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All Journal Indonesian Journal of Geography Bulletin of Scientific Contribution : Geology Journal of Tropical Soils IJOG : Indonesian Journal on Geoscience Journal of Degraded and Mining Lands Management Techno LPPM Journal of Geoscience, Engineering, Environment, and Technology SAINS TANAH - Journal of Soil Science and Agroclimatology EnviroScienteae Jurnal Mineral, Energi dan Lingkungan Pharmed: Journal of Pharmaceutical Science and Medical Research KURVATEK Jurnal Mineral, Energi dan Lingkungan Indonesian Journal on Geoscience Indonesian Journal on Geoscience Journal of Earth and Marine Technology (JEMT) Jurnal Pengabdian Teknologi Tepat Guna International Journal of Science and Society (IJSOC) Prosiding Seminar Nasional Teknologi Industri Berkelanjutan International Journal of Hydrological and Environmental for Sustainability Petro : Jurnal Ilmiah Teknik Perminyakan Jurnal Indonesia Sosial Teknologi Jurnal Ilmiah Geologi pangea Asian Journal of Social and Humanities

Dwi Fitri Yudiantoro

Unknown Affiliation

Author-ID : 6034401

Religion Agriculture, Biological Sciences & Forestry Automotive Engineering Biochemistry, Genetics & Molecular Biology Chemical Engineering, Chemistry & Bioengineering Civil Engineering, Building, Construction & Architecture Computer Science & IT Decision Sciences, Operations Research & Management Earth & Planetary Sciences Economics, Econometrics & Finance Education Electrical & Electronics Engineering Energy Engineering Environmental Science Industrial & Manufacturing Engineering Languange, Linguistic, Communication & Media Law, Crime, Criminology & Criminal Justice Materials Science & Nanotechnology Mechanical Engineering Medicine & Pharmacology Physics Public Health Social Sciences Transportation

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ETNOBOTANI TANAMAN ANTIPIRETIK MASYARAKAT DUSUN MESU BOTO JATIROTO WONOGIRI JAWA TENGAH Arum Suproborini; Mochamad Soeprijadi Djoko Laksana; Dwi Fitri Yudiantoro
Pharmed: Journal of Pharmaceutical Science and Medical Research Vol 1, No 1 (2018)
Publisher : Universitas PGRI Madiun

Traditional medicine in Indonesia has been known to the public long before formal health services with modern medicine. Indonesia has many species of plants that have properties to cure various diseases and some other useful properties for human health. Antipyretic plants are plants that have the property as a febrifuge. The content of flavonoids in plants merit as a reliever fever (antipyretic). This study aims to determine the garden plants that can be utilized by the community as a febrifuge. (antipyretic). The research method used is survey method. The location of the observation and sampling of the plants was done by purposive random sampling technique by plot plot size 2x2 meter, 5x5 meter (adjust the location of the land). Based on research and observation, there are 8 species of antipyretic plants tumeric (Curcuma domestica), papaya (Carica papaya), dadap (Erythrina sp), hibiscus (Hibiscus rosasinensis), rambutan (Nephelium lappaceum), banana ( Musa paradisiaca), soursop (Annona muricata), and yam (Pachirrhyzus erosus) which can be utilized by the local community.

Process and Mineralogy of Volcanic Materials on the South Side of the Old Lawu Volcano in Java Island Mohammad Nurcholis; Dwi Fitri Yudiantoro; Darban Haryanto; Ahmad Bagus Dianputra; Krishna Aji
SAINS TANAH - Journal of Soil Science and Agroclimatology Vol 16, No 2 (2019): December
Publisher : Universitas Sebelas Maret

