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Bentonite

Bentonite is a naturally occurring absorbent aluminium phyllosilicate clay, primarily composed of montmorillonite, a smectite-group mineral with the general formula (Na,Ca)_{0.33}(Al,Mg)2(Si_4O{10})(OH)_2 \cdot nH_2O, formed through the in-situ alteration and devitrification of volcanic ash or tuff deposits over geological time. This rock exhibits exceptional colloidal and plastic properties due to its layered structure, which allows interlayer water molecules and exchangeable cations like sodium or calcium to facilitate significant swelling—up to 10–15 times its dry volume upon hydration—making it highly versatile for industrial applications. The 's key physical properties include high (typically 70–100 meq/100g), low permeability when compacted, and strong adsorptive abilities, which stem from its fine (often <2 μm) and negative surface charge. Chemically, bentonite is across a wide range and resistant to many environmental conditions, though its swelling behavior varies by type: sodium bentonite (Na-bentonite) swells more dramatically than calcium bentonite (Ca-bentonite). Geologically, major deposits occur in regions with ancient volcanic activity, such as the formations in , , which host about 70% of the world's known supply, underscoring its economic importance as a non-metallic resource. Bentonite's applications span multiple industries, leveraging its binding, sealing, and purifying capabilities; it serves as a key component in drilling muds for and gas to stabilize boreholes and remove cuttings, as a bonding agent in foundry sands for , and in pelletizing to improve handling and efficiency. Additionally, it is used in for slurry walls and liners due to its low (<10^{-9} m/s when hydrated), in and pharmaceuticals as a thickener and absorbent, and in for animal feed pelleting and amendment to enhance retention. Its role in , such as adsorbing and toxins, further highlights its biomedical and ecological value.

Composition and Properties

Chemical Composition

Bentonite is an impure clay material that consists predominantly of , a key member of the group of clay minerals. This composition gives bentonite its characteristic absorbent and swelling properties, with forming the primary structural component in natural deposits. The general chemical formula for in bentonite is (\ce{Na,Ca})_{0.33}(\ce{Al,Mg})_2(\ce{Si_4O_{10}})(\ce{OH})_2 \cdot n\ce{H_2O}, where variations occur depending on the dominant interlayer cations such as sodium or calcium. Key elemental constituents include silicon and aluminum as the primary framework elements, along with magnesium, sodium, calcium, and iron substituting in the octahedral and tetrahedral sheets, while molecules occupy interlayer spaces, contributing up to 15-20% by weight in the natural state. These elements form a layered structure that defines bentonite's mineralogical identity. Natural bentonite deposits typically contain 50-90% , with the remainder comprising impurities such as , , , , , and iron oxides that influence the material's overall purity and processing requirements. These accessory minerals can vary by deposit but generally do not exceed 50% in high-quality bentonite sources. In contrast, fuller's earth, sometimes referred to as non-swelling bentonite, differs in composition by primarily consisting of (attapulgite) or non-plastic calcium-rich variants, often with higher content and lacking the high-swelling dominance of true bentonite. This distinction arises from fuller's earth's formation in different sedimentary environments, resulting in lower purity and reduced interlayer cation exchange potential.

Physical and Chemical Properties

Bentonite, primarily composed of , exhibits distinctive physical and chemical properties arising from its layered silicate structure with negatively charged surfaces. These properties, including high , swelling behavior, and adsorption affinity, stem from the mineral's ability to interact with and ions in its interlayer spaces. One of the key chemical properties of bentonite is its high (CEC), typically ranging from 70 to 100 meq/100 g, which results from the negatively charged layers that attract and exchange cations such as sodium, calcium, and magnesium. This capacity enables bentonite to bind and release ions, influencing its behavior in aqueous environments. Bentonite demonstrates remarkable swelling properties, capable of absorbing up to 10–15 times its dry volume in to form thixotropic gels that exhibit shear-thinning behavior under stress. The mechanism involves the of interlayer cations, which expand the spacing and allow molecules to diffuse between the layers, creating a viscous, gel-like . In its wet state, bentonite displays high plasticity and viscosity, making it moldable and suitable for forming cohesive masses, while in the dry state, it achieves low permeability due to its compact structure and minimal void spaces. Bentonite maintains structural stability up to approximately 500–600 °C, with dehydroxylation of occurring around 600–750 °C, leading to irreversible structural changes in the lattice. Suspensions of sodium-type bentonite typically have a pH in the range of 8 to 10, reflecting the alkaline nature of the exchangeable sodium ions. Additionally, bentonite possesses significant adsorption capacity for organic compounds and , facilitated by its high surface area and sites, allowing it to sequester pollutants such as lead, , and organic dyes from solutions.

