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All Journal Bulletin of Scientific Contribution : Geology IJOG : Indonesian Journal on Geoscience Journal of Geoscience, Engineering, Environment, and Technology Jurnal Geologi dan Sumberdaya Mineral (Journal of Geology and Mineral Resources) Buletin Sumber Daya Geologi Kumawula: Jurnal Pengabdian Kepada Masyarakat Eduvest - Journal of Universal Studies Journal of Geosciences and Applied Geology Geoid - Journal of Geodesy and Geomatics

Nana Sulaksana

Faculty of Technical Geology, Padjadjaran University, Jatinangor 45363

Author-ID : 390789

Aerospace Engineering Agriculture, Biological Sciences & Forestry Civil Engineering, Building, Construction & Architecture Computer Science & IT Decision Sciences, Operations Research & Management Earth & Planetary Sciences Economics, Econometrics & Finance Education Energy Engineering Environmental Science Health Professions Neuroscience Physics Social Sciences

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PROSPECTIVE ZONE AREA FOR AGRICULTURE AND RESIDENTIAL BASED ON GEOLOGICAL DISASTER POTENTIALS IN SOUTH BANDUNG REGION SULAKSANA, NANA; Isandarsyah, Teuku Yan Waliana Muda; Rifai, Achmad; Raditya Rendra, Pradnya Paramarta; Sulastri, Murni
Journal of Geological Sciences and Applied Geology Vol 3, No 1 (2019): Journal of Geological Sciences and Applied Geology
Publisher : Faculty of Geological Engineering, Universitas Padjadjaran

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.24198/gsag.v3i1.21366

The number of residents in Bandung continues to increase every year, especially in the southern part of Bandung. The development of residential areas needs to get attention from the local government and people in Bandung, especially to evaluate various geological hazards such as floods, landslide, earthquake, and other. Research methodolgy is qualitative method by interviewing local community and analyzing landsat image using Google Earth and Digital Earth Model (DEM) image to know land use in the research area. In addition, quantitative methods are also used with superimposed manual statistical analysis and weighting methods using Microsoft Excel, Global Mapper, and Mapinfo software. The result of research shows that South Bandung area has Land Suitability Score > 130 (Residential Area) and Land Suitability Score > 135 (Agriculture Area) which are categorized as very good settlement and education area; Land Suitability Score 116-130 (Residential Area) and Land Suitability Score 92-135 (Agriculture Area) are categorized as an obstacle area with various constraints such as water supply, disaster, and others but can still be overcome by artificial engineering. Land Suitability Score <116 (Residential Areas) and Land Suitability Score <92 (Agricultural Area) are limitation area that are not feasible to be used as residential and educational areas, a variety of constraint reduction efforts can be done but require very high cost. Therefore it is suggested to convert the area into conservation. It is concluded that the best areas to be used as residential and agricultural areas are located in the Banjaran District such as Banjaran, Kamasan, Sindangpanon, and Tarajusari Village.

GEOLOGY OF BUAHDUA AREA, SUMEDANG DISTRICT, WEST JAVA PROVINCE Raditya Rendra, Pradnya Paramarta; Sulaksana, Nana
Journal of Geological Sciences and Applied Geology Vol 3, No 3 (2019): Journal of Geological Sciences and Applied Geology
Publisher : Faculty of Geological Engineering, Universitas Padjadjaran

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.24198/gsag.v3i3.25731

Buahdua area is located in Sumedang District, West Java Province with coordinate 107°53’52,30” E - 107°59’18,83” E and 6°44’2,15” S - 6°38’38,39” S. This research aims to identify and characterize the geology of Buahdua area and its surrounding. This research used field observation, studio, and laboratory analysis method. Digital maps used to carried out processing step in studio and field tools such as geological hammer, camera, GPS, and compass used to carried out field observation. Rock samples are taken for laboratory analysis. Based on field observation, studio, and laboratory analysis, the research area can be divided into four morphology unit namely very gentle sloping hill, gentle sloping hill, rather steep hill, and steep hill morphology unit. Also, the research area has four drainage patterns namely anastomotic, subdendritic, subparalel, and subrectangular drainage pattern. The lithostratigraphic units in the research are can be divided into three units namely claystone (Tmbl), sandstone (Tmbpl), and volcanic breccia (Kbv) unit, and alluvium (Kal). The geological structures developed in the research area are shear joint and oblique fault (Cikandung and Kamal oblique fault). Geological history of the research area was started from middle Miocene (N9) when claystone unit was deposited in deep marine environment. In middle Miocene (N9 - N10), sandstone unit was deposited in deep marine environment. After those rock unit, there was tectonic activity in Pliocene - Plistocene caused geological structures, shear joint and oblique fault. Occurences volcanic activity after tectonic activity caused volcanic breccia unit was deposited. After those process, alluvium was deposited in Cikandung River until now.

