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STUDI TATA AIR DI SUB DAS BATI-BATI DAS MALUKA KALIMANTAN SELATAN Rahman Rahman; Syarifuddin Kadir; Badaruddin Badaruddin
Jurnal Sylva Scienteae Vol 3, No 3 (2020): Jurnal Sylva Scienteae Vol 3 No 3, Edisi Juni 2020
Publisher : Universitas Lambung Mangkurat

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.20527/jss.v3i3.2191

Abstract

Watersheds that are scattered throughout the territory of Indonesia, constitute a whole natural ecosystem that is intact from the mountainous ecosystem in the upstream to the downstream coastal ecosystem. The area of critical land in South Kalimantan increased to 761,042.6 ha. Critical land maps show that most of the land in the Maluka watershed belongs to the Critical Somali group with an area of 55,214.73 ha and critical land 10,369.88 ha, in which the function of the forest area is a serious threat to the carrying capacity of the watershed. The purpose of this study is to determine the flow regime coefficient, annual flow coefficient, and water use index in the Bati-Bati watershed of the Maluka Watershed. The research method that is carried out by data collection is data of water discharge, water level, and river flow velocity. Analysis of the data used is the study through giving weight, class assignment, score calculation, and assessment of each sub criteria for determining watershed classification. The Flow Regime Coefficient value is 11.89 with a score of 1.00 rating criteria into the "medium" qualification. Annual Flow Coefficient 0.64 with a score of 1.50 which entered the recovery qualification "very high". Water use index value in April 2018 was 0.460 with a score of 0.75 which was included in the "low" recovery qualification and in May 2018 it was 0.663 with a score of 1.00 which was included in the "medium" recovery qualification.
ANALISIS TINGKAT BAHAYA EROSI (TBE) DI DAS DUA LAUT KABUPATEN TANAH BUMBU Eka Hardiana; Syarifuddin Kadir; Yusanto Nugroho
Jurnal Sylva Scienteae Vol 2, No 3 (2019): Jurnal Sylva Scienteae Vol 2 No 3, Edisi Juni 2019
Publisher : Universitas Lambung Mangkurat

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (811.717 KB) | DOI: 10.20527/jss.v2i3.1833

Abstract

Erosion is the process of eroding the surface layer of soil due to surface flow. Erosion degrades soil quality as a medium grows on vegetation. This study aims to analyze the magnitude of the erosion rate and identify the level of erosion hazard in the DAS Dua Laut. Research method using USLE (Universal Soil Loss Equation) method with observation point using purposive sampling taking into account the land slope class.The results showed that from all units of DAS Dua Laut, the highest erosion value was found on slope> 25-40% with scrubland cover that was 231,78 ton /ha/year, while on slope> 8-15% with vegetation rubber obtained the lowest value of 10.53 tons /ha/year.This shows that land conversion gives influence to the rate of erosion especially on steep slopes. The erosion hazard level of all land units and land cover shows variations in land class in the form of very light classes (0-SR), light (1-R), medium (II S and III S), weight (III B) and very heavy (IV- SB).Keywords; soil erosion, DAS Dua Laut, Erosion Hazard Level
DINAMIKA PERUBAHAN PETA BATAS DAS MALUKA PROVINSI KALIMANTAN SELATAN Rudianto Rudianto; Syarifuddin Kadir; Kissinger Kissinger; Mahrus Aryadi
Jurnal Hutan Tropis Vol 8, No 3 (2020): Jurnal Hutan Tropis Vol 8 No 3 edisi November 2020
Publisher : Lambung Mangkurat University-Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (725.421 KB) | DOI: 10.20527/jht.v8i3.9740

