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    <title>DSpace Collection:</title>
    <link>http://hdl.handle.net/2117/3954</link>
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        <rdf:li rdf:resource="http://hdl.handle.net/2117/7669" />
        <rdf:li rdf:resource="http://hdl.handle.net/2117/7648" />
        <rdf:li rdf:resource="http://hdl.handle.net/2117/7390" />
        <rdf:li rdf:resource="http://hdl.handle.net/2117/7314" />
        <rdf:li rdf:resource="http://hdl.handle.net/2117/7313" />
        <rdf:li rdf:resource="http://hdl.handle.net/2117/7309" />
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    <dc:date>2013-05-21T08:22:40Z</dc:date>
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  <item rdf:about="http://hdl.handle.net/2117/7669">
    <title>Comparison between PENELOPE and electron Monte Carlo simulations of electron fields used in the treatment of conjunctival lymphoma</title>
    <link>http://hdl.handle.net/2117/7669</link>
    <description>Title: Comparison between PENELOPE and electron Monte Carlo simulations of electron fields used in the treatment of conjunctival lymphoma
Authors: Brualla Barbera, Lorenzo; Palanco Zamora, R.; Witting, A.; Sempau Roma, Josep; Sauerwein, W.
Abstract: For the treatment of conjunctival lymphoma in the early stages, external beam radiotherapy offers a curative approach. Such treatment requires the use of highly conformed small radiation beams. The beam size is so small that even advanced treatment planning systems have difficulties in calculating dose distributions. One possible approach for optimizing the treatment technique and later performing treatment planning is by means of full Monte Carlo (MC) simulations. In this paper, we compare experimental absorbed dose profiles obtained with a collimator used at the University Hospital Essen, with MC simulations done with the general-purpose radiation transport code PENELOPE. The collimator is also simulated with the hybrid MC code electron Monte Carlo (eMC) implemented in the commercial treatment planning system Eclipse (Varian). The results obtained with PENELOPE have a maximum difference with experimental data of 2.3%, whereas the eMC code differs systematically from the experimental data about 7% in the penumbra tails. We also show that PENELOPE simulations are able to obtain absorbed dose maps with an equivalent statistical uncertainty to the one found with eMC in similar CPU times.</description>
    <dc:date>2010-06-15T10:30:46Z</dc:date>
  </item>
  <item rdf:about="http://hdl.handle.net/2117/7648">
    <title>PenMesh-Monte Carlo radiation transport simulation in a triangle mesh geometry</title>
    <link>http://hdl.handle.net/2117/7648</link>
    <description>Title: PenMesh-Monte Carlo radiation transport simulation in a triangle mesh geometry
Authors: Badal Soler, Andreu; Kyprianou, Iacovos; Banh, Diem Phuc; Badano, Aldo; Sempau Roma, Josep
Abstract: We have developed a general-purpose Monte Carlo simulation code, called penMesh, that combines the accuracy of the radiation transport physics subroutines from PENELOPE and the flexibility of a geometry based on triangle meshes. While the geometric models implemented in most general-purpose codes-such as PENELOPE's quadric geometry-impose some limitations in the shape of the objects that can be simulated, triangle meshes can be used to describe any free-form (arbitrary) object. Triangle meshes are extensively used in computer-aided design and computer graphics. We took advantage of the sophisticated tools already developed in these fields, such as an octree structure and an efficient ray-triangle intersection algorithm, to significantly accelerate the triangle mesh ray-tracing. A detailed description of the new simulation code and its ray-tracing algorithm is provided in this paper. Furthermore, we show how it can be readily used in medical imaging applications thanks to the detailed anatomical phantoms already available. In particular, we present a whole body radiography simulation using a triangulated version of the anthropomorphic NCAT phantom. An example simulation of scatter fraction measurements using a standardized abdomen and lumbar spine phantom, and a benchmark of the triangle mesh and quadric geometries in the ray-tracing of a mathematical breast model, are also presented to show some of the capabilities of penMesh.</description>
