bluuebunny/crossref_metadata_2025_split huggingface dataset:
Yazın ve İhanet: Hans Joachim Schädlich'in Die Sache mit B. Yapıtında İhanet İzleğinin Aile Belleği Bağlamında İncelenmesi
Authors: AYDIN Yıldız 
Published: October 2018

1989 ve 1992 yılları Almanya tarihi bakımından en
önemli dönüm noktalarından biri olarak kabul edilmektedir. 1989 yılında bir
yandan Berlin Duvarı’nın yıkılmasıyla Doğu ile Batı arasındaki sınır ortadan
kalkar, diğer yandan 1990 yılında yaklaşık kırk yıl varlığını sürdüren
Demokratik Almanya Cumhuriyeti Federal Almanya’ya katılarak resmen yıkılır. Ne
var ki bu hızlı dönüşüm siyasal, ekinsel ve toplumsal açıdan oldukça sancılı
gerçekleşmiştir. Sözgelimi Alman toplumunun belleğine yer eden önemli olaylar
arasında Milli İstihbarat Teşkilatı’nın Doğu Almanyalı yurttaşlar tarafından
yağmalanması ve arşivlerde bulunan dosyaların bir kısmının tahrip edilmesi
sayılabilir. 1992 yılında bu kurumun arşivlerinin kamuoyuna açık tutulması ise
tartışmaları yeniden alevlendirmiştir, çünkü bazı dosyalar gizlice basın yayına
sızdırılmış ve kimi önemli sanatçıların ve yazarların casusluk yaptığı ortaya
çıkmıştır. 1977 yılında DAC’deki baskılara fazla dayanamayarak Federal
Almanya’ya göç eden yazar Hans Joachim Schädlich ilk defa o tarihte ağabeyinin
bu kuruma kendisi hakkında bilgiler verdiğini öğrenir ve büyük düş kırıklığı
yaşar. Birkaç ay sonrasında yayımladığı Die
Sache mit B. adlı kısa öyküsünde yüzleştiği bu ihanetle hesaplaşan yazar,
geri sapım tekniği ile çocukluğundan bu yazıyı kaleme aldığı ana kadar
ağabeyinin aile içindeki rolünü ve ağabey kardeş ilişkilerini çarpıcı bir dille
aktarır. Son derece yoğun bir biçimde özyaşamöyküsel öğelere göndergeler
taşıyan bu öyküde gerçeklere ulaşma istenci içinde bocalayan anlatıcı,
belleğindeki aile anılarını aktararak bu ihaneti sorgulamaktadır. Ağabeyi
Karlheinz Schädlich ise bu utançla daha fazla yaşayamayacağını anladığından
olsa gerek 2007 yılında intihar eder. Bu çalışmada tarihsel, ekin siyasal ve
özyaşamsal kaynaklardan hareketle yazarın ihanet izleğine nasıl yaklaştığı
sorgulanacak, sonrasında ise Die Sache
mit B. öyküsü M. Halbwachs’ın aile belleği kuramı çerçevesinde ele
alınacaktır ve bu tür aile anılarının yansıtıldığı özyaşamsal veya yaşamöyküsel
öğelerin aktarıldığı yazınsal metinlerin yorumlanması veya daha iyi
anlaşılmasında ne tür katkı sağlayacağı ortaya konacaktır.&nbsp;
Casas de citas
Authors: Parra Bañón José Joaquín 
Published: October 2018

En estas Casas de citas, las casas son la arquitectura y las citas son la literatura: aquí se analizan y se reivindican las relaciones íntimas entre una y otra. La casa es el lugar y la cita es la palabra. Casas de citas es el lugar de la palabra: el espacio y el tiempo en el que la palabra tiene su lugar y en el que la palabra construye el lugar de los acontecimientos, de los pensamientos y de las sensaciones. Casas de citas también cobija las palabras del lugar: las formas, las luces, los orificios y las atmósferas que se expresan por sí mismas; las piedras que hablan enhebradas en las voces ajenas que nombran, que delimitan o narran cada ámbito. Porque también, como este volumen comparado pone en evidencia, la casa puede ser la literatura y la cita ser la arquitectura. Venecia es un caso ejemplar de lo uno y de lo otro: de la una carnalmente entreverada en la otra.
Biodiesel production using reactive distillation column: Real time model predictive control in Matlab Simulink
Authors: KARACAN Suleyman 
Published: October 2018

