Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Laura V. Krone"'
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 15, Pp n/a-n/a (2024)
Abstract Along a climate gradient in the Chilean coastal mountains, we investigated denudation rates using the meteoric cosmogenic nuclide 10Be and its ratio to stable 9Be, and chemical depletion fractions (CDFs) in bulk soil samples. We find that th
Externí odkaz:
https://doaj.org/article/842312441ee3435bba2d837e73e0c6f9
Autor:
Laura V. Krone, Ferdinand J. Hampl, Christopher Schwerdhelm, Casey Bryce, Lars Ganzert, Axel Kitte, Kirstin Übernickel, Armin Dielforder, Santiago Aldaz, Rómulo Oses-Pedraza, Jeffrey Paulo H. Perez, Pablo Sanchez-Alfaro, Dirk Wagner, Ute Weckmann, Friedhelm von Blanckenburg
Publikováno v:
Scientific Reports, Vol 11, Iss 1, Pp 1-15 (2021)
Abstract The weathering front is the boundary beneath Earth’s surface where pristine rock is converted into weathered rock. It is the base of the “critical zone”, in which the lithosphere, biosphere, and atmosphere interact. Typically, this fro
Externí odkaz:
https://doaj.org/article/127a87e9c54f4c688f95e83536c76b35
The weathering front, the interface beneath Earth’s surface where unweathered bedrock is converted into weathered rock, is a zone where chemical disequilibrium results in some of the most intense mineralogical transformations. These are focused int
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::07b6bd0e59c9c391ab6cd778753c3a2e
https://doi.org/10.5194/egusphere-egu21-9541
https://doi.org/10.5194/egusphere-egu21-9541
Autor:
Ute Weckmann, Lars Ganzert, Jeffrey Paulo H. Perez, Santiago Aldaz, Ferdinand Hampl, Christopher Schwerdhelm, Pablo Sanchez-Alfaro, Laura V. Krone, Rómulo Oses-Pedraza, Dirk Wagner, Armin Dielforder, Axel Kitte, Friedhelm von Blanckenburg, Casey Bryce, Kirstin Übernickel
Publikováno v:
Scientific Reports
Scientific Reports, Vol 11, Iss 1, Pp 1-15 (2021)
Scientific Reports, Vol 11, Iss 1, Pp 1-15 (2021)
The weathering front, the boundary beneath Earth’s surface where unweathered bedrock is converted into weathered rock, is the base of the critical zone. Typically, this front is located no more than 20 m deep in granitoid rock in humid climate zone
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::32eac97429e1aa045c7e9176d6998fb5
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5006658_1/component/file_5007108/5006658.pdf
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5006658_1/component/file_5007108/5006658.pdf