Fe2O3 Review: Nanostructure, Synthesis Methods, and Applications

 

Novita1, Ramlan2, Marzuki Naibaho3, Masno Ginting4, Syahrul Humaidi5, Tulus Na Duma6

Department of Physics, Universitas Sumatera Utara, Indonesia1,5,6

Department of Physics, Universitas Sriwijaya, Indonesia2

Research Center for Advanced Materials, National Research, and Innovation Agency (BRIN), Indonesia3,4

Email: [email protected]1, [email protected]2, [email protected]3, [email protected]4, [email protected]5, [email protected]6

Keywords

 

ABSTRACT

 Fe2O3, Nanostructures, Synthetic Methods, Applications.

 

Iron sand, which contains magnetite iron ore, exhibits unique magnetic properties when exposed to magnetic fields. Iron ore content, including α-Fe2O3, FeTiO3, Magnetite (Fe3O4), and others, provides potential uses in various industries such as electronics, energy, chemical, ferrofluids, catalysts, and biomedicine. The location of the discovery of iron sand can affect its mineral characteristics and geological conditions. This research aims to develop innovative synthesis methods to produce hematite nanomaterials from iron sand. Nano-size hematite nanoparticles exhibit unique characteristics, including an increase in specific surface area that is beneficial in applications such as gas sensors, catalysts, lithium-ion batteries, and the manufacture of permanent magnets. Through a literature review, this article presents comprehensive insights into the characteristics of iron sand, variations in synthesis methods, and the structure of hematite nanoparticles. Applications of hematite nanoparticles in water treatment, catalysis, and energy storage are also detailed. This article is expected to contribute to the development of innovative nanomaterial technologies as well as explore the potential of iron sand resources for wider industrial applications.

 

 

INTRODUCTION

Iron sand is one type of sand containing magnetite iron ore. The iron ore content in this sand gives it unique properties in the form of magnetic properties. When exposed to external magnetic fields, iron sand can exhibit magnetic behavior and even attract metal objects. This phenomenon makes iron sand not only an object of geological exploration, but also a valuable resource in industrial contexts such as, electronics, energy, chemistry, ferrofluids, catalysts, and biomedicine (Aziz, 2021; Basavegowda et al., 2017; Fatih et al., 2021; Mulyani et al., 2022; Nengsih et al., 2023; Puspitaningrum et al., 2017; Susilawati et al., 2018; Tadic et al., 2021; Widodo et al., 2020).

Iron sand contains various magnetic minerals such as α-Fe2O3, FeTiO3, SiO2, Magnetite (Fe, Maghemite) γ-Fe2O3, Alumina (Al2O3), and Rutile (TiO2). Iron sand can also contain impurities such as clay, non-metallic minerals, or organic material. Iron sand generally has a black or dark brown color, reflecting a significant magnetite content. The size and shape of iron sand grains can vary this is due to deposition processes such as erosion or transport by water. The characteristics of iron sand may vary depending on the mineral composition and geological conditions in which iron sand is found Kandungan Senyawa Ki (Abdel-Karim & Barakat, 2017; Ibrahim et al., 2022; Tan et al., 2024).

Iron sand can be found in various locations around the world. Iron sand mines are often located in coastal areas, rivers, or lakes that are places of deposition of sedimentary material. In its use, iron sand found in nature needs to be synthesized first to produce pure hematite content (Sismanto et al., 2019).

Current research highlights an innovative synthesis method that can produce nanomaterials from pure hematite. Hematite in the nanoscale has shown unique and distinct characteristics compared to its bulk form. With nanosize, the specific surface area of hematite can increase significantly while maintaining its magnetic properties. The wider surface provides benefits in a variety of applications such as gas sensors, catalysts, lithium-ion batteries, and pigments, and can also be utilized in the manufacture of permanent magnets (Kiswanto et al., 2023; Meijer & Rossi, 2021).

By reviewing the latest literature and research, this review article will compile a comprehensive understanding of the characteristics of iron sand based on the location of its discovery, explore various methods that can be used to produce hematite nanoparticles, and decipher the structure of hematite nanoparticles. Various applications of hematite nanoparticles will also be discussed to determine their development. This article is expected to provide new insights into the potential of iron sand resources and contribute to the development of innovative nanomaterial technologies.

 

METHODS

This literature research method review will begin by investigating the various literature sources that have been presented to understand the characteristics of iron sand based on the location of its discovery. Consideration will be given to the content of magnetic minerals and impurities in iron sand, as well as variations in grain size and shape affected by the deposition process. Next, research will focus on innovative synthesis methods to produce hematite nanomaterials from iron sand. The analysis will cover the unique characteristics of hematite at the nanoscale, with an emphasis on increasing the specific surface area and maintaining its magnetic properties. This article will compile a comprehensive understanding of the structure of hematite nanoparticles and present various applications of hematite nanomaterials, such as gas sensors, catalysts, lithium-ion batteries, and permanent magnet manufacturing. This literature review is expected to provide new insights into the potential of iron sand resources and contribute to the development of innovative nanomaterial technologies, especially in the context of water treatment, catalysis, and energy storage.

