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Halloysite
Halloysite
Halloysite
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Halloysite
General
CategoryPhyllosilicate minerals
GroupKaolinite-Serpentine group, kaolinite subgroup
FormulaAl2Si2O5(OH)4
Strunz classification9.ED.10
Crystal systemMonoclinic
Crystal classDomatic (m)
(same H-M symbol)
Space groupCc
Unit cella = 5.14, b = 8.9,
c = 7.214 [Å]; β = 99.7°; Z = 1
Identification
ColorWhite; grey, green, blue, yellow, red from included impurities.
Crystal habitSpherical clusters, massive
CleavageProbable on {001}
FractureConchoidal
Mohs scale hardness2–2.5
LusterPearly, waxy, or dull
DiaphaneitySemitransparent
Specific gravity2–2.65
Optical propertiesBiaxial
Refractive indexnα = 1.553–1.565
nβ = 1.559–1.569
nγ = 1.560–1.570
Birefringenceδ = 0.007
References[1][2][3]

Halloysite is an aluminosilicate clay mineral with the empirical formula Al2Si2O5(OH)4. Its main constituents are oxygen (55.78%), silicon (21.76%), aluminium (20.90%), and hydrogen (1.56%). It is a member of the kaolinite group. Halloysite typically forms by hydrothermal alteration of alumino-silicate minerals.[4] It can occur intermixed with dickite, kaolinite, montmorillonite and other clay minerals. X-ray diffraction studies are required for positive identification. It was first described in 1826, and subsequently named after, the Belgian geologist Omalius d'Halloy.

Structure

[edit]

Halloysite naturally occurs as small cylinders (nanotubes) that have a wall thickness of 10–15 atomic aluminosilicate sheets, an outer diameter of 50–60 nm, an inner diameter of 12–15 nm, and a length of 0.5–10 μm.[5] Their outer surface is mostly composed of SiO2 and the inner surface of Al2O3, and hence those surfaces are oppositely charged.[6][7] Two common forms are found. When hydrated, the clay exhibits a 1 nm spacing of the layers, and when dehydrated (meta-halloysite), the spacing is 0.7 nm. The cation exchange capacity depends on the amount of hydration, as 2H2O has 5–10 meq/100 g, while 4H2O has 40–50 meq/100g.[8] Endellite is the alternative name for the Al2Si2O5(OH)4·2(H2O) structure.[8][9]

Owing to the layered structure of the halloysite, it has a large specific surface area, which can reach 117 m2/g.[10]

Formation

[edit]
Electron micrograph of halloysite nanotubes[6]
Halloysite nanotubes intercalated with ruthenium catalytic nanoparticles[6]

The formation of halloysite is due to hydrothermal alteration, and it is often found near carbonate rocks. For example, halloysite samples found in Wagon Wheel Gap, Colorado, United States are suspected to be the weathering product of rhyolite by downward moving waters.[4] In general the formation of clay minerals is highly favoured in tropical and sub-tropical climates due to the immense amounts of water flow. Halloysite has also been found overlaying basaltic rock, showing no gradual changes from rock to mineral formation.[11] Halloysite occurs primarily in recently exposed volcanic-derived soils, but it also forms from primary minerals in tropical soils or pre-glacially weathered materials.[12] Igneous rocks, especially glassy basaltic rocks are more susceptible to weathering and alteration forming halloysite.

Often as is the case with halloysite found in Juab County, Utah, United States the clay is found in close association with goethite and limonite and often interspersed with alunite. Feldspars are also subject to decomposition by water saturated with carbon dioxide. When feldspar occurs near the surface of lava flows, the CO2 concentration is high, and reaction rates are rapid. With increasing depth, the leaching solutions become saturated with silica, aluminium, sodium, and calcium. Once the solutions are depleted of CO2 they precipitate as secondary minerals. The decomposition is dependent on the flow of water. In the case that halloysite is formed from plagioclase it will not pass through intermediate stages.[4]

Locations

[edit]

A highly refined halloysite is mined, then processed, from a rhyolite occurrence in Matauri Bay, New Zealand.[13][14][15][16] Annual output of this mine is up to 20,000 tonnes per annum.[17]

