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ANALISIS PERUBAHAN GARIS PANTAI DI PANTAI BARAT DAYA PULAU TERNATE, PROVINSI MALUKU UTARA Abdul Motalib Angkotasan; I Wayan Nurjaya; Nyoman M.N. Natih
Jurnal Teknologi Perikanan dan Kelautan Vol 3 No 2 (2012): NOVEMBER 2012
Publisher : Fakultas Perikanan dan Ilmu Kelautan

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (792.535 KB) | DOI: 10.24319/jtpk.3.11-22

Abstract

Research is a Shoreline Change Analisis along the South West Coast Ternate Island, North Molucas Province. This study aims to assess the shoreline changes from 2001 to 2011. The research was motivated by the reality on the Southwest Coast Ternate Island, accured abrasion and sedeimentasi to residential areas. There has been no comprehensive study on the extent of shoreline change is happening, and what are the factors that cause these changes. The purpose of this study was to analyze shoreline changes that occur in the Southwest Coast Ternaet island. Shoreline change analysis is done using two approaches that use DHI MIKE LITPACK models and digitized images using Landsat 7 ETM+. The results of image analysis used as a benchmark to validate the model output DHI MIKE LITPACK. Mixed model analysis results collated with the results of image analysis showed patterns of changes in the contour of the same coastline. Based on the analysis model, showed the highest abrasion occurs distasiun C (Sasa Coast) as far as 83.67 m and sedimentation occurred at station B as far as 45.69 m, based on the results of image analysis the highest abrasion occurred at station C of 27.14 m and sedimentation occurred at station E of 24.09 m . The amount of abrasion and sedimentation is affected by wave action that occurs and sand mining activities by the community in Southwest coast of the island of Ternate.
TINGKAT KERENTANAN PESISIR DI UTARA DAN TIMUR PULAU BINTAN PROVINSI KEPULAUAN RIAU TAHUN 2020 Mario Putra Suhana; Risandi Dwirama Putra; Leica Febby Shafitri; Muhamad Muliadi; Khairunnisa Khairunnisa; I Wayan Nurjaya; Nyoman Metta N. Natih
Jurnal Teknologi Perikanan dan Kelautan Vol 11 No 1 (2020): MEI 2020
Publisher : Fakultas Perikanan dan Ilmu Kelautan

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (3000.831 KB) | DOI: 10.24319/jtpk.11.11-27

Abstract

Coastal areas are unique, dynamic, and complex because they are zones of interaction between land, oceans, and atmosphere. This makes coastal areas the most vulnerable areas on Earth. To find out how big the vulnerability is in a coastal area, a study is needed to determine the vulnerability level of coastal areas and the influencing factors. Research on the coastal vulnerability level at this location was conducted in 2016 and it was concluded that the coastal vulnerability level is in the medium category. With the development of potential utilization in the area, it is necessary to conduct similar research in 2016 to find out if there is a change in vulnerability level between 2016 and 2020. The data used consisted of coastal geomorphology, tidal, Landsat 7 ETM+ and 8 OLI, sea level rise and DEM satellite imagery. Data analysis using Coastal Vulnerability Index (CVI) method. The results showed the coastal vulnerability level at the research site was in the low-medium category, with a CVI score range of 9,93-25,86. Topography, geomorphology, intensity of shoreline changes, and coastal slope are factors that can cause the vulnerability level at the research site can be very high. However, the interconnectedness between other parameters can inhibit the high level of vulnerability, making the level of coastal vulnerability at the research site to be only in the low-medium category. There was a change in vulnerability level conditions between 2016 and 2020 the level of vulnerability at the east coast decreased to a low category.
Pemanfaatan Citra Satelit Landsat -MSS Untuk Melihat Perubahann Luasan Daratan dan Magrove Akibat Sedimentasi di Laguna Segara Anakan Cilacap IG Wayan Adiwilaga; Joko Purwanto; I Wayan Nurjaya
Jurnal Ilmu-Ilmu Perairan dan Perikanan Indonesia Vol. 1 No. 1 (1993): Juni 1993
Publisher : Institut Pertanian Bogor

