Abstract
The macrostructures, visible to the naked eye or with a lens not exceeding 4 x linear were divided into two large groups: those consisting of structural elements and those without these units.
A more detailed classification of the elements, formed by geological processes, was found necessary. Special attention was paid to the internal porosity of the elements and to the occurrence of various types of coatings and root prints.
The concept of grade of structure was discussed, and a scheme of description modified.
A classification of structures without structural elements was developed in which emphasis was placed on porosity.
Samples of higher sandy soils, underlying forest and heath, were described to demonstrate specific microstructures seen in thin sections.
Brown podsolic soils and podsols were shown to have characteristic differences in the morphology and mechanical behaviour of humus components.
Original language | Dutch |
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Qualification | Doctor of Philosophy |
Awarding Institution | |
Supervisors/Advisors |
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Award date | 12 Jul 1957 |
Place of Publication | 's-Gravenhage |
Publisher | |
DOIs | |
Publication status | Published - 12 Jul 1957 |
Keywords
- soil structure
- aggregates
- soil analysis
- soil texture
- soil mechanics
- particle size distribution