Multifractal detrended fluctuation analysis of soil radon (222Rn) and thoron (220Rn) time series
Abstract We present results of Multifractal Detrended Fluctuation Analysis (MF-DFA) of soil radon (222Rn) and thoron (220Rn) time series to examine the scaling and multifractal features. Data consists of 15,692 measurements taken each over forty-minute interval. RTM 1688–2, 222Rn/220Rn electronic de...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Rafique, Muhammad [verfasserIn] Iqbal, Javid [verfasserIn] Lone, Kashif Javed [verfasserIn] Kearfott, Kimberlee Jane [verfasserIn] Rahman, Saeed Ur [verfasserIn] Hussain, Lal [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2021 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Journal of radioanalytical and nuclear chemistry - Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968, 328(2021), 1 vom: 17. März, Seite 425-434 |
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| Übergeordnetes Werk: |
volume:328 ; year:2021 ; number:1 ; day:17 ; month:03 ; pages:425-434 |
| Links: |
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| DOI / URN: |
10.1007/s10967-021-07650-x |
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| Katalog-ID: |
SPR043859704 |
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| 520 | |a Abstract We present results of Multifractal Detrended Fluctuation Analysis (MF-DFA) of soil radon (222Rn) and thoron (220Rn) time series to examine the scaling and multifractal features. Data consists of 15,692 measurements taken each over forty-minute interval. RTM 1688–2, 222Rn/220Rn electronic device has been used for measurement purposes. Seasonal periodicities have been removed from the data and MF-DFA was employed on de-seasonalized data. Original 222Rn and 220Rn time series have been converted into surrogated and shuffled time series. MF-DFA has also been applied to the surrogated and shuffled series to examine the multifractality nature. Results of the study show that %${}_{{{\text{Orig}}}}^{222} {\text{Rn}}%$, %${}_{{{\text{Surr}}}}^{222} {\text{Rn}}%$ and %${}_{{{\text{Orig}}}}^{220} {\text{Rn}}%$, %${}_{{{\text{Surr}}}}^{220} {\text{Rn}}%$ time series are long-range positively correlated and an increase or decrease in either of radionuclide concentrations will be followed by another increase or decrease of concentrations in future measurements. The %${}_{{{\text{Shuff}}}}^{220} {\text{Rn}}%$ time series has an independent or short-range dependent structure called white noise and the shuffled time series exhibit a very weak multifractality. | ||
| 650 | 4 | |a MF-DFA |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a radon ( |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Rn) |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a thoron ( |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Rn) |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Time series seasonal periodicities |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Multifractality nature |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Iqbal, Javid |e verfasserin |4 aut | |
| 700 | 1 | |a Lone, Kashif Javed |e verfasserin |4 aut | |
| 700 | 1 | |a Kearfott, Kimberlee Jane |e verfasserin |4 aut | |
| 700 | 1 | |a Rahman, Saeed Ur |e verfasserin |4 aut | |
| 700 | 1 | |a Hussain, Lal |e verfasserin |4 aut | |
