Search results for: HORIZONTAL CYLINDER

• Description of symmetrical prolate ellipsoid magnetic signature parameters-Be = 50 mT, I = 70 deg, z = 20 m, q = 80 deg, j = 45 deg, a =4 m, e = 8, mr = 100

  Open Research Data

  open access

  • M. Wołoszyn
  • K. Pankowska

  - series: magnetic signatures

  The Earth magnetic field (Fig.1): BE – total magnetic flux density, BEx – x component of the Earth magnetic flux density, BEy = 0  y component of the Earth magnetic flux density, BEz – z component of the Earth magnetic flux density, I – inclination of the Earth magnetic field.

• Description of symmetrical prolate ellipsoid magnetic signature parameters-Be = 50 mT, I = 70 deg, z = 200 m, q = 180 deg, j = 135 deg, a =4 m, e = 4, mr = 100

  Open Research Data

  open access

  • M. Wołoszyn
  • K. Pankowska

  - series: magnetic signatures

  The Earth magnetic field (Fig.1): BE – total magnetic flux density, BEx – x component of the Earth magnetic flux density, BEy = 0  y component of the Earth magnetic flux density, BEz – z component of the Earth magnetic flux density, I – inclination of the Earth magnetic field.

• Description of symmetrical prolate ellipsoid magnetic signature parameters-Be = 50 mT, I = 70 deg, z = 200 m, q = 80 deg, j = 135 deg, a =4 m, e = 4, mr = 100

  Open Research Data

  open access

  • M. Wołoszyn
  • K. Pankowska

  - series: magnetic signatures

  The Earth magnetic field (Fig.1): BE – total magnetic flux density, BEx – x component of the Earth magnetic flux density, BEy = 0  y component of the Earth magnetic flux density, BEz – z component of the Earth magnetic flux density, I – inclination of the Earth magnetic field.

• Description of symmetrical prolate ellipsoid magnetic signature parameters-Be = 50 mT, I = 70 deg, z = 50 m, q = 80 deg, j = 135 deg, a =4 m, e = 4, mr = 100

  Open Research Data

  open access

  • M. Wołoszyn
  • K. Pankowska

  - series: magnetic signatures

  The Earth magnetic field (Fig.1): BE – total magnetic flux density, BEx – x component of the Earth magnetic flux density, BEy = 0  y component of the Earth magnetic flux density, BEz – z component of the Earth magnetic flux density, I – inclination of the Earth magnetic field.

• Description of symmetrical prolate ellipsoid magnetic signature parameters-Be = 50 mT, I = 70 deg, z = 200 m, q = 100 deg, j = 45 deg, a =4 m, e = 8, mr = 100

  Open Research Data

  open access

  • M. Wołoszyn
  • K. Pankowska

  - series: magnetic signatures

  The Earth magnetic field (Fig.1): BE – total magnetic flux density, BEx – x component of the Earth magnetic flux density, BEy = 0  y component of the Earth magnetic flux density, BEz – z component of the Earth magnetic flux density, I – inclination of the Earth magnetic field.

• Description of symmetrical prolate ellipsoid magnetic signature parameters-Be = 50 mT, I = 70 deg, z = 10 m, q = 90 deg, j = 45 deg, a =4 m, e = 8, mr = 100

  Open Research Data

  open access

  • M. Wołoszyn
  • K. Pankowska

  - series: magnetic signatures

  The Earth magnetic field (Fig.1): BE – total magnetic flux density, BEx – x component of the Earth magnetic flux density, BEy = 0  y component of the Earth magnetic flux density, BEz – z component of the Earth magnetic flux density, I – inclination of the Earth magnetic field.

• Description of symmetrical prolate ellipsoid magnetic signature parameters-Be = 50 mT, I = 70 deg, z = 200 m, q = 90 deg, j = 135 deg, a =4 m, e = 4, mr = 100

  Open Research Data

  open access

  • M. Wołoszyn
  • K. Pankowska

  - series: magnetic signatures

  The Earth magnetic field (Fig.1): BE – total magnetic flux density, BEx – x component of the Earth magnetic flux density, BEy = 0  y component of the Earth magnetic flux density, BEz – z component of the Earth magnetic flux density, I – inclination of the Earth magnetic field.

