Search Results (1,919)

Analytical studies of archeological materials often face challenges, such as the merging of heterogeneous, multidimensional datasets from complementary analytical techniques, and incorporating site- and user-defined parameters. In this study, a data fusion methodology is applied that combines micro-X-ray fluorescence (micro-XRF) spectrometry and handheld Raman spectroscopy to investigate degradation layers and identify pollution sources on two monuments in an urban background: the Temple of Hephaestus and the Byzantine Church of Ag. Theodoroi, in Athens, Greece. A total of 12 samples were collected for laboratory measurements and 32 in situ measurements were conducted. Statistical and unsupervised machine learning tools, namely correlation analysis, Principal Component Analysis and k-means clustering, were applied to the merged datasets. Additionally, selected elements’ ratios were calculated to infer their sources. The black crusts were identified as heterogeneous mixtures of calcium sulfate dihydrate, calcite, and particulate pollutants, with their composition reflecting their preservation state. Vehicular emission indicators were dominant in both sites, while secondary domestic heating pollutant indicators were more prevalent at Ag. Theodoroi. Orientation had a minor role compared to pollutant sources in differentiating degradation patterns. The integrated comparison of the different outputs highlighted the interpretive potential of the approach, particularly in improving the readability of the multivariate structure and supporting the development of targeted conservation strategies for monuments in polluted urban contexts. Full article

Deep-to-ultra-deep marine carbonate reservoirs represent an important frontier for hydrocarbon exploration in the Tarim Basin, yet fluid sources and accumulation processes in the Ediacaran (Sinian) succession remain poorly constrained due to extreme burial depth and complex tectono-thermal evolution. Here, we investigate fracture–vug reservoirs of the Sinian Qigebulake Formation in Well LT3 (Tabei Uplift) using an integrated dataset including petrography and cathodoluminescence, fluid-inclusion microthermometry, fluorescence and Raman spectroscopy, in situ major/trace element analysis and C–O–Sr isotope geochemistry, and LA-ICP-MS carbonate U–Pb dating of authigenic minerals. The paragenetic sequence comprises early dolomite (Dol-I), later dolomite (Dol-II), co-precipitated calcite (Cal-I) and quartz (Qtz-I), and late solid bitumen (Bit). Dolomite veins show PAAS-normalized REE patterns and 87Sr/86Sr ratios (0.70918–0.70984; average 0.70942) comparable to the surrounding Sinian marine wall rocks, indicating precipitation from diagenetic fluids dominated by closed-system water–rock interaction. In contrast, Cal-I displays LREE enrichment, pronounced positive Eu anomalies (δEu = 4.91–7.21), radiogenic ⁸⁷Sr/⁸⁶Sr ratios (0.71161–0.71417; average 0.71256), and negative δ¹⁸O_VPDB values (down to −9.439‰), suggesting a large-scale influx of deep-seated, high-temperature, Sr-rich hydrothermal fluids likely linked to fault-assisted fluid circulation. Fluid inclusions record four hydrocarbon charging episodes, evolving from lower- to higher-maturity oils and ultimately to dry gas. Dol-II hosts pale-yellow to pale-blue oil inclusions, whereas Cal-I and Qtz-I predominantly contain deep-blue oil inclusions and methane-rich gas inclusions (Raman peak near 2917 cm⁻¹). Carbonate U–Pb ages constrain dolomite precipitation to the Middle Ordovician (~468–463 Ma) and hydrothermal-related carbonate filling to the Early Triassic (~247–244 Ma). Collectively, these results support a time-resolved evolution in which early diagenetic fluid circulation in a marine carbonate system was overprinted by a later hydrothermal pulse that modified pore structures and thermal conditions, followed by late-stage deep burial leading to cracking of retained liquids, widespread bitumen formation, and methane charging. This framework provides new information on the constraints for fluid–rock interaction and hydrocarbon evolution in deep marine carbonate successions. Full article