Activities of Old Lawu volcano in the past resulted in various soil development in the south side of the volcano, especially in the area of the east side of Wonogiri and west side of Ponorogo, that located in the Java island. This area is also famous as herbal crops producer for raw materials of traditional herbal medicine industry. The purpose of this research is to identify the process of exposure of the parent materials in the Old Lawu volcanic environment, the development of the soil parent materials, and the mineralogy variation. Four Sites with different geological formation were observed, and each Site was selected for soil profile identification on the process of weathering of rocks. All layers of each profile were then sampled and then sand fraction of the fine earth particle was determined for the mineral type using X-ray diffraction (XRD). The results showed that materials of the Old Lawu volcanic activity that was of quaternary period had sized material of gravel, sand, silt, and clay. These materials were then exposed and undergone the process of weathering, transportation, and sedimentation according to the landform at that period. The development of soil as geoheritage in this region was influenced by the material size, landform, and settling process. There are four typologies of the environment on the soil development at the present study, there are: (1) Soil that developed in the inter-fluvial basins is characterized by thick soil and a clear horizon differentiation process as a feature of maturity stage of soil development. (2) Soil developed on the slope of hill area is characterized by shallow in solum and it is in early-stage soil development. (3) Soil developed on the volcanic materials that were transported and sedimented in the river environment is characterized by the thick soil above the layered fine size parent material with a variety of color. (4) Soil developed on the tertiary breccia showed early soil development.

KEANEKARAGAMAN TANAMAN BUAH DAN KANDUNGAN MERKURI KAWASAN PENAMBANGAN EMAS RAKYAT DUSUN MESU DESA BOTO JATIROTOWONOGIRI JAWA TENGAH Arum Suproborini; Sunarto Sunarto; Wiryanto Wiryanto; Dwi Fitri Yudiantoro; Muhammad Nurcholis; Dewi Sri Sayudi; Mirzam Abdurrachman
EnviroScienteae Vol 13, No 1 (2017): EnviroScienteae Volume 13 Nomor 1, April 2017
Publisher : Universitas Lambung Mangkurat

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.20527/es.v13i1.3508

The processing of gold by means of amalgamation produces mercury wastes. Mercury wastes can pollute the environment. This study aims to determine the diversity of fruit crops and mercury content in the gold mining area of Dusun Mesu. The research method used is survey method, measurement, field observation, and laboratory analysis. The types of plants found are recorded, the number and the diameter. Samples of roots, stems, and leaves of plants were analyzed mercury contents in the laboratory. Based on the results of the analysis, there were 7 types of fruit plants, as many as 32 individuals with the type of vegetation seedling, stake, poles, and trees. The results of calculation of diversity index (H¹), uniformity index (E), and dominance index (C) at all growth rates show low diversity (H = 0.02222 - 0.86648), low uniformity (E = 0.00403-0) , 27959), low dominance (C = 0,0000162 - 0,08). The content of mercury in the soil ranges from 0.001 to 0.044 mg/m³. The content of mercury in fruit crops ranges from <0.0001 - 0.0168%, and soil pH ranges from 4 to 6.8.

POTENSI UNSUR TANAH JARANG (RARE EARTH ELEMENTS) DI LUMPUR PANAS SIDOARJO, Indonesia Handoko Teguh Wibowo; Bambang Pratisho; C. Prasetyadi; Dwi Fitri Yudiantoro
Prosiding SENASTITAN: Seminar Nasional Teknologi Industri Berkelanjutan Prosiding SENASTITAN Vol. 02 2022
Publisher : Institut Teknologi Adhi Tama Surabaya

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (513.803 KB)

Terminologi lumpur sidoarjo (Lusi) sebagai sebuah gunung lumpur saat ini sudah tidak relevan lagi. Berdasarkan analisis geokimia menunjukkan bukti-bukti jejak gunung api pada Lusi dan sudah berkorelasi positif, sehingga Lusi dapat dikatakan sebuah sistem hidrotermal pada cekungan sedimen. Sistem hidrotermal selalu berkaitan dengan pengkayaan mineral terutama pada lapisan lempung. Fluida geotermal bersifat asam, potensial melarutkan unsur logam, sehingga kandungan unsur pada lumpur akan terpengaruh. Lusi termasuk ke dalam sistem endapan epitermal sulfida rendah (low ephitermal sulfide) dengan zona ubahan argilik yang ditandai oleh pembentukan mineral lempung yang bertemperatur rendah seperti kaolinit, smektit dan illit Adanya sistem hidrotermal yang bekerja pada Lusi dengan karakteristik tersebut membuat Lusi memiliki peluang untuk pengkayaan unsur tanah jarang. Hasil analisis laboratorium menggunakan metode ICP dan XRF didapat konsentrasi pelimpahan unsur tanah jarang seperti Ce, Dy, Eu, Gd, La, Nd, Pr, Sc, Sm dan Y yang relatif tinggi.

