Zobrazeno 1 - 10
of 304
pro vyhledávání: '"F. C. Ugolini"'
Autor:
White, Sidney E.
Publikováno v:
Arctic and Alpine Research, 1972 Apr 01. 4(2), 177-180.
Externí odkaz:
https://www.jstor.org/stable/1550400
Autor:
Mansfield, A. W.
Publikováno v:
Arctic, 1968 Mar 01. 21(1), 55-55.
Externí odkaz:
https://www.jstor.org/stable/40507494
Autor:
Roberts, Brian
Publikováno v:
Journal of Animal Ecology, 1968 Oct 01. 37(3), 725-726.
Externí odkaz:
https://www.jstor.org/stable/3090
Autor:
Luisa Massaccesi, François Courchesne, Stefania Cocco, Giuseppe Corti, Alberto Agnelli, F. C. Ugolini
Publikováno v:
Geoderma. 289:82-96
The skeleton water-extractable fines (SWEF) is a soil fraction smaller than 2 mm located at the interface between rock fragments (RF) and fine earth (FE). It is made of illuvial and/or RF weathering products comprising neoformed clay-size particles a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::94d1f1d8765db4b5c3f4d33597c7918c
https://doi.org/10.1016/j.geoderma.2016.11.026
https://doi.org/10.1016/j.geoderma.2016.11.026
Publikováno v:
Communications in Soil Science and Plant Analysis. 41:72-87
Recycling organic waste in agricultural soils is a valid solution. We performed short‐term experiments to investigate the fate of urban sludge and composts, in mine spoils, cultivated or uncultivated, and reclaimed soils located in Florence and Mil
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::01d7a123caa16a31804ab94fa83697de
https://doi.org/10.1080/00103620903360288
https://doi.org/10.1080/00103620903360288
Autor:
James G. Bockheim, F. C. Ugolini
Publikováno v:
Geoderma. 144:1-8
The first mention of Antarctic soils dates back to 1916, when Jensen reported on analyses of samples collected in the McMurdo area during the British Antarctic Expedition, 1907–1909. With the advent of the International Geophysical Year in 1958, an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::72d2a0aa47c0014a97f3de9117c1f2e9
https://doi.org/10.1016/j.geoderma.2007.10.005
https://doi.org/10.1016/j.geoderma.2007.10.005
Publikováno v:
Geoderma. 142:112-126
Volcano flanks are usually covered by deposits of fine materials (tephra) with variable thickness originated by the explosive activity. The deposits form bedded sequences of tephra layers often alternated with paleosols. Pyroclastic successions on Et
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::680af0efed26c0b5268448989bd73687
https://doi.org/10.1016/j.geoderma.2007.08.003
https://doi.org/10.1016/j.geoderma.2007.08.003
Autor:
Ioana Taina, Giuseppe Corti, Giovanni Bolla, Giacomo Certini, Francesca Tescari, F. C. Ugolini
Publikováno v:
CATENA. 69:161-169
At about 1000 m above sea level in the Vallombrosa Forest, northern Apennines, Central Italy, a dense pan that meets the diagnostic criteria for fragipans is discontinuously distributed. The unusual slope-parallel “digitate” distribution of the p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8dffeb235c0aa8f36343972478bfbccd
https://doi.org/10.1016/j.catena.2006.05.005
https://doi.org/10.1016/j.catena.2006.05.005