Garuda - Garba Rujukan Digital

p-Index From 2021 - 2026

4.881

P-Index

This Author published in this journals

All Journal POSITRON Jurnal Penelitian Fisika dan Aplikasinya (JPFA) TELKOMNIKA (Telecommunication Computing Electronics and Control) Jurnal Fisika Unand Emerging Science Journal Jurnal Penelitian Pendidikan IPA (JPPIPA) Logista: Jurnal Ilmiah Pengabdian Kepada Masyarakat Jurnal Ilmu Fisika MONSU'ANI TANO Jurnal Pengabdian Masyarakat Riyadhoh : Jurnal Pendidikan Olahraga BERNAS: Jurnal Pengabdian Kepada Masyarakat Warta Pengabdian Andalas: Jurnal Ilmiah Pengembangan Dan Penerapan Ipteks

Marzuki Marzuki

Department Of Physics, Faculty Of Mathematics And Natural Sciences, Universitas Andalas, Padang 2516, West Sumatra, Indonesia

Author-ID : 1133611

Religion Agriculture, Biological Sciences & Forestry Humanities Astronomy Biochemistry, Genetics & Molecular Biology Chemical Engineering, Chemistry & Bioengineering Chemistry Civil Engineering, Building, Construction & Architecture Computer Science & IT Dentistry Earth & Planetary Sciences Education Electrical & Electronics Engineering Energy Environmental Science Languange, Linguistic, Communication & Media Materials Science & Nanotechnology Mathematics Medicine & Pharmacology Neuroscience Nursing Physics Public Health Social Sciences Veterinary Other

Published : 67 Documents Claim Missing Document

Claim Missing Document

Articles

1 2 3 4 5

Karakteristik Ketinggian Melting Layer di Indoneisa Berdasarkan Radar Hujan Yang Terpasang di Satelit TRMM Dwianda, Rany Audia; Marzuki, Marzuki
Jurnal Ilmu Fisika Vol 10, No 2 (2018): Published in September 2018
Publisher : Universitas Andalas

Ketinggian melting layer atau freezing level height (FH) di Indonesia telah diteliti melalui data radar hujan yang terpasang di satelit Tropical Rainfall Measuring Mission (TRMM). Data yang digunakan adalah data TRMM 2A25 versi 7 selama 2011-2013. Nilai FH dari TRMM dibandingkan dengan nilai yang direkomendasikan oleh model ITU-R P.839. FH di Indonesia memiliki variasi musiman dan diurnal yang signifikan. Rata-rata bulanan FH menunjukkan pola bimodal dengan dua puncak dan dua lembah, mirip dengan pola curah hujan dan temperatur permukaan air laut di Indonesia. Puncak FH teramati pada bulan-bulan basah (musim hujan) ketika temperatur permukaan air laut tinggi. Nilai FH mencapai puncaknya pada sore hari yaitu sekitar jam 18-19 waktu setempat. Adanya perbedaan pola FH antara darat dan laut yang menandakan adanya pengaruh sirkulasi darat-laut (land-sea breezes). Pada dini dan pagi hari, hujan dengan FH > 5 km tidak teramati di daratan tetapi pada siang dan sore hari jumlahnya meningkat, terutama di Sumatera, Kalimantan dan Papua. Nilai FH tertinggi yang teramati dalam penelitian ini adalah 5,55 km yang teramati pada 2013, dan nilai terendah adalah 4,40 km, yang teramati pada 2012. Sebagian besar hujan yaitu sekitar 82% dari total data, memiliki FH lebih rendah dari yang direkomendasikan oleh ITU-R P.839 (5 km). Dengan demikian, model ITU-R menakar FH lebih tinggi dari semestinya. Selain itu, asumsi nilai FH yang konstan (5 km) dalam model ITU-R juga tidak tepat karena nilai FH di Indonesia menunjukkan variasi diurnal dan musiman yang signifikan.Â Kata kunci : melting layer, Indonesia, TRMM-PR, ITU-R P.839, variasi diurnal, variasi musimanÂ

Pemanfaatan Data Satelit Tropical Rainfall Measuring Mission 3A25 dan 3B43 Sebagai Input Model ITU-R untuk Mengestimasi Intensitas Curah Hujan di Indonesia Harysandi, Dea Kurnia; Marzuki, Marzuki
Jurnal Ilmu Fisika Vol 11, No 2 (2019): Published in September 2019
Publisher : Universitas Andalas