Reanalysis LUSI Stratigraphic Based on Cutting of Banjarpanji#1 Well Handoko Teguh Wibowo; Bambang Prastistho; C Prasetyadi; Dwi Fitri Yudiantoro
Journal of Earth and Marine Technology (JEMT) Vol 3, No 1 (2022)
Publisher : Lembaga Penelititan dan Pengabdian kepada Masyarakat - Institut Teknologi Adhi Tama Suraba

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31284/j.jemt.2022.v3i1.3602

The subsurface configuration or stratigraphy of the Sidoarjo Hot Mudflow (Lumpur Sidoarjo/LUSI) is used to see what formations are transported out and how the material properties can be known from the well log data of Banjarpanji#1 or BJP#1 well. There is something unusual about the BJP#1 log, namely the presence of solid volcanic sandstone at a depth of 6000-9297 ft where drilling ended. This abnormality was investigated by reanalyzing volcanic sandstone by reading the well log data which is drilling data during the exploration of the Banjarpanji-1 well by PT. Lapindo Brantas, Inc. which consists of rock logs as a result of predictions (prognosis) and facts found (actual) were then compared with the interpretation of the results of the investigation team with BP MIGAS 2006 which was then confirmed by petrographic and paleontological analysis. The unusual occurrence is the LUSI stratigraphic arrangement changes based on findings in volcanic sandstone sequences that were once considered part of the Kalibeng Formation of Plio-Pliestocene age, then changed to solid volcanic sandstone units of Middle Miocene age with a depositional environment in the outer neritic-upper bathyal.

Evolution Magmatism of Nagasari Volcano Dieng, Central Java, Indonesia Dwi Fitri Yudiantoro; Intan Paramita Haty; Setia Pambudi; Elisabet Magdalena; Armala Putri; I. Takashima; M. Abdurrachman
Journal of Geoscience, Engineering, Environment, and Technology Vol. 7 No. 4 (2022): JGEET Vol 07 No 04 : December (2022)
Publisher : UIR PRESS

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25299/jgeet.2022.7.4.10084

Nagasari Volcano, part of the Dieng volcanic complex, is one of the unique volcanoes in Central Java. Around this volcano grow eruption craters, volcanic cones, and pyroclastic flow ridges. There were several 14 eruption centers around Mount Nagasari, so it is necessary to know the development of magmatism evolution. The aims of the research to determine the evolutionary development of magmatism. The methodology used is geological mapping and petrographic analysis. The observations of rocks found in the study area include andesite lava, lapilli-tuff, fallen pyroclastic breccias, and flow pyroclastic breccias. Meanwhile, geological mapping and petrographic observations of volcanic rock samples show that the evolution of magmatism in the study area from the oldest to the youngest is basaltic magma that formed Prau Volcano in the pre-caldera period. On the other hand, magmatism in the post-caldera I period was of the type of pyroxene andesite forming the Gembol to Jimat Volcano group. In contrast, in the post-caldera II period, the hornblende-biotite andesite group formed the Dieng Kulon to Kendil group.

Magma Evolution of Ngebel Volcano, Ponorogo, East Java, Indonesia Dwi Fitri Yudiantoro; Dyah Rini Ratnaningsih; Puji Pratiknyo; Mahreni Mahreni; Dewi Sri Sayudi; Intan Paramita Haty; Hafiz Hamdalah; Mirzam Abdurrachman; Isao Takashima; Wisnu Ismunandar; Richzkey Muhammad; Demi Ganjar Sampurno
Indonesian Journal on Geoscience Vol 10, No 1 (2023)
Publisher : Geological Agency

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.17014/ijog.10.1.51-62

The magma evolution of Ngebel Volcano, both temporally and spatially, is represented by the characteristics of its lava. Ngebel Volcano, located in East Java, is a Quaternary andesitic stratovolcano. This volcano is part of the Wilis Volcanic Complex. The volcanism stage of Ngebel Volcanic Complex can be divided into the Jeding with andesitic basalt (SiO2 49 - 59%), pyroxene andesite Kemlandingan (SiO2 49 - 59%), Manyutan with hornblende andesite (SiO2 49 - 59%), and Ngebel with dacite (SiO2: 49 - 59%). The variation of major elements combined with petrographic features such as plagioclase, pyroxene, hornblende, quartz, and opaque minerals from basaltic andesite to dacite is interesting. The minerals show that the magma differentiation process of Ngebel Volcanic Complex is the results of fractional crystallization of magma. The purpose of this study is to determine the evolution of magma from volcanic rocks of which stratigraphic positions have been determined. The analytical methodology used is petrographic and geochemical analysis. Detailed temporal evolution shows that magma from the Ngebel Volcanic Complex underwent a differentiation process that changed the magma composition from mafic to more felsic.

