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Fahrudin Fahrudin
Program Studi Teknik Geologi, Fakultas Teknik, Universitas Diponegoro, Jl. Prof. Soedarto, SH, Kampus Undip Tembalang, Semarang 50275
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ETIKA PERGAULAN DALAM ALQURAN DAN IMPLIKASINYA TERHADAP PEMBELAJARAN PAI DI SEKOLAH Pranoto, Agus; Abdussalam, Aam; Fahrudin, Fahrudin
TARBAWY : Indonesian Journal of Islamic Education Vol 3, No 2 (2016): November 2016
Publisher : Universitas Pendidikan Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (450.278 KB) | DOI: 10.17509/t.v3i2.4514

Abstract

UPAYA GURU PENDIDIKAN AGAMA ISLAM DALAM MENINGKATKAN BUDAYA RELIGIUS DI SMPN 44 BANDUNG Fahrudin, Fahrudin; Firdaus, Endis; Shafiyullah, Alhadi
TARBAWY : Indonesian Journal of Islamic Education Vol 7, No 2 (2020): November 2020
Publisher : Universitas Pendidikan Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.17509/t.v7i2.26312

Abstract

Abstract. The role of the Islamic Religious Education teacher in learning is very important, especially in instilling students’ religious values. With the application of the religious culture of students in daily life at school, it will have a major influence on the attitudes and practice of students’ religious teachings in their daily life. In general, this study aims to describe the efforts of Islamic Education teachers in improving religious culture at SMPN 44 Bandung. Specifically, the purpose of this study is to describe the planning, implementation, constraints, and outcomes of the religious culture program at SMPN 44 Bandung. This research uses a qualitative approach with descriptive methods. The results of this study indicate that the PAI teacher in improving religious culture at SMPN 44 Bandung can be said to be quite successful, especially in changing the character or behavior of students. Abstrak. Peranan guru Pendidikan Agama Islam dalam pembelajaran sangat penting, khususnya dalam menanamkan nilai-nilai religius siswa. Dengan diterapkannya budaya religius siswa dalam kehidupan sehari-hari di sekolah akan besar pengaruhnya terhadap sikap dan pengamalan ajaran agama siswa dalam kehidupan sehari-hari. Secara umum penelitian ini bertujuan untuk mendeskripsikan upaya  guru PAI dalam meningkatkan budaya religius di SMPN 44 Bandung. Secara khusus tujuan penelitian ini adalah untuk mendeskripsikan  perencanaan, pelaksanaan, kendala, dan hasil dari program budaya religius di SMPN 44 Bandung. Penelitian ini menggunakan pendekatan kualitatif dengan metode deskriptif.  Hasil dari penelitian ini menunjukkan bahwa guru PAI dalam meningkatkan budaya religius di SMPN 44 Bandung ini bias dikatakan cukup berhasil, khususnya dalam merubah akhlak atau perilaku siswa yang sebelumnya kurang baik menjadi baik.  Kata kunci: Upaya Guru PAI, Budaya Religius, PAI di Sekolah
NILAI-NILAI PENDIDIKAN DALAM QS. AL MĀ’ŪN DAN IMPLIKASINYA TERHADAP PEMBELAJARAN PAI DI PERSEKOLAHAN (Studi Tafsīr tentang QS. al-Mā’ūn) Noviana, Nabila Fajrina; Abdussalam, Aam; Fahrudin, Fahrudin
TARBAWY : Indonesian Journal of Islamic Education Vol 3, No 1 (2016): May 2016
Publisher : Universitas Pendidikan Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (392.454 KB) | DOI: 10.17509/t.v3i1.3458

Abstract

KONSEP PENDIDIKAN ISLAM PERSPEKTIF MAHMUD YUNUS DAN IMPLIKASINYA TERHADAP PEMBELAJARAN PAI DI SEKOLAH Nurza, Ashfira; Rahmat, Munawar; Fahrudin, Fahrudin
TARBAWY : Indonesian Journal of Islamic Education Vol 5, No 2 (2018): November 2018
Publisher : Universitas Pendidikan Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (271.391 KB) | DOI: 10.17509/t.v5i2.16753

