Sürdürülebilir Kalkınma Amaçları
Yazarlar
- Gul, Muhammet(85)
- Serdar, Osman(72)
- Güler, Ömer(68)
- Akkurt, Nevzat(61)
- Baskonus, Haci Mehmet(54)
- Alataş, Mevlüt(53)
- Paksoy, Mehmet Yavuz(53)
- Yucesan, Melih(53)
- Bulut, Hasan(51)
- Tekin, H.O.(51)
- ALMisned, Ghada(48)
- Yildirim, Numan(48)
- Benzer, Fulya(47)
- Kocabaş, Mehmet(45)
- Yildirim, Nuran Cikcikoglu(44)
- Kutlu, Banu(41)
- Ince, Muharrem(39)
- Zengin, Gokhan(39)
- Batan, Nevzat(37)
- Utku, Anıl(35)
- Celik, Erkan(33)
- Topal, Murat(32)
- Ezer, Tülay(31)
- Tanyol, Mehtap(31)
- Can, Erkan(30)
- Sulaiman, Tukur Abdulkadir(29)
- Aslan, Naim(28)
- Özkul, İskender(28)
- Aslan, Alper(27)
- Cakilcioglu, Ugur(27)
- Erguven, Gokhan Onder(27)
- Kutluyer, Filiz(27)
- Kök, Mediha(27)
- Ates, Mehmet(26)
- Erten, Fusun(26)
- Kahraman, Gökhan(26)
- Onat, Onur(26)
- Dal, Nursel Alp(25)
- Danabas, Durali(25)
- Say, Yakup(25)
Yayınlar
- MakaleAçık Erişim2010Scopus SJRQ1A new algorithm for automatic classification of power quality events based on wavelet transform and SVM
Eristi, Hueseyin; Demir, Yakup
This paper presents a new approach for automatic classification of power quality events, which is based on the wavelet transform and support vector machines. In the proposed approach, an effective single feature vector representing three phase event signals is extracted after signals are applied normalization and segmentation process. The kernel and penalty parameters of the support vector machine (SVM) are determined by cross-validation. The parameter set that gives the smallest misclassification error is retained. ATP/EMTP model for six types of power system events, namely phase-to-ground fault, phase-to-phase fault, three-phase fault, load switching, capacitor switching and transformer energizing, are constructed. Both the noisy and noiseless event signals are applied to the proposed algorithm. Obtained results indicate that the proposed automatic event classification algorithm is robust and has ability to distinguish different power quality event classes easily. (C) 2009 Elsevier Ltd. All rights reserved.
AtıfWoS78OpenAlex106
İncele - MakaleYalnız künye2009Scopus SJRQ1²⁰⁷Pb- ²⁰⁶Pb, ⁴⁰Ar- ³⁹Ar and fission-track geothermochronology quantifying cooling and exhumation history of the Kaman- Kırşehir region intrusions, Central Anatolia, Turkey
Otlu, Nazmi; Güney, Özlem; Heizler, Matt; Jonckheere, Raymond C.; Tichomirowa, Marion; Boztuğ, Durmuş
Kaman-Kırşehir yöresi granitik intrüzyonları, Torid-Anatolid platformu (TAP) ve yitim zonu üzerinde gelişen Orta Anadolu Ofiyolitini (OAO) içeren okyanusal ada yayı arasında Senomaniyen–Türoniyen’de gerçekleşen kıta-okyanusal ada yayı çarpışması sonrası gerilme rejiminde oluşmuşlardır. Bu granitoyidler, kuzeyden güneye doğru, Çamsarı kuvars siyeniti, Hamit kuvars siyeniti, Bayındır nefelin-kankrinit siyeniti, Durmuşlu nefelin-nozeyan-melanit siyenit porfiri ve Baranadağ kuvars monzoniti birimlerinden oluşur. Bu intrüzif kayaçlar, Orta Anadolu Kristalin Karmaşığına (OAKK) ait metamorfik kayaçlarla OAO’ne ait birimleri sıcak dokanakla keser ve Geç Paleosen–Erken/Orta Eosen yaşlı sedimanter birimler tarafından uyumsuz olarak örtülürler. Çamsarı kuvars siyenitinin tek zirkon ²⁰⁷Pb- ²⁰⁶Pb buharlaşma yaşı 95.7±5.1 My olarak bulunmuştur; Hamit ve Baranadağ birimlerinin yaşları ise birbirlerinden ayırt edilemeyecek derecede yakın olup, ağırlıklı ortalama yaşları 74.3±4.5 My olarak belirlenmiştir. Benzer şekilde, Hamit ve Baranadağ birimlerinin amfibol ⁴⁰Ar- ³⁹Ar yaşları da birbirlerinden ayırt edilemeyecek derecede yakındır ve ağırlıklı ortalama yaş 72.7±0.1 My olarak belirlenmiştir. Çamsarı, Hamit, Baranadağ ve Durmuşlu birimlerinin apatit fizyon izi yaş verilerinin (deniz düzeyinden) yüksekliğe göre değişimleri incelendiğinde, ~57 ve ~61 My aralığında oldukça hızlı bir yükselme hızıyla (> 1 km/My) yüzeylendikleri belirlenmiştir. Böyle bir yüzeylenme tarihçesi, aynı zamanda, fizyon izi uzunluk ölçümlerine dayalı zaman-sıcaklık modelleme çalışmalarıyla da desteklenmiştir. Apatit fizyon izi jeotermokronolojisi verileriyle belirlenen Erken–Orta Paleosen yaşlı bu hızlı yüzeylenmenin, İzmir-Ankara-Erzincan (İAE) okyanusunun kapanmasını takiben TAP ve Avrasya Levhası (AL) arasında gelişen kıta-kıta çarpışmasına bağlı sıkışma rejimiyle meydana geldiği ve hatta bu sırada Orta Anadolu önülke basenlerinin de (OAÖB) açıldığı ileri sürülmektedir.
