Natural Radionuclide Concentrations by γ-Ray Spectrometry in Granitic Rocks of the Sol Hamed Area, Southeastern Desert of Egypt, and Their Radiological Implications

Abstract

The occurrence of heavy radioactive minerals in construction supplies such as granite has drawn attention to the extraction of heavy radioactive minerals. Granitic rocks were identified to serve an essential economic role in the study area’s surrounding locations. As a result, the current study attempted to detect the activity concentrations of ²³⁸U, ²³²Th, and ⁴⁰K in the granitic rock samples tested and estimate the radiological dangers associated with these rocks. The obtained data on activity concentrations for ²³⁸U (610 ± 1730 Bq kg⁻¹), ²³²Th (110 ± 69 Bq kg⁻¹) and ⁴⁰K (1157 ± 467 Bq kg⁻¹) in the granitic samples (GR) were higher than the recommended worldwide average. The radioactive levels found in the samples were caused by radioactive materials being altered and trapped inside granite faults. The exposure to gamma radiation from the granitic rocks were assessed via various radiological parameters, such as radium equivalent content (856 Bq kg⁻¹), absorbed dose rate (Dair) in the air (396 nGy/h), and annual effective dose for either outdoor (0.48 mSv y⁻¹) or indoor (1.9 mSv y⁻¹). Statistical analysis was performed to detect the correlations between radioactive concentrations and radiological parameters. The radioactive effects contributed by the uranium minerals were associated with the granitic rocks. Based on the analysis, the radioactive levels in the examined granitic surpassed the acceptable limits; therefore, they are not safe to use in building and infrastructure applications and may cause adverse health effects.

1. Introduction

The primary sources of natural radioactivity in the environment are terrestrial radioactivity and cosmic radiation. The human body is exposed to ionizing radiation from naturally occurring radioactive materials (NORM). People can be exposed to terrestrial radiation by two main approaches. First is external exposure to gamma radiation emitted from ²³⁸U, ²³²Th, and ⁴⁰K. The second is internal exposure from inhaled radon gas and its daughters [1,2,3,4]. According to the Agency for Toxic Substances and Disease Registry (ATSDR), long-term radioactive exposure causes significant ailments that include oral necrosis, chronic lung disease, leukopenia, and anemia [5,6].

In recent years, multiple investigations of high natural background areas around the world have achieved more awareness in risk appraisal due to whole-body exposures of inhabitants to long-term low-level radiation [7]. Previous research has shown that high levels of radiation are caused by the presence of radionuclides in high concentrations in granite rocks, soils, sediments, and other materials. Granite rocks and sediments, among other geological elements, play an essential role in construction materials and other infrastructure applications [8,9], aside from the radioactivity moving from one zone to the next and accumulating [10,11]. As a result, several researchers have found that national surveys conducted around the world in recent decades have yielded distinguishing results in terms of detecting natural radionuclides in granite rocks and sediments [12,13,14].

The Sol Hamed granites are low to moderate circular relief hills with a hollow structure and extensive weathering. These granitic rocks are divided into two primary intrusions: coarse-grained granite with a pinkish-grey tint and fine-grained granite with a grey color. Quartz, K-feldspar, plagioclase, and biotite make up the mineral. Apatite, zircon, magnetite, and pyrite are examples of accessory minerals. The latter material is frequently oxidized and removed, leaving cubic-shaped vugs and patches of red hematite in its place. Another phase of granitic intrusion, extensively worn reddish to fine-grained pink granite, intrudes on the coarse-grained granite. This granitic appears as a thin peripheral strip with limited exposure and in batches that crosscut the previously formed granite. Quartz, K-feldspar, plagioclase, biotite, and muscovite are the primary minerals in fine-grained granite. Accessory minerals include apatite, zircon, titanite, and ilmenite. According to geochemical evidence, both varieties of Sol Hamed granites were formed from K-rich calc-alkaline magma. Manganese oxides can be found in stains at joints, fractures, and dispersions within the rock [10].

In comparison to the many places researched in Egyptian deserts, the investigated area was chosen for the examination task because of the economic value of the heavy minerals accumulated in granite and sedimentary rocks. Generally, the granitic rocks in the studied area are highly weathered, jointed, and cavernous. The intensity of the weathering and development of the cavernous shapes is directly related to the percentage of biotite and muscovite content, and the fracturing intensity. The present work is unique in that it detected radioactive levels in the analyzed granitic, which can be used in building materials and infrastructure applications. Various radioactive parameters were identified in addition to the evaluation of public exposure to radiation via the analysis of radiological dangers. Radium equivalent activity (Ra_eq) absorbed dose rate (D_air), annual effective dose (AED), external (H_ex), and internal (H_in) hazard indices were some of the radiological risks. In addition, the annual gonadal dose equivalent (AGDE) and the excess lifetime cancer risk (ELCR) were computed.