One of the largest halloysite deposits in the world is Dunino, near Legnica in Poland.[18] It has reserves estimated at 10 million tons of material. This halloysite is characterized by layered-tubular and platy structure.[19]

The Dragon mine, located in the Tintic district, Eureka, Utah, US deposit contains catalytic quality halloysite. The Dragon Mine Deposit is one of the largest in the United States. The total production throughout 1931–1962 resulted in nearly 750,000 metric tons of extracted halloysite. Pure halloysite classified at 10a and 7a are present.[20]

Applications

[edit]

Commercial

Uses of the halloysite produced at the Matauri Bay deposit in New Zealand include porcelain and bone china by manufacturers in various countries, particularly in Asia.[13][14][15][16]

Laboratory studies

  • Halloysite is an efficient adsorbent both for cations and anions. It has also been used as a petroleum cracking catalyst, and Exxon has developed a cracking catalyst based on synthetic halloysite in the 1970s.[21] Owing to its structure, halloysite can be used as filler in either natural or modified forms in nanocomposites. Halloysite nanotube can be intercalated with catalytic metal nanoparticles made of silver, ruthenium, rhodium, platinum or cobalt, thereby serving as a catalyst support.[6]
  • Halloysite has been evaluated for use in the sorption of CO2[22] and CH4.[23]
  • Due to its nanostructure, halloysite is used as the main nanostructured filler in multifunctional mixed matrix membranes (MMMs), opening up new possibilities in the separation of gaseous and liquid mixtures [24] and water purification.[25]
  • Besides supporting nanoparticles, halloysite nanotubes can also be used as a template to produce round well-dispersed nanoparticles (NPs). For example, bismuth and bismuth subcarbonate NPs with controlled size (~7 nm) were synthesized in water. Importantly, when halloysite was not used, large nanoplates instead of round spheres are obtained.[26]
  • Halloysite is also used to purify water, e.g. from two azo dyes were removed from aq. solutions. by adsorption on a Polish halloysite from Dunino deposit.[27]
  • Halloysite have many advantages and reported as a nanocontainer.[28][29]
  • Halloysite can also be used to produce porous silicon nanotubes as anode materials for Li-ion batteries through the selective etching of aluminium oxide and thermal reduction.[30]
  • As a nanofiller in nanocomposite e.g. thermoplastic polyurethane acting on the mechanical, physicochemical and biological properties.[31]

Chemistry and mineralogy

[edit]

Typical chemical and mineralogical analyses of two commercial grades of halloysite are:[32]

Product name Premium Yunnan
Country New Zealand China
Area Northland Yunnan
SiO2, % 49.5 42.7
Al2O3, % 35.5 37.0
Fe2O3, % 0.29 0.10
TiO2, % 0.09 <0.05
CaO, % - -
MgO, % - -
K2O, % - <0.05
Na2O, % - <0.05
LOI, % 13.8 19.8
Halloysite, % 92 99.1
Cristobalite, % 4 -
Quartz, % 1 0.1

References

[edit]
Revisions and contributorsEdit on WikipediaRead on Wikipedia

Halloysite

View on Grokipedia
from Grokipedia
Halloysite is a naturally occurring belonging to the group of 1:1 phyllosilicates, characterized by its distinctive tubular morphology and chemical composition of Al₂Si₂O₅(OH)₄·nH₂O, where n=2 in the hydrated form (halloysite-10Å) and n=0 in the dehydrated form (halloysite-7Å). This mineral forms hollow nanotubes with an inner lumen diameter of 10–30 nm, an outer diameter of 40–70 nm, and lengths ranging from 200 nm to 2 μm, resulting from the curvature of its alternating tetrahedral silica and octahedral alumina layers in a . Structurally similar to but distinguished by its rolled-layer configuration, halloysite exhibits a disordered structure that enhances its reactivity, with a high up to 184.9 m²/g, pore volume up to 0.353 cm³/g, and thermal stability. Its surface properties include a negatively charged outer silica layer and a positively charged inner alumina lumen at neutral , enabling selective adsorption and . Physically, it appears white to colorless, soft, and plastic when wet, often occurring in tubular, spheroidal, or platy morphologies depending on formation conditions. Halloysite primarily forms through the of parent rocks such as feldspars and micas, or via hydrothermal alteration, and is ubiquitous in soils, weathered rocks, and residual deposits worldwide. Significant occurrences include hydrothermal deposits in the United States (e.g., Tintic district, , with nearly pure halloysite production exceeding 750,000 metric tons historically), residual clays in North Carolina's Spruce Pine area, and volcanic-derived deposits in , , and . Applications of halloysite leverage its nanotubular structure and low toxicity, spanning traditional uses in ceramics for , refractories, and tiles due to its high alumina content (>30 wt%) and whiteness, to advanced roles as nanofillers in polymer composites, adsorbents for , and carriers in drug delivery systems for sustained release of therapeutics like . Its biocompatibility supports biomedical applications, including and coatings, while industrial uses extend to , production, and .

