8 results on '"Mc Ginnity, P."'
Search Results
2. Editorial: Natural and artificial radionuclides as tracers of ocean processes
- Author
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Jixin Qiao, Núria Casacuberta, and Paul MC. Ginnity
- Subjects
ocean processes ,ocean dynamics ,natural and anthropogenic radioisotopes ,radioactive sources ,radiotracer applications ,data portals ,Science ,General. Including nature conservation, geographical distribution ,QH1-199.5 - Published
- 2023
- Full Text
- View/download PDF
3. Treated Choroidal Melanoma with Late Metastases to the Contralateral Orbit
- Author
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Sonia George, Carole A. Cooke, Gerald F. Mc Ginnity, Steve White, and Laksmi Venkatraman
- Subjects
Pathology ,RB1-214 - Abstract
Choroidal melanoma is the commonest adult primary intraocular tumour, 1 and usual sites of secondary spread are to liver, bone and lung. Although delayed recurrence of ipsilateral orbital melanoma is well documented, metastasis to the contralateral orbit is a rarely encountered phenomenon. We describe a case of metastatic spread to the contralateral orbit in a patient 12 years after proton beam radiotherapy of choroidal melanoma.
- Published
- 2009
- Full Text
- View/download PDF
4. Tracking of Airborne Radionuclides from the Damaged Fukushima Dai-Ichi Nuclear Reactors by European Networks
- Author
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Masson, O., Baeza, A., Bieringer, J., Brudecki, K., Bucci, S., Cappai, M., Carvalho, F.P., Connan, O., Cosma, C., Dalheimer, A., Didier, D., Depuydt, G., De Geer, L.E., De Vismes, A., Gini, L., Groppi, F., Gudnason, K., Gurriaran, R., Hainz, D., Halldórsson, Ó., Hammond, D., Hanley, O., Holeý, K., Homoki, Zs., Ioannidou, A., Isajenko, K., Jankovic, M., Katzlberger, C., Kettunen, M., Kierepko, R., Kontro, R., Kwakman, P.J.M., Lecomte, M., Leon Vintro, L., Leppänen, A.-P., Lind, B., Lujaniene, G., Mc Ginnity, P., Mahon, C. Mc, Malá, H., Manenti, S., Manolopoulou, M., Mattila, A., Mauring, A., Mietelski, J.W., Møller, B., Nielsen, Sven Poul, Nikolic, J., Overwater, R.M.W., Pálsson, S. E., Papastefanou, C., Penev, I., Pham, M.K., Povinec, P.P., Ramebäck, H., Reis, M.C., Ringer, W., Rodriguez, A., Rulík, P., Saey, P.R.J., Samsonov, V., Schlosser, C., Sgorbati, G., Silobritiene, B. V., Söderström, C., Sogni, R., Solier, L., Sonck, M., Steinhauser, G., Steinkopff, T., Steinmann, P., Stoulos, S., Sýkora, I., Todorovic, D., Tooloutalaie, N., Tositti, L., Tschiersch, J., Ugron, A., Vagena, E., Vargas, A., Wershofen, H., Zhukova, O., Masson, O., Baeza, A., Bieringer, J., Brudecki, K., Bucci, S., Cappai, M., Carvalho, F.P., Connan, O., Cosma, C., Dalheimer, A., Didier, D., Depuydt, G., De Geer, L.E., De Vismes, A., Gini, L., Groppi, F., Gudnason, K., Gurriaran, R., Hainz, D., Halldórsson, Ó., Hammond, D., Hanley, O., Holeý, K., Homoki, Zs., Ioannidou, A., Isajenko, K., Jankovic, M., Katzlberger, C., Kettunen, M., Kierepko, R., Kontro, R., Kwakman, P.J.M., Lecomte, M., Leon Vintro, L., Leppänen, A.-P., Lind, B., Lujaniene, G., Mc Ginnity, P., Mahon, C. Mc, Malá, H., Manenti, S., Manolopoulou, M., Mattila, A., Mauring, A., Mietelski, J.W., Møller, B., Nielsen, Sven Poul, Nikolic, J., Overwater, R.M.W., Pálsson, S. E., Papastefanou, C., Penev, I., Pham, M.K., Povinec, P.P., Ramebäck, H., Reis, M.C., Ringer, W., Rodriguez, A., Rulík, P., Saey, P.R.J., Samsonov, V., Schlosser, C., Sgorbati, G., Silobritiene, B. V., Söderström, C., Sogni, R., Solier, L., Sonck, M., Steinhauser, G., Steinkopff, T., Steinmann, P., Stoulos, S., Sýkora, I., Todorovic, D., Tooloutalaie, N., Tositti, L., Tschiersch, J., Ugron, A., Vagena, E., Vargas, A., Wershofen, H., and Zhukova, O.