Biodiesel is a renewable fuel source that consist of alkyl esters obtained from vegetable oil and animal fats. Biodiesel is typically produced via transesterification, which is the reaction of vegetable oils with a short-chain alcohol to produce alkyl esters and glycerol by using an appropriate catalyst. Reactive distillation is integrated operations that conveniently combine reaction and separation into a single unit. It is an effective alternative to the traditional combination of reactor and separation units especially when involving in reversible reactions, such as vegetable oil transesterification, or consecutive chemical reactions. Biodiesel production process by reactive distillation is a high degree nonlinear structure and multi-input and multi-output system. Because of this state, reactive distillation systems should be controlled. In this study, reboiler heat duty used as a manipulated variable to control the temperature of the bottom product. Model Predictive Control (MPC) was carried out and control results was satisfactorily obtained.
FIELD CORRELATION BETWEEN PRECIPITATION-EL NINO RELATED VARIATION AND CORAL ?18O
Authors: Cahyarini Sri Yudawati , Suwargadi B. 
Published: October 2018

Coral ?18O from Maudulung-Indonesia was analyzed using Finnigan MAT 251. Using statistical analysis from KNMI database is obtained that the seasonal mean field correlation between coral ? 18OSOI shows strong correlation during October. Field correlation of precipitation-coral ? 18O shows opposite pattern between eastern Pacific and western Pacific during strong El Nino event. Keywords: coral ?18O, field correlation, El NiÃ±o, Maudulung Sumba. Kandungan ?18O dalam koral dari wilayah Maudulung, Sumba, dianalisis dengan menggunakan Finnigan MAT 251. Korelasi spasial antara ?18O dengan SOI dalam skala musiman tinggi selama bulan Oktober. Korelasi spasial ini dilakukan dengan menggunakan fasilitas analisa statistik dalam database KNMI. Korelasi spasial antara presipitasi- coral ?18O menunjukkan pola-pola yang berlawanan antara wilayah timur dan barat Pasifi selama El NiÃ±o. Kata kunci: Koral ?18O, korelasi spasial, El NiÃ±o, Maudulung Sumba.
REVIEW OF COASTAL CHARACTERISTICS OF IRON SAND DEPOSITS IN CILACAP CENTRAL JAVA
Authors: Kurnio Hananto 
Published: October 2018

