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All Journal MANAJEMEN HUTAN TROPIKA Journal of Tropical Forest Management Jurnal Ilmu Pertanian Indonesia Jurnal Teknologi Perikanan dan Kelautan Jurnal Ilmu dan Teknologi Kelautan Tropis Jurnal Ilmu-Ilmu Perairan dan Perikanan Indonesia Forum Pasca Sarjana Maspari Journal ILMU KELAUTAN: Indonesian Journal of Marine Sciences Jurnal Ilmu Lingkungan POSITRON Biologi Edukasi : Jurnal Ilmiah Pendidikan Biologi Maspari Journal JAM : Jurnal Aplikasi Manajemen Al-Ahkam Jurnal Perikanan dan Kelautan Jurnal Pengelolaan Sumberdaya Alam dan Lingkungan (Journal of Natural Resources and Environmental Management) Widyariset Jurnal Kelautan Tropis BERITA BIOLOGI Journal of Applied Geospatial Information JURNAL ENGGANO Omni-Akuatika MAJALAH ILMIAH GLOBE BULLETIN OF THE MARINE GEOLOGY Jurnal Pengelolaan Perikanan Tropis (Journal Of Tropical Fisheries Management) Dinamika Maritim Jurnal Penelitian Perikanan Indonesia Jurnal Kelautan Nasional Jurnal Segara Jurnal Sosial Ekonomi Kelautan dan Perikanan Jurnal Penginderaan Jauh dan Pengolahan Data Citra Digital International Journal of Remote Sensing and Earth Sciences (IJReSES) JURNAL METEOROLOGI DAN GEOFISIKA STI Policy and Management Journal Widyariset Jurnal Bali Membangun Bali COJ (Coastal and Ocean Journal) Depik Jurnal Ilmu-Ilmu Perairan, Pesisir dan Perikanan Depik Jurnal Ilmu-Ilmu Perairan, Pesisir, dan Perikanan Journal of Fisheries & Marine Jurnal Meteorologi dan Geofisika Jurnal Penginderaan Jauh dan Pengolahan Data Citra Digital The International Journal of Remote Sensing and Earth Sciences (IJReSES)

I Wayan Nurjaya

Bogor Agricultural University

Author-ID : 2891603

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Fate of Heavy Metals Pb and Zn in the West Season at Jeneberang Estuary, Makassar Najamuddin .; Tri Prartono; Harpasis S Sanusi; I. Wayan Nurjaya
ILMU KELAUTAN: Indonesian Journal of Marine Sciences Vol 22, No 3 (2017): Ilmu Kelautan
Publisher : Marine Science Department Diponegoro University

The pollutant quantity of heavy metals entering water environment does not give complete answer toward the generated effect and risk, however it needs thoroughly study related to the pollutant dynamic. The aim of this research was to investigate the fate of Pb and Zn in water, such as: distribution, behavior, and reactivity (case study: Jeneberang Estuary, Makassar). Pb and Zn concentrations were determined using Atomic Absorption Spectrophotometry (AAS). The distribution of dissolved Pb and Zn showed a pattern that the lowest concentration was in the fresh water (the river zone), whereas the highest concentration was in the salt water (the marine zone). The distribution pattern of particulate Pb and Zn showed that the highest concentration was in the fresh water (the river zone) and the salt water (the marine zone), whereas the lowest concentration was in the estuary zone. The behavior of dissolved Pb and Zn tended to increase the concentration (desorption) along the increased salinity gradient. The residual fraction was the dominant component of geochemical fractions in the sediment that indicated the sources of Pb and Zn mainly derived from a natural process and the reactivity was low in the water. Keywords: distribution, behavior, reactivity, lead, zinc, pollution

Variation of Tidal Range Based On Hijra Calendar And Its Relation With Ethno-Oceanography of The Sama Tribe In Eastern Indonesia Salnuddin Salnuddin; I Wayan Nurjaya; Indra Jaya; Nyoman M.N Natih
ILMU KELAUTAN: Indonesian Journal of Marine Sciences Vol 22, No 2 (2017): Ilmu Kelautan
Publisher : Marine Science Department Diponegoro University

