Geochemical and Radiological Characterization of Granitic-Derived Highland Coffee Soils in Chiang Mai, Thailand

Abstract

Granitic soils in the Highlands support the cultivation of Arabica coffee in northern Thailand; however, their geochemical and radiological properties are inadequately defined. This study examined major oxides, trace elements, natural radionuclides, and extractable phosphorus in granitic-derived coffee soils from the Agricultural Innovation Research, Integration, Demonstration, and Training Center (AIRID) in Chiang Mai. Twenty soil samples were obtained from 10 locations at two depth intervals (0–30 cm and 30–60 cm). Major and trace elements were analyzed via X-ray fluorescence (XRF), natural radionuclides were analyzed through high-purity germanium (HPGe) gamma spectrometry, and extractable phosphorus was determined using the Bray II method. The soils demonstrate remarkably high ⁴⁰K activity concentrations (1.2–1.9 kBq kg⁻¹) and increased K₂O contents (4.9–7.8 wt%), about three to five times more than worldwide soil averages according to Reimann & de Caritat, indicating enrichment from potassium-rich granitic rocks. Major oxide compositions suggest extensive tropical weathering, characterized by elevated SiO₂ (>60 wt%) and Al₂O₃ (>14 wt%), alongside significant depletion of CaO and MgO (<1 wt%). In topsoil, Bray II–extractable phosphorus constitutes 10–25% of total phosphorus and has a robust positive connection with P₂O₅ (R² = 0.95, p < 0.001), signifying surface accumulation and restricted vertical mobility. Multivariate analysis indicates lithogenic grouping of trace elements with negligible vertical redistribution. These findings establish a geochemical and radiological baseline for highland coffee soils in northern Thailand, with implications for soil fertility assessment, soil–plant transfer research, and evaluations of natural radioactive exposure related to coffee production.

1. Introduction

Soil fertility in high-elevation coffee plantations is strongly controlled by the underlying geological parent material [1]. In the granitic terrains that dominate the northern highlands of Thailand, soils are derived primarily from quartz, K-feldspar, plagioclase, biotite, and amphibole. During progressive chemical weathering, trace elements are released from these primary minerals in a predictable sequence. Transition metals such as Co, Ni, Cr, V, Cu, Ga, Zn, and Pb are mainly supplied by the gradual decomposition of mafic minerals (biotite and amphibole), whereas elements such as Th, U, Y, Nb, and Sr are largely associated with accessory minerals (e.g., monazite, xenotime, apatite, and zircon) and with secondary Fe- and Al-oxide phases [1,2,3]. These mineral-derived geochemical signatures can persist in tropical, well-drained upland soils and provide a robust framework for interpreting nutrient dynamics and trace element behavior. Potassium (K) is one of the most important macronutrients controlling the growth and productivity of Coffea arabica in upland environments. Unlike nitrogen and phosphorus, potassium is not structurally incorporated into organic matter and is therefore retained mainly in exchangeable pools derived from the weathering of K-bearing minerals, such as K-feldspar and micas. Potassium availability is further regulated by adsorption onto Fe–Al oxides and by leaching losses under high rainfall conditions [3]. Coffee cultivators in northern Thailand grow Arabica coffee on elevated granitic soils that have had significant tropical weathering, leading to acidic conditions, poor base saturation, and a reduction in exchangeable calcium and magnesium due to extensive leaching from monsoon precipitation [4]. Despite granitic parent materials providing significant potassium via the weathering of K-feldspar and mica, this frequently results in nutrient imbalance rather than optimal fertility, as increased K availability may be associated with deficiencies in Ca, Mg, and micronutrients, negatively impacting nutrient uptake efficiency and yield stability [5,6]. Phosphorus supply is a continual limitation as phosphate is significantly adsorbed onto iron and aluminum oxides generated through extensive weathering, diminishing fertilizer efficacy and elevating production expenses [7,8,9]. The issues are intensified by steep gradients and substantial precipitation, which facilitate erosion and nutrient depletion in upland coffee systems [10]. Comprehending the geochemical and radiological properties of these soils is essential for differentiating lithogenic nutrient sources from human contributions, elucidating the factors influencing nutrient mobility and trace-element dynamics [11,12], and determining baseline activity concentrations of naturally occurring radionuclides, including ⁴⁰K, U, and Th, in granitic terrains [13]. This fundamental information supports soil–plant transfer studies, promotes sustainable coffee production, and provides reference radionuclide activity concentrations to support external exposure assessment and future soil–plant transfer investigations. Consequently, the natural K status of granitic soils can either reduce the need for external fertilization or, if depleted, become a major limitation to sustainable coffee production. Despite the agronomic importance of potassium, quantitative data on K concentrations and associated natural radioactivity in Thai highland soils remain limited. Granitic rocks are also naturally enriched in the radioactive isotope ⁴⁰K, as well as in uranium- and thorium-series radionuclides [14,15]. Weathering and pedogenesis can redistribute these radionuclides within the soil profile, where they may become associated with secondary oxide and clay mineral phases. Northern Thailand, particularly Chiang Mai Province, has been recognized as an area of relatively high natural background radiation compared with other regions of the country [16]. However, little information is available on the distribution of natural radionuclides specifically within agricultural soils used for coffee cultivation and on their relationships with soil mineralogy and geochemistry. While research specifically focused on radionuclide distributions in soils cultivated with coffee is limited, several peer-reviewed studies of agricultural soils in coffee-producing or geologically similar areas indicate that the activity concentrations of natural radionuclides are predominantly influenced by parent material, soil mineralogy, and geochemical processes. In southern Ecuador, a significant Andean coffee-growing area, Ramos-Lerate et al. demonstrated that the activities of ²²⁶Ra, ²³²Th, and ⁴⁰K in both cultivated and uncultivated agricultural soils are predominantly governed by geological background, with minimal impact of farm practices, underscoring the preeminence of lithogenic factors on soil radioactivity [17]. Comparable findings were documented for agricultural soils in Yemen, a conventional coffee-exporting nation, where Hussien et al. noted that the geographical variability in activity concentrations of ²²⁶Ra, ²³²Th, and ⁴⁰K is indicative of soil-forming processes and parent lithology, rather than land use alone [18]. In Brazil, a leading global coffee producer, the distribution of natural radionuclides in cultivated soils is intricately associated with pedological attributes and mineralogical composition, notably the prevalence of potassium-rich minerals and thorium-enriched accessory phases [19,20]. Collectively, these studies demonstrate that radionuclide concentrations in agricultural soils of coffee-growing areas are primarily geogenic and closely related to soil mineralogy and geochemistry, underscoring the necessity for site-specific characterization in evaluating radionuclide dynamics within coffee cultivation systems. In addition to potassium and natural radionuclides, phosphorus (P) behavior in highly weathered tropical soils is strongly influenced by Fe–Al oxide phases, which can immobilize phosphate through specific adsorption reactions. As a result, surface accumulation of P from repeated fertilizer application is common, whereas vertical mobility is typically limited. Understanding the coupled behavior of P, K, trace elements, and natural radionuclides in granitic-derived soils is therefore essential for evaluating long-term soil fertility, nutrient-use efficiency, and environmental geochemical baselines in upland agroecosystems. This study aims to: (i) quantify the major and trace element composition of granitic-derived highland coffee soils in Chiang Mai, Thailand; (ii) determine the activity concentrations of the natural radionuclides ⁴⁰K, ²³⁸U, and ²³²Th in soil profiles and analyze their correlation with K content; (iii) assess vertical variations in extractable and total P; and (iv) identify the predominant lithogenic and pedogenic influences on element distributions through multivariate statistical analysis.