AtıfTR Dizin11
İncele - MakaleYalnız künye2009Scopus SJRQ1²⁰⁷Pb- ²⁰⁶Pb, ⁴⁰Ar- ³⁹Ar and apatite fission-track geothermochronology revealing the emplacement, cooling and exhumation history of the karaçayır syenite (N Sivas), East-Central Anatolia, Turkey
Heizler, Matt; Jonckheere, Raymond C.; Tichomirowa, Marion; Türksever, Esra; Boztuğ, Durmuş
Sivas (İç-Doğu Anadolu) yöresinde Paleozoyik yaşlı kabuksal metasedimanter kayaçları sıcak dokanakla kesen ve Geç Paleosen– Eosen yaşlı Tokuş formasyonuyla uyumsuz olarak örtülen Karaçayır siyeniti tek zirkon ²⁰⁷Pb- ²⁰⁶Pb buharlaşma, biyotit ⁴⁰Ar- ³⁹Ar ve apatit fizyon izi jeotermokronolojisi yöntemleriyle incelenmiştir. Tek zirkon ²⁰⁷Pb- ²⁰⁶Pb buharlaşma yaş tayini çalışmaları sonucunda Karaçayır siyenitinin intrüzyon yaşı 99.0±11.0 My (Senomaniyen–Turoniyen) olarak belirlenmiştir. Biyotit ⁴⁰Ar- ³⁹Ar yaş tayini çalışmaları ~65 My civarında bir soğuma yaşı vermiştir. Apatit fizyon izi yaş tayini ve iz uzunluk ölçüm çalışmalarına dayalı sıcaklıkzaman (T-t) modelleme verileri, Karaçayır siyenitinin 58 ile 61 My aralığında (Orta Paleosen) yıllık 1 mm’den daha hızlı olan tektonik yükselme ile yüzeylendiğini ortaya koymuştur. Orta Paleosen yaşlı bu tektonik yükselmenin, Avrasya levhasının (AL) altına ve kuzeye doğru dalmakta olan İzmir-Ankara-Erzincan (İAE) okyanusunun kapanması sonucu, İAE kenet kuşağı boyunca meydana gelen ve AL ile Torid-Anatolid platformunun (TAP) kenetlenmesini sağlayan kıta-kıta çarpışması ile meydana gelen sıkışma rejiminden kaynaklandığı ileri sürülmektedir. Bu sıkışma rejimi, aynı zamanda, Orta Anadolu önülke havzalarının gelişimini de sağlamıştır.
