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All Journal Jurnal Ilmu dan Teknologi Kelautan Tropis Maspari Journal Jurnal Akuatika Maspari Journal Jurnal Kelautan : Indonesian Journal of Marine Science and Technology Forum Geografi Pedagogia: Jurnal Pendidikan JURNAL ILMIAH GEOMATIKA MAJALAH ILMIAH GLOBE Sumatra Journal of Disaster, Geography and Geography Education Jurnal Geografi JURNAL BUANA Jurnal Kelautan Nasional Jurnal Segara Spatial : Wahana Komunikasi dan Informasi Geografi Science and Environmental Journals for Postgraduate Jurnal Kependudukan dan Pembangunan Lingkungan (JKPL) Jurnal Buana

Aprizon Putra

Universitas Negeri Padang

Author-ID : 487752

Agriculture, Biological Sciences & Forestry Humanities Biochemistry, Genetics & Molecular Biology Civil Engineering, Building, Construction & Architecture Decision Sciences, Operations Research & Management Earth & Planetary Sciences Education Environmental Science Immunology & microbiology Library & Information Science Materials Science & Nanotechnology Mathematics Public Health Social Sciences Other

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KARAKTERISTIK ARUS LAUT PERAIRAN TELUK BENOA â BALI Tanto, Try Al; Wisha, Ulung Jantama; Kusumah, Gunardi; Pranowo, Widodo S.; Husrin, Semeidi; Ilham, Ilham; Putra, Aprizon
GEOMATIKA Vol 23, No 1 (2017)
Publisher : Badan Informasi Geospasial in Partnership with MAPIN

ABSTRAKPerairan Teluk Benoa merupakan kawasan semi tertutup dengan mulut sempit yang memisahkan antara Pulau Serangan dan Tanjung Benoa. Arus laut perairan Teluk Benoa, yang dekat pantai berperan penting dalam proses transpor sedimen di daerah pantai yang merupakan daerah gelombang mulai pecah hingga ke arah garis pantai. Tujuan penelitian adalah mengetahui karakteristik arus laut yang terjadi, analisis dari penyajian secara scatter plot dan stic plot, sehingga diketahui faktor dominan pembangkit arus tersebut. Data arus laut diperoleh dari hasil pengukuran pihak swasta menggunakan alat ukur ADCP. Analisis arus laut dengan scatter dan stic plot untuk melihat arah dominan arus, serta melihat hubungan kejadian arus dengan pasang surut air laut, selain itu juga dengan perhitungan kisaran kecepatan arus yang terjadi selama pengukuran. Hasil yang diperoleh adalah arus laut di perairan Teluk Benoa berkisar antara 0,001 - 1,715 m/s (pengamatan bulan Juni - Juli 2015). Kecepatan arus pada mulut teluk lebih besar (maksimal sebesar 1,715 m/s), sedangkan di dalam teluk kecepatan arus lebih rendah (maksimal sebesar 0,883 m/s). Pada saat air pasang, arah arus dominan ke arah dalam teluk dan saat air laut surut arah dominan arus ke arah luar teluk. Kesimpulan yang diperoleh adalah kejadian arus laut di perairan Teluk Benoa lebih dominan berupa arus pasang surut. Saat kondisi bulan purnama kecepatan arus lebih tinggi dari pada saat posisi bulan separuh (kuarter pertama atau ketiga). Pada umumnya, pada mulut teluk memiliki arus yang cukup tinggi sebagai akibat celah sempit, dengan pola yang tidak beraturan akibat pengaruh perlintasan kapal dan aktivitas keluar masuk teluk.Kata kunci: arus laut, karakteristik arus laut, arus pasang surut, Teluk BenoaABSTRACTBenoa Bay waters is a semi-enclosed area with quite a narrow mouth that separates the Serangan Island and Tanjung Benoa. Ocean currents in Benoa Bay, which is close to the beach plays an important role in the process of sediment transport in the beach area where is the waves began to break up towards the shoreline. The research objective was to know the characteristics of ocean currents that occur, from the analysis of the scatter and stic plot, so itâs known that the dominant factor of the current generator. The data of ocean currents obtained from the measurement of private parties using ADCP measuring instrument. Analysis of ocean currents with scatter and stic plot to see the dominant direction of current, and to see the relationship of current occurrence with the tide, besides also with calculation of current velocity. The results obtained are ocean currents in the Benoa Bay waters ranged from 0,001 to 1,715 m/s (observations in June-July 2015). Flow velocity at the mouth of the bay is greater (maximum of 1,715 m/s), while in the lower bay flow speed (maximum of 0,883 m/s). At high tide, the dominant current direction towards the bay and vice versa during low tide predominant direction of flow towards the outside of the bay. The conclusion is the incidence of ocean currents in the Benoa Bay waters is predominantly influenced by the tidal current. When the full moon conditions the current velocity is higher than at half month position. In general, at the mouth of the bay has a current high enough as a result of the narrow gap, with irregular pattern due to the influence and activities of ship crossings in and out of the bay.Keywords: ocean current, characteristics of ocean current, tidal current, Benoa Bay

