Mineral Composition Research Articles

Efficacy of the Probiotic L. brevis in Counteracting the Demineralizing Process of the Tooth Enamel Surface: Results from an In Vitro Study

Background. Enamel plays an essential role in protecting the underlying layers of the human tooth; therefore, preserving it is vital. This experimental study aimed to evaluate the potential ability of L. brevis to counteract the action of a demineralizing agent on dental enamel morphology and mineral composition in vitro. Methods. The sample consisted of 12 healthy human posterior teeth. The coronal portion of each tooth was subdivided into two equal parts longitudinally. The specimens were randomly divided into four groups: artificial saliva, L. brevis suspension, demineralizing agent (DA), and DA plus L. brevis . Scanning electron microscopy (SEM) and energy-dispersive X-ray spectroscopy (EDS) were used to evaluate the surface micromorphology and the mineral content, respectively. The statistical analysis was conducted using a one-way ANOVA, followed by Tukey’s post hoc test. Results. SEM analysis did not highlight significant changes in the enamel microstructure of L. brevis -treated specimens compared to the control. DA-induced damage to the enamel structure was drastically reduced when the specimens were contextually exposed to the probiotic. The treatment with DA substantially reduced the weight % of crucial enamel minerals, i.e., Ca and P. Notably, the probiotic was able to reverse the demineralization process, bringing Ca and P weight % back to basal levels, including the Ca/P ratio. Conclusions. The findings indicate that L. brevis is able to efficiently protect the dental enamel surface from the damage caused by DA and increase the enamel resistance to demineralization. Overall, L. brevis confirms its efficacy in preventing or counteracting the action of carious lesions through a novel mechanism that protects the tooth surface under a chemical challenge that mimics the caries process.

Regional features of camel milk composition and properties in the Republic of Kazakhstan

Camel milk, renowned for its distinctive nutritional qualities, has captured the interest of scientific researchers due to its potential health benefits. This study aims to compare the biochemical composition of camel milk sourced from two distinct regions of Kazakhstan: Jetisu and Mangystou. Analytical methods were employed to achieve this objective, including gas chromatography for fatty acid analysis, chemical methods for physicochemical parameter determination, and assessment of amino acid, fatty acid, mineral, and vitamin content. In samples from the Jetisu region, protein content ranged from 3.61% to 3.70%, fat from 3.85% to 4.64%, and lactose from 4.80% to 4.85%. In comparison, samples from the Mangystou region exhibited protein content ranging from 3.65% to 3.81%, fat from 4.72% to 5.75%, and lactose from 4.21% to 4.28%. Regarding amino acid composition, Mangystou region samples contained more essential amino acids per 100 g of protein than Jetisu region samples: 41.29 g versus 38.20 g, respectively. Additionally, the Jetisu region sample contained 64.291% saturated fatty acids, while the Mangystou region sample had 62.135%, indicating differences in fatty acid composition based on geographical origin. In terms of mineral composition, camel milk from the Mangystou region exhibited higher calcium and zinc content compared to Jetisu region samples, with calcium and zinc content measured at 124.50 mg/100 g and 490.15 μg/100 g, respectively, for Mangystou samples, and 112.50 mg/100 g and 321.24 μg/100 g, respectively, for Jetisu samples. Overall, the study underscores regional variances in camel milk's biochemical composition, which can impact its nutritional and biological value. These findings provide dairy product producers in Kazakhstan with enhanced opportunities to create healthy, high-quality dairy products.

Effect of Culinary Treatments on Nutritional and Anti- nutritional Profils of Sesame Oilcake for Use in Fighting Protein Malnutrition