GEOPLANOLOGY MODELING IN THE PLANNING AREA OF MAJALENGKA, WEST JAVA Nurohim, Dede; Princessca, Channia; Khoirullah, Nur; Sulaksana, Nana; Waliana, Teuku Yan
Journal of Geological Sciences and Applied Geology Vol 2, No 6 (2018): Journal of Geological Sciences and Applied Geology
Publisher : Faculty of Geological Engineering, Universitas Padjadjaran

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.24198/gsag.v2i6.20871

Based on the geological condition, the study area consisted of carbonate sandstone units (Tmbp), claystone units (Tml), non-carbonate sandstone units (Tpbp), andesitic intrusions (Ia), volcanic breccia units (Qbv), and alluvium (Qal) units. The different types of constituent rocks will affect the innate characteristics or properties of the rock. The regional genetic units explain kinship relations between lithology, morphology, and tectonics. It is used to determine the genetic processes that occur in an area which will later be developed into the smallest units in the geological analysis. In terms of spatial planning, the geological analysis is needed to produce an ideal area in terms of water adequacy, environmental carrying capacity, and disaster. In accordance with Law No. 11 of 2011 concerning the district development plan of Majalengka, then a layout plan emerged that would be applied to the area. Especially in the research area, land suitability covers a possible area that has a value of> 131, spread in the north to the west of the research area, with high to the very high land capability to be developed. The constrained area which has a value of 121-131 is spread in the north to south of the research area, with the ability of the land to be developed. And the limitation area has a value of <121 dominating in the northwest to the southeast of the research area, with low land capacity - very low to be developed. Based on the analysis, there are still some areas that are not in accordance with the pattern of development which should be mainly the development of protected areas.

MORPHOMETRY AND MORPHOTECTONIC OF CIANTEN AND CISAAT WATERSHED ON QUATERNARY VOLCANIC TERRAIN, GARUT, WEST JAVA Sipahutar, Sumahang R.; Sukiyah, Emi; Sulaksana, Nana
Journal of Geological Sciences and Applied Geology Vol 2, No 4 (2018): Journal of Geological Sciences and Applied Geology
Publisher : Faculty of Geological Engineering, Universitas Padjadjaran

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.24198/gsag.v4i2.18280

The research area is located in the Baluburlimbangan, Garut regency, West Java Province.Geographically, the research area is located at 107° 52' 23.32" E - 107° 59' 30.04" E and 6° 57'28.21" S - 7° 3' 39.23" S. Research object comprise Cianten and Cisaat watershed which will becompared based on morphometric and morphotectonic parameters. Observations carried outdirectly in the field and data analysis carried out in the studio. Research result shows that researcharea can be classified into medium – weak active tectonic area. It is proved by bifurcation ratio(Rb), drainage density (Dd), and sinuosity of mountain front (Smf). Active tectonic condition is alsoindicated by geology structure formed in research area such lineament of ridge and valley, anddrainage pattern.Keywords: Cianten, Cisaat, morphometry, morphotectonic, watershed

PEMBERDAYAAN POTENSI UMKM BIDANG KULINER PASCA PANDEMI COVID-19 DI DAERAH RANCAEKEK, KABUPATEN BANDUNG, JAWA BARAT Raditya Rendra, Pradnya Paramarta; Sulaksana, Nana; Sukiyah, Emi; Sulastri, Murni
Kumawula: Jurnal Pengabdian Kepada Masyarakat Vol 7, No 3 (2024): Kumawula: Jurnal Pengabdian Kepada Masyarakat
Publisher : Universitas Padjadjaran

