Detail of a photo: Large angular boulder beside a shallow pebbly stream in a grassy mountain valley, below steep forested slopes and rocky peaks under a dramatic blue sky, in heavily processed colours.
EGU Blogs

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It needn’t be Hell with soil

This is one of the pictures the year has left. In it, two Muslim militiamen armed with machetes are registering a Christian in the Miskine neighborhood, in Bangui (Central African Republic), December 13, 2013. About 1,600 and 3,000 French soldiers already there of the African MISCA international mission were not able to stop violence and chaos. …[Read More]

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Monday paper: A dual isotope approach to isolate soil carbon pools of different turnover times

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 …[Read More]

Imaggeo on Mondays: A feast of pancakes

The thought of pancake ice always makes me a little hungry – I just can’t help thinking about stacks of syrup-drowned pancakes, or crepes covered wish sugar and doused with lemon juice – but the science of pancake ice is quite a tempting topic too! Pancake ice occurs in areas where ice formation is repeatedly …[Read More]

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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 erosion …[Read More]

My year in 2013

Inspired by Martin Eve (link), I decided to make a documentation of academic-related stuff I’ve achieved in 2013. The last year was mostly occupado by the first year of my PhD, but other academic-ish stuff too as complimentary activities to research. This is kinda like a personal diary of ‘achievements’, as well as a documentation …[Read More]

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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 …[Read More]

Dense rocks rise higher because isostasy says so

From space, the Brandberg Igneous Complex looks like a coffee-coloured birthmark set upon the bony complexion of the Namibian desert. Perfectly circular, its peaks soar in a ring of mighty topography, its massive granite cliffs etched with the muscular definition of spheroidal weathering. Its bulk seems to rise out of the barren landscape, driven upward …[Read More]