Controlled-release fertilizer (CRF) improves fertilizer-use efficiency through sustained nutrient release, but its rate-dependent effects on the growth and physiology of Paeonia delavayi seedlings remain unclear. In this study, germinated seeds of P. delavayi with radicles 3–4 cm in length were grown under container nursery conditions with four CRF application rates: (CK, 0 kg·m⁻³), treatment 1 (T1, 0.6 kg·m⁻³), treatment 2 (T2, 1.2 kg·m⁻³), and treatment 3 (T3, 2.4 kg·m⁻³). Morphological traits, root characteristics, biomass accumulation, physiological parameters, and chlorophyll fluorescence were evaluated, and Pearson correlation and fuzzy membership analyses were used to compare overall treatment performance within the tested range. CRF significantly promoted seedling height, leaf number, petiole length, and biomass accumulation, although the promoting effect did not increase continuously with fertilizer rate. By June, seedling height in T2 was 160% greater than that in CK, while aboveground biomass increased by 552% and 574% in T2 and T3, respectively. Root morphological traits were not significantly affected, suggesting that CRF primarily promoted aboveground development and biomass production. Medium and high CRF rates increased leaf superoxide dismutase (SOD) activity by 42% and 103%, respectively, and peroxidase (POD) activity by 163% and 250%, respectively. Aboveground starch content was 45% higher in T2 than in CK. In contrast, photosynthetic pigment contents and the chlorophyll a/b ratio were not significantly affected by CRF. Chlorophyll fluorescence analysis showed that Fv/Fm remained stable among CRF treatments (0.78–0.82) and was significantly higher than that in CK (0.65), whereas the actual quantum yield of PSII [Y(II)] did not differ significantly among treatments. Relative to CK, the quantum yield of non-photochemical quenching [Y(NPQ)] increased from 0.20 to 0.40 in T2, while the quantum yield of non-regulated energy dissipation in PSII [Y(NO)] decreased from 0.37 to 0.24–0.22 in T2–T3. Pearson correlation and fuzzy membership analyses ranked the treatments as T2 > T3 > T1 > CK, indicating that T2 performed most favorably within the tested range, although its advantage over T3 was small. Overall, an appropriate CRF rate promoted P. delavayi seedling growth and was associated with changes in biomass accumulation, antioxidant enzyme activity, carbon assimilate storage, and chlorophyll fluorescence parameters. Full article

This study designed an integration of anaerobic digestion, partial nitrification/Anammox (PN/A), and Fenton process to efficiently treat high-concentration organic liquor wastewater (HCLW). Results indicated that when the diluted ten-fold mixture of boiler bottom water and cellar bottom water with the ratio of 5:1 was used as influent, the average concentrations of COD, TN, NH₄⁺-N, NO₂⁻-N, and NO₃⁻-N in effluent of biological treatment for this process were 180.00, 12.64, 1.74, 0.13, and 2.45 mg/L, respectively. To meet the requirement for direct discharge of HCLW, Fenton oxidation with 600 mg H₂O₂/L and 300 mg Fe²⁺/L was used to further reduce the COD concentration. Three-dimensional fluorescence spectra analysis revealed that the process effectively altered the organic molecular structure and degraded some large molecular proteins. Microbial community analysis showed that Methanobacterium (20.98% → 31.52%) and Methanosaeta (9.70% → 19.34%) in AD, Azoarcus (no detected → 10.49%) and Nitrosomonas (1.68% → 6.16%) in PN, and Candidatus_Brocadia (18.80% → 20.31%) and Ignavibacterium (no detected → 5.11%) in Anammox were dominant in this system. This study provided a pioneering industrial solution for the efficient and stable treatment of HCLW. Full article