Model yang dikeluarkan oleh International Telecommunication Union-Radiocommunication Sector (ITU-R) digunakan secara luas untuk menentukan intensitas curah hujan dalam pemodelan penjalaran gelombang elektromagnetik dalam medium hujan. Parameter yang digunakan untuk menentukan intensitas curah hujan adalah curah hujan rata-rata tahunan (Mt) dan probabilitas hujan (P0). Input data dari model ITU-R berasal dari data 40-year ECMWF re-analysis (ERA-40) dengan resolusi spasial dan temporal yang rendah. Penelitian ini menguji penggunaan data satelit Tropical Rainfall Measuring Mission (TRMM) 3A25 dan 3B43 yang memiliki resolusi spasial yang lebih baik sebagai input data ITU-R (ITU-R P.837-6). Data TRMM yang digunakan adalah data dari tahun 1998 sampai 2014. Hasil estimasi dibandingkan dengan model ITU-R standar dan kemudian divalidasi dengan data rain gauge di Kototabang dan data DBSG3 untuk Bandung. Hasil penelitian menunjukkan bahwa penggunaan data TRMM 3A25 dan 3B43 sebagai input model ITU-R P.837-6 cukup akurat untuk mengestimasi curah hujan di Indonesia. Nilai root mean square error (RMSE) dan persentase error yang didapatkan dari data TRMM dan model ITU-R tidak jauh berbeda ketika dibandingkan dengan data rain gauge dan DBSG3. Untuk keseluruhan data di Kototabang, nilai RMSE dari TRMM dan ITU-R berturut-turut adalah 21,97 dan 16,70 mm/h dengan persentase error 16,28% dan 9,63%. Untuk Bandung, nilai RMSE ketika dibandingkan dengan data DBSG3 adalah 8,72 mm/h (TRMM) dan 1,72 mm/h (ITU-R) dengan persentase error 16,18% (TRMM) dan 11,13% (ITU-R). Dengan demikian, ITU-R dengan input ERA-40 lebih akurat dari ITU-R dengan input TRMM 3A25 dan 3B43 untuk mengestimasi intensitas curah hujan menitan di Indonesia.Kata kunci: Intensitas curah hujan, TRMM, ITU-R P.837-6, Indonesia

Rancang Bangun Sistem Pengukuran Diameter Butiran Air Menggunakan Fotodioda Array dan Transceiver nRF24L01+ Awaluddin, Awaluddin; Harmadi, Harmadi; Marzuki, Marzuki
Jurnal Ilmu Fisika Vol 11, No 2 (2019): Published in September 2019
Publisher : Universitas Andalas

Telah dilakukan rancang bangun sistem pengukuran diameter butiran air menggunakan fotodioda array dan transceiver nRF24L01+. Sistem pengukuran diameter butiran air terdiri dari laser dioda, fotodioda array, mikrokontroler Arduino Uno R3 dan transceiver nRF24L01+. Pengukuran dilakukan saat butiran air yang berasal dari wadah, dengan variasi ukuran diameter; 1 mm, 2 mm, dan 3 mm, melewati sinar laser dan ditangkap oleh fotodioda array. Fotodioda array mengubah cahaya menjadi sinyal listrik dalam bentuk tegangan keluaran dan diolah menggunakan mikrokontroler Arduino Uno R3. Data yang dihasilkan dikirim secara telemetri nirkabel dengan menggunakan transceiver nRF24L01+ dan ditampilkan pada PC dan LCD dalam bentuk hasil pengukuran. Karakterisasi sensor fotodioda array menghasilkan nilai koefisien determinasi (R2) sebesar 0,997 dan nilai fungsi transfer yaitu 21,975eâ€“0,004x yang dimasukkan ke dalam program. Hasil pengujian memperlihatkan semakin rendah tegangan menandakan diameter butiran air hujan semakin besar. Hasil pengukuran diameter butiran air memiliki nilai error rata-rata 0,66. Sistem memiliki jarak pengiriman maksimum 1000 m tanpa penghalang dan jarak pengiriman minimum 550 m dengan penghalang.Kata kunci: fotodioda array, pengukuran butiran air, transceiver nRF24L01+

Analisis Variasi Diurnal Curah Hujan di Sumatera Barat Menggunakan Data Rain Gauge dan IMERG Suryanti, Krisna; Fitriyani, Dian; Muharsyah, Robi; Marzuki, Marzuki
POSITRON Vol 10, No 2 (2020): Vol. 10 No. 2 Edition
Publisher : Fakultas Matematika dan Ilmu Pengetahuan Alam, Univetsitas Tanjungpura