To tackle protein malnutrition, the valorization of sesame cake has been initiated. A by-product of sesame oil extraction, it is commonly used as livestock feed. However, it could be used to enrich staple foods and improve their nutritional value, particularly in rural areas where access to quality protein sources is limited. In order to highlight its nutritional richness, certain soaking, roasting and hulling treatments were used to assess their impact on nutritional quality. Then extraction of the oil from the seeds using a mechanical press to obtain sesame cake was proceeded. Standard methods were used for physicochemical characterization of nutritional, mineral and anti-nutritional compounds. The results showed that the sesame oilcake obtained from the various treatments contained significant levels of total protein (26.55- 36.72g/100g DM), residual lipids (24.19- 32.37g/100g DM), carbohydrates (10.86- 18.74g/100g DM), ash (4.32 - 6.19 g/100g DM) and fiber (10.71-20.76 g/100g DM). Similarly, evaluation of the mineral composition of these meal concentrates showed their richness in phosphorus (20.47 - 176.66 mg/100g DM), calcium (15.75 - 467.42 mg/100g DM), magnesium (13.45 - 340.33 mg/100g DM), iron (4.90-14.70 mg/100g DM), and zinc (0.71-4.39 mg/100g DM). However, these sesame cake concentrates also contained anti-nutritional factors such as oxalates (0.48 - 1.04 mg/100g DM), phytates (0.08 - 0.12 mg/100g DM), saponins (0.084 - 1.10 mg/100g DM) and tannins (0.33 - 1.36 mg/100g DM). Fortunately, these were considerably reduced by pretreatment. Indeed, a 40.07, 83.33, 64.64 and 60.95% reduction in tannins, phytates, oxalates and saponins respectively were observed. The considerable reduction in anti-nutrients in the various cakes is an advantage for the digestibility and nutrient availability of this feed. Its high protein and mineral content could therefore be considered for use in protein malnutrition.

Production of Biscuits from Wheat, Almond and Pawpaw Flour Blends and Investigating It’s Physicochemical and Texture Characteristics

Biscuit, also known as a cookie is a nutritive snack produced from dough that is transformed into an appetizing product through the application of heat in an oven. This study was aimed at evaluating the quality of biscuit produced from wheat, African almond and pawpaw flour blends. From the flours, blends were made and six (6) samples, A to F formulated. Sample A (100 % wheat flour) was used as the control, B (60 % Wheat flour: 0 % Almond Flour: 40 % Pawpaw Flour), C (60 % Wheat flour: 10 % Almond Flour: 30 % Pawpaw Flour), D (60 % Wheat flour: 20 % Almond Flour: 20 % Pawpaw Flour), E (60 % Wheat flour: 30 % Almond Flour: 10 % Pawpaw Flour), F (60 % Wheat flour: 40 % Almond Flour: 0 % Pawpaw Flour). The physical, proximate, anti-nutrients, vitamins, minerals, antioxidants and sensory properties of the biscuits were evaluated using standard methods. For physical parameters of the biscuit, the weight ranged from 8.86 g-10.60 g, diameter from 6.60 mm- 6.80 mm, the spread ratio from 0.58-0.61, breaking strength from 0.25 kg- 0.29 kg and thickness ranged from 11.08 mm- 11.43 mm. The anti-nutrients content of the biscuits were considerably low and within safe limits. The results showed an increase in ash, fibre, fats and protein content while the carbohydrate content of the biscuit reduced upon substitution of wheat flour with almond and pawpaw flours. The vitamin content of the biscuit was also improved especially the vitamin A content upon addition of pawpaw flour. The result for mineral composition showed a significant increase from 46.00-89.35mg/100g for sodium, potassium from 323.44-486.95 mg/100g, calcium from 189.46-356.88mg/100g, magnesium from 44.34-132.88 mg/100g and phosphorus from 155.33-428.45mg/100g.6. Antioxidant activity also increased from 2.12-3.69mgAAE/g. The biscuit samples were all rated high in terms of their sensory attributes especially samples with high proportion of almond flour. This research indicates that almond and pawpaw flours are suitable for biscuit production especially at 40% and 10% substitution for almond and pawpaw flours respectively.