Introduction and Classification

Definition and Composition

Halloysite is a 1:1 dioctahedral belonging to the kaolin-serpentine group. It consists of alternating layers of tetrahedral silica sheets and octahedral alumina sheets, forming a fundamental structure common to kaolin minerals. The of halloysite is Al₂Si₂O₅(OH)₄ · nH₂O, where n = 2 for the hydrated form (halloysite-10Å) and n = 0 for the dehydrated form (halloysite-7Å). This composition reflects its nature, with oxygen, , aluminum, and as primary elements, and variable interlayer water content distinguishing it from related minerals like . Halloysite is recognized as a valid species by the International Mineralogical Association (IMA), with status approved as a pre-IMA species established in 1826. The mineral's name derives from the Belgian Jean-Baptiste Julien d'Omalius d'Halloy (1783–1875), who first studied a tubular sample from , ; it was formally named halloysite in 1826 by French Pierre Berthier in his honor.

Varieties

Halloysite occurs primarily in two varieties distinguished by their degree of hydration and corresponding interlayer spacing: the hydrated halloysite-10Å and the dehydrated halloysite-7Å. The hydrated form, halloysite-10Å, contains interlayer molecules that expand the basal spacing to approximately 10.1 Å, while the dehydrated form, halloysite-7Å, exhibits a collapsed structure with a basal spacing of about 7.2 Å following the loss of this . These varieties are typically tubular in morphology, with halloysite-10Å maintaining a more open interlayer configuration that supports its hydration state. The transition between these varieties occurs through dehydration of halloysite-10Å, often induced by heating above 100°C or environmental conditions, resulting in the formation of halloysite-7Å; this process is generally irreversible, as the dehydrated structure resists rehydration due to structural rearrangements and the absence of suitable conditions for water reinsertion. X-ray diffraction (XRD) serves as a key diagnostic tool for identifying these varieties, with halloysite-10Å showing a characteristic basal reflection peak at 10.0–10.2 Å and halloysite-7Å displaying a broader or weaker peak at 7.1–7.3 Å, reflecting the differences in layer stacking and disorder. In addition to these dominant forms, minor varieties exist, such as platy halloysite, which features flat, platelet-like particles rather than tubes and is less common, often observed in specific geological settings with larger particle sizes up to 50 μm. Intermediate forms, blending characteristics of both hydrated and dehydrated states, can also appear in certain deposits due to partial hydration or environmental variability. These less prevalent variants influence the mineral's reactivity and are identified through combined XRD and morphological analysis.

Properties

Physical and Optical Properties

Halloysite typically exhibits a to pale yellow or brown color, influenced by impurities such as iron oxides, though it can also appear light gray, buff, or pale blue in purer forms. Its Mohs hardness ranges from 1 to 2, making it a soft suitable for various industrial applications without causing abrasion. The specific gravity is 2.0 to 2.65, lower than that of due to the presence of tubular voids that reduce overall density. In terms of morphology, halloysite predominantly forms tubular or cylindrical particles, with lengths typically ranging from 0.2 to 5 μm and outer diameters of 20 to 100 nm, while inner lumens measure 10 to 70 nm; these dimensions contribute to its high and surface area. The 10 hydrated variety (halloysite-10 ) loses interlayer at temperatures around 50-60°C, transitioning to the 7 form (halloysite-7 ), depending on ambient humidity levels. Structural collapse occurs upon dehydroxylation above 500°C, leading to metahalloysite formation. Optically, halloysite is biaxial negative, with refractive indices of nα = 1.553–1.565, nβ = 1.559–1.569, and nγ = 1.560–1.570, and a low of δ = 0.005–0.007. is weak to absent, often not distinctly marked in thin sections. These properties vary slightly with hydration state, as the fully hydrated 10 form has a lower average refractive index around 1.522 compared to 1.548 for the 7 form.