AtıfTR Dizin7İncele - MakaleYalnız künye2009Scopus SJRQ3Synthesis of New Polymeric Resin and Its Application in Solid Phase Extraction of Copper in Water Samples Using STAT-FAAS
Timur, Irfan; Senkal, B. Filiz; Kaplan, Olcay; Kaya, Gokce; Ozcan, Cemile; Karaaslan, Nagihan M.; Yaman, Mehmet
- MakaleYalnız künye2009Scopus SJRQ4The Effects of Commercial Diet Supplemented with Mannanoligosaccharide (MOS) and Vitamin B12 on the Growth and Body Composition of the Carp (Cyprinus carpio L. 1758)
Atar, Hasan Huseyin; Ates, Mehmet
Four hundred carp fries (Cyprinus carpio L. 1758) with average initial weight of 1.1 +/- 0.05 g and total average length of 4.04 +/- 0.04 cm, was fed for a period of 90 days with the addition of commercial feed Mannanoligosaccharide (MOS) and vitamin B-12. The carps were divided into four different groups and fed through different feeds (Control; group A with MOS, group B with vitamin B-12, group C with a the combination of MOS + vitamin B-12). The effects of feeding through MOS and vitamin B-12 in different proportions on the parameters such as growth in view of live weight and total length, survival rate, feed conversion, condition factor and protein efficacy for the carp fries was studied. The best growth in view of live weight was maintained through MOS and vitamin B-12 combination in group C (4.51 +/- 0.13 g), while the best growth in terms of length was obtained through MOS in group A (6.68 +/- 0.08 cm). As a consequence, the growth parameters of the carp fries fed through commercial feeds with the addition of MOS and vitamin B-12 in different doses under empirical conditions shown affirmative effects on the survival rate, feed assessment, condition factor and protein efficacy.
AtıfWoS5İncele - MakaleAçık Erişim2009Scopus SJRQ2Acrylamide concentrations in grilled foodstuffs of Turkish kitchen by high performance liquid chromatography-mass spectrometry
Kaplan, Olcay; Kaya, Gokce; Ozcan, Cemile; Ince, Muharrem; Yaman, Mehmet
For over ten years, there has been a considerable interest in determination of acrylamide in foodstuffs. It was known that both protein-rich and carbohydrates-rich foods cooked at high-temperatures can cause acrylamide formation. However, carbohydrates-rich foods such as potato chips and biscuit samples have been the common studied foods compared with protein-rich foods such as meat samples. In this study, determination of acrylamide in these two group foods was examined using HPLC-MS. For this purpose, firstly, the parameters that are thought to affect the response in the HPLC-MS analysis were optimized. The optimized conditions were found to be 0.3 ml min(-1) for flow rate of mobile phase, 40 mu l for injection volume, 5 degrees C for column temperature and 70 V for fragmentor potential. The optimized method was applied for the determination of acrylamide levels in Turkish foodstuffs including grilled meat and chicken samples, potato chips, coffee and biscuit. The obtained concentrations for all studied foods were in the range of 20-250 mu g kg(-1). The results showed that acrylamide concentrations highly varied depending on the kind of food samples. (C) 2009 Elsevier B.V. All rights reserved.
AtıfWoS36OpenAlex45İncele - MakaleYayıncıda açık erişim2009Scopus SJRQ1207Pb-206Pb, 40Ar-39Ar and Fission-Track Geothermochronology Quantifying Cooling and Exhumation History of the Kaman-Kirsehir Region Intrusions, Central Anatolia, Turkey
Boztug, Durmus; Güney, Ozlem; Heizler, Matt; Jonckheere, Raymond C.; Tichomirowa, Marion; Otlu, Nazmi
The Kaman-Kirsehir region intrusions were generated in a post-collisional extensional setting following Cenomanian-Turonian docking of an oceanic island arc, comprising the supra-subduction zone (SSZ) Central Anatolian ophiolite (CAO), onto the Tauride-Anatolide Platform (TAP). These granitoids have been named, from N to S, the Camsari quartz syenite, Hamit quartz syenite, Bayindir nepheline-cancrinite syenite, Durmuslu nepheline-nosean-melanite syenite porphyry and Baranadag quartz monzonite. They intrude the crustal metasediments of the Central Anatolian Crystalline Complex (CACC) and CAO and are unconformably overlain by Upper Paleocene to Lower-Middle Eocene sediments. The single-zircon Pb-207-Pb-206 evaporation age of the Camsari unit is 95.7 +/- 5.1 Ma; those of the Hamit and Baranadag units are indistinguishable with a weighted mean of 74.3 +/- 4.5 Ma. The amphibole 40Ar-39Ar ages of the Hamit and Baranadag units are almost identical with a weighted mean of 72.7 +/- 0.1 Ma. The apatite fission-track age vs elevation plot for the Camsari, Hamit, Durmuslu and Baranadag samples reveals rapid exhumation (>1 km/Ma) between similar to 57 and similar to 61 Ma, consistent with the results of track-length modelling. This Early-Middle Paleocene rapid exhumation is thought to result