Multivariate statistical analysis of bioavailability of heavy metals and mineral characterization in selected species of coastal flora

This study presents a thorough investigation into the concentration of heavy metals and mineral composition within four distinct coastal flora species: Cyperus conglomeratus, Halopyrum mucronatum, Sericostem pauciflorum, and Salvadora persica. Employing rigorous statistical methodologies such as Pearson coefficient correlation, principal component analysis (PCA), analysis of variance (ANOVA), and interclass correlation (ICC), we aimed to elucidate the bioavailability of heavy metals, minerals, and relevant physical characteristics. The analysis focused on essential elements including copper (Cu), iron (Fe), manganese (Mn), zinc (Zn), magnesium (Mg2+), calcium (Ca2+), sodium (Na+), potassium (K+), and chloride (Cl–), all of which are known to play pivotal roles in the ecological dynamics of coastal ecosystems. Through PCA, we discerned distinctive patterns within PC1 to PC4, collectively explaining an impressive 99.65% of the variance observed in heavy metal composition across the studied flora species. These results underscore the profound influence of environmental factors on the mineral composition of coastal flora, offering critical insights into the ecological processes shaping these vital ecosystems. Furthermore, significant correlations among mineral contents in H. mucronatum; K+ with content of Na+ (r = 0.989) and Mg2+ (r = 0.984); as revealed by ICC analyses, contributed to a nuanced understanding of variations in electrical conductivity (EC), pH levels, and ash content among the diverse coastal flora species. By shedding light on heavy metal and mineral dynamics in coastal flora, this study not only advances our scientific understanding but also provides a foundation for the development of targeted environmental monitoring and management strategies aimed at promoting the ecological sustainability and resilience of coastal ecosystems in the face of ongoing environmental challenges.

Multi-scale, open-system magmatic and sub-solidus processes contribute to the chemical and isotopic characteristics of the Jurassic Guadalupe Igneous Complex, Sierra Nevada, California, USA

The chemical and isotopic characteristics of a solidified pluton represent the integration of magmatic and sub-solidus processes operating across a range of spatial and temporal scales during pluton construction, crystallization, and cooling. Disentangling these processes and understanding where chemical and isotopic signatures were acquired requires the combination of multiple tools tracing processes at different time and length scales. We combine whole-rock oxygen and Sr-Nd isotopes, zircon oxygen isotopes and trace elements, and mineral compositions with published high-precision U-Pb zircon geochronology to evaluate differentiation within the bimodal Guadalupe Igneous Complex, Sierra Nevada, California (USA). The complex was constructed in ~300 k.y. between 149 and 150 Ma. Felsic magmas crystallized as centimeter- to meter-sized segregations in gabbros in the lower part of the complex and as granites and granophyres structurally above the gabbros. A central mingling zone separates the mafic and felsic units. Pluton-wide δ18O(whole-rock), δ18O(zircon), and Sr-Nd isotopic ranges are too large to be explained by in situ, closed-system differentiation, instead requiring open-system behavior at all scales. Low δ18O(whole-rock) and δ18O(zircon) values indicate assimilation of hydrothermally altered marine host rocks during ascent and/or emplacement. In situ differentiation processes operated on a smaller scale (meters to tens of meters) for at least ~200 k.y. via (1) percolation and segregation of chemically and isotopically diverse silicic interstitial melt from a heterogeneous gabbro mush; (2) crystal accumulation; and (3) sub-solidus, high-temperature, hydrothermal alteration at the shallow roof of the complex to modify the chemical and isotopic characteristics. Whole-rock and mineral chemistry in combination with geochronology allows deciphering open-system differentiation processes at the outcrop to pluton scale from magmatic to sub-solidus temperatures over time scales of hundreds of thousands to millions of years.

Numerical simulation of concrete strength based on microstructure and mineral composition analysis using micro-CT and XRD technology

The investigation of mechanical properties in porous materials, such as concrete, has been a significant area of interest in the fields of civil engineering and architecture. Traditional macroscopic mechanical testing methods are limited due to destructive experimental conditions, time-consuming procedures, and the inability to characterize internal structures. To overcome these limitations, researchers have utilized microscopic factors with micro-CT and simulation models. Different simulation methods demand mechanical parameters to effectively model the constituent materials; however, there exists variability in the amount and standard values of these input parameters, which leads to a decrease in the reliability of the obtained results. In order to tackle this issue, a novel approach is proposed, which integrates mineral component analysis using X-ray diffraction (XRD) and establishes coefficients to minimize the number of necessary input parameters. Simulation results demonstrate excellent agreement with experimental measurements, accurately reproducing the stages of elastic deformation, failure, and fracture in the stress-strain curve of concrete. Our findings reveal that changes in the concrete skeletal structure, microstructure, and mineral composition significantly influence compressive strength. Coarse aggregates and high-mechanical-performance minerals, in particular, have a substantial impact. Additionally, the mechanical properties show a significant linear relationship with the strength reduction coefficient of aggregates and concrete cores. In conclusion, the proposed method, combining CT scanning and XRD with FDEM, proves to be a reliable and practical approach for accurately assessing the mechanical properties of concrete. This methodology simplifies the intricate processes associated with the time-intensive parameter calibration, leading to a more efficient parameter allocation procedure. As a result, this method enhances concrete design, promotes a better understanding of parameter impacts, and enables accurate prediction of concrete behavior across diverse scenarios.