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.24198/kumawula.v7i3.45956

Rancaekek merupakan salah satu wilayah penyangga Jatinangor yang saat ini merupakan kawasan pendidikan di Jawa Barat. Beberapa perguruan tinggi seperti Unpad, ITB, Ikopin, dan IPDN menjadikan UMKM berpotensi untuk bertambah di daerah Rancaekek. Saat terjadi pandemi Covid-19, banyak pelaku UMKM kuliner di Desa Rancaekek Kulon yang mengalami penurunan penjualan. Hal tersebut banyak diakibatkan oleh kurangnya pengetahuan mengenai pengembangan bisnis, strategi pemasaran, literasi digital, dan lainnya. Jika sebelumnya, para pelaku UMKM masih dihantui rasa khawatir saat pandemi maka di awal tahun 2023 adalah waktu yang tepat untuk mulai mengembangkan usaha. Oleh karena itu, kegiatan sosialisasi berkaitan dengan pemberdayaan UMKM dirasa perlu diadakan di daerah Rancaekek dengan pendekatan Participatory Rural Appraisal (PRA) modifikasi. Tujuannya agar para pelaku UMKM siap menghadapi kondisi pasar yang lebih dinamis pasca pandemi Covid-19. Kegiatan ini dilakukan melalui studi literatur data sekunder yang diperoleh dari pihak Desa Rancaekek Kulon, observasi lapangan dengan cara memetakan dan wawancara para pelaku UMKM kuliner di Desa Rancaekek Kulon, serta sosialisasi. Sosialisasi dilakukan sebagai bagian dari stimulus kepada pelaku UMKM kuliner untuk dapat mengembangkan ide kreasi dan inovasi disertai pemahaman mengenai literasi digital sebagai salah satu hal penting menghadapi era digital saat ini. Kegiatan ini diharapkan dapat bermanfaat bagi masyarakat pelaku UMKM kuliner untuk dapat terus mengembangkan usahanya dengan bantuan dan pendampingan dari pihak seperti mitra usaha, para akademisi, serta pemerintah daerah setempat agar roda perekonomian semakin baik dan berdampak baik bagi masyarakat setempat.

HUBUNGAN ANTARA INDEKS GRADIEN PANJANG SUNGAI DAN HIPSOMETRI PADA RESPON MORFOTEKTONIK DI CEKUNGAN BANDUNG BAGIAN TIMUR Rendra, Pradnya Paramarta Raditya; Sukiyah, Emi; Hadian, Mohamad Sapari Dwi; Daliman, Shaparas Binti; Sulaksana, Nana
Bulletin of Scientific Contribution: GEOLOGY Vol 22, No 3 (2024): Bulletin of Scientific Contribution : GEOLOGY
Publisher : Fakultas Teknik Geologi Universitas Padjadjaran

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.24198/bsc geology.v22i3.56414

Penelitian dilakukan di Cekungan Bandung bagian timur yang secara geologi tersusun oleh dominasi batuan vulkanik berumur Kuarter. Penelitian ini bertujuan untuk mengungkap hubungan antar aspek morfotektonik yang terdiri dari indeks gradien panjang sungai (SL) dan hipsometri (HI) dalam merespon aktivitas tektonik di daerah penelitian. Penelitian dilakukan menggunakan media citra DEM (Digital Elevation Model) melalui dukungan SIG (Sistem Informasi Geografis) di studio. Perangkat lunak ArcGIS 10.0 digunakan dalam proses pengolahan citra serta Microsoft Excel digunakan dalam proses perhitungan dan analisis data. Berdasarkan hasil penelitian, daerah penelitian terdiri dari enam DAS, yaitu DAS Citarik Hulu, Cijalupang, Ciwirama, Ciburial, Cikeruh, dan Cimande yang sebagian besar berada pada morfologi perbukitan dan gunung hingga pedataran dengan kemiringan lereng mulai dari sangat curam hingga datar. Daerah penelitian memiliki enam pola pengaliran sungai, yaitu pola radial, subradial, subdendritik, parallel, subparallel, dan anastomotik. Secara umum, keenam pola pengaliran tersebut menunjukkan bahwa daerah penelitian didominasi area berlereng curam hingga sangat curam dan tersusun oleh batuan vulkanik di bagian utara, timur, dan selatan, berlereng landai hingga datar dan tersusun oleh material lepasan di bagian tengah hingga barat, serta dipengaruhi struktur geologi minor. Hal ini dibuktikan dari hasil perhitungan nilai SL (113,24 – 409,75) dan HI (0,22 – 0,50) yang menunjukkan respon aktivitas tektonik rendah hingga cukup tinggi. Selain itu, korelasi nilai SL dan HI menunjukkan tingkat hubungan sangat kuat yang tercermin dari koefisien korelasi (r) = 0,932, yaitu semakin besar nilai SL maka semakin besar pula nilai HI.

