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CT结肠成像扁平息肉表面的对比剂涂层:病变的检出标记

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国际医学放射学杂志 2014年第3期 305-306页

作者： D.H.Kim j.L.Hinshaw M.G.Lubner A.Munoz del rio B.D.Pooler P.j.Pickhardt 唐光健 Department of Radiology University of Wisconsin Medical SchoolE3/311 Clinical Science Center 600 Highland Ave.MadisonWI 53792-3252USA

摘要目的评价扁平息肉在口服对比剂时涂层的出现率,此征象可能提高病变的检出,成为CT结肠成像(CTC)筛查的影响因素。方法本回顾性观察研究于单一机构内进行。

关键词：扁平息肉结肠成像涂层检出对比剂病变 CT

Zircon chemistry and new laser ablation U–Pb ages for uraniferous granitoids in SW Cameroon

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Acta Geochimica 2020年第1期39卷 43-66页

作者： V.F.Embui C.E.Suh j.M.Cottle j.Etame j.Mendes C.M.Agyingi A.Vishiti E.M.Shemang B.Lehmann Department of Geology University of BueaP.O.Box 63BueaSouth West RegionCameroon Ore Treatment Laboratory Institute of Geological and Mining Research(IRGM)P.O.Box 4110YaoundeNlongkakCameroon Department of Geology Mining and Environmental ScienceUniversity of BamendaP.O.Box 39BambiliCameroon Department of Earth Sciences and Earth Research Institute Webb Hall 2028University of CaliforniaSanta BarbaraCA 93106-9630USA Laboratory of Geosciences Natural resources and Environment Department of Earth SciencesFaculty of ScienceUniversity of DoualaP.O.Box 24157DoualaCameroon Department of Civil Engineering University Institute of TechnologyUniversity of DoualaP.O.Box 8698DoualaCameroon Departamento de Geologia IGEOUniversidade Federal do Rio de JaneiroCidade UniversitariaRio de Janeiro 21910-949Brazil Department of Earth and Environmental Sciences Botswana International University of Science and TechnologyPrivate Bag 16PalapyeBotswana Mineral Resources Technical University of ClausthalClausihal-ZellerfeldGermany

The Ekomedion two-mica granite,southwestern Cameroon,has potential for uranium and molybdenum ***,we present LA-ICP-MS U-Pb ages,Lu-Hf isotope characteristics,trace element concentrations and Ti-geothermometry of zircon from this granite hosting U-Mo mineralization in pegmatitic *** majority of zircon are CL-dark though some CL-bright cores were also identified.U-Pb zircon age data range from 121±3 to743±11 Ma with only 5 of 34 ages being near *** concordant mean age of 603±12 Ma is similar to ages of granitic intrusions along the Central African Shear Zone in *** ages with mean of261±6 Ma reveal open system behavior with respect to Pb and/or *** e Hfi values range from-20.3 *** implies that U-Mo was remobilized during partial melting of the surrounding *** Th/U>0.1 as well as an increasing Hf with decreasing Th/U indicates that fractional crystallization was the main factor that controlled U-Mo mineralization in pegmatitic pods.Y and Y/Ho ratios cluster from 29 to 33 close to the chondritic ratio of 28 and indicate fractionation of Y and Ho with low F contents during the earliest stages of *** stage accumulation of F-rich magmatic-hydrothermal fluids impacted U-Mo mineralization as a *** contains a prominent negative Eu anomaly pointing to a fractionating system rich in *** Ti-in-zircon temperatures span 672℃to1232℃with the temperatures at the high end reflecting interference from mineral inclusions in the zircon grains while the lower temperature values are linked to crystallization.

关键词： Zircons Uranium-molybdenum Cameroon

What a few hairs can tell us about the resource use of giant armadillos

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Integrative Zoology 2023年第1期18卷 129-142页