Systematic characterisation, mineral analysis, and valorisation of lignocellulosic waste into sustainable indigenous Ganoderma lucidum production from Pakistan

ABSTRACT Ganoderma lucidum is a remarkable medicinal macro fungus widely known for its extraordinary healing qualities. Indigenous G. lucidum collected from Punjab, Pakistan, was morpho-⁠anatomically and phylogenetically characterised. After characterisation, it was evaluated for vegetative and reproductive growth potential and subjected to mineral analysis of both wild and cultivated basidiomata of G. lucidum. Among various tested nutrient agar media, maximum G. lucidum mycelial density and growth rate were noted on CEA medium at 32°C. For spawn production, barley grains were found to be the most appropriate medium. The suitability of various types of lignocellulosic substrates was checked for better yield in minimum period of time. The combination of sawdust + wheat straw proved to be the most efficient substrate for the best yield with the maximum number of flushes. Small differences were observed in essential and trace mineral quantities (except nickel) in both wild and cultivated basidiomata, revealing the negligible effect of artificial substrates on the mineral composition of G. lucidum. These findings conclude that indigenous G. lucidum is capable of indoor cultivation on several locally available media and substrates. Cultivating this tremendous medicinal mushroom on a large scale in Pakistan could prove crucial from a pharmaceutical perspective. Providing cultures and fruiting bodies of G. lucidum to the food and therapeutic industries would eliminate their dependence on the availability of G. lucidum for a specific period of the year.

ALTERNATIVE NON-TRADITIONAL SOURCES OF FEED PROTEIN AND AMINO ACIDS

The article presents a literature review on the risks of the global problem of fodder protein and protein amino acids in the feeding of agricultural animals and poultry. Alternative ways of solving it are due to the production and use of non-traditional feed raw materials in feed diets. A number of scientists consider atypical agricultural biotechnological products obtained from insects to be one of the alternative sources of fodder protein and amino acids and see prospects in the development of their production. The most common subjects for study in this regard are crickets, locusts, silkworm larvae, flies, worms, etc. Their protein value, amino acid, fatty acid and mineral composition, the content of vitamins, and other biologically active substances are studied. The development of this direction is considered one of the ways to solve a number of urgent environmental and fodder problems on a biological basis. Рurpose of the research was to study the protein value and complete amino acid composition of flour from insects, namely flour from the larvae of the BSF fly, crickets and snails, and the methods of its determining: crude protein by the Kjeldahl method, digestible protein with the help of 0,2% pepsin, and the digestibility coefficient, and the principles of conducting researches, as well as the characteristics of methods for determining the content of replaceable and essential amino acids, including sulfur-containing, using the Kapel-105M capillary electrophoresis system. As a result of the research, it was found that cricket flour is the least valuable in terms of protein value (digestible protein and digestibility coefficient), and it is also poor in the content of nonessential and essential amino acids, compared to other studied types of insect flour. The best indicators of protein value were noted in the flour from BSF fly larvae in terms of the content of crude and digestible proteins, as well as the digestibility coefficient, which is 75.6%, which indicates its good digestibility by the bodies of animals and birds. The highest content of amino acids is contained in the flour from BSF fly larvae. Taking into account the above results of crude protein content, digestibility, and digestibility in this sample, amino acid digestibility will also be higher compared to other flour samples. In addition, flour from BSF fly larvae is rich in sulfur-containing amino acids. The content of tryptophan and histidine, compared to other types of raw materials, is the highest. The studied samples of insect flour contain a complete set of essential and nonessential amino acids, but BSF fly larvae flour and snail flour are more valuable for essential amino acids.