Abstract

A study on the dynamics of the Change Dynamics of the Maluka Watershed Boundary Map in South Kalimantan Province, which aims to analyze the Maluka Watershed Boundary is a large-scale approach, analyzing the dynamics of changes in some watershed characteristics (morphological and morphometric aspects) and conducting a policy direction towards the Compilation of the Maluka Watershed Boundary Watershed. The results of the Maluka watershed boundary scale of 1:50.000 there are changes and improvements in watershed boundaries in the downstream watershed due to river drainage, dredging, river displacement caused by human activities, new watersheds formed and SRTM level 30 x 30 m resolution, line repair and correction coastal and river networks and optical remote sensing. Morphometric and morphologic characteristics of Watersheds Significant changes in watershed area and administration area (reduced by 4.678 Ha or 5,3%). Other properties did not change significantly (Hydrologic DAS: 2 sub-watersheds, namely the Bati-Bati sub-watershed and Banyuhirang sub-watersheds), (Watershed shape: elongated (Rc <0,5)), (Slope class: flat 90,24%, steep and rather steep 2,14%), (Altitude/Elevation) Watershed: 2 masl to 50 masl 81,71%, above 300 masl 4,37%), (Watershed orientation: heading east to west in a straight direction, middle watershed symmetrical ballooning), (flow density, index value: 1,09 medium category) and (DAS flow pattern: Dendritic). Policy recommendations are suggested to synchronize the implementation of UU No. 23 Tahun 2014 and UU No. 37 Tahun 2014 in terms of carrying out the mandate of PP. 37 Tahun 2012, namely the implementation of the management of watershed management in the context of conservation of land, water in the ecosystem/watershed unit by giving the mandate to assist the task of sub-affairs management of watershed management from the provincial government to the district / city government.
PENGAYAAN VEGETASI PENUTUPAN LAHAN UNTUK PENGENDALIAN TINGKAT KEKRITISAN DAS SATUI PROVINSI KALIMANTAN SELATAN Syarifuddin Kadir; Badaruddin Badaruddin
Jurnal Hutan Tropis Vol 3, No 2 (2015): Jurnal Hutan Tropis Volume 3 Nomer 2 Edisi Juli 2015
Publisher : Lambung Mangkurat University-Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (2920.745 KB) | DOI: 10.20527/jht.v3i2.1519

Abstract

Kajian ini bertujuan untuk mengetahui kondisi vegetasi penutupan lahan dan tingkat kekritisan lahan di DAS Satui Provinsi Kalimantan Selatan. Penentuan tingkat kekritisan lahan dan kondisi vegetasi pentupan  lahan  serta  arahan  pengendaliannya  dilakukan  melalui  metode  pendekatan  secara  spasial terhadap kondisi tutupan lahan dengan memanfaatkan sistem informasi Geografis. Hasil kajian diperoleh bahwa: 1) kondisi eksisting: a) vegetasi tutupan hutan seluas 49.703,37 ha (32 %), tutupan vegetasi non hutan 83.694,61 ha (54 %); b) lahan tidak bervegetasi 20.123,65 ha (13 %). Lahan dengan kriteria kritis (kritis dan sangat kritis) seluas 34.435,67 ha (22,43 %). 2) Arahan penurunan tingkat kekritisan lahan; a) pengayaan tutupan vegetasi hutan menjadi seluas 66.975,57 ha (44 %), sedangkan lahan terbuka, semak belukar dan pertambangan  berkurang  seluas  17.782,99  ha  (12  %);  b)  berdasarkan  pengayaan  vegetasi  menurunkan tingkat kekritisan lahan menjadi lahan kritis 1.536,82 ha (1,01%); c) pengayaan tutupan vegetasi hutan dan penurunan tingkat kekritisan lahan dapat meningkatkan fungsi DAS Satui sebagai pengatur tata air untuk mengendalikan kerawanan banjir dan menigkatkan produktivitas lahan untuk kesejahteraan masyarakat.Kata Kunci: Lahan kritis, vegetasi tutupan lahan, DAS
PENGENDALIAN BANJIR BERDASARKAN KELAS KEMAMPUAN LAHAN DI SUB DAS MARTAPURA KABUPATEN BANJAR KALIMANTAN SELATAN Syarifuddin Kadir; Karta Sirang; Badaruddin Badaruddin
Jurnal Hutan Tropis Vol 4, No 3 (2016): Jurnal Hutan Tropis Volume 4 Nomer 3 Edisi November 2016
Publisher : Lambung Mangkurat University-Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.20527/jht.v4i3.3619