Formation and Occurrence

Geological Formation

Bentonite originates from the and of or tuff, processes that transform unstable into clay minerals primarily in marine or freshwater environments. This alteration commonly involves glassy volcanic materials, such as rhyolitic ash, which undergo and reactions over millions of years, breaking down the silica-rich structure into layered silicates. A key mechanism in bentonite formation is the development of minerals, the dominant component including , through the interaction of with magnesium-rich waters that facilitate of aluminosilicates and incorporation of interlayer cations. These conditions promote the swelling properties characteristic of bentonite by allowing expandable layers in the . Many bentonite deposits are associated with geological formations from the and periods, reflecting widespread volcanic activity during these eras that supplied the precursor ash. In deeper burial settings, in bentonite can experience illitisation, a diagenetic process involving the gradual fixation of ions into the interlayer sites, converting expandable layers to non-expandable and forming K-bentonite under elevated temperatures and pressures. This transformation reduces the clay's swelling capacity and is driven by the availability of from surrounding sediments or fluids.

Global Deposits and Mining

Bentonite deposits occur globally in regions associated with ancient volcanic activity, where layers of have weathered into clay. The largest concentrations are found , particularly in Wyoming's and other sedimentary formations, which host extensive beds formed from Cretaceous-age ash falls. Other significant deposits exist in Greece's , India's and states, China's and provinces, and Turkey's Aegean and Central Anatolian areas. These locations account for the majority of commercial production, with deposits typically consisting of lenticular beds ranging from a few meters to tens of meters thick. The dominates global bentonite production, outputting 4.36 million metric tons in 2023 (estimated at 4.8 million metric tons in 2024), with contributing approximately 95% of the national total through operations in three primary geologic districts. follows as the second-largest producer at around 3.7 million metric tons, followed by (2.1 million metric tons), (2.49 million metric tons), and (1.11 million metric tons). Worldwide production reached about 20.3 million metric tons in 2023 (estimated at 21 million metric tons in 2024), reflecting steady demand for applications, with estimates suggesting reserves exceed several billion tons due to the abundance of untapped volcanic-derived deposits. Bentonite is predominantly extracted via open-pit , as deposits are generally shallow, lying 10 to 30 meters below the surface in accessible sedimentary layers. Operations involve removing with bulldozers and scrapers, followed by selective of the clay beds, which are often 1 to 4 meters thick, using front-end loaders and haul trucks for transport to processing sites. This method is efficient for the large, near-surface extents of most deposits, minimizing the need for underground techniques. Environmental management in bentonite mining emphasizes dust suppression and site reclamation to mitigate impacts from dry clay handling and land disturbance. Dust control measures include applying water via trucks or chemical suppressants like magnesium chloride on haul roads and stockpiles, while enclosures and wetting agents reduce airborne particulates during loading. Reclamation efforts restore mined lands to equal or better pre-mining conditions through reseeding native vegetation and reshaping topography, in compliance with federal and state regulations such as the U.S. Surface Mining Control and Reclamation Act. Post-2020 updates to Mine Safety and Health Administration (MSHA) rules have strengthened dust monitoring requirements, mandating more frequent sampling and lower exposure limits for workers, alongside enhanced water management protocols to limit usage in arid regions like Wyoming. In terms of trade, the serves as the leading exporter, shipping 800,000 tons in 2023 (estimated at 700,000 tons in 2024), primarily to , , and , with export values reaching $197 million in 2023. Demand in has surged, driven by industrial growth in and oil , with regional imports increasing by 8.4% in 2022 and the Asia-Pacific market projected to expand at a 5.9% CAGR through 2035. This trend underscores shifting global supply dynamics, with Asian producers like and balancing local consumption and exports.