作者： Marcelo MAGIOLI Nina ATTIAS Gabriel MASSOCATO Danilo KLUYBER Marcelo Zacharias MOREIRA Katia Maria Paschoaletto Micchi de Barros FERRAZ Adriano Garcia CHIARELLO Arnaud L.j.DESBIEZ Instituto Pró-Carnívoros AtibaiaSão PauloBrazil Centro Nacional de Pesquisa e Conservação de Mamíferos Carnívoros(CENAP) Instituto Chico Mendes de Conservação da Biodiversidade(ICMBio)AtibaiaSão PauloBrazil Instituto de Conservação de Animais Silvestres(ICAS) Campo GrandeMato Grosso do SulBrazil Instituto de Pesquisas Ecológicas Organização Não GovernamentalNazaréPaulistaSão PauloBrazil Houston Zoo HoustonTexasUSA Naples Zoo at Caribbean Gardens NaplesFloridaUSA Laboratório de Ecologia Isotópica Centro de Energia Nuclear na AgriculturaUniversidade de São PauloPiracicabaSão PauloBrazil Laboratório de Ecologia Manejo e Conservação de Fauna Silvestre(LEMaC)Departamento de Ciências FlorestaisEscola Superior de Agricultura“Luiz de Queiroz”(ESALQ)Universidade de São Paulo(USP)PiracicabaSão PauloBrazil Departamento de Biologia Faculdade de FilosofiaCiências e LetrasUniversidade de São Paulo(USP)Ribeirão PretoSão PauloBrazil RZSS-Royal Zoological Society of Scotland(RZSS) MurrayfieldEdinburghUK

Understanding of resource requirements of vulnerable species is key for conservation ***,we used sta-ble carbon(δ13C)and nitrogen isotopes(δ15N)of hair from giant armadillos(Priodontes maximus)to understand individual resource *** collected hair from 19 giant armadillos analyzing 34 samples from the Brazilian Pan-tanal and compared the resource use between sexes and age *** also assessed the relationship of isotopic values with individuals’body mass and the habitat type *** observed a wide variation in resource use by giant armadillos,showing that individuals consume prey that feeds on distinct resources and occupies different habitat types,indicating that there is individual variation in foraging *** giant armadillos presented a mixed diet(C3/C4 resources,forests/open areas),but a quarter of individuals had strictly C4 diets(open areas).Males are more prone to forage on C4 resources,presenting an isotopic niche 2.6-times larger than that of *** presented diets more associated with habitats with high arboreal cover(C3 resources,forests),while adults foraged more in open areas(C4 resources).This result is mirrored by the positive relationship betweenδ13C values and body mass,suggesting that larger giant armadillos tend to feed more in open *** observed thatδ13C values decreased as individuals increased the use of habitats with high arboreal *** stress the importance of con-serving the natural mosaic in the Pantanal landscape for the species persistence,given that giant armadillos require all habitat types to fulﬁll their dietary,spatial,and developmental needs.

关键词： diet ontogenetic changes resource partitioning stable isotopes telemetry

Acute hepatitis with autoimmune features after COVID-19 vaccine:coincidence or vaccine-induced phenomenon?

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Gastroenterology Report 2022年第1期10卷 628-631页

作者： jose M.Pinazo-Bandera Alicia Hernandez-Albujar Ana Isabel Garcia-Salguero Isabel Arranz-Salas Raul j.Andrade Mercedes Robles-Diaz Division of Gastroenterology and Hepatology Instituto de Investigacion Biomedica de Malaga-IBIMAHospital Universitario Virgen de la VictoriaUniversidad de MalagaMalagaSpain Division of Anatomical Pathology Hospital Universitario Virgen de la VictoriaMalagaSpain Centro de Investigacion Biomedica en Red de Enfermedades Hepaticas y Digestivas(CIBERehd) MadridSpain

Introduction Autoimmune diseases result from a breach of immunological self-tolerance and tissue damage by autoreactive T *** acute respiratory syndrome coronavirus-2(SARS-CoV-2)infection is characterized by an inflam... 详细信息

关键词： autoimmune vaccine acute

Impact of nitrogen doping on growth and hydrogen impurity incorporation of thick nanocrystalline diamond films

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Chinese Physics B 2011年第5期20卷 433-438页

作者：顾利萍唐春玖江学范 j.L.Pinto Department of Physics Jiangsu Key Laboratory for Advanced Functional MaterialsChangshu Institute of Technology Department of Physics I3N(Institute for NanostructuresNanomodelling and Nanofabrication)University of AveiroCampus Universita'rio de Santiago3810-193 AveiroPortugal

A much larger amount of bonded hydrogen was found in thick nanocrystalline diamond （NCD） films produced by only adding 0.24% N2 into 4% CH4/H2 plasma, as compared to the high quality transparent microcrystalline diamond （MCD） films, grown using the same growth parameters except for nitrogen. These experimental results clearly evidence that defect formation and impurity incorporation （for example, N and H） impeding diamond grain growth is the main formation mechanism of NCD upon nitrogen doping and strongly support the model proposed in the literature that nitrogen competes with CHx （x = 1, 2, 3） growth species for adsorption sites.