Mineable iron sand deposits in Cilacap â€“ southern coastal area of Central Java have certain coastal characteristics that need to be studied in order to understand its depositional environment. With the knowledge of such environment, it can be applied to look for other places prospective of iron sand deposits that have the same characteristics especially recently when Cilacapâ€™s deposits were almost depleted. Coastal characteristics of iron sand deposit in Cilacap is shown by successive sandy beach ridges separated by marshy valleys typical of prograded coasts and by dunes of sand elongated parallel to the shore line with elevation varies from 0 m to 15 m above sea level. The iron sand deposit was derived from denudation of andesite and â€œOld Andesite Formationâ€ enriched in magnetite and ilmenite minerals in the steep elevated and deeply weathered rock hinterlands of Cilacap. High sediment loads of Serayu Basin in the hinterland (3,500-4,500 ton/km2/year; Citarum River basin only 800-1,200 ton/km2/year) was causing extensive deposition of iron sand in the coastal zone. Key words: coast, characteristic, iron sand, Cilacap Endapan pasir besi yang dapat ditambang di Cilacap â€“ pesisir selatan Jawa Tengah memiliki karakteristik pantai tertentu yang perlu dikaji agar dapat dipahami lingkungan pengendapannya. Dengan pengetahuan tentang lingkungan pengendapan tersebut, dapat diterapkan untuk mencari daerah-daerah lain prospek endapan pasir besi yang memiliki karakteristik yang sama terutama pada akhir-akhir ini ketika endapan Cilacap akan habis. Karakteristik pantai endapan pasir besi di Cilacap dicirikan oleh urutan pematang pantai berpasir yang dipisahkan oleh lembah-lembah berawa khas pantai maju dan oleh gumuk-gumuk pasir memanjang sejajar dengan garis pantai dengan ketinggian bervariasi dari 0 m hingga 15 m dari muka laut. Endapan pasir besi di daerah ini berasal dari proses denudasi andesit dan â€œFormasi Andesit Tuaâ€ yang kaya akan mineral magnetit dan ilmenit pada pedalaman Cilacap dengan kondisi elevasi curam dan batuan sangat terlapukkan. Muatan sedimen yang tinggi dari Cekungan Serayu di pedalaman tersebut (3.500-4.500 ton/km2/tahun; cekungan Sungai Citarum hanya 800-1.200 ton/km2/tahun) menyebabkan pengendapan yang sangat luas pasir besi di wilayah pantai. Kata kunci: pantai, karakteristik, pasir besi, Cilacap
SUBMARINE LANDSLIDE AND LOCALIZED TSUNAMI POTENTIALITY OF MENTAWAI BASIN, SUMATRA, INDONESIA
Authors: Permana Haryadi , Singh C. 
Published: October 2018

The new bathymetry and seismic data were acquired during the PreTI-Gap marine survey (February 15 to March 6, 2008). The survey was carried out along the NE margin of Mentawai Island using multi-beam swath bathymetry equipment, and 28-channels seismic streamer and four-airgun source. The first target was the Mega Island region near the epicenter of the 2007 great earthquake. The shallow bathymetry is characterized as a flat coral platform suggesting that 200 km elongated plateau is slowly subsiding without any active faults. Further north, from South Pagai to North of Siberut Islands, the seafloor morphology changes significantly. The deep and wide canyons or valleys produce very rough seafloor morphology between 50 and 1100 m water. In general, the submarine topography shows two break slopes at different depths. Between slope breaks, the undulating, hilly and circular features dominate, possibly caused by landslides. A push-up ridge is observed that dams the sediments eroded within a steep slope northeastward side. The seismic reflection data acquired along 14 dip seismic lines at the NE flank of Mentawai Islands, from Siberut to the South of Pagai Islands. We observed a set of southwestward dipping back thrust bounding the NE margin of the Mentawai Island. Keywords: submarine landslide, tsunami, Mentawai basin, Sumatra. Data batimetri dan seismik baru telah dihasilkan selama survey kelautan PreTi-Gap (15 Februari hingga 6 Maret 2008). Survei dilaksanakan sepanjang tepian timurlaut P. Mentawai menggunakan peralatan multibeam, seismic saluran ganda 28 kanal dengan sumber energi airgun. Sasaran pertama adalah memetakan kawasan pulau dekat pusat gempa tahun 2007. Kenampakan batimetri dangkal dicirikan dengan adanya dataran terumbu karang yang secara perlahan mengalami penurunan tanpa aktifitas sesar. Lebih jauh ke Utar, dari Pagai Selatan ke utara P. Siberut, morfologi dasar laut memperlihatkan perubahan secara signifikan, dimana lembah dasar laut memiliki lebar dan beda kedalaman antara 50 hingga 1100 meter. Secara umum, topografi dasar laut memperlihatkan dua kemiringan pada kedalaman yang berbeda dengan dicirikan adanya kenampakan perlipatan, perbukitan dan bentuk yang melingkar diperkirakan sebagai hasil gelinciran. Sebanyak 14 line data seismik refleksi pada sayap bagian timurlaut P. Mentawai, dari Siberut hingga ke selatan P. Pagai memperlihatkan adanya bukti sesar naik yang miring ke arah baratdaya yang masih satu set dengan tepian timurlaut P. Mentawai. Kata kunci: longsoran bawah laut, tsunami, Cekungan Mentawai, Sumatra.
SUBSURFACE GEOLOGICAL CONDITION OF SEVERAL LAND COASTAL ZONE IN INDONESIA BASED ON THE GSSI GROUND PROBING RADAR (GPR) RECORD INTERPRETATION
Authors: Budiono Kris , Latuputty Godwin 
Published: October 2018

