Estudo de cerâmicas avançadas para fins de blindagem balística

The research involving new materials has always been considered as a differential in the development of a technology company. This occurred naturally since ancient times, often motivated by reasons of a certain age, where the most common material used was also the name of your time and may be cited as an example the Bronze Age, and later was the Iron. Currently, the use of firearms are they used in resolving conflicts between countries, or a more equivocal, as an instrument of social banditry make innovations in the area of shielding welcome, whether for personal use, in the form of vests or vehicle such as cars, tanks and even aircraft. In this context, is a Silicon Carbide Ceramic, with low density and high hardness. Thus, the aim of this study is the evaluation and comparison of these materials, seeking to improve their properties by means of additives such as boron and silicon metal and amorphous YAG. For this work, the specimens were pre-shaped by means of uniaxial later to be referred for isostatic pressing and sintering. The maximum percentage for each additive was 5%, except for the YAG whose percentage was 8.2% (mass percentage). All compositions were subjected to the same tests (x-ray diffraction, apparent density, optical microscopy, Vickers hardness, scanning electron Microscopita), so that one could draw a comparison between the materials under study, samples that showed better mechanical properties and micro structural, related here by hardness testing and microscopy (optical and SEM) were the silicon carbide doped with YAG and alumina samples, demonstrating the potential of these materials for ballistic protection. Other compositions have high porosity, which is highly undesirable, since in order to harmful influences on the mechanical properties discussed below

High-resolution stratigraphy of Central and Southern Adriatic Quaternary deposits of sub-Milankovian climate change on Mediterranean circulation