- Abstract
Radioactive emissions into the atmosphere from the damaged reactors of the Fukushima Dai-ichi nuclear power plant (NPP) started on March 12th, 2011. Among the various radionuclides released, iodine-131 (131I) and cesium isotopes (137Cs and 134Cs) were transported across the Pacific toward the North American continent and reached Europe despite dispersion and washout along the route of the contaminated air masses. In Europe, the first signs of the releases were detected 7 days later while the first peak of activity level was observed between March 28th and March 30th. Time variations over a 20-day period and spatial variations across more than 150 sampling locations in Europe made it possible to characterize the contaminated air masses. After the Chernobyl accident, only a few measurements of the gaseous 131I fraction were conducted compared to the number of measurements for the particulate fraction. Several studies had already pointed out the importance of the gaseous 131I and the large underestimation of the total 131I airborne activity level, and subsequent calculations of inhalation dose, if neglected. The measurements made across Europe following the releases from the Fukushima NPP reactors have provided a significant amount of new data on the ratio of the gaseous 131I fraction to total 131I, both on a spatial scale and its temporal variation. It can be pointed out that during the Fukushima event, the 134Cs to 137Cs ratio proved to be different from that observed after the Chernobyl accident. The data set provided in this paper is the most comprehensive survey of the main relevant airborne radionuclides from the Fukushima reactors, measured across Europe. A rough estimate of the total 131I inventory that has passed over Europe during this period was
- Published
- 2011
5. Tracking of Airborne Radionuclides from the Damaged Fukushima Dai-Ichi Nuclear Reactors by European Networks
- Author
-
Masson, Olivier, Baeza, A., Bieringer, Jacqueline, Brudecki, K., Bucci, S., Cappai, M., Carvalho, F. P., Connan, O., Cosma, C., Dalheimer, Axel, Didier, D., Depuydt, G., De Geer, L. E., De Vismes, Anne, Gini, L., Groppi, F., Gudnason, K., Gurriaran, R., Hainz, D., Halldorsson, O., Hammond, D., Hanley, O., Holey, K., Homoki, Zsolt, Ioannidou, A., Isajenko, Krzysztof A., Janković, Marija M., Katzlberger, Christian, Kettunen, M., Kierepko, Renata, Kontro, R., Kwakman, P. J. M., Lecomte, M., Vintro, L. Leon, Leppanen, A-P, Lind, B., Lujaniene, G., Mc Ginnity, P., Mc Mahon, C., Mala, Helena, Manenti, S., Manolopoulou, M., Mattila, A., Mauring, A., Mietelski, Jerzy W., Moller, Bredo, Nielsen, S. P., Krneta-Nikolić, Jelena D., Overwater, R. M. W., Palsson, S. E., Papastefanou, C., Penev, I., Pham, M. K., Povinec, Pavel Peter, Rameback, H., Reis, M. C., Ringer, Wolfgang, Rodriguez, A., Rulik, Petr, Saey, P. R. J., Samsonov, V., Schlosser, C., Sgorbati, G., Silobritiene, B. V., Soderstrom, C., Sogni, R., Solier, L., Sonck, M., Steinhauser, Georg, Steinkopff, Thomas, Steinmann, P., Stoulos, S., Sykora, Ivan, Todorović, Dragana, Tooloutalaie, N., Tositti, L., Tschiersch, Jochen, Ugron, A., Vagena, E., Vargas, A., Wershofen, Herbert, Zhukova, O., Masson, Olivier, Baeza, A., Bieringer, Jacqueline, Brudecki, K., Bucci, S., Cappai, M., Carvalho, F. P., Connan, O., Cosma, C., Dalheimer, Axel, Didier, D., Depuydt, G., De