Based on Ethno–Oceanography of the Sama tribe in Eastern Indonesia, they measured and determined tidal range when Sya’ban taking place. Why do they do so? The questions and objective of this study were intended to respond the scientific fundamental of Ethno-Oceanography of the Sama tribe. In order to achieve the objective of this study, the tidal range value in each Hijra month was compared and analyzed statistically (ANOVA). Tidal Analysis results showed that the tidal range at Sya’ban was higher and the deviation was lower than the other months. Moreover, ANOVA results showed that Sya’ban was significantly different (P<0.05) on Highest High Water Level (HHWL) throughout Hijra month. Keywords: Sama Tribe, Sya’ban, Hijra Calendar

Prediksi Sebaran Suhu dari Air Buangan Sistem Air Pendingin PT. Badak NGL di Perairan Bontang Menggunakan Model Numerik Kasman Kasman; I Wayan Nurjaya; Ario Damar; Ismudi Muchsin; Zaenal Arifin
ILMU KELAUTAN: Indonesian Journal of Marine Sciences Vol 15, No 4 (2010): Ilmu Kelautan
Publisher : Marine Science Department Diponegoro University

Tingginya suhu buangan air pendingin PT. Badak NGL yang dilepas ke Perairan Bontang menyebabkan terganggunya berbagai sumberdaya pesisir yang ada disekitarnya. Karena itu perlu diketahui pola sebaran suhu agar dampak yang mungkin timbul dapat diminimalkan. Penelitian ini bertujuan untuk memprediksi pola sebaran suhu dari buangan air pendingin PT. Badak NGL di Perairan Bontang, Kalimantan Timur. Prediksi dilakukan dengan menggunakan model hidrodinamika dan transpor suhu 3-D yang dimodifikasi dari model POM (Princeton Ocean Model). Gaya pembangkit yang digunakan dalam model adalah pasang surut, debit buangan air pendingin dan debit sungai. Pemilihan langkah waktu (t)=0,5 detik, dengan 118 grid (barat-timur) dan 187 grid (utara-selatan), ukuran grid Δx=Δy=30 m. Nilai awal : u=v=ζ=0, T0 = 28 °C dan S0 = 32 ‰. Verifikasi elevasi dan suhu antara hasil model dengan hasil pengukuran menunjukkan kesesuaian yang baik dengan nilai korelasi 0,97 dan Kesalahan Relatif Rata-rata (Mean Relative Error/MRE) 1,31% untuk verifikasi elevasi, korelasi 0,90 dan MRE 5,17% untuk verifikasi suhu permukaan pada saat bulan purnama serta korelasi 0,87 dan MRE 7,12% saat bulan perbani. Hasil simulasi menunjukkan perbedaan pola sebaran suhu permukaan paling ekstrim ditemukan pada saat purnama untuk kondisi cuplik pasang maksimum dan surut maksimum. Perbedaan terutama terlihat pada Stasiun 8 (Muara Kanal Pendingin) yakni 41 °C saat surut maksimum dan saat pasang maksimum (ΔT=6 °C). Adapun perbedaan suhu antara lapisan atas dan lapisan bawah yang cukup besar ditemukan di Stasiun C yakni sekitar 2,54 C saat untuk skenario musim kemarau dan 2,32 C untuk skenario musim hujan Kata kunci : POM, buangan air pendingin, sebaran suhu, debit sungai, model numerik, Perairan Bontang High temperature of cooling water discharge of PT. Badak NGL that released to Bontang waters caused disturbances to the coastal resources in its surrounding. Therefore, it is urgent to understand the pattern of thermal dispersion in order to minimize the possible impacts occurred. This research was aimed to predict the pattern of thermal dispersion from cooling water discharge of PT. Badak NGL in Bontang waters, East Kalimantan. Prediction was done using hydrodynamic model and 3-D thermal transport modified from POM (Princeton Ocean Model). Driving forces used in this model were tides, flows of cooling water discharge and rivers discharge. Choice of time step (t)=0.5 second, with 118 grids (west-east) and 187 grids (north-south), grid size Δx=Δy=30 m. Initial value : u=v=ζ=0, T0 = 28 °C and S0 = 32 ‰. Verification of elevation and temperature between results of models and direct measurement showed a good suitability with correlation value was 0.97 and Mean Relative Error (MRE) 1.31% for elevation verification, correlation 0.90 MRE 5.17% and correlation 0.87 MRE 7.12% for thermal verification during spring and neap tides, repectively. Results simulation revealed the most extreem difference in pattern surface thermal dispersion that found during spring tide for sampling condition of maximum tide and ebb. Distinct difference was especially found at station 8 (mixing point) i.e. 41 °C during maximum ebb and 35 °C during maximum high tide. Whereas, significantly high thermal difference between upper layer and bottom layer was found at station C i.e. around 2,54 °C for dry season scenario and 2,32 °C for wet season scenario Key words: POM, cooling-water discharge, thermal dispersion, rivers discharge, numerical model, Bontang waters