OPTIMALISASI PEMANFAATAN SISTEM AGROFORESTRI SEBAGAI BENTUK ADAPTASI DAN MITIGASI TANAH LONGSOR Rendra, Pradnya Raditya; Sulaksana, Nana; Alam, Boy Yoseph C.S.S.S.
Bulletin of Scientific Contribution Vol 14, No 2 (2016): Bulletin of Scientific Contribution
Publisher : Fakultas Teknik Geologi Universitas Padjadjaran

Landslide is a natural disaster that often occur in Indonesia and cause a significant impact. Landslide may occur due to static factor (slope) and dynamic factor (land use). Landslide mitigation can be done to prevent the negative impact of landslide. Landslide mitigation through slope stabilization can be done with vegetative technique. Vegetative technique as a landslide mitigation with sustainable land production is also known as agroforestry. Agroforestry is a land use systems made by various technologies through the utilization of annual crops, perennial crops, and/or livestock , either alternately or at the same time in a certain period to form ecological, social, and economic interactions. Agroforestry system has more advantages than other land use systems. One of the advantage of this system is can be used on steep slope area. Multistory agroforestry system can prevent landslide by forming soil organic material, improving soil structure, and making soil more stable. Utilization of multistory agroforestry system with various types of storied canopy trees considered as appropiate landslide mitigation because the closure of canopy tress are tightly and stratified, their root system is excellent, and the soil cover such as grasses and shrubs is important to prevent landslide. Furthermore, agroforestry system can also be used to produce food crops, fodder, honey, building materials, and medicinal materials. Keyword : Agroforestry, mitigation, slope, landslide. Tanah longsor merupakan bencana alam yang sering terjadi di Indonesia dan menimbulkan dampak cukup besar. Tanah longsor dapat terjadi akibat faktor statis (kemiringan lereng) dan faktor dinamis (tata guna lahan). Mitigasi tanah longsor dilakukan untuk mencegah dampak negatif tanah longsor. Mitigasi tanah longsor melalui stabilisasi lereng dapat dilakukan dengan rekayasa vegetatif. Rekayasa vegetatif sebagai mitigasi tanah longsor dengan produksi lahan berkelanjutan tersebut disebut juga sebagai sistem agroforestri. Agroforestri merupakan sistem penggunaan lahan yang dilakukan dengan berbagai teknologi melalui pemanfaatan tanaman semusim, tanaman tahunan, dan/atau ternak dalam waktu bersamaan atau bergiliran pada periode tertentu sehingga terbentuk interaksi ekologi, sosial, dan ekonomi. Sistem agroforestri memiliki lebih banyak kelebihan dibandingkan sistem penggunaan lahan lain. Salah satu kelebihan sistem ini adalah dapat digunakan pada lahan berlereng curam. Sistem agroforestri multistrata dapat mencegah tanah longsor dengan membentuk bahan organik tanah, memperbaiki struktur tanah, dan membuat tanah menjadi lebih stabil. Pemanfaatan sistem agroforestri multistrata dengan berbagai jenis tanaman tajuk bertingkat dinilai sebagai langkah tepat mitigasi tanah longsor karena adanya penutupan tajuk pepohonan yang rapat dan bertingkat, sistem perakaran yang sangat baik, serta penutup tanah berupa rerumputan dan semak belukar yang sangat penting untuk menghindari tanah longsor. Selain itu, sistem agroforestri juga dapat dimanfaatkan sebagai penghasil bahan pangan, pakan ternak, madu, bahan bangunan, dan bahan obat. Kata kunci :Agroforestri, mitigasi, lereng, longsor.

