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All Journal BULETIN OSEANOGRAFI MARINA Journal of Oceanography Journal of Marine Research TRANSIENT: Jurnal Ilmiah Teknik Elektro International Journal of Marine and Aquatic Resource Conservation and Co-existence Jurnal Kelautan Tropis Indonesian Journal of Oceanography

Nugroho Agus D

Unknown Affiliation

Author-ID : 248348

Agriculture, Biological Sciences & Forestry Decision Sciences, Operations Research & Management Earth & Planetary Sciences Electrical & Electronics Engineering Environmental Science Other

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Sebaran Sedimen Tersuspensi di Perairan Teluk Awur Jepara menggunakan Citra Landsat 8 Petrus Subardjo; Agus Anugroho Dwi Suryoputro; Ibnu Praktikto
Buletin Oseanografi Marina Vol 9, No 1 (2020): Buletin Oseanografi Marina
Publisher : Universitas Diponegoro

Sedimen tersuspensi dianggap sebagai sedimen yang didistribusikan oleh arus laut. Arus sepanjang pantai (longshore current) berperan besar terhadap proses perpindahan sedimen di perairan. Gelombang laut yang yang membentuk sudut terhadap garis pantai menyebabkan arus sepanjang pantai Transpor sedimen yang disebabkan oleh arus sepanjang panti sering menimbulkan permasalahan erosi pantai dan pendangkalan perairan. Perairan Teluk Awur memiliki bentuk teluk dan tanjung yang memungkinkan terjadinya arus sepanjang pantai. Potensi adanya proses erosi dan sedimentasi di perairan Teluk Awur membuat pentingnya kajian mengenai pola sebaran sedimen tersuspensi. Penelitian ini mampu menjelaskan tentang pola sebaran sedimen tersuspensi di perairan Teluk Awur, Kecamatan Tahunan, Kabupaten Jepara. Metode yang digunakan untuk penentuan sedimen tersuspensi menggunakan pengindraan jauh dan data yang digunakan yaitu citra satelit landsat-8. Kandungan sedimen tersuspensi tertinggi berada di Desa Teluk Awur dan Desa Demaan. Kandungan tertinggi sebesar ± 67,54 mg/L dan semakin menjauhi pantai konsentrasi menurun. Tingginya kadungan sedimen tersuspensi dipengaruhi oleh proses mixing dan intensitas curah hujan. Suspended sediments are considered as sediments distributed by ocean currents. Current along the coast (longshore current) plays a major role in the process of transfer of sediment in the waters. Sea waves that form angles to the coastline cause currents along the coast Sediment transport caused by currents along the orphanage often cause erosion and coastal silting problems. The waters of Teluk Awur have the shape of bays and headlands which allow currents along the coast. The potential for erosion and sedimentation in the Awur Bay waters makes it important to study the pattern of suspended sediment distribution. This research is able to explain the pattern of suspended sediment distribution in Awur Bay waters, Annual District, Jepara Regency. The method used to determine suspended sediment uses remote sensing and the data used are Landsat-8 satellite imagery. The highest suspended sediment content was in Teluk Awur Village and Demaan Village. The highest content of ± 67.54 mg / L and increasingly away from the beach decreased concentration. The high suspended sediment content is influenced by the mixing process and the intensity of rainfall.

STUDY OF MIXED LAYER DEPTH VARIATION IN LIRAN ISLAND WATERS, SOUTHWEST MALUKU, APRIL 2016 Andriana Kartina Wingtyas; Agus Anugroho Dwi; Anindya Wirasatriya; Muslim Muslim; Teguh Agustiadi
International Journal of Marine and Aquatic Resource Conservation and Co-existence Vol 2, No 1 (2017): IJMARCC
Publisher : International Journal of Marine and Aquatic Resource Conservation and Co-existence