This volume is a collection of the work done in a three years-lasting PhD, focused in the analysis of Central and Southern Adriatic marine sediments, deriving from the collection of a borehole and many cores, achieved thanks to the good seismic-stratigraphic knowledge of the study area. The work was made out within European projects EC-EURODELTA (coordinated by Fabio Trincardi, ISMAR-CNR), EC-EUROSTRATAFORM (coordinated by Phil P. E. Weaver, NOC, UK), and PROMESS1 (coordinated by Serge Bernè, IFREMER, France). The analysed sedimentary successions presented highly expanded stratigraphic intervals, particularly for the last 400 kyr, 60 kyr and 6 kyr BP. These three different time-intervals resulted in a tri-partition of the PhD thesis. The study consisted of the analysis of planktic and benthic foraminifers’ assemblages (more than 560 samples analysed), as well as in preparing the material for oxygen and carbon stable isotope analyses, and interpreting and discussing the obtained dataset. The chronologic framework of the last 400 kyr was achieved for borehole PRAD1-2 (within the work-package WP6 of PROMESS1 project), collected in 186.5 m water depth. The proposed chronology derives from a multi-disciplinary approach, consisting of the integration of numerous and independent proxies, some of which analysed by other specialists within the project. The final framework based on: micropaleontology (calcareous nannofossils and foraminifers’ bioevents), climatic cyclicity (foraminifers’ assemblages), geochemistry (oxygen stable isotope, made out on planktic and benthic records), paleomagnetism, radiometric ages (14C AMS), teprhochronology, identification of sapropel-equivalent levels (Se). It’s worth to note the good consistency between the oxygen stable isotope curve obtained for borehole PRAD1-2 and other deeper Mediterranean records. The studied proxies allowed the recognition of all the isotopic intervals from MIS10 to MIS1 in PRAD1-2 record, and the base of the borehole has been ascribed to the early MIS11. Glacial and interglacial intervals identified in the Central Adriatic record have been analysed in detail for the paleo-environmental reconstruction, as well. For instance, glacial stages MIS6, MIS8 and MIS10 present peculiar foraminifers’ assemblages, composed by benthic species typical of polar regions and no longer living in the Central Adriatic nowadays. Moreover, a deepening trend in the paleo-bathymetry during glacial intervals was observed, from MIS10 (inner-shelf environment) to MIS4 (mid-shelf environment).Ten sapropel-equivalent levels have been recognised in PRAD1-2 Central Adriatic record. They showed different planktic foraminifers’ assemblages, which allowed the first distinction of events occurred during warm-climate (Se5, Se7), cold-climate (Se4, Se6 and Se8) and temperate-intermediate-climate (Se1, Se3, Se9, Se’, Se10) conditions, consistently with literature. Cold-climate sapropel equivalents are characterised by the absence of an oligotrophic phase, whereas warm-temeprate-climate sapropel equivalents present both the oligotrophic and the eutrophic phases (except for Se1). Sea floor conditions vary, according to benthic foraminifers’ assemblages, from relatively well oxygenated (Se1, Se3), to dysoxic (Se9, Se’, Se10), to highly dysoxic (Se4, Se6, Se8) to events during which benthic foraminifers are absent (Se5, Se7). These two latter levels are also characterised by the lamination of the sediment, feature never observed in literature in such shallow records. The enhanced stratification of the water column during the events Se8, Se7, Se6, Se5, Se4, and the concurring strong dilution of shallow water, pointed out by the isotope record, lead to the hypothesis of a period of intense precipitation in the Central Adriatic region, possibly due to a northward shift of the African Monsoon. Finally, the expression of Central Adriatic PRAD1-2 Se5 equivalent was compared with the same event, as registered in other Eastern Mediterranean areas. The sequence of substantially the same planktic foraminifers’ bioevents has been consistently recognised, indicating a similar evolution of the water column all over the Eastern Mediterranean; yet, the synchronism of these events cannot be demonstrated. A high resolution analysis of late Holocene (last 6000 years BP) climate change was carried out for the Adriatic area, through the recognition of planktic and benthic foraminifers’ bioevents. In particular, peaks of planktic Globigerinoides sacculifer (four during the last 5500 years BP in the most expanded core) have been interpreted, based on the ecological requirements of this species, as warm-climate, arid intervals, correspondent to periods of relative climatic optimum, such as, for instance, the Medieval Warm Period, the Roman Age, the Late Bronze Age and the Copper Age. Consequently, the minima in the abundance of this biomarker could correspond to relatively cooler and more rainy periods. These conclusions are in good agreement with the isotopic and the pollen data. The Last Occurrence (LO) of G. sacculifer has been dated in this work at an average age of 550 years BP, and it is the best bioevent approximating the base of the Little Ice Age in the Adriatic. Recent literature reports the same bioevent in the Levantine Basin, showing a rather consistent age. Therefore, the LO of G. sacculifer has the potential to be extended to all the Eastern Mediterranean. Within the Little Ice Age, benthic foraminifer V. complanata shows two distinct peaks in the shallower Adriatic cores analysed, collected hundred kilometres apart, inside the mud belt environment. Based on the ecological requirements of this species, these two peaks have been interpreted as the more intense (cold and rainy) oscillations inside the LIA. The chronologic framework of the analysed cores is robust, being based on several range-finding 14C AMS ages, on estimates of the secular variation of the magnetic field, on geochemical estimates of the activity depth of 210Pb short-lived radionuclide (for the core-top ages), and is in good agreement with tephrochronologic, pollen and foraminiferal data. The intra-holocenic climate oscillations find out in the Adriatic have been compared with those pointed out in literature from other records of the Northern Hemisphere, and the chronologic constraint seems quite good. Finally, the sedimentary successions analysed allowed the review and the update of the foraminifers’ ecobiostratigraphy available from literature for the Adriatic region, thanks to the achievement of 16 ecobiozones for the last 60 kyr BP. Some bioevents are restricted to the Central Adriatic (for instance the LO of benthic Hyalinea balthica , approximating the MIS3/MIS2 boundary), others occur all over the Adriatic basin (for instance the LO of planktic Globorotalia inflata during MIS3, individuating Dansgaard-Oeschger cycle 8 (Denekamp)).

