Torn, M. S., Kleber, M., Zavaleta, E. S., Zhu, B., Field, C. B., Trumbore, S. E. 2013. A dual isotope approach to isolate soil carbon pools of different turnover times. Biogeosciences, 10, 8067-8081. DOI: 10.5194/bg-10-8067-2013. Abstract Soils are globally significant sources and sinks of atmospheric CO2. Increasing the resolution of soil carbon turnover estimates is important for predicting the ...[Read More]
Monday paper: Combined use of stable isotopes and fallout radionuclides as soil erosion indicators in a forested mountain site, South Korea
Meusburger, K., Mabit, L., Park, J.-H., Sandor, T., Alewell, C. 2013. Combined use of stable isotopes and fallout radionuclides as soil erosion indicators in a forested mountain site, South Korea. Biogeosciences 10, 5627-5638. DOI: 10.5194/bg-10-5627-2013, 20133 Abstract The aim of this study is to assess and to validate the suitability of the stable nitrogen and carbon isotope signature as soil e ...[Read More]
Cold soil in the groove
Often, soils from cold regions, such as Arctic soils, show polygonal forms in their surface. These polygons are formed because of the freeze-thaw cycle, characteristic of permafrost. What is permafrost? Permafrost is a subsurface soil layer which stays permanently frozen (below 0 oC) during long periods of time, usually more than two consecutive years. Most extensive permafrost areas can be found ...[Read More]
Monday paper: Modelling soil organic carbon stocks in global change scenarios: a CarboSOIL application
Muñoz-Rojas, M., Jordán, A., Zavala, L. M., González-Peñaloza, F. A., De la Rosa, D., Pino-Mejias, R., and Anaya-Romero, M. 2013. Modelling soil organic carbon stocks in global change scenarios: a CarboSOIL application. Biogeosciences, 10, 8253-8268, DOI: 10.5194/bg-10-8253-2013. Abstract Global climate change, as a consequence of the increasing levels of atmospheric CO2 concentration, may ...[Read More]