Chemical Properties

Halloysite is a dioctahedral 1:1 composed of alternating tetrahedral sheets dominated by Si⁴⁺ cations and octahedral sheets primarily occupied by Al³⁺ cations, forming a neutral layer with minimal permanent negative charge due to limited isomorphous substitution. This configuration contrasts with 2:1 clays like smectites, where extensive substitution of lower-valence cations (e.g., Al³⁺ for Si⁴⁺ in tetrahedral sheets or Mg²⁺ for Al³⁺ in octahedral sheets) generates significant layer charge and high (CEC). In halloysite, such substitutions are rare, resulting in a low CEC typically ranging from 5 to 10 meq/100 g, which limits its reactivity compared to smectites' CEC of 80–150 meq/100 g. The surface chemistry of tubular halloysite arises from its rolled morphology, creating distinct inner and outer surfaces with opposing charges. The internal lumen is lined with aluminol (Al-OH) groups that confer a positive charge, particularly at neutral to acidic , while the external surface features (Si-O-Si) groups that impart a negative charge across a broad range. This charge asymmetry enables selective adsorption, with the positively charged lumen favoring anions and the negatively charged exterior attracting cations. Halloysite exhibits pH-dependent surface charge behavior, reflected in its , with an (IEP) around 4–5 where net charge is zero. Below the IEP, the surface becomes positively charged due to of aluminol and groups; above it, leads to negative charge dominance. Chemically, halloysite is stable in acidic conditions, resisting dissolution in dilute to moderate acids like HCl, but it dissolves in strong bases such as concentrated NaOH or KOH, where aluminosilicate bonds hydrolyze. This stability profile stems from its kaolinite-like composition, making it suitable for applications requiring acid resistance but vulnerable to alkaline environments.

Crystal Structure

Layer Arrangement

Halloysite possesses a 1:1 phyllosilicate layer structure, consisting of a single tetrahedral sheet of composition SiO₄ linked to a single octahedral sheet of composition Al(OH)₃ through shared apical oxygen atoms. The tetrahedral sheet features corner-sharing SiO₄ tetrahedra arranged in hexagonal rings, while the octahedral sheet comprises edge-sharing Al(OH)₆ octahedra with dioctahedral occupancy, where only two-thirds of the sites are filled by Al³⁺ cations. This bonding via apical oxygens creates a fundamental layer approximately 0.72 nm thick, characteristic of the kaolinite group minerals to which halloysite belongs. The layers in halloysite are stacked in an alternating sequence, primarily held together by weak van der Waals interactions supplemented by hydrogen bonds between the hydroxyl groups of the octahedral sheet in one layer and the basal oxygen atoms of the tetrahedral sheet in the adjacent layer. These interlayer forces result in a basal spacing of about 0.72 nm in the dehydrated form, with stacking often exhibiting some disorder or regular displacements (such as t₁ and t₂ vectors) that contribute to the overall . In the dehydrated state, the hydrogen bonding is particularly crucial for maintaining cohesion between layers, preventing under normal conditions. A defining feature of halloysite's layer arrangement is the intrinsic slight arising from the dimensional misfit between the tetrahedral and octahedral sheets, where the tetrahedral sheet is slightly larger than the octahedral sheet. This mismatch, on the order of 1-2%, induces strain that is accommodated by minor rotations in the tetrahedral sheet or by layer , distinguishing halloysite from strictly planar arrangements. In comparison to , halloysite shares the identical 1:1 layer composition and bonding scheme but exhibits greater propensity for structural strain due to this misfit, which in halloysite promotes rolling of the layers into tubular forms rather than the flat, pseudo-hexagonal plates typical of kaolinite. While kaolinite compensates for the misfit primarily through tetrahedral rotations to achieve planarity, the persistent strain in halloysite leads to a more dynamic layer arrangement conducive to morphological variations.