ABSTRACTLiran Island waters are located between two seas, the Banda Sea and the Timor Sea. These waters are also the border between Republic of Indonesia and the Democratic Republic of Timor Leste (RDTL). The thickness of mixed layer depth in Liran Island waters are vary. This is assumed as a result of the influence of transition season I wind that blew in the area in April 2016. This study aims to determine the variation of the thickness layer mixed layer Liran Island waters, Southwest Maluku District on April 2016 caused by the transition season I wind. The methodology that used in this research is descriptive method with quantitative approach. The main data that used in this study is in situ sea temperature data, while the supporting data that used in this study is wind data which measured directly in the field for 9 days. The result of this research is based on determination of layer mixed layer using criterion ΔT = 1.0 0C. The west part of Liran Island had thinnest layer mixed layer depth that is about 20 - 38 m. The east part of Liran Island waters had the thickest mixed layer depth which up to 55 m. Meanwhile, the north part of Liran Island waters had a thickness of mixed layer between the eastern and western waters of 40 m. This related to the wind that blowing from the southwest to the northeast and causing a downwelling phenomenon in the east part of Liran Island waters and upwelling phenomenon in the west part of Liran Island waters while the north part of Liran Island waters did not get a great influence from the movement of the wind because of its location which protected by Liran Island itself. Key words: mixed layer depth, the transitional monsoon I, Liran Island waters

BATHYMETRY MAPPING STUDY AS A CONSIDERATION IN DETERMINING SHIPPING CHANNEL IN PRAMUKA ISLAND WATERS, SERIBU ISLANDS, DKI JAKARTA Agus Anugroho D.S; Petrus Subardjo; Bintang Yosua Cristian M.
International Journal of Marine and Aquatic Resource Conservation and Co-existence Vol 2, No 1 (2017): IJMARCC
Publisher : International Journal of Marine and Aquatic Resource Conservation and Co-existence

ABSTRACTBathymetry is a method or technique in determining sea-depth or seabed profile from the result of sea-depth analysis. Bathymetry data is an important data used as shipping channel consideration, especially in Pramuka Island Waters, Seribu Islands, DKI Jakarta. Determining shipping channel in Pramuka Island Waters is really important as the reference for secure sea traffic. The purpose of this study is to know bathymetry condition used as consideration in determining shipping channel in Pramuka Island Waters, Seribu Islands, DKI Jakarta. This reasearch was conducted in August, 4th – 6th 2016 on waters and dock of Pramuka Island, Seribu Islands, DKI Jakarta. The materials used as objects of this study are tidals, bathymetry and seabed morphology in Pramuka Island, Seribu Islands, DKI Jakarta. This research used case study method, i.e., research methods conducted intensively and detailed on a case, can be environment, certain situation to reveal or to understand something and the result can not be used in other areas. Case study in this research is knowing sea-depth. In this case, the result of this research which are bathymetry and shipping channel, cannot applied in other areas. Data processing using software Surfer 9.0, Arc Gis 10.3 and Microsoft Excel. The result of this research indicate that sea-depth in research location have depth between -0,7 until -38,6 m. Seabed morphology in Pramuka Island Waters was included in sloping category, with the slope value of 2,57% untill 10,12%. Tidal type is diurnal type with Formzahl value 3,34. Consideration of shipping channel due to vessel traffic is channel from North Jakarta direction and from other islands direction heading Pramuka Island. Key words: bathymetry, shipping channel, pramuka island waters

THE INFLUENCE OF OCEAN CURRENTS TOWARDS DISTRIBUTION OF TOTAL SUSPENDED SOLIDS VERTICALLY IN CILALANANG ESTUARY, DISTRICT INDRAMAYU Gentur Handoyo; Petrus Subardjo; Agus Anugroho Dwi; Muhammad Sulaiman
International Journal of Marine and Aquatic Resource Conservation and Co-existence Vol 2, No 1 (2017): IJMARCC
Publisher : International Journal of Marine and Aquatic Resource Conservation and Co-existence

