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Penerapan Technology Acceptance Model (TAM) dalam Pengujian Model Penerimaan Aplikasi MasjidLink Mulyanto, Agus; Sumarsono, Sumarsono; Niyartama, Thaqibul Fikri; Syaka, Annisa Khodista
Semesta Teknika Vol 23, No 1 (2020): MEI 2020
Publisher : Semesta Teknika

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MasjidLink is an Android-based application to provide news and information relating to mosques in the Yogyakarta Special Region. Behavioral aspects that influence tamir when using MasjidLink are need to measure, so that can define the level of acceptance. The TAM (Technology Acceptance Model) approach was used in this research to analyze factors of takmir acceptance towards MasjidLink. The measurement of acceptanceÂ towards MasjidLink with TAM is expected to showing the actual perspective of tamir so canÂ helps the further developing of this applications. Testing research instruments through validity and reliability. All research instruments have a value of more than 0.5 so that it can be declared as valid instruments. TAM variable in this study has an alpha cronbatch value of more than 0.7, so that all of these research variables are said to be reliable. Perceived ease of use has a percentage value 72.68% which states that mosque takmir agrees with the ease of use of the MasjidLink application. Perception of usefulness has a percentage 72.11% which states that the mosque takmir agrees with the usefulness of the MasjidLink application. Acceptance of the application has a percentage value 71.31% which states that the mosque takmir agrees with the acceptance of the MasjidLink application. The results of descriptive statistical analysis on TAM have the smallest percentage of variables, there is the percentage of MosqueLink acceptance with the value is 71.31%. This can be used to enhance the development of MasjidLink by focusing on the acceptance of the MasjidLink application.Â MasjidLink is an Android-based application to provide news and information relating to mosques in the Special Region of Yogyakarta. Currently, MasjidLink is a new mosque information management application that was launched and started to implemented by several takmir mosques in the Special Region of Yogyakarta. Takmir's acceptance of the MasjidLink application is one of the factors that support the continued use of the application. The measurement of the mosque takmir acceptance on the MasjidLink application is done by the TAM (Technology Acceptance Model) method. This study aims to evaluate the application of MasjidLink application with the TAM method so that the perception of takmir and the factors that influence takmir in using the application can be known. The research method used is a quantitative method, which uses a questionnaire as a tool to collect data on 125 users of the MasjidLink application. The results showed acceptance of mosque takmir on MasjidLink application had a positive influence on 3 TAM variables, namely the perception of user convenience 72.68%, perceived usefulness of 72.11%, and technology acceptance 71.31%. This shows that the application developer can focus on improving the acceptance of the MasjidLink application variable because the variable percentage is smaller than other variables.

Pemanfaatan Solar Cell Sebagai Sumber Energi Alternatif dan Media Pembelajaran Praktikum Siswa Di Pondok Pesantren “Nurul Iman” Sorogenen Timbulharjo, Sewon, Bantul, Yogyakarta Menuju Pondok Mandiri Energi Muchammad Abrori; Sugiyanto Sugiyanto; Thaqibul Fikri Niyartama
Jurnal Bakti Saintek: Jurnal Pengabdian Masyarakat Bidang Sains dan Teknologi Vol. 1 No. 1 (2017)
Publisher : Fakultas Sains dan Teknologi, UIN Sunan Kalijaga Yogyakarta

Salah satu usaha manusia dalam mengurangi pemanasan global atau penggunaan listrik PLN yang berbahan bakar fosil adalah dengan penggunaan sel surya. Pemasangan sel surya ini efektif karena wilayah Indonesia berada di daerah tropis. Penggunaan sel surya di Pondok Pesantren Nurul Iman sangat membantu karena kebutuhan energi listrik di Pondok Pesantren Nurul Iman sangat besar. Hal ini dapat dihitung dari biaya yang dikeluarkan per bulan oleh Pondok Pesantren Nurul Iman, pada bulan Agustus 2015 sebesar Rp. 1.372.100,-. Dengan audit energi dapat dikurangi beban yang digunakan sebesar 1.250 watt. Kalau penggunaan lampu rata-rata 12 jam listrik dapat dihemat sebesar Rp. 436.271,- per bulan. Penghematan lampu dengan surya sel yang dapat dilakukan sebesar Rp. 77.555,- per bulan. Lebih dari sepertiga yang dapat dikurangi biaya listriknya dengan sel surya.