Abstract

This research aims to find the concept of education according to Mahmud Yunus and its implication to Islamic Religious Education at school. This research is library research by using qualitative-descriptive approach. Based on this research, it is known that Islamic Education goal according to Mahmud Yunus is to form noble character (akhlak mahmudah) of the students and they are experts in both general and religious sciences. Materials of Islamic Education in Mahmud Yunus’ view in geleral can be divided ito three: math, skill,and drawing. In specific, Mahmud Yunus divides materials of Islamic Education based on levels of education.Methods of Islamic Education to him are story telling, question-answer, discussion, modelling, accustoming, and speech. The last, evaluation of Islamic Education used are school examination, general examination, and modern examination. The concept of education according to Mahmud Yunus, in the researchers’ view has implication to the process of Islamic Religious Education insctruction at school, either in the goal, materials, method, or in the evaluation.Penelitian ini bertujuan untuk menemukan konsep pendidikan Islam perspektif Mahmud Yunus dan  implikasinya terhadap pembelajaran PAI di sekolah.Penelitian ini menggunakan metode penelitian deskriptif melalui pendekatan kualitatif dengan menggunakan teknik studi literatur. Berdasarkan hasil penelitian diketahui bahwa tujuan pendidikan Islam perspektif Mahmud Yunus adalah membentuk akhlak mulia peserta didik dan peserta didik dapat dihandalkan dalam ilmu umum dan ilmu agama.Materi pendidikan Islam perspektif Mahmud Yunus secara umum dibagi menjadi tiga yaitu matematika, keterampilan, dan melukis. Secara khusus Mahmud Yunus membagi materi Pendidikan Islam berdasarkan tingkat pendidikan.Metode pendidikan Islam yaitu metode kisah, metode tanya jawab, metode diskusi, metode teladan, metode pembiasaan dan metode ceramah. Evaluasi pendidikan Islam yang digunakan yaitu berupa ujian sekolah, ujian umum, dan ujian modern. Konsep pendidikan Islam perspektif Mahmud Yunus ini memiliki implikasi terhadap proses pembelajaran PAI di sekolah, baik pada tujuan pembelajaran, materi pembelajaran, metode pembelajaran, dan evaluasi pembelajaran.
ANALISIS FASIES DAN PERMODELAN SIKUEN STRATIGRAFI BATUAN KARBONAT LINTASAN KORIDO, FORMASI WAINUKENDI, KABUPATEN SUPIORI, PAPUA Joshua Shima; Hadi Nugroho; Fahrudin Fahrudin; Asep Kurnia Permana
Geological Engineering E-Journal Vol 6, No 1 (2014): Volume 6, Nomor 1, Tahun 2014
Publisher : Program Studi Teknik Geologi, Fakultas Teknik, Universitas Diponegoro

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Abstract

Korido is located in Supiori District , Papua , Indonesia . This area is in the north of the Central Range and included in the North Irian Basin which is the fore arc basin (Mc Adoo & J.C. Haebig, 1999). Own research area based on geology map created by Masria et al ( 1981) composed by Wainukendi Formation which is composed predominantly by carbonate sedimentary rocks .The purpose of this study is to determine the pattern of lithology and lithological boundaries were obtained from measured stratigraphy along the trajectory of research which is then integrated with the micro facies analysis and facies zone were obtained by petrographic analysis to determine the depositional environment and depositional processes that occur in Wainukendi Formation. More over, the relative age determination is also done based on the analysis of large benthic foraminifera so the deposition process can be integrated with relative age . The ultimate goal of this research is to integrate field data, micro facies analysis results and deposition process analysis results to create a model of sedimentation, determining stratigraphic marker, and the determines system tract that develops in Wainukendi Formation in the study area .The method used in this research is geological mapping focused on stratigraphy subjects in Korido area to get  lithostratigraphy sequence, platform type, sedimentation processes, and laboratory analysis include petrographic analysis to determine micro facies and facies zone and paleontological analysis to determine the relative age which then integrated to obtain stratigraphic marker and systems tract that develops in Wainukendi Formation. From the analysis of platform type showed the type of platform existing in this area is rimmed shelf type which is then used as a reference in micro facies analysis according to Wilson (1975) to obtain 4 facies zone that exist in this study area is reef platform margin , slope , toe of slope apron and deep shelf . Based on the analysis of the deposition process obtained 3 cycles of sedimentation that occurred from Wainukendi Formation . From the results of this analysis are used in determining the stratigraphic sequence to obtain stacking patterns that evolve based sequence boundary and its systems tract is composed of LST - TS - MFS - TST - HST so that obtain a full cycle changes in accommodation space and sediment supply where there is an increase in accommodation space which was offset by an increase in the supply of sediment in LST phase is characterized by progradation and agradation, an increase in the supply of sediment is lower than the increase in accomodation space in TST phase is characterized by retrogradation, and lastly, a decrease in accommodation space while sediment supply rate is still high in HST phase characterized by progradation.
PENGARUH SEEPAGE DAN KESTABILAN LERENG TERHADAP OPTIMALISASI GEOMETRI LERENG TAMBANG BUKIT M AIR LAYA BLOK TIMUR, UNIT PERTAMBANGAN TANJUNG ENIM Diana Ariana; Henarno Pudjihardjo; Fahrudin Fahrudin; Joko Tunggal
Geological Engineering E-Journal Vol 6, No 1 (2014): Volume 6, Nomor 1, Tahun 2014
Publisher : Program Studi Teknik Geologi, Fakultas Teknik, Universitas Diponegoro

