Výsledky vyhledávání - "S. B. Edinger"

Gravel dispersion on a granite pediment (East Mojave Desert, California): a short-term look at erosional processes

Autor: S. B. Edinger-Marshall, L. J. Lund

Publikováno v: Earth Surface Processes and Landforms. 24:349-359

Hypotheses about the influence of surface shape, landscape unit and vegetation cover on gravel dispersion were tested on a shallowly dissected portion of a low-sloping granite pediment in the East Mojave Desert of California. Painted gravels (2 to 20

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::87f3f4b2ae14bc7fe1a045f5b3927794
https://doi.org/10.1002/(sici)1096-9837(199904)24:4<349::aid-esp971>3.0.co

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Block Diagrams and Soil Profile Characteristics in Soil Genesis and Classification Courses

Autor: S. B. Edinger, L. J. Lund

Publikováno v: Journal of Agronomic Education. 20:86-92

One objective of a soil morphology, genesis, and classification course is to teach students how to generate reasonable hypotheses to explain soil distributions on landscapes. By the end of the course, students can begin to make predictions regarding

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::4185c43bbaedcb61c91cf8690d90deee
https://doi.org/10.2134/jae1991.0086

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Celadonite and its Transformation to Smectite in an Entisol at Red Rock Canyon, Kern County, California

Autor: D. A. Reid, Robert C. Graham, L. H. Bowen, S. B. Edinger, Jarel O. Ervin

Publikováno v: Clays and Clay Minerals. 36:425-431

A green, Lithic Torriorthent soil derived from a celadonite-rich, hydrothermaUy altered basalt immediately north of the Mojave Desert region in southern California was studied to investigate the fate of the celadonite in a pedogenic weathering enviro

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::92b06dbb791c68c2e93c9ff0613847cd
https://doi.org/10.1346/ccmn.1988.0360507

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M�ssbauer study of a California desert celadonite and its pedogenically-related smectite

Autor: L. H. Bowen, S. B. Edinger, Robert C. Graham, E. DeGrave, D. A. Reid

Publikováno v: Physics and Chemistry of Minerals. 16

Celadonite from the northwestern Mojave Desert area of California was examined by detailed Mossbauer spectroscopy at temperatures from 10 K to 400 K. In addition to the predominant Fe3+ doublet with isomer shift δ∼0.4 mm s−1 and quadrupole split

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::fa2e867af00a2a46504cb6d5a206bcda
https://doi.org/10.1007/bf00223320

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