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Autor:
Xiaolei Sun, Ni Tang, Bárbara Fuentes, Ghazal Moradi, Wenqin Huang, Qian Zhang, Daniel Contreras, Franko Arenas, Simon Matthias May, Nina Sibers, Wulf Amelung, Roland Bol, Erwin Klumpp
Organic carbon (OC) in the hyper-arid Atacama Desert soils is known to be extremely low (0.1-0.01%). OC can accumulate on soil colloids (1-1000 nm) and nanoparticles (1-100 nm) due to its high specific surface area. Small-sized colloids may be transf
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::696ef91a1a36d2e3a23735b94757e6df
https://doi.org/10.5194/egusphere-egu22-11761
https://doi.org/10.5194/egusphere-egu22-11761