Geer, L. E., De Vismes, Anne, Gini, L., Groppi, F., Gudnason, K., Gurriaran, R., Hainz, D., Halldorsson, O., Hammond, D., Hanley, O., Holey, K., Homoki, Zsolt, Ioannidou, A., Isajenko, Krzysztof A., Janković, Marija M., Katzlberger, Christian, Kettunen, M., Kierepko, Renata, Kontro, R., Kwakman, P. J. M., Lecomte, M., Vintro, L. Leon, Leppanen, A-P, Lind, B., Lujaniene, G., Mc Ginnity, P., Mc Mahon, C., Mala, Helena, Manenti, S., Manolopoulou, M., Mattila, A., Mauring, A., Mietelski, Jerzy W., Moller, Bredo, Nielsen, S. P., Krneta-Nikolić, Jelena D., Overwater, R. M. W., Palsson, S. E., Papastefanou, C., Penev, I., Pham, M. K., Povinec, Pavel Peter, Rameback, H., Reis, M. C., Ringer, Wolfgang, Rodriguez, A., Rulik, Petr, Saey, P. R. J., Samsonov, V., Schlosser, C., Sgorbati, G., Silobritiene, B. V., Soderstrom, C., Sogni, R., Solier, L., Sonck, M., Steinhauser, Georg, Steinkopff, Thomas, Steinmann, P., Stoulos, S., Sykora, Ivan, Todorović, Dragana, Tooloutalaie, N., Tositti, L., Tschiersch, Jochen, Ugron, A., Vagena, E., Vargas, A., Wershofen, Herbert, and Zhukova, O.
- Abstract
Radioactive emissions into the atmosphere from the damaged reactors of the Fukushima Dai-ichi nuclear power plant (NPP) started on March 12th, 2011. Among the various radionuclides released, iodine-131 ((131)I) and cesium isotopes ((137)Cs and (134)Cs) were transported across the Pacific toward the North American continent and reached Europe despite dispersion and washout along the route of the contaminated air masses. In Europe, the first signs of the releases were detected 7 days later while the first peak of activity level was observed between March 28th and March 30th. Time variations over a 20-day period and spatial variations across more than 150 sampling locations in Europe made it possible to characterize the contaminated air masses. After the Chernobyl accident, only a few measurements of the gaseous (131)I fraction were conducted compared to the number of measurements for the particulate fraction. Several studies had already pointed out the importance of the gaseous (131)I and the large underestimation of the total (131)I airborne activity level, and subsequent calculations of inhalation dose, if neglected. The measurements made across Europe following the releases from the Fukushima NPP reactors have provided a significant amount of new data on the ratio of the gaseous (131)I fraction to total (131)I, both on a spatial scale and its temporal variation. It can be pointed out that during the Fukushima event, the (134)Cs to (137)Cs ratio proved to be different from that observed after the Chernobyl accident. The data set provided in this paper is the most comprehensive survey of the main relevant airborne radionuclides from the Fukushima reactors, measured across Europe. A rough estimate of the total (131)I inventory that has passed over Europe during this period was LT 1% of the released amount. According to the measurements, airborne activity levels remain of no concern for public health in Europe.
