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Volumetric Balance and Marshall Response of AC-WC Mixtures Incorporating Kampar River Sand as a Partial Replacement for Stone Dust Cover

Volumetric Balance and Marshall Response of AC-WC Mixtures Incorporating Kampar River Sand as a Partial Replacement for Stone Dust

Open Access
|Sep 2026

Figures & Tables

Table 1:

Main properties of the constituent aggregate materials

Material/propertyBulk specific gravitySSD specific gravityApparent specific gravityAbsorption/result [%]
Crushed aggregate, 19 mm2.4772.5232.5981.881
Crushed aggregate, 12 mm2.5542.5712.5980.659
Stone dust2.6312.6322.6330.040
Kampar River sand2.5802.6302.7202.040
Los Angeles abrasion [%]---27.18
Table 2:

Characteristics and processing temperatures of the 60/70 penetration-grade binder

Property/processStandardTest conditionResult
PenetrationSNI 2456:201125 °C, 5 s61.4 [0.1 mm] (6.14 mm)
Softening pointSNI 2434:2011Initial water temperature 25 °C; two results48.15 [°C] (48.25; 48.05)
DuctilitySNI 2432:201125 °C; pulling rate 5 cm/min146.5 [cm]
Kinematic viscositySNI 06-6837-2002 / ASTM D2170135 °C300 [cSt] (300 mm2/s)
Mixing temperatureLaboratory procedureRecorded operating temperature160 [°C]
Compaction temperatureLaboratory procedureRecorded operating range140–150 [°C]
Binder specific gravitySNI 2441:2011 / ASTM D7025 °C1.030 [g/cm3] (1.03 kg/L)

* Note. The reported softening point is the mean of two measurements, 48.25 and 48.05 °C. The equivalent units 300 cSt and 300 mm2/s are both provided for clarity. A value of Gb = 1.030 was used in all volumetric calculations.

Table 3:

Aggregate proportions during the replacement stage

Fine-fraction replacement [%]19-mm aggregate [%]12-mm aggregate [%]Stone dust [%]River sand [% of total aggregate]River sand [%] of fine fraction
013.0026.0061.000.000
513.0026.0057.953.055
1013.0026.0054.906.1010
1513.0026.0051.859.1515
2013.0026.0048.8012.2020
Figure 1:

Recalculated combined gradations at the five river-sand replacement levels

Figure 2:

Fine materials used in the study: (a) stone dust and (b) Kampar River sand

Figure 3:

Source location of Kampar River sand: (a) Sumatra context, (b) regional Riau context, and (c) the Danau Bingkuang Kampar River corridor. Base map: Google Maps; location information provided by PT Sumber Mineral Riau; adapted by the authors

Figure 4:

Documentation of materials, compacted specimens, and Marshall testing: (a) aggregate weighed and packaged by batch, (b) compacted Marshall specimens, and (c) loading apparatus

Figure 5:

Marshall indicator curves used to determine the optimum binder content (binder content 5.0–6.5%)

Table 4:

Recalculated combined gradations and the adopted AC-WC specification envelope

Sieve size [mm]Passing, 0% [%]Passing, 5% [%]Passing, 10% [%]Passing, 15% [%]Passing, 20% [%]Lower limit [%]Upper limit [%]
4.75061.8762.2662.6563.0463.435369
2.36046.5646.9547.3447.7348.123353
1.18034.8935.5436.1836.8337.472140
0.60027.4627.4527.4427.4327.411430
0.30015.7715.5515.3315.1114.89922
0.1507.917.617.317.016.71615
0.0755.955.675.395.104.8249

* Note. The recalculated gradations account for the contribution of all four aggregate components at each sieve size. As shown in Table 4 and Figure 1, every mixture remained within the adopted AC-WC gradation envelope.

Table 5:

Specimen-level data from separate batches at binder contents of 5.9 and 6.0%

Binder content [%]SpecimenGmbGmmVIM [%]VMA [%]VFA [%]Stability [kg] / Flow [mm] / MQ [kg/mm]
5.912.2992.4014.2616.4574.131351.3 / 3.15 / 428.98
5.922.2972.4014.3216.5173.801322.2 / 3.11 / 425.15
5.932.2972.4014.3416.5273.751394.9 / 3.21 / 434.54
5.9Mean2.2982.4014.3116.4973.891356.1 / 3.16 / 429.61
6.012.3062.3973.7916.2776.691060.7 / 3.10 / 342.16
6.022.3072.3973.7716.2576.811176.9 / 3.05 / 385.88
6.032.3082.3973.7316.2277.001133.3 / 3.05 / 371.59
6.0Mean2.3072.3973.7616.2576.831123.7 / 3.07 / 366.41
Figure 6:

Effect of river-sand replacement on mean Marshall stability and Marshall quotient

Figure 7:

Mean VMA and VIM responses relative to the adopted specification limits

Table 6:

Marshall results at 5.9% binder content, reported as the mean ± standard deviation of three specimens

