2015
DOI: 10.1140/epjst/e2015-02397-7
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222Rn and CO2 at Las Cañadas Caldera (Tenerife, Canary Islands)

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Cited by 11 publications
(3 citation statements)
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References 33 publications
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“…Silva et al [39] discuss the application of continuous radon monitoring at the Furnas volcano (São Miguel Island, Azores), illustrating the stumbling blocks encountered when trying to resolve radon patterns in complex geological settings. Martin-Luis et al [40] report on radon and CO 2 monitoring at the Teide volcano (Tenerife, Canary Islands) emphasizing the distinct behavior of the two gases and its association with environmental conditions. Steinitz et al [41] also discuss results from radon monitoring in Tenerife suggesting an extra-terrestrial (solar) component driving temporal variability.…”
Section: Volcanic Applicationsmentioning
confidence: 99%
“…Silva et al [39] discuss the application of continuous radon monitoring at the Furnas volcano (São Miguel Island, Azores), illustrating the stumbling blocks encountered when trying to resolve radon patterns in complex geological settings. Martin-Luis et al [40] report on radon and CO 2 monitoring at the Teide volcano (Tenerife, Canary Islands) emphasizing the distinct behavior of the two gases and its association with environmental conditions. Steinitz et al [41] also discuss results from radon monitoring in Tenerife suggesting an extra-terrestrial (solar) component driving temporal variability.…”
Section: Volcanic Applicationsmentioning
confidence: 99%
“…6). The latter finding is consistent with previous results demonstrating the presence of additional periodicities of about 12, 8, 6 hours, etc., in the Coimbra data [8] as well as other environmental radon records [64][65][66][67]. Taken together, the part of the spectrum between about 3 hours and 1 day should not be used for estimating a spectral slope associated with possible long-range memory, since it mainly reflects the presence of periodic components in the signal.…”
Section: Power Spectral Densitymentioning
confidence: 99%
“…During the past few decades, long‐term radon monitoring has been conducted within geological media such as shallow soil, country rock, alluvial deposits, ground water, and hot springs and has revealed the following results: (1) A typical cyclical daily signature in radon temporal variability [ Lehmann et al , ; Martín‐Luis et al , ; Schubert and Schulz , ; Alparone et al , ; Fujiyoshi et al , ; Sundal et al , ; Choubey et al , ]: (2) longer radon signals, of several days [ Steinitz et al , ; Richon et al , ; Barbosa et al , ; Eff‐Darwich et al , ; Inan et al , ; Nikolopoulos et al , ]; and (3) long‐term seasonal patterns [ Perrier et al , ; Ghosh et al , ; Barbosa et al , ; Choubey et al , ; Richon et al , ; Zafrir et al , ; Martin‐Luis et al , ].…”
Section: Introductionmentioning
confidence: 99%