2. Materials and Methods

2.1. Geological Setting

One of the most important areas of the Eastern Desert of Egypt is the Sol Hamed area. It is located in the southern Eastern Desert of Egypt, about 40 km to the north from the Egyptian Sudanese borders, between latitude 22°16’40”–22°18’30” N and longitude 36°14’20”–36°16’30” E, at a distance of about 30 km southwest of Abu Ramad city, on the Red Sea. The study area is low, and has moderate to high relief and is remarked by Gabal El Sela (557 m) and scattered isolated hills separated by sand and gravels of wadi deposits. The Sol Hamed area lies in the southern half of the Elba topographic sheet, a southeastern desert of Egypt that includes metagabbros, while the surrounding areas contain muscovite granites, mica granites, metavolcanicalsts, younger metavolcanics, older metavolcanics, serpentinites, and related rocks (Figure 1 [15]). It is part of the late Precambrian–early Paleozoic Pan-African Orogeny that formed the Arabian Nubian Shield (950–450 Ma), and covers an area of around 73.5 km². The Sol Hamed area forms an elongated belt trending NNW–SSE. The main valleys dissecting the area are the Eikwan valley and Yoider valley.

2.2. Sampling and Radioactive Detection

Different kinds of granitic rocks (coarse grained granite (CG), fine-grained granite (FG), bostonite (B), and lamprophyre (L)), in addition to lamprophyre dykes, were observed in the Sol Hamed area. Nine samples for each granite were collected from the Sol Hamed area. Then, the crushing and sieving processes were carried out to prepare the samples for radioactive measuring. About 250 g of the granite rocks were inserted into a plastic container and stored for 30 days to achieve the radioactive equilibrium between radium and its daughters.

For radiation detection and measurements in granitic rock (GR) samples, a NaI crystal detector combined with a high-voltage-driven photomultiplier tube (PMT) (manufacturer, city and country) was utilized due to its quick, nondestructive, and highly efficient nature. A Gamma spectrometer (state manufacturer, city and country) with a 76 × 76 mm² NaI (Tl) crystal was applied to detect the radioactive concentrations of ²³⁸U, ²³²Th, and ⁴⁰K. A spectroscopy amplifier and a multichannel analyzer were part of the pulse data and management analysis equipment, which was coupled to computer with a SPTR-ATC software (AT-1315) The ²³⁸U, ²³²Th, and ⁴⁰K had gamma energies of 1764 keV (I = 15.30%) from ²¹⁴Bi, 2614 keV (I = 99.754%) from ²⁰⁸Ti, and 1460 keV (I = 10.66%) from ⁴⁰K [16,17]. Approved reference materials such as RGU-1, RGTh-1, and RGK-1 were used, and their densities after pulverization were comparable to the densities of the building materials. The gamma rays released by the granitic rock samples were detected by a NaI detector, and their spectra were examined using SPTR-ATC software (AT-1315). The activity concentration for each granitic sample was determined from the intensity of the spectral line, taking into account geometry, mass, coupling time, and detector performance. An empty sealed vessel with the same dimensions was introduced into the spectrometer assembly to scrutinize the background radiation. The efficiency of the calibration was performed as follows: the container was designed while assuming that the radioactivity in the measurement samples was uniformly dispersed. The minimum detection activity (MDA)s of 2, 4, and 12 Bq kg⁻¹ for ²³⁸U, ²³²Th, and ⁴⁰K, respectively, were used in the granitic samples, which were calculated up to 2000 s. The error-propagation equation for systematic and random measurement errors was used to estimate the general uncertainty of radiation levels. Efficiency of the calibration had systematic errors from 0.5 to 2%, while radioactivity values had random errors of up to 5% [18].

Table 1. Important radiological parameters and indices.