2. Materials and Methods

2.1. Study Area and Sampling

The study was conducted in the Agricultural Innovation Research, Integration, Demonstration, and Training Center (AIRID; 18°55′19.6″ N, 98°48′55.0″ E, Figure 1) located within the Nhong Hoi Highland Agricultural Research Station, Pong Yang Sub-district, Mae Rim District, Chiang Mai Province, Thailand. The site lies at an elevation of 850–900 m above sea level, with an average slope of 18–25° [21]. The climate is tropical, characterized by three seasons influenced by Pacific typhoons and the southwest monsoon; mean annual precipitation is 1354 mm (mainly April–August) and mean annual temperature is 28.5 °C (range: 10.3 °C in January to 39.8 °C in July–August). Geologically, the area belongs to the Central Granitic Belt and is underlain by granodiorite and monzogranite intrusions rich in K-feldspar, quartz, and biotite (Petrographic analysis, Ref. [22]). These lithologies give rise to Ferralsols (WRB classification, Ref. [23]) with naturally high potassium concentrations. At elevations around 1000 m, fertilization is typically applied in May, August, and October, with a harvest period of approximately nine months. At AIRID and its associated demonstration sites, research encompasses seedling production, planting on sloped highland terrain, fertilization scheduling, pest and disease management, and post-harvest evaluation, often integrated into community outreach and agritourism programs such as ‘from seed to cup’ coffee educational experiences [24]. Coffee is grown in areas with Ferralsols originating from granitic parent materials characteristic of the Central Granitic Belt in northern Thailand, influencing soil fertility, nutrient composition, and hydrological dynamics [24]. The distribution of soil types in the broader region can be obtained from national and international soil survey databases, facilitating the development of schematic soil maps to depict AIRID’s edaphic context [24].

Root distribution studies on Coffea spp. have shown that 30–55% of total root biomass occurs within the upper 10–30 cm of soil, and approximately 95% of roots are confined to the top 30 cm in clayey substrates [25,26,27,28]. Accordingly, soil samples were collected at two depth intervals—0–30 cm (root-active zone) and 30–60 cm (sub-surface layer)—to capture vertical variations in elements.

On 13 July 2023, ten sampling points were established across a relatively homogeneous portion of the coffee farm. At each point, an auger was used to retrieve composite samples from the two depth intervals described above. The locations were selected to represent the range of topographic positions (e.g., slope aspect and curvature) and management practices present within the study area. This sampling design follows a stratified random approach commonly used in agronomic soil surveys to depict the spatial diversity of soil parameters within the study area. Before sampling, the coffee farm was categorized into distinct strata according to observable site factors that affect soil growth and nutrient distribution. Sampling locations within each stratum were selected at random while ensuring a minimum distance to prevent spatial clustering. A total of ten sampling points were selected within the study area to ensure representative coverage of the observed variability in soil properties (see Figure 1).

Figure 1. The Agricultural Innovation Research, Integration, Demonstration, and Training (AIRID) site (18°55′19.6″ N, 98°48′55.0″ E) within the Nhong Hoi Highland Agricultural Research Station is marked [29].

Figure 1. The Agricultural Innovation Research, Integration, Demonstration, and Training (AIRID) site (18°55′19.6″ N, 98°48′55.0″ E) within the Nhong Hoi Highland Agricultural Research Station is marked [29].