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10.1007/s10967-021-07650-x doi (DE-627)SPR043859704 (DE-599)SPRs10967-021-07650-x-e (SPR)s10967-021-07650-x-e DE-627 ger DE-627 rakwb eng 540 ASE 35.00 bkl Rafique, Muhammad verfasserin aut Multifractal detrended fluctuation analysis of soil radon (222Rn) and thoron (220Rn) time series 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract We present results of Multifractal Detrended Fluctuation Analysis (MF-DFA) of soil radon (222Rn) and thoron (220Rn) time series to examine the scaling and multifractal features. Data consists of 15,692 measurements taken each over forty-minute interval. RTM 1688–2, 222Rn/220Rn electronic device has been used for measurement purposes. Seasonal periodicities have been removed from the data and MF-DFA was employed on de-seasonalized data. Original 222Rn and 220Rn time series have been converted into surrogated and shuffled time series. MF-DFA has also been applied to the surrogated and shuffled series to examine the multifractality nature. Results of the study show that %${}_{{{\text{Orig}}}}^{222} {\text{Rn}}%$, %${}_{{{\text{Surr}}}}^{222} {\text{Rn}}%$ and %${}_{{{\text{Orig}}}}^{220} {\text{Rn}}%$, %${}_{{{\text{Surr}}}}^{220} {\text{Rn}}%$ time series are long-range positively correlated and an increase or decrease in either of radionuclide concentrations will be followed by another increase or decrease of concentrations in future measurements. The %${}_{{{\text{Shuff}}}}^{220} {\text{Rn}}%$ time series has an independent or short-range dependent structure called white noise and the shuffled time series exhibit a very weak multifractality. MF-DFA (dpeaa)DE-He213 radon ( (dpeaa)DE-He213 Rn) (dpeaa)DE-He213 thoron ( (dpeaa)DE-He213 Rn) (dpeaa)DE-He213 Time series seasonal periodicities (dpeaa)DE-He213 Multifractality nature (dpeaa)DE-He213 Iqbal, Javid verfasserin aut Lone, Kashif Javed verfasserin aut Kearfott, Kimberlee Jane verfasserin aut Rahman, Saeed Ur verfasserin aut Hussain, Lal verfasserin aut Enthalten in Journal of radioanalytical and nuclear chemistry Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968 328(2021), 1 vom: 17. März, Seite 425-434 (DE-627)320578011 (DE-600)2017242-4 1588-2780 nnns volume:328 year:2021 number:1 day:17 month:03 pages:425-434 https://dx.doi.org/10.1007/s10967-021-07650-x lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 35.00 ASE AR 328 2021 1 17 03 425-434 |
| spelling |
10.1007/s10967-021-07650-x doi (DE-627)SPR043859704 (DE-599)SPRs10967-021-07650-x-e (SPR)s10967-021-07650-x-e DE-627 ger DE-627 rakwb eng 540 ASE 35.00 bkl Rafique, Muhammad verfasserin aut Multifractal detrended fluctuation analysis of soil radon (222Rn) and thoron (220Rn) time series 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract We present results of Multifractal Detrended Fluctuation Analysis (MF-DFA) of soil radon (222Rn) and thoron (220Rn) time series to examine the scaling and multifractal features. Data consists of 15,692 measurements taken each over forty-minute interval. RTM 1688–2, 222Rn/220Rn electronic device has been used for measurement purposes. Seasonal periodicities have been removed from the data and MF-DFA was employed on de-seasonalized data. Original 222Rn and 220Rn time series have been converted into surrogated and shuffled time series. MF-DFA has also been applied to the surrogated and shuffled series to examine the multifractality nature. Results of the study show that %${}_{{{\text{Orig}}}}^{222} {\text{Rn}}%$, %${}_{{{\text{Surr}}}}^{222} {\text{Rn}}%$ and %${}_{{{\text{Orig}}}}^{220} {\text{Rn}}%$, %${}_{{{\text{Surr}}}}^{220} {\text{Rn}}%$ time series are long-range positively correlated and an increase or decrease in either of radionuclide concentrations will be followed by another increase or decrease of concentrations in future measurements. The %${}_{{{\text{Shuff}}}}^{220} {\text{Rn}}%$ time series has an independent or short-range dependent structure called white noise and the shuffled time series exhibit a very weak multifractality. MF-DFA (dpeaa)DE-He213 radon ( (dpeaa)DE-He213 Rn) (dpeaa)DE-He213 thoron ( (dpeaa)DE-He213 Rn) (dpeaa)DE-He213 Time series seasonal periodicities (dpeaa)DE-He213 Multifractality nature (dpeaa)DE-He213 Iqbal, Javid verfasserin aut Lone, Kashif Javed verfasserin aut Kearfott, Kimberlee Jane verfasserin aut Rahman, Saeed Ur verfasserin aut Hussain, Lal verfasserin aut Enthalten in Journal of radioanalytical and nuclear chemistry Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968 328(2021), 1 vom: 17. März, Seite 425-434 (DE-627)320578011 (DE-600)2017242-4 1588-2780 nnns volume:328 year:2021 number:1 day:17 month:03 pages:425-434 https://dx.doi.org/10.1007/s10967-021-07650-x lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 35.00 ASE AR 328 2021 1 17 03 425-434 |