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Abstract

Penelitian ini bertujuan untuk melihat perubahan luasan daratan dan mangrove di perairan laguna Segara Anakan Cilacap dengan menggunakan citra sate lit Landsat-MSS. Proses sedimentasi yang intensif di perairan ini menimbulkan adanya perubahan daratan. Sumbangan sedimen yang terbesar berasal dari sungai Citanduy. Pada tang gal 13-16 Februari 1985, sedimen yang masuk ke Segara Anakan sebesar 82,52 ton atau 1,68 tonfJam dengan laju pengendapan sebesar 0,731 ton/m2 atau 9,8kg/m2fJam. Sedangkan pada bulan Juni 1989, sedimen yang masuk ke Segara Anakan sebesar 2134,66 ton atau 2,98 tonfJam, sedimen yang diendapkan sebesar 9,41 ton/m2 atau 13,69 kg/m2/jam. Hasil analisis korelasi linier antara perubahan daratan dan mangrove terhadap waktu menunjukkan bahwa perubahan luasan daratan terhadap waktu berkorelasi 0,998, sedangkan perubahan luasan mangrove terhadap waktu berkorelasi -0,960. Kondisi ini disebabkan oleh adanya kegiatan penebangan pohon mangrove secara liar, perubahan peruntukan lahan hutan mangrove menjadi persawahan, pertambakan dan pemukiman.Kata-kata kunci: citra satelit LANDSAT-MSS, sedimentasi, mangrove, laguna Segara Anakan
KAJIAN KAPASITAS ASIMILASI BEBAN PENCEMARAN ORGANIK DAN ANORGANIK DI PERAIRAN TELUK JOBOKUTO KABUPATEN JEPARA JAWA TENGAH Harpasis S Sanusi; Richardus F Kaswadji; I Wayan Nurjaya; Rita Rafni
Jurnal Ilmu-Ilmu Perairan dan Perikanan Indonesia Vol. 12 No. 1 (2005): Juni 2005
Publisher : Institut Pertanian Bogor

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Abstract

Perairan pantai (Teluk Jobokuto) merupakan tempat penampungan berbagai macam limbah buangan termasuk limbah industri, pertanian, dan pemukiman. Limbah tersebut sangat bervariasi dalam komposisi secara fisika maupun biokimia. Permasalahannya secara umum pembuangan limbah ke dalam perairan pantai berasal dari sumber yang tidak terkontrol seperti pertanian (runoff), peningkatan jumlah penduduk, yang secara cepat akan meningkatkan beban limbah. Aktivitas-aktivitas tersebut akan berdampak terhadap penurunankualitas perairan, sehingga evaluasi tentang kapasitas asimilasi menjadi penting. Penelitian ini bertujuan untuk menganalisis kondisi kapasitas asimilasi beban pencemar, kualitas air, sedimen dan biologi perairan. Hasil penelitian menunjukkan bahwa beban limbah tertinggi disumbang TSS sebesar 157.40 ton/hari dari sungai Jepara. Nilai beban limbah tersebut masih dibawah nilai kapasitas beban Teluk Jobokuto. Proses percampuran menunjukkan tipe estuari perairan Teluk Jobokuto termasuk tipe estuari campuran sebagian, laju pengenceranadalah 9.09 hari. Kualitas air seperti TSS, DO, BOD5, NH3-N, NO3, NO2, PO4, dan TOM secara umum masih sesuai kriteria baku mutu kualitas air untuk biota laut (Kepmen No. 02/MENKLH/I/1988). Berdasarkan analisis STORET, perairan Teluk Jobokuto relatif belum tercemar. Sedimen didominasi fraksi pasir (50.53 – 92.41%) dan bahan organik tertinggi adalah C-org(0.91-3.36%). Secara umum, kondisi sedimen berada dalam zona oksidasi - transisi. Struktur komunitas fitoplankton dan makrozoobentos memperlihatkan indeks keanekaragaman yang sedang dan tidak terdapat dominansi spesies. Berdasarkan uraian tersebut menunjukkan ondisi kapasitas asimilasi beban pencemar di perairan Teluk Jobokuto masih dalam keadaan belum terlampaui.Kata kunci: kapasitas asimilasi, kapasitas beban, waktu pencucian, proses percampuran, zona diskontinuitas oksidasi
Semarang waterfront city is a unique ecosystem with a great variety of potentialities as well as problems in the utilization of natural resources, particularly in the trade-off between economic growth and ecological preservation. Based on those conditions, the research is mainly focused upon designing some scenarios on environmental management, which ensure a profitable synergy of all stakeholders without sacrificing the principles of environmental conservation. Secondly, it is to design an inte Bambang Kanti Laras; Marimin .; I Wayan Nurjaya; Sugeng Budiharsono
Forum Pasca Sarjana Vol. 34 No. 4 (2011): Forum Pascasarjana
Publisher : Forum Pasca Sarjana