PENDEKATAN METODE NORMALIZED DIFFERENCE VEGETATION INDEX (NDVI) DAN LYZENGA UNTUK PEMETAAN SEBARAN EKOSISTEM PERAIRAN DI KAWASAN PESISIR TELUK BENOA, BALI Putra, Aprizon
GEOMATIKA Vol 23, No 2 (2017)
Publisher : Badan Informasi Geospasial in Partnership with MAPIN

Perubahan secara spasial pada ekosistem pesisir yang terjadi di kawasan pesisir Teluk Benoa Bali seperti tutupan mangrove telah berubah menjadi lahan untuk tambak, pelabuhan, permukiman, pembangunan tol laut serta reklamasi pulau. Dimana perubahan tutupan lahan berdampak pada ekosistem pesisir, hal tersebut menyebabkan terjadinya degradasi lingkungan seperti sedimentasi, intrusi air laut dan banjir pasang. Penelitian ini bertujuan untuk mengetahui perubahan sebaran ekosistem pesisir seperti mangrove dan terumbu karang menggunakan citra Spot-6 tahun 2006, 2012 dan 2015 serta citra Landsat 7+ETM tahun 1997. Metode untuk laju perubahan didapat dari analisis secara overlay menggunakan Sistem Informasi Geografis (SIG). Dimana untuk perubahan sebaran mangrove yaitu dengan membedakan objek mangrove dengan non mangrove dengan analisis Normalized Difference Vegetation Index (NDVI), sedangkan perubahan sebaran terumbu karang yaitu dengan persamaan algoritma Lyzenga untuk ekstraksi informasi dasar perairan. Pemetaan ekosistem pesisir di kawasan Teluk Benoa dengan memanfaatkan citra resolusi tinggi Spot-6 dan di dukung dengan citra Landsat 7+ETM sangat membantu memberikan kenampakan mencakup wilayah lebih luas dibandingkan dengan pengamatan langsung di lapangan. Adapun hasil analisis perubahan sebaran mangrove yaitu: 1) tahun 2006 ke tahun 2012 dengan perubahan -89,98 ha; dan 2) tahun 2012 ke tahun 2015 dengan perubahan -60,62 ha. Sedangkan perubahan kondisi terumbu karang yaitu: 1) tahun 1997 ke tahun 2006 dengan perubahan -69,07 ha; 2) tahun 2006 ke tahun 2012 dengan perubahan -90,51 ha; dan 3) tahun 2012 ke tahun 2015 dengan perubahan 112,47 ha. Sebaran terumbu karang dominan berada di luar Teluk Benoa.