Archeologia e storia del Fayyum durante il Nuovo Regno

La presente ricerca prende in esame le dinamiche archeologiche e storiche della regione egiziana del Fayyum durante il Nuovo Regno (1552 – 1069 a.C.). L’elaborato è suddiviso in quattro parti: la prima analizza tutti i contesti archeologici che hanno restituito materiale databile al Bronzo Tardo, la seconda riguarda, invece, la catalogazione di tutti i documenti iscritti provenienti dalla regione e databili al medesimo periodo. La terza parte rappresenta la sintesi dei dati acquisiti nelle due precedenti sezioni e descrive il divenire storico regionale tra XVIII, XIX e XX dinastia, mentre la quarta parte, un’appendice prosopografica, chiude l’intero studio. I contesti archeologici fayyumici che hanno restituito materiale databile al Bronzo Tardo sono solamente sette: Gurob, el-Lahun, Haraga, Hawara, Medinet Madi, Shedet e Tebtynis. La distribuzione della documentazione tende a concentrarsi, dal punto di vista territoriale nell’area d’ingresso della regione, mentre dal punto di vista cronologico sono molto ben attestate la seconda metà dell’epoca thutmoside, l’età amarniana e la prima parte dell’epoca ramesside. Per quanto la documentazione regionale pertinente al Nuovo Regno sia estremamente rarefatta, soprattutto se paragonata a quella contestualizzabile cronologicamente ad altri periodi storici, un’attenta analisi delle testimonianze porta a collocare il Fayyum in una fitta trama di rapporti politici, economici e militari non solo con il resto del Paese ma anche con altre aree geografiche, esterne all’Egitto.

Celti e Reti tra V e I sec. a.C. Oggetti tipo LaTène all'interno della cerchia culturale Fritzens-Sanzeno (arco alpino centro-orientale)

The study of the objects LaTène type found in middle-eastern alpine region (Trentino Alto Adige-Südtirol, Engadina, North Tirol, Voralberg and Villach basin) is aimed to a better comprehension of the complex net of relationships established among the Celts, settled both in the central Europe territories and, since the IV century b.C., in the Po Plain, and the local populations. The ancient authors, who called the inhabitants of this area Raeti, propose for this territory the usual pattern according to which, the population of a region was formed consequently to a migration or was caused by the hunting of pre-existing peoples. The archaeologists, in the last thirty years, recognized a cultural facies typical of the middle-eastern alpine territory during the second Iron Age, and defined that as Fritzens-Sanzeno culture (from the sites of Fritzens, Inn valley, and Sanzeno, Non Valley). The so-called Fritzens-Sanzeno culture spread out without breaks from the material culture of the final Bronze Age and the first Iron Age. This local substratum, characterized by a ceramic repertoire strongly standardized, by peculiar architectural solutions and by a particular typology of rural sacred places (Brandopferplätze), accepted, above all during the second Iron Age, the strong influences coming from the Etruscan world and from the Celtic one (evident in the presence of objects of ornament, of glass artefacts, of elements of the weaponry and of coins). The objects LaTène type become, with different degrees of reliability, important markers of the relationships existing between the Celts and the Raeti, although the ways of interaction (cultural influence, people's movements, commercial exchanges, gifts among élites etc.) is not still clear. The revision of published data and the study of unpublished materials allows to define a rich and articulated picture both to chronological level and to territorial one.

Lo sviluppo dell'allevamento in Emilia-Romagna Aspetti economici e implicazioni sociali nella gestione della risorsa animale durante l’età del Bronzo