Parameter	Symbol	Definition	Formula
Radium equivalent activity	Raeq	Radium equivalent activity is a weighted sum of the 226Ra, 232Th, and 40K activities according to the hypothesis that 370 Bq kg−1 of 226Ra, 259 Bq/kg of 232Th, and 4810 Bq/kg of 40K attain the same dose rates of gamma rays.	Raeq (Bq kg−1) = ARa + 1.43 ATh + 0.077 AK
External hazard index	Hex	The external hazard index comprises the radiological parameters applied to assess of the hazard of γ-radiation	${\mathrm{H}}_{\mathrm{ex}}=\frac{A_U}{370}$$+\frac{A_{Th}}{259}$$+ \frac{A_K}{4810}$
Internal hazard index	Hin	The internal hazard index is applied to the internal exposure from radon and its decay products.	${\mathrm{H}}_{\mathrm{in}}=\frac{A_U}{185}$$+\frac{A_{Th}}{259}$$+\frac{A_K}{4810}$
Radiation level index	Iγ	The other index used to estimate the level of γ-radiation hazard associated with the natural radionuclides in the samples was suggested by a group of experts due to the different combinations of specific natural activities in the sample.	${\mathrm{I}}_{\mathsf{\gamma }}=\frac{A_{Ra}}{150}$$+\frac{A_{Th}}{100}$$+\frac{A_K}{1500}$
Absorbed dose rate	D (nGy/h)	The absorbed dose rate is the radioactive factor that was applied to detect the effect of gamma radiation at 1 m from the radiation sources in the air due to the concentrations of 238U, 232Th, and 40K	Dair (nGy h−1) = 0.430 AU + 0.666 ATh + 0.042 AK
Outdoor annual effective dose	AEDout	The annual effective dose is a radioactive factor utilized to detect the exposure level for radiation during a stationary duration (1 year).	AEDout (mSv/y) = Dair (nGy/h) × 0.2 × 8760 (h/y) × 0.7 (Sv/Gy) × 10−6 (mSv/nGy)
Indoor annual effective dose	AEDin		AEDin (mSv/y) = Dair (nGy/h) × 0.8 × 8760 (h/y) × 0.7 (Sv/Gy) × 10−6 (mSv/nGy)
Annual gonadal dose equivalent	AGDE	The annual gonadal dose equivalent is the radioactive parameter used to estimate the doses absorbed by the gonads due to exposure to gamma radiation.	AGDE (mSv y−1) = 3.09 ARa + 4.18 ATh + 0.314 AK
Excess lifetime cancer risk	ELCR	Excess lifetime cancer risk is the radioactive factor applied to detect fatal cancer resulting from gamma radiation exposure.	ELCR = AEDout × DL × RF

illustrates the radiological hazard parameters computed based on the activity concentrations of ²³⁸U, ²³²Th, and ⁴⁰K, and presents the mathematical formulas used.

3. Results

3.1. Petrographic Investigation

The radioactive minerals were mainly represented by uraninite, uranophane, thorianite, monazite, and columbite. Uraninite was detected in the samples collected from the Sol Hamed altered granites. Uraninite is always present where economic uranium mineralization occurs [19]. Under polarized light, uraninite appears as cubes smaller than one millimeter that are randomly scattered throughout the host and sometimes partly altered to uranophane in the highly ferruginated portion of the rock (Figure 2).

Uranophane is considered one of the most important economic-secondary uranium deposits. It is a monoclinic uranyl silicate mineral fairly common in the oxidized zone of most deposits [20]. In the present study, uranophane occurred as films, patches, and crusts, either on outcrops or in fractures. They were massive mineralizations with platy and granular forms, and showed dull, greasy, and/or waxy luster. Their colors ranged from beautiful canary yellow to lemon, but pale yellow films were common. They occurred either in discrete forms or as an alteration product of pitchblende in the form of core and periphery replacements.

Thorianite is a rare mineral, and may contain up to about 12% thorium oxide. Thorium occurs in several minerals, including thorite (ThSiO₄), thorianite (ThO₂ + UO₂), and monazite. Macroscopically, it is nearly opaque, being transparent in thin fragments. In transmitted light, it is yellowish-orange, red, brownish-yellow, brownish-black, or black.

Monazite, which is considered one of the most important sources of rare earth elements, is enriched in thorium and uranium. Monazite occurs as egg-shaped crystals ranging in color from lemon yellow to honey yellow, and sometimes red as a result of staining with iron oxides.

Columbite occurs as an alteration product phase in the Sol Hamed shear zone, brownish- to yellowish-dark grey in color. Rare metal minerals of mineralized altered granites within El Sela shear zones are columbite–tantalite minerals as ferrocolumbite, pyrochlore, and fergusonite; Th-minerals (cheralite, uranothorite, and huttonite monazite), Hf-zircon; monazite; and xenotime [21].