2.2. Radiological Analysis

The soil samples were dried at 110 °C and stored in pre-weighed polystyrene containers (U8; outer diameter = 50 mm, inner diameter = 48 mm, height = 62 mm), following the method described in Hosoda et al. (2013) and then left to reach radioactive stored for >28 days prior to measurement to ensure secular equilibrium between ²²⁶Ra and its short-lived progeny ²²²Rn [30]. The natural radionuclide measurements were conducted using an HPGe detector (EGPC 100-P15, CANBERRA, Meriden, CT, USA). Each measurement was run for 80,000 s. Radionuclide concentrations were decay-corrected to the sampling date. Calibration was performed using standard gamma volume sources (MX033U8PP; Japan Radioisotope Association, Tokyo, Japan), which contained nine mixed nuclides (¹⁰⁹Cd, ⁵⁷Co, ¹³⁹Ce, ⁵¹Cr, ⁸⁵Sr, ¹³⁷Cs, ⁵⁴Mn, ⁸⁸Y, and ⁶⁰Co) with five different thicknesses (5, 10, 20, 30, and 50 mm) according to the Japanese Nuclear Regulation Authority. Minimum detectable activities (MDAs) were evaluated based on measurements conducted with a counting time of 80,000 s and were derived from the analysis software (Spectra Explorer software version 2.13), which reported detection limits for the gamma lines used in activity determination. Under these measurement conditions, MDAs were on the order of (1.2–1.5) × 10⁻² Bq g⁻¹ for ⁴⁰K (1460.8 keV), (2.0–2.6) × 10⁻³ Bq g⁻¹ for the ²³⁸U decay series (assessed via ²¹⁴Pb and ²¹⁴Bi assuming secular equilibrium), and (4.0–5.0) × 10⁻³ Bq g⁻¹ for the ²³²Th decay series (via ²²⁸Ac at 911.2 keV). Variability among samples reflects differences in sample mass, detector efficiency at specific gamma energies, and background levels, rather than analytical inconsistency. The activity concentrations of ⁴⁰K were ascertained utilizing the 1460.75 keV gamma line. The decay series of ²³⁸U was calculated indirectly by gamma emissions from ²¹⁴Pb (295.22 and 351.99 keV) and ²¹⁴Bi (609.31, 1120.29, and 1238.11 keV), whereas the decay series of ²³²Th was quantified using ²²⁸Ac (338.70, 911.20, and 968.80 keV), ²¹²Pb (238.63 keV), and ²⁰⁸Tl (583.14 and 860.37 keV). Measurement uncertainties are stated to vary from several percent to under 10%. Annual effective doses were estimated for an outdoor agricultural worker exposure scenario using internationally recommended conversion coefficients and an outdoor occupancy factor of 0.2.

Absorbed dose rates in air (D, nGy h⁻¹) were estimated from the measured activity concentrations of the ²³⁸U series, ²³²Th series, and ⁴⁰K using internationally recommended conversion coefficients. The absorbed dose rate was calculated using the following equation:

$$\mathrm{D}=0.462A_U+0.604A_{Th}+0.0417A_K$$

(1)

where $A_U$, $A_{Th}$, and $A_K$ represent the activity concentrations (Bq kg⁻¹) of the ²³⁸U series, ²³²Th series, and ⁴⁰K, respectively. The coefficients (nGy h⁻¹ per Bq kg⁻¹) were adopted from UNSCEAR (2000) [13].

2.3. Geochemical Analysis

Soil samples were combusted at 800 °C for 8 h to remove organic matter and carbonates prior to geochemical analysis. Following combustion, 0.5 g of each sample was fused with 5.0 g of flux to produce a borate glass bead using an electrical fusion system (Bead & Fuse Sampler TK-4100, Amena Tech, Yokohama, Japan) at 1141 °C. The flux consisted of a lithium borate mixture containing 67% Li₂B₄O₇ and 33% LiBO₂. Fusion was performed in Pt–Au crucibles (95% Pt, 5% Au). After fusion, the melt was rapidly quenched to obtain a homogeneous glass bead suitable for XRF analysis. Elemental concentrations were measured using a wavelength-dispersive X-ray fluorescence (WD-XRF) spectrometer (ZSX Primus IV, Rigaku, Japan) operated under vacuum conditions, with calibration performed using certified geological reference materials.

Major and trace elements were quantified by X-ray fluorescence spectrometry following borate fusion. Major oxides determined included SiO₂, Al₂O₃, Fe₂O₃, MgO, CaO, MnO, Na₂O, K₂O, and P₂O₅. Trace elements (Ba, Ce, Co, Cr, Cu, Ga, Nb, Ni, Pb, Rb, Sr, Th, U, V, W, Y, Zn, Zr, and As) were measured to support the interpretation of weathering intensity, lithogenic controls, and potential anthropogenic contributions.

To compare XRF-derived potassium concentrations with HPGe-measured ⁴⁰K activities, ⁴⁰K was independently estimated from K₂O values using a mass-basis conversion. Elemental potassium was first derived from K₂O using the molar-mass ratio (2M K/1M K₂O = 0.83015). The potassium concentration was then converted from wt% to g kg⁻¹ (1 wt% = 10 g kg⁻¹), and ⁴⁰K activity was calculated assuming a specific activity of 31.1 Bq g⁻¹ for natural potassium (⁴⁰K (Bq kg⁻¹) = K₂O (wt%) × 258.3).

All K₂O concentrations are reported on an oven-dry basis (110 °C), and the calculated ⁴⁰K activities therefore correspond to the same oven-dry mass basis. No LOI correction or normalization to 100% was applied to the oxide data; thus, no dry-versus-ignited inconsistency is introduced in the conversion.