Spatial Analysis of the River Line and Land Cover Changes in the Kampar River Estuary: The Influence of the Bono Tidal Bore Phenomenon Putra, Aprizon; Wisha, Ulung Jantama; Kusumah, Gunardi
Forum Geografi Vol 31, No 2 (2017): December 2017
Publisher : Universitas Muhammadiyah Surakarta

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.23917/forgeo.v31i2.5290

The Kampar River estuary is well known for a tidal-bore phenomenon called âBono wavesâ. The emergence of Bono waves has a significant influence on the estuary system of Kampar River. Scoured materials, resulting from the hydraulic jump of the tidal bore, are carried into the middle of the river. These materials are then deposited when the velocity of the river decreases as a result of the collision of the tidal current from the sea and the river flow. The aim of this was to determine the area of erosion and sedimentation with respect to the river line and perform land-cover change analysis for the area around the Kampar River estuary for the years of 1990, 2007, 2010 and 2016. The method employed was the supervised maximum likelihood (SML) classifications, which uses an overlay technique to yield alternate information on the river line and land-cover changes in the form of time-series data. The largest erosion occurred during 1990â2007, for which the average change reached 2.36 ha/year. The smallest erosion occurred during 2010â2016, when the change reached 0.41 ha/year. The largest land-cover change was found during 1990â2016, which occurred in the land for agriculture/plantations (11.57 ha/year), building/settlement (48.11 ha/year) and scrubland (30.88 ha/year). The other types of land cover, such as bare land and sediment deposition, varied every single year. The changes to the river line are caused by land-cover changes, and the Bono waves that lead to erosion and sedimentation that is not stable in the middle of the river and downstream.

KESESUAIAN EKOWISATA DI PULAU PASUMPAHAN, KOTA PADANG Tanto, Try Al; Putra, Aprizon; Yulianda, Fredinan
MAJALAH ILMIAH GLOBE Vol 19, No 2 (2017)
Publisher : Badan Informasi Geospasial

ABSTRAKPulau Pasumpahan terletak di Kecamatan Bungus Teluk Kabung, Kota Padang merupakan salah satu tempat tujuan wisata kepulauan. Tujuan penelitian ini yaitu menginventarisasi potensi sumber daya pesisir dan mengkaji kesesuaian kawasan dalam mendukung ekowisata Pulau Pasumpahan. Metode yang digunakan dalam kajian berupa pemetaan dan analisis kesesuaian kawasan ekowisata yang dilakukan dengan perhitungan skor dan bobot parameter yang digunakan. Hasil yang diperoleh adalah indeks kesesuaian ekowisata tertinggi terdapat pada potensi wisata pantai (rekreasi) yaitu sebesar 79,91% (sangat sesuai). Dari 9 sampel pengukuran yang tersebar di sekeliling pulau, 8 di antaranya menunjukkan nilai sangat sesuai, hanya satu titik yang menunjukkan sesuai bersyarat karena banyak sampah bertebaran di pantai dan perairan keruh. Untuk kesesuaian wisata snorkeling sebesar 51-68,13% (cukup sesuai) dan kesesuaian wisata selam sebesar 50-68,83% (cukup sesuai). Namun satu titik di sekitar pengukuran sebelah barat laut, sangat berpotensi dikembangkan untuk wisata selam menjadi lebih baik karena kondisi soft coral yang sangat indah berada pada kedalaman sekitar 6 m dengan dasar slope, cocok digunakan sebagai objek penyelaman. Sedangkan untuk wisata snorkeling pada lokasi barat laut tersebut tidak cocok, namun berpotensi untuk dikembangkan di sepanjang pulau yang memiliki pantai, melihat cukup lebar dan luasnya hamparan karang. Kesimpulan yang diperoleh adalah ekowisata bahari cukup potensi dikembangkan di Pulau Pasumpahan, di antaranya wisata pantai (rekreasi) (sebesar 79,91%/sangat sesuai), wisata selam, dan wisata snorkeling.Kata kunci:Â Â Â ekowisata bahari, kesesuaian kawasan, wisata pantai, wisata selam, wisata snorkeling, Pulau Pasumpahan - Kota PadangABSTRACTPasumpahan Island is located in the Bungus Teluk Kabung District, Padang City is one of the archipelago tourist destinations. The objective of the research is to inventory the potential of coastal resources and assess the regional suitability in supporting ecotourism of Pasumpahan Island. The method used in the study is the mapping and analysis of the suitability of ecotourism is done by calculating a score and weighting parameters used. The results obtained are the highest suitability index contained on coastal tourism potentials (recreation) is 79.91% (very suitable). 8 samples among 9 measurement points are around the island shows very suitable value, only one point showing the suitable conditional because a lot of trash were scattered on the beach and muddy waters. To suitability snorkeling by 51-68.13% (suitable enough) and diving by 50-68.83% (suitable enough). But one point around the northwest measurement is very likely to be developed for diving to be better because the conditions were very beautiful soft corals and a basic profile at a depth of 6 m started slope, suitable for use as a dive attraction. As for the snorkeling at the northwest location is not suitable, but has the potential to be developed along the island which has a coastal, looking quite a width and breadth of the reef flat. The conclusion are enough potential for marine ecotourism developed in Pasumpahan Island, such as coastal tourism (recreational) (amounting to 79.91% / very appropriate), diving and snorkeling ecotourism.Keywords: marine ecotourism regional suitability, beach tourism, snorkeling, diving, Pasumpahan Island, Padang City

