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Karakterisasi Aliran Uap-Kondensat pada Saluran Mendatar Berdasarkan Pengukuran Temperatur Sukamta, Sukamta; Indarto, Indarto; Purnomo, Purnomo; Rokhmat, Tri Agung
Jurnal Semesta Teknika Vol 17, No 1 (2014): MEI 2014
Publisher : Jurnal Semesta Teknika

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Abstract

The objective of the current investigation is to find out temperature distribution regimes in a horizontal pipe when condensation process is happened.  The research was conducted at Pusat Studi Ilmu Teknik Universitas Gadjah Mada. The experiment apparatus consists of an inner annulus pipe made from copper (din = 17.2 mm, do = 19 mm) with the length of 1.8 m. The outer annulus pipe is a galvanized iron pipe (din = 108.3 mm, do = 114.3 mm) with the length of 1.6 m. Thermocouples type K 36 TT OMEGA with chromel (+) and alumel (-) materials were used as temperature sensors, to detect the spread of temperature in radial or axial direction along the pipe. The measurement ranged from -50 to 260 oC, with an accuracy of 0.01 °C. A data logger of RX 40 serial (OMRON, 20 Channels) was used to read and record temperature data with the sampling rate of 5 Hz. In the experiment, the water (H2O)was heated using a boiler to generate steam which was then flowed and condensed inside the annulus pipe to form a steam-condensate two-phase flow in horizontal pipe. On the other hand, the water was used as a coolant in the outer of annulus pipe. The results indicated that the temperature distribution regimes are influenced by axial posisition.The farther distances from the inlet the lower the temperatures being recorded which indicate the increase of film condensate thickness. Such phenomena can affect slugging in the location.
Identifikasi Pola Aliran Dua Fasa Uap-Kondensat Berdasarkan Pengukuran Beda Tekanan pada Pipa Horisontal Sukamta, Sukamta; Indarto, Indarto; Purnomo, Purnomo; Rohmat, Tri Agung
Jurnal Semesta Teknika Vol 13, No 1 (2010): MEI 2010
Publisher : Jurnal Semesta Teknika

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Abstract

An experiment of two-phase flow patterns of steam-condensate based on differential pressure measurement in horizontal tube was conducted by varying the flow rate of the steam. The experiment utilised annulus pipe with inner section test pipe was made from copper and outer section was made from Galvanized Iron Pipe (GIP) wrapped with a 10-mm-thick insulation. The pipe was 1.6 meter length, and 4 inch outer diameter and 17 mm inner diameter. The two-phase flow regime was investigated based on pressure gradien between its inlet and outlet. In order to support the result, visualition was conducted using a ¾ inch diameter and 1.3 m length of transparent pipe connected with the test pipe section. Five variations of steam flow rate ranging from 0.00211361 m3/s to 0.007078511 m3/s were selected. The results show that for lowest steam flow rate, stratified flow pattern was identified while for the ot her variations, stratified, wavy, plug and slug flow pattern were observed. Wavy flow pattern occured on transition of stratified to slug or plug. Annular flow pattern was not observed in this experiment. Generally speaking, an increase in steam flow rate resulted in a more significant pressure gradient signals.
Study on The Physical Characteristics and Hydrology of 15 Watershed in East Java Indarto, Indarto
Forum Geografi Vol 27, No 2 (2013): December 2013
Publisher : Universitas Muhammadiyah Surakarta

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Abstract

The study demonstrated the application of statistical method to describe physical and hydro-meteorological characteristics by means of time series analysis.  Fifteen(15) watersheds in East Java were selected for this study. Data input for the analysis include: physical data, rainfall and discharge. Physical data of the watershed (topography, river network, land use, and soil type) are extracted from existing database and treated using GIS Software. Daily rainfall data were collected from existing pluviometers around the region. Daily discharge data were obtained from measurement station located at the outlet of each watershed. Areal Rainfall for each watershed was determined using average value of existing pluviometers around the watershed and determined using simple arithmetic method. These time series data are then imported to RAP (River Analysis Package).  Analysis on the RAP, include: general statistical, flow duration curve (FDC), and baseflow analysis. The result then presented in graphic and tables. Research shows that among the watersheds have different physical and hydrological characteristics.
Prosedur Kalibrasi dan Validasi Model SMAR untuk Mendeskripsikan Proses Hujan Aliran di Sub-DAS Rawatamtu Indarto, Indarto
Jurnal Teknik Sipil Vol 19, No 3 (2012)
Publisher : Institut Teknologi Bandung

