ANALYZING THE EFFECTS OF LAND USE ON SOIL EROSION IN SOUTHWESTERN CHINA USING FALLOUT RADIONUCLIDES
Using 137Cs and 210Pb concentrations in detrital sediment, we are able to estimate the depth and timing of erosion in the upstream watershed. 137Cs, which results from atmospheric testing of nuclear weapons, is a tracer for erosion of surface material exposed during the 1950s-1960s. Samples that contain 137Cs must be the result of both minimal and shallow erosion. 210Pb is a tracer for current surface material, due to its ongoing deposition. The presence of 210Pb indicates slow, surface erosion. Thus, watersheds with high erosion during the deforestation will have little to no detectable 137Cs, while watersheds with slow erosion during reforestation will have detectable 210Pb. The basins studied include Red, Yangtze, Salween, Mekong, Irrawaddy. Prior research measured in situ and meteoric 10Be, which we can compare to the short-lived FRN data.
Preliminary data show that only 3 of 59 detrital samples have detectable 137Cs. The absence of 137Cs indicates erosion rates were high during the time of deforestation. However, 42 of the 59 samples have detectable 210Pb. The moderate levels of 210Pb indicate that erosion has since slowed. Since 137Cs and 210Pb are grain size dependent, future work will include measuring FRN concentration in <63μm fraction and leaching samples to improve detectability for 210Pb. These data suggest that reforestation may have decreased erosion rates in southwestern China.