Productivity, morphology and mineral composition of forage palm clones biostimulated with humic substances

Productivity, morphology and mineral composition of forage palm clones biostimulated with humic substances

Deep bed filtration and formation damage by particles with distributed properties

Current models for deep bed filtration describe particles with uniform properties. Yet, the sizes, densities, and mineral composition of particles vary significantly in the same injection well. The aim of this work is to provide an effective mathematical model for water injection of particles with distributed properties and formation damage prediction. We average the set of traditional population balance equations for single-property particles and obtain one upscaled equation. The upscaled equation for particle retention rate contains a non-linear function of suspended concentration, which we call the 'suspension function'. We derive analytical solutions for the upscaled equation for linear (coreflood) and radial (well injectivity) flows. Then we treat lab coreflood data to determine the model suspension function and provide a model for well injectivity prediction. The retention profile for the flow of uniform particles has an exponential form. Frequently reported in the literature, hyper-exponential forms have been hypothetically explained by multiple particle properties. The inverse solution allows revealing the individual filtration coefficients for binary mixtures from total breakthrough concentrations during coreflood. Treatment of the data from lab experiments reveals individual filtration coefficients that belong to common intervals. For the first time, deep bed filtration of particles with distributed properties is upscaled and presented using a single equation that reflects the particle property distribution. This equation provides an effective mathematical model for tuning lab coreflood data, determines the model function, and uses it for injectivity decline prediction.

Polyvinyl alcohol (PVA) films: insights from crosslinking and plasticizer incorporation

Abstract The properties of polyvinyl alcohol (PVA) films are intricately influenced by factors such as polymer structure, fabrication method, the addition of plasticizers, and the molecular weight of monomers. In this research, we explore the implication of PVA films using a solution casting method to crosslink the polymer with boric acid (H3BO4), glycerol, and citric acid. This approach is compared with pure PVA films, establishing a valuable benchmark. High-concentration PVA membranes, incorporating glycerol as a plasticizer at specific concentrations, were also fabricated to broaden the experimental scope. Tensile strength tests, physicochemical property measurements, scanning electron microscopy (SEM), and X-ray diffraction (XRD) analyses were conducted to gain insights into the microstructure, surface characteristics, and mineral composition of the films. This comprehensive approach aims to enhance our understanding of the intricate relationship between PVA, plasticizers, and crosslinking agents, providing valuable insights for applications across diverse industries, including packaging, construction, and biomedical fields. The overarching objective of this research is to revolutionize the construction industry by developing polymer films that serve as the foundation for self-healing materials, fostering durability and innovation.

The effect of structural preservation conditions on pore structure of marine shale reservoir: a case study of the Wufeng-Longmaxi Formation shale, Southern Sichuan Basin, China

The marine shale within the Sichuan Basin constitutes China’s significant shale gas production, featuring old formation age, high degree of thermal evolution, multiple tectonic movements, and complex structural conditions. However, there are significant differences in the shale gas preservation conditions and reservoir quality in different areas, limiting future large-scale exploration and development. Pore structure significantly influences shale reservoir quality, gas content, and exploration of shale gas occurrence, migration, and enrichment mechanisms. The influence of structural-dominated preservation conditions on shale pore structures is essential to comprehend for effective shale gas exploitation. This study employs field-emission scanning electron microscopy in conjunction with other techniques (low-temperature N2 adsorption, low-temperature CO2 adsorption, and nuclear magnetic resonance) for detailed analyses of the pore structure across varied structural zones, revealing the influence of structural attributes, fault systems, depth of burial, and formation pressure on pore architecture, and examining the relationship between pore structure and shale gas preservation conditions. The results show that stable structural condition is conducive to the development and preservation of shale pores. Structural compression causes inorganic and organic pores to become narrow and elongated due to shrinkage, with a significant increase in microfractures. The porosity of shale with stable structural conditions exhibits markedly increased porosity compared to samples under structural compressions. Under conditions of similar TOC and mineral composition, the pore size distribution (PSD), pore volume (PV), and specific surface area (SSA) of shale after structural compression are significantly lower than those of samples with stable structural conditions. As the burial depth increases, the shale porosity shows a decreasing trend, but the decrease is limited. Burial depth significantly impacts the SSA and PV of high-TOC samples (3%–6%). As the burial depth increases, both SSA and PV show a significant decreasing trend. When the burial depth reaches 4000 m, SSA and PV tend to concentrate. The formation pressure coefficient is an important factor for the development and preservation of shale pores, and porosity is positively correlated with the formation pressure coefficient. Increased formation pressure coefficient indicates superior preservation conditions and enhanced pore development.

