Application of 222Rn to the Analysis of the Exchange between River Water and Groundwater.

Hamada, Hiromasa; Komae, Takami

doi:10.3769/radioisotopes.43.12_770

Cited by 12 publications

(1 citation statement)

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“…When the component of groundwater in surface water is large, the 222 Rn concentration in the surface water increases. The measurement of 222 Rn concentration in water can therefore be used to identify groundwater seepage into surface water 2,3,5,6,13,15 . However, because the 222 Rn concentration in surface water is too low to measure, it is necessary to concentrate 222 Rn content in water samples.…”

Section: Introductionmentioning

confidence: 99%

Monitoring of Radon-222 Concentration in Surface Waters of the Ban Phai Subwatershed Northeast Thailand Using a Method to Concentrate Radon by Air-circulation

Hamada

Sukchan²

2008

JARQ

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Radon-222 ( 222 Rn) concentration in surface water is a useful indicator for groundwater seepage. However, the natural concentration of 222 Rn in surface water is too low to measure. It is therefore necessary to concentrate 222 Rn content in water samples before analysis. This is a difficult operation requiring specialized equipment. We developed a method of measurement of 222 Rn concentration in surface water (a method to concentrate radon by air-circulation) and applied it to detect groundwater seepage in the Ban Phai subwatershed, northeast Thailand. We also measured electric conductivity to determine whether dissolved ions in water were brought by groundwater. In areas of high-elevation (>180 m above sea level), 222 Rn concentration in surface water was low, indicating that the velocity of subsurface water flow was slow even in the rainy season. This result supported a flow velocity previously calculated from the permeability of surface soil and the hydraulic gradient. Our measurements of 222 Rn concentrations revealed that groundwater can be obtained by digging to a depth of about 1 m in the river bed in some areas. In areas of low-elevation (<160 m above sea level), electric conductivity increased markedly in the dry season. This was attributed to evaporation, rather than the effect of groundwater seepage, because the 222 Rn concentration was low, suggesting little influence of groundwater.

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