Il dibattito sullo sviluppo delle culture dell’età del Bronzo nel territorio dell’Emilia-Romagna sta portando una rinnovata attenzione sull’area romagnola. Le indagini si sono concentrate sull’area compresa tra il fiume Panaro e il Mare Adriatico, riconoscibile nell’odierna Romagna ed in parte della bassa pianura emiliana. Si trattava un territorio strategico, un vero e proprio crocevia socio-economico fra la cultura terramaricola e quelle centro italiche di Grotta Nuova. La presente ricerca di dottorato ha portato alla ricostruzione dei sistemi di gestione e di sfruttamento delle risorse animali in Emilia-Romagna durante l’Età del Bronzo, con particolare attenzione alla definizione della capacità portante ambientale dei diversi territori indagati e delle loro modalità di sfruttamento in relazione alla razionalizzazione della pratiche di allevamento. Sono state studiate in dettaglio le filiere di trasformazione dei prodotti animali primari e secondari definendo, quindi, i caratteri delle paleoeconomie locali nel processo di evoluzione della Romagna durante l’età del Bronzo. La ricerca si è basata sullo studio archeozoologico completo su 13 siti recentemente indagati, distribuiti nelle provincie di: Bologna, Ferrara, Ravenna, Forlì/Cesena e Rimini, e su una revisione completa delle evidenze archeozoologiche prodotte da studi pregressi. Le analisi non si sono limitate al riconoscimento delle specie, ma hanno teso all’individuazione ed alla valutazione di parametri complessi per ricostruire le strategie di abbattimento e le tecniche di sfruttamento e macellazione dei diversi gruppi animali. E’ stato possibile, quindi, valutare il peso ecologico di mandrie e greggi sul territorio e l’impatto economico ed ecologico di un allevamento sempre più sistematico e razionale, sia dal punto di vista dell’organizzazione territoriale degli insediamenti, sia per quanto riguarda le ripercussioni sulla gestione delle risorse agricole ed ambientali in generale.

Per una storia della cerealicoltura in Italia settentrionale dal Neolitico all’Età del Ferro: strategie adattive e condizionamenti ambientali.

Il presente elaborato si occupa della storia della cerealicoltura in un percorso diacronico dal Neolitico all’Età del Ferro. Sono presentate le analisi carpologiche di 14 siti archeologici dell’Italia settentrionale, esaminati secondo le più moderne tecniche di indagine archeobotanica.

Populationsgenetik kupfer- und bronzezeitlicher Bevölkerungen der osteuropäischen Steppe

Mit der vorliegenden Arbeit wurden erstmals prähistorische Bevölkerungsstrukturen in der osteuropäischen Steppe von der Oberthrakischen Tiefebene bis zur Wolga populationsgenetisch untersucht. Mit Multiplex-PCR und 454-Sequencing wurden von 65 kupfer- und bronzezeitlichen Individuen die Hypervariable Region I und 30 Abschnitte der coding region der mitochondrialen DNA analysiert. Außerdem wurden bis zu 20 putativ selektierte autosomale SNPs und ein geschlechtsspezifischer Locus genotypsiert. Zu Vergleichszwecken wurden veröffentlichte prähistorische DNA-Daten aus Westeurasien und moderne DNA-Sequenzen herangezogen. Die Ergebnisse stützen die Annahme, dass frühneolithische Bauern aus Südosteuropa durch demische Diffusion an der Etablierung der Viehwirtschaft in der Steppe beteiligt waren. Die durchweg niedrigen FST-Werte zwischen der frühbronzezeitlichen Jamnaja-Kultur in der Steppe und den aufeinanderfolgenden neolithischen Kulturen Mitteleuropas sprechen für regelmäßige Kontakte. Die der Jamnaja-Kultur nachfolgende Katakombengrabkultur ist von einem hohen Anteil der in nord- und osteuropäischen Jäger/Sammler-Populationen verbreiteten Haplogruppe U4 geprägt. Niedrige FST-Werte zwischen den prähistorischen Steppenpopulationen und der heutigen Bevölkerung Mittel- und Osteuropas weisen auf genetische Kontinuität hin. Die nukleären Genotypenfrequenzen bestätigt dies. Der moderne europäische Genpool lässt sich nach aktuellem Kenntnisstand auf drei Wurzeln zurückführen: indigene Mesolithiker, frühe Bauern aus dem Nahen Osten und eine nordeurasische Komponente jungpalaeolithischen Ursprungs. Letztere könnte vielleicht über die nordpontische Population in das Erbgut spätneolithischer Europäer gelangt sein.