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Abstract

Semarang waterfront city is a unique ecosystem with a great variety of potentialities as well as problems in the utilization of natural resources, particularly in the trade-off between economic growth and ecological preservation. Based on those conditions, the research is mainly focused upon designing some scenarios on environmental management, which ensure a profitable synergy of all stakeholders without sacrificing the principles of environmental conservation. Secondly, it is to design an interaction model among variables in the bio-physic, economy and social subsystems, in order to increase sources of learning and sustainable use of natural resources. Using a dynamic system, the main inputs of the designed model are the feasibility of natural resources management as a product of extended cost-benefit analysis (ECBA), the suitable option of natural resources management, as an input of comparative performance index (CPI), the integrated sustainability of using multidimensional scaling, the suitable land-use planning through geographic information system (GIS). From those main inputs the waterfront city environmental management policy can be observed as an output of analytical hierarchy processes (AHP).  The feasibility study shows that all of natural resources management options are feasible to be developed, where sustainable management, sustainable harvest and beach protected areas depict the most feasible management options.  Based on the results of the integrated sustainability research using multidimension scaling, the management of waterfront cities has to prioritize attention to the five important factors, i.e., (1) the issues of community empowerment; (2) the rate of land utilization; (3) the contribution of the industrial sector; (4) the availability of electricity and; (5) the availability of community organizations. Key words: sustainable environmental management, coastal and marine zone, dynamic and spatial dynamic system, waterfront policy strategy
Semarang waterfront is a unique ecosystem which has a variety potentialities and problem of using some natural resources, especially in the trade-off between economic growth and ecological preservation.  Generally the handling operation of waterfront city in Indonesia is not effective, caused by (1) low budged and increase the poverty; (2) over loaded investment; (3) destroyed of ecology and ecosystem; (4) the lost of local wisdom; and (5) other problem in commonly urban city.  Based on these co Bambang Kanti Laras; Marimin .; I Wayan Nurjaya; Sugeng Budiharsono
Forum Pasca Sarjana Vol. 34 No. 2 (2011): Forum Pascasarjana
Publisher : Forum Pasca Sarjana

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Abstract

Semarang waterfront is a unique ecosystem which has a variety potentialities and problem of using some natural resources, especially in the trade-off between economic growth and ecological preservation.  Generally the handling operation of waterfront city in Indonesia is not effective, caused by (1) low budged and increase the poverty; (2) over loaded investment; (3) destroyed of ecology and ecosystem; (4) the lost of local wisdom; and (5) other problem in commonly urban city.  Based on these conditions, this research aimed to design an environmental management policy ensuring a profitable synergy of all stakeholders without sacrificing the principles of environmental conservation.  The objective of this study was to analyze the index and sustainability status of the Semarang waterfront area, based on five sustainable dimensions.  Secondary data resources have been used from literature study and references, primary data have been received from questionairy feedback and expert judgement survey.  The analysis  used multi dimensional scalling (MDS) method, called Rap-WITEPA, and the results were stated in the index and sustainability status.The second objective was to analyze the attributes that affect sensitivity on index and sustainability status and the effect of error using Laverage and Monte Carlo Analysis.  The result of this study show that ecological dimension was in the status of less sustainable (49,34), economical dimension was sufficient sustainable (53,96), socio-culture dimension was sufficient sustainable (52,21), dimension of infrastructure and technology was sufficient sustainable (56,72) and dimension of law & institutional was the highest sufficient sustainability value index (57,19).  Out of 94 attributes analyzed, there were 50 attributes need to be handled immediately as they affect sensitivity on the increase of index and sustainability status with negligible error in the level of 95% confidence limit.  It was concluded that an important factor of waterfront city handling operation design in Semarang is social community development, land use efficiency, industry contribution, electricity, and local society organization.   Key words: sustainability index, sustainability status, waterfront city
This research to study relation between environment parameter, plankton abundance and primary productivity with abundance of tiger prawn post larvae and milk fish fry, calculates plankton predating rate speed by tiger prawn post larvae and milk fish fry and other larva and studies plankton population dynamics, tiger prawn post larvae and milk fish fry before, at the time and after peak season.  Result of research indicates that some environment parameters significant differs according to observa Nur Asia Umar; Richardus F. Kaswadji; Ario Damar; Ismudi Muchsin; I Wayan Nurjaya
Forum Pasca Sarjana Vol. 32 No. 2 (2009): Forum Pascasarjana
Publisher : Forum Pasca Sarjana