STUDI DEFORMASI PERMUKAAN PUNCAK GUNUNG MERAPI PADA TAHUN 1993 – 1995, DI PERBATASAN PROVINSI DAERAH ISTIMEWA YOGYAKARTA DAN JAWA TENGAH Gary Artha Widyananda; Dwi Fitri Yudiantoro; Intan Paramita Haty; Nurnaning Aisyah
Jurnal Ilmiah Geologi PANGEA Vol 9, No 2 (2022): Jurnal Ilmiah Geologi PANGEA
Publisher : PROGRAM STUDI TEKNIK GEOLOGI FAKULTAS TEKNOLOGI MINERAL UPN "VETERAN" YOGYAKARTA

Show Abstract | Download Original | Original Source | Check in Google Scholar

Secara geografis, lokasi penelitian terletak pada koordinat X1: 438120mE; Y1: 9167090mN; X2: 439750mE; Y2: 9167090mN; X3: 439750mE; Y3: 9165680mN; dan X4: 438120mE; Y4: 9165680mN. Penelitian menggunakan data sekunder, data deformasi telah diperoleh melalui pengukuran GPS pada periode 1993-1995(Beauducel, 1998) berupa koordinat dan vektor perpindahan titik GPS puncak pada periode 1993-1995, data tersebut menunjukkan pola deformasi yang tidak simetris. Bersumber pada penelitian oleh Aisyah dkk (2018), menerangkan deformasi tidak simetris tahun 2006 dan 2010 yakni dengan penggunaan metode kombinasi block movement serta inflasi sumber tekanan, maka pada periode 1994-1995 dapat dijelaskan menggunakan metode yang sama, sementara itu pada periode 1993-1994 hanya diterapkan inflasi sumber tekanan. Geomorfologi yang terdapat di puncak Gunung Merapi adalah bentuk asal vulkanik, dengan bentuk lahan berupa lereng aliran lava (V1), lereng endapan aliran piroklastik (V2), kawah (V3) serta kubah lava (V4). Pola pengaliran yang berkembang yakni radial sentrifugal. Diskontinuitas struktural pada puncak Gunung Merapi berupa rekahan dan batas antara bekas aliran lava. Vulkanostratigrafi (sumber erupsi) pada puncak Gunung Merapi dapat dibagi menjadi Merapi Tua (Satuan Aliran Lava Andesit Piroksen Merapi 2) dan Merapi Muda (Satuan Aliran Lava Andesit Piroksen Merapi 3, Satuan Endapan Aliran Piroklastik Muda dan Guguran Merapi, serta Satuan Aliran Lava Andesit Piroksen Merapi 4). Terdapat dua blok yang bergerak secara signifikan, masing-masing diperkirakan bergerak ke arah barat laut dan selatan-barat daya. Perkiraan lokasi sumber tekanan pada periode 1993-1994 yakni 600 m di bawah puncak Gunung Merapi, sementara itu pada periode 1994-1995 sekitar 740 m dibawah puncak. Pada periode 1993-1994 diestimasikan total nilai perubahan volume injeksi magma yakni sebesar 80.8 x, sedangkan periode 1994-1995 total perubahan volume injeksi magma diperkirakan sebesar 90.8 x. Pergerakan blok ke arah barat laut dan selatan-barat daya disebabkan perubahan volume serta tekanan pada sumber, yang dikontrol oleh diskontinuitas struktural di sekitar puncak berupa rekahan maupun batas antara bekas aliran lava, di bagian barat laut berupa batas antara aliran lava 1957 dan 1888, selanjutnya di bagian selatan yakni batas antara lava 1911-1913 dan lava 1888-1909.

