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Methods of Monitoring Groundwater Radon,In this chapter, we will present methods of monitoring groundwater radon including groundwater sampling and radon determination. Radon distributions in groundwater near an active fault are discussed. The application of groundwater radon for earthquake prediction research is also briefly reviewed.

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inveigh

Anomalous Radon Decline at Antung Hot Spring Before the 2003 Mw 6.8 Chengkung Earthquake,ore the 1978 Izu-Oshima-Kinkai earthquake in Japan. Both observations at Antung and Izu suggest that the groundwater radon, when monitored at suitable geological sites, can be a sensitive tracer for strain changes in the crust preceding an earthquake.

cardiovascular

muster

Pre-operative Management and Vascular Accessthe in-situ development of gas bubbles in water-saturated brittle rock prior to the 2008 . 5.4 Antung earthquake. In addition, aquifer transmissivity determined from well tests can complement groundwater radon as an earthquake precursor.

muster

https://doi.org/10.1007/978-981-10-6304-6will also be discussed. Both springs, Paihe and Byakko, are small unconfined aquifers. The groundwater-radon concentration in an unconfined aquifer is markedly affected by precipitation. Unlike a confined aquifer, an unconfined aquifer can be used for earthquake warnings only in the dry season.

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Ahmad Khaleghnejad Tabari,Ehsan Moradie Antung hot spring, this chapter will also illustrate the application of recurrent radon anomalies for forecasting local main earthquakes occurring on the Longitudinal Valley Fault in the Taiwan subduction zone.

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Anomalous Radon Declines in Small Unconfined Aquifers: Corroboration of Favorable Geological Conditwill also be discussed. Both springs, Paihe and Byakko, are small unconfined aquifers. The groundwater-radon concentration in an unconfined aquifer is markedly affected by precipitation. Unlike a confined aquifer, an unconfined aquifer can be used for earthquake warnings only in the dry season.