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Hairul Basri
Universitas Syiah Kuala
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Analysis of Soil Quality as Hydrological Disaster Mitigation Efforto in Krueng Jreue Sub-Watershed, Great Aceh (retracted due to double publication) Helmi Helmi; Hairul Basri; Sufardi Sufardi; Helmi Helmi
Aceh International Journal of Science and Technology Vol 6, No 2 (2017): August 2017
Publisher : Graduate Program of Syiah Kuala University

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.13170/aijst.6.2.5654

Abstract

This paper is retracted by editor due to publication ethics missconducted by author (simultaneously publication in other journal).
Development of Rainfall-runoff Model Using Tank Model: Problems and Challenges in Province of Aceh, Indonesia Hairul Basri
Aceh International Journal of Science and Technology Vol 2, No 1 (2013): April 2013
Publisher : Graduate Program of Syiah Kuala University

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (639.857 KB) | DOI: 10.13170/aijst.2.1.574

Abstract

Abtstract - Rainfall-runoff model using tank model founded by Sugawara has been widely used in Asia. Many researchers use the tank model to predict water availability and flooding in a watershed. This paper describes the concept of rainfall-runoff model using tank model, discuss the problems and challenges in using of the model, especially in Province of Aceh, Indonesia and how to improve the outcome of simulation of tank model. Many factors affect the rainfall-runoff phenomena of a wide range of watershed include: soil types, land use types, rainfall, morphometry, geology and geomorphology, caused the tank model usefull only for concerning watershed. It is necessary to adjust some parameters of tank model for other watershed by recalibrating the parameters of the model. Rainfall runoff model using the tank model for a watershed scale is more reasonable focused on each sub-watershed by considering soil types, land use types and rainfall of the concerning watershed. Land use data can be enhanced by using landsat imagery or aerial photographs to support the validation the existing of land use type. Long term of observed discharges and rainfall data should be increased by set up the AWLR (Automatic Water Level Recorder) and rainfall stations for each of sub-watersheds. The reasonable tank model can be resulted not only by calibrating the parameters, but also by considering the observed and simulated infiltration for each soil and land use types of the concerning watershed. Key words: rainfall-runoff model, tank model, infiltration, land use types, soil types, watershed
Physical Characteristics Of The Krueng Seunagan Watershed And River Storage Capacity Against Peak Discharge Afriadi Ihsan; Muhammad Rusdi; Hairul Basri
Aceh International Journal of Science and Technology Vol 10, No 3 (2021): December 2021
Publisher : Graduate Program of Syiah Kuala University

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (897.754 KB) | DOI: 10.13170/aijst.10.3.19150

Abstract

Peak discharge information is indispensable for flood control planning by taking into account the physiographic factors of the watershed. Flood occurs because the capacity of the watershed and river channels is smaller than the flood discharge. One of the causes of rivers' reduced flood flow capacity is vegetation cover and land use that cannot store rainfall. Thus, this paper aims to determine the peak discharge from the watershed's physical characteristics and land-use changes by comparing the river storage capacity in the Krueng Seunagan watershed. The rational method is used to calculate the peak discharge. Some of the data used in this study are the shapefile map provided by Geospatial Information Agency, land use, rainfall, soil types, and Landsat 8 OLI/TIRS digital imagery. Analysis of the physical characteristics of the watershed consists of morphology and morphometry. Land use in the area of the Krueng Seunagan watershed increased the peak discharge during the observation year (2003-2017). Besides the land-use factor, discharge is also influenced by high rainfall intensity and runoff coefficient obtained from land use analysis. In the Krueng Seunagan watershed area, the C value obtained was 0.0505 – 0.0720, indicating that the Krueng Seunagan watershed area was classified as good or harmless. The river flow density of 0.53 belongs to the medium category. The river flow increases and decreases in the flood water level, which is neither too fast nor too slow. The roundness index of the Seunagan watershed of 1.0004 indicates that the basins are widened or circular and, consequently, the rate and volume of surface runoff are fast. Krueng Seunagan watershed runoff coefficient increased by 42.51% and rainfall intensity by 37.05%, while discharge increased by 95.31%. The discharge capacity that the Krueng Seunagan River Basin can accommodate from the measurement results in the downstream watershed is 158.47 m3/sec. While the peak discharge using the rational method gets a value that varies in each year of observation from (2003-2017). The peak discharge value in 2003 amounted to 183.52 m3/sec, and the highest in 2017 amounted to 358.44 m3/sec. This shows that the river holding capacity in the Krueng Seunagan watershed will not accept the amount of peak discharge, and consequently, the flood will always occur.
Flood Rate Assessment of the Woyla River Watershed, Aceh Province, Indonesia Rifa Alayani; Sugianto Sugianto; Hairul Basri
Aceh International Journal of Science and Technology Vol 10, No 2 (2021): August 2021
Publisher : Graduate Program of Syiah Kuala University