PEMBELAJARAN FISIKA MENGGUNAKAN MODEL COOPERATIVE LEARNING DITINJAU DARI PRESTASI BELAJAR SISWA Siti Fatimah; Ika Kartika; Thaqibul Fikri Niyartama
Jurnal Kependidikan Vol. 42, No.1 (2012)
Publisher : Universitas Negeri Yogyakarta

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.21831/jk.v42i1.2226

Tujuan penelitian ini untuk mengetahui perbedaan dan tanggapan pembelajaran fisika dengan model Cooperative Learning tipe FSLC dan SGD pokok bahasan getaran dan gelombang terhadap prestasi belajar siswa kelas VIII. Metode penelitian yang digunakan adalah eksperimen. Populasi penelitian ini siswa MTs Plus Az-Zahro Cisumur Kabupaten Cilacap dengan penyampelan secara purposif. Instrumennya adalah tes, angket, observasi, dan dokumentasi. Data dianalisis dengan Anava Satu Jalur. Hasil penelitian menunjukkan bahwa (1) pembelajaran fisika dengan menggunakan model Cooperative Learning tipe FSLC berpengaruh secara signifikan terhadap prestasi belajar siswa. Pada ranah kognitif diperoleh Fhitung = 4,8 dengan F = 4,03. Pada ranah afektif diperoleh F = 7,35 dengan F tabel(5%)= 4,03. Pada ranah psikomotorik diperoleh F hitung = 13,04 dengan F hitung tabel(5%) = 4,03; (2) tanggapan siswa terhadap pembelajaran fisika yang menggunakan model Cooperative Learning tipe FSLC berkategori baik (83%) dan tanggapan siswa yang menggunakan tipe SGD berkategori cukup baik (77,5%).

PEMETAAN SEBARAN BATUAN PENYUSUN PAGAR CANDI DI SITUS CANDI LOSARI DUSUN LOSARI, DESA SALAM, KECAMATAN SALAM, KABUPATEN MAGELANG BERDASARKAN METODE MAGNETIK Novi Dwi Ariani; Thaqibul Fikri Niyartama; Nugroho Budi Wibowo
Berkala Arkeologi Vol 33 No 1 (2013)
Publisher : Balai Arkeologi Yogyakarta

Mapping geophysics research was conducted by geomagnetic method to know anomaly pattern of magnetic pole and to know distribution location and depth of temple gate composing stone in Losari Temple Site by using magnetic data. Data collection used Proton Precessions Magnetometer (PPM) G-856AX by area width of 88 km x 40 km and measurement space of 3 meter used looping method. Field data was corrected by daily variation and IGRF (International Geomagnetics Reference Field) correction and then reduction to pole. The slice modeling was conducted on local anomaly map on height of 6 meter. The result of the local magnetic field anomalies incision then interpolated to get an idea of the spread and depth of rocks making up the fence Losari temple. Local anomaly map shows that anomaly position lies in southwest, southeast, and northeast from main temple. Based from interpolated distribution of magnetic pole anomaly is dominated in depth of 2 meter to 4 meter.

PEMETAAN SEBARAN BATUAN PENYUSUN PAGAR CANDI DI SITUS CANDI LOSARI DUSUN LOSARI, DESA SALAM, KECAMATAN SALAM, KABUPATEN MAGELANG BERDASARKAN METODE MAGNETIK Novi Dwi Ariani; Thaqibul Fikri Niyartama; Nugroho Budi Wibowo
Berkala Arkeologi Vol. 33 No. 1 (2013)
Publisher : BRIN

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.30883/jba.v33i1.10

Mapping geophysics research was conducted by geomagnetic method to know anomaly pattern of magnetic pole and to know distribution location and depth of temple gate composing stone in Losari Temple Site by using magnetic data. Data collection used Proton Precessions Magnetometer (PPM) G-856AX by area width of 88 km x 40 km and measurement space of 3 meter used looping method. Field data was corrected by daily variation and IGRF (International Geomagnetics Reference Field) correction and then reduction to pole. The slice modeling was conducted on local anomaly map on height of 6 meter. The result of the local magnetic field anomalies incision then interpolated to get an idea of the spread and depth of rocks making up the fence Losari temple. Local anomaly map shows that anomaly position lies in southwest, southeast, and northeast from main temple. Based from interpolated distribution of magnetic pole anomaly is dominated in depth of 2 meter to 4 meter.

