Studia Quaternaria最新文献_第3页

Remote Sensing of a Roman Pottery Workshop. Report on a Geophysical Survey Carried out in Crikvenica (Ancient Ad Turres, Croatia) 罗马陶器作坊的遥感。在克列克韦尼察(克罗地亚古Ad Turres)进行的地球物理调查报告

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Studia Quaternaria Pub Date : 2017-01-01 DOI: 10.1515/squa-2017-0010

F. Welc, Goranka Lipovac Vrkljan, Ana Konestra, Tea Rosic

{"title":"Remote Sensing of a Roman Pottery Workshop. Report on a Geophysical Survey Carried out in Crikvenica (Ancient Ad Turres, Croatia)","authors":"F. Welc, Goranka Lipovac Vrkljan, Ana Konestra, Tea Rosic","doi":"10.1515/squa-2017-0010","DOIUrl":"https://doi.org/10.1515/squa-2017-0010","url":null,"abstract":"Abstract The paper presents results of a geophysical survey conducted in Crikvenica, a town located at the north-eastern Adriatic Sea coast in Croatia. The main aim was to identify extent of a Roman pottery workshop discovered to the north of the present town, at the site known as “Igralište”. The performed magnetic and GPR surveys within the area of the modern playground in Crikvenica revealed a large number of anomalies that may be connected with anthropogenic activity during different periods, both in modern and ancient times. The first group consists of anomalies generated by remnants of the modern underground infrastructure. Magnetic and ground-penetrating radar maps revealed anomalies in the north-western part of the modern playground that can be very likely interpreted as remains of a large ceramic kiln dated back to the Roman Period, similar to the kiln discovered during the excavations located further to the north. Finally, the survey performed within the Crikvenica football stadium clearly indicates that the integration of different Ground Penetrating Radar and magnetic methods allows for a detailed and effective identification of buried archaeological structures in large areas.","PeriodicalId":42625,"journal":{"name":"Studia Quaternaria","volume":null,"pages":null},"PeriodicalIF":0.6,"publicationDate":"2017-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"67306837","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 5

Reading of Ground-Penetrating Radar (GPR) Images of Prehistoric Flint Mine; Case Study from Krzemionki Opatowskie Archaeological Site In Central Poland 史前燧石矿探地雷达图像读取波兰中部Krzemionki opatowski考古遗址案例研究

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Studia Quaternaria Pub Date : 2016-12-01 DOI: 10.1515/squa-2016-0012

F. Welc, R. Mieszkowski, L. Conyers, J. Budziszewski, Artur Jedynak

引用次数: 5

Weathering Rind Age Assignment of Neoglacial Deposits in the Okstindan Mountains, Northern Norway 挪威北部奥克斯坦丹山脉新冰川沉积物的风化层年龄测定

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Studia Quaternaria Pub Date : 2016-12-01 DOI: 10.1515/squa-2016-0013

W. Mahaney

{"title":"Weathering Rind Age Assignment of Neoglacial Deposits in the Okstindan Mountains, Northern Norway","authors":"W. Mahaney","doi":"10.1515/squa-2016-0013","DOIUrl":"https://doi.org/10.1515/squa-2016-0013","url":null,"abstract":"Abstract Previous soil stratigraphic analysis of soil morphogenesis in the Okstindan Mountains established a Late Neoglacial soil evolutionary sequence based on historically monitored and radio carbon-dated moraine positions over the last ~3.0 cal yr BP. Thus pedon evolution ranged from C/Cu→Ah/Cox/Cu→pedostratigraphic succession of Ah/C/Cu/Lb/ Cub/Ahb/Coxb/Cub pro files with a max i mum rind weathering time of ~1.0 kyr. Following successive re treat phases of Neoglacial ice, weathering rind development continued apace on moraines, each rind population recording weathering time fol lowing successive glacier still stands. The age of the youngest deposits falls within the period 1900-1910 AD, or the last 100 yrs, with variable moraine positions all documented by historical depictions of the position of the Austre Okstindan glacial lobe prior re treating to its present position. The next older group of deposits is considered to have been emplaced near the end of the LIA or around ~1800 AD, with time of rind development set at 200 yr, possibly older. The old est moraine set within the late Neoglacial sequence lies atop a pedostratigraphic column, the upper-most soil radio carbon dated at ~1.0 yr BP. Given the range of mean rind development across this thresh old of deposits, from 0.22 ±0.03 mm in the inner group, 0.66 ±0.07mm in the middle group, to 1.38 ±0.15 mm in the outer, older group, it is clear that finite measurements at several sites within a suite of deposits, some dated by radio carbon, can evenly discriminate be tween deposits in a glacial succession.","PeriodicalId":42625,"journal":{"name":"Studia Quaternaria","volume":null,"pages":null},"PeriodicalIF":0.6,"publicationDate":"2016-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"67306605","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

