Citation
M. De Boodt, . and A. M. Mokhtaruddin, . Evaluation of sensitivity to slaking by bulk density measurements of disrupted fragments (aggregates). pp. 90-94. ISSN 0126-6128
Abstract
The study shows that other than the four factors viz: slaking dispersion carbonate or gypsum content and flocculation the size and bulk density of disrupted aggregates are also important when classifying the soils into their corresponding water coherence classes. It was found that for the Ultisols and the Oxisols the aggregates will not slake further if they have a size of 1 mm and a bulk density of at least 1.7g cm3.
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Abstract
The study shows that other than the four factors viz: slaking dispersion carbonate or gypsum content and flocculation the size and bulk density of disrupted aggregates are also important when classifying the soils into their corresponding water coherence classes. It was found that for the Ultisols and the Oxisols the aggregates will not slake further if they have a size of 1 mm and a bulk density of at least 1.7g cm3.
Additional Metadata
| Item Type: | Article |
|---|---|
| AGROVOC Term: | Bulk density (soil) |
| AGROVOC Term: | Dispersions |
| AGROVOC Term: | Carbonates |
| AGROVOC Term: | Gypsum |
| AGROVOC Term: | Flocculation |
| AGROVOC Term: | Soil aggregates |
| AGROVOC Term: | Diameter |
| AGROVOC Term: | Soil erosion |
| AGROVOC Term: | Aluminium |
| AGROVOC Term: | Soil organic matter |
| Geographical Term: | Malaysia |
| Depositing User: | Ms. Suzila Mohamad Kasim |
| Last Modified: | 28 Apr 2025 00:40 |
| URI: | http://webagris.upm.edu.my/id/eprint/22901 |
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