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Abstract

Abstrak. Model SMAR (Soil Moisture Accounting Rainfall Model) merupakan salah satu model hidrologi pada RRL (Rainfall Runoff Library) yang dapat digunakan untuk menghitung aliran permukaan (Run Off) dari suatu DAS. Data masukan utama untuk model adalah data hujan dan evapotranspirasi. Artikel ini membahas prosedur kalibrasi dan validasi model untuk mendeskripsikan proses hujan - aliran pada skala harian. Artikel juga memaparkan tentang manfaat user-interface dan visualisasi yang ada pada software (model) tersebut. Model dikalibrasi menggunakan data debit yang diperoleh dari sub-DAS Rawatamtu (Jawa Timur). Kombinasi dua metode (generic dan manual) digunakan selama proses kalibrasi dan validasi. Kalibrasi dilakukan pada separuh periode rekaman yang tersedia, sedangkan validasi dilakukan pada separuh periode yang ke dua. Hasil kalibrasi dan validasi dievaluasi menggunakan kriteria: Koefisien Nash-Sutcliffe, Koefisien korelasi (correlation coefficient) danperbedaan Run Off (difference in Run Off). Kalibrasi dan validasi menggunakan metode generic maupun manual menunjukkan bahwa model mampu mereproduksi proses utama dari Hujan menjadi Aliran (debit terhitung) pada sub-DAS tersebut. Hasil juga menunjukkan bahwa performance model kurang optimal pada periode validasi, hal ini dikarenakan keterbatasan data yang digunakan. Data yang lebih lengkap diperlukan untuk mengevaluasi performance model.Abstract. The Soil Moisture Accounting Rainfall Model (SMAR) is one of Rainfall Runoff Library Models (RRL) used to calculate Run-Off from rainfall and evapotranspiration data. This article shows the procedure to calibrate the model. Furthermore, this article also show the benefit of software fitur and user interface. Model is calibrated and validated using discharge data otained from Rawatamtu sub-Watershed (East Java). Two methodes (generic and manual) were exploited for the calibration and validation procceses. The result was evaluated by using the criteria of: Nash-Sutcliffe Coefficient, Coefficient of Correlation and difference in run-off. Calibration is conducted at the first half of recording periods, while validation is conducted at the second half of recording periods. The result shows that both generic and manual method can describe Rainfall to Run-Off process of the watershed, during calibration periode. However, during validation period model performance is not satisfied, due to the limit of data used. More data is needed to evaluate the model performance.
Variabilitas Spasial Hujan Harian di Jawa Timur Indarto, Indarto
Jurnal Teknik Sipil Vol 20, No 2 (2013)
Publisher : Institut Teknologi Bandung