Strategie insediative, economiche e scambi culturali nell'Appennino bolognese e romagnolo nell'eta' del Bronzo

Il seguente lavoro analizza lo sviluppo dell’occupazione territoriale dell’area collinare e montana del bolognese e della Romagna nell’età del Bronzo. Si sono censite le attestazioni archeologiche relative all’età del Bronzo nell’area di studio, per analizzare le tendenze insediative e le loro eventuali modificazioni nel corso del tempo, onde individuare le strategie alla base del scelta del luogo da insediare e le eventuali vie di percorrenza. Attraverso l’analisi tipologica del materiale rinvenuto nei vari contesti si è cercato di determinare le influenze culturali provenienti dal centro Italia o dalla zona terramaricola. Per raggiungere questo obbiettivo si sono analizzati i dati di archivio della Soprintendenza ai beni archeologici dell’Emilia Romagna e l’Archivio Renato Scarani, protagonista delle ricerche archeologiche in Emilia Romagna per il periodo degli anni ’50-’70 del XX secolo, recentemente acquisito dall’Università di Bologna. Ai dati desunti dagli archivi, che in molti casi hanno chiarito le vicende concernenti le indagini ed i posizionamenti di molti dei siti segnalati ed esplorati tra la seconda metà del XIX e gli anni ’70 del XX secolo, che costituiscono la maggioranza del campione analizzato, si sono aggiunti i dati recentemente acquisiti a seguito degli scavi a Monterenzio Località Chiesa Vecchia (Bo), uno dei siti più importanti (per stratigrafia conservata e per contesto territoriale) dell'Appennino Bolognese.

Populationsgenetik eisenzeitlicher Reiternomaden der Eurasischen Steppe

Vorliegende Dissertation beschäftigt sich mit der Populationsgenetik eisenzeitlicher Bevölkerungen der Eurasischen Steppe, die mit der skythischen Kultur assoziiert werden. Für die Analysen wurden 30 Fragmente der kodierenden Region und die HVR1 (16040–16400) des mitochondrialen Genoms, sowie 20 phänotypische Marker untersucht. Die Marker wurden durch Multiplex-PCRs angereichert, mit einem probenspezifischen barcode versehen und einer parallelen Sequenzanalyse mit dem 454 GS FLX Sequenzierer unterzogen. 97 Individuen wurden erfolgreich analysiert, von denen 19 aus dem Westen der Eurasischen Steppe und 78 aus dem Bereich des Altai-Gebirges stammen. Die populationsgenetischen Analysen ergaben geringe genetische Distanzen zwischen den skythischen Populationen aus dem Bereich des Altai-Gebirges, die sich vom 9. bis zum 3. Jahrhundert vor Christus erstrecken, was für eine kontinuierliche Bevölkerungsentwicklung sprechen könnte. Weiterhin finden sich geringe genetische Distanzen zwischen den Gruppen im Osten und Westen der Eurasischen Steppe, was auf eine gemeinsame Ursprungspopulation, oder zumindest Genfluss hinweisen kann. Die Ergebnisse aus dem Vergleich mit neolithischen und bronzezeitlichen Referenzpopulationen aus Zentralasien und den angrenzenden Gebieten weisen auf die Möglichkeit eines gemeinsamen zentral-asiatischen Ursprungs hin, zeigen aber auch, dass die östlichen und westlichen Gruppen der Eisenzeit jeweils zusätzlich lokalem Genfluss ausgesetzt waren. Die Allelfrequenzen der phänotypischen Marker deuten auf einen größeren europäischen Einfluss auf das östliche Zentralasien in der Eisenzeit hin, oder ansteigenden Genfluss aus Ostasien nach der Eisenzeit.

Die Problematik des sogenannten Bettpaneels von Ugarit

Gegenstand meiner Arbeit ist das Bettpaneel von Ugarit und seine komplexe Ikonographie, die Motive unterschiedlicher künstlerischer Traditionen des Alten Orients vereint. Das Bettpaneel bietet die einmalige Gelegenheit, das gesamte Bildprogramm eines Möbels zu untersuchen und die Entwicklung des levantinischen Kunsthandwerks der Späten Bronzezeit (2. Hälfte des 2. Jt.s v. Chr.) besser zu verstehen, besonders in Bezug auf Prestigegüter. Bereits 1952 ist das Bettpaneel im Königspalast von Ugarit entdeckt, jedoch bisher noch nicht monographisch abhandelt worden.rnEs wird gezeigt, dass das Bettpaneel von Ugarit ein hervorragendes Erzeugnis des lokalen Kunsthandwerks ist, gleichzeitig aber die kontinuierliche Übernahme fremder Motive bezeugt.rnWelche Vorbilder haben diese Rezeption begünstigt? Handelte es sich dabei um bewusste Anpassung an heimische Vorstellungen oder vielmehr um getreue Wiedergabe? Warum ließen sich die ugaritischen Handwerker von fremden Kunsttraditionen inspirieren? rnDank der detaillierten Untersuchung des Bettpaneels von Ugarit lassen sich diese wesentlichen Fragen über die Mechanismen der sozialen und kulturellen Interaktionen zwischen den Zivilisationen des Ostmittelmeergebiets im 2 Jt.s v. Chr. endgültig antworten.