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Abstract

This research to study relation between environment parameter, plankton abundance and primary productivity with abundance of tiger prawn post larvae and milk fish fry, calculates plankton predating rate speed by tiger prawn post larvae and milk fish fry and other larva and studies plankton population dynamics, tiger prawn post larvae and milk fish fry before, at the time and after peak season.  Result of research indicates that some environment parameters significant differs according to observation period and season.  Highest abundance of tiger prawn post larva, milk fish fry and other larva reaches to 29067, 7733 and 54400 ind/1000 m3. Highest grazing rate to population of phytoplankton and plankton (phytoplankton + zooplankton) found when predator consisted of tiger prawn post larva, milk fish fry and other larva with grazing rate up to 125 cells/liter/hour and 129 plankter /liter/hour respectively.  Highest predating rate to zooplankton population when predator consist of tiger prawn post larva and milk fish fry and there is phytoplankton as their prey up to 12 individual/liter/hour.  The certain plankton species significant correlation and estimated as natural food of tiger prawn post larva and milk fish fry that is some types of diatom and crustaceae from zooplankton.  Plankton population dynamics especially controlled by predator by tiger prawn post larva, milk fish fry and other larva, while influence of environment parameter is small relative. Abundance of each phytoplankton and zooplankton ranged from 583-28563 cells/liter and 22-3413 ind/liter.  Average abundance of phytoplankton and zooplankton significant differs higher at peak season compare  before and after tiger prawn post larva and milk fish fry season. Predator-prey relation between phytoplankton and zooplankton shows phase change which succession between phytoplankton controls to zooplankton phases with zooplankton control to phytoplankton.  Abundance of plankton influences abundance of population of tiger prawn post larva and milk fish fry especially after peak season.  There is concordance of time between peak abundance of tiger prawn post larva and milk fish fry and other larva with peak abundance of phytoplankton and zooplankton.   Key words : population dynamics, predating, predating rate, predator, prey, phytoplankton, zooplankton, tiger prawn post larva, milk fish fry, other larva, Pinrang
Dinamika Perubahan Mangrove Menjadi Tambak dan Total Suspended Solid (TSS) di Sepanjang Muara Berau Ety Parwati; Kadarwan Soewardi; Tridoyo Kusumastanto; Mahdi Kartasasmita; I Wayan Nurjaya
Biologi Edukasi: Jurnal Ilmiah Pendidikan Biologi Vol 3, No 1 (2011): Biologi Edukasi: Jurnal Ilmiah Pendidikan Biologi
Publisher : Universitas Syiah Kuala

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Abstract

The mangrove conversion become fish pond, bareland or others has an impact in water quality. One of water quality parameter is Total Suspended Solid (TSS), increasing TSS means the rising in pollution.  Landsat remote sensing data with multi channels used in studying the dynamic of mangrove – fishpond change and TSS along the Berau waters. Several regions with its variation are used in that dynamic studying.  The TSS algorithm for Berau waters is TSS (mg/l) = 3.3238 * exp (34.099*Red Band) , Red band=the atmospheric reflectance band 2 validated with field data. The result study is the conversion of mangrove become fish pond has the strong indication in the rising TSS .
ETHNOOCEANOGRAPHY DAN TITIK TEMU ASPEK SYAR’I DALAM PENENTUAN AWAL BULAN RAMADHAN DAN SYAWAL OLEH JOGURU KESULTANAN TIDORE Salnuddin Salnuddin; I Wayan Nurjaya; Indra Jaya; Nyoman M.N Natih
Al-Ahkam Volume 27, Nomor 1, April 2017
Publisher : Faculty of Sharia and Law, Universitas Islam Negeri (UIN) Walisongo Semarang

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (3091.196 KB) | DOI: 10.21580/ahkam.2017.27.1.1073