3.2. Radioactivity Analysis

The coarse-grained granite phase was characterized by radioelement contents ranging from 1.3 to 53.6 ppm for eU with a mean value of 11.9 ppm, from 5 to 57.6 ppm for eTh with a mean value of 27.5 ppm, and from 1.5% to 6.3% for K with mean value of 3.8% (

Table 2. Values of eU (ppm), eTh (ppm), and K (%), as well as eTh/eU and eTh/K ratios and (eU- eTh/3.5) parameter for the Sol Hamed granitic rocks.

Rock Type	eU (ppm)	eTh (ppm)	eK (%)	eTh/eU	eTh/eK	eU-eTh/3.5
CG	1.4	10.5	2.4	7.5	4.4	−1.6
	53.6	57.6	6.3	1.1	9.1	37.1
	6.52	23.7	3.8	3.63	6.2	−0.3
	1.3	9.4	2.1	7.23	4.5	−1.4
	9.9	57.4	5.6	5.8	10.3	−6.5
	5.33	26.4	4	4.9	6.6	−2.2
	2.1	5	1.5	2.2	3.3	0.7
	20	38.5	5.5	1.9	7.0	9
	6.5	19	3.3	2.9	5.8	1.1
Ave.	11.9	27.5	3.8	4.2	6.3	4
FG	2.3	13.5	3	5.9	4.5	−1.6
	42.1	38.9	5.1	0.9	7.6	31
	7.6	24.6	4	3.2	6.1	0.6
	1.2	12	2.4	10	5	−2.2
	9.1	49	5.2	5.4	9.4	−4.9
	6.56	36	4.5	5.5	7.9	−3.7
	6.49	7.8	2.1	1.2	3.7	4.3
	40	50.2	5.3	1.3	9.5	25.7
	14.5	28.7	3.9	1.9	7.4	6.3
Ave.	14.4	29	4	3.9	6.8	6.2
B	2.8	13.4	3	4.8	4.5	−1
	39.1	53.3	5.8	1.4	9.2	23.9
	19	25	3.8	1.3	6.6	11.9
	11.2	23.5	3.9	2.1	6	4.5
	30	47.1	5.2	1.6	9.1	16.5
	3.9	15	3	3.9	5	−0.4
	49.5	57.4	6.3	1.2	9.1	33.1
	26	30.5	2.9	1.2	10.5	17.3
	13.2	28.3	4.4	2.1	6.4	5.1
Ave.	21.6	32.6	4.3	2.2	7.4	12.3
L	2.2	1.2	0.1	0.6	24	1.9
	760	34.9	4.5	0.1	7.8	750
	40.3	15.2	2.6	0.4	5.8	35.9
	6	4.1	1.7	0.7	2.4	4.8
	68.2	44.7	4.3	0.7	10.4	55.4
	420.5	35.5	4.7	0.1	7.6	410.4
	26	16.6	2.8	0.6	5.9	21.3
	4.2	3.9	1.5	0.9	2.6	3.1
	20.3	16.8	2.6	0.8	6.5	15.5
Ave.	149.7	19.2	2.8	0.5	8.1	144.3
Earth’s crust	2.9	10.8	2.7
Safety for building	4	12.3	1.6

). The remobilization parameter (eU- eTh/3.5) ranged from–6.5 to 37.1 with a mean value of 4.

The fine-grained granite had radioelement contents ranging from 1.2 to 42.1 ppm for eU with a mean value of 14.4 ppm, from 7.8 to 50.2 ppm for eTh with a mean value of 29 ppm, and from 2.1% to 5.3% for K with a mean value of 4%. The remobilization parameter (eU- eTh/3.5) ranged from–4.9 to 31 with a mean value of 6.2.

The bostonite dykes had concentrations ranging from 2.8 to 49.5 ppm for eU with a mean value of 21.6 ppm, from 13.4 to 57.4 ppm for eTh with a mean value of 32.6 ppm, and from 2.9 to 6.3% for K with a mean value of 4.3%. The (eU- eTh/3.5) ranged from–0.4 to 33.1 with a mean value of 12.3.

The eU, eTh, and K values for lamprophyre dykes ranged from 2.2 to 760 ppm, from 1.2 to 44.7 ppm, and from 0.1% to 4.7%, with mean values of 149.7 ppm, 19.2 ppm, and 2.8%, respectively. The (eU- eTh/3.5) ranged from 1.9 to 750 with a mean value of 144.3.

The obtained results for the Sol Hamed granitic area revealed that the lamprophyre dykes had the highest mean value for ²³⁸U (149.7 ppm), while the highest mean values for ²³²Th and ⁴⁰K were recorded in the bostonite dykes (32.6 ppm, 4.3%).