The GSSI Ground Penetrating radar have been used to profile the shallow depth of subsurface geology of several area of Land Coastal zone in Indonesia Analysis of a large data base of GPR profile from natural subsurface geological condition along the land coast line have allowed identification of reflection configuration that characterize this type of sub surface geological environment. In many contamination problem, the geological information of coastal area is sparse and drill-core description only gives a limited picture of the geometry of inhomogeneties. The Ground-Probing Radar (GPR) method is a promising tool for resolving changes of physical properties in subsurface geological condition at the scale of natural inhomogeneties arising from changing lithology composition. The objective of present work are to examine whether and to what extent the characteristic lithofacies of subsurface lithology can be recognised as mapable reflection pattern on ground probing radar (GPR) reflection profiles in order to gain information about the subsurface geometry of subsurface geology in coastal area. Key word: Subsurface geology, coastal zone, Ground Probing Radar Ground probing radar produksi GSSI telah dipergunakan untuk membuat penampang geologi bawah permukaan dangkal di beberapa kawasan pantai Indonesia. Analisa data dasar penampang GPR dari geologi bawah permukaan di kawasan pantai dapat memperlihatkan konfigurasi reflector yang mencerminkan jenis lingkungan geologi bawah permukaan. Dalam masalah kontaminasi, informasi geologi di daerah pantai yang dihasilkan dari pemboran inti hanya dapat memperlihatkan gambaran yang sederhana tentang geometri ketidakseragaman. Metoda ground probing radar merupakan alat bantu yang menjanjikan untuk menanggulangi masalah sifat fisik kondisi geologi bawah permukaan pada skala ketidak seragaman yang sebenarnya dari perubahan komposisi litologi. Tujuan utama dari penelitian ini adalah untuk menguji sampai sejauh mana karakteristik litofasies dari litologi bawah permukaan dapat dilihat sebagai pola refleksi yang dapat dipetakan dalam penampang GPR dengan maksud untuk mendapatkan informasi geometri geologi bawah permukaan di daerah pantai. Kata kunci: Geologi bawah permukaan, zona pantai, â€œGround probing radarâ€
STRUCTURAL GEOLOGICAL CONTROL ON THE MINERALIZATION ON TABUAN ISLAND,SEMANGKO BAY, SOUTH SUMATERA, INDONESIA
Authors: Kurnio Hananto , Schampera Ulrich Schwarz 
Published: October 2018

Mineralization have been discovered on Tabuan Island, Semangko Bay, South Sumatera, Indonesia. Tabuan Island belongs to the Neogene Sunda-Banda magmatic arc system. Tabuan Island is a tectonic horst structure which belongs to the subduction-related, magmatically active Barisan zone along the active continental margin of western Sumatera. Basaltic-andesitic volcanics of the late Oligocene to earliest Miocene Hulusimpang Formation are distributed in a broad zone along and subparallel to the regional Semangko Fault and are hosts for several epithermal-style auriferous deposits. The occurrence of hydrothermal mineralization was first suggested from seismic identification of small intrusive bodies which form elongated northwest-southeast ridges passing through the island. Surface sampling campaigns on the island revealed significant hydrothermal alteration and mineralization with pervasive occurrences of sulphide minerals. Detailed mineralogical and geochemical studies at the Federal Institute for Geoscience and Natural Resources show pronounced disseminations and vein-type mineralization. Mineralization shows moderate enrichments in Au, Ag, Zn, Pb, Cu, As, Sb, Ba, and Mn. The association of subaerial island arc volcanism and subvolcanic intrusive bodies, the regional extensional and strike-slip structural regime, and the occurrence of epithermal-style alteration and mineralization in the same volcanic sequence along the coastal zone of Semangko Bay and on Tabuan Island reveal the great potential of this region for epithermal type Au-Ag and base metal deposits. On Tabuan Island, delineation of structural blocks and fault systems suggests that normal faults and margins of grabens may have acted as fluid channelling structures. Key words: structural geology, mineralization, Tabuan Island, Semangko Bay
THE DEVELOPMENT OF PORONG ESTUARY
Authors: Hernawan Undang 
Published: October 2018

