Zobrazeno 1 - 10
of 48
pro vyhledávání: '"R. J. St. Arnaud"'
Autor:
R. J. St. Arnaud, E. P. Whiteside
Chemical, physical, and micropedological studies were made of Orthic Black, Orthic Dark Grey, Dark Grey Wooded, and Orthic Grey Wooded profiles developed from relatively uniform glacial till material. The general gradation of morphological properties
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::99ee75cef587a08256f6459fce472d61
https://doi.org/10.2136/sssaspecpub1.c29
https://doi.org/10.2136/sssaspecpub1.c29
Publikováno v:
Soil Science Society of America Journal. 56:193-201
Publikováno v:
Soil Science. 149:112-120
Publikováno v:
Soil Science Society of America Journal. 54:281-287
Publikováno v:
Canadian Journal of Soil Science. 69:629-637
The soil macropore system was analyzed with the help of image analysis, comparing images from computed-tomography (CT) scanning with images obtained from thin sections. The images obtained with the two methods were analyzed with an image analyzer (IB
Autor:
A. R. Mermut, R. J. St. Arnaud
Publikováno v:
Soil Science Society of America Journal. 47:536-541
Two clayey soils (Indian Head and Balcarres Associations) and two fine loamy soils (Swinton and Weyburn Associations), all currently classified under the Chernozemic order (Borolls), were used in this study to establish the micromorphology of soils w
Publikováno v:
Soil Science Society of America Journal. 53:575-582
Publikováno v:
Soil Science Society of America Journal. 48:613-620
Seven termite mounds built by three Macrotermes species (M. michaelseni, M. subhyalinus, and M. herus) at five different sites were studied micropedologically. Construction units and void patterns were considered as integral parts of mound constructi
Autor:
R. J. St. Arnaud, A. R. Mermut
Publikováno v:
Canadian Journal of Soil Science. 61:243-260
The nature and distribution of carbonates in calcareous horizons from several Saskatchewan soils were examined micromorphologically. Carbonate minerals were found to occur in several distinct forms which included skeletal grains and plasma, cutanic a
Publikováno v:
Canadian Journal of Soil Science. 54:447-456
The Ah horizons of a Brown–Dark Brown–Black–Dark Gray–Gray Luvisolic sequence of Canadian grassland and forest soils were studied. Clay-associated humus was present in greater proportions in the grassland than in forest soils, particularly in