Chen, H., Zhang, W., Gilliam, F., Liu, L., Huang, J., Zhang, T., Wang, W., Mo, J. 2013. Changes in soil carbon sequestration inPinus massoniana forests along an urban-to-rural gradient of southern China. Biogeosciences 10, 6609-6616. DOI: 10.5194/bg-10-6609-2013 Abstract Urbanization is accelerating globally, causing a variety of environmental changes such as increases in air temperature, precipitation, atmospheric CO2, and nitrogen (N) deposition. However, the effects …[Read More]
Soil System Sciences
Monday paper: Changes in soil carbon stocks in Brazil due to land use: paired site comparisons and a regional pasture soil survey
Assad, E. D., Pinto, H. S., Martins, S. C., Groppo, J. D., Salgado, P. R., Evangelista, B., Vasconcellos, E., Sano, E. E., Pavão, E., Luna, R., Camargo, P. B., Martinelli, L. A. 2013. Changes in soil carbon stocks in Brazil due to land use: paired site comparisons and a regional pasture soil survey. Biogeosciences 10, 6141-6160. DOI: 10.5194/bg-10-6141-2013 Abstract In this paper we calculated soil carbon stocks in Brazil studying 17 paired sites where soil …[Read More]
EGU2014 SSS Best Flyer Award
It’s time to vote for your favourite EGU2014 SSS flyer! Votes will be received until March 31st 2014 (votes after that deadline will not be included). You can access the contest rules here: http://static2.egu.eu/media/filer_public/2013/11/27/egu-sssd_2014_bfa_awards.pdf. What’s your fav? Vote at:
Soils going red: Terra rossa
The term “terra rossa” comes from the Italian for “red soil” or “red earth”. Although terra rossa exists in other places in the world, these soils are common in areas with Mediterranean-type climates: alternation of a rainy and cool-to warm-dry season. The terra rossa soil is heavy and clay-rich (silty-clay to clayey) soil, strongly reddish, …[Read More]
Monday paper: Comparing soil biogeochemical processes in novel and natural boreal forest ecosystems
Quideau, S. A., Swallow, M. J. B., Prescott, C. E., Grayston, S. J., Oh, S.-W. 2013. Comparing soil biogeochemical processes in novel and natural boreal forest ecosystems. Biogeosciences, 10, 5651-5661. DOI: 10.5194/bg-10-5651-2013 Abstract Emulating the variability that exists in the natural landscape prior to disturbance should be a goal of soil reconstruction and land reclamation efforts following resource extraction. Long-term ecosystem sustainability within reclaimed landscapes …[Read More]
Short time for submitting abstracts to the EGU2014 Programme on Soil Science
Deadlines Have you submitted yours? Be aware of deadlines: 16 January 2014: Deadline for receipt of abstracts 30 January 2014: Cancellation of Support Applicants who did not answer 04 February 2014: Letter of acceptance 12 March 2014: Letter of schedule 31 March 2014: Deadline for letters of invitation 31 March 2014: Deadline for early registration …[Read More]
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]
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]
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]
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]