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Abstract

Kestabilan lereng merupakan salah satu hal terpenting dalam proses eksploitasi tambang batubara. Diperlukan penyelidikan geoteknik dalam perancangan desain yang aman dan efektif sehingga penambangan batubara dapat dioptimalisasikan. Daerah penelitian dilakukan pada tambang Bukit M Air Laya Blok Timur Unit Pertambangan Tanjung Enim. Lokasi tambang ini berada disebelah barat sungai, penelitian ini dimaksudkan untuk mengetahui pengaruh pola aliran dan kestabilitan lereng dalam optimalisasi geometri lereng.Metode penelitian yang digunakan adalah dengan cara melakukan interpretasi data log bor  untuk mengetahui karakteristik tiap lapisan penyusun daerah tersebut meliputi data permeabilitas, kohesi, sudut geser serta bobot isi yang nantinya akan diolah menggunakan software Geoslope Seep/w dilakukan untuk mengetahui seberapa besar debit yang akan merembes dan Geoslope Slope/w dilakukan untuk mengetahui nilai faktor keamanan suatu lereng.Analisis rembesan terhadap kestabilan lereng dimodelkan dengan 2 penampang dengan jarak boundary tambang dari sungai yaitu 100m. Dua penampang memiliki elevasi tambang dibawah sungai Enim yaitu penampang C-C’ menghasilkan debit sebesar 3.186e-08 m3/s, penampang D-D’ menghasilkan debit sebesar 4.768e-08 m3/s. Analisa Slope/w dihasilkan Fk Penampang C-C’ = 1.754 (Stabil) Penampang D-D’= 2.509 (Stabil). Penampang E-E’ =2.310 (Stabil). Untuk desain pelebaran lereng /boundary tambang dilakukan pula analisa kelerengan pada lereng utara dan selatan sebanyak 3 penampang dihasilkan Fk penampang G-G’ memiliki FK 1.992 (U) dan 1.583 (S). penampang H-H’ 1.855 (S) dan penampang I-I’ 1.608 (U) dan 1.904 (S). Dari hasil kajian optimalisasi pelebaran dengan jarak 100 m dari Sungai Enim ke boundary tambang memiliki FK overall slope > 1.72 dengan pengaruh pola aliran dari sungai ke tambang maupun tambang ke sungai dikategorikan tidak terlalu besar sehingga pada daerah ini layak untuk diperlebar atau dioptimalkan.
EVALUASI GROUTING PADA SECTION RETAINING WALL – B (DOWNSTREAM) DI KALI SEMARANG, KELURAHAN PANGGUNG LOR, KOTA SEMARANG, JAWA TENGAH Khalaksita Amikani Asbella; Dwiyanto Joko Suprapto; Fahrudin Fahrudin; Citra Ningtyas
Geological Engineering E-Journal Vol 6, No 1 (2014): Volume 6, Nomor 1, Tahun 2014
Publisher : Program Studi Teknik Geologi, Fakultas Teknik, Universitas Diponegoro