Tubular Morphology

Halloysite's distinctive tubular morphology results from the spontaneous rolling of its fundamental layers into cylindrical nanotubes, driven by lattice strain caused by the mismatch between the adjacent tetrahedral silica and octahedral alumina sheets. This intrinsic misfit in the sheet dimensions and bonding configurations generates tensile stress that favors over a planar , with the octahedral sheet forming the inner wall of the tube to minimize energy. The rolling typically produces multilayered cylinders comprising 15-40 layers in the wall, resulting in robust, open-ended nanotubes that distinguish halloysite from its platy counterpart. The dimensions of these nanotubes vary by deposit but generally feature a wall thickness of 10-20 nm, corresponding to the stacked layers, an inner lumen of 10-40 nm, an outer of 40-70 nm, and lengths ranging from 0.5 to several microns. This nanoscale architecture provides mechanical stability while maintaining accessibility at both ends of the tube. The hydrated 10 form of halloysite, with its interlayer molecules, supports and stabilizes the rolled configuration more effectively during formation, promoting tighter and more consistent tubular habits. Upon , halloysite transitions to the 7 form, where loss of the interlayer contracts the layer spacing from approximately 10 to 7 ; the tubular shape largely persists. Scanning microscopy (SEM) and (TEM) are essential techniques for visualizing and confirming the tubular habit, revealing the cylindrical or prismatic cross-sections and distinguishing halloysite's rolled morphology from the flat, pseudohexagonal plates of through high-resolution imaging of wall layering and lumen voids.

Formation and Occurrence

Geological Formation

Halloysite primarily forms through hydrothermal alteration of minerals such as feldspars and under low-temperature conditions ranging from 50 to 200°C, where circulating hot waters facilitate the dissolution and recrystallization of parent materials into tubular clay structures. This process often occurs along faults or joints in volcanic or granitic rocks, involving the leaching of silica and bases in silica-enriched environments, leading to pseudomorphic replacement of the original minerals. The resulting halloysite is typically hydrated and exhibits a 10 Å basal spacing due to interlayer incorporation during formation. In surficial weathering environments, halloysite develops via the intense chemical breakdown of aluminosilicates in soils, particularly through the leaching of soluble bases like and sodium, followed by partial silica removal, which is favored in tropical and subtropical climates with high rainfall and good drainage. This pedogenic process transforms primary minerals such as feldspars or into secondary clays, with continuous water availability preventing dehydration and promoting the hydrated form of halloysite over . Acidic conditions, often enhanced by organic acids from decaying , accelerate the dissolution and maintain low levels (typically below 8) that stabilize the mineral's interlayer hydration. Secondary formation of halloysite occurs in sedimentary settings as an alteration product of pre-existing clays like , where fluctuating fluid chemistry in wet but periodically drying environments allows for the intercalation of molecules and structural reorganization. These transformations take place over geological timescales, spanning thousands to millions of years, influenced by sustained flow, gradients, and activity that control the rate of leaching and precipitation. In such contexts, halloysite often neoforms directly from or other silicates in lagoonal or tidal-flat deposits, preserving its tubular morphology through environmental stability.