Scales of Impact: Settlement History and Landscape Change in the Gordion Region, Central Anatolia

The expansion of agriculture in the Near East during the middle Holocene significantly altered the physical landscape. However, the relationship between the scale of agriculture and the magnitude and timing of the environmental impacts is not well known. The Gordion Regional Survey provides a novel dataset to compare settlement density during archaeological periods to rates of environmental disruption. Sediment samples from alluvial cores directly date the environmental disruption, which can be matched to period-specific settlement intensities in the watershed as constructed from archaeological survey ceramics. Degradation rates rose sharply within a millennium of the earliest Chalcolithic occupation. Early Bronze Age (EBA) land use induced the greatest rates of environmental degradation, although settlement density was relatively low on the landscape. The degradation rate subsequently decreased to one-third its early peak by the Iron Age, even as settlement intensity climbed. This trajectory reveals how complex interaction effects can amplify or subdue the responses of the landscape-land use system. Prior to settlement, landscape soil reservoirs were highly vulnerable, easily tipped by early agricultural expansion. Subsequent reduced rates of erosion are tied both to changes in sociopolitical organization and to depletion of the vulnerable soil supply.

The role of peat decomposition in patterned mires: a case study from the central Swiss Alps

A number of hydrological, botanical, macro- and micro-climatological processes are involved in the formation of patterned peatlands. La Grande Tsa at 2336 m a.s.l. is probably the highest bog in the central Swiss Alps and is unique in its pattern. In two of five pools there is in the contact zone between the basal peat and the overlying gyttja an unconformity in the depth-age models based on radiocarbon dates. Palynostratigraphies of cores from a ridge and a pool confirm the occurrence of an unconformity in the contact zone. We conclude that deepening of the pools results from decomposition of peat. The fact that the dated unconformities in the two pools and the unconformity in the ridge-core all fall within the Bronze Age suggest they were caused by events external to the bog. We hypothesize that early transhumance resulted in anthropogenic lowering of the timberline, which resulted in a reduction in the leaf-area index and evapotranspiration, and in higher water levels and thus pool formation.

Archaeological Discoveries on Schnidejoch and at Other Ice Sites in the European Alps

Only a few sites in the Alps have produced archaeological finds from melting ice. To date, prehistoric finds from four sites dating from the Neolithic period, the Bronze Age, and the Iron Age have been recovered from small ice patches (Schnidejoch, Lötschenpass, Tisenjoch, and Gemsbichl/Rieserferner). Glaciers, on the other hand, have yielded historic finds and frozen human remains that are not more than a few hundred years old (three glacier mummies from the 16th to the 19th century and military finds from World Wars I and II). Between 2003 and 2010, numerous archaeological finds were recovered from a melting ice patch on the Schnidejoch in the Bernese Alps (Cantons of Berne and Valais, Switzerland). These finds date from the Neolithic period, the Early Bronze Age, the Iron Age, Roman times, and the Middle Ages, spanning a period of 6000 years. The Schnidejoch, at an altitude of 2756 m asl, is a pass in the Wildhorn region of the western Bernese Alps. It has yielded some of the earliest evidence of Neolithic human activity at high altitude in the Alps. The abundant assemblage of finds contains a number of unique artifacts, mainly from organic materials like leather, wood, bark, and fibers. The site clearly proves access to high-mountain areas as early as the 5th millennium BC, and the chronological distribution of the finds indicates that the Schnidejoch pass was used mainly during periods when glaciers were retreating.