ABSTRACTCilalanangriver located in the village of EretanWetan, District Indramayu. There are Fishery Harbor Beach (PPP) and shipping activities in this region is quite high. Activities in the PPP could potentially lead to silting due to the material carried by the river flow. The purpose of this study to determine the concentration of total suspended sediment (TSS) and the influence of ocean currents on the TSS in Cilalanang Estuary, District Indramayu. The research is located at coordinates 1080 4’ 53.400” EL -1080 5’ 50.215” EL and 60 19’ 26.709” SL - 6019’ 26.720” SL. The method used in this research is quantitative method. Analysis of the TSS is done by making the TSS distribution maps using ArcGIS10.5 and modeling ocean currents using MIKE 21. The results showed that the concentration of TSS at low tide toward the high tide is worth between 286-888 mg / l whereas when the high tide towards low tide worth between 348-553 mg / l. Dominant ocean current direction at the time of low tide to the hightide leads to the southwest. This causes TSS concentration coming out of the mouth of the river converge toward the southwest near the shore. In conditions of high tide toward low tide the dominant current direction leads to the northeast. This led to the spread of TSS concentration coming out mouth of the river away from the shore. Key words: Cilalanang River, IndramayuDistrict,Ocean Currents, Ocean Tides, Total Suspended Solids

Korelasi Klorofil-a dengan Nutrien dan Kualitas Perairan di Pulau Seruni Karimunjawa Indonesia Rikha Widiaratih; Agus Anugroho Dwi Suryoputra; Gentur Handoyo
Jurnal Kelautan Tropis Vol 25, No 2 (2022): JURNAL KELAUTAN TROPIS
Publisher : Universitas Diponegoro

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.14710/jkt.v25i2.14170

Seruni Island is one of the islands located in the easternmost and is an uninhabited island in Karimunjawa, Jepara Regency, Central Java. Seruni Island has a tourist attraction, namely a stretch of white sand, coral reefs, and which is currently used by local people for seaweed cultivation. There are still many tourism opportunities and marine utilization that have not been utilized optimally. Knowing the availability of chlorophyll-a and its correlation with nutrients (ammonia, nitrate, and phosphate) and water quality on Seruni Island can provide an initial overview of the fertility conditions of the waters on Seruni Island so that other marine utilization opportunities can be wide opened. In situ data are collected such as seawater samples, which are then analyzed in the laboratory, as well as water quality parameters including salinity, pH, DO, temperature and brightness. Although Seruni Island is an uninhabited island, however, it is possible that there will be runoff from the surrounding inhabited islands, which will increase the concentration of chlorophyll-a. The results showed that chlorophyll-a had a high and negative correlation with nutrients, namely ammonia (r=-0.985), and water quality, namely temperature and brightness (r=-0.895 and r=-0.734). Pulau Seruni merupakan salah satu pulau yang lokasinya terletak paling timur dan merupakan pulau tidak berpenghuni di Karimunjawa, Kabupaten Jepara Jawa Tengah. Pulau Seruni memiliki daya tarik wisata yaitu hamparan pasir putih, terumbu karang, dan yang saat ini dimanfaatkan masyarakat setempat untuk budidaya rumput laut. Masih banyak peluang wisata dan pemanfaatan bahari yang belum dimanfaatkan secara optimal. Dengan mengetahui ketersediaan klorofil-a dan korelasinya terhadap nutrien (ammonia, nitrat dan fosfat) dan kualitas perairan di Pulau Seruni dapat memberikan gambaran awal terkait kondisi kesuburan perairan yang ada di Pulau Seruni, sehingga dapat terbuka peluang pemanfaatan bahari lainnya. Data in situ yang diambil berupa sampel air laut, yang selanjutnya dianalisis di laboratorium, serta parameter kualitas perairan meliputi salinitas, pH, DO, suhu dan kecerahan. Walaupun Pulau Seruni merupakan pulau yang tidak berpenghuni, namun demikian tidak menutup kemungkinan terdapat limpasan massa air yang berasal dari pulau sekitarnya yang berpenghuni yang berdampak pada meningkatnya konsentrasi klorofil-a. Hasil penelitian menunjukkan klorofil-a memiliki korelasi yang tinggi dan bernilai negatif dengan nutrient, yaitu ammonia (r=-0,985), dan kualitas perairan yaitu suhu dan kecerahan (r=-0,895 dan r=-0,734). Kata kunci : klorofil-a, nutrient, kualitas perairan, Korelasi, P.Seruni