- Published
- 2011
6. Tracking of Airborne Radionuclides from the Damaged Fukushima Dai-Ichi Nuclear Reactors by European Networks
- Author
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Masson, O., primary, Baeza, A., additional, Bieringer, J., additional, Brudecki, K., additional, Bucci, S., additional, Cappai, M., additional, Carvalho, F.P., additional, Connan, O., additional, Cosma, C., additional, Dalheimer, A., additional, Didier, D., additional, Depuydt, G., additional, De Geer, L.E., additional, De Vismes, A., additional, Gini, L., additional, Groppi, F., additional, Gudnason, K., additional, Gurriaran, R., additional, Hainz, D., additional, Halldórsson, Ó., additional, Hammond, D., additional, Hanley, O., additional, Holeý, K., additional, Homoki, Zs., additional, Ioannidou, A., additional, Isajenko, K., additional, Jankovic, M., additional, Katzlberger, C., additional, Kettunen, M., additional, Kierepko, R., additional, Kontro, R., additional, Kwakman, P.J.M., additional, Lecomte, M., additional, Leon Vintro, L., additional, Leppänen, A.-P., additional, Lind, B., additional, Lujaniene, G., additional, Mc Ginnity, P., additional, Mahon, C. Mc, additional, Malá, H., additional, Manenti, S., additional, Manolopoulou, M., additional, Mattila, A., additional, Mauring, A., additional, Mietelski, J.W., additional, Møller, B., additional, Nielsen, S.P., additional, Nikolic, J., additional, Overwater, R.M.W., additional, Pálsson, S. E., additional, Papastefanou, C., additional, Penev, I., additional, Pham, M.K., additional, Povinec, P.P., additional, Ramebäck, H., additional, Reis, M.C., additional, Ringer, W., additional, Rodriguez, A., additional, Rulík, P., additional, Saey, P.R.J., additional, Samsonov, V., additional, Schlosser, C., additional, Sgorbati, G., additional, Silobritiene, B. V., additional, Söderström, C., additional, Sogni, R., additional, Solier, L., additional, Sonck, M., additional, Steinhauser, G., additional, Steinkopff, T., additional, Steinmann, P., additional, Stoulos, S., additional, Sýkora, I., additional, Todorovic, D., additional, Tooloutalaie, N., additional, Tositti, L., additional, Tschiersch, J., additional, Ugron, A., additional, Vagena, E., additional, Vargas, A., additional, Wershofen, H., additional, and Zhukova, O., additional
- Published
- 2011
- Full Text
- View/download PDF
7. Margueritte S. Murphy, Material Figures: Political Economy, Commercial Culture, and the Aesthetic Sensibility of Charles Baudelaire
- Author
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Mc Ginnity, Orla
- Published
- 2015
- Full Text
- View/download PDF
8. Seafood dose parameters: Updating 210 Po retention factors for cooking, decay loss and mariculture.
- Author
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Johansen MP, Carpenter JG, Charmasson S, Gwynn JP, Mc Ginnity P, Mori A, Orr B, Simon-Cornu M, and Osvath I
- Subjects
- Animals, Humans, Seafood analysis, Cooking, Fishes, Crustacea, Radiation Monitoring, Polonium analysis
- Abstract
210 Po has been identified as one of the main contributors to ingestion doses to humans, particularly from the consumption of seafood. The amount of210 Po activity concentration data for various types of seafood has increased greatly in recent times. However, to provide realistic seafood dose assessments, most210 Po data requires correction to account for losses that can occur before the seafood is actually consumed. Here we develop generic correction factors for the main processes associated with reduction of210 Po in seafood - leaching during cooking, radioactive decay between harvest and consumption, and sourcing from mariculture versus wild-caught. When seafood is cooked, the overall mean fraction of210 Po retained is 0.74 for all cooking and seafood types, with the means for various seafood types and cooking categories ranging from 0.56 to 1.03. When considering radioactive decay during the period between harvest and consumption, the overall mean fraction remaining is 0.81 across all seafood preservation/packaging types, with estimates ranging from 0.50 (canned seafood) to 0.98 (fresh seafood). Regarding mariculture influence, the available limited data suggest marine fish and crustaceans raised with processed feed have about one order of magnitude lower (×0.10)210 Po muscle content than wild-caught seafood of the same or similar species, although this ratio varies. Overall, this study concludes that210 Po activity concentrations in seafood at the time of ingestion may be reduced to only about 55% compared to when it was harvested. Therefore, correction factors must be applied to any data derived from environmental monitoring in order to achieve realistic dose estimates. The data also suggest lower210 Po ingestion doses for consumers who routinely favour cooked, long shelf-life and farmed fish/crustaceans. However, more data is needed in some categories, especially for cooking of molluscs and seaweed, and for the210 Po content in all farmed seafood., Competing Interests: Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper., (Crown Copyright © 2023. Published by Elsevier Ltd. All rights reserved.)- Published
- 2023
- Full Text
- View/download PDF
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