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Abstract

Kali Semarang is one of the watering pattern that was in Semarang, Central Java, which runs from Pandanaran heading north toward the Java Sea. At the time of Semarang and surrounding areas have a condition that there are no rocks exposed at the surface because it is an area of older alluvium and river stage consisting of loose material such as clay, so this area has soft soil conditions until very soft. Lowering occurs in the area of construction of the embankment caused by the soft soil in the area around the construction of the embankment. Judging from the condition of the soil is soft and very soft, so we must be careful in determining the appropriate and correct methods for prevention of ground movement. Based on the soil conditions in the area of Kali Semarang, a study was undertaken using data SPT (Standard Penetration Test) to see the condition of the soil strength, and then to increase the strength of the soil used a method which is the method of grouting.From the results of drilling conducted at the Gate House point E1 +10 m, known at depth 0-2 m of sand sized loose gravel gray. At a depth of 2-20 m in the form of clay sized soft to very soft with gray. From SPT test data at Gate House point E1 +10 m, obtained N - SPT values <2 (very soft) at a depth of 2.8 to 5.8 m and a depth of 10.4 to 11.7 m. 2-3 N - SPT values (soft) is at a depth of 7.8 to 8.8 m and a depth of 13.4 to 19.3 m. SPT N - values (very dust) contained in an area close to the surface that is at a depth of 1.4 m.Once implemented method of grouting on Retaining Wall section B point 13 +1 m, +2 m point C10, and C18 +2 m point, a change in the value of the SPT test that the higher the value of N-SPT 4 (very dust) its value changed to 10 -15 (rather dense). N-SPT value of 0-1 (very soft), and the N-SPT values 2-3 (soft) turned into a N-SPT values 3-4 (soft), the value of N-SPT 5-7 (firm,) and N-SPT values 8-13 (stiff). To pile foundation bearing capacity changes from 16.57 tons to 35,98 tons to 53,03 tons. From the results of this investigation obtained good results for the purpose of grouting method successfully to increase the carrying capacity of the soil at the study site.Judging from its success with the implementation of the construction of grouting method can be resumed because the carrying capacity of the land has allowed it to withstand the load of the building to be erected.
REKONSTRUKSI STRUKTUR GEOLOGI DAERAH SUPIORI TIMUR – SELATAN, KABUPATEN SUPIORI, PULAU BIAK, PAPUA Fadlillah Rumanda; Wahju Krisna Hidajat; Fahrudin Fahrudin; Joko Wahyudiono
Geological Engineering E-Journal Vol 6, No 2 (2014): Wisuda Periode Juli - Oktober 2014
Publisher : Program Studi Teknik Geologi, Fakultas Teknik, Universitas Diponegoro

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Abstract

Papua and Papua New Guinea are had geology condition are very complex involving interaction between two plates, the Australian Plate and the Pacific Plate. New Guinea formed the result of the movement of oblique convergence (convergence oblique). The products of convergence are shrinkage and formed strike-slip structures and subduction which occur in Papua on 10 Ma. Sorendiweri Strait seen horizontal and vertical fault motion that separated the Biak Island and Supiori Island thar can be identified with the alignment on the satellite image.The purpose of this study was to determine the geological conditions in the study area, the pattern of structures, the main stress that formed the geological structure and reconstruct of geological structures in the study area. The Field research methods are field observation on Supiori track. Record the characteristics of the rock on each formation, measurement of geological structures such as bedding plane, joint and fault plane. Analysis methods such as analysis of alignment manually and visually interpreted on a satellite image DSM (Digital Surface Map). Stereographic analysis of geological structures, combining field data and analysis of alignment to determine the type of structure zone with rotated stress analysis and subsidiary structures method.Geological conditions consist of Oligocene clastic limestone Wainukendi Formation. and Miocene non-clastic limestones Wafordori Formation. Pattern geological structure on Wainukendi Formation., NE-SW normal faults, WSW-ENE strike-slip faults and NE-SW thrust fault. Wafordori Formation., NE-SW normal faults, NE-SW thrust fault. N-S trending major stress is the main primary stress, NE-SW and NW-SE sharpness trending are local stress. Reconstruction of geological structures of the study area began with N-S primary stress that formed E-W Maru reverse fault, NE-SW Soren sinisral fault and NW-SE Maruu, Yondonkir, Maryadori, Biniki dextral fault. The NE-SW trending secondary stress formed NW-SE Kepudari thrust fault, Yon reverse fault and Donkir reverse fault at south of the study area. 
ANALISIS SENSITIVITAS PEMODELAN ANALOG SANDBOX UNTUK MENGETAHUI PERKEMBANGAN STRUKTUR SESAR NAIK Dimas Asmarakandy; Dwiyanto Joko Suprapto; Fahrudin Fahrudin
Geological Engineering E-Journal Vol 6, No 2 (2014): Wisuda Periode Juli - Oktober 2014
Publisher : Program Studi Teknik Geologi, Fakultas Teknik, Universitas Diponegoro