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10.1007/s10967-021-07650-x doi (DE-627)SPR043859704 (DE-599)SPRs10967-021-07650-x-e (SPR)s10967-021-07650-x-e DE-627 ger DE-627 rakwb eng 540 ASE 35.00 bkl Rafique, Muhammad verfasserin aut Multifractal detrended fluctuation analysis of soil radon (222Rn) and thoron (220Rn) time series 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract We present results of Multifractal Detrended Fluctuation Analysis (MF-DFA) of soil radon (222Rn) and thoron (220Rn) time series to examine the scaling and multifractal features. Data consists of 15,692 measurements taken each over forty-minute interval. RTM 1688–2, 222Rn/220Rn electronic device has been used for measurement purposes. Seasonal periodicities have been removed from the data and MF-DFA was employed on de-seasonalized data. Original 222Rn and 220Rn time series have been converted into surrogated and shuffled time series. MF-DFA has also been applied to the surrogated and shuffled series to examine the multifractality nature. Results of the study show that %${}_{{{\text{Orig}}}}^{222} {\text{Rn}}%$, %${}_{{{\text{Surr}}}}^{222} {\text{Rn}}%$ and %${}_{{{\text{Orig}}}}^{220} {\text{Rn}}%$, %${}_{{{\text{Surr}}}}^{220} {\text{Rn}}%$ time series are long-range positively correlated and an increase or decrease in either of radionuclide concentrations will be followed by another increase or decrease of concentrations in future measurements. The %${}_{{{\text{Shuff}}}}^{220} {\text{Rn}}%$ time series has an independent or short-range dependent structure called white noise and the shuffled time series exhibit a very weak multifractality. MF-DFA (dpeaa)DE-He213 radon ( (dpeaa)DE-He213 Rn) (dpeaa)DE-He213 thoron ( (dpeaa)DE-He213 Rn) (dpeaa)DE-He213 Time series seasonal periodicities (dpeaa)DE-He213 Multifractality nature (dpeaa)DE-He213 Iqbal, Javid verfasserin aut Lone, Kashif Javed verfasserin aut Kearfott, Kimberlee Jane verfasserin aut Rahman, Saeed Ur verfasserin aut Hussain, Lal verfasserin aut Enthalten in Journal of radioanalytical and nuclear chemistry Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968 328(2021), 1 vom: 17. März, Seite 425-434 (DE-627)320578011 (DE-600)2017242-4 1588-2780 nnns volume:328 year:2021 number:1 day:17 month:03 pages:425-434 https://dx.doi.org/10.1007/s10967-021-07650-x lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 35.00 ASE AR 328 2021 1 17 03 425-434 |
| allfieldsGer |
10.1007/s10967-021-07650-x doi (DE-627)SPR043859704 (DE-599)SPRs10967-021-07650-x-e (SPR)s10967-021-07650-x-e DE-627 ger DE-627 rakwb eng 540 ASE 35.00 bkl Rafique, Muhammad verfasserin aut Multifractal detrended fluctuation analysis of soil radon (222Rn) and thoron (220Rn) time series 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract We present results of Multifractal Detrended Fluctuation Analysis (MF-DFA) of soil radon (222Rn) and thoron (220Rn) time series to examine the scaling and multifractal features. Data consists of 15,692 measurements taken each over forty-minute interval. RTM 1688–2, 222Rn/220Rn electronic device has been used for measurement purposes. Seasonal periodicities have been removed from the data and MF-DFA was employed on de-seasonalized data. Original 222Rn and 220Rn time series have been converted into surrogated and shuffled time series. MF-DFA has also been applied to the surrogated and shuffled series to examine the multifractality nature. Results of the study show that %${}_{{{\text{Orig}}}}^{222} {\text{Rn}}%$, %${}_{{{\text{Surr}}}}^{222} {\text{Rn}}%$ and %${}_{{{\text{Orig}}}}^{220} {\text{Rn}}%$, %${}_{{{\text{Surr}}}}^{220} {\text{Rn}}%$ time series are long-range positively correlated and an increase or decrease in either of radionuclide concentrations will be followed by another increase or decrease of concentrations in future measurements. The %${}_{{{\text{Shuff}}}}^{220} {\text{Rn}}%$ time series has an independent or short-range dependent structure called white noise and the shuffled time series exhibit a very weak multifractality. MF-DFA (dpeaa)DE-He213 radon ( (dpeaa)DE-He213 Rn) (dpeaa)DE-He213 thoron ( (dpeaa)DE-He213 Rn) (dpeaa)DE-He213 Time series seasonal periodicities (dpeaa)DE-He213 Multifractality nature (dpeaa)DE-He213 Iqbal, Javid verfasserin aut Lone, Kashif Javed verfasserin aut Kearfott, Kimberlee Jane verfasserin aut Rahman, Saeed Ur verfasserin aut Hussain, Lal verfasserin aut Enthalten in Journal of radioanalytical and nuclear chemistry Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968 328(2021), 1 vom: 17. März, Seite 425-434 (DE-627)320578011 (DE-600)2017242-4 1588-2780 nnns volume:328 year:2021 number:1 day:17 month:03 pages:425-434 https://dx.doi.org/10.1007/s10967-021-07650-x lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 35.00 ASE AR 328 2021 1 17 03 425-434 |
| allfieldsSound |
10.1007/s10967-021-07650-x doi (DE-627)SPR043859704 (DE-599)SPRs10967-021-07650-x-e (SPR)s10967-021-07650-x-e DE-627 ger DE-627 rakwb eng 540 ASE 35.00 bkl Rafique, Muhammad verfasserin aut Multifractal detrended fluctuation analysis of soil radon (222Rn) and thoron (220Rn) time series 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract We present results of Multifractal Detrended Fluctuation Analysis (MF-DFA) of soil radon (222Rn) and thoron (220Rn) time series to examine the scaling and multifractal features. Data consists of 15,692 measurements taken each over forty-minute interval. RTM 1688–2, 222Rn/220Rn electronic device has been used for measurement purposes. Seasonal periodicities have been removed from the data and MF-DFA was employed on de-seasonalized data. Original 222Rn and 220Rn time series have been converted into surrogated and shuffled time series. MF-DFA has also been applied to the surrogated and shuffled series to examine the multifractality nature. Results of the study show that %${}_{{{\text{Orig}}}}^{222} {\text{Rn}}%$, %${}_{{{\text{Surr}}}}^{222} {\text{Rn}}%$ and %${}_{{{\text{Orig}}}}^{220} {\text{Rn}}%$, %${}_{{{\text{Surr}}}}^{220} {\text{Rn}}%$ time series are long-range positively correlated and an increase or decrease in either of radionuclide concentrations will be followed by another increase or decrease of concentrations in future measurements. The %${}_{{{\text{Shuff}}}}^{220} {\text{Rn}}%$ time series has an independent or short-range dependent structure called white noise and the shuffled time series exhibit a very weak multifractality. MF-DFA (dpeaa)DE-He213 radon ( (dpeaa)DE-He213 Rn) (dpeaa)DE-He213 thoron ( (dpeaa)DE-He213 Rn) (dpeaa)DE-He213 Time series seasonal periodicities (dpeaa)DE-He213 Multifractality nature (dpeaa)DE-He213 Iqbal, Javid verfasserin aut Lone, Kashif Javed verfasserin aut Kearfott, Kimberlee Jane verfasserin aut Rahman, Saeed Ur verfasserin aut Hussain, Lal verfasserin aut Enthalten in Journal of radioanalytical and nuclear chemistry Dordrecht [u.a.] : Springer Science + Business Media B.V., 1968 328(2021), 1 vom: 17. März, Seite 425-434 (DE-627)320578011 (DE-600)2017242-4 1588-2780 nnns volume:328 year:2021 number:1 day:17 month:03 pages:425-434 https://dx.doi.org/10.1007/s10967-021-07650-x lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 35.00 ASE AR 328 2021 1 17 03 425-434 |
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English |
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Enthalten in Journal of radioanalytical and nuclear chemistry 328(2021), 1 vom: 17. März, Seite 425-434 volume:328 year:2021 number:1 day:17 month:03 pages:425-434 |