Pengaruh Arus terhadap Sebaran Horizontal Suhu dan Salinitas pada 3 Kedalaman yang Berbeda di Perairan Samudera Hindia Bagian Selatan Pulau Jawa Sagita Difa Wardhani; Agus Anugroho Dwi Suryo; Warsito Atmodjo; Elis Indrayanti; Baskoro Rochaddi
Indonesian Journal of Oceanography Vol 3, No 2 (2021): Indonesian Journal of Oceanography
Publisher : University of Diponegoro

Perairan Samudera Hindia bagian Selatan Pulau Jawa merupakan perairan yang dinamis karena dipengaruhi oleh sistem monsun yang memicu sistem arus musim. Perubahan kecepatan arus dapat menyebabkan pergerakan lapisan pada permukaan laut yang membangkitkan pengadukan dan percampuran secara horizontal sehingga kecepatan dan arah arus merupakan salah satu faktor penting penyebaran suhu maupun salinitas pada kolom perairan. Keterkaitan yang kompleks antar parameter oseanografi di perairan Samudera Hindia bagian selatan Pulau Jawa terutama kondisi arus, angin, suhu, dan salinitas sangat menarik untuk diteliti dan dipelajari. Tujuan penelitian ini yakni mengetahui pengaruh arus terhadap sebaran horizontal suhu dan salinitas pada mixed layer, thermocline/halocline, dan deep layer. Pada penelitian ini menggunakan data arus, suhu, dan salinitas bulanan (Januari 2014-Desember 2018) reanalysis dari Marine Copernicus. Data tersebut diolah menggunakan Interactive Data Language (IDL) dengan metode komposit dan korelasi pergrid. Berdasarkan hasil penelitian didapatkan bahwa arus permukaan Musim Peralihan 2 bergerak paling kencang mencapai 0,266 m/s, dengan suhu permukaan terpanas yakni 30oC pada Musim Peralihan 1 dan kadar salinitas tertinggi berada pada lapisan dalam mencapai 34,8-34,875 psu terutama saat Musim Peralihan 1. Pengaruh arus terhadap sebaran horizontal suhu dan salinitas pada mixed layer, thermocline/halocline, dan deep layer cukup lemah yang dibuktikan dengan semakin kencang arus maka nilai suhu belum tentu rendah dan nilai salinitas tinggi.

Penggunaan Seismik Refleksi Dalam Pencarian Potensi Endapan Timah di Perairan Laut Bangka Muhammad Alif Achyansyah; Baskoro Rochaddi; Alfi Satriadi; Muslim Muslim; Agus Anugroho Dwi Suryoputro; Azis Rifai; Muh Yusuf
Indonesian Journal of Oceanography Vol 2, No 4 (2020): Indonesian Journal of Oceanography
Publisher : University of Diponegoro

