Multi-Analytical Approach for Characterization of Archaeological Meroatic Potsherds

Citation: Siddig FE, Elbashir AA, Lepper V (2019) Multi-Analytical Approach for Characterization of Archaeological Meroatic Potsherds. Int J Exp Spectroscopic Tech 4:023 Accepted: March 23, 2019; Published: March 25, 2019 Copyright: © 2019 Siddig FE, et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. *Corresponding author: Abdalla Ahmed Elbashir, Department of Chemistry, Faculty of Science, University of Khartoum, Khartoum, Sudan, Tel: +249912989405


Introduction
known culture creation of ancient Nubia, and it is rightly famed for the fine workmanship and unique decoration according to Adams [3]. The samples details shown in Table 1. General geological back-ground to explanation somehow of the dissimilarity in the mineralogical composition of sites. The Nile, with its binary main branches -the White Nile and the Blue Nile -combine at Khartoum, runs over the county. The Atbara River, with its headstream in Ethiopia, arrives the main river system around 300 km north of Khartoum. The three branches have a different mineralogical composition, therefore donating to the variant in the mineralogical composition of the coming together area [4]. The White Nile brings rounded monocrystalline quartz with a minor quantity of feldspar, the sediments of the Blue Nile hold commonly mafic volcanic particles, K-feldspar, and biotite, besides the Atbara River donates volcanic rock remains augite, and olivine. The Nile alluvium in the areas north of the union is labeled considered as extra homogeneous, enclosing mineral sets of quartz, feldspars, amphiboles, clinopyroxenes, mica, round fragments of primary volcanic rock, and phytoliths of plants, which are mostly formed from weathering of the basaltic Ethiopian Hilltops [5]. The archaeological locations of the Royal City and Meroe have together situated were located in lengthways the eastern cut banks of the Nile: Meroe is located 150 km north northern of Khartoum [6].
The studies stimation of firing temperature and the type of atmospheric firing phase are suitable to give condition are important to provide us a well understanding of the civilization that made In the existent study, ancient potsherds were studied by many analytical approaches. XRD and FT-IR were used for the mineralogical characterization, XRF, SEM-EDX for morphological, structural and chemical assessment. XRF for the determination of the elemental composition and SEM-EDX for morphological, structural and chemical assessment.

Materials and Methods
Six ancient Meroitic potsherds ( Figure 1) were dated toward the 4 th century BC, the description of pottery samples listed in Table 1. the potteries methods [7]. Fourier transform infrared spectroscopy (FT-IR) is a useful technique to study the minerals and their decompositiontransformation manners of pottery [8,9] estimate the firing condition [10] beside X-ray diffraction is alternative analytical instrument principally used for the mineral/phase investigation of potteries which informs us by the raw materials of the samples [11,12]. As well, XRF has experienced used too as co-dependent analysis that can be used, getting elements to range above Sodium to Uranium [13].

Thermogravimetric analysis (TGA)
Thermogravimetric analysis (TGA) was carried out by PT1000 Thermogravimetric LINSEIS with thermal advantage software. The experimentation was accomplished with a heating rate 10 °C/ min the samples heat up to 950 °C in high purity atmosphere.

X-Ray fluorescence (XRF)
Elemental components of the pottery were considered by X-ray fluorescence spectrometer (XRF), the samples grind down to the power by mortar and pestle, then 1 gram pressed in 2 cm 2 circular disk. The X-ray isotopic source was used to measure the samples utilizing 109 Cd which has regular energy 22.6 Kev. Si (Li) detector, The

Fourier Transform Infrared Spectroscopy (FT-IR)
FT-IR is obtained with FT-IR 8400S Shimadzu (Japan) with a pyroelectric detector operating in the mid Infrared region (400-4000 cm -1 ) with a characteristic resolution of 4.0 cm -1 in transmittance mode, using KBr discs. The fixing of peaks and smoothing were performed by IR-solution software in the device done the working window 4000-400 cm -1 .