History

Discovery and Naming

Bentonite was first identified in near Rock River in , within the Benton Shale formation. This initial discovery highlighted the material as a distinctive clay occurring in outcrops associated with alterations, marking the beginning of scientific interest in its unique properties. The term "bentonite" was formally proposed in 1898 by Wyoming state geologist Wilbur C. Knight, who named it after the Fort Benton Shale near Rock River, , drawing from similar geological exposures around . initially considered naming the clay "taylorite" after rancher William , whose property hosted a key deposit, but changed it upon learning the name was already in use for another mineral. This nomenclature emphasized the clay's association with the Benton Formation, a widespread stratigraphic unit. Early observations distinguished bentonite from other clays like kaolin due to its remarkable swelling capacity, expanding several times its dry volume upon . Knight described it as an "unusual clay" with high and colloidal behavior, unlike the non-swelling, less absorbent kaolin, which set bentonite apart as a material suitable for specialized applications. In the late , initial scientific classifications began linking bentonite to the mineral , a smectite-group clay named in after deposits near Montmorillon, . This connection recognized bentonite's predominant composition as montmorillonite, highlighting shared structural and swelling characteristics derived from volcanic origins.

Historical Uses and Development

The utilization of bentonite in industrial applications began to expand in the early , particularly following the 1901 oil well discovery in , which underscored the need for effective viscosifiers in drilling operations. Although initial drilling fluids relied on natural clays, bentonite's swelling properties soon made it a preferred additive for stabilizing boreholes and removing cuttings, with commercial shipments from Wyoming deposits starting as early as 1888 and gaining traction in oil and gas exploration by the . This period marked bentonite's transition from minor uses, such as by teamsters for horse care, to a key component in the burgeoning . In the and , bentonite's applications diversified into , driven by the industry's growth. It was adopted as a bonding agent in foundry sands for casting iron and , with production facilities like those in Upton and Newcastle, , established in 1926 to meet demand. Concurrently, bentonite facilitated the of , particularly , by acting as a to form durable pellets for blast furnaces, enhancing efficiency in ore processing and contributing to the expansion of global output. During , bentonite found strategic roles in military applications due to its absorbent and sealing capabilities. It was incorporated into packets to protect equipment and supplies from moisture, adhering to military specifications like MIL-D-3464E for reliable performance in harsh conditions. Postwar developments from the late 1940s onward broadened bentonite's consumer and industrial footprint. In 1947, Edward Lowe inadvertently pioneered modern cat litter by suggesting granulated clay—such as —for a neighbor's cat box, leading to the commercialization of absorbent litters that revolutionized pet care. By the 1950s, bentonite became a standard fining agent in , particularly for clarifying white wines and stabilizing proteins to prevent haze, with sodium varieties from U.S. deposits proving most effective in adsorbing unstable compounds. Since 2000, bentonite has seen innovative applications in , where it serves as a base for composites used in and . These advancements involve modifying bentonite with to enhance adsorption of pollutants, with reviews highlighting improved efficiency in removing and dyes through layered structures. Such developments underscore bentonite's evolving role in high-tech materials, building on its historical versatility.

Types

Sodium Bentonite

Sodium bentonite is characterized by a predominance of sodium cations (Na⁺) over calcium cations (Ca²⁺) in the interlayer positions of its structure, distinguishing it from other bentonite variants through enhanced osmotic swelling behavior. This high sodium content facilitates greater hydration and dispersion in compared to calcium-dominant forms, primarily due to the larger hydrated and lower of Na⁺ ions. Upon contact with water, sodium bentonite exhibits remarkable swelling, expanding 5 to 15 times its original dry volume as interlayer water layers form and osmotic pressures drive layer separation. This property arises from the weak electrostatic forces between the negatively charged silicate layers and the exchangeable interlayer cations, allowing extensive interlayer expansion. The primary deposits of sodium bentonite are located in the , with serving as the leading production region, accounting for the majority of global supply. A significant portion of produced sodium bentonite, estimated at around 40% as of 2023, originates from these U.S. sources and is directed toward industrial fluid formulations. Key properties of sodium bentonite include its ability to form high-viscosity gels with low permeability when dispersed in aqueous systems, making it suitable for sealing and roles. These rheological characteristics stem from the clay's high (CEC), which typically ranges from 80 to 150 meq/100 g, enabling strong interactions with surrounding electrolytes and polymers. The CEC reflects the total negative charge on the montmorillonite surfaces available for cation substitution, directly influencing swelling and gelation efficiency. Calcium bentonite can be transformed into sodium bentonite through a process known as sodium activation, involving treatment with (Na₂CO₃) to facilitate . This activation typically entails mixing the clay with 2-5% Na₂CO₃ by weight, followed by heating and rehydration to replace interlayer Ca²⁺ with Na⁺, thereby enhancing swelling capacity. The resulting material exhibits properties akin to naturally occurring sodium bentonite, broadening supply options for high-swelling applications. Sodium bentonite holds a dominant position in the , comprising approximately 65-70% of total bentonite due to its versatile swelling and rheological attributes. This market leadership is driven by abundant reserves in key regions like and increasing demand for specialized clay products.