Analisis Zona Gerakan Tanah Menggunakan Metode Geolistrik Konfigurasi Wenner di Desa Gerbosari Kecamatan Samigaluh Nur Faqhina Mentari; Thaqibul Fikri Niyartama; Nugroho Budi Wibowo; Andi Andi
Wahana Fisika Vol 9, No 1 (2024): June
Publisher : Universitas Pendidikan Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.17509/wafi.v9i1.68570

Gerakan tanah di Desa Gerbosari berpotensi berdampak pada pemukiman dan fasilitas umum. Informasi mengenai litologi memiliki peran yang penting untuk mitigasi gerakan tanah yang akan terjadi. Penelitian ini bertujuan untuk mengetahui litologi dan zona gerakan tanah dengan metode geolistrik konfigurasi Wenner. Pengukuran geolistrik dilakukan sebanyak 7 lintasan pada zona berpotensi mengalami gerakan tanah. Panjang lintasan yang digunakan 300 m (5 lintasan), 260 m (1 lintasan) dan 240 m (1 lintasan). Pengolahan data menggunakan software Res2Dinv dan Surfer. Hasil pengolahan dari Res2Dinv berupa model penampang 2 dimensi yang menunjukkan nilai resistivitas daerah penelitian yaitu sebesar 0,481-636 Ωm. Daerah dengan zona rentan gerakan tanah yaitu pada resistivitas 0,481-151 Ωm (formasi Kebobutak) dan 0,481-8,52 Ωm (formasi Jonggarangan) yang diduga mengandung lempung dan batu pasir. Zona gerakan tanah tersebar hampir seluruh daerah penelitian, mulai dari kawasan penduduk hingga persawahan pada kedalaman 2,50-62,5 m. Land movement in Gerbosari Village has the potential to have an impact on settlements and public facilities. Information about lithology has an important role to mitigate soil movement that will occur. This study aims to determine the lithology and zone of ground movement with the Wenner configuration geoelectric method. Geoelectric measurements were carried out as many as 7 passes in the zone with the potential to experience ground movement. The track lengths used are 300 m (5 tracks), 260 m (1 track) and 240 m (1 track). Data processing using Res2Dinv and Surfer software. The processing results of Res2Dinv are in the form of a 2-dimensional cross-sectional model that shows the resistivity value of the research area, which is 0.481-636 Ωm. Areas with soil movement prone zones are at resistivities of 0.481-151 Ωm (Kebobutak formation) and 0.481-8.52 Ωm (Jonggarangan formation) which are thought to contain clay and sandstone. The soil movement zone is spread almost all over the study area, from populated areas to rice fields at a depth of 2.50-62.5 m.

Identification Lithology of Land Movement Zone using the Schlumberger Configuration Geoelectric Method in Samigaluh Distric Kulon Progo Septiana, Rena; Niyartama, Thaqibul Fikri; Wibowo, Nugroho Budi
JPSE (Journal of Physical Science and Engineering) Vol 9, No 1 (2024): JPSE (Journal of Physical Science and Engineering)
Publisher : Universitas Negeri Malang

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Samigaluh Subdistrict in Kulon Progo Regency, Yogyakarta, is prone to landslides. The objective of this study is to determine the subsurface lithology in the land movement zone. The research was conducted using the Schlumberger configuration geoelectric method. Measurements were carried out deploying six lines with line lengths ranging from 100 to 150 m. The results identified a vertical distribution of subsurface rock resistivity values to a depth of 74.05 m with a value of 0.06-13749.51 Ωm. The lithology consists of soil (14.18-361.23 Ωm), clay (0.06-42.73 Ωm), sandstone (0.35-123.44 Ωm), conglomerate (1372.7-10168.66 Ωm), and andesite 13749.51 Ωm. Damage to buildings and roads were found around the formation boundary where the damage is located in the Kebobutak formation.

Pemodelan Peak Ground Accleration (PGA) dan Intensitas Gempabumi berdasarkan Pengukuran Mikrotremor pada Kawasan Longsor di Desa Kalongan, Ungaran Timur Nugroho Budi Wibowo; Thaqibul Fikri Niyartama; Andi Andi; Rena Septiana; Erlina Widianingrum; Ahdian Azri Bustari; Iktifal Ajie Arif
Jurnal Fisika Unand Vol 13 No 2 (2024)
Publisher : Universitas Andalas

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25077/jfu.13.2.225-233.2024

The landslide in Kalongan Village affected an area of 5 hectares and has the potential to experience further landslides. Landslides can occur with triggers of external factors such as earthquakes. The Peak Ground Acceleration (PGA) parameter can represent the impacts that occur on the surface in the form of earthquake intensity (MMI). Kalongan Village is 25.5km from the epicenter of the Ambarawa earthquake on 27 May 2023. This study aims to modeling the PGA microzonation and the intensity of the Ambarawa earthquake in the avalanche zone in Kalongan Village. The PGA model is based on measurements of 72 microtremor data in the avalanche zone using the Kanai method. Parameters of the Ambarawa earthquake with a magnitude of 2.5 and a depth of 5 km. The results of PGA modeling in the avalanche zone varied between 1.0-7.1 gal or I-II MMI values. The results of the PGA modeling show that aftershocks can occur if the strength of the Ambarawa earthquake reaches M=4 or 7.1-50.8 gal. The strength of the earthquake is equivalent to the intensity of II-V MMI.