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31315/jigp.v9i2.9503

Secara geografis, lokasi penelitian terletak pada koordinat X1: 438120mE; Y1: 9167090mN; X2: 439750mE; Y2: 9167090mN; X3: 439750mE; Y3: 9165680mN; dan X4: 438120mE; Y4: 9165680mN. Penelitian menggunakan data sekunder, data deformasi telah diperoleh melalui pengukuran GPS pada periode 1993-1995(Beauducel, 1998) berupa koordinat dan vektor perpindahan titik GPS puncak pada periode 1993-1995, data tersebut menunjukkan pola deformasi yang tidak simetris. Bersumber pada penelitian oleh Aisyah dan kawankawan (2018),menerangkan deformasi tidak simetris tahun 2006 dan 2010 yakni dengan penggunaan metode kombinasi block movement serta inflasi sumber tekanan, maka pada periode 1994-1995 dapat dijelaskan menggunakan metode yang sama, sementara itu pada periode 1993-1994 hanya diterapkan inflasi sumber tekanan. Geomorfologi yang terdapat di puncak Gunung Merapi adalah bentuk asal vulkanik, dengan bentuk lahan berupa lereng aliran lava (V1), lereng endapan aliran piroklastik (V2), kawah (V3) serta kubah lava (V4). Pola pengaliran yang berkembang yakni radial sentrifugal. Diskontinuitas struktural pada puncak Gunung Merapi berupa rekahan dan batas antara bekas aliran lava. Vulkanostratigrafi (sumber erupsi) pada puncak Gunung Merapi dapat dibagi menjadi Merapi Tua (Satuan Aliran Lava Andesit Piroksen Merapi 2) dan Merapi Muda (Satuan Aliran Lava Andesit Piroksen Merapi 3, Satuan Endapan Aliran Piroklastik Muda dan Guguran Merapi, serta Satuan Aliran Lava Andesit Piroksen Merapi 4). Terdapat dua blok yang bergerak secara signifikan, masing-masing diperkirakan bergerak ke arah barat laut dan selatan-barat daya. Perkiraan lokasi sumber tekanan pada periode 1993-1994 yakni 600 m di bawah puncak Gunung Merapi, sementara itu pada periode 1994-1995 sekitar 740 m dibawah puncak. Pada periode 1993-1994 diestimasikan total nilai perubahan volume injeksi magma yakni sebesar 80.8 x, sedangkan periode 1994-1995 total perubahan volume injeksi magma diperkirakan sebesar 90.8 x. Pergerakan blok ke arah barat laut dan selatan-barat daya disebabkan perubahan volume serta tekanan pada sumber, yang dikontrol oleh diskontinuitas struktural di sekitar puncak berupa rekahan maupun batas antara bekas aliran lava, di bagian barat laut berupa batas antara aliran lava 1957 dan 1888, selanjutnya di bagian selatan yakni batas antara lava 1911-1913 dan lava 1888-1909.Kata kunci: Gunung Merapi, Deformasi, GPS, Block movement, Sumber Tekanan.

Studi Hidrogeokimia Air Tanah di Daerah Kebumen Bagian Barat, Indonesia Setia Pambudi; Budi Sulistijo; Dwi Fitri Yudiantoro; Intan Paramita Haty
Jurnal Ilmiah Geologi PANGEA Vol 9, No 1sp (2022): Jurnal Ilmiah Geologi PANGEA Edisi Spesial
Publisher : PROGRAM STUDI TEKNIK GEOLOGI FAKULTAS TEKNOLOGI MINERAL UPN VETERAN YOGYAKARTA