Abstract

Land use conducted in accordance with its ability to protected areas or farm area in a watershed will provide benefits for the benefit of the water system and the welfare of society. Land use do not match the capabilities and purposes may increase the risk of floods. Balitbangda South Kalimantan (2010) states that the period from 2007 to 2010, flood in Banjar regency as many as 10 districts and 65 villages. The purpose of this research is to know the land ability class become the reference for determining the direction of the use and the utilization of the land, While the expected benefits to be a reference for flood control measures for the short and long term. The determination of land capability class is done through spatial approach method by utilizing Geographic information system. The study results obtained: 1) domination of the land capability class parameters:  a) slope, > 65% area of 31.46%; b) drainage, either 94.2%; c) The volume of surface rocks, lots of 36.5%; d) the erosion was 49.7%; e) the soil depth in 66.6%; f) soil texture, subtle bit; sandy clay, clay 57.95%. 2) land capability class sub-watershed Riam Kiwa sub watershed Martapura III to VIII. 3) Flood control optimally through forest rehabilitation based on land capability class in the sub watershed Martapura.Banjir merupakan suatu kondisi aliran air sungai pada suatu DAS yang tingginya melebihi muka air sungai normal, sehingga melimpas dari palung sungai yang menyebabkan adanya genangan pada lahan rendah disisi kiri kanan sungai. Penggunaan lahanyang dilaksanakan sesuai dengan kemampuannya pada kawasan lindung dan atau kawasan budidaya pertanian pada suatu DAS akan memberikankeuntungan untuk kepentingan tata air  dan kesejahteraan masyarakat. Penggunaan lahan yang dilakukan tidak sesuai dengan kemampuan dan peruntukannya dapat meningkatkan risiko bencana banjir. Balitbangda Provinsi Kalimantan Selatan (2010) menyatakan bahwa periode 2007-2010 terjadi bencana banjir di Kabupaten Banjar sebanyak 10 kecamatan dan 65 desa. Tujuan penelitian ini  mengetahui kelas kemampuan lahan menjadi acuan penentuan arahan penggunaan lahan, sedangkan manfaat yang diharapkan agar dapat menjadi acuan pengendalian kerawanan banjir untuk jangka pendek dan jangka panjang.  Penentuan kelas kemampuan lahan dilakukan melalui metode pendekatan secara spasial dengan memanfaatkan sistem informasi Geografis. Hasil kajian diperoleh : 1) dominasi parameter kelas kemampuan lahan: a) kelerengan, > 65 % seluas 31,46 %; b) drainase, baik 94,2%; c) Volume Batuan Permukaan, banyak 36,5%; d) erosi sedang 49,7%; e) kedalaman tanah dalam 66,6%; f) tekstur tanah, Agak halus; liat berpasir, lempung 57,95%. 2) kelas kemampuan lahan sub-sub DAS Riam Kiwa sub DAS Martapura III sampai IV dan VI sampai VIII. 3)Pengendalian banjir secara optimal melalui rehabilitasi hutan dan lahan berdasarkan kelas kemampuan lahan di sub DAS Martapura Kabupaten Banjar.
EVALUASI DINAMIKA KERENTANAN LINGKUNGAN BERDASARKAN KERAPATAN VEGETASI DI DAERAH ALIRAN SUNGAI TABUNIO Syarifuddin Kadir; Ichsan Ridwan; Wahyuni Ilham; Nurlina Nurlina
Jurnal Hutan Tropis Vol 9, No 3 (2021): JURNAL HUTAN TROPIS VOLUME 9 NOMER 3 EDISI NOVEMBER 2021
Publisher : Lambung Mangkurat University-Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.20527/jht.v9i3.12335

Abstract

A Watershed is an ecosystem whose first component consists of natural resources vegetation, land, water, and human resources. Tabunio watershed covering an area of 62,558.56 hectares consists of 10 sub-watersheds. The Normalized Difference Vegetation Index (NDVI) is used in vegetation density analysis. Vulnerability of environmental damage is the condition of a region that has the potential for environmental damage due to human activities and or activities that have the potential to cause environmental impacts.The purpose of vegetation density analysis is carried out for the evaluation of environmental vulnerability dynamics in Tabunio watershed, i.e: 1). Knowing changes in land cover; 2. Knowing the classification of vegetation density; 3. Determine efforts to increase vegetation density. The benefits of this analysis are to obtain directives that can have a positive impact on the control of flood suppliers' vulnerability and environmental vulnerability by determining forest and land rehabilitation techniques.Based on the results of mapping and analysis obtained: 1) changes in land cover in 2005-2020 are dominant in forest land cover, open land, settlements, plantations, swamp farming, shrubs, and mining; 2) Vegetation density in the upstream sub-watershed is dominated by the classification of dense and very tight vegetation density; 3) The green revolution of the upstream watershed is dominated for ecological purposes with dense and very close vegetation, the central part of the watershed is dominated for ecological, economic and social with tight vegetation, downstream green revolution watershed dominated for economic and social interests with dense and sparse vegetation
TINGKAT BAHAYA EROSI DALAM RANGKA REHABILITASI HUTAN DAN LAHAN DI SUB-SUB DAS RIAM KIWA KABUPATEN BANJAR Agung Hananto; Muhammad Ruslan; Syarifuddin Kadir
Jurnal Hutan Tropis Vol 10, No 2 (2022): Jurnal Hutan Tropis Volume 10 Nomer 2 Edisi Juli 2022
Publisher : Lambung Mangkurat University-Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.20527/jht.v10i2.14119