Amplitude Variations of Tidal Harmonic Constituents in Bitung Station (Variasi Amplitudo Konstituen Harmonik Pasang Surut Utama di Stasiun Bitung) Salnuddin Salnuddin; I Wayan Nurjaya; Indra Jaya; Nyoman M N Natih
ILMU KELAUTAN: Indonesian Journal of Marine Sciences Vol 20, No 2 (2015): Ilmu Kelautan
Publisher : Marine Science Department Diponegoro University

Perhitungan konstituen harmonik pasang surut masih menggunakan metode konvensional, pengembangan metode dominan pada sistem komputasinya dan menggunakan sistem penanggalan Masehi. Penelitian ini bertujuan untuk mengetahui, apakah amplitudo konstituen harmonik yang dihitung dari pengelompokan data berdasarkan penanggalan Hijriah memberikan karakter yang relatif sama (stabil) dibulan yang sama dibandingkan dengan penanggalan Masehi. Perbandingan tersebut dilakukan pada 10 konstituen harmonik utama pasang surut, guna membandingkan perhitungan tunggang air dari nilai konstituen dan dari Metode Suku Sama (MSS). Hasil analisis data menunjukkan bahwa nilai deviasi amplitudo sangat kecil dari masing-masing konstituen harmonik pada perhitungan berdasarkan sistem kalender Hijriah, dimana amplitudo pada bulan Sya’ban relatif stabil dan lebih tinggi dibandingkan pada bulan lainnya. Nilai koefisien determinan (R2) untuk data awal pasang surut pada fase bulan baru (BB) dan bulan purnama (BP) lebih tinggi dibandingkan data awal pada fase bulan lainnya. ANOVAmenghasilkan konstituen K1dan S2terpengaruh jika data dimulai saat fase bulan kuartil I (KW1) dan purnama (BP), sedangkan saat fase awal kuartil 2 (KW2) terjadi pada konstituen P1 dan K2, MS4 dan M4. Dengan demikian, perhitungan amplitudo konstituen harmonik lebih optimum jika data dimulai saat fase bulan baru atau mengikuti penanggalan Hijriah.

Chart Datum and Bathymetry Correction To Support Managing Coral Grouper In Lepar And Pongok Island Waters, South Bangka Regency Sudirman Adibrata; Fredinan Yulianda; Mennofatria Boer; I Wayan Nurjaya
ILMU KELAUTAN: Indonesian Journal of Marine Sciences Vol 23, No 4 (2018): Ilmu Kelautan
Publisher : Marine Science Department Diponegoro University