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Abstract

Abstrak. Dua variabel digunakan untuk memaparkan variabilitas spasial hujan harian di Jawa Timur, yaitu: (1) Hujan-24jam-maksimal dan (2) Hari-Hujan. Data hujan diperoleh dari 946 lokasi stasiun hujan yang tersebar merata di seluruh wilayah Provinsi. Analisis spasial dilakukan menggunakan ESDA (Exploratory Spatial Data Analysis) yang ada pada ArcGIS Geostatistical Analyst. Tool yang digunakan mencakup: Histogram dan QQ-Plot. Selanjutnya, peta distribusi spasial (hujan-24jam-maksimal dan hari-hujan) di seluruh wilayah Jawa Timur dibuat dengan menggunakan metode Interpolasi Inverse Distance Weigthing (IDW). Hasil analisa menunjukkan Histogram dan Normal QQ-Plot untuk hari-hujan mendekati distribusi normal, sedangkan untuk hujan-24jam-maksimal lebih condong ke kanan. Statistik nilai hujan-24jam-maksimal yang diperoleh adalah: minimal = 32 mm, rerata = 137 mm, maximum = 332 mm, and median = 130 mm/hari. Nilai ringkasan distribusi statistik lainnya adalah:  standar deviasai = 50,37; koefisien kemencengan = 0,99; dan koefisien kurtosis = 4,3. Statistik untuk variabel hari-hujan, menunjukkan nilai minimal = 4 hari/tahun dan maksimal = 184 hari/tahun. Sedangkan, nilai rerata = 81 hari/tahun dan nilai median = 80 hari/tahun. Histogram juga menampilkan nilai standar deviasi = 23,74; koefisien skewness = 0,28; dan koefisien curtosis = (3,6). Penelitian menunjukkan kemampuan dan manfaat ESDA untuk menggambarkan variabilitas spasial hujan harian dengan lebih detail.Abstract. Two variabel (maximum-24hour-rainfall and number of rainfall-day) were used to describe the spatial variabiity of Daily Rainfall phenomena in East Java regions. Daily rainfall data were collected from 946 pluviometres spread around the regions. Spatial analyst were exploited by means of Exploratory Spatial Data Analysis (ESDA) available at ArcGIS Geostatistical Analyst. Histogram and QQ-Plot were used for the analysist. Furthermore, thematic map visualized the spatial variability of daily rainfall data over the region was produced using Inverse Distance Weighting (IDW) interpolation method. Results shows that both Histogram and Normal QQ-Plot for number-ofrainffal-day are close to normal distribution, however spatial distribution of 24-hour rainfall data is quitely distorsed to standard normal distribution. Statistical resume obtained from 24hour-rainfall data are : minimum = 32 mm/day, average = 137 mm/day, maximum = 332 mm/day, median = 130 mm/day, standard deviation = 50,37, coefficient of skewness = 0,99, and Coefficient of Curtosis = 4,3. Other statistical value resumed from number of rainy-day are : minimum = 4 day/year, average = 81 day/year, maximum = 184 day/year, and median = 80 day/year, standard deviation = 23,74, coefficient of skewness = 0,28, and Coefficient of curtosis = 3,6. The research demonstrate the capability and benefit of those statistical tool to describe spatial variability of daily rainffal phenomenon in East Java Regions.
Performance of Porous-Venturi Microbubble Generator for Aeration Process Afisna, Lathifa Putri; Juwana, Wibawa Endra; Indarto, Indarto; Deendarlianto, Deendarlianto; Nugroho, Fellando Martino
Journal of Energy, Mechanical, Material and Manufacturing Engineering Vol 2, No 2 (2017)
Publisher : University of Muhammadiyah Malang

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (698.696 KB) | DOI: 10.22219/jemmme.v2i2.5054

Abstract

Qualified and preserved water is declining due to metal, waste, and hazardous chemicals contamination. Demand on fresh water raises and leads to the efforts on processing waste water with effective and efficient technology. Microbubble generator technology developed lately to result dissolved oxygen for raising microorganisms to decompose waste in waste water. This research used porous-ventury microbubble generator with 30° inlet angle and 20° outlet angle, placed in the center of 280 cm x 60 cm x 40 cm aquarium for experiment. This research aimed to find out bubble distribution and microbubble generator (MBG) performance. Measurement on bubble distribution conducted using Phantom Control Camera. Obtained data analyzed using MATLAB R2016a, while MBG performance measured using pressure transducer. Analysis conducted on variations of gas debit (0,1 lpm; 0,4 lpm., and 1 lpm) and water debit (30- 80 lpm) effects toward performance parameters, such as hydraulic power (Lw) and bubble generating efficiency (ηB). Results show that the greatest microbubbles’ diameter is 150- 500 μm, hydraulic power (Lw) increases with the inclining water debit (QL), effect of gas debit variation exert low effect towards Lw, and declining number of bubble generating efficiency (ηB) parameter with the inclining number of the water debit (QL).
KARAKTERISTIK PENDIDIHAN DALAM CELAH SEMPIT REKTANGULAR VERTIKAL DENGAN VARIASI TEMPERATUR AWAL PLAT Catrawedarma, I Gusti Ngurah Bagus; Indarto, Indarto; Juarsa, Mulya
Media Mesin: Majalah Teknik Mesin Vol 18, No 1 (2017)
Publisher : Universitas Muhammadiyah Surakarta