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1521.662 KB) | DOI: 10.13170/aijst.10.2.19701

Abstract

This study aims to assess Flood susceptibility and flood hazard levels and obtain the distribution of hazard levels and flood hazards in the Woyla watershed, Aceh Province. This research design generally uses a descriptive survey method and divide into several stages, such as data collection, data processing, data presentation, and delivery of research results. Each determinant of flood-prone areas includes a land slope, altitude, soil texture, drainage, land cover, and rainfall, analyzed spatially utilizing a map. Furthermore, based on the map, the regions are described based on the values that have been divided into classes. The results showed that the level of flood vulnerability in the Woyla watershed was divided into five classes, namely; the non-vulnerable class with an area of 14.88 Ha / 0.01%, low prone with an area of 90,731.62 Ha / 35.45%, medium with an area of 57,120.35 Ha / 22.32%, high with an area of 44,918.15 Ha / 17.55%, and very high with an area of 63,151.72 Ha / 24.67%. Also obtained a map of the distribution of flood hazard areas, the Woyla watershed area is divided into five classes, namely; the very light class with an area of 179,146.15 Ha / 70.00%, mild with an area of 32,868.84 Ha / 12.84%, moderate with an area of 20,129.93 Ha / 7.87%, danger with an area of 6.007. 29 Ha / 2, 35%, and very dangerous with an area of 17,784.51 Ha / 6.95%. The level of flood vulnerability in the Woyla watershed is dominant in West Aceh Regency, which is in the very high and high category classes with a total area of 56,876.65 Ha and 23,527.40 Ha. Meanwhile, the level of flood hazard in the Woyla watershed is also more dominant in West Aceh Regency than falls into the most dangerous and dangerous class category with a total area of 17,784.51 Ha and 6,007.29 Ha. With the largest part in the very light class at the flood hazard level of 179,146.15 ha.
Potential Biomass Evaluation on Forest Plant Stands In Aceh Province, Indonesia: A Case Study of Forest Product Utilization Permit for Cultivated Forest Area by PT. Acehnusa Indrapuri Hairul Basri; Dahlan D; Deden Nurochman
Aceh International Journal of Science and Technology Vol 1, No 3 (2012): December 2012
Publisher : Graduate Program of Syiah Kuala University

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (249.535 KB) | DOI: 10.13170/aijst.1.3.135

Abstract

Abstract – Development of industrial forest plantation currently has a primary function to produce timber for the fulfillment of the pulp and paper industry raw matter. In times of growing trees plantations have the ability to absorb carbon dioxide gases (CO2) in the atmosphere throught the process of photosynthesis which builds biomass stands and produce oxygen gases (O2). The potency of forest stands biomass and build a model standing stock biomass using the Normalized Difference Vegetation Index (NDVI) value from Satellite Imagery was investigated. Types of crops grown in Forest Product Utilization Permit for Cultivated Forest Area in PT.Acehnusa Indrapuri are A.mangium and E.urophylla plantations with area approximately 15,500.59 ha. The results showed the biomass content at the lowest value 16.81 tons per hectare with the NDVI Value of 0.342 whereas the highest content of biomass amounted to 145.750 tons per hectare in NDVI value 0.813. The content of plant biomass of forest stands can be expected by NDVI values using the model equation Y = 250.32 X 2 -15.221X- 3.3623 with R2 of 97.27%
Inggris Mirza Junianto; Sugianto Sugianto; Hairul Basri
Jurnal Penelitian Pendidikan IPA Vol. 9 No. 3 (2023): March
Publisher : Postgraduate, University of Mataram

