Atmospheric 210Pb as a tracer for soil organic carbon transport in a coniferous forest

What is it about?

It deals on the 210Pbex flow and organic carbon cycle in forest ecosystem and highlights the use of the radiolead as a tracer of soil organic carbon, and insights the possibilities to develop a solid model to explain erosion-derived global warming based on this particular radioisotope.

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Why is it important?

As the radiolead is a natural existing radioisotope it provides the opportunity to study erosion-derived organic carbon redistribution and emission to the atmosphere globally.