Hulless barley (Hordeum vulgare L. var. nudum) on the Qinghai–Tibet Plateau is consistently exposed to intense solar irradiance, yet whether and how reproductive spikes and flag leaves partition photoprotection remains unclear. Here, we compared a pigmented black landrace (Cai Peng Zi, CPZ) with a white cultivar (Zang Qing 3000, ZQ3000) across early, middle, and late spike coloration stages under field conditions. By integrating measurements of anthocyanin and chlorophyll contents, chlorophyll fluorescence parameters, and rapid light-response curves, we dissected organ-specific strategies in photochemistry and energy dissipation in spikes and flag leaves. The results showed that anthocyanin accumulation in CPZ spikes increased significantly during spike coloration, while chlorophyll a and the chlorophyll a/b ratio declined, indicating a shift from light harvesting to photoprotection in reproductive tissues. This pigment transition coincided with reduced PSII performance (declines in QY_max, qP, and qL) but stable non-photochemical quenching (NPQ and qN), pointing to reduced photochemical capacity with relatively stable energy dissipation in the spike. In contrast, CPZ leaves maintained higher QY_max than ZQ3000 but exhibited a pronounced decline in NPQ and qN at late stages, reflecting CPZ’s attenuated regulated energy dissipation capacity. Rapid light-response analysis further supported differences between organs and cultivars. Under high PAR, ZQ3000 spikes exhibited steeper declines in Y(II) and stronger downregulation of ETR(II), whereas CPZ spikes showed more moderate decreases; in leaves, ZQ3000 maintained consistently lower Y(NO) and higher Y(NPQ), indicating greater reliance on regulated energy dissipation. Collectively, our results reveal how pigment-mediated screening in reproductive structures and dynamic regulation of energy dissipation in leaves are coordinated to optimize light-use efficiency in high-altitude environments, providing physiological insights for breeding resilient hulless barley varieties. Full article

Whey proteins readily form complexes with polyphenols, the structure and functionality of which are influenced by factors such as polyphenol concentration and heat treatment. However, previous studies have largely examined these factors independently, and limited information is available regarding how the sequence of heat application (pre- vs. post-complexation) interacts with varying polyphenol concentrations to modulate the structure–function relationship of whey protein-polyphenol systems. This study investigated the effects of different heating conditions and gallic acid (GA) concentration on structural and functional properties of whey protein isolate–gallic acid (WPI-GA) complexes at pH 7.0. The treatments included native whey protein isolate (WPI), preheated WPI, native WPI-GA complexes, and WPI-GA complexes at two ratios (1:0.5 and 1:1 w/w) and heated either before or after complexation. GA addition and heat treatment increased turbidity and particle size, indicating enhanced complexation. The zeta potential showed minimal change, suggesting limited involvement of electrostatic interactions. Fluorescence quenching increased with GA concentration, confirming interactions between GA and WPI. Heat treatments increased fluorescence intensity and surface hydrophobicity, likely due to protein unfolding and exposure of hydrophobic regions. Higher GA concentration enhanced antioxidant activity, reduced foaming capacity, and did not affect emulsifying properties. Preheating also decreased the foaming capacity of the complexes, whereas post-heating restored it. Both heat treatments reduced the emulsifying activity index (EAI) but increased the emulsion stability index (ESI) compared with native WPI. Overall, this study provides insight into how GA concentration and heating sequence influence the complexation and functionality of WPI, contributing to a better understanding of protein–polyphenol interactions in bioactive-enriched dairy systems. Full article

This study presents a novel, rapidly synthesized geopolymer foam fabricated from granite industrial waste using microwave sintering, reducing the demolding time from 7 days to 3 min and the overall processing time to 24 h, while enhancing mechanical performance. Five sample compositions (G1–G5) were prepared with varying granite powder and alkaline solution ratios, cured in a microwave for 3 min, and sintered for an additional 3 min. X-ray fluorescence (XRF), compressive strength tests, water absorption, thermogravimetric analysis (TGA), differential thermal analysis (DTA), and Fourier transform infrared spectroscopy (FTIR) were used for thorough characterization. The compressive strength increased progressively from 13 MPa (G1) to 20 MPa (G5), the total porosity decreased from 33.33% to 18.58%, the water absorption reached a minimum of 2.02% (G5), and the bulk density rose from 1.143 to 1.49 g/cm³. XRF analysis confirmed Si/Al molar ratios of 6.5–11.4, indicating enhanced aluminosilicate network development. FTIR confirmed progressive geopolymerization, with integrated Si-O-T band areas increasing from 41,900 a.u. (G1) to 44,680 a.u. (G5). The microwave sintering approach consumed over 90% less active energy than conventional thermal curing, significantly reducing associated CO₂ emissions and thereby supporting SDG 7, SDG 12, and SDG 13. These results position granite-waste-derived geopolymer foam as a high-performance, energy-efficient alternative to conventional fired bricks and cement-based construction materials. Full article

