One of the chief characteristics of podsol soils is the accumulation of organic matter and sesquioxides in the B horizon of these soils. In recent years several workers have studied characteristics of soluble organic matter leaching from the overlying organic layer of these soils and passing downward through the profile. However, it has not been established that these organic materials or any part of these are deposited in the B horizon of podsol soils, or if the organic matter leached from the organic layer in aqueous solution is similar in nature to the organic matter deposited in the B horizon.
Identifer | oai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.110170 |
Date | January 1956 |
Creators | Coffin, David Earle. |
Contributors | DeLong, W.A. (Supervisor) |
Publisher | McGill University |
Source Sets | Library and Archives Canada ETDs Repository / Centre d'archives des thèses électroniques de Bibliothèque et Archives Canada |
Language | English |
Detected Language | English |
Type | Electronic Thesis or Dissertation |
Format | application/pdf |
Coverage | Master of Science. (Department of Agricultural Chemistry.) |
Rights | All items in eScholarship@McGill are protected by copyright with all rights reserved unless otherwise indicated. |
Relation | alephsysno: NNNNNNNNN, Theses scanned by McGill Library. |
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