Articles | Volume 13, issue 7
https://doi.org/10.5194/se-13-1161-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/se-13-1161-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Preface: State of the art in mineral exploration
Geosciences Barcelona (Geo3Bcn-CSIC), Barcelona, Spain
Ramon Carbonell
Geosciences Barcelona (Geo3Bcn-CSIC), Barcelona, Spain
Solveig Pospiech
Institute for Resource Ecology, Helmholtz-Zentrum
Dresden-Rossendorf, Dresden, Germany
Department of Earth Sciences, Uppsala University, Uppsala, Sweden
Fraunhofer Institute for Wind Energy Systems IWES, Bremen, Germany
Liam A. Bullock
Geosciences Barcelona (Geo3Bcn-CSIC), Barcelona, Spain
Fernando Tornos
Instituto de Geociencias (IGEO, CSIC-UCM), Madrid, Spain
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Against common understanding, Amazon basin upland soils contain average carbon, nitrogen and sulfur concentrations similar to, e.g., European soils. The same applies for average C / N ratios. Post-forest land (e.g., pasture land, plantations) show up to 20 % of carbon and nitrogen losses after deforestation. Distinct seasonal dynamics are visible for the generally low pH-values and very low electrical conductivities in soil solution – a likely driver of seasonal element mobility.
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Joaquina Alvarez-Marrón, Fernando Bastida, Ernest Rutter, Ramon Carbonell, and Charlotte M. Krawczyk
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I. Flecha, R. Carbonell, and R. W. Hobbs
Solid Earth, 4, 543–554, https://doi.org/10.5194/se-4-543-2013, https://doi.org/10.5194/se-4-543-2013, 2013
J. Alcalde, D. Martí, C. Juhlin, A. Malehmir, D. Sopher, E. Saura, I. Marzán, P. Ayarza, A. Calahorrano, A. Pérez-Estaún, and R. Carbonell
Solid Earth, 4, 481–496, https://doi.org/10.5194/se-4-481-2013, https://doi.org/10.5194/se-4-481-2013, 2013
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