Substituting hydrocarbon fuels such as methane (CH₄) with ammonia (NH₃) reduces CO₂ emissions in gas turbines, but ammonia’s low reactivity challenges flame stability. Dual-swirl staged combustors using a low thermal power (P_pilot) pilot flame can stabilise the main flame. This work compares the morphologies and stabilities of NH₃/air premixed swirl flames using ammonia and methane pilot flames (APF and MPF). Flame imaging and simultaneous OH-NH planar laser-induced fluorescence (PLIF) are employed to analyse flame morphology. Main flame stability is assessed by measuring the lean blow-off equivalence ratio (ϕ_b,main). The results show that MPF significantly outperforms APF in main flame stabilisation. At P_pilot = 1.2–1.8 kW (14.2–21.3% of P_main), the dual-swirl flames exhibit a stratified structure, with OH concentrated in the pilot stage. Flames with MPF exhibit considerably lower ϕ_b,main than those with APF. For example, at P_pilot = 1.6 kW, ϕ_b,main is reduced to 0.42 with MPF, compared to 0.56 with APF, demonstrating MPF’s superior stabilisation capability. MPF can reduce CO₂ emissions by 82.4–87.6% compared to a CH₄ flame of equivalent thermal power. Two stabilisation modes are identified, namely primary recirculation zone-dominated and pilot-dominated modes. These findings demonstrate that a low-power MPF provides an effective strategy for enhancing ammonia flame stability and reducing CO₂ emissions in gas turbines. Full article

Achieving stable partial nitritation (PN) in mainstream municipal wastewater treatment is critical for energy-efficient anammox-based nitrogen removal. However, selectively suppressing nitrite-oxidizing bacteria (NOB) while retaining ammonia-oxidizing bacteria (AOB) remains challenging. This study investigated the performance and microbial mechanisms of PN in a membrane-aerated biofilm reactor (MABR) under zero-pressure aeration. The results showed that zero-pressure aeration achieved a nitrite accumulation ratio (NAR) of 82.14%, significantly higher than that under constant aeration (13.2%) and intermittent aeration (53.5%). Zero-pressure aeration led to a significant increase in the fluorescence intensities of tyrosine/tryptophan protein in extracellular polymeric substances. 16S rRNA sequencing revealed that zero-pressure aeration achieved a modest reduction in the relative abundance of NOB Nitrospira from 3.39% to 2.74% while increasing the relative abundance of AOB Nitrosomonas from 0.04% to 1.09%. Enzyme activity assays further showed that zero-pressure aeration significantly decreased nitrite oxidoreductase (NXR) activity while maintaining ammonia monooxygenase (AMO) and hydroxylamine oxidoreductase (HAO) activities, providing direct functional evidence for NOB suppression. Zero-pressure operation required no external air supply, representing a passive aeration strategy for PN. These results suggest that zero-pressure aeration may reshape the competition between AOB and NOB by enriching AOB and suppressing NOB, providing a new energy-efficient pathway for mainstream nitrogen removal. Full article

The Liwu copper deposit, located on the western margin of the Yangtze Block, is a typical metamorphic-hosted polymetallic Cu deposit with significant deep exploration potential. To constrain its mineralization-forming processes and primary halo characteristics, this study focuses on the Heiniudong ore segment. Based on portable X-ray fluorescence (XRF) data obtained from drill cores and underground samples, a comprehensive geochemical analysis of 20 elements was conducted. Elemental background values and anomaly thresholds were determined using the iterative sigma (σ) elimination method. Pearson correlation analysis and hierarchical cluster analysis were applied to identify element associations, while the Grigorian zonation index method was employed to investigate axial zoning patterns of primary halos. The results demonstrate that Cu exhibits strong positive correlations with S, Fe, Ag, Cd, Sn, and Bi, indicating a medium- to high-temperature hydrothermal sulfide mineralization system. The primary halo displays well-defined vertical zonation, with Ba–Sr–Sb–As representing the front halo, Zn–Pb–Cu–Ag–Sn–Fe–Cd the near-ore halo, and Bi–Mo–W–Th the tail halo. A clear axial zonation sequence is established. The vertical variation in the geochemical ratio (As × Sr × Sb)/(Mo × Bi × W) exhibits a characteristic “low–high–low–high” pattern, reflecting the superposition of the front halo of a deeper concealed orebody with the tail halo of the upper known orebody under multistage hydrothermal remobilization and structural overprinting. Integrated with the coexistence of front halo and tail halo anomalies and strong alteration in drill hole WT03, the results indicate that the southwestern extension of WT03 along southwest-dipping ductile–brittle detachment structures represents the most promising deep exploration target. Full article