Lithological Interpretation of Landslide Zone of Arjuna Road Kalongan Village East Ungaran Use Geomagnetic Method Bustari, Ahdian Azri; Andi, Andi; Wibowo, Nugroho Budi; Niyartama, Thaqibul Fikri
POSITRON Vol 14, No 2 (2024): Vol. 14 No. 2 Edition
Publisher : Fakultas Matematika dan Ilmu Pengetahuan Alam, Univetsitas Tanjungpura

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.26418/positron.v14i2.75655

Arjuna Road in Kalongan Village, East Ungaran, which connects Semarang Regency with Demak Regency, has been cut off due to a landslide. Lithology as an internal controlling factor of landslide occurrence is important to be investigated. Research on the disaster has been conducted to determine the magnetic field anomaly and to interpret subsurface lithology using the geomagnetic method. The research was conducted on the landslide zone at Arjuna Road and its surrounding area using the geomagnetic method with looping data acquisition. The research area includes residential areas and plantation areas of residents with a research area of 1.3 Ã— 0.8 km2 with a total of 104 measurement points. Through the results and analysis of the research, it can be determined that the magnetic field anomalies in the research area range from 17.1 - 882.2 nT where the landslide zone dominantly has a high anomaly indicating the closer the area is to bedrock, and for residential areas and local plantations, the magnetic field anomalies vary from low to high depending on the topography and sediment thickness in the area. In addition, the subsurface lithology in the study area consists of clay soil, claystone, tuff, and volcanic breccia. The impermeable nature of the tuff and the water-low permeable clay soil causes the boundary between the clay soil and tuff layers to become slippery when water seepage occurs, resulting the landslides.

Pemodelan 3D Kawasan Longsor Berdasarkan Data Geolistrik Konfigurasi Schlumberger di Kecamatan Ungaran Timur Widyaningrum, Erlina; Niyartama, Thaqibul Fikri; Wibowo, Nugroho Budi; Andi, Andi
Jurnal Geosains dan Teknologi Vol 7, No 1 (2024): April 2024
Publisher : Universitas Diponegoro

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.14710/jgt.7.1.2024.29-35

Desa Kalongan merupakan daerah yang mengalami tanah longsor yang sangat ekstrim pada tahun 2022. Tanah longsor di desa ini terjadi di sekitar pemukiman warga sehingga sangat membahayakan apabila terjadinya longsor secara terus menerus. Salah satu faktor utama penyebab terjadinya tanah longsor yaitu bidang gelincir. Penelitian ini bertujuan untuk melakukan pemodelan 3D dan menganalisis bidang gelincir berdasarkan pemodelan 3D kawasan longsor sebagai penyebab terjadinya tanah longsor di Desa Kalongan. Daerah penelitian terletak di Desa Kalongan Kecamatan Ungaran Timur Kabupaten Semarang. Pengukuran geolistrik sebanyak 11 titik pengukuran dengan panjang lintasan bervariasi antara 120 m s.d. 300 m. Hasil pemodelan multilog 3D menunjukkan distribusi nilai dan susunan lapisan bawah permukaan berdasarkan nilai resistivitasnya. Hasil pemodelan stratigrafi menunjukkan tiga klasifikasi stratigrafi pada daerah penelitian yaitu batuan sedimen (material longsor) dengan nilai resistivitas 1,05 Ωm s.d. 659,16 Ωm, batuan sedimen (diduga sebagai bidang gelincir) dengan nilai resistivitas 0,31 Ωm s.d. 38,45 Ωm, dan batuan dasar dengan nilai resistivitas 469,96 Ωm s.d. 4.130,37 Ωm. Berdasarkan hasil pemodelan tersebut bidang gelincir berasal dari batuan sedimen dengan nilai resistivitas yang rendah yaitu 0,31 Ωm s.d. 38,45 Ωm yang diidentifikasikan sebagai batulempung dan dominan mengarah dari selatan menuju utara.

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