Variability of Cation-Exchange Capacity (CEC) of Fen Peats in Vertical Profiles from Eastern and Central Poland in Relation to Function of Peatlands as Natural Geological Barriers 波兰东部和中部沼泽泥炭垂直剖面阳离子交换容量(CEC)变化与泥炭地天然地质屏障功能的关系

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Studia Quaternaria Pub Date : 2016-12-01 DOI: 10.1515/squa-2016-0011

Paweł Rydelek, A. Bąkowska, Piotr Zawrzykraj

{"title":"Variability of Cation-Exchange Capacity (CEC) of Fen Peats in Vertical Profiles from Eastern and Central Poland in Relation to Function of Peatlands as Natural Geological Barriers","authors":"Paweł Rydelek, A. Bąkowska, Piotr Zawrzykraj","doi":"10.1515/squa-2016-0011","DOIUrl":"https://doi.org/10.1515/squa-2016-0011","url":null,"abstract":"Abstract An analysis of cation-exchange capacity(CEC) variability of peats is presented in vertical pro files from eastern and central Po land. CEC values were com pared with ash con tent (Ac), pH and CaCO3 content. Eight peatlands were selected for re search in the fol lowingareas: War saw Plateau (2 objects), Siedlce Plateau (2 objects), Lubartów Plateau (2 objects), Nałęczów Table land (1 object) and Dobrohusk Depression (1 object). The peatlands represented a fen peat type of similar botanic compositions of sediments, but they differed in the area, peat thickness and drain age conditions. Characteristic regular i ties in CEC variability were noted in the peatlands and there were three types of CEC variability in vertical pro files. Carbonate peats (types 1 and 2) had the high est pH and definitely the high est values of CEC. In vertical pro files, there was also a zonation, but the regularities similar to non-carbonate peats were not observed. Different distribution of phys i cal and chem i cal parameters were establishedin vertical pro files in partly drained peatlands (with a muck layer on top) with non-carbonate peats (type 3) and there were three distinct zones in vertical pro files, with different Ac and CEC. Determination of the vertical CEC variability and other phys i cal and chem i cal parameters in peatlands made it possible to distinguish zones with potentially most beneficial isolation conditions.","PeriodicalId":42625,"journal":{"name":"Studia Quaternaria","volume":null,"pages":null},"PeriodicalIF":0.6,"publicationDate":"2016-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1515/squa-2016-0011","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"67306653","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 1

Application of Electrical Resistivity Imaging and Land Surveying in the Analysis of Underground Construction Impact on the Warsaw Scarp 电阻率成像与土地测量在华沙断崖地下工程影响分析中的应用

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Studia Quaternaria Pub Date : 2016-12-01 DOI: 10.1515/squa-2016-0008

Ł. Kaczmarek, R. Mieszkowski, M. Woźniak, Tomasz Dybciak

{"title":"Application of Electrical Resistivity Imaging and Land Surveying in the Analysis of Underground Construction Impact on the Warsaw Scarp","authors":"Ł. Kaczmarek, R. Mieszkowski, M. Woźniak, Tomasz Dybciak","doi":"10.1515/squa-2016-0008","DOIUrl":"https://doi.org/10.1515/squa-2016-0008","url":null,"abstract":"Abstract The paper presents the analysis of the II Underground Line construction’s impact on the Warsaw Scarp with the use of the electrical resistivity imaging (ERI, also known as the electrical resistivity tomography) and further total station position measurements.The underground passes under the scarp perpendicular in the area of Dynasy Street 6, in Down-town district.The electrical resistivity imaging was performed for recognition of the geological structure and a potential land slide surface or zone.The gradient system was used during the prospection. In these analyses, the longitudinal section was 40 m long, and the depth of survey amounted to 6 m. In the case of the 200 m long transverse section, the resulted depth of survey was 30 m.The geophysical image of the longitudinal section,does not contain loosening soil zones,which could indicates lip surface.Next, total station measurements, which were tied to the archival geodetic observations’ results, were carried out. The aim of the measurements was to verify the activity of the horizontal and vertical displacements. The TBM excavation process led to summary vertical displacements up to approx. 24 mm and horizontal displacements amounting to approx. 13 mm. To sum up, the current land surveys reveals minor under ground line’ s construction impact on the scarp displacement. Nevertheless, the sensitive urban environment requires further monitoring, especially that the operation loads can result in displacement rate change.","PeriodicalId":42625,"journal":{"name":"Studia Quaternaria","volume":null,"pages":null},"PeriodicalIF":0.6,"publicationDate":"2016-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"67306115","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 2