New Rock Magnetism and Magnetic Fabrics Studies on the Late Triassic Volcanic Rocks from Qaidam Block, Northern Tibetan Plateau

The Qaidam Block, located at the northern Qinghai–Tibet Plateau, is a pivotal area in unraveling the closure time of the Kunlun Ocean basin which might have recorded the transformation process between the Proto-Tethys and Paleo-Tethys Ocean basins. However, the late Triassic position of the Qaidam Block remains enigmatic, largely due to the scarcity of paleomagnetic data essential for quantitatively determining its paleolatitude. The widespread presence of the Elashan formation, particularly along the southern periphery of the Qaidam block, presents good material for conducting paleomagnetic work. Nevertheless, the primary magnetic carriers preserved within the Elashan formation might be influenced by multiple tectonic thermal events, particularly those associated with collisions between southern blocks and the Qaidam Block. Here we present rock magnetism and magnetic fabrics studies to identify the content and composition of magnetic minerals within the Elashan formation. The rock magnetic and petrologic results show that the magnetic carriers in the samples from the Elashan formation are dominated by magnetite with a small amount of goethite, pyrrhotite, and hematite. The results of Anisotropy in Magnetic Susceptibility indicate that the south of the Longwalangku section might not be obviously influenced by the tectonic events. Our results also provided guidance for future paleomagnetic research, emphasizing the importance of conducting further sampling away from adjacent faults, particularly in the southern Longwalangku area.

Provenance and paleoenvironmental studies of Bima and Dukul Formations in the Yola Basin, Northern Benue Trough, Nigeria.

Sedimentological studies of some areas located within latitudes 11035’E & 12000’E, and longitudes 9014’N & 9025’N were undertaken to delineate the surface lithologies of the Yola sub-basin, in the Northern Benue Trough. Field observations of the surficial deposits at Mayolope, Taana, Kpasam and Bille revealed that they are Bima Formation while the ones in Abare are Dukul Formation. Paleoenvironmental studies based on the characteristics of lithofacies of these exposed sections and laboratory assessments of some selected samples showed that the Bima Formation was deposited in a continental setting while the Dukul Formation was deposited in a low-energy marine setting. Petrographic studies of framework components showed that the samples of the Bima Formation were predominated by quartz minerals, leading to their identifications as sandstones and classifications as quartzarenites while the samples of the Dukul Formation were limestones and were classified as bioclastic packstones. Heavy mineral compositions of the sandstones revealed their provenance; Zircon and Tourmaline with a combined amount of 60.1% suggested igneous and low-grade metamorphic rocks while rutile and staurolite with a total amount of 27.7% indicated contributions from high-grade metamorphic rocks.

Pore Fractal Characteristics between Marine and Marine–Continental Transitional Black Shales: A Case Study of Niutitang Formation and Longtan Formation