Replacement [% of fine fraction]Gmm*GsbGmbStability [kg]Flow [mm]MQ [kg/mm]VMA [%]VFA [%]VIM [%]Pbe [%] **
02.4012.5892.298 ± 0.0011356.13 ± 36.593.16 ± 0.05429.56 ± 4.7216.49 ± 0.0473.89 ± 0.214.31 ± 0.045.462
52.4012.5882.313 ± 0.0021951.87 ± 58.713.12 ± 0.02626.30 ± 20.3815.91 ± 0.0776.88 ± 0.423.68 ± 0.085.448
102.4012.5862.319 ± 0.0091753.30 ± 160.073.45 ± 0.04508.31 ± 47.5915.60 ± 0.3278.24 ± 1.873.40 ± 0.365.419
152.4012.5852.351 ± 0.0012063.27 ± 38.483.70 ± 0.01557.62 ± 8.9714.42 ± 0.0385.55 ± 0.202.08 ± 0.035.404
202.4012.5832.355 ± 0.0011869.53 ± 183.953.84 ± 0.03487.49 ± 51.0114.21 ± 0.0486.50 ± 0.271.92 ± 0.045.375
Specification---≥ 8002–4≥ 250≥ 15≥ 653–5-

* Note. Results are reported as the mean ± standard deviation of three independent batches. *The appendix reported Gmm = 2.401 for all mixtures, whereas Gsb was calculated or reported separately for each composition. VIM, VMA, and VFA were recalculated from specimen-level Gmb.

** Pbe was derived from Gse = 2.6196 and the Gsb of each composition; it was not measured directly. Gmm should still be verified for each composition before these data are used as the basis for a field mixture design.

Table 7:

Specimen-level Gmb and Gmm data for the replacement stage at 5.9% binder content

Replacement [% fine fraction]SpecimenGsbGmbGmmVIM [%]VMA [%]VFA [%]
012.5892.2992.4014.2516.4674.21
022.5892.2972.4014.3116.5273.89
032.5892.2972.4014.3316.5373.83
512.5882.3122.4013.7015.9976.81
522.5882.3152.4013.5815.8877.59
532.5882.3112.4013.7416.0276.59
1012.5862.3092.4013.8116.0876.32
1022.5862.3252.4013.1615.5179.63
1032.5862.3242.4013.2015.5579.44
1512.5852.3502.4012.1114.5985.57
1522.5852.3512.4012.0714.5785.77
1532.5852.3522.4012.0414.5485.97
2012.5832.3542.4011.9514.4686.50
2022.5832.3562.4011.8714.3987.03
2032.5832.3552.4011.9014.4286.79

* Note. VIM, VMA, and VFA were recalculated using the composition-specific Gsb values, specimen-level Gmb values, and the Gmm value reported in the laboratory appendix. Because composition-specific Gmm values were not available, the table supports transparency of the current calculation basis but does not replace the need for future Gmm verification.

Table 8:

Compact pass/fail summary for the adopted Marshall and volumetric criteria

Replacement [% fine fraction]Stability ≥ 800 kgFlow 2–4 mmMQ ≥ 250 kg/mmVMA ≥ 15%VFA ≥ 65%VIM 3–5%Overall
0PassPassPassPassPassPassPass
5PassPassPassPassPassPassPass
10PassPassPassPassPassPassPass
15PassPassPassFailPassFailFail
20PassPassPassFailPassFailFail

* Note. Pass/fail status was assigned from the mean values in Table 6 and the adopted limits used in this study. The 15 and 20% mixtures failed overall because their VMA and VIM values were below the specified limits, even though their mechanical indicators satisfied the adopted thresholds.

Table 9:

Table caption, the numbering is automatic, use “Update Field”

Responsedf1df2FpEta-squared
Gmb [-]410111.949< 0.0010.978
Stability [kg]41016.911< 0.0010.871
Flow [mm]410319.646< 0.0010.992
MQ [kg/mm]41015.372< 0.0010.860
VMA [%]410131.026< 0.0010.981
VFA [%]410120.855< 0.0010.980
VIM410111.949< 0.0010.978

* Note. Eta-squared represents the proportion of total variation associated with replacement level. The ANOVA for Gmb, VMA, VFA, and VIM was recalculated from specimen-level mass data using the composition-specific Gsb values. The large effect sizes should not be interpreted as overcoming the limitations of the small number of replicates or the need to verify Gmm for each composition.

DOI: https://doi.org/10.2478/cee-2027-0021 | Journal eISSN: 2199-6512 (formerly 1336-5835) | Journal ISSN: 1336-5835
Language: English
Submitted on: Jul 12, 2026
Accepted on: Aug 6, 2026
Published on: Sep 17, 2026
Published by: University of Žilina
In partnership with: Paradigm Publishing Services
Publication frequency: 4 issues per year

© 2026 Doni Rinaldi Basri, Rahmat Tisnawan, Novreta Ersyi Darfia, Zulham Shadri, published by University of Žilina
This work is licensed under the Creative Commons Attribution 4.0 License.