Zobrazeno 1 - 10
of 25
pro vyhledávání: '"Frederic Leuther"'
Publikováno v:
Vadose Zone Journal, Vol 23, Iss 4, Pp n/a-n/a (2024)
Abstract Evaporation of soil water depends not only on climatic conditions, soil surface roughness, soil texture, and soil hydraulic properties but also on the soils’ macrostructure. Evaporation is characterized by water losses over time for a defi
Externí odkaz:
https://doaj.org/article/e7ddce9aaab846e5a99e44dd15975f17
Autor:
Steffen Schlüter, Frederic Leuther, Lukas Albrecht, Carmen Hoeschen, Rüdiger Kilian, Ronny Surey, Robert Mikutta, Klaus Kaiser, Carsten W. Mueller, Hans-Jörg Vogel
Publikováno v:
Nature Communications, Vol 13, Iss 1, Pp 1-14 (2022)
Carbon sequestration in soils has rarely been observed at microscopic scales. Here the authors reveal the impact of soil moisture regimes in shaping carbon stabilization and mineralization patterns tied to the pore network.
Externí odkaz:
https://doaj.org/article/41f09f6eeb0945c7bcf230b92ab341bd
Autor:
Helmut Geistlinger, Frederic Leuther
Publikováno v:
Vadose Zone Journal, Vol 17, Iss 1 (2018)
Evaporation—a key process for water exchange between soil and atmosphere—is controlled by convective and diffusive surface fluxes that determine the functional time dependence of the evaporation rate (). Recent studies demonstrated that only a po
Externí odkaz:
https://doaj.org/article/d96918dc18ff4670b78db4c5e0b1c4a0
Publikováno v:
Vadose Zone Journal, Vol 17, Iss 1 (2018)
X-ray radiography is a suitable approach to study water dynamics in undisturbed soil. However, beam hardening impairs the deduction of soil moisture changes from X-ray attenuation, especially when studying infiltration of water into cylindrical soil
Externí odkaz:
https://doaj.org/article/e72e9087724a453b978f3fb5f54b435d
Autor:
Frederic Leuther
Soil structure is a dynamic property of soils, which refers to temporal changes in the spatial arrangement of pores, organic matter, and minerals. As for many chemical reactions, also soil structure can be at a state of dynamic equilibrium, in which
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ca4ca984300bfb144e1322a267c49ecb
https://doi.org/10.5194/egusphere-egu23-15721
https://doi.org/10.5194/egusphere-egu23-15721
Soil structure is a key feature in controlling microbial access to organic matter in soils. The spatial arrangement of solids and pores in agricultural soils is shaped by the used tillage and crop system. However, spatial heterogeneities make it diff
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ba43fefbc0166205d96f12240a501817
https://doi.org/10.5194/egusphere-egu23-8157
https://doi.org/10.5194/egusphere-egu23-8157
Autor:
Tobias Ludwig Hohenbrink, Conrad Jackisch, Wolfgang Durner, Kai Germer, Sascha Christian Iden, Janis Kreiselmeier, Frederic Leuther, Johanna Clara Metzger, Mahyar Naseri, Andre Peters
Soil hydraulic properties (SHP), particularly soil water retention capacity and hydraulic conductivity of unsaturated soils, are among the key properties that determine the hydrological functioning of terrestrial systems. Some large collections of SH
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cebe6de06cd87cfe88ffd0572b371eb4
https://essd.copernicus.org/preprints/essd-2023-74/
https://essd.copernicus.org/preprints/essd-2023-74/
Soil structure is a dynamic property of soils, which refers to temporal changes in the spatial arrangement of pores, organic matter, and minerals. Its turnover, i.e. the irreversible redistribution of soil constituents, determines essential soil func
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::85da7694ba4a9fe77085eccce405297b
https://pub.epsilon.slu.se/31050/
https://pub.epsilon.slu.se/31050/
Autor:
Steffen Schlüter, Frederic Leuther
Publikováno v:
SOIL, Vol 7, Pp 179-191 (2021)
The ploughing of soils in autumn drastically loosens the soil structure and, at the same time, reduces its stability against external stresses. A fragmentation of these artificially produced soil clods during wintertime is often observed in areas wit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8fb9d3f2eebf44b235794c875e2a3178
https://doi.org/10.5194/soil-7-179-2021
https://doi.org/10.5194/soil-7-179-2021
Soil structure is a dynamic property of soils which undergoes continuous changes due to various abiotic and biotic drivers. At the same time, the spatial arrangement of pores, organic matter and minerals influences soil functions, such as storage and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b3922128770222bf0914355cc8396473
https://doi.org/10.5194/egusphere-egu22-1063
https://doi.org/10.5194/egusphere-egu22-1063