• Description of symmetrical prolate ellipsoid magnetic signature parameters-Be = 50 mT, I = 70 deg, z = 200 m, q = 80 deg, j = 45 deg, a =4 m, e = 8, mr = 100

  Open Research Data

  open access

  • M. Wołoszyn
  • K. Pankowska

  - series: magnetic signatures

  The Earth magnetic field (Fig.1): BE – total magnetic flux density, BEx – x component of the Earth magnetic flux density, BEy = 0  y component of the Earth magnetic flux density, BEz – z component of the Earth magnetic flux density, I – inclination of the Earth magnetic field.

• Description of symmetrical prolate ellipsoid magnetic signature parameters-Be = 50 mT, I = 70 deg, z = 20 m, q = 100 deg, j = 45 deg, a =4 m, e = 8, mr = 100

  Open Research Data

  open access

  • M. Wołoszyn
  • K. Pankowska

  - series: magnetic signatures

  The Earth magnetic field (Fig.1): BE – total magnetic flux density, BEx – x component of the Earth magnetic flux density, BEy = 0  y component of the Earth magnetic flux density, BEz – z component of the Earth magnetic flux density, I – inclination of the Earth magnetic field.

• Description of symmetrical prolate ellipsoid magnetic signature parameters-Be = 50 mT, I = 70 deg, z = 20 m, q = 80 deg, j = 135 deg, a =4 m, e = 1, mr = 100

  Open Research Data

  open access

  • M. Wołoszyn
  • K. Pankowska

  - series: magnetic signatures

  The Earth magnetic field (Fig.1): BE – total magnetic flux density, BEx – x component of the Earth magnetic flux density, BEy = 0  y component of the Earth magnetic flux density, BEz – z component of the Earth magnetic flux density, I – inclination of the Earth magnetic field.

• Description of symmetrical prolate ellipsoid magnetic signature parameters-Be = 50 mT, I = 70 deg, z = 10 m, q = 80 deg, j = 135 deg, a =4 m, e = 1, mr = 100

  Open Research Data

  open access

  • M. Wołoszyn
  • K. Pankowska

  - series: magnetic signatures

  The Earth magnetic field (Fig.1): BE – total magnetic flux density, BEx – x component of the Earth magnetic flux density, BEy = 0  y component of the Earth magnetic flux density, BEz – z component of the Earth magnetic flux density, I – inclination of the Earth magnetic field.

• Description of symmetrical prolate ellipsoid magnetic signature parameters-Be = 50 mT, I = 70 deg, z = 10 m, q = 100 deg, j = 135 deg, a =4 m, e = 4, mr = 100

  Open Research Data

  open access

  • M. Wołoszyn
  • K. Pankowska

  - series: magnetic signatures

  The Earth magnetic field (Fig.1): BE – total magnetic flux density, BEx – x component of the Earth magnetic flux density, BEy = 0  y component of the Earth magnetic flux density, BEz – z component of the Earth magnetic flux density, I – inclination of the Earth magnetic field.

• Description of symmetrical prolate ellipsoid magnetic signature parameters-Be = 50 mT, I = 70 deg, z = 50 m, q = 90 deg, j = 135 deg, a =4 m, e = 4, mr = 100

  Open Research Data

  open access

  • M. Wołoszyn
  • K. Pankowska

  - series: magnetic signatures

  The Earth magnetic field (Fig.1): BE – total magnetic flux density, BEx – x component of the Earth magnetic flux density, BEy = 0  y component of the Earth magnetic flux density, BEz – z component of the Earth magnetic flux density, I – inclination of the Earth magnetic field.

• Description of symmetrical prolate ellipsoid magnetic signature parameters-Be = 50 mT, I = 70 deg, z = 10 m, q = 80 deg, j = 45 deg, a =4 m, e = 8, mr = 100

  Open Research Data

  open access

  • M. Wołoszyn
  • K. Pankowska

  - series: magnetic signatures

  The Earth magnetic field (Fig.1): BE – total magnetic flux density, BEx – x component of the Earth magnetic flux density, BEy = 0  y component of the Earth magnetic flux density, BEz – z component of the Earth magnetic flux density, I – inclination of the Earth magnetic field.

• Description of symmetrical prolate ellipsoid magnetic signature parameters-Be = 50 mT, I = 70 deg, z = 20 m, q = 80 deg, j = 135 deg, a =4 m, e = 4, mr = 100

  Open Research Data

  open access

  • M. Wołoszyn
  • K. Pankowska

  - series: magnetic signatures

  The Earth magnetic field (Fig.1): BE – total magnetic flux density, BEx – x component of the Earth magnetic flux density, BEy = 0  y component of the Earth magnetic flux density, BEz – z component of the Earth magnetic flux density, I – inclination of the Earth magnetic field.

