“…Other disadvantages of the CT were suggested by Wigum et al (1997), who pointed out an original restriction of the test only on aggregates containing amorphous varieties of SiO 2 and an influence of variable aggregate grading and the presence of minor or trace amounts of dust influencing the amount of dissolved silica. Ramos (2013) found CT to be poorly sensitive to slowly reactive granitic aggregates. Rolim et al (2012) suggested increasing the grain size of aggregates used in the CT to 0.3/1.18 mm and to prolonge the test period up to 168 h. quartzite (Q0B, f-j), quartz meta-greywacke (Q7C, k-o), and chert (Q3, p-t) taken from aggregate sections unaffected by ASR (a, f, k, p), and from AMBs after 1 (b, g, l, q), 5 (c, h, m, r), 9 (d, i, n, s), and 14 (e, j, o, t) days of testing Quantitative assessment of alkali silica reaction potential of quartz-rich aggregates: comparison… Although the AMBT gives a clear distinction between reactive and non reactive aggregates, it has been criticised in recent studies (e.g., Shayan and Morris 2001;Lindgård et al 2010;Ramos et al 2011).…”