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Abstract

Pemodelan sandbox adalah salah satu jenis pemodelan analog dalam ilmu geologi yang memiliki tujuan utama yaitu simulasi gaya, deformasi dan evolusi struktur cekungan sedimen. Terbentuknya struktur geologi berupa sesar naik (thrust atau backthrust fault) diakibatkan oleh sistem tektonik konvergen dan dapat dimodelkan dengan pemodelan sandbox. Penelitian ini bertujuan untuk memahami mekanisme dan sekuen deformasi dari sistem sesar naik dengan mengetahui hasil deformasi yang berupa pola struktur geologi; mempelajari perkembangan morfologi, pola dan distribusi struktur pada sistem tektonik konvergen; mengetahui variabel pengujian dalam pembentukan deformasi pada pemodelan sandbox. Penelitian dilakukan dari tahap persiapan hingga pelaksanaan. Persiapan yang dilakukan adalah pewarnaan, pengeringan dan pengayakan bahan model yaitu pasir kuarsa Formasi Ngrayong dengan dua macam ukuran butir; kategori ukuran pasir kasar (30-50 mesh) dan kategori ukuran pasir halus (60-80 mesh). Selanjutnya melakukan uji konsistensi alat sandbox. Hingga terakhir menentukan kondisi batas pemodelan seperti ukuran butir, ketebalan dan basement. Pada tahap pelaksanaan, data yang dihasilkan yaitu; foto/ gambar hasil pemodelan, waktu pergerakan dan jumlah sesar yang terbentuk, jarak pemendekan dan perubahan dip sesar, serta perkembangan morfologinya. Struktur yang terbentuk yaitu thrust dan backthrust fault. Morfologi yang terbentuk merupakan sabuk sesar thrust yang perkembangannya ditandai oleh terbentuknya struktur-struktur sesar baru. Jumlah sesar bertambah dan sudut kemiringan sesar pun cenderung bertambah seiring dengan meningkatnya pemendekan. Semakin tebal lapisan pasir maka jumlah sesar yang terbentuk lebih sedikit sebaliknya semakin tipis lapisan maka jumlah sesar yang terbentuk lebih banyak. Perbedaan ukuran butir material akan menghasilkan pola struktur dan jumlah sesar yang berbeda pula.
ANALISIS PROVENANCE, DIAGENESIS DAN LINGKUNGAN PENGENDAPAN SERTA PENGARUH TERHADAP KUALITAS RESERVOIR BATUPASIR FORMASI TALANG AKAR, SUMUR FA-21, CEKUNGAN JAWA BARAT UTARA Fahmi Abdillah; Hadi Nugroho; Fahrudin Fahrudin; Agus Priyantoro
Geological Engineering E-Journal Vol 6, No 2 (2014): Wisuda Periode Juli - Oktober 2014
Publisher : Program Studi Teknik Geologi, Fakultas Teknik, Universitas Diponegoro

