Conveners
Session 10 - Nuclear Microprobe Applications: Geology and Environmental Science
- Per Kristiansson (Lund University, Physics Department, Nuclear Physics)
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Mr Josef Buchriegler (Helmholtz-Zentrum Dresden-Rossendorf, Germany)11/07/2014, 09:00Invited Technical Oral CommunicationA new PIXE-beamline equipped with a full-field energy dispersive X-ray camera [1,2] has recently been put into operation at HZDR. This so-called SLcam® comprises poly-capillary optics guiding the proton-induced X-ray fluorescence radiation towards a 264×264 pixel pnCCD-chip, each with an energy resolution of 156 eV (@Mn Kα). Two X-ray optics are available, with a magnification of one and six,...Go to contribution page
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Mr Linus Ros (Division of Nuclear Physics, Department of Physics, Lund University, Sweden)11/07/2014, 09:30Oral CommunicationMany primitive meteorites show elevated D/H-ratios relative to terrestrial material. It is believed that this is due to the preservation of the organic molecules which were formed in the presolar molecular cloud [1]. The D/H-ratio varies considerably between different classes of meteorites. This isotopic variation is due to different degrees of mixing of the presolar material with solar system...Go to contribution page
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Dr Maciek Borysiuk (Division of Nuclear Physics, Department of Physics, Lund University, Sweden)11/07/2014, 09:50Oral CommunicationIsotopic fractionation of light elements such as carbon, oxygen and nitrogen is a basis of many analytical tools in hydrology, geology, paleobiology and paleogeology. The goal of the current experiment is to investigate if a nuclear microprobe could be utilized for those applications. Particularly we focus on measurement of oxygen isotopic ratio. The measurement of stable isotopes of oxygen...Go to contribution page
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Teresa Pinheiro (IBB, Instituto Superior Técnico, Universidade de Lisboa, Lisboa, Portugal)11/07/2014, 10:10Oral CommunicationStudies of phytoplankton elemental composition constitutes a direct measurement of environmental changes, allowing anticipating consequences of anthropogenic alterations to organisms, ecosystems and global marine geochemical cycles. Traditional bulk size-fractionation techniques used to measure phytoplankton elemental composition may present ambiguous results due to considerable detrital...Go to contribution page