Suitability of Seagrass Ecosystem for Marine Ecotourism in Padang City, West Sumatera Province Tanto, Try Al; Putra, Aprizon; Hermon, Dedi; Damanhuri, Harfiandri
Forum Geografi Vol 32, No 1 (2018): July 2018
Publisher : Universitas Muhammadiyah Surakarta

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.23917/forgeo.v32i1.5306

Seagrass ecosystems are exciting parts of the tropical coastal region that are potential for ecotourism activities. Marine ecotourism sector in the city of Padang has begun to develop within last few years. This development has not only positive impacts but also negative threats to the environment. Therefore, carefully select the most suitable areas for this purpose is important. This article aims to propose the potential areas for seagrass ecotourism in Padang city based on Geographic information system (GIS) analysis. We used spatial analysis to develop the seagrass ecotourism suitability index that is also potentially applicable to other areas. The results of the analysis show that area of the seagrass ecosystem in Nirwana beach (23.75 ha), Cindakir beach (2.56 ha), and Pasumpahan island (5.46 ha) with a total area of the seagrass ecosystem overall in Padang City (31.78 ha). These areas have been overgrown by Thalassia hemprichii with coverage >50 â 75 % in Nirwana beach, 25 â 50 % in Cindakir beach and Pasumpahan Island. The suitable areas for seagrass ecotourism were found on the beach of Nirwana (covers 84% as very suitable), Cindakir beach (covers 73 % as moderately suitable) and Pasumpahan island (covers 78 % as moderately suitable). We found that activities of local communities decreased the suitability of Cindakir beach and Pasumpahan island because these activities increase the abundance of mud in the substrate of waters.

KERENTANAN PESISIR TERHADAP PERUBAHAN IKLIM DI TIMUR LAUT PROVINSI BALI Putra, Aprizon; Husrin, Semeidi; Tanto, Try Al; Pratama, Roka
MAJALAH ILMIAH GLOBE Vol 17, No 1 (2015)
Publisher : Badan Informasi Geospasial