In cold and arid regions, the durability of asphalt pavement materials is often inadequate, and the hot mixing process further accelerates pavement ageing and releases harmful gases. To address the high-viscosity of pavement materials in such regions, lower mixing temperatures, extend the construction duration, and enhance pavement durability, this study systematically investigates a warm-mix technology for rubber-composite-modified asphalt. First, the influence of processing conditions on the viscosity-reducing effect was examined, and the optimal warm-mix preparation process was determined. Second, the properties of warm-mix rubber-modified asphalt were optimised through high- and low-temperature rheological testing. Finally, the mechanism of warm-mix modification was elucidated using microscopic techniques such as scanning electron microscopy, fluorescence microscopy and infrared spectroscopy. The results show that the 40-mesh pelletised desulphurised rubber treated with activator at a 5:1 ratio of activator at 220 °C for 50 h exhibits the optimal viscosity reduction effect. As the proportion of cracked rubber increases, the viscosity-reducing effect first intensifies and then diminishes optimal results are achieved at a dosage of 5%; the optimal comprehensive performance is achieved at a 5% proportion, where the asphalt simultaneously exhibits excellent high-temperature stability and low-temperature crack resistance. The cracking process effectively disrupts the cross-linked network structure of rubber, significantly reducing viscosity while enhancing the compatibility and stability of the asphalt system. Notably, the proposed warm-mix process reduces the production temperature of rubber-modified asphalt by 40–60 °C and lowers its viscosity by approximately 30% compared to conventional asphalt. This improvement provides crucial support for low-temperature construction and viscosity control of rubber-modified asphalt in cold and arid regions. Full article

Background: Endogenous estradiol/progesterone (E2/P4) regulates neuronal mitochondrial bioenergetics and redox balance. However, the effects of combined oral contraceptive (COC) steroids under physiologically relevant hormonal conditions remain poorly understood. Therefore, this study aims to investigate how COC steroids modulate mitochondrial function within the defined E2/P4 hormonal milieus. Methods: Human SH-SY5Y cells (Cytion) were starved for 48 h in Cytion medium without FBS and with 1% ITS, and then exposed for 48 h to six conditions: vehicle (F0); follicular-like E2/P4 (F1); luteal-like E2/P4 (F2); F1 + dienogest/ethinylestradiol (DNG/EE; F3); F2 + DNG/EE (F4); and DNG/EE alone (F5). The primary endpoints were mitochondrial membrane potential (JC-1 red/green ratio) and ROS (H₂DCFDA/DCF); nitric oxide (DAF-FM) was also recorded. Hoechst 33342 nuclear fluorescence served both as a per-well proxy of cell number and as a proportionality factor for normalization. Results: Follicular- and luteal-like backgrounds were associated with distinct ΔΨm/ROS set-points. The addition of DNG/EE was accompanied by background-dependent shifts, generally characterized by higher DCF signals and lower JC-1 ratios relative to the vehicle, whereas DAF-FM did not reveal statistically robust changes in NO. Hoechst-based normalization preserved these patterns, suggesting that the observed effects likely reflect per-cell functional modulation rather than differences in cell number, although modest, background-dependent variations in proliferation were observed, with DNG/EE associated with a greater increase in ROS under follicular-like conditions and a more pronounced ΔΨm membrane potential in a luteal-like milieu. Conclusions: These findings suggest that neuroendocrine background may influence mitochondrial ΔΨm/ROS states in SH-SY5Y cells, with physiologically inspired E2/P4 milieus potentially shaping baseline conditions onto which COC components exert context-dependent effects at 48 h. These preliminary findings provide a standardized framework for subsequent image-based analyses of mitochondrial function. Full article