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.31315/jigp.v9i1sp.9411

Abstrak - Studi penilaian hidrogeokimia air tanah telah dilakukan di Kebumen bagian barat yang dicirikan dengan fitur karstnya berdasarkan parameter fisikokimia (pH, konduktivitas elektrik, zat padat terlarut, kesadahan, Ca2+, Mg2+, Fe3+, Mn2+, K+, Na+, Li+, and NH4+, HCO3-, Cl-, SO42-, NO2-, and NO3-). Data sampel air diambil dari 25 sumber air tanah dangkal berupa mata air, goa basah dan sumur. Data fisikokimianya mengindikasikan hanya ada kontaminasi alami maupun dari manusia yang sangat rendah. Dari diagram Piper ditunjukkan bahwa fasies air tanah yang berada di daerah ini adalah kalsium-magnesium bikarbonat yang mengindikasikan efek litologi karbonatan yang sangat kuat ke air tanah. Diagram Durov menunjukkan bahwa air tanah di daerah studi hanya mengalami pertukaran ion yang sangat rendah yang mengindikasikan kemurnian air tanah ini dari dampak kontaminasi alami maupun dampak antropogenik.Kata kunci: hidrogeokimia, air tanah, karst, Kebumen Abstract - A groundwater hydrogeochemistry assessment study has been conducted in western Kebumen, characterized by its karstic features based on physicochemical parameters (pH, electric conductivity, total dissolved solids, hardness, Ca2+, Mg2+, Fe3+, Mn2+, K+, Na+, Li+, and NH4+, HCO3-, Cl-, SO42-, NO2-, and NO3-). Water samples were taken from 25 shallow groundwater sources such as springs, wet caves, and wells. The physicochemical data indicates very low natural and/or human contamination. The Piper diagram shows that the groundwater facies in this area is calcium-magnesium bicarbonate, indicating a very strong effect of carbonate lithology on groundwater. The Durov diagram shows that the groundwater in the study area only undergoes very low ion exchange, indicating the purity of this groundwater from natural contamination or anthropogenic impacts.Keywords: hydrogeochemistry, groundwater, karst, Kebumen

Co-Authors Abdurrachman - Mirzam Afrilita Ahmad Bagus Dianputra Aji, Krishna Amalia Suciati Andy Wijaya Anjarwati, Retno Arifudin Idrus Arifudin Idrus Armala Putri Arum Suproborini Arum Suproborini Asfahani M. G. Bambang Prastistho Bambang Pratisho Basuki , BASUKI RAHMAD Brany Kurnianto Budi Sulistijo Budi Sulistijo Budiman, Subhan Arif C Prasetyadi C. Prasetyadi Choiriah, Siti Umiyatun Darban - Haryanto Darban Haryanto Demi Ganjar Sampurno Dewi Sri Sayudi Dewi Sri Sayudi Dian Fiantis Dyah Rini Ratnaningsih Dyah Rini Ratnaningsih Ekasara, Adam Raka Elisabet Magdalena Gary Artha Widyananda Handoko Teguh Wibowo Handoko Teguh Wibowo I. Takashima Ikhsan, Ismail Da'imul Intan Paramita Haty Intan Paramita Haty Intan Paramita Haty Intan Paramita Haty Intan Paramita Haty Irwan Irwan Isao Takashima Isao Takashima Kapid, Rubiyanto Kusumayudha, Sari Bahagiarti Ladesta, Aldis M. Abdurrachman Mahreni Mahreni Mirzam Abdurrachman Mirzam Abdurrachman Mirzam Abdurrachman Mochamad Soeprijadi Djoko Laksana Mochamad Soeprijadi Djoko Laksana, Mochamad Soeprijadi Djoko Mohammad Apriniyadi Mohammad Nurcholis, Mohammad Muchamad Ocky Bayu Nugroho Muhammad Nurcholis Muhammad Nurcholis Muhammad Syaifudin Muhammad Syaifudin Nurnaning Aisyah Nurnaning Aisyah Prasetyadi, C Prasetyadi, Carolus Prasetyawati Umar, Emi Prastistho, Bambang Pratomo, Septyo Uji Puji Pratiknyo Purwanto Purwanto Radityo Prakoso Raharjati, Ni'matul Azizah Ramonada Taruna Perwira Retno Anjarwati Retno Anjarwati Richzkey Muhammad Rubiyanto Kapid Rubiyanto Kapid Rubiyanto Kapid Setia Pambudi Setiawati, Tri Candra Setyorini, Dyah Ayu Soesilo, Joko Sri Aminah Suwartikaningsih Suherman Dwi Nuryana Sunarto Sunarto Suproborini, Arum - Susila Herlambang Sutarto Sutarto Sutarto Sutarto Sutarto Sutarto Suwartikaningsih, Sri Aminah Temmy Wikaningrum Wibowo, Handoko Teguh Wiryanto Wiryanto Wisnu Ismunandar Yatini Yoni, Dian Rahma Yuda, Himes Fitra

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