PERAN ASPEK GEOMORFOLOGI DALAM MENENTUKAN KARAKTERISTIK ENDAPAN DEBRIS AVALENCHES GUNUNG PAPANDAYAN, GARUT, JAWA BARAT Nursalim, Asep; Sulaksana, Nana; Sukiyah, Emi
Bulletin of Scientific Contribution Vol 14, No 1 (2016): Bulletin of Scientific Contribution
Publisher : Fakultas Teknik Geologi Universitas Padjadjaran

Studies in this research are the characteristics of one of material deposits from the volcanoes eruption. Volcanic activity in Indonesia is a natural phenomenon that can occur at any time. Both material losses and loss of life will always happen at any moment in particular that deal directly with the volcano. The volcanic activity was resulted is deposition of debris avalanches. The study was conducted deposition of debris avalanches in complex of Papandayan volcanoes, Garut, West Java.In this study conducted by the interpretation of high resolution image data , and morphometry sub watershed for the morphologic aspects. The study was conducted to compare the deposited of debris avalanches from the eruption in 1772 and the eruption of 2002. Descriptive analysis of physical properties indicate a difference in both the materials. Deposition of debris avalanches in 1772 showed that sediment material is dominated by the matrix with widespread distribution . While the deposition of debris avalanches in 2002 are dominant fragment sizes and larger components and distribution concentrated in the upper reaches of the river that flows into the Cimanuk river. Both of debris avalanches are absent a scoria, pumice and large juveniles, which is one parameter of explosive. Analysis of watershed morphometry showed different drainage densities in both materials, which is conducted to determine the resistance response of rocks whereas deposited debris avalanches. Keywords : Eruption, Debris avalanches, G. Papandayan. Studi dalam penelitian ini mengenai karakteristik salah satu endapan material hasil erupsi gunung api. Aktifitas gunung api di Indonesia merupakan salah satu fenomena alam yang dapat terjadi setiap saat. Kerugian baik materi maupun korban jiwa akan selalu terjadi setiap saat di khususnya yang berhadapan langsung dengan gunung api tersebut. Salah satu hasil dari aktifitas gunung api tersebut menghasilkan endapan debris avalanches. Penelitian endapan debris avalanches ini dilakukan di komplek Gunung api Papandayan, Kabupaten Garut, Jawa Barat.Dalam penelitian ini dilakukan dengan cara interpretasi data citra resolusi tinggi, dan morfometri sub DAS untuk aspek morfologinya. Penelitian dilakukan untuk membandingkan endapan debris avalanches hasil erupsi tahun 1772 dan erupsi tahun 2002. Hasil analisis deskriptif sifat fisik menunjukkan adanya perbedaan kedua endapan tersebut. Endapan debris avalanches tahun 1772 menunjukkan material endapan yang didominasi oleh matrik dengan penyebaran yang luas. Sedangkan endapan debris avalanches tahun 2002 dominan ukuran fragmen dan komponen yang besar dan penyebarannya terkonsentrasi di hulu sungai yang mengalir ke sungai Cimanuk. Kedua endapan tidak ditemukan pumis dan skoria serta juvenil yang besar yang merupakan salah satu parameter eruspsi eksplosif. Dari analisis morfometri daerah aliran sungai memperlihatkan kerapatan pengaliran yang berbeda di kedua endapan, yang dilakukan untuk mengetahui respon resistensi batuan dimana endapan debris avalanches diendapkan. Kata kunci : Erupsi, Debris avalanches, G. Papandayan.

VALUASI BAHAN GALIAN GOLONGAN C (BGGC) DI KABUPATEN CIREBON DITINJAU DARI PENGELOLAAN DAN INVESTASI Sulaksana, Nana
Bulletin of Scientific Contribution Vol 4, No 1 (2006): Bulletin of Scientific Contribution
Publisher : Fakultas Teknik Geologi Universitas Padjadjaran

In order to optimize the ability of mineral resources which are utilized to give people a more prosperous life, we need not only an adequate mining management which is appropriate with the characteristic of the mineral resources but also a stocktaking of the existence of the mineral resources in a form of map information which is included in a work identification and a mapping of mineral potencies. Exploiting the mineral resources optimally by maximizing added values and minimizing negative impacts of mineral resources exploitation, will increase the PAD (Original Local income) and labour absorption. Therefore, research continuity is essential to create in order to collect the basic information of the mineral potencies, especially constructive and industrial deposits, hopefully it will be able to support the exploitation activity. Work identification and mapping of a mineral potency represents the most basic need now, considering that Cirebon Regency has to be ready to implement the Local Autonomy based on the constitution number 22 Year 1999st, especially in a mining field. The result of the work identification will become a basic and main force for the Mining and Energy Department in Cirebon Regency in order to promote its natural resources and to accelerate duties on mine workings building and supervision.

