaten Lima Puluh Kota agar para guru fisika mampu mengelola laboratorium dengan baik sehingga dapat digunakan untuk kegiatan praktikum maupun proses pembelajaran. Rencana kegiatan PKM antara lain 1) Memberikan sosialisasi pengelolaan laboratorium, 2) Melakukan pengembangan Laboratorium Percontohan Implementasi Merdeka Belajar, 3) Melakukan diskusi pembuatan alat-alat praktikum dari peralatan sederhana, 4) Melakukan diskusi pembuatan modul praktikum/ buku petunjuk praktikum, dan 5) Melakukan monitoring awal dan lanjutan terhadap laboratorium dibeberapa sekolah yang berada di Kebupaten Lima Puluh Kota.

Co-Authors -, Renanto Adi Susilo Afdal, Afdal Afdhal Muttaqin Afrizal Afrizal Ahmad Fauzi Pohan Ahmad Rizqy Shubri Ahmad Zul Amal Zaini Ardian Putra Arif Budiman Arif Ismul Hadi Astuti Astuti Astuti Astuti Astuti Aulya Rahayu Aulya Rahayu Aulya Rahayu, Aulya Awaluddin Awaluddin Awaluddin Awaluddin Ayu Putri Ningsih Ayu Putri Ningsih Bella Deswanti Bunga Aprilia Dahyunir Dahlan Dea Kurnia Harysandi Dea Kurnia Harysandi Deasy Arisa Dedi Mardiansyah Dian Fitriyani Dinda Maulani Adfy Dwi Pujiastuti Dwi Puryanti Dwianda, Rany Audia Elfira Saufina Elfira Saufina Elvaswer Elvaswer Fadilla Monica Fadli Nauval Faridah Salma Feri Helmi Basri Feriska Handayani Irka, Feriska Handayani Fery Kurnia Sandi Gina Felita Harmadi Harmadi Harysandi, Dea Kurnia Helmi Yusnaini Helmi Yusnaini Helmi Yusnaini Helmi Yusnaini Hiroyuki Hashiguchi Hiroyuki Hashiguchi Hiroyuki Hashiguchi Hiroyuki Hashiguchi Hiroyuki Hashiguchi Hiroyuki Hashiguchi Hiroyuki Hashiguchi Hiroyuki Hashiguchi Hiroyuki Hashiguchi Hiroyuki Hashiguchi, Hiroyuki Ikhwan Fikri Maulidan Imam Taufik Imam Taufiq Indah Rahayu Iqbal Ramadhan Irza Utami L. Luini Lismalini Lismalini Lismalini, Lismalini Lisna Meylani Lusi Fitrian Sani Lusi Fitrian Sani Lusi Fitrian Sani, Lusi Fitrian Melly Angglena Meqorry Yusfi Meri Yoseva Mohammad Ali Shafii Mora Mora Mora Mora Mora Muchtia Rahma Muchtia Rahma, Muchtia Muhammad Arif Muhammad Kahfi Muharsyah, Robi Muldarisnur, Mulda Mutya Vonnisa Muzirwan Muzirwan Naela Amalia Zulfa Nauval, Fadli Nina Nina Nini Firmawati Nor Azlan Mohd Aris Novianti Indrastuti Nugroho, Susilo Nur Fadillah Nurdin Nurdin Nurul Hasanah Poltak Sandro Rumahorbo Poltak Sandro Rumahorbo, Poltak Sandro Puja Kasmailen Putri Rahmad Rasyid Rahmad Rasyid Rahmat Rasyid Ramacos Fardela Ramadani Safitri Ramadani Safitri Ramadhan, Ravidho Rani Delvihardini Rany Audia Dwianda Ravidho Ramadhan Ravidho Ramadhan Ravidho Ramadhan Ravidho Ramadhan Ravidho Ramadhan Ravidho Ramadhan Rifa Lihayati Rini Oktaviani Rio Chandra Rio Chandra, Rio Robi Muharsyah Salma, Faridah Selly Tridaiana Shimomai, Toyoshi Sholihun, Sholihun Silvia Wahyuni Solly Aryza Sri Hamdiyessi Sri Handani Sri Herlinda Sri Mai Dewi Sri Oktamuliani Sri Wahyuni Sri Wahyuni Sucy Lestari Wirma Sugeng Nugroho Suryanti, Krisna Suryanto, Wiwit Syarifatul Ulfah Toyoshi Shimomai Toyoshi Shimomai Toyoshi Shimomai Toyoshi Shimomai Toyoshi Shimomai Toyoshi Shimomai Trengginas Eka Putra Sutantyo Triana Vitri Triana Vitri, Triana Ulfa Azmi Usna, Sri Rahayu Alfitri Vira Friska Vira Friska Vira Friska Wendi Harjupa Wildian Wildian Wira Indrayani Yudi Saputra Zul Ikram Zulfi Zulfi Zulfi

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