Calcium Bentonite

Calcium bentonite is characterized by a predominance of calcium ions (Ca²⁺) over sodium ions in the exchangeable cation positions of its structure, distinguishing it from the sodium-dominant variant. This composition imparts low-swelling properties, with the clay typically expanding only 2-3 times its dry volume upon , compared to 5-15 times for sodium bentonite. The reduced swelling arises from weaker of calcium ions, leading to less interlayer while maintaining high adsorptive capacity for applications focused on rather than sealing. The material exhibits superior bonding in dry conditions and greater dry tensile strength, making it suitable for processes requiring structural integrity without excessive moisture sensitivity. Its (CEC) generally falls in the range of 70-90 meq/100 g, lower than that of sodium bentonite due to differences in purity and associated impurities, and it demonstrates minimal gelling in aqueous suspensions. These properties stem from the tighter interlayer structure and higher iron content often present in calcium varieties. Calcium bentonite occurs naturally in non-marine deposits, primarily resulting from the of in terrestrial or freshwater settings, as opposed to the marine origins typical of sodium types. Major global deposits are found in , notably in Greece's Island, where extensive mining operations extract high-purity calcium bentonite from Miocene volcaniclastic rocks. These deposits can be ion-exchanged to produce sodium bentonite for broader industrial use. Commonly referred to as in its absorbent form, calcium bentonite is widely utilized for decolorizing and refining oils and fats by adsorbing colorants and impurities during processing. Its high purity and gentle adsorptive nature also support specialized applications, such as additives in to bind mycotoxins like aflatoxins, thereby reducing toxicity in diets, and in as a mild absorbent in facial masks and powders for .

K-Bentonite and Other Variants

K-bentonite, also known as , is a diagenetically altered form of characterized by / (I/S) mixed-layer clays resulting from the fixation of ions (K+). This alteration transforms the original structure into a more stable, potassium-rich illitic clay, distinguishing it from sodium or calcium bentonites by its reduced expandability. The formation of K-bentonite occurs through burial diagenesis, where converts to at depths exceeding 1 km and temperatures typically below 100°C, with K+ sourced from interstitial fluids in non- or environments. This illitization process collapses the interlayer spacing and diminishes swelling capacity, often progressing in thin beds within sedimentary sequences. As part of the broader illitisation seen in bentonite evolution, it preserves volcanic signatures useful for stratigraphic correlation. Significant occurrences of K-bentonite are found in strata of the , featuring up to 80 thin layers in clusters of 8–15 beds within marine carbonates. Similar deposits appear in Late limestones of northwestern . Due to its thermal stability and fine particle size, K-bentonite from deposits like Dolná Ves in is used in ceramics for manufacturing floor and wall tiles. Other variants include sulfur bentonite, a granular composite of 90% elemental and 10% bentonite, designed for slow-release sulfur fertilizers to address deficiencies and lower for nutrient uptake. The bentonite acts as a , enabling controlled degradation and conversion in agricultural soils. Polymer-modified bentonite enhances mechanical and hydraulic stability by incorporating polymers that bond clay particles, improving resistance to wet-dry cycles and aggressive leachates in geosynthetic clay liners for waste containment. This modification extends , reducing permeability in high-pH or saline environments. Recent acid-activated variants of bentonite, treated with sulfuric or to increase surface area and , serve as heterogeneous catalysts in , such as esterification of fatty acids for and of hydrocarbons. These modifications yield Brønsted and acid sites, boosting activity in reactions like nitrobenzene production under conditions.