The data processing, statistical analysis, and visualization were conducted using Python 3.12 within a Google Colab environment. Data manipulation and numerical operations were performed using pandas (v2.2.2) and numpy (v2.0.2). Visualization employed matplotlib (v3.10.0) and seaborn (v0.13.2). Prior to multivariate analysis, major oxide data were centered and scaled using Z-score normalization. Principal component analysis (PCA) was applied to the standardized dataset to identify dominant geochemical patterns. K-means clustering was subsequently performed on the PCA scores of the first two principal components, resulting in the classification of samples into three compositional clusters [31]. Hierarchical clustering and additional statistical routines were implemented using scipy (v1.16.3). Major oxide concentrations are compositional data constrained by constant-sum effects. In this study, Z-score standardization was applied to explore relative variation patterns; however, no log-ratio transformation was performed. Therefore, PCA and clustering results are interpreted descriptively as visualization tools for relative geochemical gradients rather than as formal compositional-data analysis. Interpretations are supported by independent elemental trends and geological reasoning.

2.4. Bray II Extraction

A 2.5 g aliquot of sieved soil (<2 mm) was placed into a 50 mL bottle, to which 25 mL of Bray II extractant (0.03 N NH₄F, 0.1 N HCl) was added. The mixture was shaken for 1 min and subsequently filtered. An aliquot (1–5 mL) of the clear filtrate was transferred into a 25 mL volumetric flask, followed by the addition of 5 mL of molybdenum color reagent (MCR). The volume was adjusted to 25 mL with distilled water, mixed thoroughly, and allowed to develop color for 10 min. Absorbance was measured at 882 nm using a UV–Vis spectrophotometer. Phosphorus concentrations were quantified using an external calibration curve prepared from potassium dihydrogen phosphate (KH₂PO₄) standard solutions. Calibration standards with concentrations of 0, 0.2, 0.4, 0.6, 0.8, and 1.0 mg P L⁻¹ were prepared by serial dilution and processed using the same extraction and color-development procedures as the soil samples. The calibration curve was constructed by linear regression of absorbance measured at 882 nm versus phosphorus concentration and was verified to be linear prior to sample analysis.

Extractable phosphorus was measured using the Bray II method. A subsample of soil was shaken with Bray II extractant, filtered, and analyzed colorimetrically. Total phosphorus measured via XRF was compared with extractable fractions to evaluate accumulation and mobility.

3. Results

3.1. Natural Radionuclide ⁴⁰K Enrichment

The activity concentrations of ⁴⁰K measured by HPGe gamma spectrometry ranged from 1.2 ± 0.1 to 1.9 ± 0.2 kBq kg⁻¹ (n = 20). The ⁴⁰K activities estimated from K₂O using the stated conversion factor (⁴⁰K = 258.3 × K₂O, where K₂O is in wt%, oven-dry basis) ranged from 1.2 to 1.9 kBq kg⁻¹ and showed strong agreement with HPGe-measured values (Supplementary Figure S1), confirming internal analytical consistency and mass-basis alignment between methods. This difference can be attributed to contrasting geological settings. The present study area is developed on granitic parent material characterized by abundant K-bearing feldspars and mica minerals, which naturally elevate potassium and associated ⁴⁰K levels. In contrast, soils in the Kong Khaek subdistrict are derived from non-granitic lithologies with lower primary potassium content, resulting in lower background ⁴⁰K activity concentrations. The observed differences, therefore, reflect lithogenic controls rather than anthropogenic inputs [16].

Table 1. Comparison of major oxide concentrations (oven-dry basis) from the studied soils and previous studies of Thai paddy soil and the global median [32].

Parameter	This Study (Coffee Soils)	Thai Paddy Soils (Median)	Global Median
40K activity (kBq/kg)	1.2–1.9	0.2–1.1	–
K₂O (%)	4.9–7.8	0.8	1.7
SiO₂ (%)	70.5–76.3	75.1	70.6
Fe₂O₃ (%)	3.8–4.2	3.8–4.2	5.7
CaO (%)	0.2–0.4	0.3	2.1
MgO (%)	0.4–0.6	0.5	0.8

summarizes representative major oxide concentrations from the studied soils. Median K₂O contents reached 5.3% (range 4.9–7.8%).

The ²³⁸U–series activity concentrations, determined from ²¹⁴Pb and ²¹⁴Bi under equilibrium conditions, ranged from approximately 0.07 to 0.10 kBq kg⁻¹, with a mean value of approximately 0.085 kBq kg⁻¹. The consistency between daughter radionuclides within counting uncertainties indicates stable equilibrium and reliable measurement conditions. These values fall within typical background levels reported for granitic soils.

The ²³²Th–series activities, derived from ²²⁸Ac, ²¹²Pb, and ²⁰⁸Tl, ranged from approximately 0.10 to 0.13 kBq kg⁻¹, with a mean value of approximately 0.1 kBq kg⁻¹. Agreement among daughter radionuclides confirms equilibrium within the thorium decay series. Compared with global soil averages, the measured uranium- and thorium-series activities are within expected ranges for granitic terrains and do not indicate anomalous enrichment.

Overall, the radionuclide distributions demonstrate that the radiological characteristics of the AIRID soils are controlled primarily by granitic parent material, with pronounced enrichment in ⁴⁰K and typical background levels of uranium and thorium.

Radiation Dose Assessment

Absorbed dose rates in air were estimated using internationally recommended conversion coefficients for the ²³⁸U–series, ²³²Th–series, and ⁴⁰K based on the measured activity concentrations according to Equation (1). The total absorbed dose rates ranged from approximately 65 to 95 nGy h⁻¹, with a mean value of approximately 80 nGy h⁻¹ across the study area. The contribution of ⁴⁰K dominated the total dose due to its elevated activity concentrations (1.2–1.9 kBq kg⁻¹), while the uranium- and thorium-series radionuclides provided smaller but measurable contributions.

