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Regional Calibration of Erosion Radiotracers (210Pb and 137Cs): Atmospheric Fluxes to Soils (Northern Spain)
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文摘
Inventories of radionuclides commonly used to studyenvironmental processes, especially in erosion research,were determined in soil cores from two distant river basinsin northern Spain. Results showed that 210Pb atmosphericfluxes correlate very well with mean annual rainfallacross the region, and this is also the case for 137Csinventories but only on the basin scale. Therefore wesuggest that 210Pb is a better candidate as a radiotracerfor soil erosion studies. In this region, the equation 210Pb flux(Bq m-2 yr-1) = (0.19 ± 0.02) × rainfall (mm yr-1) - (24± 17) can be used as a calibration to estimate input 210Pbfluxes, a key parameter in soil erosion studies andmodels, when mean annual rainfall is known.

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