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Jahresschrift für mitteldeutsche Vorgeschichte, Bd. 74 (1991): Jahresschrift für Mitteldeutsche Vorgeschichte

Acta Praehistorica et Archaeologica, Bd. 50 (2018)

Jahresschrift für mitteldeutsche Vorgeschichte, Bd. 65 (1982): Jahresschrift für Mitteldeutsche Vorgeschichte

Jahresschrift für mitteldeutsche Vorgeschichte, Bd. 68 (1985): Jahresschrift für Mitteldeutsche Vorgeschichte

The Klyuchevskaya group of volcanoes (KGV) located in the northern part of Kamchatka has the highest magma production rate for any arc worldwide and several of its volcanoes have been studied in considerable detail [e.g. Kersting & Arculus, 1995; Pineau et al., 1999; Dorendorf et al., 2000; Ozerov, 2000; Churikova et al., 2001, 2012, 2015; Mironov et al., 2001; Portnyagin et al., 2007, 2015; Turner et al., 2007]. However, some volcanoes of the KGV including Late-Pleistocene volcanoes Bolshaya Udina, Malaya Udina, Ostraya Zimina, Ovalnaya Zimina, and Gorny Zub were studied only on a reconnaissance basis [Timerbaeva, 1967; Ermakov, 1977] and the modern geochemical studies have not been carried out at all. Among the volcanoes of KGV these volcanoes are closest to the arc trench and may hold information on geochemical zonation with respect to across arc source variations. We present the first major and trace element data on rocks from these volcanoes as well as on their basement. All rocks are medium-calc-alkaline basaltic andesites to dacites except few low-Mg basalts from Malaya Udina volcano. Phenocrysts are mainly olivine, pyroxene, plagioclase and magnetite, Hb-bearing andesites and dacites are rarely found only in subvolcanic intrusions at Bolshaya Udina volcano. Lavas are geochemically similar to the active Bezymianny volcano, however, individual variations for each volcano exist in both major and trace elements. Trace element geochemistry is typical of island arc volcanism. Compared to KGV lavas all studied rocks form very narrow trends in all major element diagrams, which almost do not overlap with the fields of other KGV volcanoes. The lavas are relatively poor in alkalis, TiO2, P2O5, FeO, Ni, Zr, and enriched in SiO2 compared to other KGV volcanics and show greater geochemical and petrological evidence of magmatic differentiation during shallow crustal processing. Basement samples of the Udinskoe plateau lavas to the east of Bolshaya Udina volcano have similar geochemical composition (trace element enriched high-K basaltic andesites and andesites) and similar eruption age of 274 ka [Calkins et al., 2004] as typical plateau lavas below the northern KGV. This research was supported by RFBR-DFG grant # 16-55-12040.

Aquifer Storage and Recovery (ASR) was a pilot project for solving flood and drought problem in the northern part of Chao Phraya River basin, Thailand. This part of Thailand always faces flooding in rainy season and drought during dry season every year. The overexploitation of groundwater during dry season leads to continuously decline of water level in this area. In this project, the excessive surface water during rainy season was stored by injection of this treated surface water through recharge wells into the underground aquifers. This would serve to raise the water level, which can be extracted for use during the dry season. To assess the efficiency of the ASR process some tracers are required. The aim of this study is to prove the suitability of natural tracers to follow up the artificial recharge process; emphasis will be placed on Strontium (Sr) isotopic composition. The results showed that the change in 87Sr/86Sr ratios could be observed during an artificial recharge due to the different isotopic fingerprint of surface water and groundwater. However, the flow direction of the injected water cannot be clearly interpreted because of the limited number of monitoring wells, small distance between each monitoring well and the short duration of injection., Open-Access-Publikationsfonds 2016

In der Rehabilitation nach Knie- oder Hufttotalendoprothese (TEP) stellen bewegungstherapeutische Interventionen den zentralen Inhalt dar. Die entsprechende Evidenz ist allerdings luckenhaft, und es mangelt an tragfahigen Aussagen uber Dosis-Wirkungs-Beziehungen, wodurch der Einfluss der Bewegungstherapie auf den Rehabilitationsverlauf unklar bleibt. Dies wirft, auch angesichts der hohen und voraussichtlich weiter ansteigenden Fallzahlen sowie der bestehenden Resourcenknappheit im Gesundheitssystem, die Frage nach der Legitimitat fur die umfangreiche bewegungstherapeutische Leistungserbringung in der Rehabilitation nach Knieoder Huft-TEP auf.