Indonesia merupakan negara kepulauan yang kaya akan sumber daya alam mineral salah satunya adalah timah, yang tersebar di Perairan Pulau Bangka. Secara umum timah terbentuk oleh pembentukan magma asam akibat proses peleburan kerak benua pada proses kolisi. Timah terbagi menjadi timah primer yang masih dalam bentuk batuan granit dan timah sekunder (placer) merupakan endapan timah primer yang telah mengalami pelapukan akibat proses erosi dan diendapkan di suatu tempat yang tidak jauh dari endapan timah primer. Salah satu metode untuk mengetahui potensi endapan timah adalah dengan menggunakan metode seismik refleksi, dengan pendekatan pencarian lembah sungai purba, tempat mengendapnya timah. Penelitian ini bertujuan untuk mengetahui potensi endapan timah sekunder (placer) berupa endapan kaksa, yang merupakan lapisan mengandung endapan timah, dengan melakukan perhitungan volume dan ketebalannya menggunakan metode seismik refleksi. Hasil pengolahan data seismik menunjukkan pola konfigurasi refleksi yang ditemukan antara lain parallel, chaotic, shingled dan hummocky. Korelasi antara data pemboran dan seismik refleksi menunjukkan endapan kaksa berada di lembah sungai purba yang terisi oleh endapan aluvial dan mineral kasiterit. Berdasarkan perhitungan yang dilakukan, didapatkan volume endapan kaksa, sebesar 1.078.054,15 m3, dengan ketebalan mencapai 5 meter. Indonesia is an archipelago country which is rich in mineral resources, one of them is tin, that spread in Bangka Island Waters. Generally, tin formed by acid magma formation caused by melting of continental crust process in the collision process. Tin divided to primary tin which is still in granite rock form and secondary (placer) tin which is primary tin deposit that has experienced weathering caused by erosion process and deposited in a place not far from primary tin deposit. One of method to know potential tin deposit is using seismic reflection method, with approach ancient river valley hunting, where tin was deposited. The purpose of this research is to know the potential of the secondary (placer) tin deposit in the form of kaksa deposit, this layer contains of tin deposit, with calculation of volume and thickness using seismic reflection method. The result from seismic data showed that the reflection configuration found i.a parallel, chaotic, shingled and hummocky. The correlation between drilling data and seismic data showed that kaksa deposit is located in ancient river valley that contains of alluvial deposit and cassiterit mineral. Based on the calculation, the volume of kaksa deposit is 1.078.054,15 m3, and the thickness is up to 5 meters.

Analisis Sebaran Salinitas Pasca Pembangunan Tanggul Wonokerto Sungai Bedahan Kabupaten Pekalongan Bima Andriantama; Petrus Subardjo; Gentur Handoyo; Kunarso Kunarso; Agus Anugroho Dwi Suryoputro
Indonesian Journal of Oceanography Vol 3, No 1 (2021): Indonesian Journal of Oceanography
Publisher : University of Diponegoro

Kabupaten Pekalongan merupakan wilayah yang terletak di bagian utara Pulau Jawa yang berbatasan langsung dengan laut Jawa yang banyak terdapat sungai yang bermuara langsung menuju Laut Jawa, salah satunya Muara Bedahan. Pada lokasi penelitian terdapat tambak, Tempat Pelelangan Ikan dan sebagai jalur pelabuhan kapal nelayan. Masyarakat pesisir setempat mengandalkan pasokan air payau dari aliran Sungai Bedahan, namun mereka kesulitan memperoleh air bersih sebelum Tanggul Wonokerto dibangun. Tujuan dari penelitian iniadalah untuk mengetahui pola sebaran salinitas sesaat dan sebelum Tanggul Wonokerto selesai dibangun. Penelitian ini dilakukan pada Februari 2020 dan Juni 2020 saat kondisi surut menuju pasang. Variabel yang diamati yaitu data utama berupa data salinitas, kedalaman, dan pasang surut. Titik stasiun penelitian tersebar dari sungai dekat pemukiman penduduk hingga perairan muara. Data yang diperoleh selanjutnya diolah menggunakan ODV 4 dan dianalisis secara deskriptif. Hasil penelitian menunjukkan bahwa Muara Bedahan memiliki pola distribusi salinitas di wilayah hulu penelitian hingga tanggul, sebelum tanggul jadi di permukaan (0,2D) rata-rata sekitar 11,47 ppt dan di lapisan dasar (0,8D) 15,44 ppt. Setelah tanggul jadi dipermukaan (0,2D) rata-ratanya 11,2 ppt dan di lapisan dasar (0,8D) 15,4 ppt. Kedalaman maksimum lokasi penelitian 4 m dengan tipe pasang surut wilayah Pekalongan campuran condong harian tunggal.

