Road construction requires a prime quality and a tremendous amount of aggregates, within which their quality is set by geological and geotechnical properties. Therefore, the Mesozoic limestone was studied in the vicinity of Harer and Dire Dawa towns, for the fundamental engineering assessments.
Thirty-seven Mesozoic limestone samples obtained from the area were subjected to petrographic and geotechnical analyses to work out the suitability of the rock as a road aggregate. Physical properties were investigated using ultrasonic pulse velocity (UPV), water absorption, Na2So4 soundness, and specific gravity tests. However, the mechanical properties were determined using unconfined compressive strength (UCS), Aggregate crushing value (ACV), Aggregate Impact Value (AIV), and Los Angles Abrasion value (LAAV).
The study aimed to see if the limestone aggregate complies with the globally accepted standards by employing geotechnical laboratory analyses and petrographic examination.
The petrographic observations reveal the Mesozoic limestones of the area are dominantly composed of micrite, sparite, and bioclasts with subordinate intraclasts, ooids, Fe-oxides, and dolomites. Results of the physical properties show the rock has a mean UPV of 4859 m/s, a dry specific gravity of 2.64, and very low water absorption ranging from 0.2-5.7%, and Na2So4 soundness ranges from 1-14%. Among the mechanical properties, UCS, AIV, ACV, and LAAV range from 20.5-180.5Mpa, 8-20%, 24-34%, and 18.9-31.1%, respectively.
Based on the aforementioned results, the limestones of the area are suitable for aggregate in road construction as they’re complying with ERA, AASHTO, ASTM, and BS standards used for pavement works.

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Figure 7
This is a list of supplementary files associated with this preprint. Click to download.
Plates 1-2. The photomicrographs of (1) ML-29 (M=Medium grained micritic groundmass, long stick-like bi-valves (white arrows)), (2) sample #17 (Fe-oxides along the pressure solution seam (white arrow), M=Fine grained micritic groundmass)
Plates 3-4. The photomicrographs of (3) sample CL-90, (4) sample #72
Plates 5-6. The photomicrographs of (5) sample ML-28, and (6) sample 86
Plates 7-8. The photomicrographs of (7) ML-24 with rhombohedral dolomite crystals (white arrows) and D (dolomite) (8) fossiliferous micritic limestone of sample #70 with dominant pressure solution and oxidation along the pressure solution seam (yellow arrow) F-Foraminifera, B-Bryozoans, C-Calcispheres.
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Posted 19 Jan, 2021
Posted 19 Jan, 2021
Road construction requires a prime quality and a tremendous amount of aggregates, within which their quality is set by geological and geotechnical properties. Therefore, the Mesozoic limestone was studied in the vicinity of Harer and Dire Dawa towns, for the fundamental engineering assessments.
Thirty-seven Mesozoic limestone samples obtained from the area were subjected to petrographic and geotechnical analyses to work out the suitability of the rock as a road aggregate. Physical properties were investigated using ultrasonic pulse velocity (UPV), water absorption, Na2So4 soundness, and specific gravity tests. However, the mechanical properties were determined using unconfined compressive strength (UCS), Aggregate crushing value (ACV), Aggregate Impact Value (AIV), and Los Angles Abrasion value (LAAV).
The study aimed to see if the limestone aggregate complies with the globally accepted standards by employing geotechnical laboratory analyses and petrographic examination.
The petrographic observations reveal the Mesozoic limestones of the area are dominantly composed of micrite, sparite, and bioclasts with subordinate intraclasts, ooids, Fe-oxides, and dolomites. Results of the physical properties show the rock has a mean UPV of 4859 m/s, a dry specific gravity of 2.64, and very low water absorption ranging from 0.2-5.7%, and Na2So4 soundness ranges from 1-14%. Among the mechanical properties, UCS, AIV, ACV, and LAAV range from 20.5-180.5Mpa, 8-20%, 24-34%, and 18.9-31.1%, respectively.
Based on the aforementioned results, the limestones of the area are suitable for aggregate in road construction as they’re complying with ERA, AASHTO, ASTM, and BS standards used for pavement works.

Figure 1

Figure 2

Figure 3

Figure 4

Figure 5

Figure 6

Figure 7
This is a list of supplementary files associated with this preprint. Click to download.
Plates 1-2. The photomicrographs of (1) ML-29 (M=Medium grained micritic groundmass, long stick-like bi-valves (white arrows)), (2) sample #17 (Fe-oxides along the pressure solution seam (white arrow), M=Fine grained micritic groundmass)
Plates 3-4. The photomicrographs of (3) sample CL-90, (4) sample #72
Plates 5-6. The photomicrographs of (5) sample ML-28, and (6) sample 86
Plates 7-8. The photomicrographs of (7) ML-24 with rhombohedral dolomite crystals (white arrows) and D (dolomite) (8) fossiliferous micritic limestone of sample #70 with dominant pressure solution and oxidation along the pressure solution seam (yellow arrow) F-Foraminifera, B-Bryozoans, C-Calcispheres.
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