To define a realistic exposure condition, annual effective doses were estimated assuming an outdoor agricultural worker exposed to external gamma radiation from soil. An outdoor occupancy factor of 0.2 was applied in accordance with UNSCEAR recommendations for individuals engaged in agricultural activities [13]. Under this scenario, annual effective doses ranged from approximately 0.08 to 0.12 mSv yr⁻¹, with a mean value of approximately 0.1 mSv yr⁻¹.

Although the absorbed dose rates are slightly higher than the global median outdoor terrestrial value (~59 nGy h⁻¹), the calculated annual effective doses remain well below the worldwide average natural radiation exposure of 2.4 mSv yr⁻¹ reported by UNSCEAR. The elevated dose rates are therefore attributable to the naturally high potassium content of the granitic parent material rather than anthropogenic contamination, and they do not indicate radiological concern for external exposure of agricultural workers in the study area [13].

3.2. Controls on Element and Radionuclide Mobility in Granitic-Derived Soils

Radionuclide mobility in the examined soils is primarily governed by lithogenic and pedogenic factors, with soil mineralogy and oxide composition exerting strong control over element retention and dispersion [33]. The granitic parent material of the study area contributes to elevated background levels of naturally occurring radionuclides and trace elements, consistent with previous findings that radionuclide behavior in soils is largely dictated by mineral-associated sorption and immobilization processes [33]. Iron and aluminum oxide phases, which are abundant in strongly weathered tropical soils, possess high specific surface areas that promote effective adsorption of trace elements and radionuclides, thereby limiting their mobility [34]. These oxides and oxyhydroxides play a central role in adsorption, ion transport, and sorption stability, acting as major sinks that restrict vertical migration of both lithogenic and fertilizer-derived elements [34]. Radionuclide studies further demonstrate that relatively immobile species frequently associate with weakly crystalline Fe–Al minerals and organic matter under typical soil conditions, further impeding downward transport within the soil profile [35]. Agricultural management practices may enhance localized accumulation of nutrient-related elements, particularly phosphorus and potassium; however, these inputs generally do not override dominant pedogenic controls on element mobility [36,37,38,39]. The presence of Fe–Al oxides and clay minerals in these granitic soils substantially increases sorption capacity, restricting vertical redistribution even for elements introduced through fertilization [40,41,42]. Overall, the integrated geochemical and radiological evidence indicates that element mobility in these granitic-derived soils is limited, with mineralogical and oxide controls prevailing over simple leaching or vertical transport mechanisms [43]. Major oxide concentrations on an oven-dry (110 °C) basis are summarized in

Table 2. Comparison of major oxide concentrations (%) on an oven-dry basis reported in the literature, including data for granitic-derived soils and Thai paddy soils [32,44,45].

Elements	This Study		Thai Paddy Soils	Worldwide Average
	0–30 cm (Surface)	30–60 cm (Subsurface)
SiO₂	72.5 ± 4.2	75.3 ± 3.8	71.1–75.1	70.6
TiO₂	0.35 ± 0.04	0.34 ± 0.03	0.9	0.8
Al₂O₃	15.3 ± 0.8	14.8 ± 0.9	15.9	13.5
Fe₂O₃	4.2 ± 0.3	4.0 ± 0.4	3.8–4.2	5.7
MnO	0.15 ± 0.03	0.14 ± 0.02	0.04	0.1
MgO	0.35 ± 0.05	0.33 ± 0.04	0.5	0.8
CaO	0.21 ± 0.05	0.18 ± 0.04	0.3–0.4	2.1
Na₂O	0.28 ± 0.05	0.26 ± 0.04	0.3	0.9
K₂O	6.8 ± 0.9	5.9 ± 1.0	0.7–0.8	1.7
P₂O₅	0.18 ± 0.05	0.11 ± 0.04	0.01	0.2

.

3.3. Multivariate Analysis of Trace Elements

3.3.1. Correlation Structure of Trace Elements

Principal Component Analysis (PCA) was employed as an exploratory multivariate approach to reduce dimensionality and mitigate multicollinearity among major and trace elements, thereby facilitating identification of the dominant geochemical gradients influencing soil composition. Prior to PCA, all variables were centered and scaled using Z-score normalization to ensure equal weighting of elements with differing units and variances. K-means clustering was subsequently applied to PCA scores to classify samples within a standardized, low-dimensional space highlighting meaningful compositional variation. Clustering was performed using the scores of the first two principal components (PC1 and PC2), which together explain the majority of variance in the major-oxide dataset (Figure 2).

The number of clusters (k = 3) was selected based on convergence of the within-cluster sum of squares and the geochemical interpretability of the resulting groupings. Rather than relying on formal cluster optimality diagnostics, the clustering solution is supported by its consistency with independent geochemical evidence, including major-oxide distributions, trace-element correlation patterns, depth-related trends, and hierarchical clustering results. Accordingly, the multivariate analysis is interpreted descriptively, with emphasis on robust compositional structure rather than inferential cluster validation.

Multivariate analysis integrating both major and trace elements revealed coherent and interpretable geochemical groupings across the AIRID soils. Cluster 1 comprises most samples and is characterized by slightly higher standardized Na₂O and K₂O and comparatively lower Al₂O₃–Fe₂O₃–TiO₂, indicating relatively alkali-richer compositions within the dataset. Cluster 2 contains only I-30 and J-30 and shows strong SiO₂ enrichment coupled with pronounced depletion of Na₂O and K₂O, separating these silica-rich samples from the main population. Cluster 3 is enriched in Al₂O₃, Fe₂O₃, TiO₂, MnO, and MgO and depleted in SiO₂ and K₂O, consistent with a more oxide/residual-mineral–influenced composition.