Analisis Batimetri Guna Perencenaan Pengerukan Kolam Pelabuhan I, Tanjung Priok, Jakarta Utara Yeremia Sudibyo; Agus Anugroho Dwi Suryoputro; Hariyadi Hariyadi; Petrus Subardjo; Rikha Widiaratih
Indonesian Journal of Oceanography Vol 3, No 2 (2021): Indonesian Journal of Oceanography
Publisher : University of Diponegoro

Kolam Pelabuhan I Tanjung Priok, Jakarta merupakan pelabuhan yang digunakan untuk aktivitas pelayaran dan bongkar muat kapal. Informasi mengenai batimetri sangat diperlukan guna menunjang kegiatan dalam pelayaran. Tujuan dari penelitian ini yaitu memetakan batimetri di area kolam pelabuhan dan mengetahui area pengerukan di Kolam Pelabuhan I Tanjung Priok, Jakarta. Penelitian dilaksanakan pada tanggal 22 Agustus sampai dengan 27 September 2018 di Kolam Pelabuhan I Tanjung Priok, Jakarta Utara. Penelitian ini dilakukan dengan menggunakan Singlebeam Echosounder Teledyne Odom Echotrack MKII untuk mengetahui kedalaman kolam pelabuhan. Pengolahan data menggunakan perangkat lunak Hypack 15.0, ArcGIS 10.3 dan Surfer 14.0 untuk menghasilkan kontur kedalaman. Hasil penelitian menunjukan bahwa kedalaman perairan Pelabuhan Tanjung Priok berkisar antara 6 hingga 15 meter. Kedalaman pelabuhan memiliki kontur yang semakin renggang apabila semakin masuk ke bagian dalam kolam pelabuhan.

Analisis Spektrum Gelombang Di Perairan Pulau Panjang Mizan Zikrullah Abdulkadir; Indra Budi Prasetyawan; Denny Nugroho Sugianto; Agus Anugroho Dwi Suryoputro; Heriyoso Setyono; Petrus Subardjo
Indonesian Journal of Oceanography Vol 1, No 1 (2019): Indonesian Journal of Oceanography
Publisher : University of Diponegoro

Pulau Panjang merupakan salah satu pulau yang dikategorikan sebagai pulau kecil dan terdapat di Kelurahan Ujungbatu, Kecamatan Jepara, Kabupaten Jepara, Provinsi Jawa Tengah. Masalah yang dihadapi Pulau Panjang adalah erosi yang semakin menggerus bibir pantai dan mulai merusak bangunan yang berada di pinggir pantai. Tujuan dilakukannya penelitian ini adalah untuk mengetahui spektrum gelombang dan karakteristik gelombang di Perairan Pulau Panjang, Jepara, Jawa Tengah. Metode yang digunakan dalam penelitian ini bersifat kuantitatif. Software yang digunakan dalam penelitian ini adalah Surface Water Modelling System (SMS) dengan modul STWAVE. Hasil pengolahan data lapangan menunjukkan bahwa tinggi gelombang maksimum adalah sebesar 0,435 meter dengan periode 6,5 detik. Tinggi gelombang signifikan (Hs) 0,219 meter dengan periode gelombang signifikan (Ts) 3,1 detik. Hasil pemodelan spektrum gelombang menunjukkan bahwa nilai energi gelombang berbanding lurus dengan nilai tinggi gelombangnya. Pulau Panjang is one of the islands which is categorized as a small island and is located in Ujungbatu Village, Jepara District, Jepara Regency, Central Java Province. The problem faced by Panjang Island is erosion which increasingly erodes the shoreline and begins to damage buildings on the beach. The purpose of this study is to knowing the wave spectrum and characteristic of waves at Panjang Island, Jepara. The research was conducted on 7 March – 11 March 2019 at Panjang Island Waters. The methods used in this study were quantitative methods. The software used in this study is the Surface Water Modelling System (SMS) with STWAVE module. The result of the field data shows that the maximum wave height was 0,435 meters with a period of 6,5 seconds. Significant wave height (Hs) was 0,219 meters with a significant wave period (Ts) of 3,1 seconds. Based on the result of wave spectrum models it can be concluded that the wave energy value have linear condition with the wave height value.