Corrected bathimetry data is highly required to improve the quality of sea floor map, for a range of purposes including coastal environmental monitoring and management. This research was aimed to know chart datum values used for correctting bathymetry data at Bar-cheeked coral trout grouper (Plectropomus maculates) fishing ground in Lepar and Pongok Island waters 02o57’00”S and 106o50’00”E and 02o53’00”S and 107o03’00”E, respectively, South Bangka Regency, Indonesia. The study was carried out from November 2016 to October 2017, tidal data used for 15 days from September 16–30, 2017 using simple random sampling technique with the total of 845 points of measurements. To calculate tyde harmonic constituents values this study employed admiralty method resulting 10 major components. Results of this research indicated that harmonic coefficient values of M2, M2, S2, N2, K1, O1, M4, MS4, K2, and P1, were 0.0345 m, 0.0608 m, 0.0276 m, 0.4262 m, 0.2060 m, 0.0119 m, 0.0082 m, 0.0164 m, and 0.1406 m, respectively. Values of mean sea level, chart datum, and F, were 0.9620 m, 0.0500 m, and 0.0664 m, respectively, with diurnal type (F= 6.64). Correcting bathymetry values of surveyed location results a deviation about 1.2 m in depth. The calculated chart datum as well as corrected bathymetry provides information that can be used as vertical refrerence datum for generating sea floor map for determining the fishing ground area of bar-cheeked coral trout grouper. Fishing depth usually ranges between 4.2 and 40.8 m. Average water depth in the fishing ground ranged from 14.7 to 22.5 m.

JAVA COASTAL CURRENT AT NORTHWEST AND SOUTHEAST MONSOON IN SOUTHWEST SUMATRA La Ode Nurman Mbay; I Wayan Nurjaya
Widyariset Vol 14, No 2 (2011): Widyariset
Publisher : Pusbindiklat - LIPI

The Java Coastal Current (JCC) is valuable information since its supplies water mass to South Indonesian water. The data analysis was done using temperature, salinity and depth informations from CTD (Conductivity, Temperature, and Depth). Those informations was calculated based on Neuman and Pierson (1966) with 600 db in reference level, in order to obtain the dynamic topography and geostrophy velocity. The results showed that there was a dynamic depth divergence between shore and the off shore, both was occured in Northwest monsoon and Southeast monsoon. Hence it was acting as a trigger of the geostrophy current toward Southeast with maximum velocity was 18.81 cms -1 and 1.53 sv of transport volume.

ANALISIS TINGKAT PENCEMARAN AIR DENGAN METODE INDEKS PENCEMARAN DI TELUK YOUTEFA, JAYAPURA, PROVINSI PAPUA Janviter Manalu; I Wayan Nurjaya; Surjono HS; Kholil Kholil
BERITA BIOLOGI Vol 10, No 6 (2011)
Publisher : Research Center for Biology-Indonesian Institute of Sciences

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.14203/beritabiologi.v10i6.1942

Youtefa Bay is one of the potential natural recources, is located on the western side of Jayapura City,Papua province.The waters has beenutilized for fishery, transportation and ecotourisme.Youtefa Bay surroundings are settlements where the most of residents are fishermen and farmers.The aim of this study is to determine the pollution level of the Youtefa Bay,approached by pollution index method.The results showed that the water condition of Youtefa Bay was slightly to moderately polluted.Due to pollution, it is therefore very importance to periodically monitor the water quality of the Youtefa Bay to maintain its sustainability.

EVALUASI PERUBAHAN GARIS PANTAI PESISIR TIMUR BANGKA DENGAN METODE DIGITAL SHORELINE ANALYSIS SYSTEM Yogi Cahyo Ginanjar; Yonvitner Yonvitner; I Wayan Nurjaya
Jurnal Perikanan dan Kelautan Vol 11, No 2 (2021)
Publisher : JURNAL PERIKANAN DAN KELAUTAN

