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Microstructural studies on recycled aggregate concrete            427


           embedded with low-viscosity epoxy resin. This stabilises the sample by filling pores
           and cracks so that it better withstands stresses imposed during grinding and polish-
           ing as well as preserving the original microstructure and distribution of components
           by minimising debonding of particles from softer phases (Detwiler et al., 2001;
           Jana, 2006). After resin hardening, samples for metallographic examination are
           mechanically ground and polished with progressively finer abrasives. Etching or
           staining follows to selectively develop characteristic colours for the different phases
           of concrete, allowing their identification (Jana, 2006). Petrographic examination
           requires production of thin sections through which light can be transmitted (Jana,
           2006). After epoxy curing the sample is further mounted on a glass microscope
           slide, cut to a thickness of approximately 1 mm and then ground to a final thickness
           around 20 μm. The resolution limit in OM is approximately 0.2 μm, restraining the
           practical magnification limit to B1500 3 (Holik, 1993). Petrographic examination
           is preferable over metallographic examination in determining the abundance of fine
           features such as fly ash particles, residual unhydrated cement grains or primary calcium
           hydroxide (Jana, 2006). Overall, OM allows to examine the large-scale features and
           relationships in concrete, providing information on compositional, textural, minera-
           logical, and microstructural properties at the submillimetric and microscale (Jana, 2006).


           14.2.2 Scanning electron microscopy
           High magnification and spatial resolution higher than those produced by optical
           microscopes are necessary to resolve the details of individual features of concrete
           (Diamond, 2004), featuring the use of scanning electron microscopy (SEM) since
           the early 1970s (Diamond, 1972, 1976; Diamond et al., 1974). SEM produces
           images by probing the sample with a focused beam of electrons, which interact
           with atoms in the surface to produces various signals that contain information about
           the material (Goldstein et al., 1981). Depending on the specific equipment magnifi-
           cation in the 100,000 3 order of magnitude is possible, which is at least two orders
           of magnitude higher than that achievable with the best optical microscopes
           (Goldstein et al., 1981; Pham et al., 2011). Additionally, SEM equipment can be
           coupled to chemical analysis apparatus, either energy dispersive X-ray spectroscopy
           (EDS) or wavelength dispersive X-ray spectroscopy, to detect the characteristic X-
           rays produced by interaction of electrons with the sample material. This allows an
           estimate to be made on the abundance and distribution of elements in the sample
           surface. While early SEM studies were mainly carried out in secondary electron
           (SE) mode, the use of backscattered electrons came into play (Scrivener and
           Gartner, 1987) and were generalised in the mid-1980s. SE images result from
           inelastic interaction of the electron beam with the surface (Goldstein et al., 1981)
           rendering information on morphological features (namely size, shape and distribu-
           tion) of constituents. SE is adequate for observation of flat surfaces and fracture
           surfaces of cementitious materials, revealing a wealth of information such as types
           of aggregates, mineralogical and textural properties of the paste, bond between
           aggregates and paste, secondary deposits in voids and cracks, pore distribution, and
           areas of interest to be further examined by compositional analysis (Jana, 2006).
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