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Abstract

The necessary of technology at this time resulted the necessary of energy resources will increasing, and it also result the scarcity of energy resources. One of the energy resources that is still used as a major energy resource is oil and gas. To overcome these problems, exploration activities at this time needs to be further improved. In the field of exploration, one of the most important things to know is reservoir. Reservoir quality is important for us to know so that we can determine whether an area has hydrocarbon potential to be developed or not. The main parameters of reservoir quality are porosity and permeability.In this study discussed the analysis of provenance, diagenetic and depositional environment of the sandstone reservoir of Talang Akar Formation, North West Java Basin and from the results of the analysis will be associated with the effect on reservoir quality. To determine the reservoir quality based on these parameters, can be done by several methods such as petrographic, cores, SEM and XRD analysis. From the analysis that has been done can be seen that the provenance of Talang Akar sandstone is Granite. So it can be seen that the Talang Akar sandstone which the provenance is Granite has good reservoir quality, with porosity values ranging from 19.04% to 24.28% and permeability ranging between 30-674 mD or belonging to the class good - very good (Koesoemadinata, 1980). Then the diagenetic process that occurs is compaction, cementation, replacement and dissolution. The process of compaction, cementation and replacement leads to reduced rock porosity values ranging from 2.25 to 11.5%, while the dissolution process resulting in increased rock porosity is about 1.5 - 2%. The depositional environment of the Talang Akar Sandstone is Upper Delta front. Rock facies in the upper delta front has good reservoir quality, with porosity values range from 19.04% to 24.28% and permeability range between 30-674 mD or belonging to the class is good - very good (Koesoemadinata, 1980). 
Co-Authors A'yun, Fatihatul A.A. Ketut Agung Cahyawan W Aam Abdussalam, Aam Abda Abda Abdul Bashith Abdul Qodir Abdullah, Sirajudin H. Abhitah, Athallah Nabiel Aceng Kosasih, Aceng Achmad Faqihuddin ACHMAD, IRFAN ZINAT Adi Pranata, Mohammad Sofyan aditya, Aditya Purnadani Afandy, Arief Rahman Afian, Nanang Nur Afifi, A. Nawawi Alfan Agung Wibowo Agus Fakhruddin Agus Priyantoro Ahmad Shofiyuddin Ichsan Ahmad Syamsu Rizal, Ahmad Syamsu Ahmad Syauqi Hidayatillah Ahyar Ahyar Ainul Yaqin, Ifandi, Ghazali, Aji, Fabian Ismu Alfaini, Ainul Yaqin Alfionita, Feni Almaliki, Muh. Alwi Amarullah, Moh. Amudin, Amudin Anter Venus Anton Anton Aras, Irianto Arif Alfiansyah Arif Alfiansyah Arifin, Agus Zainul Asep Kurnia Permana Asep Kurnia Permana Asih Priyati Asmawati Asmawati Asrianti, Nadia Putri Asrin Asrin Bakti, Arifin Aria Bakti, Lalu Arifin Aria Bambang Hari Kusumo Budhi Martana Bustan Choirunisa, Maria Choirunisa Citra Ningtyas Citra Ningtyas Dadi Setiadi Damora Rhakasywi David, Jerico Dewi Nur Asih Dian Safitri Diana Ariana Diana Ariana Diana Puspita Sari Dimas Asmarakandy Dimas Asmarakandy Diraharja, Rifat Satrio Dusturia, Nida Dwi Pramita, Riska Dwi Supriyanto, Muhammad Sofyan Dwiyanto Joko Suprapto Dwiyanto Joko Suprapto Dwiyanto Joko Suprapto Dyah Ika Rinawati Edi Suresman Efendi, Jauhari Ega Naufal, Hanif Endis Firdaus, Endis Erna Hernawati, Erna Erny Erny, Erny Fadlillah Rumanda Fadlillah Rumanda Fahmi Abdillah Fahmi Abdillah Fajar Islamy, Mohammad Rindu Fajriya, Siti Fakhrurrozi, Pupu Fakhrurrozi, Pupu