Variasi diurnal adalah salah satu komponen utama variasi atmosfer di kawasan tropis yang menimbulkan dampak terhadap siklus hidrologi dan bidang terkait. Sebagai interaksi antara daratan dan lautan sekitarnya, fenomena ini dipengaruhi oleh kondisi topografi. Penelitian ini bertujuan untuk menganalisis variasi diurnal dari akumulasi, frekuensi dan intensitas curah hujan dalam kaitannya dengan topografi di Sumatera Barat menggunakan data rain gauge dari 17 stasiun selama 2014â€’2019. Pola diurnal dan semidiurnal curah hujan dimodelkan melalui metode dekomposisi harmonik menggunakan discrete Fourier transform (DFT). Secara umum, akumulasi dan frekuensi curah hujan daerah pesisir pantai dan dataran tinggi, lebih besar daripada daerah dataran rendah. Namun sebaliknya, intensitas curah hujan lebih besar di dataran rendah daripada wilayah pesisir pantai dan dataran tinggi. Secara umum puncak intensitas curah hujan terjadi pada pukul 15.00â€’16.00 WIB pada daerah pesisir pantai dan pada pukul 17.00â€’18.00 WIB di dataran rendah. Hujan memiliki frekuensi kemunculan tertinggi pada pukul 16.00â€’18.00 WIB di sebagian besar daerah pesisir pantai dan pada pukul 19.00â€’21.00 WIB di dataran rendah. Puncak akumulasi hujan terjadi pada pukul 16.00â€’19.00 WIB di sebagian besar daerah pesisir pantai dan pada pukul 20.00â€’22.00 WIB di dataran rendah. Puncak curah hujan pada pagi hari juga ditemukan di pulau-pulau kecil pada kawasan Sumatera Barat. Selain puncak dominan pada sore hari, beberapa lokasi memiliki puncak kedua yang intensitasnya lebih rendah. Puncak dari akumulasi, frekuensi dan intensitas curah hujan dari rain gauge konsisten dengan data integrated multi-satellite retrievals for GPM (IMERG) tetapi puncak curah hujan dari data IMERG satu jam lebih lambat daripada data rain gauge, sebagaimana pernah ditemukan oleh peneliti sebelumnya. Akumulasi, frekuensi dan intensitas curah hujan diurnal sesuai dengan pola distribusi variasi diurnal temperatur dan kelembaban relatif.

Long-Term Change in Characteristics of Cloud Vertical Structures Over Sumatra from Radiosonde Observations Lismalini, Lismalini; Marzuki, Marzuki; Shafii, Mohammad Ali
Jurnal Ilmu Fisika Vol 13, No 1 (2021): Published in March 2021
Publisher : Universitas Andalas

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25077/jif.13.1.41-53.2021

Study on the vertical structure of cloud in Indonesia in terms of climate change is still very limited. We investigated the long-term change in characteristics of cloud vertical structures over Sumatra from three radiosonde observation stations in this work. The cloud base height (CBH), cloud top height (CT), and the number of cloud layers were retrieved using relative humidity (RH) profiles from radiosonde observation. The height of the cloud base is determined by taking the height of the layer with relative humidity (RH) value > 84% with at least a 3% jump in the RH from the ground level. Sumatraâ€™s most frequently observed cloud layer is a one-layer cloud with an average occurrence rate of > 60%, which is slightly larger than the one-layer cloud globally. The percentage of appearance values at the Padang station, Pangkal Pinang, and Medan are 63.58%, 69.50% and 66.05%. The appearance of low-level clouds also dominates in Sumatra compared to other cloud types. CT and CBH increase with the number of years including all seasons. This is in line with the increase in temperature in Indonesia reported by previous researchers. On the other hand, the cloudsâ€™ thickness, especially for the cloud with one layer, varies from one location to another. The thickness of clouds decreases at Padang station and does not change at Pangkal Pinang and Medan stations.