X-ray diffraction (XRD)
X-ray diffraction (XRD) analysis was performed by EXPERT-PRO diffractometer system, the Goniometer: PW3050/60 (Theta/theta), using Cu Kα (λ = 1.54060 Å). The diffraction patterns were done at 2θ angle, within range 3-70˚ with step size [˚2θ] = 0.0200 at a scan step time 0.5 s. The measuring temperature of 25 °C, the generator sitting 40 mA, Table 2: FT-IR wavenumbers (cm -1 ) of potsherds with corresponding vibrational assignments.   Quartz basal reflection in XDR at (4.26, 2.28, 2.24, 1.85, 1.54 and 1.45 Å) while in FT-IR in the band at 694 cm -1 is linked to vibrations of Si-O bonds in mineral quartz [19], and quartz occurrence is also showed by the doublet at around 777 and 798 cm -1 [20]. Besides, the absorption bands at 475 cm -1 assigned to bending vibrations of Si-O, Al-O bonds perform [21]. The bands 645 cm -1 band is due to Al-O stretching vibrations in AlO 6 octahedra [22] while the band at 877 cm -1 (MER-01) attributed to the existence of calcite [12] and dehydroxylation of kaolinite minerals which is accomplished at 800 °C plus octahedral sheet structure in the clay minerals missing [23].  [23,24] shown in (Figure 3a).

FT-IR absorption bands in wave numbers (cm -1 ) with comparative intensities
The statement of the FTIR spectra pattern is in agreement with the literature, the thing makes FT-IR informative is that the ability of detection of any amorphous components in the sample while XRD can analysis only crystalline phases and agreements information about the typical structure, disordered SiO 4 tetrahedra in usually amorphous phases that formed through clay firing will moreover broaden this band In the firing process structural changes that happen will disturb the point of Si-O stretching and deformation bands in FTIR results [25]. The Si-O stretching bands at around 1000 cm -1 in the FTIR spectra of all pottery samples ( Figure 2) shifts towards higher frequencies with increasing temperature, bands (1037, 1031 and 1041 cm -1 ) in the samples (MER-01, MER-02 and MER-06) respectively at 700 °C. While the bands (1085, 1076 and 1081 cm -1 ) in the samples (MER-03, MER-04 and MER-05) at 900 °C. that, it is possible to estimate the firing temperature range of the samples as 700-900 °C, this excellent agreement with the assumption resulting from XRD and SEM-EDX [25].

Thermogravimetric analysis (TGA)
Characteristic thermal analysis curves (TGA), of the potsherds observed in heating up to 900 °C are shown in (Figure 4a and Figure 4b). TGA results was a complementary study to estimate the firing temperature from the specific thermal reaction in potsherds under controlled firing atmosphere combined with other spectroscopic approaches like FT-IR and XRD, for the investigation of pottery samples [11,24]. CANBERRA amplifier model 2020 with high voltage supply 600 V.

Scanning Electron Microscope-Energy Dispersive X-ray (SEM-EDX)
The microphotograph analysis was performed on an EVO ® LS 10 scanning electron microscope at 20 KV an accelerating voltage and 1-3 nA a beam current. The fresh fraction of each sample coated with a thin layer of palladium/gold. The extreme magnification in the technique is 1000.0000 times. The elemental investigation was performed by using the Oxford INCA EDX energy dispersive spectrometer, for the characterization of the X-ray emitted by the sample to examine the elemental chemical composition currently identified by SEM.