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.33512/jpk.v11i2.12226

Kawasan pesisir timur Bangka merupakan kawasan wilayah pesisir yang rentan terhadap tekanan faktor alam seperti bencana gelombang ekstrim dan abrasi serta faktor non alam (manusia). Tujuan penelitian ini adalah untuk mengevaluasi perubahan garis pantai pesisir timur Bangka. Data yang digunakan dalam penelitian ini berupa data citra satelit Landsat 7 tahun 2001 dan citra satelit Landsat 8 tahun 2020, data pasang surut dan batimetri dari BIG (Badan Informasi Geospasial), data angin, data arus dan gelombang yang diperoleh dari Marine Copernicus. Analisis perubahan garis pantai menggunakan kombinasi antara metode End Point Rate (EPR) dan Net Shoreline Movement (NSM) yang merupakan add-in pada aplikasi ArcGIS. Hasil evaluasi perubahan garis pantai pesisir timur Bangka sejak tahun 2001 sampai dengan 2020 menunjukkan bahwa jarak abrasi dengan metode EPR berkisar antara 0,00 sampai -34,07 meter/tahun dan dengan metode NSM berkisar antara 0,00 sampai -647,26 meter sepanjang 175,42 km. Jarak akresi dengan metode EPR berkisar antara 0,00 sampai 34,14 meter/tahun dan dengan metode NSM berkisar antara 0,00 sampai 648,75 meter sepanjang 175,42 km garis pantai yang diteliti.

ANALISIS SENSITIVITAS LINGKUNGAN OSCP (OIL SPILL CONTINGENCY PLAN) DI PESISIR SELATAN DELTA MAHAKAM, PROVINSI KALIMANTAN TIMUR Mursalin Mursalin; I Wayan Nurjaya; Hefni Effendi
Jurnal Pengelolaan Sumberdaya Alam dan Lingkungan (Journal of Natural Resources and Environmental Management) Vol. 4 No. 1 (2014): Jurnal Pengelolaan Sumberdaya Alam dan Lingkungan (JPSL)
Publisher : Graduate School Bogor Agricultural University (SPs IPB)

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.29244/jpsl.4.1.84

The research was one part of oil spill contingency plan (OSCP) developed for Delta Mahakam area, where oil & gas exploration and exploitation linked with rich biodiversity supporting coastal community livelihood. Environmental sensitivity analysis for OSCP only do two early stages of OSCP scope, which integrated with the dangers of coastal vulnerability. This analysis mapped environmental component from oil pollution become sensitivity rangking as an effort to support response development strategies and priorities for the coastal resources protection. The aims of this research were (1) to establish environment sensitivity rank and (2) to identify primary factor supporting the environmental sensitivity for OSCP in south Delta Mahakam area. The result of analysis showed environmenal sensitivity was 62.37% (517.52 km), its mean very high sensitivity. Then the high sensitivity criteria was 11.31% (94 km). The criteria of medium sensitivity was 11.92% (99 km). While for low sensitivity and very low sensitivity respectively were 1.78% (15 km) and 12.64% (105 km). Based on Principal Component Analysis (PCA), 36.01% variability was explained by axis of factor 1. The others variability 18.53% and 13.93% were explained by axis of the factor 2 and factor 3. Axis of factor 1 for coastal exposure (EK), oil residence index (OR), coastal type (TP), and biological resources (SH) had a quite large linear combinations coefficient, amounted to 0.94 (EK&OR), 0.83 (TP) and 0.75 (SH). This indicated a very high contribution for environmental sensitivity OSCP level drafting. On axis of factor 2, the linear coeffisien combinations for the resource utilization of port (PL) was 0.83 and settlement (PM) was 0.85. Axis of factor 3 contributed 0.75 and 0.66 on migas platform (PO) and placement of passive fishing gear/catchment area (AT). However, the utilization of coastal resources for PL, PM, PO and AT were on axis of factor 2 and factor 3 had a considerable distance with its SI variable. This possible caused by each variable percentage distribution which the value was very minor ranged 0.001-0.52%, so its not representated coastal resources elements closeness with SI variable in the study area.Keywords: Environmental Sensitivity, Oil Spill Contingency Plan, Mahakam Delta

PREDIKSI LUASAN AREA TERPAPAR TSS DARI KEGIATAN DREDGING PADA ALUR PEMASANGAN PIPA RC-06 DI ESTUARI DELTA MAHAKAM I Wayan Nurjaya; Andri Purwandani
Jurnal Pengelolaan Sumberdaya Alam dan Lingkungan (Journal of Natural Resources and Environmental Management) Vol. 9 No. 1 (2019): Jurnal Pengelolaan Sumberdaya Alam dan Lingkungan (JPSL)
Publisher : Graduate School Bogor Agricultural University (SPs IPB)