Global Deposits

Halloysite deposits occur worldwide in diverse geological settings, primarily as residual accumulations from the in-situ of parent rocks such as rhyolites and feldspar-rich volcanics, sedimentary layers in beds and marine environments, and hydrothermal veins formed through alteration by hot, silica-rich fluids. These deposit types influence the mineral's purity and morphology, with residual and hydrothermal origins often yielding higher concentrations of tubular halloysite compared to sedimentary ones. Global reserves are estimated in the tens of millions of tons, though economically viable high-purity deposits (with nanotube content ranging from 10% to over 90%) are more limited, concentrated in specific regions. Global halloysite production exceeds 82,000 metric tons annually as of 2025. In , some of the highest-purity halloysite deposits are found in the , particularly at Matauri Bay, where residual of volcanic rhyolites has produced clays with up to 50% halloysite content and prominent nanotube structures suitable for advanced applications; annual production reached approximately 80,000 tons (as of the early 2010s). China's extensive reserves, primarily in sedimentary and residual kaolin formations, include significant halloysite occurrences in provinces like ( area, yielding 50,000 tons annually) and (Dafang), with overall kaolin resources exceeding 4 billion tons, of which halloysite constitutes notable portions in high-purity masses crystallized from aluminum- and silicon-rich solutions. In the United States, the Dragon Mine in Utah's Tintic district hosts one of the largest high-purity deposits, a hydrothermal vein system replacing with up to 100% halloysite and nanotube content over 90%, with historical production of nearly pure halloysite exceeding 750,000 metric tons (1931-1962); recent estimates (as of ) indicate remaining reserves of approximately 501,200 tons of ore containing 64% halloysite, and small-scale production continues intermittently as of 2023. Industrial-grade deposits in , derived from residual of in the bauxite region, contribute to broader kaolin reserves surpassing 0.5 billion tons, though with lower tubular proportions around 10-30%. Australia's major halloysite resources are located in the Eucla Basin of , featuring sedimentary deposits with exceptional purity up to 95% and high nanotube yields from Cenozoic marine sediments, alongside smaller residual occurrences in like Burracoppin. In , halloysite is prevalent in the Amazon Basin's sedimentary kaolin deposits along the Capim and Jari Rivers, formed from weathered granitic rocks, accounting for 90% of the country's kaolin production (over 2 million tons annually) with halloysite-kaolinite mixtures typically at 20-50% nanotube content, though pure tubular forms are less common. Indonesia's halloysite is associated with volcanic residual soils in regions like and , where hydrothermal and weathering processes in pyroclastic deposits yield halloysite-rich clays, but large-scale commercial reserves remain underdeveloped compared to other areas. Other notable deposits include Turkey's hydrothermal sites in (high-purity, 95%, with 50,000 tons reserves) and Poland's Dunino sedimentary deposit, with measured resources of approximately 471,000 tons (as of 2019) and typical purity requiring processing for industrial use.

Applications

Industrial Uses

Halloysite, a kaolin-group valued for its whiteness, plasticity, and , finds established applications in several bulk industrial sectors. Its high alumina content (typically >30 wt%) and fine make it suitable as a functional additive, enhancing material properties without requiring nanoscale modifications. Primary uses include ceramics production, manufacturing, and oilfield operations, where it serves as a cost-effective extender and improver of performance metrics. In the ceramics industry, halloysite is incorporated as a key ingredient in and formulations to improve whiteness, mechanical strength, and firing behavior. Due to its similar molecular structure to , it blends seamlessly with other clays, contributing to translucency in high-end and tiles while reducing shrinkage during . For instance, beneficiated halloysite from deposits like those in is used in premium production, where it enhances aesthetic qualities and durability. Halloysite serves as an extender and filler in the paper and coatings sectors, where it boosts opacity, receptivity, and surface smoothness. In paper production, it is added to coatings (up to 10-15% by weight) to achieve higher levels (around 90% ISO) and better print quality, particularly in glossy magazines and . Its low absorption and fine particle distribution (predominantly <2 μm) prevent excessive thickening during application, making it preferable over coarser kaolins in some formulations. In industrial coatings, halloysite acts as a pigment extender, improving hiding power and weather resistance in architectural paints. In the oil and gas industry, halloysite is utilized in drilling fluids to control viscosity, stabilize borehole walls, and mitigate lost circulation. As a non-swelling clay alternative to , it provides shear-thinning properties that facilitate efficient cuttings removal while minimizing formation damage in water-sensitive formations. Typical formulations include 5-20% halloysite by weight in water-based muds, enhancing fluid stability under high temperatures (up to 150°C). Its tubular morphology aids in sealing micro-fractures, reducing fluid loss rates to below 10 mL/30 min in API tests. Additional traditional applications include halloysite as an absorbent in cat litter products, where its porous structure enables effective odor control and clumping, and as a reinforcing filler in rubber and plastics to improve tensile strength and abrasion resistance. Historically, purified halloysite has been used as a white pigment in paints and inks, leveraging its high refractive index for better coverage. In rubber compounding, loadings of 10-30 phr enhance modulus without significantly increasing viscosity, suitable for tire sidewalls and conveyor belts. Industrial processing of halloysite involves beneficiation techniques such as selective mining, dispersion in water, grinding to liberate fine particles (<10 μm), and classification via sedimentation or hydrocyclones to isolate tubular fractions from quartz impurities. Dry grinding is avoided when possible to preserve morphology, with wet attrition mills used instead to achieve 80-90% recovery of high-purity clay (>95% halloysite content). This processed material is then dried, calcined if needed for reactivity, and packaged for end-use.