Standardized values represent deviations from the dataset mean expressed in units of standard deviation and indicate relative enrichment or depletion rather than absolute concentration differences. When interpreted together with PCA loadings, these values define cluster positions along dominant geochemical gradients and link cluster differentiation primarily to mineralogical composition and weathering processes rather than concentration magnitude alone, as illustrated in Figure 2.

Trace-element distributions closely mirror the major-element clustering structure. As shown in the standardized trace-element heatmap (Figure 3), mafic-associated elements.

Hierarchical clustering of standardized trace-element data in Figure 4 further supports these relationships, separating trace elements into mafic-derived, felsic-derived, and accessory-mineral-associated groups, while samples cluster primarily according to geochemical similarity rather than soil depth. This pattern indicates that parent-material inheritance exerts a stronger control on trace-element distributions than vertical redistribution processes.

The supplementary Figure S2 provided a strong positive relationship observed between total phosphorus (P₂O₅ determined by XRF) and Bray II–extractable phosphorus in surface soils (Pearson correlation, r = 0.97, p < 0.001). Paired t-tests comparing surface (0–30 cm) and subsurface (30–60 cm) soils were conducted for major oxides and trace elements. To account for multiple comparisons, p-values were adjusted using the Benjamini–Hochberg false discovery rate (FDR) procedure. After adjustment, P₂O₅ remained significantly different between depths (FDR-adjusted p < 0.05), whereas all other elements showed no statistically significant depth-related differences (adjusted p > 0.05).

3.3.2. Implications for Soil Genesis

The multivariate geochemical patterns indicate that the highland soils of Chiang Mai retain strong mineralogical signatures inherited from their granitic parent materials. Coherent mafic-associated signals reflect limited mobility of transition metals, while the distinct behavior of Ba and Rb highlights persistent contributions from K-bearing minerals relevant to potassium availability in coffee agroecosystems. Accessory-element patterns suggest ongoing weathering of trace minerals coupled with sorption onto Fe–Al oxide surfaces.

Chiang Mai Province is recognized for its elevated natural background radiation levels in Thailand [16], with reported average soil ⁴⁰K activities of approximately 0.7 kBq kg⁻¹, exceeding global averages [16,46]. In the present study, soils from the Chiang Mai coffee field exhibit exceptionally high ⁴⁰K activity concentrations, ranging from 1.2 to 1.9 kBq kg⁻¹, corresponding to approximately three to five times the global average soil value (~0.4 kBq kg⁻¹) [13,22].

4. Discussion

4.1. Soil Geochemical Characteristics and Fertility Implications

The increased concentrations of SiO₂ and Al₂O₃ present in the examined soils substantially influence soil fertility and physical properties. Elevated SiO₂ levels signify the dominance of quartz and silica-rich sand and silt constituents, which are chemically inert and contribute negligibly to nutrient availability [1]. Thus, soils with high SiO₂ concentrations typically exhibit poor inherent nutrient stocks and limited buffering capacity, making crop yields largely dependent on external fertilizer applications and organic matter fluctuations [47]. Elevated Al₂O₃ concentrations signify the prevalence of aluminosilicate clay minerals and aluminum-rich secondary phases generated by extensive weathering [48]. Although these minerals enhance soil structure and aggregation, they are typically linked to a poor cation exchange capacity per unit mass and a high sorption of phosphorus, hence diminishing its availability to plants. Moreover, aluminum-rich soils frequently display acidic conditions, which can further restrict nutrient availability and root development if inadequately handled [34]. The combined presence of quartz-rich coarse fractions and clay-rich aluminum-bearing phases results in soils that are generally well drained but susceptible to erosion and characterized by moderate to poor water-holding capacity. These properties are typical of strongly weathered tropical soils derived from granitic parent material and highlight the need for careful soil management practices to sustain long-term soil fertility and agricultural productivity.

The amalgamation of quartz-rich coarse fractions and clay-rich aluminum-bearing phases results in well-drained yet erosion-susceptible soils with moderate to poor water retention capacity [49]. These characteristics are indicative of extensively worn tropical soils originating from granitic parent material and necessitate meticulous management, including the incorporation of organic matter and erosion mitigation, to maintain enduring soil fertility and agricultural output [49].

4.2. Potassium Content and ⁴⁰K Activity Concentrations

The AIRID soils exhibit substantially higher than reported medians for Thai paddy soils (0.8%) and global averages (1.7%) [32]. Other major oxides (SiO₂, Fe₂O₃, CaO, MgO) fall within ranges typical of strongly weathered granitic soils in the region. The measured activities are higher than those reported for soils in the Kong Khaek subdistrict of Chiang Mai (0.2–1.1 kBq kg⁻¹; Autsavapromporn et al., 2024) [16]. The elevated K₂O contents and corresponding ⁴⁰K activities indicate that the AIRID soils possess a naturally high potassium reservoir, which may reduce the need for supplemental K fertilization in Arabica coffee cultivation. The average specific activity of ⁴⁰K in soil: 0.4 ± 0.024 kBq kg⁻¹ [13,46]. These values exceed global terrestrial ⁴⁰K averages but remain well below the worldwide average natural radiation exposure of 2.4 mSv yr⁻¹ under the defined outdoor exposure scenario, indicating elevated natural background but no radiological concern for agricultural workers [13]. The results are interpreted cautiously with emphasis on consistent geochemical patterns rather than isolated significance values. Full major oxide data for all samples are provided in Supplementary Table S1.

In addition to ⁴⁰K, the activity concentrations of ²³⁸U- and ²³²Th-series radionuclides were evaluated to provide a comprehensive radiological characterization. While measurable, their activities fall within typical background ranges for granitic terrains and contribute less to the total absorbed dose compared with ⁴⁰K. The relative dose contribution is dominated by ⁴⁰K, followed by the ²³²Th-series and minor contributions from the ²³⁸U-series, a distribution characteristic of highly weathered granitic systems in tropical environments.