• Description of symmetrical prolate ellipsoid magnetic signature parameters-Be = 50 mT, I = 70 deg, z = 100 m, q = 100 deg, j = 135 deg, a =4 m, e = 4, mr = 100

  Open Research Data

  open access

  • M. Wołoszyn
  • K. Pankowska

  - series: magnetic signatures

  The Earth magnetic field (Fig.1): BE – total magnetic flux density, BEx – x component of the Earth magnetic flux density, BEy = 0  y component of the Earth magnetic flux density, BEz – z component of the Earth magnetic flux density, I – inclination of the Earth magnetic field.

• Description of symmetrical prolate ellipsoid magnetic signature parameters-Be = 50 mT, I = 70 deg, z = 50 m, q = 90 deg, j = 45 deg, a =4 m, e = 8, mr = 100

  Open Research Data

  open access

  • M. Wołoszyn
  • K. Pankowska

  - series: magnetic signatures

  The Earth magnetic field (Fig.1): BE – total magnetic flux density, BEx – x component of the Earth magnetic flux density, BEy = 0  y component of the Earth magnetic flux density, BEz – z component of the Earth magnetic flux density, I – inclination of the Earth magnetic field.

• Description of symmetrical prolate ellipsoid magnetic signature parameters-Be = 50 mT, I = 70 deg, z = 200 m, q = 90 deg, j = 45 deg, a =4 m, e = 8, mr = 100

  Open Research Data

  open access

  • M. Wołoszyn
  • K. Pankowska

  - series: magnetic signatures

  The Earth magnetic field (Fig.1): BE – total magnetic flux density, BEx – x component of the Earth magnetic flux density, BEy = 0  y component of the Earth magnetic flux density, BEz – z component of the Earth magnetic flux density, I – inclination of the Earth magnetic field.

• Description of symmetrical prolate ellipsoid magnetic signature parameters-Be = 50 mT, I = 70 deg, z = 20 m, q = 90 deg, j = 135 deg, a =4 m, e = 1, mr = 100

  Open Research Data

  open access

  • M. Wołoszyn
  • K. Pankowska

  - series: magnetic signatures

  The Earth magnetic field (Fig.1): BE – total magnetic flux density, BEx – x component of the Earth magnetic flux density, BEy = 0  y component of the Earth magnetic flux density, BEz – z component of the Earth magnetic flux density, I – inclination of the Earth magnetic field.

• Description of symmetrical prolate ellipsoid magnetic signature parameters-Be = 50 mT, I = 70 deg, z = 10 m, q = 100 deg, j = 45 deg, a =4 m, e = 8, mr = 100

  Open Research Data

  open access

  • M. Wołoszyn
  • K. Pankowska

  - series: magnetic signatures

  The Earth magnetic field (Fig.1): BE – total magnetic flux density, BEx – x component of the Earth magnetic flux density, BEy = 0  y component of the Earth magnetic flux density, BEz – z component of the Earth magnetic flux density, I – inclination of the Earth magnetic field.

• Description of symmetrical prolate ellipsoid magnetic signature parameters-Be = 50 mT, I = 70 deg, z = 100 m, q = 80 deg, j = 135 deg, a =4 m, e = 4, mr = 100

  Open Research Data

  open access

  • M. Wołoszyn
  • K. Pankowska

  - series: magnetic signatures

  The Earth magnetic field (Fig.1): BE – total magnetic flux density, BEx – x component of the Earth magnetic flux density, BEy = 0  y component of the Earth magnetic flux density, BEz – z component of the Earth magnetic flux density, I – inclination of the Earth magnetic field.

• Description of symmetrical prolate ellipsoid magnetic signature parameters-Be = 50 mT, I = 70 deg, z = 200 m, q = 80 deg, j = 135 deg, a =4 m, e = 1, mr = 100

  Open Research Data

  open access

  • M. Wołoszyn
  • K. Pankowska

  - series: magnetic signatures

  The Earth magnetic field (Fig.1): BE – total magnetic flux density, BEx – x component of the Earth magnetic flux density, BEy = 0  y component of the Earth magnetic flux density, BEz – z component of the Earth magnetic flux density, I – inclination of the Earth magnetic field.