关键词： thick nanocrystalline diamond films nitrogen doping crystalline quality

A FINITE ELEMENT SOLVER FOR NAVIER-STOKES EQUATIONS VIA VORTICITY AND VELOCITY

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Transactions of Nanjing University of Aeronautics and Astronautics 2001年第Z1期18卷 115-118页

作者： Zhu jiang Abimael F D Loula Laboratório Nacional de Computaco Científica, MCT,Av Getúlio Vargas 333, 25651 070 Petrópolis, Rj, Brazil Laboratório Nacional de Computacao Cientifica MCTAy Getulio Vargas 333 25651-070 Petrópolis R J Brazil

The incompressible Navier Stokes equations are solved via variables of vorticity and velocity. Firstly, a rigorous variational framework with the equivalence between the velocity pressure and the vorticity velocity formulations is presented in a Lipschitz domain. Next, a class of Galerkin finite element approximations of the corresponding variational form is introduced, and a convergence analysis is given for the Stokes problem. Finally, an iterative finite element solver for the Navier Stokes problem is proposed.

关键词： incompressible Navier-Stokes equations vorticity-velocity formulation finite element approximations convergence analysis

Combined U-Pb SHRIMP and Hf isotope study of the Late Paleozoic Yaminue Complex,rio Negro Province,Argentina:Implications for the origin and evolution of the Patagonia composite terrane

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Geoscience Frontiers 2013年第1期4卷 37-56页

作者： Carlos j.Chernicoff Eduardo O.Zappettini joao O.S.Santos Neal j.McNaughton Elena Belousova National Scientific and Technical Research Council(CONICET) Argentina Argentine Geological-Mining Survey(SEGEMAR) Argentina Argentine Geological-Mining Survey(SEGEMAR).Argentina University of Western Australia PerthWA 6009Australia Redstone Resources.Perth.WA 6849.Australia john de Laeter Centre Curtin UniversityPerthWA 6102Australia ARC National Key Centre for Geochemical Evolution and Metallogeny of Continents(GEMOC) Macquarie UniversitySydneyNSW 2109Australia

We have carried out zircon U-Pb SHRIMP dating and Hf isotope determinations on a biotite paraschist and on a tonalitic orthogneiss of the Yaminué Complex, and re-evaluate this complex in the broader context of the tectonic evolution of the Patagonia composite terrane. In the metasedimentary unit （msuYC）, the youngest detrital zircon dated at 318 ± 5 Ma （Mississippian/Pennsylvanian boundary） indicates a Pennsylvanian （or younger） depositional age. The three main age populations peak at 474, 454 and 374 Ma. Preliminary Hf isotope data for two detrital zircons （447 and 655 Ma） yielded ε（Hf） values of -0.32 and 0.48, indicating that their primary sources contained small amounts of recycled crustal components （of Calymmian age; TDM 1.56 Ga）. Zircons from the orthogneiss （miuYC; intrusive into msuYC） show a crystallization age of 261.3 - 2.7 Ma （Capitanian; late middle Permian） which is broadly coeval with deformation, and Neoarchean-Paleoproterozoic inheritance. Meaningful core-rim relationship between Neoarchean zircon cores and late Permian rims is well defined, indicating the occurrence of Archean crust in this sector of Patagonia. Hf TDM of Permian zircons is mainly Meso-Paleoarchean （2.97-3.35 Ga）, with highly negative e（Hf） values （ca, -33）. Hf TDM of inherited Neoarchean zircon cores is also Meso-Paleoarchean （3.14-3.45 Ga） but more juvenile （ε（Hf） = -0.3）. Hf isotopes reinforce the presence of unexposed ancient crust in this area. Combining geological and isotope data, as well as geophysical models, we identify the Yaminué Complex within the La Esperanza-Yaminué crustal block flanked by two other, distinct crustal blocks： the Eastern block which forms part of the Patagonia terrane sensu stricto, located in the eastern Patagonian region, and the Western block forming part of the Southern Patagonia terrane. Their origins and timing of amalgamation to form the Patagonia composite terrane are also discussed.

