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Svenja Roosch
Two perspectives on soil structure have often been juxtaposed in the past: the “solid phase” or “aggregate” perspective and the “pore” perspective. The debate intensified recently with several opinion papers, letters to the editor, and ed
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::53b62b22f49b3633e3a78b3e151b61dd
https://doi.org/10.5194/egusphere-egu23-7649
https://doi.org/10.5194/egusphere-egu23-7649
Soil structure is complex and dynamic on various scales. Soil heterogeneity as an expression of soil structural complexity develops over time and is controlled by biological, physical and geochemical processes and their interactions. Biotic and abiot
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8a799eee3c56579bef827aeb2be3895b
https://doi.org/10.5194/egusphere-egu23-16345
https://doi.org/10.5194/egusphere-egu23-16345
Soil microaggregates are considered to play an important role in soil functioning and soil organic carbon (SOC) is of great importance for the formation and stabilization of these aggregates. The loss of SOC can occur, for example, after a change in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::68a6e75404b618b28814eb1d6104ad4f
https://doi.org/10.5194/egusphere-egu2020-17358
https://doi.org/10.5194/egusphere-egu2020-17358