Isotopic composition of the radioactive fallout in Eastern Poland after the Chernobyl accident
Abstract After the Chernobyl accident the radioactivity of air, soil, dust and grass samples, originating from Eastern Poland was investigated by gamma-ray techniques. The isotopic composition of the radioactive fission products in these samples was determined. By combining the obtained results with...
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E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
1987 |
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| Umfang: |
31 |
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| Reproduktion: |
Springer Online Journal Archives 1860-2002 |
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| Übergeordnetes Werk: |
in: Journal of radioanalytical and nuclear chemistry - 1968, 117(1987) vom: Juni, Seite 379-409 |
| Übergeordnetes Werk: |
volume:117 ; year:1987 ; month:06 ; pages:379-409 ; extent:31 |
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NLEJ194883833 |
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| 520 | |a Abstract After the Chernobyl accident the radioactivity of air, soil, dust and grass samples, originating from Eastern Poland was investigated by gamma-ray techniques. The isotopic composition of the radioactive fission products in these samples was determined. By combining the obtained results with those from other groups the evolution of the activity ratio in air for some isotopes was gathered. It is suggested that this evolution may be related to the differences in the deposition velocities of various elements. The distributions of the activity ratio in the measured samples indicate different transport and deposition properties for the volatile and nonvolatile fission products. It is concluded that the main part of the released nonvolatile products was deposited in the form of hot particles. | ||
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| 700 | 1 | |a Batsch, T. |4 oth | |
| 700 | 1 | |a Jaracz, P. |4 oth | |
| 700 | 1 | |a Kurcewicz, W. |4 oth | |
| 700 | 1 | |a Mirowski, S. |4 oth | |
| 700 | 1 | |a Szeflińska, G. |4 oth | |
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| 700 | 1 | |a Szweryn, B. |4 oth | |
| 700 | 1 | |a Wilhelmi, Z. |4 oth | |
| 700 | 1 | |a Józefowicz, E. T. |4 oth | |
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(DE-627)NLEJ194883833 DE-627 ger DE-627 rakwb eng Isotopic composition of the radioactive fallout in Eastern Poland after the Chernobyl accident 1987 31 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract After the Chernobyl accident the radioactivity of air, soil, dust and grass samples, originating from Eastern Poland was investigated by gamma-ray techniques. The isotopic composition of the radioactive fission products in these samples was determined. By combining the obtained results with those from other groups the evolution of the activity ratio in air for some isotopes was gathered. It is suggested that this evolution may be related to the differences in the deposition velocities of various elements. The distributions of the activity ratio in the measured samples indicate different transport and deposition properties for the volatile and nonvolatile fission products. It is concluded that the main part of the released nonvolatile products was deposited in the form of hot particles. Springer Online Journal Archives 1860-2002 Pieńkowski, L. oth Jastrzebski, J. oth Tys, J. oth Batsch, T. oth Jaracz, P. oth Kurcewicz, W. oth Mirowski, S. oth Szeflińska, G. oth Szeflinski, Z. oth Szweryn, B. oth Wilhelmi, Z. oth Józefowicz, E. T. oth in Journal of radioanalytical and nuclear chemistry 1968 117(1987) vom: Juni, Seite 379-409 (DE-627)NLEJ188994238 (DE-600)2017242-4 1588-2780 nnns volume:117 year:1987 month:06 pages:379-409 extent:31 http://dx.doi.org/10.1007/BF02166042 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 117 1987 6 379-409 31 |
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(DE-627)NLEJ194883833 DE-627 ger DE-627 rakwb eng Isotopic composition of the radioactive fallout in Eastern Poland after the Chernobyl accident 1987 31 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract After the Chernobyl accident the radioactivity of air, soil, dust and grass samples, originating from Eastern Poland was investigated by gamma-ray techniques. The isotopic composition of the radioactive fission products in these samples was determined. By combining the obtained results with those from other groups the evolution of the activity ratio in air for some isotopes was gathered. It is suggested that this evolution may be related to the differences in the deposition velocities of various elements. The distributions of the activity ratio in the measured samples indicate different transport and deposition properties for the volatile and nonvolatile fission products. It is concluded that the main part of the released nonvolatile products was deposited in the form of hot particles. Springer Online Journal Archives 1860-2002 Pieńkowski, L. oth Jastrzebski, J. oth Tys, J. oth Batsch, T. oth Jaracz, P. oth Kurcewicz, W. oth Mirowski, S. oth Szeflińska, G. oth Szeflinski, Z. oth Szweryn, B. oth Wilhelmi, Z. oth Józefowicz, E. T. oth in Journal of radioanalytical and nuclear chemistry 1968 117(1987) vom: Juni, Seite 379-409 (DE-627)NLEJ188994238 (DE-600)2017242-4 1588-2780 nnns volume:117 year:1987 month:06 pages:379-409 extent:31 http://dx.doi.org/10.1007/BF02166042 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 117 1987 6 379-409 31 |