关键词： Yaminue Complex U-Pb SHRIMP geochronology Hf isotopes Tectonics North Patagonian Massif Argentina

Paleoproterozoic juvenile magmatism within the northeastern sector of the Sao Francisco paleocontinent:Insights from the shoshonitic high Ba-Sr Montezuma granitoids

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Geoscience Frontiers 2020年第5期11卷 1821-1840页

作者： Samuel Moreira Bersan Alice Fernanda de Oliveira Costa Andre Danderfer Francisco Roberio de Abreu Cristiano Lana Glaucia Queiroga Craig Storey Hugo Moreira Universidade Federal de Ouro Preto Programa de Pos-graduacaoDepartamento de GeologiaCampus Morro do CruzeiroOuro PretoMGCEP 35400-000Brazil Universidade Federal de Ouro Preto Departamento de GeologiaCampus Morro do CruzeiroOuro PretoMGCEP 35400-000Brazil Sustain Geologia Ltda Teresa M.Valadares 503/502Belo HorizonteMGCEP 30575-160Brazil University of Portsmouth School of Earth and Environmental SciencesBurnaby BuildingBurnaby RoadPortsmouthPO13QLUK

New,integrated petrographic,mineral chemistry,whole rock geochemical,zircon and titanite UPb geochronology,and zircon Hf isotopic data from the Montezuma granitoids,as well as new geochemical results for its host rocks represented by the Corrego Tingui Complex,provides new insights into the late-to post-collisional evolution of the northeastern Sao Francisco paleocontinent.U-Pb zircon dates from the Montezuma granitoids spread along the Concordia between ca.2.2 Ga to 1.8 Ga and comprise distinct *** I have crystallization ages between ca.2.15 Ga and 2.05 Ga and are interpreted as inherited *** II zircon dates vary from 2.04 Ga to1.9 Ga and corresponds to the crystallization of the Montezuma granitoids,which were constrained at ca.2.03 Ga by the titanite U-Pb *** age zoning is common within the ca.1.8 Ga Group III zircon ages,being related to fluid isotopic re-setting during the Espinhaco rifiting ***εHf(t)analysis show dominantly positive values for both Group I(-4 to+9)andⅡ(-3 to+8)zircons and TDM2 model ages of 2.7-2.1 Ga and 2.5-1.95 Ga,***,the Montezuma granitoids are weakly peraluminous to metaluminous magnesian granitoids,enriched in LILES and LREE,with high to moderate Mg#and depleted in some of the *** lithochemical signature,added to the juvenile signature of both inherited and crystallized zircons,allowed its classification as a shoshonitic high Ba-Sr granitoid related to a late-to post-collisional lithosphere delamination followed by asthenospheric *** this scenario,the partial melting of the lithospheric mantle interacted with the roots of an accreted juvenile intra-oceanic arc,being these hybrid magma interpreted as the source of the Montezuma *** Corrego Tingui Complex host rocks are akin to a syn-to late-collisional volcanic arc granitoids originated from the partial melting of ancient crustal *** results presented in this study have revealed the occurrence of j

关键词： Zircon U–Pb-Hf Titanite U–Pb High Ba–Sr Late-to post-collisional Sao Francisco paleocontinent

Titanium Alloy Surface Modification by a Spatio-Temporal Atmospheric Pressure DBD Afterglow

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Plasma Science and Technology 2007年第6期9卷 670-673页

作者： E.PANOUSIS F.CLEMENT j.F.LOISEAU N.SPYROU B.HELD j.LARRIEU F.GUERTON Laboratory of Gas Electronics and Plasmas-Pau University 64000 PauFrance Electrotechnic Materials LaboratoryUniversity of Patras26500 Patras-RioGreece Laboratory of Gas Electronics and Plasmas-Pau University 64000 PauFrance Electrotechnic Materials Laboratory University of Patras26500 Patras-RioGreece Laboratoire Interdisciplinaire de Spectroscopie Electronique University of Namur5000 NamurBelgium

The experimental work reported here is devoted to the study of the modifications inflicted on the surface of titanium alloy specimens by an atmospheric pressure dielectric barrier discharge（DBD） reactor in both spatial and temporal afterglow conditions. A commercially available （AcXys Technologies） modified reactor system was used for the surface treatment of the TiA6V4 titanium alloy that is widely used in the aeronautical industry. Wettability surface characterisation and XPS analyses are performed to give a macroscopic and microscopic insight to the surface modifications. Best operating conditions, at constant input energy, were obtained for a duty cycle equal to 10%.

关键词： DBD titanium alloy atmospheric pressure