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Enthalten in Journal of radioanalytical and nuclear chemistry 328(2021), 1 vom: 17. März, Seite 425-434 volume:328 year:2021 number:1 day:17 month:03 pages:425-434 |
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Rafique, Muhammad @@aut@@ Iqbal, Javid @@aut@@ Lone, Kashif Javed @@aut@@ Kearfott, Kimberlee Jane @@aut@@ Rahman, Saeed Ur @@aut@@ Hussain, Lal @@aut@@ |
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Data consists of 15,692 measurements taken each over forty-minute interval. RTM 1688–2, 222Rn/220Rn electronic device has been used for measurement purposes. Seasonal periodicities have been removed from the data and MF-DFA was employed on de-seasonalized data. Original 222Rn and 220Rn time series have been converted into surrogated and shuffled time series. MF-DFA has also been applied to the surrogated and shuffled series to examine the multifractality nature. Results of the study show that %${}_{{{\text{Orig}}}}^{222} {\text{Rn}}%$, %${}_{{{\text{Surr}}}}^{222} {\text{Rn}}%$ and %${}_{{{\text{Orig}}}}^{220} {\text{Rn}}%$, %${}_{{{\text{Surr}}}}^{220} {\text{Rn}}%$ time series are long-range positively correlated and an increase or decrease in either of radionuclide concentrations will be followed by another increase or decrease of concentrations in future measurements. 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|
| author |
Rafique, Muhammad |
| spellingShingle |
Rafique, Muhammad ddc 540 bkl 35.00 misc MF-DFA misc radon ( misc Rn) misc thoron ( misc Time series seasonal periodicities misc Multifractality nature Multifractal detrended fluctuation analysis of soil radon (222Rn) and thoron (220Rn) time series |
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540 ASE 35.00 bkl Multifractal detrended fluctuation analysis of soil radon (222Rn) and thoron (220Rn) time series MF-DFA (dpeaa)DE-He213 radon ( (dpeaa)DE-He213 Rn) (dpeaa)DE-He213 thoron ( (dpeaa)DE-He213 Time series seasonal periodicities (dpeaa)DE-He213 Multifractality nature (dpeaa)DE-He213 |
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ddc 540 bkl 35.00 misc MF-DFA misc radon ( misc Rn) misc thoron ( misc Time series seasonal periodicities misc Multifractality nature |
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ddc 540 bkl 35.00 misc MF-DFA misc radon ( misc Rn) misc thoron ( misc Time series seasonal periodicities misc Multifractality nature |
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ddc 540 bkl 35.00 misc MF-DFA misc radon ( misc Rn) misc thoron ( misc Time series seasonal periodicities misc Multifractality nature |
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Multifractal detrended fluctuation analysis of soil radon (222Rn) and thoron (220Rn) time series |
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Multifractal detrended fluctuation analysis of soil radon (222Rn) and thoron (220Rn) time series |
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Rafique, Muhammad |
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Rafique, Muhammad Iqbal, Javid Lone, Kashif Javed Kearfott, Kimberlee Jane Rahman, Saeed Ur Hussain, Lal |
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Elektronische Aufsätze |
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Rafique, Muhammad |
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10.1007/s10967-021-07650-x |
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multifractal detrended fluctuation analysis of soil radon (222rn) and thoron (220rn) time series |
| title_auth |
Multifractal detrended fluctuation analysis of soil radon (222Rn) and thoron (220Rn) time series |
| abstract |