Estimation of Raindrop Size Distribution Parameters Using Lightning Data over West Sumatra Salma, Faridah; Marzuki, Marzuki; Hashiguchi, Hiroyuki; Nauval, Fadli
Jurnal Ilmu Fisika Vol 13, No 2 (2021): Published in September 2021 (COMING ISSUE)
Publisher : Universitas Andalas

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25077/jif.13.2.92-100.2021

In situ observations of raindrop size distributions (DSDs) are still limited, especially in the tropics. Therefore, this study develops an alternative method to calculate DSD parameters by utilizing lightning data from the World-Wide Lightning Location Network (WWLLN) observation. DSD data was obtained from Parsivel's observations in the equatorial regions of Indonesia, i.e., Kototabang (100.32â—¦E, 0.20â—¦S, 865 m above mean sea level/ASL), Padang (100.46Â°E, 0.915Â°S, 200 m ASL), and Sicincin (100.30Â°E, 0.546Â°S, 134 m ASL). A gamma distribution parameterized the DSD. Three analysis domains were examined, with a grid of 0.1Â° x 0.1Â°, 0.5Â° x 0.5Â°, and 1Â° x 1Â°.Â We examined the possibility to calculate the near-instantaneous DSD parameter, so three short time intervals, namely, one, five and ten minutes, were used. The results showed that the number of lightning strokes does not adequately correlate with DSD parameters. This is observed in all time intervals and analysis domains. Thus, the use of lightning data to calculate DSD parameters is not possible for short time interval of DSD (near instantaneous DSD). However, lightning data can estimate the average DSD parameters for an average time of more than one hour, as recommended by previous studies.

Comparison of Bright Band Radar from GPM and MRR Observation in West Sumatera Ramadhan, Ravidho; Marzuki, Marzuki; Vonnisa, Mutya; Harmadi, Harmadi; Hashiguchi, Hiroyuki; Shimomai, Toyoshi
Jurnal Penelitian Fisika dan Aplikasinya (JPFA) 2021: Articles in Press
Publisher : Universitas Negeri Surabaya

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.26740/jpfa.v11n1.p%p

AbstractThe Bright band (BB) measurement from NS scan on Global Precipitation Measurement (GPM) had been compared with Micro Rain Radar (MRR) which is installed in Kototabang, West Sumatera (0.23o S; 100.32oE; 865 m above sea level). The GPM data were collected from December 2014 to June 2018 and compared with MRR observation from January 2012 to August 2016. The BB values from these instruments were also compared with the values recommended by the International Telecommunication Union Recommendation (ITU-R) P.839. The BB from GPM and MRR shown slightly diurnal and seasonal variations. BB observations from GPM and MRR show good agreement with slightly difference in diurnal and seasonal variations. BB observations are more similar when the intensity of solar radiation is lower, ie at night (18.00-24.00 LT) until dawn (00.00-06.00 LT). Furthermore, MRR determined a slight bimodal pattern in the seasonal variation while GPM did not, it cause variation in observation of both instrument quite significant in seasonal variation. The largest different from the seasonal variation was observed in the summer season (Juni-August(JJA)). Moreover the measurement of the mean BB is still below the Freezing Height Level (FHL) value from ITU-R model, the measurement of both instruments obtained a high number than FHL considerably (>36 %). It showed the constant value for FHL in West Sumatera that would cause the attenuation estimation of microwaves to be less accurate.

International Telecommunication Union-Radiocommunication Sector P.837-6 and P.837-7 performance to estimate Indonesian rainfall Marzuki Marzuki; Dea Kurnia Harysandi; Rini Oktaviani; Lisna Meylani; Mutya Vonnisa; Harmadi Harmadi; Hiroyuki Hashiguchi; Toyoshi Shimomai; L. Luini; Sugeng Nugroho; Muzirwan Muzirwan; Nor Azlan Mohd Aris
TELKOMNIKA (Telecommunication Computing Electronics and Control) Vol 18, No 5: October 2020
Publisher : Universitas Ahmad Dahlan

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.12928/telkomnika.v18i5.14316

This work evaluated the performance of International Telecommunication Union-Radiocommunication Sector (ITU-R) P.837-6 and P.837-7 models (Annex 1) to estimate one-minute rainfall rates in Indonesia. In addition to the default ITU-R P.837-6, the input of ITU-R P.837-6 is also modified using data which has better spatial resolution, i.e. a combination of Tropical Rainfall Measuring Mission (TRMM) 3A25 and 3B43 (ITU-R+3A25+3B43), 3B42 and 3B43 (ITU-R+3B42+3B43), Global Satellite Mapping of Precipitation (ITU-R+GSMaP), and Global Precipitation Measurement (ITU-R+GPM). Among the five test sites, the default ITU-R P.837-6 and ITU-R+3A25+3B43 could predict one-minute rainfall rates at two locations accurately. The ITU-R P.837-7 exhibited a marginally better performance for sites that had a high percentage of very heavy rain, particularly at large (1%) and small (0.001%) percentages of time exceeded. The spatial distribution of rainfall rate produced by ITU-R P.837-7 and ITU-R+3A25+3B43 was closer to the pattern demonstrated by recent satellite precipitation measurements.