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Abstract

Analisis perpindahan kalor pendidihan untuk mengetahui pengaruh temperatur awal plat utama terhadap karakteristik pendidihan yang meliputi waktu rewetting, pola rewetting, fluks kalor, serta Critical Heat Flux (CHF) telah dipelajari berdasarkan kurva pendidihan dan fluks kalor yang dihitung dari transien temperatur permukaan plat, yang merupakan hasil eksperimen dengan menggunakan 2 plat vertikal dengan celah sempit antar plat utama dan penutup adalah 1 mm. Debit dan temperatur air pendingin ditetapkan sebesar 0,09 lt/detik dan temperatur saturasi. Temperatur awal plat utama divariasikan dari 500oC, 550oC, dan 600oC. Hasil analisis menunjukkan bahwa waktu rewetting terendah sebesar 30 sekon dan tertinggi sebesar 290 sekon. CHF tertinggi sebesar 750 kW/m2 dan terendah sebesar 400 kW/m2. Semakin tinggi temperatur awal plat, maka semakin lama waktu rewettingnya. Perubahan temperatur awal plat utama tidak mempengaruhi pola rewetting. Semakin tinggi temperatur awal plat, maka nilai CHF-nya semakin rendah. Daerah didih film tidak sesuai dengan kasus pool boiling. Pada daerah transisi, semakin rendah temperatur awal plat, maka semakin mendekati korelasi Murase. Nilai CHF mendekati korelasi Leinhard. Titik Leidenfrost sesuai dengan korelasi Zuber. Daerah didih inti mendekati korelasi Murase untuk superheat vapor.
Study on The Physical Characteristics and Hydrology of 15 Watershed in East Java Indarto, Indarto
Forum Geografi Vol 27, No 2 (2013): December 2013
Publisher : Universitas Muhammadiyah Surakarta

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.23917/forgeo.v27i2.2374

Abstract

The study demonstrated the application of statistical method to describe physical and hydro-meteorological characteristics by means of time series analysis.  Fifteen(15) watersheds in East Java were selected for this study. Data input for the analysis include: physical data, rainfall and discharge. Physical data of the watershed (topography, river network, land use, and soil type) are extracted from existing database and treated using GIS Software. Daily rainfall data were collected from existing pluviometers around the region. Daily discharge data were obtained from measurement station located at the outlet of each watershed. Areal Rainfall for each watershed was determined using average value of existing pluviometers around the watershed and determined using simple arithmetic method. These time series data are then imported to RAP (River Analysis Package).  Analysis on the RAP, include: general statistical, flow duration curve (FDC), and baseflow analysis. The result then presented in graphic and tables. Research shows that among the watersheds have different physical and hydrological characteristics.
The Visualization Study on the Slug Flow Mechanisms of the Air-Water Two-Phase in a 50 mm Horizontal Pipe Dinaryanto, Okto; Hudaya, Akhmad Zidni; Deendarlianto, Deendarlianto; Indarto, Indarto
SENATIK STT Adisutjipto Vol 4 (2018): Transformasi Teknologi untuk Mendukung Ketahanan Nasional [ ISBN 978-602-52742-0-6 ]
Publisher : Sekolah Tinggi Teknologi Adisutjipto

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (560.273 KB) | DOI: 10.28989/senatik.v4i0.171

Abstract

The slug flow phenomena are often encountered in various industrial applications such as petroleum, process, and power plant. The presence of slug flow should be avoided as it causes structural damage due to resonance, corrosion and pipes blast. From the view point of multiphase flow, the understanding of the slug initiation mechanism is very important in pipeline design. This research is conducted using horizontal transparent acrylic pipes with diameters of 50 mm with a variation on the superficial velocity of water between 0,1 m/s and 0,77 m/s and superficial velocity of air between 0,31 m/s and 6,2 m/s. In the present experimental study, the slug initiation mechanisms was explained by visual observation by using high speed video cameras. As the results, the slug flow initiation mechanism were clarified. Furthermore, the proposed of flow initiation map was introduced.
Preliminary Assessment of Morphometric and Hydrological Properties of Six Watersheds in the Eastern Part of East Java Indarto, Indarto; Hidayah, Entin
Forum Geografi Vol 33, No 1 (2019): July 2019
Publisher : Universitas Muhammadiyah Surakarta