Fathoni, Ilham Fauzi, Ade Fikri Fauzi, Muhammad Ihsan Fauziah, Arum Febriana, Indah Karima Febriana, Miftakhul Jannah Firdausi, Jinnani Fitri Wahyuni Fitri, Maulidatul Fitriyah Fitriyah Francisco, Jeremi Fuad Muhammad Fuzie Priatamphatie, Fuzie Garniwa, Nanang Ghazali, M. Ghufron, Moh Idil Gunawan, Rizaldi Chandra Gustiawati, Resty Hadi Nugroho Hadi Nugroho Hamdani, Moh. Ulil Absor Hamzah, Muhammad Fakhri Haqiqi, M. Deni Hendrayadi, Dedik Henry Binsar Hamonangan Sitorus Hery Heryanto Hidayaturrohman, Qisthi Alhazmi Hopiana, Nida Husnah, Dalilatul I Gusti Made Kusnarta Ifandi Ifandi Iman, M. Kamilul Imawan, Yuli Indra Kusuma Isnaini, Putri Lailatul Jaenuri Jaenuri Jamaluddin Majid jannah, lailatul Januar Aziz Zaenurrohman Jeinanda, Vidia Puti Joko Tunggal Joko Tunggal Joko Wahyudiono Joko Wahyudiono Joko Wahyudiono Joshua Shima Joshua Shima juwariyah, tatik Kafin, Achmad Kahfi, Nazih Sadatul Kallaba, Yulianti Khalaksita Amikani Asbella Khalaksita Amikani Asbella Khoiriyah, Binti Kiki Fatmala, Kiki Kosim, Mohammad Nanang Lalu Sukardi Lestari, Eka Dwi Lukmana, M. Arifudin Lukmana, Muhammad Arifudin M. Ridwan Hidayatulloh, M. Ridwan Mahardhika, Dhika Bayu Mahfudi, Mohammad Khoiri Mahrup Mahrup Mahrup, Mahrup Maman Abdurrahman Masruroh, Nuril MASYHUR, AHMAD Ma’ali, Izzul Mia Rhianti, Ghefira Mirasari, Titi Montreano, Donny Muhamad Ali Muhamad Parhan Muhammad Ridwan Muhammad Ridwan Hidayatulloh, Muhammad Ridwan Muhammad Roehil Amin, Ayatullah,, Mochammad Sofyan Dwi, Dimas Hidayatullah, Ghufron Shodiqin, Muhammad Sarjan Muhammad Subhan Muhammad Zaironi Muhlis, Nur Khozim Mukhammad Sofyan Rizka A Mulya, Viona Santi Mulyadi, Henki Desri Mulyana Abdullah Mulyana, Arif Mulyati Munawar Rahmat Mundzir, Ali Murad, Murad Muslih Muslih Mustari, Muhammad Muthi’ah, Nadia Nabila Fajrina Noviana, Nabila Fajrina Nabilatus Sa'adah, Rashika Narulita Santi Nasrulloh, Ilham Netriwati Novitasari, Ita Nur Cholis Nurhedi, Moh. Nurza, Ashfira Nurza, Ashfira Nurzati, Syarif Adhika Adhin Oktavitasari, Dini Padusug, Padusung Padusung Prabawanto, Sufiyani Pramono, Setio Pranoto, Agus Pranoto, Agus Prasetyo Hadi Prasetyo, Eko Andi Priyambudi, Gathot Pudjihardjo Henarno Putri Pratiwi, Metalis Putri, Fadila Rahmatika Qomariyah, Nurul Ulfa Rachman, Muhammad Nanda Fatur Ramadhan, Muh Syahru Ratnasari, Iis Rianda Dirkareshza Rica Rachmawati Ridha, Azhari Ali Rizal, Moh Syaiful Rizki Wahyu Yunian Putra Rizzasila Widiartha Rohmaniati, Baiq Siti Rolly Afrinaldi Romadhoni, Riyan Rusmawati Rusmawati, Rusmawati Sa'diyah, Iis Sari, Maula Sari, Retna Sarjan, M Sa’adah, Rashika Nabilatus Seandi Taroreh, Bangkit Selvia, Siska Ita Septin, Althearae Nira Septiyaningsih, Rina Shadiqul W , K Shafa, Naura Shafiyullah, Alhadi Shakila, Nur Asri Shodiqin, Ghufron Shofi, Ahmad SHOLIHIN, MOH. Sidiq, Abdullatif Sigit Pradana Siti Saniah, Siti Sitti Chaeriah Ahsan Soemeinaboedhy, I Nym Sri Wahyuni Sugiarto S Sukartono Sulasminingsih, Sri Sumarno, Ardawi Sunaika, Sunaika Sunarsih Sunarsih Sundussiyah, Sundussiyah Supriyadi Supriyadi Suryo, Taufik Hadi Susilowat, Lolita Endang Sutarya, Muhamad Farad Suwardji Syafei, Makhmud Syahruddin Hattab Syaifuddin, Ahcmad Syaiful Rizal Tajidan, Tajidan TATANG HIDAYAT, TATANG Taufik Hidayat Taupiqqurrahman Tedi Purbangkara Tengku Riza Zarzani N Tidar, Anisa Nava Tri Retnaningsih Soeprobowati Tri Winarno Tri Winarno Turmudi Ummi Kulsum Vydia Ridha Ariati Wafiqah, Wafiqah Wahju Krisna Hidajat Wahyuni, Tri Indah Warjono, Warjono Wawan Hermawan Wawan Hermawan Widya Kurniawan Yahya, M. Wildan Bin H.M. Zainal Abidin, Moh Ali Zainal Arifin Zainullah, M. Rizki Zuhdiyah Matienatul Iemaaniah