Abstract

Tujuan penelitian ini adalah untuk menganalisis variasi Tingkat Bahaya Erosi  yang diduga terjadi, dan merumuskan upaya rehabilitasi hutan dan  lahan berdasarkan variasi Tingkat Bahaya Erosi di Sub-Sub DAS Riam Kiwa Kabupaten Banjar.  Metode pengumpulan data dilakukan dengan menggunakan cara observasi, pengamatan lapangan terhadap data biofisik, serpeti vegetasi, lahan dan data iklim.  Data dianalisis menggunakan model USLE, Tabulasi dan Content Analysis. Hasil penelitian menunjukkan bahwa TBE relatif bervariasi, dari TBE I-R (Ringan), II-S (Sedang), III-B (Berat) dan IV-SB (Sangat Berat). Luas TBE tergolong I-R (Ringan), II-S (Sedang) penutup lahan HLKS dan TBE II-S (Sedang) penutup lahan PLK UL-06 sebesar  2.798,81 ha (26,42%).  Luas TBE tergolong III-B (Berat), IV-SB (Sangat Berat) penutup lahan PLK (kecuali UL-06), SBK, LTB  sebesar 7.796,5 ha (73,58%). Arahan rehabilitasi hutan dan lahan yang direkomendasikan terdapat 4 (empat) kelompok: a) Penutup lahan HLKS UL-01, UL-02 tetap dipertahankan sebagai HLKS dengan pemeliharaan (tindakan silvikulture) 238,75 ha, b) PLK UL-06 tetap dipertahankan sebagai PLK dengan pemeliharaan (penanaman menurut garis kuntor dan menggunakan teras guludan) 2.560,24 Ha, c) Penutup lahan  SBK UL-03, UL-04 1.063,47 ha dan PLK UL-07, UL-08 5.449,21 ha dikonversi menjadi Agroforestry dan d) Penutup lahan  SBK UL-05 400,70 ha, penutup lahan PLK UL-09 423,66 ha dan LTB UL-10, UL-11, UL-12  883,27 ha dikonversi menjadi Hutan Tanaman dengan kegiatan Reboisasi. Agroforestry dan Reboisasi diikuti dengan metode mekanik, seperti  pembuatan teras guludan dan  penanaman menurut garis kontur
ANALISIS LAJU INFILTRASI PADA TEGAKAN PINUS, MAHONI, AKASIA DAN MERSAWA DI KOTA BANJARBARU Mujari Rahman; Syarifuddin Kadir; Badaruddin Badaruddin
Jurnal Sylva Scienteae Vol 5, No 4 (2022): Jurnal Sylva Scienteae Vol 5 No 4 Edisi Agustus 2022
Publisher : Universitas Lambung Mangkurat