    <dc:date>2010-06-14T12:22:43Z</dc:date>
  </item>
  <item rdf:about="http://hdl.handle.net/2117/7390">
    <title>Natural and anthropogenic radionuclides in airborne particulate samples collected in Barcelona (Spain)</title>
    <link>http://hdl.handle.net/2117/7390</link>
    <description>Title: Natural and anthropogenic radionuclides in airborne particulate samples collected in Barcelona (Spain)
Authors: Valles Murciano, M. Isabel; Camacho García, Antonia; Ortega Aramburu, Miguel Javier; Serrano, Ivana; Blázquez Pérez, Sonia M.; Perez, S</description>
    <dc:date>2010-05-27T11:02:52Z</dc:date>
  </item>
  <item rdf:about="http://hdl.handle.net/2117/7314">
    <title>Analysis of outdoor radon pregeny concentration measured at the Spanish radioactive aerosol automatic monitoring network</title>
    <link>http://hdl.handle.net/2117/7314</link>
    <description>Title: Analysis of outdoor radon pregeny concentration measured at the Spanish radioactive aerosol automatic monitoring network
Authors: Arnold Arias, Dèlia; Vargas Drechsler, Arturo; Ortega Aramburu, Miguel Javier
Abstract: An analysis of 10-year radon progeny data,provided by the Spanish automatic radiological surveillance network, in relation to meteorology is presented. Results show great spatial variability depending mainly on the station location and thus,the surrounding radon exhalation rate. Hourly averages show the typical diurnal cycle with an early morning maximum and a minimum at noon,except for one&#xD;
mountain station, which shows an inverse behaviour. Monthly averaged values show lower concentrations during months with higher atmospheric instability.</description>
    <dc:date>2010-05-19T09:28:30Z</dc:date>
  </item>
  <item rdf:about="http://hdl.handle.net/2117/7313">
    <title>Analysis of radon origin by backward atmospheric transport modelling</title>
    <link>http://hdl.handle.net/2117/7313</link>
    <description>Title: Analysis of radon origin by backward atmospheric transport modelling
Authors: Arnold Arias, Dèlia; Vargas Drechsler, Arturo; Vermeulen, A.T.; Verheggen, B.; Seibert, P.
Abstract: This work shows how ambient radon concentrations measured at Cabauw station in central Netherlands are influenced by transport from different regions under typical transport conditions occurring during&#xD;
April and November, 2007 by means of atmospheric Lagrangian particle dispersion modelling in a receptor-oriented approach. Four specific regions have been isolated to assess their contribution to the modelled radon ambient concentrations at Cabauw, and two different radon flux assumptions. Westerly flows coming from the ocean are poor in radon and do not increase radon air concentrations unless there is some fetch over the British Isles. Continental transport, mainly from eastern and southern Europe, significantly increases radon background concentrations, reaching increments of 3 Bq m-3. A constant&#xD;
0.66 atoms cm-2 s-1 radon flux over land and zero over water bodies is a good approximation for the source term in order to study regional contributions and modulation of the radon background.</description>
    <dc:date>2010-05-19T09:00:53Z</dc:date>
  </item>
  <item rdf:about="http://hdl.handle.net/2117/7309">
    <title>Activity size distributions for long-lived radon decays products in aerosols collected in Barcelona (Spain)</title>
    <link>http://hdl.handle.net/2117/7309</link>
    <description>Title: Activity size distributions for long-lived radon decays products in aerosols collected in Barcelona (Spain)
Authors: Camacho García, Antonia; Valles Murciano, M. Isabel; Vargas Drechsler, Arturo; González Perosanz, M.; Ortega Aramburu, Miguel Javier
Abstract: The activity median aerodynamic diameters(AMADs)oflong-lived radon decay product(210Pb, 210Po) in aerosols collected in the Barcelona area(NortheastSpain)during the period from April 2006 toFebruary 2008 arepresented.The 210Po mean AMAD was 420nm, while the 210Pb mean AMAD was 500nm.&#xD;
The temporal evolution of 210Pb and 210Po AMADs shows maxima in autumn and winter and minima in spring and summer. 210Pb AMAD are being used to estimate the mean-residence time of atmospheric aerosols.</description>
    <dc:date>2010-05-18T13:51:45Z</dc:date>
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