Evaluation of Sensitivity to Slaking by Bulk Density Measurements of Disrupted Fragments (Aggregates)
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 Ultis...
| Main Authors: | , |
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| Format: | Article |
| Language: | English English |
| Published: |
1983
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| Online Access: | http://psasir.upm.edu.my/id/eprint/2188/ http://psasir.upm.edu.my/id/eprint/2188/1/Evaluation_of_Sensitivity_to_Slaking_by_Bulk_Density.pdf |
| _version_ | 1848839176585216000 |
|---|---|
| author | Mokhtaruddin, A.M Boodt, M |
| author_facet | Mokhtaruddin, A.M Boodt, M |
| author_sort | Mokhtaruddin, A.M |
| building | UPM Institutional Repository |
| collection | Online Access |
| description | 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 ofat least
1.7 g cm-3 |
| first_indexed | 2025-11-15T07:07:17Z |
| format | Article |
| id | upm-2188 |
| institution | Universiti Putra Malaysia |
| institution_category | Local University |
| language | English English |
| last_indexed | 2025-11-15T07:07:17Z |
| publishDate | 1983 |
| recordtype | eprints |
| repository_type | Digital Repository |
| spelling | upm-21882013-05-27T06:59:25Z http://psasir.upm.edu.my/id/eprint/2188/ Evaluation of Sensitivity to Slaking by Bulk Density Measurements of Disrupted Fragments (Aggregates) Mokhtaruddin, A.M Boodt, M 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 ofat least 1.7 g cm-3 1983 Article NonPeerReviewed application/pdf en http://psasir.upm.edu.my/id/eprint/2188/1/Evaluation_of_Sensitivity_to_Slaking_by_Bulk_Density.pdf Mokhtaruddin, A.M and Boodt, M (1983) Evaluation of Sensitivity to Slaking by Bulk Density Measurements of Disrupted Fragments (Aggregates). Pertanika, 6 (3). pp. 90-94. English |
| spellingShingle | Mokhtaruddin, A.M Boodt, M Evaluation of Sensitivity to Slaking by Bulk Density Measurements of Disrupted Fragments (Aggregates) |
| title | Evaluation of Sensitivity to Slaking by Bulk Density
Measurements of Disrupted Fragments (Aggregates) |
| title_full | Evaluation of Sensitivity to Slaking by Bulk Density
Measurements of Disrupted Fragments (Aggregates) |
| title_fullStr | Evaluation of Sensitivity to Slaking by Bulk Density
Measurements of Disrupted Fragments (Aggregates) |
| title_full_unstemmed | Evaluation of Sensitivity to Slaking by Bulk Density
Measurements of Disrupted Fragments (Aggregates) |
| title_short | Evaluation of Sensitivity to Slaking by Bulk Density
Measurements of Disrupted Fragments (Aggregates) |
| title_sort | evaluation of sensitivity to slaking by bulk density
measurements of disrupted fragments (aggregates) |
| url | http://psasir.upm.edu.my/id/eprint/2188/ http://psasir.upm.edu.my/id/eprint/2188/1/Evaluation_of_Sensitivity_to_Slaking_by_Bulk_Density.pdf |