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.29303/jppipa.v9i3.2963

Abstract

This study aims to analyze changes in land cover and mangrove crown density in Langsa Barat District for the period 2000-2020. The method used in this study is the maximum likelihood classification (MLC) to determine changes in mangrove land cover while determining mangrove density using the NDVI equation. Based on the results of the analysis of changes in mangrove land cover there was an increase and decrease in area. In 2000 the area of ​​mangrove land was 1,039.17 ha, then increased in area in 2005 amounted to 1.325,59 ha (27.56%).  In 2010, the mangrove area decreased by 1.145,22 ha (15.75%).  In 2015, the mangrove area increased to 1,357.10 ha (18.50%), and finally, in 2020 there was an increase in the mangrove area to 2.027.05 ha (49.37%). While the analysis of mangrove crown density using NDVI value from 2000 to 2020, the highest crown density value was in 2020 with the category of the dense crown density of 1,509.40 ha (74.46%), while the medium crown density value was recorded in 2020 namely 517.49 ha (25.53%). Meanwhile, the lowest sparse category canopy density value was recorded in 2020 with an area of ​​0.17 ha (0.01%).
Evaluasi Debit Puncak Sub DAS Krueng Seulimum Kabupaten Aceh Besar Intan Ridha Putri; Muhammad Rusdi; Hairul Basri
Jurnal Ilmiah Mahasiswa Pertanian Vol 4, No 2 (2019): Mei 2019
Publisher : Fakultas Pertanian, Universitas Syiah Kuala

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (508.078 KB) | DOI: 10.17969/jimfp.v4i2.11072

Abstract

Abstrak. Pemanfaatan lahan yang kurang bijak oleh masyarakat dapat menyebabkan terjadinya gangguan ekosistem seperti terganggunya tata air pada suatuDAS sehingga bisa mengakibatkan terjadinya banjir dan erosi. Karakteristik banjir cenderung makin besar ditandai dengan peningkatan debit puncak.Dilihat dari penyebabnya, peristiwa banjir tersebut banyak disebabkan karena adanya alih fungsi lahan dan pemanfaatan lahan yang tidak tepat. Penelitian ini bertujuan untuk mengetahui besarnya perubahan debit puncak yang terjadi pada tahun 2010 dan 2017 pada Sub DAS Krueng Seulimum Kabupaten Aceh Besar.Penelitian ini dilaksanakan pada Sub DAS Krueng Seulimum Kabupaten Aceh Besar. Penelitian ini menggunakan metode survei deskriptif dengan menggunakan data atribut dan data spasial. Data atribut berupa data curah hujan harian maksimum tahun 2010 dan 2017. Data spasial berupa citra satelit penggunaan lahan tahun 2010 diperoleh melalui google earth pro, citra satelit penggunaan lahan tahun 2017 diperoleh melalui SAS Planet. Hasil penelitian menunjukkan nilai koefisien limpasan meningkat dari 0,056 tahun 2010 menjadi 0,061 tahun 2017. Nilai debit puncak mengalami peningkatan, dimana pada tahun 2010 nilai debit puncak sebesar 32,896 m3/dt menjadi 39,102 m3/dt pada tahun 2017. Hal ini dikarenakan adanya perubahan penggunaan lahan pada hutan sehingga kemampuan daya serap tanah terhadap air hujan semakin menurun. Secara umum kondisi Sub DAS Krueng Seulimum masih tergolong baik karena peningkatan nilai koefisien limpasan dan debit puncak tidak terlalu signifikan.Of Peak Discharge Evaluation On Sub Watershed Of Krueng Seulimum Aceh Besar DistrictAbstract.  Unwise use of land by society can cause of disturbance ecosystem as disturbed water system on watersheds that result in occurrence flood and erosion. The characteristics of floods tend to be greater marked by an increase in peak discharge. Seen from causes, events flood that is many because existence take over function land and utilization land that is not right. This research aim for knowing the magnitude changes in the peak discharge that occur in 2010 and 2017 on Subwatershed of Krueng Seulimum Aceh Besar District. The research was conducted on Subwatershed of Krueng Seulimum Aceh Besar District. This research use descriptive survey method using attribute data and spatial data. Attribute data in the form of maximum daily rainfall data in 2010 and 2017. Spatial data form of land use satellite imagery in 2010 was obtained through google earth pro, satellite imagery of land use in 2017 was obtained through SAS Planet.The study states use value coefficient runoff increase from 0,056 in 2010 to be 0,061 in 2017. Peak discharge value experience increase, where in 2010 the peak discharge value amounting to 32,896 m3/dt becomes 39,102 m3/dt in 2017. This is due to land use changes in the forest so that the capability to absorption land agains rain water descreases. In generally condition on Sub watershed of Krueng Seulimum  still classified good because the increase in values runoff coefficient and peak discharge  is not too significant.
perubahan sifat fisika tanah di lahan kering tanah ultisol dengan jenis tanaman dan mulsa jagung Muzakki Muzakki; Manfarizah Manfarizah; Hairul basri
Jurnal Ilmiah Mahasiswa Pertanian Vol 3, No 2 (2018): Mei 2018
Publisher : Fakultas Pertanian, Universitas Syiah Kuala