Mineral analysis
The mineralogical composition of the investigated potsherds was carried out by FT-IR and XRD techniques. The FT-IR results are shown in ( Figure  2) and listed in Table 2 within range 400-4000 cm -1 . While XRD spectra are presented in (Figure 3a and Figure 3b) and the crystalline minerals of XRD results listed in Table 3. The absorption band around 1640 cm -1 is frequently assigned to O-H bending vibration and also can arise from vibrations of the SiO 2 network and is frequently hidden by water O-H band. The absorption band around 1640 cm -1 is frequently assigned to O-H bending vibration of water O-H band [14]. The existence of the band around 535 cm -1 in both (MER-01, MER-04) samples, revealed that, the presence of iron oxides. Which indicated that point out these samples, they were fired in the temperature more than 750 °C in open atmosphere firing condition and it is may confirmed from the red color of the potsherds samples [11,15]. While sample MER-05 contains monganite which may suggest the firing temperature between 800-900 °C [16]. While MER-03 sample contains anatase, which is a common thermal stable phases impurity of both clays and sands [13]. Anatase, a TiO 2 polymorph which is commonly formed over the gel or hydrothermal technique still regularly present in linkage with brookite, albite and quartz. Indeed, this phase of titanium oxide mostly transforms into rutile which is a mineral from which up to 70% of titanium oxide at about 850 °C [17], thus, this polymorph be able to use to determine the firing temperature of ceramic [18]. and Ca define the origin of the clay minerals and firing atmosphere adopted selected by the artisans. In particular, the nature of the clay whether calcareous (CaO > 6%) or non-calcareous (CaO < 6%) clay can be identified from the percentage of Calcium Oxides (CaO) from the XRF data, it should be noted that all the samples were non-calcareous, these suggestions show that the sources of the clay did not contain calcite [28,29].
Some trace elements like Mn, Zr, Ti, Nb might be used as geochemical 'fingerprints' guide, as they are related to particular petrological types [30]. The zirconium content is similarly small quantities in the samples most likely related to the igneous phases, upcoming from the granite and pegmatite regional rocks [31].

SEM-EDX analysis
The elemental concentration of the three potteries studied under SEM, beside EDX are given in (Figures 6, Figure 7 and Figure 8). The EDX indicated obviously point to low refractory clay [32] and all the three samples had relatively high iron The figure characterizes the thermograms of non-calcareous (calcite-free) and calcareous (calcite-rich) potsherds. The mass-loss as a result of the thermal manner was determined by the thermogravimetric analysis (TGA). The peak pause of the dehydration and dehydroxylation were firm according to Drebushchak, et al. [26]. The peak interval of the dehydration is defined from RT (room temperature) to 350 °C and the dehydroxylation from 350 to 600 °C. Even if in some potsherds dehydroxylation is not clear, the exterior of massloss in the TGA curves in the temperature interval of 350-600 °C indicates that this process takes place and can be measured. In pottery containing calcite an additional mass-loss is detected in the interval from 600 to 850 °C because of decarbonation of the calcite in the potsherds [27].

X-Ray fluorescence (XRF) analysis
The elemental analysis obtained by XRF results of the six potsherds is shown in ( Figure  5). it is obvious that the most abundant common elements are Ca, Fe, and Ti. The composition of Fe   Au. The elemental concentration of these elements is summarized in beside table. In the spectrum 1 area (MER-03) the elemental composition only O, Al, Si were recognized in addition very small quantities of Ti, Fe, Au may this could be planted fiber, which could have arisen naturally in the Nile clay, it is as well probably that plant ingredients might be combined to the clay as temper [6]. The composition in the another grain spectrum 2,3 areas content in agreement with the chemical analysis of XRF.
The sample (MER-01) did not reveal vitrification ( Figure 6) from the elemental analysis shows, it is of the non-calcareous category, according to Maniatis and Tite [33], low refractory non-calcareous clay formed in oxidizing firing condition with no vitrification stage were fired < 800 °C, The (MER-02) ( Figure 7) and (MER-03) (Figure 8)   The chemical composition of the trace elements revealed high concentrations of characteristic elements like Ti, Zr and Nb. A preliminary statement that the (MER-03) was prepared at a different workshop using different clay-beds could be drawn. The primary results of this study do not necessarily imply that all the pottery of those regions are appropriate to the same chronological form have similar physicochemical characteristics. This current archaeometrical research of pottery is predictable to deliver useful evidence on pottery folklore, line of work and cultural altercation through time.
are approximately different (MER-03) respectively, contain Si, Al, O, Mg, Ca and Fe. Furthermore, the spectrum 4 area is containing also Al, O, Si as major elements besides Fe, Ti and Au. The results show various samples composition, due to different raw materials used and manufacturing techniques applied by artisans [22].

Conclusions
In this paper the multi-analytical approach has been used to study the potsherds excavated in the Meroitic archaeological sites in Sudan. The results obtained showed that potsherds were made with quite different raw mat erials. Quartz and feldspars mineral (Albite), anatase and moganite in the XRD analysis It is confirmed with FT-IR, TGA and SEM results. As a result, may show firing temperature at 700-900 °C in oxidizing atmosphere condition. The procedural approach was well applied to the mineralogical, chemical and thermal