We present a prediction model for digital printers and more specifically for electrophotographic devices. On the one hand, we propose an electrophotographic simulation model which estimates the microscopic structure of any printed toner layer based on its input halftone bitmap. Applying BOUGUER-BEER-LAMBERT's law, the obtained spatial toner arrangement yields the spectral transmittance distribution for non-light scattering colors. On the other hand, we introduce an extension to the KUBELKA-MUNK (KM) model, which allows to compute the halftone reflectance spectra from the estimated transmittance spectra. The extended KM model bridges the gap between the mathematical description of the optical point spread function of common office papers and the experimental results of simple reflectance measurements. With the combination of the models, we are capable of predicting the reflectance spectra of a printed monochrome wedge with a mean estimation error of less than CIELAB ΔE*94 = 1.

Frank Wiese, Mike Reich and Gernot Arp (Eds.) “Spongy, slimy, cosy & more ; 99-112

Due to its simplicity, the theory of KUBELKA-MUNK [1] has found a wide acceptance for modeling the optical properties of light scattering materials. However, the concept is not explicitly adapted to predict halftone prints on paper. In this respect, a recent improvement was given by BERG. Our approach is an extension of BERG'S model in order to reduce the gap between the mathematical description of the paper's point spread function and the experimental results of simple reflectance measurements.

To monitor time trends of obesity in children, data from the school-entry screening programs (SEU) are widely used. By using data from the SEU in North Rhine-Westphalia (NRW), Germany, from 1996 to 2008, it was investigated, if age distribution is changing over time and if changes influence the overall proportion of obese children in NRW. In addition, the time trend of obesity in three age groups of children before school entry is shown. Children who were examined during SEU are becoming younger (1996: 75.3 months; 2008: 71.3 months, on average). The observed stagnation of obesity in NRW in recent years also persists when the influence of different age patterns are taken into account. Younger children are less obese than older ones. A sustained increase in the proportion of younger children during SEU might influence the overall proportion of obese children in the future. Thus, it should be discussed which procedures should be used to increase the quality of the indicator that is used for public health reporting and is generated by data from SEU.

Technical report, 297

Technical Report / ETH Zurich, Department of Computer Science, 261

ETH, Eidgenössische Technische Hochschule Zürich, Departement Informatik, Institut für Theoretische Informatik, 224

ETH, Eidgenössische Technische Hochschule Zürich, Departement Informatik, Institut für Theoretische Informatik, 171

Die Geowissenschaften

ETH, Eidgenössische Technische Hochschule Zürich, Departement Informatik, Institut für Theoretische Informatik, 103

During the Variscan orogeny in Central Europe, partial melting in the lower continental crust formed granitic magmas, which intruded into the upper crust and left compounds of Ca (plus Eu2+), Mg, etc. in the lower crust. From the late Paleozoic decomposition of the tonalitic upper crust, sedimentary graywackes were produced reflecting the composition of this crust. The repeated reworking of the sedimentary cover caused the formation of sands. Sandstones as their products of consolidation contain increasing fractions of quartz and decreasing feldspar from Carboniferous and Triassic to Cretaceous age. A distinct negative Eu anomaly characterizes the majority of these rocks. The latter is imprinted by the Variscan magmatism. Quartz as used for numerous Medieval wood ash glasses is marked for its Central European origin by a distinct negative Eu anomaly in contrast to many soda glasses produced outside Germany mostly with a small or none Eu anomaly.