The lowest mean value for ²³⁸U was observed for the coarse-grained granite (11.9 ppm), while the lowest mean values for ²³²Th and ⁴⁰K were observed in the lamprophyre dykes (19.2 ppm, and 2.5%).

A general review of the average values for eU, eTh, and K obtained for different rock types from El Sela area clarified high radioactivity levels. These figures were greater than those published for the Earth’s crust, and they were also higher than the safety standards for building materials. The frequency distributions of activity concentrations of the studied radionuclides confirmed these results, as shown in Figure 3, Figure 4, Figure 5 and Figure 6.

3.3. Geochemistry of U and Th in the Studied Rocks

The relationships between the natural radionuclides (U, Th, and K) of the rocks tested were computed (Table 2), and are diagrammatically shown in Figure 7 and Figure 8.

Positive correlations between Th and U were observed for coarse-grained granite, fine-grained granite, bostonite, and lamprophyre (R = 0.7, 0.6, 0.9, and 0.6, respectively), suggesting magmatic processes exerted a significant influence on radioelement concentration (Figure 7a and Figure 8a).

Figure 5b and Figure 6b illustrate that there was a strong positive correlation between Th and K (R = 0.96, 0.97, 0.9, and 0.9), and between U and K (R = 0.8, 0.7, 0.8, and 0.7) for coarse-grained granite, fine-grained granite, bostonite, and lamprophyre, respectively (Figure 6 and Figure 7 ).

The variations in Th and U in the Th/U ratio showed a negative correlation for all samples tested, as illustrated in Figure 7d,e and Figure 8d,e. This result confirmed the concept that magmatic processes at least partly governed the radioactive element distribution in these rocks.

The average value of the Th/U ratio for coarse-grained granite (4.2) and fine-grained granite (3.9) was greater than the Clark value (3.5), demonstrating that the radioelements in the investigated rocks were not extensively fractionated during weathering or implicated in the metasomatic activity [22].

On the other hand, the average value of the Th/U ratio for bostonite (2.2) and lamprophyre (0.5) was less than 3.5 (Clark value), which denoted enrichment of uranium and implicated reducing conditions. This result was confirmed by the average values of remobilization parameters of 12.3 and 144.3 for these rocks, respectively.

The cross plot of eTh/eU and eTh/K ratios presented in Figure 7f and Figure 8f displays that these samples were found in the fixed-U and leached-U sectors. The average values for eTh/K of 6.3, 6.8, 7.4, and 8.1 were >2 × 10⁻⁴ for coarse-grained granite, fine-grained granite, bostonite, and lamprophyre, respectively. These values denoted thorium enrichment in the studied rocks.

3.4. Radioactive Concentrations in Granitic Rocks

Table 3. Descriptive statistics of ²³⁸U, ²³²Th, and ⁴⁰K activity concentrations of the studied granitic rock.

Radionuclides	N *	Mean	SD **	Min	Max	Skewness	Kurtosis	CV, %
		Bq kg−1	Bq kg−1	Bq kg−1	Bq kg−1
Coarse-grained (CG)
238U	9	146	206	16	662	2.4	6.1	141
232Th	9	111	80	20	233	0.7	−0.9	72
40K	9	1199	528	469	1971	0.1	−1.4	44
Fine-grained (FG)
238U	9	178	192	14	519	1.4	0.3	108
232Th	9	117	64	31	203	0.0	−1.5	55
40K	9	1234	379	657	1658	−0.4	−1.4	31
Bostonite (B)
238U	9	267	196	34	611	0.5	−0.6	74
232Th	9	132	65	54	233	0.5	−1.3	50
40K	9	1332	396	907	1971	0.5	−1.2	30
Lamprophyre (L)
238U	9	1849	3267	27	9386	2.0	3.4	177
232Th	9	78	63	5	181	0.5	−1.2	82
40K	9	862	482	31	1471	−0.2	−0.6	56
GR + L
238U	36	610	1730	14	9386	4.5	20.8	284
232Th	36	110	69	5	233	0.4	−1.0	63
40K	36	1157	467	31	1971	−0.2	−0.5	40

* N = the number of samples, ** SD = standard deviation.