Secara garis besar, morfologi pesisir timur laut Bali dikategorikan sebagai âMountainous Coast" yaitu pesisir yang terbentuk dari aktivitas gunung api Tersier-Resen dari gunung Agung (3.142 mdpl). Sungai-sungai yang bermuara umumnya bersifat sub radial karena pengaruh gelombang dan arus laut lebih dominan dari arus sungai, maka beberapa sungai mengalir sejajar dengan garis pantai (spit) sebelum bermuara ke laut. Pengaruh endapan sungai dan gunung api menyebabkan pesisir timur laut Bali memiliki sedimen pasir hitam, kerakal dan bongkah yang terbentuk oleh proses-proses vulkanik. Adapun tujuan penelitian ini adalah untuk mengetahui zona wilayah pesisir yang rentan terhadap perubahan iklim di timur laut Bali. Metode penelitian yang digunakan yaitu dengan Indeks Kerentanan Pesisir (IKP) dimana data-data yang digunakan terdiri dari data geospasial dan data oseanografi yang diolah menjadi angka-angka secara kuantitatif. Hasil analisa data penelitian menunjukkan, pesisir timur laut Bali dikategorikan sebagai wilayah dengan kerentanan pesisir sedang â sangat tinggi, dimana dari 20 titik pengamatan dengan panjang garis pantai Â± 60 km memperlihatkan hasil IKP untuk Profil 3 dan 9 memiliki kerentanan sangat tinggi ( > 4), sedangkan untuk Profil 1, 2, 4, 5, 6, 7, 8, 11, 12, 13, 14, 16, 17, 18, 19, dan 20 memiliki kerentanan tinggi (3 â 4), dan Profil 10, 15 memiliki kerentanan sedang (2 â 3).Kata kunci: kerentanan pesisir, perubahan iklim, timur laut BaliABSTRACTIn general, morphology of the northeastern coast of Bali is categorized as "Mountainous Coast" which is a coastal that was formed by volcanic activity Tersier-Resen from Mount Agung (3.142 mdpl).The rivers that empties to the sea generally in a sub radial form due to the influence of waves and ocean currents are more dominant than the rivers, hence several rivers flowi parallelly toward the coastline (spit) before emptying into the sea. Effect of stream sediment and volcanic cause the northeastern coastal Bali contains black sand sediment, gravel and boulders were formed by volcanic processes. The purpose of this study was to determine the coastal zone areas in the Northeastern Bali that are vulnerable to climate change. The method used was a Coastal Vulnerability Index (CVI) where the data used consisted of geospatial and oceanographic data that were processed into quantitative figures. Results of analyses shows that the northeastern coastal Bali categorized as coastal regions with moderate to very high vulnerability. Among the 20 observation points along Â± 60 kms coastline,the CVI in Profile 3 and 9 show a very high vulnerability (> 4), while CVI at Profile 1, 2, 4, 5, 6, 7, 8, 11, 12, 13, 14, 16, 17, 18, 19 and 20 show high vulnerability (3 â 4), and CVI at Profile 10, 15 show moderate vulnerabilities (2 â 3).Keywords: Coastal Vulnerability, Climate Change, Northeastern Bal

The Suitability Ecotourism Beach Based Geopasial in Padang City, Indonesia Putra, Aprizon; Al Tanto, Try
Sumatra Journal of Disaster, Geography and Geography Education Vol 1 No 1 (2017): Sumatra Journal of Disaster, Geography and Geography Education
Publisher : Sumatra Journal of Disaster, Geography and Geography Education

Padang city has a coastline 80.24 km with a water area 72,000 ha, and 19 small islands. Overall, coastal in Padang consists of beach sloping 41.52 km, cliff 22.08 km, muddy 8.19 km, and type of artificial beach in form of building coastal protection. Research aims for identify suitability for ecotourism beach (category of recreation beach and mangrove). Methodology used ie with matrix of suitability ecotourism beach using geospatial approach. Research results for suitability category recreation beach in 24 locations in beach Padang 18 locations are in category of very suitable with a value 82.28 % and only beach in Bung Hatta University are in category conditional with a value 27 %. Suitability category ecotourism mangrove in 19 locations in beach Padang 6 location is in a category is in accordance with a value 92.11 % and 4 location is in a category conditional/not suitable to value 50.88 %.