Vertical Characteristics of Raindrops Size Distribution over Sumatra Region from Global Precipitation Measurement Observation Ravidho Ramadhan; . Marzuki; . Harmadi
Emerging Science Journal Vol 5, No 3 (2021): June
Publisher : Ital Publication

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.28991/esj-2021-01274

The climatology of the vertical profile of raindrops size distribution (DSD) over Sumatra Region (10° S – 10° N, 90° E – 110° E) has been investigated using Global Precipitation Measurement (GPM) level 2 data from January 2015 to June 2018. DSD's vertical profile was observed through a vertical profile of corrected radar reflectivity (Ze) and two parameters of normalized gamma DSD, i.e., mass-weight mean diameter (Dm) and total drops concentration (Nw). Land-ocean contrast and rain type dependence of DSD over Sumatra were clearly observed. The values of Dm and Nw were larger in the land than in the ocean. Negative and positive gradients of Dm toward the surface were dominant during stratiform and convective rains, respectively, consistent with the Z gradient. Moreover, the negative gradient of stratiform rain in the ocean is larger than in land. Thus, the depletion of large drops is dominant over the ocean, which is due to the break-up process that can be observed from the increase of Nw. Raindrop growth of convective rains is more robust over the ocean than land that can be seen from a larger value of Dmgradient. The BB strength is slightly larger over land and coastal region than over the ocean, indicating that the riming process is more dominant over land and coastal regions than the ocean. Doi: 10.28991/esj-2021-01274 Full Text: PDF

Retrieval of Vertical Structure of Raindrop Size Distribution from Equatorial Atmosphere Radar and Boundary Layer Radar Mutya Vonnisa; Toyoshi Shimomai; Hiroyuki Hashiguchi; Marzuki Marzuki
Emerging Science Journal Vol 6, No 3 (2022): June
Publisher : Ital Publication

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.28991/ESJ-2022-06-03-02

This work develops an algorithm to retrieve the vertical structure of the raindrop size distribution (DSD) of rain from simultaneous observations of 47 MHz Equatorial Atmosphere Radar (EAR) and 1.3 GHz Boundary Layer Radar (BLR) at Koto Tabang, West Sumatra, Indonesia (0.20°S, 100.32°E, 865 m above sea level). EAR is sensitive to the detection of turbulence, and BLR is susceptible to identifying precipitation echo. The EAR Doppler spectrum broadening effects due to turbulence and finite radar beam width were reduced using the convolution process. The Gaussian function was used to model the turbulence Doppler spectrum. A non-linear least-squares fitting method was applied to retrieve DSD parameters. Subsequently, the equations to estimate DSD using this dual-frequency algorithm assume the gamma DSD model to retrieve the distribution from the Doppler spectrum of precipitation echo. The precipitation events on April 23, 2004 on the Coupling Processes in the Equatorial Atmosphere (CPEA-I) project have been analyzed. Results show that the precipitation spectrum obtained using the dual-frequency method is higher, more precise, and well-fitted than the single-frequency method, meaning the dual-frequency method has great potential to be used in observing the microphysical process and remote sensing application analysis of DSD in Indonesia, particularly at Koto Tabang. The analyses show various microphysical processes that occur in the rain, such as coalescence, evaporation, break-up, and condensation. Furthermore, for the purpose of easier remote sensing application analysis of profile DSD characteristics, we use a DSD ΔΖMP parameter. ΔΖMP is a rain rate insensitive DSD parameter representing mean drop size. The trend of ΔZMP is not totally uniform with regards to rain rate and reflectivity factors, with ΔZMP higher in the first half of the event and becoming lower toward the end. This suggests that we have to use different Z-R relations within the event. Doi: 10.28991/ESJ-2022-06-03-02 Full Text: PDF