• Description of symmetrical prolate ellipsoid magnetic signature parameters-Be = 50 mT, I = 70 deg, z = 100 m, q = 90 deg, j = 45 deg, a =4 m, e = 8, mr = 100

  Open Research Data

  open access

  • M. Wołoszyn
  • K. Pankowska

  - series: magnetic signatures

  The Earth magnetic field (Fig.1): BE – total magnetic flux density, BEx – x component of the Earth magnetic flux density, BEy = 0  y component of the Earth magnetic flux density, BEz – z component of the Earth magnetic flux density, I – inclination of the Earth magnetic field.

• Description of symmetrical prolate ellipsoid magnetic signature parameters-Be = 50 mT, I = 70 deg, z = 200 m, q = 90 deg, j = 135 deg, a =4 m, e = 1, mr = 100

  Open Research Data

  open access

  • M. Wołoszyn
  • K. Pankowska

  - series: magnetic signatures

  The Earth magnetic field (Fig.1): BE – total magnetic flux density, BEx – x component of the Earth magnetic flux density, BEy = 0  y component of the Earth magnetic flux density, BEz – z component of the Earth magnetic flux density, I – inclination of the Earth magnetic field.

• Description of symmetrical prolate ellipsoid magnetic signature parameters-Be = 50 mT, I = 70 deg, z = 10 m, q = 80 deg, j = 135 deg, a =4 m, e = 4, mr = 100

  Open Research Data

  open access

  • M. Wołoszyn
  • K. Pankowska

  - series: magnetic signatures

  The Earth magnetic field (Fig.1): BE – total magnetic flux density, BEx – x component of the Earth magnetic flux density, BEy = 0  y component of the Earth magnetic flux density, BEz – z component of the Earth magnetic flux density, I – inclination of the Earth magnetic field.

• Description of symmetrical prolate ellipsoid magnetic signature parameters-Be = 50 mT, I = 70 deg, z = 20 m, q = 90 deg, j = 45 deg, a =4 m, e = 8, mr = 100

  Open Research Data

  open access

  • M. Wołoszyn
  • K. Pankowska

  - series: magnetic signatures

  The Earth magnetic field (Fig.1): BE – total magnetic flux density, BEx – x component of the Earth magnetic flux density, BEy = 0  y component of the Earth magnetic flux density, BEz – z component of the Earth magnetic flux density, I – inclination of the Earth magnetic field.

• Kaizen concept in the process of a quality improvement in the company

  Publication

  • M. Jakubiec
  • E. Brodnicka

  - Przedsiębiorstwo we współczesnej gospodarce - teoria i praktyka - Year 2016

  Artykuł dotyczy tematyki doskonalenia jakości, które może być realizowane w przedsiębiorstwie za pomocą koncepcji ciągłego doskonalenia Kaizen. Główny cel artykułu koncentruje się na analizie praktycznego zastosowania koncepcji Kaizen w celu eliminacji marnotrawstwa i ciągłego doskonalenia obszarów działalności przedsiębiorstwa. Rozdział został podzielony na dwie części: teoretyczną i poznawczą. W pierwszej, teoretycznej części,...

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• Sensitivity of the Baltic Sea level prediction to spatial model resolution

  Publication

  • M. Kowalewski

  - Year 2017

  he three-dimensional hydrodynamic model of the Baltic Sea (M3D) and...

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• Linezolid-resistant Enterococcus faecium strains isolated from one hospital in Poland –commensals or hospital-adapted pathogens?

  Publication

  • B. Krawczyk
  • M. Wysocka
  • R. Kotlowski
  • M. Bronk
  • M. Michalik
  • A. Samet

  - PLOS ONE - Year 2020

  One of the most pressing problems of enterococci infections is occurring resistance to linezolid, which is an antibiotic used in the treatment of infections caused by vancomycin-resistant strains (VRE). The main objective of our research was to investigate the relationship of 19 linezolid-resistant E. faecium isolates from 18 patients hospitalized at Clinical Hospital in Gdansk (Poland). One of the LZDREF was isolated in 2003...