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (394.29 KB) | DOI: 10.17969/jimfp.v3i2.7470

Abstract

Abstrak :Penelitian ini bertujuan untuk mengetahui pengaruh penggunaan mulsa jagung dan jenis tanaman dilahan kering tanah Ultisol terhadap beberapa sifat fisika tanah. Penelitian menggunakan Rancangan Petak Terpisah pola RAK 3 x 4 dengan 3 ulangan. Faktor yang diteliti yaitu jenis tanaman dan mulsa jagung. Faktor jenis tanaman terdiri dari 3 taraf yaitu ; jagung, kedelai dan kacang tanah. Faktor s mulsa jagung terdiri atas 4 taraf  yaitu ; kontrol, tanpa mulsa, mulsa jagung 5 ton ha-1 dan mulsa jagung 10 ton ha-1 . Hasil penelitian menunjukkan bahwa perlakuan jenis tanaman  memberikan pengaruh nayata terhadap indeks stabilitas agtregat. Terdapat pengaruh interaksi antara perlakuan jenis tanaman dan mulsa jagung terhadap partikel density. Changes of soil physical properties on Soil Sloping Land Ultisol with types of plants and Mulch on cornAbstract. This research aims to know the influence of the use of the mulching corn and plant type dilahan dry land of Ultisol against some physical properties of the soil. The research of using Separate Swath Design pattern SHELF 3 x 4 with 3 replicates. Factors examined, i.e. the type of mulch and plant corn. Crop factor consists of 3 levels namely; corn, soybeans and peanuts. Factor s mulching maize consists of 4 levels, namely; control, without mulch, mulch corn 5 ton ha-1 and mulching corn 10 ton ha-1. The results showed that the treatment plant type influence nayata against agtregat stability index. There is the influence of the interaction between the treatment plant and mulch in corn against particle density..
Kajian Alih Fungsi Lahan Pertanian Menjadi Non Pertanian di Kabupaten Bireuen Syarifah Renny Fauzi; Hairul Basri; Helmi Helmi
Jurnal Ilmiah Mahasiswa Pertanian Vol 1, No 1 (2016): November 2016
Publisher : Fakultas Pertanian, Universitas Syiah Kuala

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (244.723 KB) | DOI: 10.17969/jimfp.v1i1.981