Abstract

Ethnooceanography and the intersection of shar'i aspects to determination of the early of Ramadan and Shawwal by Joguru Sultanate of Tidore. The determination of the early of the new month of Ramadan and Shawwal was very important for Muslims because it is related to the time of worship. Judge syara 'The Sultanate of Tidore (Joguru) has long applied the method of determining the early month of Hijri (Ramadan and Shawwal) through tidal movement observed on "akebai" included in ethooceanography and called Joguru Method (MJ). Hilal that has never been seen in Tidore and its surrounding areas in the long-term cycle of moon (34 years) caused its early moon to be inapplicable due to non-fulfillment of the requirement of hisab (hadith). MJ makes observation (rukyat) change of tidal movement on "akebai" is "ijtihād". The appropriateness of the scientific aspects of ethnoocaenography and the intersection of the shar'i aspects make it a comparative method of determining the beginning of the new month of Hijri in astronomy (hilāl). Required the expansion of the meaning of the “hilāl” as an indicator of the beginning of the month of the Hijri calendar.[]Ethnooceanography dan titik temu aspek Syar’i dalam penentuan awal bulan Ramadhan dan Syawal oleh Joguru Kesultanan Tidore. Penentuan awal bulan baru Ramadhan dan Syawal sangat penting bagi umat Islam karena berkaitan dengan waktu ibadah. Hakim syara’ Kesultanan Tidore (Joguru) telah lama mengaplikasikan metode penentuan awal bulan baru Hijriah (Ramadhan dan Syawal) melalui pergerakan pasang surut yang terpantau pada “akebai” termasuk dalam ethooceanography dan disebut dengan Metode Joguru (MJ). Hilal yang tidak pernah terlihat di wilayah Tidore dan sekitarnya selama siklus jangka panjang (34 tahun) menyebabkan hisab awal bulan tidak dapat diaplikasikan akibat tidak terpenuhinya persyaratan hisab (hadis). MJ melakukan peng­amatan (rukyat) perubahan tinggi air pada “akebai” adalah “ijtihad”. Terdapat ke­sesuaian aspek sains dari ethnoocaenography serta titik temu aspek syar’i yang menjadikan MJ berpotensi sebagai metode utama sekaligus sebagai metode pem­banding dari metode umum dalam penentuan awal bulan baru Hijriah. Diperlukan perluasan makna kata “hilal” sebagai indikator awal bulan baru penanggalan Hijriah.
CHARACTERISTIC OF PHYSICAL OCEANOGRAPHY IN EAST INDIAN OCEAN DURING POSITIVE PHASE OF INDIAN OCEAN DIPOLE (IOD) OF 1994/1995, 1997/1998, AND 2006/2007 Pramudyo Dipo; I Wayan Nurjaya; Fadli Syamsudin
Jurnal Ilmu dan Teknologi Kelautan Tropis Vol. 3 No. 2 (2011): Elektronik Jurnal Ilmu dan Teknologi Kelautan Tropis
Publisher : Department of Marine Science and Technology, Faculty of Fisheries and Marine Science, IPB University

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1795.914 KB) | DOI: 10.29244/jitkt.v3i2.7823

