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Resonant frequency ultrasonic p-waves for evaluating uniaxial compressive strength of the stabilized slag-cement sediments
Lindh, P.; Lemenkova, P. (2021). Resonant frequency ultrasonic p-waves for evaluating uniaxial compressive strength of the stabilized slag-cement sediments. Nordic Concrete Research 65(2): 39-62. https://dx.doi.org/10.2478/ncr-2021-0012
In: Nordic Concrete Research. Sciendo: Warsaw. ISSN 0800-6377; e-ISSN 2545-2819, more
Peer reviewed article  
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Keyword
    Marine/Coastal
Author keywords
    civil engineering; geophysics; seismicity; cement; slag; geotechnical engineering
Authors  Top 
  • Lindh, P.
  • Lemenkova, P., more
Abstract
    Marine sediments can be stabilized by ultra high-strength binders: cement, Cement Kiln Dust (CKD) and slag. The properties of the stabilized soil indicate potential to their reuse. This study investigated the performance of the unconfined compressive strength (UCS) in the marine sediments stabilized by binder (cement, CKD, slag), tested by ultrasonic P-waves. Materials include 194 specimens collected from the port of Gothenborg. The experiment was performed in Swedish Geotechnical Institute (SGI). The UCS of specimens stabilized by different ratio of binders (cement, CKD, slag) was tested by resonance frequencies of the elastic P-waves. The significant increase in the UCS (>1500 kPa) was recorded for the highest values of CKD and cement, and low values of slag. The correlation profiles of low water/high binder (LW/HB) cement/slag (40/60%) were controlled by curing time. The slag–cement–CKD simplex tests demonstrated UCS of samples with low/high water content and various binder ratio of cement (kg/m3). The ratio of cement binder and curing time play a critical role in the increase of UCS followed by mechanical properties of specimens and intensity of stress. The highest values exceed 1000 m/s in P-waves. The results shown high accuracy (97%) and non-contacting approach for testing UCS of sediments. Seismic methods can be applied to test the UCS of the stabilized sediments, and also in-situ via seismic CPT, surface testing or cross hole seismic testing.
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