Abstract

Penggunaan lahan pemukiman di Kabupaten Bireuen, berkembang sangat pesat dalam kurun waktu 2006 hingga 2011, yaitu seluas 8.967,76 ha atau 4,99 %, sehingga mencapai 13.272,94 ha atau 7,39 % pada tahun 2011. Pertumbuhan luas areal pemukiman mencapai 2.424,82 ha atau 1,35 % pertahunnya. Penelitian ini dilaksanakan di Kabupaten Bireuen. Analisis data citra dilakukan di kantor UPTB – PDGA BAPPEDA Aceh dan Laboratorium GIS Fakultas Pertanian Universitas Syiah Kuala untuk pembuatan peta sebaran lahan pertanian. Metode yang digunakan dalam penelitian ini yaitu metode analisis spatio temporal yang terdiri dari analisis citra satelit multi temporal, analisis Sistem Informasi Geografis (SIG), dan survey lapangan. Saat melakukan survey lapangan dilakukan juga wawancara dengan narasumber untuk mengetahui faktor, dampak dan strategi pengendalian alih fungsi lahan pertanian di Kabupaten Bireuen. Hasil penelitian menunjukkan terjadi alih fungsi lahan pertanian di Kabupaten Bireuen dalam kurun waktu 2007 hingga 2016 yaitu 387,0 Ha. Sebesar 87,702% dari 387,0 Ha alih fungsi yang terjadi menyimpang dari arahan RTRW dan hanya sebesar 12,298% yang sesuai dengan arahan RTRW. Adapun faktor – faktor penyebab alih fungsi lahan pertanian tersebut yaitu lahan yang strategis, peraturan pemerintah, harga lahan, status kepemilikan lahan dan jumlah penduduk. Dampak yang terjadi yaitu menurunnya hasil produksi pertanian, berkurangnya pendapatan petani, terjadinya kerusakan lahan dan terjadinya pencemaran lingkungan karena limbah domestik. Strategi pengendaliannya yaitu penerapan Qanun Kabupaten Bireuen No. 7 tahun 2013 tentang Rencana Tata Ruang Wilayah Kabupaten Bireuen Tahun 2012 – 2032 dan pengawasan terhadap kegiatan pembangunan di Kabupaten Bireuen.
Kajian Laju Iinfiltrasi pada Berbagai Penggunaan Lahan dan Jenis Tanah di Kecamatan Blang Jeurango RM Adjie Prakasa; Manfarizah Manfarizah; Hairul Basri
Jurnal Ilmiah Mahasiswa Pertanian Vol 6, No 3 (2021): Agustus 2021
Publisher : Fakultas Pertanian, Universitas Syiah Kuala

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (535.807 KB) | DOI: 10.17969/jimfp.v6i3.17655