Abstract

There is an inter-annual phenomenon in the Indian Ocean that occurs because of the interaction between atmosphere and ocean are known Indian Ocean Dipole (IOD). IOD is a bipolar structure that characterized by the difference of sea surface temperature to normal. The objectives of this study is to know the characteristic of physical oceanography in the eastern part of Indian Ocean during the formation phase, maturation phase and decay phases of positive IOD. The second objective was to determine the comparative characteristic of physical oceanography in the eastern Indian Ocean between the positive IOD in different years. The strengthening of the South Equatorial Current in transitional seasons I (March-May) followed by early cooling of the SST which is indicated by the formation phase of IOD. At the Southeast monsoon (June to August) and the beginning of the season transition II, there is a visible presence of upwelling in the south of Java, which is then further extends to the peak in September (maturation phase) and begin to disappear in October followed by warming of the SST on the East of Indian Ocean in November (decay phase).Keywords: Indian Ocean Dipole, upwelling, Empirical Orthogonal Function (EOF) analysis, Eastern Indian Ocean
Co-Authors . Sukenda Abdurrachman Baksir, Abdurrachman Adi Purwandana Adibrata, Sudirman Adil Mahfudz Firdaus Adil Mahfudz Firdaus Adil Mahfudz Firdaus Agus Atmadipoera Agus Saleh Atmadipoera Agus Sholeh Atmadipoera Ahmad Herison Akmala Dwi Nugraha Alan Frendy Koropitan Alimuddin, Alimuddin Amir Yarkhasy Yuliardi Andhi Setyonugroho Andi Agussalim, Andi Andri Purwandani Ari Purbayanto Ariane Koch-Larrouy Ario Damar Asep Sandra Budiman Asep Sandra Budiman Asep Sandra Budiman, Asep Sandra Baharuddin Baharuddin Bambang Kanti Laras Beale, Calvin S. Beginer Subhan Bengen, Detriech G Darmiati Dedi Sugianto Dema Okgareta Denny Alberto Satrya Gumay Derek Soto Dietrich G Bengen Dietriech G. Bengen Dietriech G. Bengen Dietriech Geoffrey Bengen Dondy Arafat Dwiyoga Nugroho Eddy Supriyono Edi Kusmanto Enang Harris Surawidjaja Esty Kurniawati Esty Kurniawati Ety Parwati Ety Parwati Ety Parwati Ety Parwati fadli syamsudin Fani Safitri Ferawati Runtuboi Ferdy Gustian Firdaus, Adil M. Franto Novico Fredinan Yulianda Harpasis S Sanusi Harpasis S Sanusi Harpasis s. Sanusi Hefni Effendi Heron Surbakti Heron Surbakti Hidayat Pawitan Holyness Nurdin Singadimedja HS, Surjono I Gusti Bagus Wiksuana Ida Bagus Made Baskara Andika IG Wayan Adiwilaga Ikbal Marus, Ikbal Indra Jaya Indra Jaya Indra Jaya Indra Jaya Irmalita Tahir, Irmalita Irzal Effendi Ismail, Firdaut Ismudi Muchsin Ismudi Muchsin John I Pariwono Joko Purwanto Joko Santoso Jonson Lumban Gaol Kadarwan Soewardi Kadarwan Soewardi Kadarwan Soewardi Kadarwan Soewardi Kasman Kasman Khairunnisa Khairunnisa Kholil Kholil Kholil Kholil Kotta, Raismin Krisna Rendi Awalludin Kusnanto La Ode Nurman Mbay Leica Febby Shafitri Leni Maryani Lerma Yuni Siagian Luky Adrianto M. Zairin Junior Mahdi Kartasasmita Mahdi Kartasasmita Mahdi Kartasasmita Mahdi Kartasasmita Manalu, Janviter Marimin , Mario Putra Suhana Mennofatria Boer Muh. Ishak Jumarang Muhamad Muliadi Muhammad Agus Muljanto MUHAMMAD AGUS SUPRAYUDI Muhammad Marzuki Mulia Purba Mulia Purba Mulia Purba Mursalin Mursalin Najamuddin N Najamuddin Najamuddin, Najamuddin Nandi Abdul Aziz Nebuchadnezzar Akbar Neviaty P Zamani Neviaty P. Zamani Noor, Hariansyah Novit Rikardi Nugraha, Teguh Nur Asia Umar Nur Audina Nyoman M N Natih Nyoman M.N Natih Paembonan, Rustam E Paputungan, Mohammad Sumiran Pramudyo Dipo Rasidi, Rasidi Rastina Ratu Almira Kismawardhani Ratuluhain, Eva Susan Richardus F Kaswadji Richardus F. Kaswadji Ridha Alamsyah Riris Aryawati Risandi Dwirama Putra Rita Rafni Riyadi Subur, Riyadi Robin Saputra Robinson Sitepu Rustam Effendi Paembonan, Rustam Effendi Saenudin Sakka Sakka Salnuddin Salnuddin, Salnuddin Salsabila, Unik Hanifah Salsabilah, Raisyah Santi Susanti, Santi Satria Yukiadi Santoso Septy Heltria Setyo Handayani Setyo Handayani Sigid Hariyadi Siolimbona, Abdul Ajiz Soma Somantri Sugeng Budiharso Sugeng Budiharsono Suhaemi Supriyono, Supri Surjono HS Syamsul Bahri Agus, Syamsul Bahri Tri Hartanto Tri Prartono Tridoyo Kusumastanto Try Al Tanto Try Al Tanto Try Al Tanto Vincentius P Siregar Wahab, Iswandi Wahyu W Pandoe Wibowo, Eko S Widodo S. Pranowo Yogi Cahyo Ginanjar Yonvitner - Yudi Setiawan Yuli Naulita Yusli Wardiatno Zibar, Zan Zulfikar, Andi