Marine shales from the Niutitang Formation and marine–continental transitional shales from the Longtan Formation are two sets of extremely important hydrocarbon source rocks in South China. In order to quantitatively compare the pore complexity characteristics between marine and marine–continental transitional shales, the shale and kerogen of the Niutitang Formation and the Longtan Formation are taken as our research subjects. Based on organic petrology, geochemistry, and low-temperature gas adsorption analyses, the fractal dimension of their pores is calculated by the Frenkel–Halsey–Hill (FHH) and Sierpinski models, and the influences of total organic carbon (TOC), vitrinite reflectance (Ro), and mineral composition on the pore fractals of the shale and kerogen are discussed. Our results show the following: (1) Marine shale predominantly has wedge-shaped and slit pores, while marine–continental transitional shale has inkpot-shaped and slit pores. (2) Cylindrical pores are common in organic matter of both shale types, with marine shale having a greater gas storage space (CRV) from organic matter pores, while marine–continental transitional shale relies more on inorganic pores, especially interlayer clay mineral pores, for gas storage due to their large specific surface area and high adsorption capacity (CRA). (3) The fractal characteristics of marine and marine–continental transitional shale pores are influenced differently. In marine shale, TOC positively correlates with fractal dimensions, while in marine–continental shale, Ro and clay minerals have a stronger influence. Ro is the primary factor affecting organic matter pore complexity. (4) Our two pore fractal models show that the complexity of the shale in the Longtan Formation surpasses that of the shale in the Niutitang Formation, and type I kerogen has more complex organic matter pores than type III, aiding in evaluating pore connectivity and flow effectiveness in shale reservoirs.

Non‐destructive quantitative analysis of melt inclusions in extraterrestrial samples: Case study of chassignite via nanoscale X‐ray computed tomography

AbstractEstimation of the composition of planetary rocks and minerals is crucial for understanding their formation processes. In this study, we present the application of X‐ray nano‐computed tomography (nano‐XCT) for non‐destructive three‐dimensional (3‐D) phase analysis and estimation of phase abundances in rare Martian meteorite samples, specifically chassignite Northwest Africa (NWA) 2737. We determined the most suitable laser power for minimizing artifacts and maximizing phase contrast. By utilizing nano‐XCT, we successfully identified and segmented primary phases in the bulk meteorite sample. Additionally, we were able to locate and segment crystallized silicate melt inclusions within the meteorite. The phase abundances in bulk NWA 2737 and within melt inclusions calculated using nano‐XCT were in good agreement with previous studies that used thin section calculations, demonstrating the reliability of nano‐XCT as a non‐destructive alternative for estimating bulk phase abundances in rare samples. This study develops a benchmarking protocol and demonstrates the efficacy of nano‐XCT as a non‐destructive technique for generating an overview of phase distribution and assemblages of melt inclusions within rare samples. Future research can benefit from combining non‐destructive 3‐D phase assemblage estimations with non‐destructive 3‐D chemical analysis techniques to achieve a fully non‐destructive parental magma composition estimation of rare cumulate samples.

Early Age Assessment of a New Course of Irish Fly Ash as a Cement Replacement

This paper explores the potential of a new source of fly ash, deposited on the site of a coal-fired power plant in Ireland dating from 1985 to 1995, as a cement replacement material. A series of X-ray diffraction (XRD) analyses on binder samples with cement replacement levels of 0, 10, 25 and 35% was undertaken to determine the fly ash’s mineralogical composition and to determine its suitability as a supplemental cementitious material (SCM). The XRD results reveal a unique mineral composition with promising characteristics for enhancing the strength and durability of concrete. The experimental results were used to calibrate a thermodynamic model to predict changing phase assemblage and hydration behaviour over time and per replacement level. Thermodynamic models have been shown to give credible predictions of the long-term performance of cements, including SCMs. The initial experimental results’ thermodynamic modelling demonstrates the feasibility of this fly ash source as a sustainable alternative to traditional cement, paving the way for more eco-friendly construction. Ash deposits dating from 1995 to 2005 and from 2005 to the present will be presented in subsequent publications.

Accretion of the lower oceanic crust at fast-spreading ridges: Insights from Hess Deep (East Pacific Rise, IODP Expedition 345)