Emerging Nanotechnological Uses

Halloysite nanotubes (HNTs) are increasingly utilized in systems owing to their hollow tubular lumen, which enables efficient encapsulation of therapeutic agents for sustained and controlled release. Drugs such as antibiotics (e.g., gentamicin and ) and anticancer agents (e.g., , , and ) can be loaded via adsorption or intercalation into the lumen, with surface modifications like or APTES significantly enhancing loading efficiency (up to ~40 wt% reported for some drugs in modified systems). These systems have demonstrated , with low observed in cell lines up to concentrations of 1000 μg/mL, and kaolin-related clays like halloysite classified as (GRAS) by the FDA for oral applications, though nanomaterial-specific approvals for injection remain pending. In vivo studies, such as DSPE-HNTs loaded with , have shown tumor inhibition in mouse models without significant adverse effects. In nanocomposites, HNTs serve as reinforcing fillers in matrices, leveraging their high and surface area (~150 m²/g) to improve mechanical properties and impart retardancy. Incorporation of 5-30 wt% HNTs into 610, for example, enhances tensile strength by up to 30% and reduces peak heat release rate by 22% (from 743 to 580 kW/m²), achieving UL-94 V-0 ratings while lowering toxic gas emissions like CO₂. Similarly, bio-inspired surface-modified HNTs in composites boost and char formation, mitigating flammability without compromising structural . These enhancements stem from the nanotubes' ability to form interfacial bonds and act as barriers, making HNT-polymer hybrids suitable for automotive and applications. Recent 2024-2025 studies have further explored HNT nanocomposites for improved mechanical, , and barrier properties in and other matrices. For , HNTs excel as adsorbents for and dyes, capitalizing on their high surface area and selective inner/outer surface chemistry. Adsorption capacities reach 25-30 mg/g for Pb²⁺ and 7-10 mg/g for Cd²⁺ under optimized conditions ( 5.5, 25°C), with geographical variations in nanotube structure influencing performance. In dye removal, HNT-based photocatalysts degrade cationic pollutants like by ~40% under UV-Vis light in 100 minutes, outperforming bare systems by a factor of 4 due to charge-selective mechanisms. Modified HNTs, such as those functionalized with groups, further boost efficiency for oil spills and organic contaminants, offering eco-friendly alternatives to synthetic sorbents. Advances in 2025 have highlighted HNTs in catalytic degradation and pollutant removal. Post-2020 advances have expanded HNT applications to sensors, , and through targeted modifications. In sensors, HNT-kojic acid-Cu nanocomposites detect electrochemically with a 68 nM limit of detection and high selectivity in biological matrices, aiding diagnostics and . For , HNT-supported Co₃O₄ nanoparticles accelerate reduction, while sulfonic acid-functionalized HNTs yield 92% from in 2021 studies. In , HNT-embedded electrospun nanofibers enhance filter performance for air purification, with the global HNT market projected to grow at a 6.1% CAGR from USD 53.5 million in 2025 to ~USD 96.7 million by 2035 (as of October 2025), driven by nanotech demand. Recent 2024 reviews emphasize structure-bioactivity relationships for expanded biomedical uses. Despite these progresses, challenges persist in , as uniform nanotube dispersion requires advanced processing, and assessments reveal at high doses (>50 mg/kg) in mice, necessitating further studies for long-term safety. Nonbiodegradability also limits intravenous uses, underscoring the need for biodegradable coatings to broaden clinical translation.

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