Coastal zone is an area of interaction between the land and the sea. Coastal dynamic is influenced by many factors, such as sedimentation and current. Development of an area in the coastal zone such as estuary is also influenced by suck factors. Development of porong estuary is analyzed by interpretation of Image data, i.e. Landsat TM data that acquired in July, 29th 1975, August, 17th 1994, August, 17th 2000, May, 19th 2002 and Quickbird imagery that acquired in April, 25th 2008. Field survey has been done on April 2008. Based on data interpretation, there are accretion and abrasion in this area. The accretion in the southern part of Porong estuary between 1975 â€“ 2008 is about 33.15 km or about 3.15 km/year equivalent to 1,492.29 Ha. The abrasion area in the northern part of Porong estuary in 33 years since 1975 till 2008 is around 0.5 km or aproximately 15.15 m/year equivalent to 222.45 Ha of wide or 6.802 Ha/year. Development of Porong delta, especially in the southern part of Porong estuary, is caused by change of pattern and main stream of Porong River from the noth to the south. This river delivered large volume of sediments and precipated at this area without or minor influence from the sea. Porong delta is a fluvial delta. Coastal characteristic is mangrove, muddy sediment and locally is sand sediment. Land use in this area is fish pond and mangrove. Key words: Porong estuary, Satellite imagery Pantai/pesisir merupakan wilayah antara daratan dan lautan yang masih dipengaruhi oleh keduanya. Dinamika pantai akan dipengaruhi oleh faktor-faktor dari daratan seperti sedimentasi dan faktor dari lautan seperti arus. Demikian halnya perkembangan suatu daerah di pesisir, seperti daerah muara, dipengaruhi oleh daratan dan lautan. Perkembangan muara Porong dianalisis berdasarkan interpretasi citra satelit, yaitu Landsat hasil perekaman 29 Juli 1975, 17 Agustus 1994, 17 Agustus 2004, 19 Mei 2002 dan citra Quickbird perekaman 25 April 2008. Survey lapangan dilaksanakan pada bulan April 2008. Berdasarkan interpretasi citra, ditemukan daerah akresi dan abrasi pada daerah penelitian. Daerah akresi ditemukan di bagian selatan daerah penelitian yaitu sekitar 33.15 km selama 1975â€“2008 atau sekitar 3.15 km/tahun dengan luasan sekitar 1,492.29 Ha. Daerah abrasi umumnya terdapat di muara Kali Porong sebelah utara, yaitu sejauh 0.5 km selama 33 tahun atau kira-kira 15.15 m/tahun dengan luasan 222.45 Ha atau sekitar 6.802 Ha/tahun. Perkembangan muara dan delta Porong, terutama di muara sebelah selatan, diperkirakan karena adanya perubahan arah utama Sungai Porong, yang berubah dari arah utara kea rah selatan. Aliran sungai ini membawa banyak sedimen dan diendapkan pada daerah ini, karena tiada atau kurangnya pengaruh dari laut. Delta Porong termasuk kawasan delta fluvial. Karakteristik daerah pantai umumnya berlumpur dengan setempat berupa pasir. Penggunaan lahan pada daerah ini umumnya berupa tambak dan mangrove. Kata Kunci : Delta Porong, citra Satelit
TYPES AND DISTRIBUTION OF CORAL REEF ON THE KARIMATA COAST, WEST KALIMANTAN
Authors: Aryanto Noor C.D. , Permanawati Yani 
Published: October 2018