Identification of Coastal Vulnerability at The North Pagai Island of Mentawai Using Smartline Method Mutmainah, Herdiana; Putra, Aprizon
Sumatra Journal of Disaster, Geography and Geography Education Vol 1 No 2 (2017): Sumatra Journal of Disaster, Geography and Geography Education Volume 1 Number 2
Publisher : Sumatra Journal of Disaster, Geography and Geography Education

Climate change and global warming have a negative impact on coastal, especially small islands. Abration and floods can be very danger and need response to minimize the disaster risks. A simple and practical method is needed to inform the location and type of coastal vulnerability and its risks along coastal segments. Smartline is a coastal management method that represents the geomorphology of coastal, hinterland and shoreline. The North Pagai is a small island, a part of the Mentawai Islands that located at the west offshore of Sumatra Island and one of the under developed areas in Indonesia. The island is surrounded by the Hindia Ocean and located on a subduction path of tectonic plate that prone to earthquakes and Tsunami. High rainfall, strong winds, the complexity of coastal morphology and also the majority of coastal residents and limited infrastructure make the problems more complicated. Tsunami in 2010 (7.7 Mw) caused the change of shoreline getting worst on The East Coast of The North Pagai Island. This study aims to identify the coastal vulnerability using Smartline method. The research was conducted on April and September 2016. The result concludes that physical aspect shows Saumangaya and Matobe Village at high and also very high level of vulnerability hence Sikakap Village at very high level. The socio-economic aspect shows that The Sikakap Village is more advanced but contrary more vulnerable to disaster in terms of population density and complex activities. The North Pagai Island is a vulnerable island from physical and socio-economic aspects.

Identification of Physical Characteristics and the Change of Mangrove Region in Coastal Southern Part of Padang City, West Sumatra - Indonesia Yatno, Triyatno Yatno; Febriandi, Febriandi; Putra, Aprizon; Kamal, Eni
Sumatra Journal of Disaster, Geography and Geography Education Vol 3 No 1 (2019): Sumatra Journal of Disaster, Geography and Geography Education (SJDGGE)
Publisher : Sumatra Journal of Disaster, Geography and Geography Education

The research about the identification of mangrove physical condition and the change of mangrove area has aims are knowing of mangrove physical condition and the change of mangrove area in the coastal region southern part of Padang city. The method used in this research is the field survey and multi-temporal satellite imagery analysis in 2001 and 2018 year. Based on the field survey at the date of August 18, 2017 generally the mangrove that found in research location i.e Rhizophora Apiculata, Rhizophora mucronata, Sonneratia alba, and Nypa. The spatial distribution of the mangrove ecosystem is dependent on the ecological conditions of the area as reflected by the types of mangrove vegetation that grows and develops in the research location. A decrease in mangrove area that occurred between of 2001 to the 2017 years i.e in the coastal region of Bungus bay i.e 5.54 ha, where the decrease in mangrove area occurred because some mangrove plants were cut down and made the settlement land, while in the region of Sungai Pisang bay happen to increase in mangrove area i.e 36.12 ha, where the increase in mangrove area occurred because of the region obstructed by big waves of the sea (protected small the islands).

Estimate Broad of Natural Mineral Resources Area Lateritic Nickel Based of Image Analysis Satellite Landsat 7 Etm+ In District Laonti, Konawe Selatan, Province of Southeast Sulawesi Putri, Sri Kandi; Nova, Sari; Lionar, Uun; Putra, Aprizon
Sumatra Journal of Disaster, Geography and Geography Education Vol 3 No 2 (2019): Sumatra Journal of Disaster, Geography and Geography Education (SJDGGE)
Publisher : Sumatra Journal of Disaster, Geography and Geography Education