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.23917/forgeo.v33i1.7858

Abstract

A hydrological process on the watersheds is driven by rainfall as the input. Physical properties  also affect the magnitude response of the watershed to produce run-off. This paper presents the identification, assessment and visualisation of morphometric and hydrological properties of the watersheds.  Six watersheds in the eastern part of East Java were used for the analysis.  Physical characteristics obtained by cropping the GIS layer with a watershed. Topographic and morphometric properties of the watersheds derived from the ASTER G-DEM2. Furthermore, hydrological properties are derived statistically by analysing available rainfall and discharge data. Hydrological data (rainfall and discharge) are available from 1996 ? 2014.  Finally, simple statistical analysis by plotting obtained values are used to interpret the relation between morphometric and hydrological properties of the watersheds. The results show the quantitative number (unit) to describe the morphometric and hydrological properties of the six watersheds that can be used for watershed classification.
Co-Authors . Agato A.J, Dyah Nirmala Achilleus Hermawan Astyanto Achmad Aminudin Achmad Subagio Adi Saputro, Endri Aditya, Mifta Afisna, Lathifa Putri Agafatmi, Izzun Agato, Agato Agung Purnomo Agus Kirwanto Agustina, Dwi Tri Ahmad Zamani, Ahmad Aisyah Tri Septiana Akhmad Andi Saputra, Akhmad Andi Akhmad Azmiardi Akhmad Zidni Hudaya Al Huda, Luqman Albert , Albert Albert Albert Alfeus Sunarso Alva Edy Tontowi Aminingtyas, Septi Andini Anasulfalah, Hakim Angelia Isabela, Anggraeni Anggita Gigih Wahyu Iriawan, Anggita Gigih Wahyu Ani Nur Fauziah, Ani Nur Aprih Santoso Aqsyari, Rizki Ardia Pramesti, Risa Ardiani Ika Sulistyawati Arifanto, Bangun Arjasari, Nova Sulung Arsyistawa, Hadana Sabila Aryandhi, Erki Atmojo, Joko Tri Atria Noviani, Nindy Auraldi Nansurya, Alga Aurasti, Dirgantara Tampan Putra Ayuwulanda, Aditya Azkiyah, Lailatul Baehaqi Bahariawan, Amal Bambang Piluharto Baskoro, Adyatmo Nindyo Bawono, Reza Luthfi Bayu Setiawan Budi Sustriawan Budiarti, Yuli Budiwiyanto, Joko Budiyanto, Nikolaus Eko Budiyono Budiyono Cahyadi, Puas Daryanto Daryanto Deendarlianto Dewi Larasati, Dewi Dewi Lieskusumastuti, Anita Dewi Puspitasari Dharma, Danang Setya Dina Irawati Djamali, R. Abdoel Djoko Santoso Dwi Budi Santoso Dwi Lestari Dwi Yuliaji Dwiyanti, Inayatus Nur Eko Kuswanto El Fahmi, Hasan Elida Novita Elok Waziiroh Endah Setyaningrum, Endah Entin Hidayah Eri Pramuja, Wanda Ernanda, Heru Ernawati, Heni Fatoni, Ramadhan Noor Rachman Febri Susanti, Rinandita Febrianto, Hendra Fithri Selva Jumeilah, Fithri Selva Fitriati, Annisa Fitriyah, Fatma Gabronino, Rosalia T Ghifari, M. Alvien Giyarto Giyarto Gusti Arya Rahardiansyah, Muhammad Halimah Halimah Hamdito, Octaviangga Handayani, Ratih Hapsari Hanif, Ihsan Hanifah, Lilik Hasan, Moh. Dwi Kurniawan Hawa Purnama Celala Ary Cane Herry Pintardi Chandra Hidayati, Anisa Husna, Syifaul I Putu Artama Wiguna Idah Andriyani IGNB. Catrawedarma Ihdina Fityatal Hasanah, Yesi Ika Yuli Ayuningrum Indah Lestari, Rohmini Indah Wulandari, Dwi Indri Kusuma Dewi, Indri Kusuma Infitharina, Erna Irsyam, Mahrus Ismail, Aem Ismu Handoyo Iswahyuni, Sri