1933
DOI: 10.1002/jpln.19330310410
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Die Klassifikation der Böden auf Grund der Zusammensetzung ihrer Kolloidfraktion. V. Versuch einer allgemeinen Bodenklassifikation

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Cited by 1 publication
(2 citation statements)
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“…-Silicalsesquioxide ratios in the colloids The data in Table 5 show that the SiO,/R,O, ratio varies from 1-65 to 2.09 and there is no correlation with pH of the soil. This is contrary to Reifenberg's (1933) conclusion that the ratio should be about 2. Furthermore, no particular ratio is peculiar to any of the three regions of ItaIy studied.…”
Section: Some Chemical Characteristics Of Several Italian Red Earthscontrasting
confidence: 92%
See 1 more Smart Citation
“…-Silicalsesquioxide ratios in the colloids The data in Table 5 show that the SiO,/R,O, ratio varies from 1-65 to 2.09 and there is no correlation with pH of the soil. This is contrary to Reifenberg's (1933) conclusion that the ratio should be about 2. Furthermore, no particular ratio is peculiar to any of the three regions of ItaIy studied.…”
Section: Some Chemical Characteristics Of Several Italian Red Earthscontrasting
confidence: 92%
“…Many investigations of the problem have clearly shown that the red earths may not be identified only by their red colour. It has been suggested (Blanck, 1930;Reifenberg, 1933), without knowledge of the Italian soils, that the red earths may be characterized by a silica/sesquioxide ratio of approximately 2.…”
Section: Introductionmentioning
confidence: 99%