shows the activity concentrations of radionuclides ²³⁸U, ²³²Th, and ⁴⁰K in the examined granitic rocks (CG, FG, B, and L). The range (mean ± SD) of ²³⁸U, ²³²Th, and ⁴⁰K activity concentrations in the granitic rocks were 14–9386 (610 ± 1730), 5–233 (110 ± 69), and 31–1971 (1157 ± 467) Bq kg⁻¹, respectively. Natural radioactivity levels varied widely due to variations in activity concentration values for ²³⁸U, ²³²Th, and ⁴⁰K in geological formations and their physical, chemical, and geochemical characteristics [23]. The findings showed that the mean values of ²³²Th and ⁴⁰K were three times higher than the global averages of 45 and 412 Bq kg⁻¹, respectively. Nonetheless, the mean uranium value was much greater than the global value of 33 Bq kg⁻¹. The presence of uranium and thorium in the chemical components of heavy minerals (including zircon, fluorite, and apatite) and some other minerals (notably uraninite, thorianite, and monazite) that were found in granitic rocks could explain the increasing levels of radioactivity [12,24]. An analysis using descriptive statistics (skewness, kurtosis, and coefficient of variation (CV)) is also included in Table 3. According to a statistical study of radionuclides in granitic rock (GR), the skewness factor was used to illustrate the asymmetric distribution. The asymmetric nature was described by positive skewness values for ²³⁸U and ²³²Th, while negative values of ⁴⁰K described the flatness of its probability distributions. The kurtosis factor also revealed the probability peak of a distribution. As a result, the probability distributions for ²³⁸U, ²³²Th, and ⁴⁰K peaked when positive values were used. For ²³⁸U, ²³²Th, and ⁴⁰K, the projected coefficient of variation (CV) values were high, with values of 93%, 99%, and 248%, respectively. This was corroborated by the presence of several radioelement-bearing minerals in the examined GR.

Figure 9a–c show the frequency distributions of ²³⁸U, ²³²Th, and ⁴⁰K activity concentrations in all the examined GR.

Table 4. Results of normality tests.

Radionuclide	Kolmogorov-Smirnov *
	DF	Statistic	p-Value
238U	36	0.40	7.7 × 10–6
232Th	36	0.12	0.70
40K	36	0.10	0.96

Asymp. sig. = asymptotic significance level; DF = degrees of freedom. * Lilliefors significance correction.

displays the normal distribution predicted for ²³²Th and ⁴⁰K activity concentrations in the GR, while multimodality distribution was perceived for ²³⁸U activity concentration.

The obtained data on ²³⁸U, ²³²Th, and ⁴⁰K activity in the current study were compared to those found in previous studies conducted in other countries (

Table 5. A comparison between the activity concentration of radionuclides presented in studied granitic rock and other areas.

Country	238U	232Th	40K	References
Egypt	610.3 ± 1730.9	109.9 ± 68.9	1157.2 ± 466.8	Present study
Palestine	71	82	780	[25]
Saudi Arabia	28.82	34.83	665.08	[26]
Spain	84	42	1138	[27]
India	25.88	42.82	560.6	[28]
Iran	77.4 ± 21	44.5 ± 12	1017.2 ± 154	[29]
Turkey	80 ± 11	101 ± 17	974 ± 102	[30]
Nigeria	63.29 ± 13.87	226.67 ± 28.05	832.59 ± 241.53	[2]
Egypt	2989 ± 2757	460 ± 311	1073 ± 560	[10]
Jordan	41.52 ± 3.23	58.42 ± 0.44	897 ± 43	[31]
Greek	74 ± 51	85 ± 54	881 ± 331	[18]
Egypt	137	82	1082	[32]

). The comparison showed that the concentrations of ²³⁸U, ²³²Th, and ⁴⁰K activity were affected by the geological characteristics of the analyzed locations.

3.5. Radiological Effects

The computed radium equivalent (Ra_eq) values for granitic rock (GR) of the Sol Hamed area altered between 36 and 9697 Bq kg⁻¹, with a mean value of 856 ± 1762 Bq kg⁻¹. The (Ra_eq) values were higher than the global approved permissible limit of 370 Bq kg⁻¹ [33]; this is an acceptable limitation that does not preserve the external dose under 1.5 mSv/y [4].

The mean value of (H_in) for GR samples was 3.9 ± 9.4. The range (H_in) values ranged from 0.17 to 51.5 in the GR of the Sol Hamed area. The external hazard index (H_ex) values for GR samples ranged from 0.09 to 26, with a mean value of 2.3 ± 4.7. The (H_in) and (H_ex) mean values in all measured GR samples in the studied area demonstrated overexposure; i.e., those values were found to be higher than the approved limit (<1) [34] (Figure 10).