Mineral exploration is one of the important activities to obtain location information about where the minerals are, but this exploration process takes years and costly especially when carried out over a wide area. Therefore through this study the application of Geographic Information Systems and Remote Sensing for mapping the distribution of potential mineral deposits of lateritic nickel (Ni) is tested. The method used is the analysis of digital data Landsat 7 ETM +. Rocessed image data by performing a technique sharpening contrast, filtering, creation of a composite image and image fusion. Image data processing is for the interpretation of visual straightness, limit unit morphology and the estimation of mineral lateritic nickel. The data as well as analysis techniques NDVI in order to obtain the pattern of vegetation density on the surface. The results showed that the presence of lateritic nickel mineral formed on ultramafic rocks undergoing the process of weathering and serpentinization. Characterized with the appearance of geological structures identified as robust and fault structures. Which are also represent on the remote sensing images as rectangular flow patterns.Ultramafic rocks are located in the morphological undulating hills. Vegetation is identified growing on ultramafic rocks are categorized as dense vegetation. Vegetation that grows in the form of a single tree with an average diameter ≤30 cm. result generating estimates of mineral potential areas of lateritic nickel has an area ranging 6.3 ha.

Co-Authors - Ilham A. Riza Farhan Abdul Hadi Putra Abdul Razak Abellia Fanny Aldeta Aditya Herfianda Aditya Saputra Adli Attamimi Agustian, CH. andi, febriandi Apriadi Agussalim Arlius Arlius, Arlius Arman A Azhari Syarief Baqi, Ahmad Iqbal Bayu Wijayanto Cipta Estri Sekarrini Damanhuri, Harfiandri Deded Chandra Dedi Hermon Dian Adhetya Arif Dwi Marsiska Driptufany Efriyeldi, Efriyeldi Eni Kamal Eni Kamal Eri Barlian Erianjoni Erianjoni Fadhilah, Lamis Tharra Fajrin Fajrin Fredinan Yulianda Fuji Astuti Febria Gunardi Kusumah Gunardi Kusumah Gunardi Kusumah H L Salim Hadi Sofyan Handayuni, Linda Heldi Heldi, Heldi Helfia Edial Hendry Frananda Henny Yulius Herdiana Mutmainah Herdiana Mutmainah, Herdiana Husrin, Semeidi Ilham . Ilham Ilham Ilham Ilham Ilham, Ilham Indang Dewata irwan meilano Iswandi U Iswandi Umar Jaya Kelvin Koko Ondara Kusumah, Gunardi Lailatur Rahmi Lia Hasmita Lionar, Uun M Ramdhan Memo Memito Mira Hasti Hasmira Muhammad Hidayat Mulya Gusman Mustapha, Muzzneena Ahmad N Nofrion Nia Naelul Hasanah Nita Yuanita Nova, Sari Novio, Rery Novitri, Awinda Nurfadhilla Nurfadhilla Nurul Rahmadilla Edgar Oktorie, Olivia Olivia Oktorie Osronita Osronita Pratama, Roka Putri, Sri Kandi Radha Karina Putri Rahmadi Prasetijo Ramadhan, Riski Rammadani Yusran Randu Prayoga Putra Ratna Wilis Roka Pratama Rusdi Rusdi Semeidi Husrin Semeidi Husrin Semeidi Husrin Semeidi Husrin Semeidi Husrin Semeidi Husrin Semeidi Husrin Semeidi Husrin Semeidi Husrin Semeidi Husrin Serly Mutia Sari Shintia Franzela Sri Mariya Suparno . T A Tanto Tanto, Try Al Tanto, Try Al Tasa Anike Triyatno Triyatno Triyatno Triyatno Triyatno, . Try Al Tanto Try Al Tanto Try Al Tanto Try Al Tanto Try Al Tanto Try Al Tanto Try Al Tanto, Try Try Al Tanto, Try Al Ulung Jantama Wisha Ulung Jantama Wisha Ulung Jantama Wisha Ulung Jantama Wisha Widodo S Pranowo Widodo S Pranowo Widodo S. Pranowo Widya Prarikeslan Wilson Novarino Wisha, Ulung Jantama Yulius Yulius Yunhendri Danhas Yurni Suasti

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