from uplift triggered by continent (TAP) - continent (Eurasian plate; EP) collision following the closure of Izmir-Ankara-Erzincan (IAE) ocean that also initiated the formation of peripheral foreland basins in central Anatolia. The Kaman-Kirsehir region intrusions were generated in a post-collisional extensional setting following Cenomanian-Turonian docking of an oceanic island arc, comprising the supra-subduction zone (SSZ) Central Anatolian ophiolite (CAO), onto the Tauride-Anatolide Platform (TAP). These granitoids have been named, from N to S, the Camsari quartz syenite, Hamit quartz syenite, Bayindir nepheline-cancrinite syenite, Durmuslu nepheline-nosean-melanite syenite porphyry and Baranadag quartz monzonite. They intrude the crustal metasediments of the Central Anatolian Crystalline Complex (CACC) and CAO and are unconformably overlain by Upper Paleocene to Lower-Middle Eocene sediments. The single-zircon Pb-207-Pb-206 evaporation age of the Camsari unit is 95.7 +/- 5.1 Ma; those of the Hamit and Baranadag units are indistinguishable with a weighted mean of 74.3 +/- 4.5 Ma. The amphibole 40Ar-39Ar ages of the Hamit and Baranadag units are almost identical with a weighted mean of 72.7 +/- 0.1 Ma. The apatite fission-track age vs elevation plot for the Camsari, Hamit, Durmuslu and Baranadag samples reveals rapid exhumation (>1 km/Ma) between similar to 57 and similar to 61 Ma, consistent with the results of track-length modelling. This Early-Middle Paleocene rapid exhumation is thought to result from uplift triggered by continent (TAP) - continent (Eurasian plate; EP) collision following the closure of Izmir-Ankara-Erzincan (IAE) ocean that also initiated the formation of peripheral foreland basins in central Anatolia.
AtıfWoS23İncele - MakaleYayıncıda açık erişim2009Scopus SJRQ1207Pb-206Pb, 40Ar-39Ar and Apatite Fission-Track Geothermochronology Revealing the Emplacement, Cooling and Exhumation History of the Karacayir Syenite (N Sivas), East-Central Anatolia, Turkey
Boztug, Durmus; Türksever, Esra; Heizler, Matt; Jonckheere, Raymond C.; Tichomirowa, Marion
The Karacayir syenite, intruding the Palaeozoic crustal metamorphics and unconformably overlain by Upper Paleocene to Eocene Tokus formation in the north of Sivas (east-central Anatolia), has been studied with respect to Pb-207-Pb-206 single zircon evaporation, biotite 40Ar-39Ar, and apatite fission-track geothermochronology. Pb-207-Pb-206 single zircon evaporation dating yields an age of 99.0 +/- 11.0 Ma (Cenomanian-Turonian) which is considered to be the intrusion age. Biotite 40Ar-39Ar age determination gives a cooling age of ca. 65 Ma. Apatite fission-track dating, combined with T-t modeling based on track-length distribution data, determines a fast tectonic exhumation with an uplift rate of > 1 mm/a which occurred 58-61 Ma ago. This Middle Paleocene fast tectonic uplift is considered to have resulted from a compressional regime induced by the collision between the Tauride-Anatolide platform (TAP) and the Eurasian plate (EP) along the Izmir-Ankara-Erzincan (IAE) suture zone following the closure of the north-dipping subducted IAE ocean which belongs to northern Neo-Tethyan realm. This compressional regime has also formed the peripheral foreland basins in central Anatolia.
AtıfWoS14İncele - MakaleAçık Erişim2009Scopus SJRQ1Heat transfer augmentation by swirl generators inserted into a tube with constant heat flux
Kurtbas, Irfan; Guelcimen, Fevzi; Akbulut, Abdullah; Buran, Dincer
A novel conical injector type swirl generator (CITSG) is devised in this study. Performances of heat transfer and pressure drop in a pipe with the CITSG are experimentally examined for the CITSGs' angle (alpha) of 30 degrees, 45 degrees and 60 degrees in Reynolds number (Re) range of 10,000-35,000. Moreover, circular holes with different numbers (N) and cross-section areas (A(h)) are drilled on the CITSG. In this way, total areas (A(t) = N . A(h)) of the holes on the CITSG are equaled each other. Besides, flow directors having three different angles (beta = 30 degrees, 60 degrees and 90 degrees) to radial direction are attached to every one of the holes. This study is a typical example for decaying flow. All experiments were conduced with air accordingly; Prandtl number was approximately fixed at 0.71. The local Nusselt number (Nu(x)), heat transfer enhancement ratio (Nu(ER)) and heat transfer performance ratio (Nu(PR)) are calculated and discussed in this paper. It is found that the Nu(ER) decreases with increase in Reynolds number, the director angle (beta), the director diameter (d), and with decrease in the CITSG angle (alpha). Likewise, variation of Nu(PR) and Nu(ER) is also essentially similar for the same independent parameters. (C) 2009 Elsevier Ltd. All rights reserved.
AtıfWoS32OpenAlex31İncele