The Influence of Natural Climatic Factors on the Geomechanical Properties of Siliceous Lime Stones from Kazimierz Dolny (Poland) 自然气候因素对波兰Kazimierz Dolny硅质石灰石地质力学性质的影响

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Studia Quaternaria Pub Date : 2016-12-01 DOI: 10.1515/squa-2016-0010

J. Pinińska, A. Bobrowska, Dominik Łukasiak

引用次数: 3

Mapping of the North-Eastern Part of Kozłowicka Buried Valley Based on Geoelectrical Data 基于地电数据的Kozłowicka隐谷东北部填图

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Studia Quaternaria Pub Date : 2016-12-01 DOI: 10.1515/squa-2016-0009

Sylwia Topolewska, M. Stępień, S. Kowalczyk

{"title":"Mapping of the North-Eastern Part of Kozłowicka Buried Valley Based on Geoelectrical Data","authors":"Sylwia Topolewska, M. Stępień, S. Kowalczyk","doi":"10.1515/squa-2016-0009","DOIUrl":"https://doi.org/10.1515/squa-2016-0009","url":null,"abstract":"Abstract The paper is aiming to determinate the extent of the north eastern arm of Kozłowicka buried valley on the grounds of own re search by means of electrical resistivity tomography- ERT and avail able archival researches. On the Hydro-geological map of Poland, Żyrardów sheet (Felter and Nowicki, 1998a, b) Kozłowicka buried valley was differentiated as an individual hydro-geological unit. The results of the anal y sis show that the ex tent of the structure, defined by its up per boundary, differs significantly from the one suggested on the sheet of Hydrogeological map of Poland. Since there was no data avail able in the north eastern part of the dis cussed arm of Kozłowicka buried valley, the northern boundary was defined only based on avail able geoelectrical sounding profiles (Czerwiñska, 1988; Topolewska, 2015). In order to confirm suggested solution, geoelectrical re search by means of electrical resistivity tomography (ERT) was con ducted. The measurements were per formed along 3 pro files located in the area of interest. The authors would like to point out the need of the us age of ERT in map ping and studying buried structures that might be ground water reservoirs. As a result, one obtains quasi-continuous image of electrical resistivity of the subsurface. Due to the contrast of electrical properties of sediments, it is possible to determine upper and bottom surfaces of buried structures, formed within glacial deposits.","PeriodicalId":42625,"journal":{"name":"Studia Quaternaria","volume":null,"pages":null},"PeriodicalIF":0.6,"publicationDate":"2016-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"67306234","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 1

Preliminary Report on Engineering Properties and Environmental Resistance of Ancient Mud Bricks from Tell El-Retaba Archaeological Site in the Nile Delta 尼罗河三角洲Tell El-Retaba考古遗址古泥砖工程性能及环境抗性初步报告

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Studia Quaternaria Pub Date : 2016-06-01 DOI: 10.1515/squa-2016-0005

