The authors have presented a good paper with valuable information (Fonseca et al., 2014), yet the contributors here offer a simple discussion related to employing the method of Kézdi (1979) to assess the internal stability and to analyse the results of the methodology.ABOUT EMPLOYING THE METHOD OF KEZDI The method of Kézdi ððD 0 15 =d 0 85 Þ max , 4Þ is one of the earliest methods to assess the internal stability of granular soils. It is an easy method, yet not very accurate. Li (2008) indicated that the method of Kézdi is very successful in evaluating the internal stability of gap-graded soils but the method is conservative in evaluating the internal stability of widely graded soils. Dallo et al. (2013) used Kézdi's method to assess the internal stability of data based on 47 tests, and they found there were 16 wrong predictions (34% wrong predictions) (13 of them are for continuous-graded soils while just three are for gap-graded soils). Chang & Zhang (2013) Kenney & Lau (1985, 1986 or (D c35 /d f 85 ) min as suggested by Dallo et al. (2013). Because of the uncertainty associated with Kézdi's method, other methods are employed to assess the internal stability of the soils tested by the authors, namely Kenney & Lau (1985, 1986, Li & Fannin (2008) and Dallo et al. (2013) methods.The Kenney and Lau method is an accurate one, as stated by Li (2008), Indraratna et al. (2011 and Dallo et al. (2013). The method of Li and Fannin is also accurate and has been verified against a large number of field and laboratory tests (Li et al., 2009); it is currently being evaluated for adoption in engineering practice (Semar et al., 2010). The method of Dallo et al. (2013) gives very good assessment for the data set that was tested by them. The discussion considered here employed these three methods to evaluate the internal stability of the soils tested by the authors and the results are shown in Table 4. As can be seen, all the soils, except soil G1 for the medium layer, are classified as internally stable soils according to the three methods. Soil G1 for the medium layer is classified as internally unstable according to both the Kenney and Lau and the Li and Fannin methods, while it is classified as internally stable according to the Dallo et al. method. From all these results it is possible to conclude that the three soils are internally stable.Based on the internal stability assessment of Kézdi's method, as shown in Fig. 5 (in the paper under discussion), it can be seen that a value of Z > 5·75 is required for internally stable soils. Following the conclusion drawn from the internal stability assessment of the Kenney and Lau, Li and Fannin, and Dallo et al. methods, the coordination number associated with internal stability cannot be obtained from the experimental tests performed by the authors. Possibly more experiments are required for soils that are classified as internally unstable according to the Kenney and Lau, Li and Fannin, or Dallo et al. methods.
ABOUT THE METHODOLOGY FOR ANALYSIS OF THE RESULTSThe authors correlate ...