Co-Authors -, Renanto Adi Susilo Afdal, Afdal Afdhal Muttaqin Afrizal Afrizal Ahmad Fauzi Pohan Ahmad Rizqy Shubri Ahmad Zul Amal Zaini Ardian Putra Arif Budiman Arif Ismul Hadi Astuti Astuti Astuti Astuti Astuti Aulya Rahayu Aulya Rahayu Aulya Rahayu, Aulya Awaluddin Awaluddin Awaluddin Awaluddin Ayu Putri Ningsih Ayu Putri Ningsih Bella Deswanti Bunga Aprilia Dahyunir Dahlan Dea Kurnia Harysandi Dea Kurnia Harysandi Deasy Arisa Dedi Mardiansyah Dian Fitriyani Dian Fitriyani Dinda Maulani Adfy Dwi Pujiastuti Dwi Puryanti Dwianda, Rany Audia Elfira Saufina Elfira Saufina Elvaswer Elvaswer Fadilla Monica Fadli Nauval Faridah Salma Feri Helmi Basri Feriska Handayani Irka, Feriska Handayani Fery Kurnia Sandi Gina Felita Harmadi Harmadi Harysandi, Dea Kurnia Helmi Yusnaini Helmi Yusnaini Helmi Yusnaini Helmi Yusnaini Hiroyuki Hashiguchi Hiroyuki Hashiguchi Hiroyuki Hashiguchi Hiroyuki Hashiguchi Hiroyuki Hashiguchi Hiroyuki Hashiguchi Hiroyuki Hashiguchi Hiroyuki Hashiguchi Hiroyuki Hashiguchi Hiroyuki Hashiguchi, Hiroyuki Ikhwan Fikri Maulidan Imam Taufik Imam Taufiq Indah Rahayu Iqbal Ramadhan Irza Utami L. Luini Lismalini Lismalini Lismalini, Lismalini Lisna Meylani Lusi Fitrian Sani Lusi Fitrian Sani Lusi Fitrian Sani, Lusi Fitrian Melly Angglena Meqorry Yusfi Meri Yoseva Mohammad Ali Shafii Mora Mora Mora Mora Mora Muchtia Rahma Muchtia Rahma, Muchtia Muhammad Arif Muhammad Kahfi Muharsyah, Robi Muldarisnur, Mulda Mutya Vonnisa Muzirwan Muzirwan Naela Amalia Zulfa Nauval, Fadli Nina Nina Nini Firmawati Nor Azlan Mohd Aris Novianti Indrastuti Nugroho, Susilo Nur Fadillah Nurdin Nurdin Nurul Hasanah Poltak Sandro Rumahorbo Poltak Sandro Rumahorbo, Poltak Sandro Puja Kasmailen Putri Rahmad Rasyid Rahmad Rasyid Rahmat Rasyid Ramacos Fardela Ramadani Safitri Ramadani Safitri Ramadhan, Ravidho Rani Delvihardini Rany Audia Dwianda Ravidho Ramadhan Ravidho Ramadhan Ravidho Ramadhan Ravidho Ramadhan Ravidho Ramadhan Ravidho Ramadhan Rifa Lihayati Rini Oktaviani Rio Chandra Rio Chandra, Rio Robi Muharsyah Salma, Faridah Selly Tridaiana Shimomai, Toyoshi Sholihun, Sholihun Silvia Wahyuni Solly Aryza Sri Hamdiyessi Sri Handani Sri Herlinda Sri Mai Dewi Sri Oktamuliani Sri Wahyuni Sri Wahyuni Sucy Lestari Wirma Sugeng Nugroho Suryanti, Krisna Suryanto, Wiwit Syarifatul Ulfah Toyoshi Shimomai Toyoshi Shimomai Toyoshi Shimomai Toyoshi Shimomai Toyoshi Shimomai Toyoshi Shimomai Trengginas Eka Putra Sutantyo Triana Vitri Triana Vitri, Triana Ulfa Azmi Usna, Sri Rahayu Alfitri Vira Friska Vira Friska Vira Friska Wendi Harjupa Wildian Wildian Wira Indrayani Yudi Saputra Zul Ikram Zulfi Zulfi Zulfi

Title

Found 67 Documents
Search

Abstract

Abstract

Abstract

Abstract

Abstract

Abstract

Abstract

Abstract

Abstract

Abstract

Title Search

Found 67 Documents Search

Abstract

Abstract

Abstract

Abstract

Abstract

Abstract

Abstract

Abstract

Abstract

Abstract

Title

Found 67 Documents
Search