Production and Processing

Extraction Methods

Bentonite is primarily extracted through open-pit methods, which are well-suited to its occurrence in shallow, unconsolidated deposits typically no deeper than 50 feet. This approach involves the removal of overlying using such as excavators, bulldozers, and scrapers to access the soft clay layers. In major producing regions like , operations employ a back-casting where mined pits are progressively filled with overburden from adjacent areas to facilitate simultaneous reclamation. In stratified deposits, selective techniques are applied to target specific layers and minimize dilution, particularly to separate sodium-rich and calcium-rich bentonite seams that may occur in alternating beds. For instance, in deposits with well-defined seams, operators use controlled excavation to isolate high-grade sodium zones, which predominate in , from calcium variants found elsewhere like . This method enhances product quality by reducing intermixing with lower-grade material. are employed for harder in areas where the covering material is more consolidated, allowing efficient removal before excavating the underlying bentonite. Overburden-to-ore ratios vary by site but commonly fall between 1:1 and 3:1 in favorable shallow deposits, such as those in Wyoming's Northern district, where overburden thicknesses of 1-4.5 meters overlie 2-3 meter bentonite beds. Safety and environmental considerations in bentonite emphasize control to mitigate respirable crystalline silica exposure, a hazard present due to the mineral's volcanic origins. sprays are routinely applied during removal and clay loading to suppress , aligning with standard practices. Post-2020 regulations, including the U.S. Mine Safety and Health Administration's 2024 final rule, have lowered the for respirable crystalline silica to 50 micrograms per cubic meter over an 8-hour shift, prompting enhanced monitoring and engineering controls in operations across .

Beneficiation and Activation

Bentonite ore, as extracted, typically contains 25-35% moisture, which must be reduced to 5-12% for , , and further to prevent and facilitate handling. This drying is commonly achieved using rotary drum dryers operating at temperatures between 100°C and 200°C, where or direct heating evaporates while minimizing structural alterations to the clay minerals. The process ensures uniform moisture content below 10%, enhancing the material's stability and preparing it for subsequent refinement steps. Beneficiation refines raw bentonite by removing impurities such as , , and other non-clay minerals to achieve a target purity exceeding 85%, improving its performance in industrial applications. This involves initial crushing to reduce particle size, followed by screening to separate coarser impurities, and in some cases, wet methods like classification or flotation to isolate high-quality fractions from materials. Dry beneficiation techniques, such as attrition scrubbing, are also employed for less contaminated deposits, yielding concentrates suitable for without excessive usage. Activation enhances bentonite's swelling capacity, cation exchange, and surface properties by modifying its interlayer cations or structure, often converting calcium-rich variants to more versatile sodium types. Sodium activation, a common process, involves treating calcium bentonite with 2-2.5 wt.% sodium carbonate (Na₂CO₃, or soda ash) in an aqueous slurry at around 100°C for 30-60 minutes, facilitating ion exchange where Na⁺ replaces Ca²⁺ and Mg²⁺ ions to boost hydration and rheological properties. This results in a material with improved dispersibility in water, essential for applications requiring high viscosity. Acid activation, typically using sulfuric acid (H₂SO₄) concentrations of 10-40% at elevated temperatures, protonates the clay lattice, dissolving impurities and expanding the interlayer space to yield high-surface-area products up to 200 m²/g, ideal for catalytic and adsorptive uses. The process increases porosity and acidity while preserving the smectite framework, though excessive treatment can lead to partial dealumination. Quality control in beneficiation and activation ensures consistency through standardized tests tailored to end-use specifications, such as bleed or filter loss tests for drilling-grade bentonite, which measure separation under to verify low loss (typically <15 mL/30 min) and . Recent advancements include organic modifications, such as intercalation with quaternary ammonium , to produce organobentonites for nanocomposites, enhancing compatibility with polymers and improving mechanical reinforcement in like gels and coatings. These modifications, often involving cetyltrimethylammonium , increase basal spacing and hydrophobicity, enabling tailored properties for environmental and composites.

Applications

Drilling Fluids and Construction

Bentonite is a key component in drilling fluids for and gas , typically incorporated at concentrations of 2-5% by weight to impart and to the . This formulation achieves a of 30-50 seconds per , which supports efficient heat dissipation from the , reduces friction on the wall, and maintains sufficient hydrostatic pressure to prevent blowouts by counterbalancing formation pressures. The gel strength provided by bentonite, ranging from 10-20 lb/100 ft², is essential for suspending and removing during circulation and ensuring stability during downtime by forming a supportive that minimizes fluid invasion into the formation. In , bentonite are employed to construct impermeable barriers such as slurry walls for and landfills, where the mixture is prepared at 20-30% solids content to achieve below 10^{-7} cm/s upon backfilling and . These walls effectively contain and prevent contaminant migration by leveraging bentonite's swelling properties to form low-permeability seals. Post-2015 developments have focused on integrating eco-friendly biodegradable additives with bentonite to enhance sustainability, reducing environmental discharge by promoting rapid degradation of spent mud while maintaining rheological performance. For example, bagasse-derived additives have been shown to improve control without compromising or strength. A practical application in involves using local bentonite to seal sandy soils in farming regions for improved efficiency, where incorporation at low rates enhanced water retention and supported early growth of seedlings by reducing seepage losses in arid conditions.