The (I_γ) for GR samples had a mean value of 2.9 ± 5.8, with lowest and highest values of 0.12 and 32.4, respectively. The mean values were lower than the permissible limit <1 (Figure 10) [35]. The values of Iγ illustrated that the GR samples in the Sol Hamed area pose a significant health risk, and are not candidates to be employed as construction materials.

The GR’s obtained (D_air) values were greater than the recommended mean worldwide value of 59 nGy/h [4]. The (D_air) values for samples of GR ranged from 16.7 to 4479 nGy h⁻¹, with a mean value of 396 ± 814 nGy h⁻¹. This showed that the GR of the Sol Hamed area is not suitable to apply in several infrastructure applications, particularly in building materials.

The (AED_out) values fluctuated from 0.02 to 5.4 mSv y⁻¹, with a mean value of 0.48 mSv y⁻¹ for the GR samples at the Sol Hamed area (

Table 6. Results of different hazard indices associated with the radioactivity of granitic rocks at Sol Hamed, Southeastern Desert, Egypt.

Granites	(Statistical parameter)	Raeq	Hin	Hex	Iγ	Dair	AEDout	AEDin	AGDE	ELCR
										×10−3
CG	Range	91–1148	0.3–4.9	0.25–3.1	0.3–4.0	43.5–528	0.05–0.64	0.21–2.5	0.31–3.6	0.18–2.27
	Mean ± SD	398 ± 337	1.5 ± 1.4	1.1 ± 0.9	1.4 ± 1.2	184 ± 154	0.23 ± 0.18	0.9 ± 0.7	1.29 ± 1.0	0.8 ± 0.6
FG	Range	142–913	0.4–3.8	0.3–2.4	0.5–3.2	67–419	0.08–0.5	0.32–2.05	0.48–2.89	0.28–1.8
	Mean ± SD	441 ± 285	1.67 ± 1.2	1.2 ± 0.7	1.6 ± 0.9	204 ± 131	0.25 ± 0.16	1.0 ± 0.64	1.4 ± 0.8	0.87 ± 0.56
B	Range	184–1096	0.6–4.6	0.5–2.9	0.7–3.8	87–504	0.1–0.6	0.4–2.5	0.6–3.5	0.37–2.1
	Mean ± SD	559 ± 315	2.2 ± 1.4	1.5 ± 0.8	2.0 ± 1.0	258 ± 143	0.3 ± 0.17	1.26 ± 0.7	1.8 ± 0.9	1.1 ± 0.62
L	Range	36–9697	0.17–51.5	0.09–26	0.12–32.4	16.7–4479	0.02–5.4	0.08–22	0.11–30	0.07–1.9
	Mean ± SD	2027 ± 3349	10.5 ± 17.8	5.5 ± 9.0	6.8 ± 11.1	936 ± 1546	1.1 ± 1.8	4.5 ± 7.5	6.3 ± 10.3	4 ± 6
GR	Range	36–9697	0.17–51.5	0.09–26	0.12–32.4	16.7–4479	0.02–5.4	0.08–22	0.11–30	0.07–19
	Mean ± SD	856 ± 1762	3.9 ± 9.4	2.3 ± 4.7	2.9 ± 5.8	396 ± 814	0.48 ± 0.99	1.9 ± 3.9	2.7 ± 15.4	1.7 ± 3.4

), which were greater than the approved worldwide mean of 0.07 mSv y⁻¹ [4].

The (AED_in) varied from 0.08 to 22 mSv y⁻¹, with a mean value of 1.9 mSv y⁻¹ for the GR samples. The mean values for (AED_in) were moderately higher than the worldwide recommended limit of 0.41 mSv y⁻¹ [4]. The high doses can be ascribed to heavy minerals such as monazite, uraninite, and thorianite, which were concentrated in the granites. Furthermore, exposure to high doses for a long period can affect unfavorable health impacts such as cancer, and cardiovascular diseases have been linked to tissue degeneration and deoxyribonucleic acid (DNA) in genes [36].

The AGDE values ranged between 0.11 and 30 mSv y⁻¹. The mean value was 2.7 ± 15.4 mSv y⁻¹, which was nine times higher than the allowable limit of 0.3 mSv y⁻¹ [4]. Therefore, the granitic rock in the Sol Hamed area is not safe to use in construction materials.

The (ELCR) values ranged from 0.07 × 10⁻³ to 19 × 10⁻³, with a mean value of 1.7 × 10⁻³ for the GR samples, which agreed with the approved value [37] (Table 6). This suggested that exposure to the gamma rays released by the examined granitic may have adverse health effects on humans over the course of their lives.