The combined geochemical and radiological evidence therefore indicates that radionuclide activities are predominantly lithogenic in origin, reflecting mineral inheritance from the granitic parent material rather than agricultural inputs or anthropogenic contamination.

4.3. Phosphorus Dynamics

Phosphorus data indicate that total P content is a strong predictor of plant-available P in the surface soil layer. The surface-to-subsurface P₂O₅ ratio of 2.5 demonstrates marked phosphorus enrichment in the upper 0–30 cm, consistent with surface fertilizer application, organic matter turnover, and the well-documented low vertical mobility of phosphorus in humid tropical soils. These results highlight the dominant influence of surface management practices on phosphorus availability within the soil profile.

The distribution of P₂O₅ between soil depths, together with its relationship to extractable phosphorus, indicates a system characterized by strong phosphorus retention dominated by Fe-oxide interactions. This pattern is consistent with ferrallitic weathering processes typical of granitic highland soils, where intense leaching and secondary mineral formation promote the accumulation of Fe–Al oxides capable of strongly adsorbing phosphate [50]. The pronounced enrichment of extractable P in surface soils is consistent with repeated fertilizer applications, a common phenomenon in managed tropical cropping systems [51]. The positive correlation between total P and extractable P suggests progressive accumulation at the surface with limited downward transport, reflecting the low mobility of phosphate in highly weathered soils [52]. The dominance of Fe and Al oxides—particularly goethite, hematite, and gibbsite—enhances phosphate adsorption through ligand exchange mechanisms, thereby restricting vertical movement but permitting gradual long-term buildup in the upper horizons [53]. This immobilization behavior has implications for soil fertility, as strongly adsorbed P may become less plant-available over time, while excess surface accumulation can increase the risk of P loss through erosion or runoff under high-rainfall conditions [54,55,56,57,58].

In ferrallitic weathering conditions characteristic of granitic highland soils, vigorous leaching facilitates the development and buildup of secondary Fe and Al oxides, including goethite, hematite, and gibbsite, which demonstrate a strong affinity for phosphate [59]. Phosphate is predominantly immobilized by inner-sphere ligand exchange processes, in which phosphate anions substitute surface hydroxyl groups on Fe–Al oxide minerals, resulting in robust and frequently irreversible surface complexes [60].

This mechanism limits vertical phosphorus mobility while facilitating surface accumulation, aligning with the observed concentration of extractable phosphorus in topsoil layers and the positive association between total and extractable phosphorus [61]. From a fertility standpoint, robust phosphate sorption diminishes immediate phosphorus availability to plants, hence heightening need on fertilizer applications to sustain sufficient soil solution phosphorus concentrations [61]. Over time, repeated fertilizer applications can result in the gradual accumulation of phosphorus in surface horizons, where heavily adsorbed phosphorus may function as a slow-release reservoir. Conversely, significant surface buildup elevates the danger of phosphorus loss by erosion or runoff during high-rainfall events, despite minimal leaching, underscoring the necessity for meticulous nutrient management in highly worn tropical soils [62].

4.4. Element Interpretation

Element mobility in the examined soils is controlled by lithogenic and pedogenic variables, with soil mineralogy and oxide concentration playing important roles in regulating contaminant dispersion and retention [33]. Granitic parent material contributes to heightened background levels of naturally occurring radionuclides and trace elements, corroborating findings that soil mineralogy significantly affects radionuclide behavior and retention in natural systems, as radionuclide interactions with soil constituents are governed by sorption and immobilization mechanisms linked to minerals [33]. Iron and aluminum oxide phases are prevalent in extensively worn tropical soils and have substantial specific surface areas that effectively adsorb trace elements and radionuclides, hence restricting their mobility [34]. Iron and aluminum oxides and oxyhydroxides affect adsorption processes, ion transport, and the stability of element sorption in soils, serving as significant sinks for elements and diminishing their vertical mobility, according to accepted soil geochemistry principles [34]. Moreover, radionuclide investigations have demonstrated that immobile species frequently correlate with weakly crystalline Fe/Al minerals and organic matter under standard soil conditions, hence further impeding their mobility within the profile [35].

Agricultural management approaches enhance the localized accumulation of nutrient-related elements (e.g., P, K) but typically do not surpass the pedogenic influence on contaminant spread [36,37,38,39]. The existence of Fe–Al oxides and clay minerals in these granitic soils increases sorption capacity, thereby restricting downward transit, even for elements introduced via fertilization [40,41,42]. The integrated geochemical and radiological data suggest that the mobility of elements in these granitic-derived soils is minimal, with mineralogical and oxide factors prevailing over basic leaching or vertical transport mechanisms [43].

4.5. Implications for Coffee Agronomy

Elemental distributions, especially K, Ca, Mg, and P behavior, are directly relevant to nutrient availability for coffee plants. High natural K reservoirs reduce dependency on fertilizer inputs, while P retention indicates potential need for P management strategies. A higher surface-to-subsurface P₂O₅ ratio indicates that phosphorus is more concentrated in the surface soil layer compared to deeper layers. This pattern reflects the accumulation of phosphorus, which might be due to surface applications of fertilizers, organic matter decomposition, and limited vertical movement of phosphorus in the soil profile.

4.6. Trace Element Behavior and Geochemical Implications

Trace element distributions in the studied soils reveal a strong lithogenic imprint that reflects the mineralogical composition of the granitic parent material. Elements such as Co, Ni, Cr, V, Cu, Ga, Pb, Zn, and As form a coherent group and consistently show strong positive relationships across both depths. These trace metals are primarily released during the weathering of biotite and amphibole, minerals that host transition metals within their octahedral layers. Their close inter-element associations and limited mobility in acidic, well-drained tropical soils allow these lithogenic signatures to be preserved even after long-term weathering [63].