J. Trzciński, M. Zaremba, S. Rzepka, F. Welc, Tom Szczepanski

{"title":"Preliminary Report on Engineering Properties and Environmental Resistance of Ancient Mud Bricks from Tell El-Retaba Archaeological Site in the Nile Delta","authors":"J. Trzciński, M. Zaremba, S. Rzepka, F. Welc, Tom Szczepanski","doi":"10.1515/squa-2016-0005","DOIUrl":"https://doi.org/10.1515/squa-2016-0005","url":null,"abstract":"Abstract The archaeological site Tell el-Retaba in north-eastern Egypt, about 35 km to the west of Ismailia city, is located in the middle of Wadi Tumilat, a shallow valley running from the Nile Delta to the Bitter Lakes, along which flows the Suez Canal. In ancient times the valley was a route between Egypt and Syro-Palestine, strongly fortified in the New Kingdom times (16th–11th century BC). Mud bricks were analyzed from two parts of the Wall 1 (core of grey-brown bricks and inner extension of green bricks) in a fortress which existed during the Ramesses II times. Grain-size composition of the studied bricks was almost identical in both parts of the wall, suggesting the same source material for a production of brick. However, significant differences were observed in physical and mechanical properties (uni-axial compressive strength) in both types of bricks. Bricks from the core had lower bulk density, higher porosity and soak faster, whereas their resistance parameters were much lower than those of the bricks from the inner extension. The reason for such large differences in brick properties was a technology of their production, particularly proportion of components, water volume added during brick formation or density degree. Brick preparation and in consequence, physical-mechanical properties had direct influence on preservation of defensive structures during environmental changes related to changes of groundwater and surface water levels or of precipitation. Ancient Egyptians responsible for construction works in mud brick structures of the fortress must have had good knowledge and experience. This could be observed particularly for the heaviest and most important construction element that is the defensive wall, founded on well-densified deposits. It was also testified by higher resistance of green bricks from the inner extensions, which probably originated slightly later and were intended to reinforce a weaker core built of grey-brown bricks.","PeriodicalId":42625,"journal":{"name":"Studia Quaternaria","volume":null,"pages":null},"PeriodicalIF":0.6,"publicationDate":"2016-06-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"67306023","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 5

Intermediate Bronze Age in Southern Levant (4200–4000 BP) – Why Did Four Cities in Transjordan Survive Urban Collapse? 南黎凡特的青铜时代中期(距今4200-4000年前)——为什么外约旦的四个城市在城市崩溃中幸存下来?

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Studia Quaternaria Pub Date : 2016-06-01 DOI: 10.1515/squa-2016-0001

Michal Bieniada

{"title":"Intermediate Bronze Age in Southern Levant (4200–4000 BP) – Why Did Four Cities in Transjordan Survive Urban Collapse?","authors":"Michal Bieniada","doi":"10.1515/squa-2016-0001","DOIUrl":"https://doi.org/10.1515/squa-2016-0001","url":null,"abstract":"Abstract The first urban culture of southern Levant collapsed and the first period of urbanisation of Canaan (Early Bronze Age I-III) terminated at around 4200 yrs BP. The Canaanites abandoned their walled cities, dispersed and underwent pastoralisation. However, the urban centres of southern Canaan were not destroyed. This fact may point to responsibility of the environmental factor and makes influence influence of anthropogenic factors uncertain, along with the most popular Amorite invasion/destruction hypothesis. A tremendous climatic change occurred at that time in many regions, affecting cultures and civilisations of the Ancient Near East and resulting in abandonment of cities, migrations and great civilizational changes. In southern Levant, virtually all cities were left in ruins with a mysterious exception in Transjordan where four cities: Aroer, Ader, Khirbet Iskander and Iktanu survived and existed throughout the period. Most probably when climatic conditions in Cisjordan excluded possibility of urban life, the ones in Transjordan conditions remained unchanged or altered in a very limited scale. It is now clear that after a period with quite humid and warm climate, the precipitation greatly diminished after 4200 yrs BP in a littoral zone of eastern Mediterranean. A part of Transjordan, probably due to presence of the Dead Sea that somehow created conditions that influenced precipitation, remained a climatic niche with decent rainfall that enabled concentration of population in and around big urban centres and continuation of urban civilisation. Warming in a littoral zone changed dew point temperature preventing formations of clouds above western slopes of Judean and Samarian Hills. Moist air, prevented from condensation was transported eastwards where it could reach ascending currents appearing over the Dead Sea. Masses of air with water vapour moving upwards could form rainy clouds in Transjordan.","PeriodicalId":42625,"journal":{"name":"Studia Quaternaria","volume":null,"pages":null},"PeriodicalIF":0.6,"publicationDate":"2016-06-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"67302908","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 4

Architectural Innovations Influenced by Climatic Phenomena (4.2 Ka Event) in the Late Old Kingdom (Saqqara, Egypt) 古王国晚期(埃及萨卡拉)受气候现象(4.2 Ka事件)影响的建筑创新

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Studia Quaternaria Pub Date : 2016-06-01 DOI: 10.1515/squa-2016-0003

K. Kuraszkiewicz

引用次数: 2