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(DE-627)NLEJ194883833 DE-627 ger DE-627 rakwb eng Isotopic composition of the radioactive fallout in Eastern Poland after the Chernobyl accident 1987 31 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract After the Chernobyl accident the radioactivity of air, soil, dust and grass samples, originating from Eastern Poland was investigated by gamma-ray techniques. The isotopic composition of the radioactive fission products in these samples was determined. By combining the obtained results with those from other groups the evolution of the activity ratio in air for some isotopes was gathered. It is suggested that this evolution may be related to the differences in the deposition velocities of various elements. The distributions of the activity ratio in the measured samples indicate different transport and deposition properties for the volatile and nonvolatile fission products. It is concluded that the main part of the released nonvolatile products was deposited in the form of hot particles. Springer Online Journal Archives 1860-2002 Pieńkowski, L. oth Jastrzebski, J. oth Tys, J. oth Batsch, T. oth Jaracz, P. oth Kurcewicz, W. oth Mirowski, S. oth Szeflińska, G. oth Szeflinski, Z. oth Szweryn, B. oth Wilhelmi, Z. oth Józefowicz, E. T. oth in Journal of radioanalytical and nuclear chemistry 1968 117(1987) vom: Juni, Seite 379-409 (DE-627)NLEJ188994238 (DE-600)2017242-4 1588-2780 nnns volume:117 year:1987 month:06 pages:379-409 extent:31 http://dx.doi.org/10.1007/BF02166042 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 117 1987 6 379-409 31 |
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(DE-627)NLEJ194883833 DE-627 ger DE-627 rakwb eng Isotopic composition of the radioactive fallout in Eastern Poland after the Chernobyl accident 1987 31 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract After the Chernobyl accident the radioactivity of air, soil, dust and grass samples, originating from Eastern Poland was investigated by gamma-ray techniques. The isotopic composition of the radioactive fission products in these samples was determined. By combining the obtained results with those from other groups the evolution of the activity ratio in air for some isotopes was gathered. It is suggested that this evolution may be related to the differences in the deposition velocities of various elements. The distributions of the activity ratio in the measured samples indicate different transport and deposition properties for the volatile and nonvolatile fission products. It is concluded that the main part of the released nonvolatile products was deposited in the form of hot particles. Springer Online Journal Archives 1860-2002 Pieńkowski, L. oth Jastrzebski, J. oth Tys, J. oth Batsch, T. oth Jaracz, P. oth Kurcewicz, W. oth Mirowski, S. oth Szeflińska, G. oth Szeflinski, Z. oth Szweryn, B. oth Wilhelmi, Z. oth Józefowicz, E. T. oth in Journal of radioanalytical and nuclear chemistry 1968 117(1987) vom: Juni, Seite 379-409 (DE-627)NLEJ188994238 (DE-600)2017242-4 1588-2780 nnns volume:117 year:1987 month:06 pages:379-409 extent:31 http://dx.doi.org/10.1007/BF02166042 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 117 1987 6 379-409 31 |
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(DE-627)NLEJ194883833 DE-627 ger DE-627 rakwb eng Isotopic composition of the radioactive fallout in Eastern Poland after the Chernobyl accident 1987 31 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract After the Chernobyl accident the radioactivity of air, soil, dust and grass samples, originating from Eastern Poland was investigated by gamma-ray techniques. The isotopic composition of the radioactive fission products in these samples was determined. By combining the obtained results with those from other groups the evolution of the activity ratio in air for some isotopes was gathered. It is suggested that this evolution may be related to the differences in the deposition velocities of various elements. The distributions of the activity ratio in the measured samples indicate different transport and deposition properties for the volatile and nonvolatile fission products. It is concluded that the main part of the released nonvolatile products was deposited in the form of hot particles. Springer Online Journal Archives 1860-2002 Pieńkowski, L. oth Jastrzebski, J. oth Tys, J. oth Batsch, T. oth Jaracz, P. oth Kurcewicz, W. oth Mirowski, S. oth Szeflińska, G. oth Szeflinski, Z. oth Szweryn, B. oth Wilhelmi, Z. oth Józefowicz, E. T. oth in Journal of radioanalytical and nuclear chemistry 1968 117(1987) vom: Juni, Seite 379-409 (DE-627)NLEJ188994238 (DE-600)2017242-4 1588-2780 nnns volume:117 year:1987 month:06 pages:379-409 extent:31 http://dx.doi.org/10.1007/BF02166042 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 117 1987 6 379-409 31 |
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isotopic composition of the radioactive fallout in eastern poland after the chernobyl accident |
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Isotopic composition of the radioactive fallout in Eastern Poland after the Chernobyl accident |