During fermentation in stirred-tank bioreactors (STBR), filamentous fungi are frequently exposed to hypoxic conditions. However, their responses, especially short-term ones (≤6 h), remain unclear. In this study, we performed a short-term multi-omics profiling in an Aspergillus oryzae hyphal dispersion mutant (AGΔ-GAGΔ) during a controlled transition to hypoxia (a decrease in dissolved oxygen (DO) from 10% to ≤1%) in a 4 L STBR. In transcriptome analysis, the genes encoding mitochondrial respiratory chain Complexes I–III were transiently downregulated at 1 h from DO depletion and were then upregulated, whereas those of Complex IV were upregulated immediately at the onset of hypoxia. In relation to this respiratory remodeling, we also observed an immediate induction of an alternative oxidase (AOX) gene. However, our metabolome data showed no significant change in the ATP level. This result could be explained by the upregulation of the glycolytic genes in hypoxic cultures. Fluorescence imaging revealed a transient increase in intracellular reactive oxygen species (ROS) in hypoxia, and metabolomics data revealed a decrease in the reduced glutathione/oxidized glutathione ratio in hypoxic cultures. Deletion of the AOX gene prolonged the ROS increase. Together, these data indicate that early hypoxia triggers a transient increase in oxidative stress, mitigated by antioxidant systems and mitochondrial respiratory rebalancing including an AOX-mediated bypass. Full article

Differential enrichment of shale oil hydrocarbon fractions exerts a fundamental control on the spatial distribution of “sweet spots” and the efficiency of unconventional resource recovery. This study investigates the continental shales of the Upper Es4 Member in the Dongying Sag, Bohai Bay Basin, through an integrated analytical framework combining Laser Scanning Confocal Microscopy (LSCM), Scanning Electron Microscopy (SEM), and high-pressure mercury intrusion. By moving beyond qualitative observations, we characterize the micro-scale partitioning of light and heavy fractions and establish a deterministic hierarchy of controlling factors. Our results indicate the following. (1) Mineral composition functions as a “primary geochemical filter,” where carbonate minerals exhibit a preferential adsorption affinity for light fractions (≤ C₁₈), while clay minerals facilitate the selective retention of heavy components (> C₁₈). (2) Pore–throat architecture acts as a “secondary mobility modulator.” A statistically significant linear correlation (R² = 0.72, p < 0.05) was identified between mean pore diameter and the light-to-heavy fluorescence ratio, suggesting that interconnected macropores in carbonate laminae provide low-resistance conduits for light oil accumulation, whereas isolated mesopores in argillaceous matrices promote heavy-component sequestration. (3) Thermal maturity (Ro) drives a progressive shift in the light-to-heavy ratio, enhancing oil fluidity and regulating the transition from adsorption-dominated to migration-dominated enrichment. This study clarifies the lithofacies-dependent coupling mechanisms between mineral diagenesis and pore-scale fractionation, providing a semi-quantitative conceptual model for shale oil sweet-spot prediction in complex lacustrine basins. Full article

This work presents the results of an archaeometric research study of the geomaterials used in the construction of the Late Antique wall of Emerita Augusta (currently Mérida, Spain). Dated to the 5th century C.E., this structure belongs to one of the best-preserved historical ensembles in Europe. In-depth knowledge of the geomaterials used in this ancient wall is essential for ensuring reliable restoration strategies and the successful long-term conservation of this monument. To this end, a rigorous sampling procedure was conducted in areas containing original archaeological remains. Samples were characterized using optical microscopy, X-ray diffraction (XRD), X-ray fluorescence (XRF), inductively coupled plasma–mass spectrometry (ICP-MS), thermogravimetry and differential thermal analyses (TGA-DTA), and scanning electron microscopy (SEM). This integrated multi-analytical approach is highly effective for the study of built heritage. The mineralogical, textural, and geochemical properties of the granites allowed for the identification of the granite types used in the wall, while the results obtained for the mortars indicated that lime, fully carbonated and transformed into calcite, was used as the binding agent. Furthermore, the binder/aggregate ratios were found to be consistent with traditional Roman mortar formulations. These findings provide a comprehensive understanding of the material provenance and construction techniques used in this landmark of late antiquity. Full article