Geotechnical index properties. Soil House Specific gravity, Gs Material finer than
Geotechnical index properties. Soil Home Distinct gravity, Gs Material finer than four.75 mm Material finer than 0.075 mm Material finer than 0.002 mm Liquid limit, wl Plastic limit, wp Shrinkage limit, ws USCS symbol Worth 2.72 one hundred 51 18 29 15 12 CLGeosciences 2021, 11, x FOR PEER REVIEW6 ofFigure Figure two. Grain size distribution of the the investigatedtill. till. 2. Grain size distribution of investigated clay clay4.two. Soil and Pore Water Compositions Figure three plots the X-ray diffraction patterns of investigated clay till. The coarse Aztreonam Autophagy sample (Figure 3a) showed quartz with diffraction peaks at 24.4 31.2 42.9 and 59.1 This validated the accuracy from the analyses for other minerals [10]. The existence of quartz in-Geosciences 2021, 11,six ofFigure two. Grain size distribution with the investigated clay till.four.two. Soil and Pore Water Compositions 4.two. Soil and Pore Water Compositions Figure three plots the X-ray diffraction patterns of investigated clay till. The coarse samFigure 3 showed X-ray diffraction patterns of investigated 42.9 and 59.1 This ple (Figure 3a) plots thequartz with diffraction peaks at 24.four 31.two clay till. The coarse sample (Figure 3a) showed quartz with diffraction peaks[10]. The, existence of, quartz in-. validated the accuracy of your analyses for other minerals at 24.four 31.two , 42.9 and 59.1 This validated the accuracy on the the investigated minerals [10]. The existence of quartz dicated the sedimentary origin of analyses for othertill [55]. Likewise, calcite at 34.4and indicated the sedimentary origin of related to deposition of Likewise, compounds and dolomite at 36.3in the sample would be the investigated till [55]. calcareouscalcite at 34.4 from dolomite at 36.3 inside the sample are associated feldspars (K-feldspar at 25.8and plagioclase seawater [56]. Additionally, several sorts ofto deposition of calcareous compounds from seawater [56]. Additionally, various sorts of feldspars (K-feldspar at 25.eight and plagioclase at 27.7and 32.7 are associated towards the deposition of volcanic debris in the Cretaceous period at 27.7 and 32.7 ) are related towards the deposition of volcanic debris inside the Cretaceous period and subsequent weathering throughout the Quaternary period. and subsequent weathering through the Quaternary period.Geosciences 2021, 11, x FOR PEER REVIEW7 of(a)(b)Figure 3. Figurediffraction patterns of investigated clay till: (a) coarse(a) coarse(b) clay sample. sample. X-ray three. X-ray diffraction patterns of investigated clay till: sample, sample, (b) clayThe clayThe clay (Figure 3b) showed showed the presence of corrensite (smectite hlorite sample sample (Figure 3b) the presence of corrensite (smectite hlorite mixed layer) that generally formshydrothermal metamorphism happens beneath low mixed layer) that Sutezolid MedChemExpress normally types through throughout hydrothermal metamorphism occurs under low pressurepressure and low temperature [57]. The occurrence of corrensite was confirmed from the and low temperature [57]. The occurrence of corrensite was confirmed from the following observations: (i) shift in peak in the basal spacing from 7.03 air-dried following observations: (i) shift in peak with the basal spacing from 7.03 (7.3for (7.three for air-dried state) to 8.41 (6.1o for EG solvated); (ii) presence of a distinct peak at a basal spacing of 2.82 (37.0for EG solvated); and (iii) absence of your very first peak (HCl solvated) due to mineral decomposition [58]. In contrast, the presence of kaolinite (14.4 24.3 and 29.1 and illite (20.7 were confirmed in the absence o.