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.29244/jpsl.9.1.135-143

In general, natural resources capable of generating foreign exchange, such as: gas, petroleum and various other minerals are found in locations that have high productivity. Conditions of waters that have high productivity serves to support the sustainability of biological resources (e.g.: fish, mangroves, seagrass beds, seaweed and coral reefs). The government in this case the Ministry of Environment and Forestry (formerly the Ministry of the Environment) actually has made the signs of a rule that must be met by business actors who conduct activities in sensitive areas to environmental changes. PT. Total E & P Indonesia (TEPI) located in Balikpapan has long been engaged in exploration and exploitation of oil and gas in the Mahakam Delta. The large flow of branches of the Mahakam River empties into the Mahakam Delta provides a promising business opportunity for the farmers to open their business. While TEPI has oil wells are scattered in the delta area, pipelines are needed to collect the oil from the wells to the processing site. Because of the large number of streams causing many oil and gas pipes to cross the river (river cross pipes) that require special handling and meet the standards of technical rules and environment set by the government to be safe from passing boats or fishing boats that pass at the location. This study was conducted to predict the extent of exposed areas of exposure, especially the TSS concentration generated from the dredging activities in the pipeline. The simulation results show that the area of impact (TSS> 80 mg / L) is 74275.13 m2 dominantly moving westward from the dredging location (RC-06 = River Crossing Pipe No. 6). The farthest distance of the affected river body (TSS> 80 mg / L) to the west is 557.00 m from RC-06. The farthest distance of the affected river body (TSS> 80 mg / L) to the northeast is 240.81 m from RC-06. The farthest distance of the affected river body (TSS> 80 mg / L) to the southeast is 216.98 m from the RC-06 location. There is no water mass with TSS> 80 mg / L entering the pond. Sedimentation due to dredging activities is not accumulated and has no impact on shrimp farming business. The results of this study is expected to make a scientific basis in helping solve the problem of compensation requested by the farmers to TEPI due to decreased tambak production.

Co-Authors . Sukenda Abdul Aziz, Nandi Abdurrachman Baksir, Abdurrachman Adi Purwandana 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 Aprilia, Jesikha Dwi 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 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 Ety Parwati fadli syamsudin Fani Safitri Ferawati Runtuboi Ferdy Gustian Firdaus, Adil M. Franto Novico Fredinan Yulianda Hari, Restu Fajar 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 I Made Budiasa I Nyoman Kanca I Wayan Gede Astawa Karang 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 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 Mahdi Kartasasmita Manalu, Janviter Marimin , Mario Putra Suhana Mennofatria Boer Muh. Adhim Adrian Muh. Ishak Jumarang Muhamad Muliadi Muhammad Agus Muljanto MUHAMMAD AGUS SUPRAYUDI Muhammad Marzuki Mulia Purba Mulia Purba Mulia Purba Mursalin Mursalin N Natih, Nyoman Metta N, Furqan Najamuddin N Najamuddin Najamuddin, Najamuddin Nebuchadnezzar Akbar Neviaty P Zamani Neviaty P. Zamani Noor, Hariansyah Nugraha, Teguh Nur Asia Umar Nur Audina Nyoman M N Natih Nyoman M.N Natih Okgareta, Dema Paembonan, Rustam E Paputungan, Mohammad Sumiran Pramudyo Dipo Rasidi, Rasidi Rastina Ratu Almira Kismawardhani Ratuluhain, Eva Susan Restu, Yunan Gilang Richardus F Kaswadji Richardus F. Kaswadji Ridha Alamsyah Rikardi, Novit 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 Siti Rohani Solihin Solihin Soma Somantri Sucantra, Made Bayu 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 Vincentius Siregar Wahab, Iswandi Wahyu W Pandoe Wang, Zheng Wibowo, Eko S Widodo S. Pranowo Yidoatimojo, Sudibyo Yogi Cahyo Ginanjar Yonvitner - Yudi Setiawan Yuli Naulita Yusli Wardiatno Zibar, Zan Zulfikar, Andi

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