Abstract

Abstrak. Tanah dan lahan seringkali dianggap sama, padahal kedua istilah tersebut memiliki makna yang berbeda. Tanah merupakan kumpulan dari benda alam di permukaan bumi yang tersusun dalam horizon-horizon, terdiri dari bahan campuran mineral, bahan organik, air dan udara, dan merupakan media untuk tumbuhnya tanaman. Tanah dianggap sebagai tubuh alam yang berdimensi (dalam dan luas) merupakan hasil kerja gaya pembangun dan penghancur dan merupakan tempat bagi tanaman. Sedangkan Lahan adalah permukaan bumi yang berupa tanah, batuan, mineral dan kandungan cairan yang terkandung didalamnya yang memiliki fungsi tersendiri yang dapat dimanfaatkan manusia, Blang jeurango merupakan salah satu kecamatan yang terletak di Kabupaten Gayo Lues dengan berbagai jenis tanaman budidaya, berupa tanaman pangan dan tanaman perkebunan. Dari berbagai penggunaan lahan, lahan tersebut memiliki kemampuan laju infiltrasi yang berbeda-beda yang pada gilirannya akan berpengaruh terhadap penyimpanan air dan ketersediaan air di dalam tanah. Kecamatan Blang jeurango rentan dengan terjadinya banjir karena laju infiltrasi daerah tersebut lebih kecil dari intensitas hujan. Besarnya banjir yang terjadi tergantung pada perbandingan kemampuan infiltrasi dan intensitas hujan. Metode yang digunakan pada penelitian ini adalah metode survei deskriptif, yaitu dengan melakukan observasi di lapangan dengan pengukuran laju infiltrasi dilakukan dengan menggunakan double ring infiltrometer. Pengamatan juga dilakukan terhadap beberapa parameter adalah: permeabilitas, bulk density, tekstur tanah, C-organik tanah, porositas, dan laju infiltrasi. Objek penelitian adalah Desa Blang Jerango di Kabupaten Gayo Lues. Nilai laju infiltrasi di Kecamatan Blang Jeurango memiliki klasifikasi laju infiltrasi agak cepat, sedang, dan agak lambat. Agak cepat (6,60 – 7,80 ) terdapat pada SPL 1,2, dan SPL 5, dan kriteria sedang (3,00 – 6,00 ) terdapat pada SPL 4, dan SPL 6, sedangkan agak lambat (0,60 – 1,80  terdapat pada SPL 3 dan SPL 7Kata kunci: Laju infiltrasi, penggunaan lahan, jenis tanahStudy Of Infiltration Rate On Various Land Use And Soil Types In Blang Jeurango DistrictAbstract. Land and land are often considered the same, even though the two terms have different meanings. Soil is a collection of natural objects on the earth's surface arranged in horizons, consisting of a mixture of minerals, organic matter, water and air, and is a medium for plant growth. Soil is considered as a natural body whose dimensions (deep and wide) are the result of the work of building and destroying forces and are a place for plants. While land is the surface of the earth in the form of soil, rocks, minerals and the liquid content contained therein which has its own function that can be utilized by humans, Blang jeurango is one of the sub-districts located in Gayo Lues Regency with various types of cultivated plants, in the form of food crops and plants. plantation. From various land uses, these lands have different infiltration rate capabilities which in turn will affect water storage and water availability in the soil. Blang Jeurango District is prone to flooding because the infiltration rate of the area is smaller than the intensity of the rain. The amount of flooding that occurs depends on the ratio of the infiltration capacity and the intensity of the rain. The method used in this study is a descriptive survey method, namely by making observations in the field by measuring the infiltration rate using a double ring infiltrometer. Observations were also made on several parameters, namely: permeability, bulk density, soil texture, C-organic soil, porosity, and infiltration rate. The object of research is Blang Jerango Village in Gayo Lues Regency. The value of the infiltration rate in Blang Jeurango Subdistrict has a classification of rather fast, medium, and rather slow infiltration rates. Slightly fast (6.60 – 7.80 )  is found in SPL 1,2, and SPL 5, and moderate criteria (3.00 – 6.00 )  found in SPL 4, and SPL 6, while a bit slower (0.60 – 1.80 ) was found in SPL 3 and SPL 7.Keywords: Infiltration rate, land use, soil type 
Co-Authors . Azmeri, . . Khairullah . Sugianto Abubakar Karim Afriadi Ihsan Ahmad Reza Kasuri Akbar Maulana Al Qarana Alfian Rusdi Ali Muhammad Muslih Amaluddin Amaluddin Andi Salasa Arif Habibal Umam Aris Marta Ashabul Anhar Ashabul Anhar Ashabul Anhar Attabari Aldin Ayu Mulia Ayuseara Putri Gayosia Bintang Bintang Chandra Priadi Dahlan D Dahlan Dahlan Darwin Darwin Deden Nurochman Devi Sundary Dian Permata Alhai Dina Firmadiana Dini Karina Efendi Efendi Eka Aulia Ellyanti Ellyanti Essy Harnelly Fadhi Maireza Putra Fajar Rahmah Faris Zahran Jemi Fatimah Aulia Silalahi Fauzi Harun Gatot Irianto Helmi Helmi Helmi Helmi Helmi Helmi Helmi Helmi Hema Hayati Heriadi Dedek Sahputra Herry Andrisa Hidayat Pawitan Husnan Husnan Husni Husni Ichsan Ichsan Ihsan Siddiq Ilham Hanafi Ilham Wijaya Indra Indra Intan Ridha Putri Intan Solehah Ismed Ramadhan Joko Widiyanto Khairini Hasri Khairullah Khairullah Khairun Purgawa Konadi Konadi Kukuh Murti Laksono Layli Nuriani Lilis Indriansyah Lisa Mutia M. Rusli Alibasyah Manfarizah Manfarizah Marisa marisa marisa Maunida Isnin Mhd Rizha Fahlevi Mira Mardhiah Mirza Junianto Mudinillah, Adam Muhammad Aygun Muhammad Hatta Muhammad Rusdi Muhammad Rusdi Muhammad Rusdi Muhammad Rusli Alibasyah Mukhsin Febi Mirza Muzakki Muzakki Niya Putri Utami Nurmala Ramadhani Lubis Oktri Sri Wahyuni Putri Ayuni Arsita Rahmad Fadhli Rasyid Alkhoir Lubis Ridha Tiara Suci Rifa Alayani RM Adjie Prakasa Roby Arnando Romano Romano Romi Rinaldi Ryan Moulana Sartika Ningsih Septyan Arief Subhan Subhan Sufardi Sufardi Sufardi Sufardi Sugianto Sugianto Sugianto Sulasutri Sulasutri Syahrul Syahrul Syahrul Syahrul Syahrul Syahrul Syahrul Syahrul Syakur Syakur Syamaun A. Ali Syamaun A. Ali Syarifah Renny Fauzi T.M. Hadhar Wijaya Teti Arabia Teuku Alvisyahrin Teuku Muhammad Afrizal Yogi Ramadhan Ritonga Yulia Dewi Fazlina Yusni Eva Cus Endang Zainabun Zainabun Zulia Chairani