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.20527/jss.v5i4.6143

Abstract

Knowing the rate of infiltration in the stands of Pinus, Mahogany, Acacia and Mersawa in Banjarbaru City, Analyzing the magnitude of infiltration capacity in the stands of Pinus, Mahogany, Acacia and Mersawa.In this study there is data retrieval and data collection, in the collection of infiltration data conducted under the stands of Pinus, Mahogany, Acacia, and Mersawa in Banjarbaru.Measurement of infiltration rate is performed 3 times on each stand Pinus, Mahogany, Acacia and Mersawa.In data collection there are two methods, namely primary data and secondary data, primary data is done directly in the field using an infiltrometer tool placed on a predetermined sample location.The required secondary data is supporting data such as location maps.In this study, the largest average infiltration rate was found in acacia stands with a value of 3.67 mm/h and the lowest at mersawa stands with a value of 1.50 mm/h.While the average capacity and volume of infiltration is the largest in acacia stands with an average capacity value of 3,589 mm /h and a volume of 1,519 mm3, while the lowest infiltration capacity and volume is in the pine stand with a value of 1,570 mm / h and the lowest volume of 0.800 mm3.Mengetahui laju infiltrasi pada tegakan Pinus, Mahoni, Akasia dan Mersawa di Kota Banjarbaru, Menganalisis besarnya kapasitas infiltrasi pada tegakan Pinus, Mahoni, Akasia dan Mersawa. Penelitian ini terdapat pengambilan data dan pengumpulan data, pada pengambilan data infiltrasi dilakukan dibawah tegakan Pinus, Mahoni, Akasia, dan Mersawa di Banjarbaru. Pengukuran laju infiltrasi dilakukan dalam 3 kali ulangan pada setiap tegakan  Pinus, Mahoni, Akasia dan Mersawa. Dalam pengumpulan data terdapat dua metode yaitu data primer dan data skunder, data primer dilakukan langsung dilapangan dengan menggunakan alat infiltrometer yang diletakan pada lokasi sampel yang sudah ditentukan. Data skunder yang diperlukan ialah data penunjang seperti peta lokasi. Dalam penelitian ini rata-rata laju infiltrasi terbesar terdapat pada tegakan akasia dengan nilai 3,67 mm/jam dan yang terendah pada tegakan mersawa dengan nilai 1,50 mm/jam. Sedangkan rata-rata kapasitas dan volume infiltrasi terbesar  pada tegakan akasia dengan nilai rata-rata kapasitas 3,589  mm/jam dan volume 1,519 mm3, sedangkan kapasitas dan volume infiltrasi terendah ada pada tegakan pinus dengan nilai 1,570 mm/jam dan volume terendah 0,800 mm3.
ANALISIS DEBIT AIR DI DAERAH TANGKAPAN AIR (DTA) BARABAI KABUPATEN HULU SUNGAI TENGAH Noraito Gultom; Badaruddin Badaruddin; Syarifuddin Kadir
Jurnal Sylva Scienteae Vol 5, No 5 (2022): Jurnal Sylva Scienteae Vol 5 No 5 Edisi Oktober 2022
Publisher : Universitas Lambung Mangkurat

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.20527/jss.v5i5.6693

Abstract

Water discharge is the rate of water flow in a river channel in a certain volume per unit time. This study aims to analyze water discharge and water level, analyze the relationship between water discharge and water level in the Barabai catchment area, Hulu Sungai Tengah Regency. Measurement of water discharge is done using the float method. The resulst obtained at the first point mean that the water discharge is 17.31 m3/second with an average water level of 1 m. At the second point the average water discharge is 15.43 m3/second  with an average water level of 0.98 m. At the third point the average water discharge is 16.61 m3/second with an average water level of 0.46 m. The relationship between water discharge and water level at the first point is 0.9835, the second point is 0.9969, and at the third point is 0.9948, which means that the three have a very strong correlationDebit air merupakan laju aliran air pada saluran sungai dalam volume persatuan waktu tertentu. Penelitian ini bertujuan untuk menganalisis debit air dan tinggi muka air, menganalisis hubungan antara debit air dan tinggi muka air di DTA Barabai Kabupaten Hulu Sungai Tengah. Pengukuran debit air dilakukan dengan menggunakan metode pelampung. Hasil yang diperoleh pada titik pertama rata-rata debit air 17,31 m3/detik dengan tingi muka air rata-rata 1 m. Pada titik kedua rata-rata debit air 15,43 m3/detik dengan tinggi muka air rata-rata 0,98 m. Pada titik ketiga rata-rata debit air 16,61 m3/detik dengan tinggi muka air rata-rata 0,46 m. Hubungan debit air dengan tinggi muka air pada titik pertama adalah 0,9835, titik kedua adalah 0,9969, dan pada titik ketiga adalah 0,9948 yang berarti ketiganya memiliki korelasi yang sangat kuat.
ANALISIS TINGKAT BAHAYA EROSI DARI VEGETASI ALANG-ALANG PADA BERBAGAI KELERENGAN DI SUB DAS BATI-BATI (DAS MALUKA) KALIMANTAN SELATAN Zainal Abidin; Syarifuddin Kadir; Eko Rini Indriyatie
Jurnal Sylva Scienteae Vol 5, No 5 (2022): Jurnal Sylva Scienteae Vol 5 No 5 Edisi Oktober 2022
Publisher : Universitas Lambung Mangkurat