Co-Authors Abdillah Ranadipura Ade Firdaus Triagusta Afidyah Vicky Antari Agus Indarjo Agus Indarjo Agus Trianto Agus Trianto Ahmad Nur Huda Aini, Firly Nur Ajub Ajulian Zahra Macrina Akhmad Hanan Aldi Nuary Nuary Aldi Nuary Nuary Alfi Satriadi Alvin Hidayat, Alvin Andita Agung Andnur, Mohammad Octa Andriana Kartina Wingtyas Angga Dwi Saputra Anggardha Ayu Pratiwi Anindya Wirasatriya Anissa Cintya Andika Asri Apriliawan Setiya Ramadhany Apriliawan Setiya Ramadhany Ari Soebekti Aris Ismanto Azis Rifai Azra, Mhd Rayhan Baskoro Rochaddi Bima Andriantama Bintang Yosua Cristian M. Dayinta Andayani Denny Nugroho Sugianto Dewi Masyitoh Syihab Dewi Vidya Nuur Isrotunnisaa Nuarita Pratiwi Dewi Vidya Nuur Isrotunnisaa Nuarita Pratiwi, Dewi Vidya Nuur Isrotunnisaa Dwi Haryo Ismunarti Dwi Haryo Ismunarti Elis Indrayanti Galih Tristianto Gentur Handoyo Gersanandi Gersanandi Hadi Endrawati Hanifa Zuhaira Hariadi Hariadi Hariyadi Hariyadi Hendana Pristiwan Hendra Frederick, Hendra Heriyoso Setyono Heryoso Setiyono Ibnu Praktikto Ibnu Pratikno Ilham Panra, Ilham Indra Budi Prasetyawan Irfan Hafizhurrahman Ivan Febriansyah Jarot Marwoto Junika Ahmad Fathonah, Junika Ahmad Karlina Putri Diani Kunarso Kunarso Lilik Maslukah Manurung, Jefri Gunawan Misbah Riyandi Fauzi Muh Yusuf Muhamad Azhar Fathurahman Muhammad Abdul Chafid Muhammad Abdul Chafid Muhammad Alif Achyansyah Muhammad Bani Putra Utama Muhammad Helmi Muhammad Helmi Muhammad Sababa Alhaq Muhammad Sulaiman Muhammad Zainuri Mukti Trenggono Muslim Muslim Osen Faber Romario Tampubolon Petrus Subardjo Pratiwy, Essy Purwanto Purwanto Puteri Kesuma Dewi Putu Suryaniti Dewi Reiner, Muhammad Rikha Widiaratih Riki Tristanto Rizky Aditya Rudhi Pribadi Rudhi Pribadi Sabilu, Kadir Sagita Difa Wardhani Siti Rahmi Prameswari Sitinjak, Dedy Febrianto Sri Redjeki Sri Yulina Sri Yulina Wulandari Sugeng Widada Surya Agung Nugroho Surya Nugraha Syaiful Syakinah Maghfirah Ayu Tarhadi Tarhadi Taufiq Hidayat Teguh Agustiadi Warsito Atmodjo Yeremia Sudibyo

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