Binders, Fillers, and Catalysts

Bentonite serves as a critical in applications, where it is incorporated at 5-10% by weight into to form green sand molds for . This addition provides essential green strength, enabling the mold to maintain integrity during the process without collapsing under the weight of molten metal. The clay's swelling properties upon create cohesive bonds between sand grains, facilitating reusable molds in high-volume production of and nonferrous castings. In iron ore pelletizing, bentonite acts as an effective binder at dosages of 0.5-1% of the moist concentrate weight, agglomerating fine particles into strong pellets suitable for feed. This low addition level ensures pellet stability during handling and firing, while also enhancing by promoting a porous structure that allows better gas penetration during . The binding mechanism relies on the clay's ability to form hydrated bridges between ore particles, improving overall pellet quality without excessive introduction. As a filler, bentonite reinforces rubber and plastics composites, with loadings up to 20% enhancing mechanical properties such as tensile strength and through its that distributes evenly. In rubber formulations, it acts as a cost-effective extender, improving resistance and processability. For plastics like , similar loadings provide dimensional stability and reduced permeability. In paper coatings, bentonite contributes to opacity by aiding filler retention and creating a surface that scatters effectively. Acid-activated bentonite functions as a catalyst in , particularly for cracking, where its modified structure facilitates the breakdown of heavy fractions into lighter products. Activation with increases the surface area to 150-300 m²/g, exposing more active sites for acid-catalyzed reactions and improving selectivity in units. This process, briefly referencing beneficiation techniques like acid treatment, enhances the clay's acidity and for industrial-scale efficiency. In ceramics, bentonite is employed as a suspending agent in glazes at 1-3% addition, preventing and settling to ensure even application and firing results. Its colloidal nature forms a thixotropic that flows under brushing shear but stabilizes at rest, maintaining glaze homogeneity without excessive . This role supports consistent performance across production batches.

Absorbents and Purifiers

Bentonite serves as an effective absorbent and purifier due to its high surface area and swelling capacity, which facilitate the adsorption of liquids and impurities in various industrial and consumer applications. Calcium bentonite, in particular, is widely used in clumping litters, where it absorbs by expanding up to times its volume and forms solid clumps that trap moisture and control odors through and bacterial inhibition. This property makes it a dominant material in the U.S. products , with clumping clay-based litters accounting for over 75% of the cat litter segment. In water purification, bentonite removes contaminants such as dyes and via cation exchange and surface adsorption. For instance, natural bentonite exhibits an adsorption capacity of 20-50 mg/g for Pb²⁺ ions, enabling efficient removal from at dosages of 1-5 g/L. Acid-activated variants enhance this capacity to up to 92.9 mg/g, making bentonite a cost-effective alternative to synthetic adsorbents in treating industrial effluents. Bentonite functions as a bleaching earth in the fining of edible oils and wines, adsorbing pigments and impurities to improve clarity and stability. In , dosages of 0.5-2% bentonite reduce content by 35-62%, effectively decolorizing crude oils like sunflower and hempseed while removing trace metals and soaps. For wine fining, additions of 0.1-1.5 g/L target haze-forming proteins and contribute to decolorization by adsorbing polyphenolic compounds, with activated forms showing higher efficiency in red varietals. In spill cleanup, bentonite absorbs oils and hydrocarbons from surfaces, with organo-modified forms achieving adsorption capacities exceeding 10 g/g for emulsions. Recent advancements incorporate nanobentonite composites, which enhance efficiency by increasing and selectivity, allowing up to 90% recovery of spilled hydrocarbons in marine environments. Emerging research in the highlights bentonite's potential for microplastic removal from , leveraging its properties to achieve over 90% efficiency in pilot-scale systems using modified bentonite columns. These applications underscore bentonite's versatility in addressing liquid and particulate pollutants without generating secondary waste.