The identification of quality and condition of the coral reef in the study areas will support the biological diversity and it frequently contains a valuable assortment of natural resources, conservation of marine biota. The environmental problem particularly on the coastal area needs a more comprehensive management due to the complexity of the rapidly growth. Karimata Archipelago geographically is located between 108o40' - 109o10' E and 1o25' - 1o50' S and administratively belongs to the Ketapang Regency (approximate 100 km west side of Ketapang). In the study area, the growth of coral reef is dominated by non-Acropora type arised between the depths 3-15m. The condition is somewhat good to good. Karimata Archipelago consist of two big islands they are Karimata Island (Studied area) and Serutu Island and also some other isles, with the topography from low land to high land having the height of about 1030 meters from sea level. Keywords: Coral reef, Karimata coast, West Kalimantan. Identifikasi kualitas dan kondisi terumbu karang di daerah penelitian dapat menopang keanekaragaman biologi yang pada akhirnya dapat berperan sebagai kawasan konservasi biota laut. Masalah kepekaan lingkungan khususnya di wilayah pantai dan pesisir memerlukan penanganan yang lebih komperhensif, karena kawasan ini relatif lebih kompleks selain perkembangannya yang demikian pesat. Gugusan kepulauan Karimata secara geografi menempati posisi 108o40' - 109o10' BT and 1o25' - 1o50' LS dan secara administrasi masuk dalam Kabupaten Ketapang (lebih-kurang berjarak 100 km ke arah barat dari Ketapang). Di lokasi telitian, keberadaan terumbu karangnya didominasi oleh jenis non-Acropora yang tumbuh baik pada kedalaman antara 3 hingga 15 m. Terumbu karang yang dijumpai dengan kondisi agak baik hingga baik. Kepulauan Karimata terdiri dari 2 pulau besar, P. Karimata di mana lokasi studi terletak dan P.Serutu dan beberapa pulau-pulau kecil dengan topografi dari dataran rendah hingga dataran tinggi (1030 m) di atas permukaan laut. Kata kunci:Terumbu karang, Pantai Karimata, Kalimantan Barat.
BIOGENIC GAS IN DELTAIC DEPOSITION ENVIRONMENT IN KAPUAS RIVER, WEST KALIMANTAN AND ITS UTILIZATIONS FOR LOCAL COMMUNITY
Authors: Kurnio Hananto , Darlan Yudi 
Published: October 2018

Biogenic gas within a deltaic deposition environment in the Kapuas rivermouth of West Kalimantan occurred in fine to very fine quartz sand reservoir of shallow boreholes of having the depth of 1-12 m below ground surface. This reservoir is covered by peaty layers of semi-impermeable property. During high tide, gas bubbling took place in the water column above the ground of these semi-impermeable layers. Utilizations of biogenic gas had been done succesfully. These works were carried out through drilling, piping, gas storage and installations for gas stove and gas electricity generator of 500 watt capacity at chief village house as an example before widely used to the local community. Keywords: Biogenic Gas; Deltaic Deposition Environment; Kapuas River; west Kalimantan, Utilization. Gas biogenik dalam suatu lingkungan pengendapan delta di muara Sungai Kapuas Kalimantan Barat terdapat dalam reservoar pasir kuarsa berukuran halus hingga sangat halus pada kedalaman bor dangkal 1-12 m di bawah permukaan tanah. Reservoar ini ditutupi oleh lapisan gambut semiimpermeabel. Selama pasang naik, gelembung gas teramati dalam kolom air di atas permukaan lapisan semi-impermeabel ini. Pemanfaatan gas biogenik telah dilaksanakan dengan sukses. Pemanfaatan ini dilakukan melalui pemboran, pipanisasi, penampungan gas dan instalasi untuk kompor gas dan generator listrik berbahan bakar gas kapasitas 500 watt di rumah Kepala Desa sebagai contoh sebelum dimanfaatkan secara luas oleh masyarakat setempat. Kata kunci: Gas Biogenik, Lingkungan Pengendapan Delta, Sungai Kapuas, Kalimantan Barat, Pemanfaatan