3.6. Multivariate Statistics

A multivariate statistical approach was used to determine the associations and relationships between activity concentrations and the related potential radiological hazard factors. This work used statistics analysis such as Pearson correlation, principal component analysis (PCA), and hierarchical cluster analysis (HCA).

Table 7. The concentrations of radionuclides ²³⁸U, ²³²Th, ⁴⁰K and the radiological hazard indices.

	238U	232Th	40K	Raeq	Hin	Hex	Iγ	Dair	AEDout	AEDin	AGDE	ELCR
238U	1
232Th	0.19	1
40K	0.21	0.95	1
Raeq	1.00	0.26	0.28	1
Hin	1.00	0.23	0.24	0.99	1
Hex	1.00	0.26	0.28	1	0.99	1
Iγ	1.00	0.27	0.29	0.99	0.99	0.99	1
Dair	1.00	0.26	0.28	1	0.99	0.99	0.99	1
AEDout	1.00	0.26	0.28	1	0.99	0.99	0.99	1	1
AED	1.00	0.26	0.28	1	0.99	0.99	0.99	1	1	1
AGDE	1.00	0.27	0.28	0.99	0.99	0.99	0.99	0.99	0.99	0.99	1
ELCR	1.00	0.26	0.28	1	0.99	0.99	0.99	1	1	1	0.99	1

shows the Pearson correlation of radioactive parameters in the Sol Hamed area. The corresponding potential radiological hazard parameters had a very strong correlation with ²³⁸U. While the ²³⁸U showed a weak correlation with the ⁴⁰K activity, concentrations as an isotope did not decay from the radioactive natural series. Moreover, there was a very strong correlation between the ²³²Th and ⁴⁰K (0.95). Thus, radiological dangers and health risks are caused by high uranium activity concentrations in GR.

A principal component analysis reduces a large number of variables to a few different types of components. Within a multivariate data collection, the PCA results-processing approach aims to find any simple underlying structure. Loadings that illustrate the changeable’s relevance to the elements are bolded for values greater than 0.7. Characterizing each item exposes a few high loadings and many near-zero loadings, allowing the rotation to achieve its objectives. Increasing the range of loadings, which drives to the extreme with negative, positive, or near-zero loadings, maximizes variance. A PCA was used in this study to examine the matrix correlations between several components using varimax rotations. Figure 11 displays the PC1 and PC2 components.

The activity concentrations of ²³⁸U and ²³²Th in the GR samples showed a strong positive in PC1 loading, which was connected to all radiological variables, and 83.30% of the variation was explained (Figure 11). As a result, the most common natural radioactive contributions in the GR at the study location were ²³⁸U activity concentrations. PC2 explained 16.24% of the variation [34].

A hierarchical clustering approach was used to analyze the data of radiological parameters. The link between all of the factors is depicted in Figure 12. There were two clusters in the dendrogram of the analyzed data in the GR of the Sol Hamed area. The ²³⁸U and radiological hazard factors made up Cluster I in the GR at the studied area. While Cluster II contained ²³²Th and ⁴⁰K, which was linked to Cluster I, this investigation revealed that the total radioactivity in GR was due to uranium minerals. Finally, the results of the cluster analysis agreed with those of the Pearson correlation and PCA analysis.

4. Conclusions

The current study examined the distribution and possible modes of natural radioactive elements in granitic samples from the Sol Hamed area of the Southeastern Desert of Egypt. The obtained data displayed ²³⁸U, ²³²Th, and ⁴⁰K activity concentrations of 610 ± 1730, 110 ± 69, and 1157 ± 467 Bq kg⁻¹, respectively, which were higher than the approved worldwide values of 33, 45, and 412 Bq kg⁻¹, respectively. The radium equivalent content absorbed dose rate, annual effective dose external and internal hazard indices, and most other radiological hazard characteristics were assessed. Furthermore, the mean values of annual gonadal dosage equivalent (2.7 mSv y⁻¹) and the increased lifetime cancer risk (1.7 × 10⁻³) were calculated. Multivariate statistical approaches were applied and illustrated that the ²³⁸U principally contributed to and was predominant in the radioactivity of the granitic rock. The granitic rock included radioactivity-bearing minerals such as zircon, monazite, uraninite, thoronite, etc. Thus, Sol Hamed granites are one of Egypt’s greatest U favorability locations for holding U mineralization and using the granitic rock in building supplies poses a health concern for the wider public.