PERAN CITRA SATELIT LANDSAT 8 DALAM IDENTIFIKASI TATA GUNA LAHAN DI WILAYAH KABUPATEN SUMEDANG RADITYA RENDRA, PRADNYA PARAMARTA; Sulaksana, Nana; Alam, Boy Yoseph C. S. S. S
Bulletin of Scientific Contribution Vol 17, No 2 (2019): Bulletin of Scientific Contribution : GEOLOGY
Publisher : Fakultas Teknik Geologi Universitas Padjadjaran

Kegiatan penelitian dilakukan di Kabupaten Sumedang yang memiliki keragaman jenis tata guna lahan. Penelitian ini dilakukan untuk mengetahui peran citra satelit Landsat 8 dalam mengungkap jenis tata guna lahan di daerah penelitian. Penelitian ini dilakukan melalui analisis citra Landsat 8 dengan dukungan Sistem Informasi Geografis di studio dan observasi ke lapangan untuk mengecek langsung jenis tata guna lahan di daerah penelitian. Perangkat lunak ArcGIS 10.0 dengan Sistem Informasi Geografis digunakan untuk mengolah dan menganalisis citra satelit Landsat 8. Berdasarkan hasil penelitian, daerah penelitian dapat dibedakan menjadi 4 kawasan, yaitu kawasan pemukiman, hutan, budidaya (ladang, kebun, dan sebagainya), serta perairan dan lahan basah (sawah). Kawasan pemukiman terkonsentrasi di daerah berkembang seperti Jatinangor, Tanjungsari, Sumedang Selatan, dan Sumedang Utara. Kawasan hutan tersebar di beberapa daerah namun sebagian besar berada di bagian selatan daerah penelitian. Kawasan budidaya dan lahan basah seperti sawah sebagian besar merupakan hasil konversi lahan kawasan hutan sehingga letaknya berdekatan dengan kawasan hutan. Kata kunci : ArcGIS, citra Landsat 8, Sistem Informasi Geografis, Sumedang, tata guna lahan

Co-Authors A. Sudradjat ACHMAD RIFAI Achmad Sjafrudin, Achmad Adjat Sudrajat Alam, Boy Yoseph C. S. S. S Andi Makawaru Yasin, Andi Makawaru Ando, Ferry Andriana Sendjaja, Yoga Asep Nursalim, Asep Bombom Rachmat Suganda, Bombom Rachmat Boy Yoseph C.S.S.S. Alam, Boy Yoseph C.S.S.S. Brilian, Ciria Humanis Burhanidunnur, Muhammad Daliman, Shaparas Binti Dewandra Bagus Eka Putra, Dewandra Bagus Eka Dicky Muslim Dudi Nasrudin Usman Emi Sukiyah Euis Tintin Yuningsih Febri Hirnawan Fikri Abdulah, Fikri G. Hartono Gentana, Dewi Hendarmawan Hendarmawan, Hendarmawan HS, Karyono Ildrem Syafri Indrakususma, Riko Ardiansyah Isandarsyah, Teuku Yan Waliana Muda Iskandarsyah, Teuku Y. M. W. Iskandarsyah, Teuku Yan Waliana Muda Iyan Haryanto, Iyan Jamal Jamal Johanes Hutabarat Kamaruddin, Hashari Khoirullah, Nur M. Nursiyam Barkah, M. Nursiyam Mega Fatimah Rosana Mohamad Sapari Hadian Muhammad Kurniawan Alfadli Muttaqin, Mochamad Aufar Novi Triany Nurasa , Heru Nurohim, Dede Nursahan, Iwan Oscar, Agus W Persulessy, Janeth Angel Pradnya P. Raditya, Pradnya P. Pradnya Paramarta Raditya Rendra Pradnya Raditya Rendra, Pradnya Raditya Princessca, Channia Puguh Setiyanto, Puguh Rendra, P Paramarta Raditya Rita Yulianti, Rita Setyorini, Dyah Ayu Sipahutar, Sumahang R. Sri Wahyuni Suherman Dwi Nuryana Sulastri, Murni Syamsul Irham, Syamsul T Yan Waliana, T Yan Trisnadiansyah, Mochamad Ridfan Vijaya Isnaniawardhani Waliana, Teuku Yan Yudhi Listiawan Yuniarti Yuskar, Yuniarti Zufialdi Zakaria, Zufialdi

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