In contrast, Ba, Rb, and Zr indicate the influence of felsic mineral components. Ba and Rb derive from K-feldspar and mica, while Zr originates almost exclusively from zircon, a highly resistant accessory mineral. The chemical durability of zircon explains the stability of Zr concentrations across depths and its well-established role as an indicator of cumulative weathering and mineral residue enrichment [64]. The opposite behavior of this felsic-associated group relative to the mafic-derived elements highlights the contrasting contributions of different mineral phases within the parent rock.

A third trace element association, including Th, U, Y, Nb, Sr, and W, reflects inputs from accessory minerals such as monazite, xenotime, apatite, and zircon, together with strong sorption by Fe- and Al-oxide phases. These oxide minerals are abundant in highly weathered granitic soils and play a key role in immobilizing many trace metals. In particular, the low mobility and oxide affinity of Th and U indicate strong retention within the soil matrix, with minimal leaching under current environmental conditions [65].

The distribution of trace elements in the AIRID soils demonstrates significant lithogenic and pedogenic influence with restricted vertical mobility. Consistent associations of Co, Ni, Cr, V, Cu, Zn, Pb, and As at both depths, along with their robust inter-element correlations, indicate a shared mineralogical source related to the weathering of biotite and amphibole. The lack of notable depth-related variations signifies robust retention by clay minerals and Fe–Al oxides in acidic tropical environments [66].

Numerous elements, such as Cu and Zn, are vital micronutrients for coffee plants; yet, their significant interaction with oxide and clay phases suggests restricted bioavailability despite low overall concentrations [67,68]. The effects of fertilizers seem subordinate to mineralogical factors, as trace elements exhibit negligible vertical redistribution and are predominantly retained in surface soils [69]. The findings indicate minimal trace-element mobility and a moderate toxicity risk, while emphasizing the possibility of micronutrient deficiencies in prolonged coffee cultivation due to robust sorption mechanisms. Depth-wise comparisons of trace element concentrations are summarized in

Table 3. Comparison of trace element concentrations between surface (0–30 cm) and subsurface (30–60 cm) soils.

Element	Surface Mean (mg/kg)	Subsurface Mean (mg/kg)	Difference (Surf–Sub)	Interpretation
Ba	2627.94	2291.04	+336.90	Surface-enriched (biological cycling)
Ce	74.95	82.59	−7.64	Slightly higher in subsurface (lithogenic)
Co	4.70	5.59	−0.89	Lithogenic, stable
Cr	14.57	16.95	−2.38	Lithogenic
Cu	18.58	19.58	−1.00	Lithogenic / micronutrient
Ga	22.24	23.70	−1.46	Lithogenic
Nb	16.97	17.26	−0.29	Lithogenic
Ni	11.07	14.63	−3.56	Lithogenic
Pb	31.97	37.91	−5.94	Lithogenic, immobile
Rb	262.14	255.67	+6.47	Surface-enriched (biocycling)
Sr	74.59	62.10	+12.49	Fertilizer-responsive
Th	29.80	30.33	−0.53	Lithogenic
U	4.18	4.12	+0.06	Slight fertilizer signal
V	24.77	29.87	−5.10	Lithogenic
W	7.29	7.60	−0.31	Lithogenic
Y	54.38	57.41	−3.03	Lithogenic
Zn	106.11	108.71	−2.60	Slight depth variation
Zr	384.71	380.52	+4.19	Accessory mineral, surface slightly higher
As	4.37	4.85	−0.48	Lithogenic

.

Depth variations in trace elements support the influence of fertilizer application on the upper soil horizon. Surface enrichment of Sr, U, Ba, and Rb is consistent with repeated inputs of P-containing fertilizers and nutrient cycling in the biologically active surface layer. Conversely, lithogenic elements (Cr, Ni, Co, V, Pb, Ga, Th, Y, Zn) exhibited slightly higher concentrations at 60 cm, reflecting their origin from parent material weathering and minimal vertical mobility. Overall, the depth distributions indicate that fertilizer-responsive elements accumulate near the surface, while most trace elements remain controlled by the granitic parent material.

These patterns have direct implications for soil fertility in highland coffee systems. High natural K-bearing mineral content provides an intrinsic reservoir of potassium, reducing dependence on external fertilizer inputs. At the same time, strong P fixation by Fe- and Al-oxides may constrain phosphorus availability despite moderate total P concentrations [70]. Furthermore, the predictable release of micronutrients from mafic minerals, such as Ni, Zn, and Cu, supports a stable micronutrient supply for coffee growth. Overall, the trace element distributions reflect a soil environment in which mineral inheritance outweighs pedogenic redistribution, offering valuable insights for guiding nutrient management and sustaining coffee production in granitic-derived highland ecosystems.

5. Conclusions

This study illustrates that the geochemical properties of the AIRID highland coffee soils are predominantly dictated by granitic parent material, with mineralogical inheritance having a more significant impact than vertical pedogenic redistribution. Major oxide and trace element distributions indicate extensive tropical weathering, marked by elevated levels of SiO₂, Al₂O₃, and K₂O, and a reduction in CaO and MgO. Consistent trace element relationships further validate lithogenic control, exhibiting restricted mobility throughout soil depths. The behavior of phosphorus suggests significant fixation by soils rich in Fe–Al oxides, which may limit phosphorus availability, while the presence of copious potassium-bearing minerals offers a considerable natural reserve of potassium that could diminish fertilizer needs. Collectively, our findings underscore the pivotal influence of parent material on nutrient availability and soil fertility in granitic highland coffee systems.