Abstract We present results of Multifractal Detrended Fluctuation Analysis (MF-DFA) of soil radon (222Rn) and thoron (220Rn) time series to examine the scaling and multifractal features. Data consists of 15,692 measurements taken each over forty-minute interval. RTM 1688–2, 222Rn/220Rn electronic device has been used for measurement purposes. Seasonal periodicities have been removed from the data and MF-DFA was employed on de-seasonalized data. Original 222Rn and 220Rn time series have been converted into surrogated and shuffled time series. MF-DFA has also been applied to the surrogated and shuffled series to examine the multifractality nature. Results of the study show that %${}_{{{\text{Orig}}}}^{222} {\text{Rn}}%$, %${}_{{{\text{Surr}}}}^{222} {\text{Rn}}%$ and %${}_{{{\text{Orig}}}}^{220} {\text{Rn}}%$, %${}_{{{\text{Surr}}}}^{220} {\text{Rn}}%$ time series are long-range positively correlated and an increase or decrease in either of radionuclide concentrations will be followed by another increase or decrease of concentrations in future measurements. The %${}_{{{\text{Shuff}}}}^{220} {\text{Rn}}%$ time series has an independent or short-range dependent structure called white noise and the shuffled time series exhibit a very weak multifractality. |
| abstractGer |
Abstract We present results of Multifractal Detrended Fluctuation Analysis (MF-DFA) of soil radon (222Rn) and thoron (220Rn) time series to examine the scaling and multifractal features. Data consists of 15,692 measurements taken each over forty-minute interval. RTM 1688–2, 222Rn/220Rn electronic device has been used for measurement purposes. Seasonal periodicities have been removed from the data and MF-DFA was employed on de-seasonalized data. Original 222Rn and 220Rn time series have been converted into surrogated and shuffled time series. MF-DFA has also been applied to the surrogated and shuffled series to examine the multifractality nature. Results of the study show that %${}_{{{\text{Orig}}}}^{222} {\text{Rn}}%$, %${}_{{{\text{Surr}}}}^{222} {\text{Rn}}%$ and %${}_{{{\text{Orig}}}}^{220} {\text{Rn}}%$, %${}_{{{\text{Surr}}}}^{220} {\text{Rn}}%$ time series are long-range positively correlated and an increase or decrease in either of radionuclide concentrations will be followed by another increase or decrease of concentrations in future measurements. The %${}_{{{\text{Shuff}}}}^{220} {\text{Rn}}%$ time series has an independent or short-range dependent structure called white noise and the shuffled time series exhibit a very weak multifractality. |
| abstract_unstemmed |
Abstract We present results of Multifractal Detrended Fluctuation Analysis (MF-DFA) of soil radon (222Rn) and thoron (220Rn) time series to examine the scaling and multifractal features. Data consists of 15,692 measurements taken each over forty-minute interval. RTM 1688–2, 222Rn/220Rn electronic device has been used for measurement purposes. Seasonal periodicities have been removed from the data and MF-DFA was employed on de-seasonalized data. Original 222Rn and 220Rn time series have been converted into surrogated and shuffled time series. MF-DFA has also been applied to the surrogated and shuffled series to examine the multifractality nature. Results of the study show that %${}_{{{\text{Orig}}}}^{222} {\text{Rn}}%$, %${}_{{{\text{Surr}}}}^{222} {\text{Rn}}%$ and %${}_{{{\text{Orig}}}}^{220} {\text{Rn}}%$, %${}_{{{\text{Surr}}}}^{220} {\text{Rn}}%$ time series are long-range positively correlated and an increase or decrease in either of radionuclide concentrations will be followed by another increase or decrease of concentrations in future measurements. The %${}_{{{\text{Shuff}}}}^{220} {\text{Rn}}%$ time series has an independent or short-range dependent structure called white noise and the shuffled time series exhibit a very weak multifractality. |
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Multifractal detrended fluctuation analysis of soil radon (222Rn) and thoron (220Rn) time series |
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| score |
7.402152 |