Abstract At mid-ocean ridges, melts that formed during adiabatic melting of a heterogeneous mantle migrate upwards and ultimately crystallize the oceanic crust. The lower crustal gabbros represent the first crystallization products of these melts and the processes involved in the accretion of the lowermost crust drive the chemical evolution of the magmas forming two thirds of Earth’s surface. At fast-spreading ridges, elevated melt supply leads to the formation of a ⁓6 km-thick layered oceanic crust. Here, we provide a detailed petrochemical characterization of the lower portion of the fast-spread oceanic crust drilled during IODP Expedition 345 at the East Pacific Rise (IODP Holes U1415), together with the processes involved in crustal accretion. The recovered gabbroic rocks are primitive in composition and range from troctolites to olivine gabbros, olivine gabbronorites and gabbros. Although textural evidence of dissolution-precipitation processes is widespread within this gabbroic section, only the most interstitial phases record chemical compositions driven by melt-mush interaction processes during closure of the magmatic system. Comparing mineral compositions from this lower crustal section with its slow-spreading counterparts, we propose that the impact of reactive processes on the chemical evolution of the parental melts is dampened in the lower gabbros from magmatically productive spreading centres. Oceanic accretion thereby seems driven by fractional crystallization in the lower gabbroic layers, followed by upward reactive percolation of melts towards shallower sections. Using the composition of clinopyroxene from these primitive, nearly unmodified gabbros, we estimate the parental melt trace element compositions of Hess Deep, showing that the primary melts of the East Pacific Rise are more depleted in incompatible trace elements compared to those formed at slower spreading rates, as a result of higher melting degrees of the underlying mantle.

Physicochemical Properties of Fortified Coconut Milk Based Chocolate - Like Drinks as Influenced by Cocoa Powder and Sugar Levels

The physicochemical, proximate, vitamins and minerals composition of fortified drinks produced from coconut milk, cocoa powder, and sugar was evaluated. Drinks samples were formulated with different concentration of coconut milk, cocoa powder and sugar levels. Samples includes: “k1 (Coconut milk 100 %), k2 (Coconut milk 99.8 % cocoa powder 0.2 %), k3 (Coconut milk 99.6 %, cocoa powder 0.4%), k4 (Coconut milk 98 %, sugar 2%), k5 (Coconut milk 97.8 %, cocoa powder 0.2%, sugar 2%), k6 ( Coconut milk 97.6 %, cocoa powder 0.4%, sugar 2%), k7 (Coconut milk 96 %, sugar 4%), k8 (Coconut milk 95.8 %, cocoa powder 0.2%, sugar 4%), k9 (Coconut milk 95.6 %, cocoa powder 0.4%, sugar 4%)”. The samples were produced and subjected to physicochemical, proximate, vitamins and minerals analysis using standard methods. Physicochemical composition, pH ranged from 6.50 (k1) to 6.72 (k9), TTA from 0.23 (k9) to 0.41 % (k1), specific gravity from 1.03 % (k1) to 1.13 % (k9), total solid from 18.91(k1) to 22.52 g/100g (k9), SNF from 7.23 (k2) to 10.25 g/100g (k8) and energy values from 124.63 (k1) to 148 Kcal/100g (k9). The proximate composition; moisture from 77.48 % (k9) to 81.09 % (k1), protein from 3.42 (k1) to 3.96 % (k9), ash from 0.71(k1) to 0.98 %(k9), crude fiber from 0.02 % (k1) to 0.06 % (k9), fat from 10.23 % (k1) to 12.27% (k9) and carbohydrate from 4.82 to 5.58% for k1 and k9. Vitamin composition, vitamin A from 1.725 to 2.469mg/100g for samples k1 and k2, Vitamin B1 from 0.044 mg/100g (k1) to 0.205 mg/100g (k9), B2 from 0.028 to 0.0114 mg/100g for k1 and k9, vitamin C from 2.981 to 5.751mg/100g for k1 and k9 and vitamin K from 0.141 to 1.137 mg/100g for k1 and k9. Mineral composition of drinks: Calcium ranged from 16. 31 to 27.05mg/100g for k1and k9, Sodium from 15.25 to 16.99 mg/100g for k1 and k9, Magnesium from 37.20 to 72.64 mg/100g for k1 and k9, Zinc from 0.677 to 3.18 mg/100g for k1 and k9, Iron from 2.87 to 3.38 mg/100g for k1 and k2, Iodine from 0.16 to 0.28 mg/100g for k1 and k9.The Cocoa powder and sugar levels improved the physicochemical, proximate, vitamins, minerals and overall nutritional profile of fortified coconut milk based chocolate drinks.