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Abstract After the Chernobyl accident the radioactivity of air, soil, dust and grass samples, originating from Eastern Poland was investigated by gamma-ray techniques. The isotopic composition of the radioactive fission products in these samples was determined. By combining the obtained results with those from other groups the evolution of the activity ratio in air for some isotopes was gathered. It is suggested that this evolution may be related to the differences in the deposition velocities of various elements. The distributions of the activity ratio in the measured samples indicate different transport and deposition properties for the volatile and nonvolatile fission products. It is concluded that the main part of the released nonvolatile products was deposited in the form of hot particles. |
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Abstract After the Chernobyl accident the radioactivity of air, soil, dust and grass samples, originating from Eastern Poland was investigated by gamma-ray techniques. The isotopic composition of the radioactive fission products in these samples was determined. By combining the obtained results with those from other groups the evolution of the activity ratio in air for some isotopes was gathered. It is suggested that this evolution may be related to the differences in the deposition velocities of various elements. The distributions of the activity ratio in the measured samples indicate different transport and deposition properties for the volatile and nonvolatile fission products. It is concluded that the main part of the released nonvolatile products was deposited in the form of hot particles. |
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Abstract After the Chernobyl accident the radioactivity of air, soil, dust and grass samples, originating from Eastern Poland was investigated by gamma-ray techniques. The isotopic composition of the radioactive fission products in these samples was determined. By combining the obtained results with those from other groups the evolution of the activity ratio in air for some isotopes was gathered. It is suggested that this evolution may be related to the differences in the deposition velocities of various elements. The distributions of the activity ratio in the measured samples indicate different transport and deposition properties for the volatile and nonvolatile fission products. It is concluded that the main part of the released nonvolatile products was deposited in the form of hot particles. |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">NLEJ194883833</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230505224703.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">070526s1987 xx |||||o 00| ||eng c</controlfield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)NLEJ194883833</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Isotopic composition of the radioactive fallout in Eastern Poland after the Chernobyl accident</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">1987</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">31</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract After the Chernobyl accident the radioactivity of air, soil, dust and grass samples, originating from Eastern Poland was investigated by gamma-ray techniques. The isotopic composition of the radioactive fission products in these samples was determined. By combining the obtained results with those from other groups the evolution of the activity ratio in air for some isotopes was gathered. It is suggested that this evolution may be related to the differences in the deposition velocities of various elements. The distributions of the activity ratio in the measured samples indicate different transport and deposition properties for the volatile and nonvolatile fission products. It is concluded that the main part of the released nonvolatile products was deposited in the form of hot particles.</subfield></datafield><datafield tag="533" ind1=" " ind2=" "><subfield code="f">Springer Online Journal Archives 1860-2002</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Pieńkowski, L.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Jastrzebski, J.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Tys, J.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Batsch, T.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Jaracz, P.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Kurcewicz, W.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Mirowski, S.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Szeflińska, G.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Szeflinski, Z.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Szweryn, B.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Wilhelmi, Z.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Józefowicz, E. T.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">in</subfield><subfield code="t">Journal of radioanalytical and nuclear chemistry</subfield><subfield code="d">1968</subfield><subfield code="g">117(1987) vom: Juni, Seite 379-409</subfield><subfield code="w">(DE-627)NLEJ188994238</subfield><subfield code="w">(DE-600)2017242-4</subfield><subfield code="x">1588-2780</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:117</subfield><subfield code="g">year:1987</subfield><subfield code="g">month:06</subfield><subfield code="g">pages:379-409</subfield><subfield code="g">extent:31</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">http://dx.doi.org/10.1007/BF02166042</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ZDB-1-SOJ</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_NL_ARTICLE</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">117</subfield><subfield code="j">1987</subfield><subfield code="c">6</subfield><subfield code="h">379-409</subfield><subfield code="g">31</subfield></datafield></record></collection>
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