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• Fuzzy soft modeling of environmental data. A study of the impact of a Phosphatic Fertilizer Plant on the adjacent environment in Gdańsk

  Publication

  • C. Sarbu
  • K. Szczepaniak
  • A. Astel
  • M. Biziuk

  - Year 2005

  Analiza podobieństwa obejmuje nie tylko zastosowanie logiki rozmytej, ale również wiele innych podejść matematycznych. Opracowano wiele algorytmów, których celem jest wyodrębnienie wyraźnych skupień (hard clusters) z danego zbioru danych. Prawdopodobnie najczęściej stosowanymi algorytmami są tzw. algorytmy c-średnie (c-means algorithms). Twarde c-średnie (hard c-means) służy do ostrej klasyfikacji, podczas której obiekt jest przypisany...

• Study on the Positioning Accuracy of GNSS/INS Systems Supported by DGPS and RTK Receivers for Hydrographic Surveys

  Publication

  • A. Stateczny
  • C. Specht
  • M. Specht
  • D. Brčić
  • A. Jugović
  • S. Widźgowski
  • M. Wiśniewska
  • O. Lewicka

  - ENERGIES - Year 2021

  Hydrographic surveys, in accordance with the International Hydrographic Organization (IHO) S-44 standard, can be carried out in the following five orders: Exclusive, Special, 1a, 1b and 2, for which minimum accuracy requirements for the applied positioning system have been set out. They are as follows, respectively: 1, 2, 5, 5 and 20 m, with a confidence level of 95% in twodimensional space. The Global Navigation Satellite System...

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• Rhythm and Colours of the Angles

  Publication

  • K. Wróblewski

  - Year 2018

  ABSTRACT The game of space was and still is a crucial aspect of visual arts. The aim of this study is to examine how the arrangement of hues, rhythms and angles of various polygons can create an impression of depth and movement on a flat surface. The so-called Penrose tiling and Ulam's spiral are mathematical models that have been applied for the painting experiment. There is a vast amount of evidence gathered over the ages that...

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• A new model of fuel spray shape at early stage of injection in a marine Diesel engine

  Publication

  • J. Grochowalska
  • P. Jaworski
  • Ł. J. Kapusta
  • J. Kowalski

  - INTERNATIONAL JOURNAL OF NUMERICAL METHODS FOR HEAT & FLUID FLOW - Year 2022

  In the cylinders of a marine diesel engine, self-ignition occurs in very shortly time after the fuel injection into the combustion chamber. Therefore, the paper present was to develop a model of diesel fuel spray for the early stage of fuel spray for in marine diesel engine. There were taken into consideration the main aspects technical such as nozzle diameter of marine engine injector and backpressure in combustion chamber. In...

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• Mercury in suspended matter of the Gulf of Gdańsk: Origin, distribution and transport at the land–sea interface

  Publication

  • A. Jedruch
  • U. Kwasigroch
  • M. Bełdowska
  • K. Kuliński

  - MARINE POLLUTION BULLETIN - Year 2017

  The coastal regions of inland seas are particularly vulnerable to Hg pollution. An important carrier of toxic Hg in the marine environment is suspended matter originating from multiple sources. The present study was conducted in the Gulf...

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• Networkig activities of general judiciary - from theory to practice

  Publication

  • P. Banasik
  • S. Morawska
  • M. Odlanicka-Poczobutt

  - e-mentor - Year 2018

  Over the last three decades, networks - as a field of research - have acquired a significant place among management sciences. Unfortunately, in the judiciary they have become a subject of more careful analyses only recently, which resulted in a large discrepancy of knowledge - both in theory and in its practical adaptation for the needs of the courts. In order to fill this cognitive gap, an attempt was made to identify levels of...

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• Environmental Role of Rime Chemistry at Selected Mountain Sites in Poland

  Publication

  • M. Godek
  • M. Błaś
  • M. Sobik
  • Ż. Polkowska
  • K. Cichała-Kamrowska
  • J. Namieśnik

  - PURE AND APPLIED GEOPHYSICS - Year 2012

  The results of field experiments on fog pollutantdeposition enhanced by local mountain climate, completed by thedendrochronological analysis of the forest response, are presentedin this paper. In spite of their low absolute altitude (1,000-1,600 ma.s.l), the Sudetes and the Silesian Beskid form a noticeable orographicbarrier for the airflow of the humid Atlantic air masses.This results in the increase of cloudiness and fog frequency...

