Summation of pulses in γ-ray spectra
Abstract It is shown that peaks formed in γ-ray spectra by summing the pulses due to γ cascades can be used to determine both the activity of the radiation source and the efficiency of detecting the γ rays. Possible sources of errors in determining these quantities were investigated. This method may...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Gromov, K. Ya. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2005 |
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| Schlagwörter: |
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| Anmerkung: |
© MAIK “Nauka/Interperiodica” 2005 |
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| Übergeordnetes Werk: |
Enthalten in: Instruments and experimental techniques - Nauka/Interperiodica, 1959, 48(2005), 1 vom: Jan., Seite 43-46 |
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| Übergeordnetes Werk: |
volume:48 ; year:2005 ; number:1 ; month:01 ; pages:43-46 |
| Links: |
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| DOI / URN: |
10.1007/s10786-005-0007-0 |
|---|
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OLC2034142624 |
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| 520 | |a Abstract It is shown that peaks formed in γ-ray spectra by summing the pulses due to γ cascades can be used to determine both the activity of the radiation source and the efficiency of detecting the γ rays. Possible sources of errors in determining these quantities were investigated. This method may be used to measure the cross sections of nuclear reactions, to analyze the background radiation when searching for rare decays, and in other applications. | ||
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| 700 | 1 | |a Samatov, Zh. K. |4 aut | |
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10.1007/s10786-005-0007-0 doi (DE-627)OLC2034142624 (DE-He213)s10786-005-0007-0-p DE-627 ger DE-627 rakwb eng 620 VZ 11 ssgn Gromov, K. Ya. verfasserin aut Summation of pulses in γ-ray spectra 2005 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © MAIK “Nauka/Interperiodica” 2005 Abstract It is shown that peaks formed in γ-ray spectra by summing the pulses due to γ cascades can be used to determine both the activity of the radiation source and the efficiency of detecting the γ rays. Possible sources of errors in determining these quantities were investigated. This method may be used to measure the cross sections of nuclear reactions, to analyze the background radiation when searching for rare decays, and in other applications. Radiation Physical Chemistry Radiation Source Nuclear Reaction Background Radiation Fominykh, V. I. aut Chumin, V. G. aut Samatov, Zh. K. aut Enthalten in Instruments and experimental techniques Nauka/Interperiodica, 1959 48(2005), 1 vom: Jan., Seite 43-46 (DE-627)129603007 (DE-600)241643-8 (DE-576)015096815 0020-4412 nnns volume:48 year:2005 number:1 month:01 pages:43-46 https://doi.org/10.1007/s10786-005-0007-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-PHY SSG-OLC-PHA SSG-OLC-DE-84 GBV_ILN_40 GBV_ILN_70 AR 48 2005 1 01 43-46 |
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10.1007/s10786-005-0007-0 doi (DE-627)OLC2034142624 (DE-He213)s10786-005-0007-0-p DE-627 ger DE-627 rakwb eng 620 VZ 11 ssgn Gromov, K. Ya. verfasserin aut Summation of pulses in γ-ray spectra 2005 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © MAIK “Nauka/Interperiodica” 2005 Abstract It is shown that peaks formed in γ-ray spectra by summing the pulses due to γ cascades can be used to determine both the activity of the radiation source and the efficiency of detecting the γ rays. Possible sources of errors in determining these quantities were investigated. This method may be used to measure the cross sections of nuclear reactions, to analyze the background radiation when searching for rare decays, and in other applications. Radiation Physical Chemistry Radiation Source Nuclear Reaction Background Radiation Fominykh, V. I. aut Chumin, V. G. aut Samatov, Zh. K. aut Enthalten in Instruments and experimental techniques Nauka/Interperiodica, 1959 48(2005), 1 vom: Jan., Seite 43-46 (DE-627)129603007 (DE-600)241643-8 (DE-576)015096815 0020-4412 nnns volume:48 year:2005 number:1 month:01 pages:43-46 https://doi.org/10.1007/s10786-005-0007-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-PHY SSG-OLC-PHA SSG-OLC-DE-84 GBV_ILN_40 GBV_ILN_70 AR 48 2005 1 01 43-46 |
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10.1007/s10786-005-0007-0 doi (DE-627)OLC2034142624 (DE-He213)s10786-005-0007-0-p DE-627 ger DE-627 rakwb eng 620 VZ 11 ssgn Gromov, K. Ya. verfasserin aut Summation of pulses in γ-ray spectra 2005 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © MAIK “Nauka/Interperiodica” 2005 Abstract It is shown that peaks formed in γ-ray spectra by summing the pulses due to γ cascades can be used to determine both the activity of the radiation source and the efficiency of detecting the γ rays. Possible sources of errors in determining these quantities were investigated. This method may be used to measure the cross sections of nuclear reactions, to analyze the background radiation when searching for rare decays, and in other applications. Radiation Physical Chemistry Radiation Source Nuclear Reaction Background Radiation Fominykh, V. I. aut Chumin, V. G. aut Samatov, Zh. K. aut Enthalten in Instruments and experimental techniques Nauka/Interperiodica, 1959 48(2005), 1 vom: Jan., Seite 43-46 (DE-627)129603007 (DE-600)241643-8 (DE-576)015096815 0020-4412 nnns volume:48 year:2005 number:1 month:01 pages:43-46 https://doi.org/10.1007/s10786-005-0007-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-PHY SSG-OLC-PHA SSG-OLC-DE-84 GBV_ILN_40 GBV_ILN_70 AR 48 2005 1 01 43-46 |
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Abstract It is shown that peaks formed in γ-ray spectra by summing the pulses due to γ cascades can be used to determine both the activity of the radiation source and the efficiency of detecting the γ rays. Possible sources of errors in determining these quantities were investigated. This method may be used to measure the cross sections of nuclear reactions, to analyze the background radiation when searching for rare decays, and in other applications. © MAIK “Nauka/Interperiodica” 2005 |
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Abstract It is shown that peaks formed in γ-ray spectra by summing the pulses due to γ cascades can be used to determine both the activity of the radiation source and the efficiency of detecting the γ rays. Possible sources of errors in determining these quantities were investigated. This method may be used to measure the cross sections of nuclear reactions, to analyze the background radiation when searching for rare decays, and in other applications. © MAIK “Nauka/Interperiodica” 2005 |
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Abstract It is shown that peaks formed in γ-ray spectra by summing the pulses due to γ cascades can be used to determine both the activity of the radiation source and the efficiency of detecting the γ rays. Possible sources of errors in determining these quantities were investigated. This method may be used to measure the cross sections of nuclear reactions, to analyze the background radiation when searching for rare decays, and in other applications. © MAIK “Nauka/Interperiodica” 2005 |
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Ya.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Summation of pulses in γ-ray spectra</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2005</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© MAIK “Nauka/Interperiodica” 2005</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract It is shown that peaks formed in γ-ray spectra by summing the pulses due to γ cascades can be used to determine both the activity of the radiation source and the efficiency of detecting the γ rays. Possible sources of errors in determining these quantities were investigated. This method may be used to measure the cross sections of nuclear reactions, to analyze the background radiation when searching for rare decays, and in other applications.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Radiation</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Physical Chemistry</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Radiation Source</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Nuclear Reaction</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Background Radiation</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Fominykh, V. I.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Chumin, V. 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