Izza, Ainul Jarwanto, Slamet Jatmika, Ujang Rangga Jayawarsa, A.A. Ketut Joan Pamungkas, Ivo Joko Tri Wibowo, Joko Tri Joko Triwibowo, Joko Joko Yulianto, Dwi Karmadi, Karmadi Katagame, Romario Kesi Widjajanti Kesi Widjajanti Khansa Azizah, Fara Kharisma, Sunandi Khasani Khasani Kiswanta Kiswanta, Kiswanta Kuntari, Saras Kurnianto, Fahmi Arif Kurniasih, Dwi Kusumaningsih, Haslinda Kuswardani Kuswardani, Kuswardani Latifah, Najwa Esthi Lestari, Ning Puji Lestari, Rohmini Indah Mahmud Rudini Mahmuddin, M Mandala, Marga Maquilling, Rebecca R Maratul Munawar, Siti Margaretha Maria Shinta Pratiwi Marsaorlina S., Imelda Maryadi , Shendy Akbar Mas'udi, Ach. Fauzan Mas'udi, Ach. Fauzan Mas'udi Masabdi, Habib Hasan Abdi Maulana, Agam Maulida H, Ardiana Nur Medha, Akbar Yuga Adhikara Miranda Juandrina, Shella Mirsanti, Faradilla Muhammad Luthfi Mulya Juarsa Murtiningsih, Dwi Naufal, Dimas Ahmad Nazdirah, Rufiani Ngizati, Naila Alfi Ningrum, Andriani Noerlita Noerlita Ningrum, Andriani Novianty, Yurike Novitasari, Meliana Nugroho, Andika Yuliana Esti Nugroho, Fellando Martino Nur Aini Nur Fauziah, Ani Nur Rokhmatun, Puji Nur Wijayanti, Anisa Nurfalitasari, Iftika Nurhayati, Isnani Nurrochim, Nurrochim Nurud Diniyah Ohee, Thomas Alva Edison Oktaviandi, Ryan Okto Dinaryanto Palgunadhi, Hasri Pamungkas, Achmad Ivo Joan Pamungkas, Qohin Hadi Pardi Pardi, Pardi Perwira, Budi Cahya Peter F Kaming Pradana Putri, Anggie Pradana, Anggie Pratiwi, Pramita Yuli Prayogo, Dimas Prihananto, Vincentius Priza Pandunata Probowati, Banun Diyah Puji Lestari, Apriliani Purnamasari, Utari Purnawiyanto, Hari Purnomo Purnomo Purnomo, P Purwanto, Joko None Puspitasary, Kiki Putra, Hereg Suswanto Putra, Narendra Bayu Rahayu, Chairiyah Umi Rahma Widyaningrum, Nova Rahmat Kurniawan Rasyid Ridha, Achmad Rejo, Rejo Reksa Belagama, Hadrian Retno Setyawati Reza Kurnia, Febria Rismawati, Ajeng Febrian Rohmi, Rohmi Rosalina, Neni Nurul Roy Waluyo Rufiani Nadzirah Rusdianti, Endang Sabngatun, Sabngatun Saddewisasi, Wyati Sakka, La Samsul Kamal Santi Dwi Astuti Saputra, Ariansyah Sarastri, Linggar Sari Wijayanti Sari, Putri Nata Satria Admaja, Tegar Savitri, Fania Savitri, Fania Mutiara Sayekti Heni Sunaryanti, Sri Septian, Taufiq Dwi Setiawan Manurung, Budi Setyoninsih, Sulis Setyorini, Catur SETYOWATI, N. Sindi Wardani, Galuh Siswoyo Soekarno Siti Maesaroh Siti Zubaidah Solly Aryza Sri Lestari Subarman, Subarman Suciyati Suciyati, Suciyati Sugiarti, Rini Sujarwo, Mohamad Wawan Sukamta Sukamta Suliman, Nageeb Mohammed Sumarsono, Agus Sumarsono, Agus Supramono Suprayitno Suprayitno Suryaningsih, Ester Putri Swandriya, Swandriya Syauqi Mubarok, Ahmad Tan, Joel B. Taradipa, Azzahra Taslikah, Taslikah Thomas S. W. Tri Agung Rohmat Tri Agung Rokhmat, Tri Agung Tri Atmojo, Joko Tri Darmayanti, Aquartuti Tri Handayani, Rina Tri Yuniarti, Tri Tsamrudin, Muhammad Tugiyono Tugiyono Verasita, Prissy Wahyurudhanto, Albertus Wardoyo, Paulus Wati, Kusuma Citra Wibawa Endra Juwana, Wibawa Endra Wibowo, Josephine Andrea Widayat, Hadi Widiastuti, Endang Retna Triwati Widiastuti, Hardhani Widiyanto, Aris Widyaningsih, Dini Retno Wiratni Wiratni, Wiratni Wulansari, Sri Mugi Yugiantoro, Darojat Yuli Budiati Yulianto, Dwi Joko Yulianto, Edwin Yundari, Yundari Yusuf Rahman