Pharmaceutical and Agricultural Uses

Bentonite, particularly in its dioctahedral form known as , is utilized in pharmaceuticals as an agent due to its ability to adsorb toxins, bacteria, and excess fluids in the , thereby reducing the duration and frequency of acute episodes in children and adults. It also serves as an by neutralizing gastric acidity and protecting the intestinal mucosa, with modified bentonite formulations showing potential to control without interfering with . The U.S. recognizes bentonite as (GRAS) for direct use, with typical internal dosages ranging from 1.5 to 3 grams per day for therapeutic applications like or digestive support, though lead risks in some products necessitate caution. In wound care, bentonite complexes promote skin regeneration in burn wounds by enhancing synthesis, , and while exhibiting anti-inflammatory effects. Calcium bentonite, noted for its low profile, is preferred in pharmaceutical formulations for internal applications due to reduced content compared to sodium variants. In , bentonite functions as an absorbent in face masks, effectively drawing out excess oil, impurities, and toxins from to improve and reduce sebum , particularly benefiting oily or acne-prone skin types. It also acts as a thickener in formulations, providing , preventing ingredient separation, and aiding in and foaming during use. Agriculturally, bentonite serves as a soil amendment to enhance water retention in sandy or low-fertility , with applications increasing available water capacity by 10-67% depending on dosage and , thereby mitigating stress for crops like . In Thailand's northeast sandy fields, bentonite additions improve and water-holding properties, supporting and resilience in rice cultivation by reducing seepage and enhancing overall field stability. As an binder, it adsorbs mycotoxins such as aflatoxins in the gastrointestinal tract of , preventing absorption and reducing toxicity without affecting nutrient . In fertilizers, sulfur bentonite granules slowly release sulfate ions (SO_4^{2-}) through microbial oxidation upon contact, providing season-long sulfur nutrition to crops while improving granule distribution and efficacy.

Environmental and Specialized Applications

Bentonite plays a critical role in environmental protection through its use in landfill liners, where compacted forms achieve hydraulic conductivities below $10^{-9} m/s, effectively preventing leachate migration into groundwater. Geosynthetic clay liners (GCLs) incorporating bentonite, typically sodium-based, swell upon hydration to form a self-sealing barrier with permeabilities as low as $10^{-9} to $10^{-12} cm/s when saturated, outperforming traditional compacted clay liners in installation efficiency and longevity. This low permeability stems from bentonite's montmorillonite structure, which expands to fill voids, as demonstrated in field applications at sites like the Broad Acre Landfill, where no leachate releases have been observed over decades. In emergency response scenarios, bentonite serves as an absorbent for chemical and oil spills due to its high swelling capacity and ability to form stable emulsions with hydrocarbons. Composite foams filled with bentonite, for instance, exhibit enhanced for oil recovery, absorbing up to several times their weight in contaminants while maintaining structural integrity for easy removal. Similarly, bentonite-based materials are deployed in nuclear waste management as engineered barriers, providing low permeability (around $10^{-12} m/s) and to isolate radioactive materials from the . Compacted bentonite buffers in repositories like those proposed for ensure thermal, hydraulic, and mechanical containment, with self-healing properties mitigating potential fractures. Bentonite functions as a in pesticide delivery systems, enabling controlled release to minimize environmental and enhance . In alginate-bentonite formulations, the clay's interlayer structure intercalates active ingredients like or chloridazon, regulating diffusion over weeks to months and reducing initial burst release by up to 50% compared to conventional granules. This approach sustains pesticide concentrations at target levels while limiting contamination. As a sealant in geosynthetic clay liners for dams and reservoirs, bentonite provides impermeable barriers against seepage, with hydration-induced swelling achieving hydraulic conductivities below $10^{-9} m/s under load. These liners, consisting of bentonite encapsulated between geotextiles, are needle-punched for resistance and used in high-load applications like dams, where they outperform geomembranes in puncture self-repair. Recent advancements highlight organo-bentonite as a for carbon capture, leveraging modifications to boost CO_2 adsorption capacities in post-combustion scenarios. Post-2022 studies demonstrate that surfactant-intercalated organo-bentonites achieve uptake rates of 1-2 mmol/g at ambient conditions, attributed to enhanced surface area and amine functionalization for . These materials address gaps in scalable, low-cost technologies by integrating with existing systems, showing regenerability over multiple cycles with minimal degradation.

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