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.20527/jss.v5i5.6694

Abstract

The type of land cover affects the level of erosion hazard in an area. The purpose of this study was to analyze the amount of erosion hazard and determine the level of erosion hazard (TBE) on the reed vegetation on various slopes in the Bati-bati sub-watershed of the Maluka watershed, South Kalimantan. Sampling of data using purposive sampling technique. Samples were taken as many as 6 land units based on vegetation, soil type, reed land cover and slope class, which were obtained from the map overlay of land units. Each sample point was taken soil samples using a sample ring to be tested in the laboratory. Then, the data were analyzed using Universal Soil Loss Equation (USLE) and Erosion Hazard Analysis (TBE). The highest number of erosion values occurred in reed Land Unit (UL) 39 with a slope of 15-25% with an erosion value of 130.96 tons/ha/year, while the lowest erosion value was found in UL 34 with a slope of 0-8 and erosion of 9.64 tons/ha/year. The erosion hazard level of the land unit under study shows the percentage of light grade (IR) occurring at UL7, UL 34, UL 50 and UL 59 with a flat slope (0-8), while the medium grade (II-S) occurs at UL. 37 with gentle slopes (8-15) and UL 39 with steep slopes (25-40)Jenis penutupan lahan berpengaruh terhadap tingkat bahaya erosi dalam suatu wilayah. Tujuan dari penelitian ini ialah menganalisis jumlah bahaya erosi dan menentukan adanya tingkat bahaya erosi (TBE) pada vegetasi alang-alang pada berbagai kelerengan di sub DAS Bati-bati DAS Maluka, Kalimantan Selatan. Pengambilan sampel data menggunakan teknik purposive sampling. Sampel diambil sebanyak 6 unit lahan berdasarkan vegetasi, jenis tanah, tutupan lahan alang-alang dan kelas kelerengan, yang didapat dari overlay peta satuan lahan. Setiap titik sampel diambil sampel tanahnya menggunakan ring sampel untuk diuji di laboratorium. Kemudian, data dianalisis menggunakan persamaan Universal Soil Loss Equation (USLE) dan Analisis Tingkat Bahaya Erosi (TBE). Jumlah nilai  erosi tertinggi terjadi pada Unit Lahan Alang-Alang (UL) 39 dengan kemiringan lereng 15-25% dengan nilai erosi sebesar130,96 ton/ha/thn, sedangkan nilai erosi terendah terdapat pada UL 34 dengan kemiringan lereng 0-8 dan nilai erosi sebesar 9,64 ton/ha/thn. Tingkat bahaya erosi dari unit lahan yang diteliti menunjukkan persentase kelas ringan (I-R) terjadi pada UL7, UL 34, UL 50 dan UL 59 dengan kemiringan lereng yang datar (0-8), sedangkan pada kelas sedang (II-S) terjadi pada UL 37 dengan kemiringan lereng landai (8-15) dan UL 39 dengan  kemiringan lereng curam (25-40).
Co-Authors Agung Hananto Akhmad Rizalli Saidy Andi Ilyasa Anggara Putra Yudha Anggi Retno Wulan Asysyifa Asysyifa Badaruddin Badaruddin Badaruddin Badaruddin Budi Susilo Daniel Itta Denny Purnomo Dina Naemah Eka Hardiana Eko Rini Indrayatie Eko Rini Indriyatie Emmy Lilimantik Fadly Hairannoor Yusran Gusti Muhammad Hatta Gusti Reni Amalinda Gusti Rusmayadi Hanif Faisol Hartinah Harman Hesty Heryani Ichsan Ridwan Jefri H Simamora Karta Sirang Karta Sirang Khairun Nisa Kissinger Kissinger Laila Indasari Lusi Anggraeni Maepadeapati Chitta Mahrus Aryadi Monika Rolina Muhammad Nasih Muhammad Nasrudin Muhammad Ruslan Muhammad Ruslan Mujari Rahman Nofitasari Nofitasari Noraito Gultom Norsaidah Norsaidah Nur Syifa Yarnie Nur Syifa Yarnie Nurlina Nurlina Rahmadi Rahmadi Rahman Rahman Ratna Liana Dewi Reynaldy Yustisio Reznandi Wiharto Fitrian Sulaxono Ria Tahfazona Ridha Hariani Rina Kanti Robby Arni Rudianto Rudianto Ruslan Ruslan Saidatul Ummah Shinta Uli Lumbantoruan Suyanto - Syahidar Khalid Syaiful Bahri Vina Delya Wahyuni Ilham Wisda Hartati Yesi Eka Pratiwi Yusanto Nugroho Zainal Abidin