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• Improving Thermal Insulation Properties for Prefabricated Wall Components Made of Lightweight Aggregate Concrete with Open Structure

  Publication

  • M. Abramski

  - Year 2017

  Porous concrete is commonly used in civil engineering due to its good thermal insulation properties in comparison with normal concrete and high compression strength in comparison with other building materials. An extremely porous concrete, called ‘lightweight aggregate concrete with open structure’ (LAC), is used in some German plants to produce prefabricated wall components. They are used mainly in hall buildings, e.g. supermarkets....

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• Permanent traffic counting stations - Expressway S6 in Gdansk (dataset containing 5-min aggregated traffic data and weather information)

  Open Research Data

  open access

  • A. Romanowska
  • W. Kustra

  The data includes traffic data from permanent traffic count station located on the expressway S6 in the Tri-City Agglomeration area in Poland. The data covers the three year period between 2014 and 2017 and one direction of traffic (southbound). 

• Sounding rocket temperature and heat transfer data

  Open Research Data

  open access

  • A. Dąbrowski

  This dataset contains temperature and heat transfer data measured during REXUS 25 sounding rocket HEDGEHOG Experiment launched from Esrange Space Centre, Kiruna, Sweden. For experiment details, please see:

• POSZUKIWANIE RELACJI DIAGNOSTYCZNYCH POMIĘDZY USZKODZENIAMI W KANALE SPALIN WYLOTOWYCH SILNIKA O ZS A SZYBKOZMIENNĄ TEMPERATURĄ SPALIN

  Publication

  • P. Puzdrowska

  - Journal of Polish CIMEEAC - Year 2019

  Temperatura spalin wylotowych tłokowego silnika spalinowego o zapłonie samoczynnym, mierzona w charakterystycznych przekrojach kontrolnych jego układu cieplno-przepływowego, może stanowić cenne źródło informacji diagnostycznej o stanie technicznym elementów ograniczających wydzielone w ten sposób przestrzenie robocze, wraz z układem turbodoładowania, ale także jego układu zasilania paliwem i wymiany czynnika roboczego. W standardowych...

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• Procesy i efektywność usuwania zanieczyszczeń z odcieków ze składowisk odpadów komunalnych w oczyszczalniach hydrofitowych

  Publication

  • E. Wojciechowska

  - Year 2013

  Oczyszczanie odcieków z SOK jest jednym z najbardziej istotnych problemów ekologicznych na świecie. Odprowadzenie odcieków do oczyszczalni ścieków komunalnych jest przeważnie niemożliwe, ze względu na ich zmienną ilość oraz skład, bardzo wysokie stężenia ChZT i azotu amonowego, a także obecność trwałych zanieczyszczeń organicznych (TZO) oraz metali ciężkich. Najlepszym rozwiązaniem jest oczyszczanie wód odciekowych na terenie składowiska....

• Atrial Fibrillation (AFIB) in the ICU: Incidence, Risk Factors, and Outcomes: The International AFIB-ICU Cohort Study*

  Publication

  • M. Wetterslev
  • M. Hylander
  • A. Granholm
  • C. Hassager
  • N. Haase
  • T. Lange
  • S. Myatra
  • J. Hästbacka
  • Y. Arabi
  • J. Shen... and 37 others

  - CRITICAL CARE MEDICINE - Year 2023

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• Two years later: Is the SARS-CoV-2 pandemic still having an impact on emergency surgery? An international cross-sectional survey among WSES members

  Publication

  • M. Reichert
  • M. Sartelli
  • M. Weigand
  • M. Hecker
  • P. Oppelt
  • J. Noll
  • I. Askevold
  • J. Liese
  • W. Padberg
  • F. Coccolini... and 357 others

  - World Journal of Emergency Surgery - Year 2022

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• Correction to: Two years later: Is the SARS-CoV-2 pandemic still having an impact on emergency surgery? An international cross-sectional survey among WSES members

  Publication

  • M. Reichert
  • M. Sartelli
  • M. Weigand
  • M. Hecker
  • P. Oppelt
  • J. Noll
  • I. Askevold
  • J. Liese
  • W. Padberg
  • F. Coccolini... and 357 others

  - World Journal of Emergency Surgery - Year 2022

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• 40th EASD Annual Meeting of the European Association for the Study of Diabetes

  Publication

  • M. Veitenhansl
  • K. Stegner
  • F. Hierl
  • C. Dieterle
  • H. Feldmeier
  • B. Gutt
  • R. Landgraf
  • A. Garrow
  • L. Vileikyte
  • A. Findlow... and 5202 others

  - DIABETOLOGIA - Year 2004

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