 

RESULTS

Coastal Areas

Coastal areas are known as places where the process of material deposition by seawater occurs. The deposition of material by seawater will affect the concentration of iron minerals. Therefore, iron sand in coastal areas has a high iron content. In addition to iron minerals, iron sand in coastal areas can also contain additional minerals such as ilmenite, magnetite, or other metal minerals. Comparison of iron sand characteristics of coastal areas in Indonesia can be seen in Table 1 (Bahfie, 2022; Kotarumalos et al., 2023).

Iron sand in coastal areas occurs due to rocks containing iron minerals eroded by sea waves and carried to the coast. In addition, the process of weathering and erosion also plays a role in forming iron mineral particles that are free from the original rock. The accumulation of iron sand along the coast or coastline occurs with the help of tides (Setiady et al., 2020).

 

Table 1. Comparison of iron sand characteristics of coastal areas in Indonesia

Location Name

Dominant Minerals

Additional Minerals

Physical, Mechanical, and Chemical Properties

Reference

Sunur Beach, West Sumatra

Magnetite, Hematite, and Ilmenite

Quartz, and anapit

Magnetic granules are large, multidomain, and mineral growth modes form lamellae.

(Fatni Mufit et al., 2006)

South Coast of West Java

Magnetite, Hematite

Silicon, Graphite, Clinoferrosilite

Not explained further

(Setianto et al., 2017)

Sampulungan Beach, South Sulawesi

Magnetite

Titanium, Chromium, Vanadium, and Manganese

It is ferrimagnetic, multidomain magnetic grain, and fine magnetic fraction.

(Tiwow et al., 2018)

Keumumu Beach, Aceh

Magnetite

Silica, Calcium, Aluminum, Potassium, and Titanium

The sand fraction is very fine, rounded and well rounded.

(Purnawan et al., 2018)

Puntaru Beach, East Nusa Tenggara

Magnetite

Aluminum, Silica, and Potassium

Softmagnetic, and ferrimagnetic

(Karbeka et al., 2020)

Ivory Coast, East Nusa Tenggara

Magnetite, and Hematite

Aluminum, Silica, Potassium, and Titanium

Not explained further

(Fithriyani et al., 2018)

North Coast, Central Java

Hematite, maghemite

Titanomagnetite, and titanohematite

Fine grain, and pseudo-single domain (PSD)

(Yulianto et al., 2003)

Kata Beach, West Sumatra

Hematite

Carbon, Aluminum, Silica, Calcium, and Manganese

Black, Difficult to reduce, and softmagnetic.

(Rianna et al., 2018)

 

River

Iron sand in rivers generally has varying grain sizes, depending on the process of transportation and deposition by water. The size of sand grains in rivers is usually smaller than the size of sand grains in coastal areas. This can occur due to the process of transportation by water until it arrives at the river can break the grain. The color of iron sand in rivers can vary, but usually has a brighter color than the color of iron sand in coastal areas (Didik et al., 2020; Nugroho & Basit, 2014).

Iron sand is often unevenly distributed along river flows due to the deposition process. The deposition process can lead to the deposition of iron sand in certain areas such as, river bends and prominent plains along the flow. In addition, strong river currents can transport and precipitate different iron particles in different parts of the water flow. The iron sand content in the river has impurities such as clay, non-metallic minerals, or organic material (Kamiludin et al., 2016).

 

Table 2. Comparison of the characteristics of river iron sand in Indonesia

Location Name

Dominant Minerals

Additional Minerals

Physical, Mechanical, and Chemical Properties

Reference

Batang Kuranji River, West Sumatra

Albite, magnetite

Quartz, halloysite, saponite, and pyrophyllite

Ferromagnetic minerals

(Afdal &; Niarti, 2013)

Central Lampung

Ilmenite, and Potassium Chloride

Not explained further

Antiferromagnetic

(Puspitarum et al., 2019)

Tor River, Papua

Magnesioferrite

Augit-aluminian

Magnetization is high saturation, and coercive field is low.

(Togibasa et al., 2018)

Sompang River, East Lombok

Silica

Aluminum, Carbon, Sodium, and Potassium

It is finely grained, and has a smaller size than river sand

(Meiliyadi et al., 2022)

Bah Bolon River, North Sumatra

Magnetite, Hematite, and Maghemite

Titanium, Aluminum, Copper. Manganese, Silica, Vanadium

It is soft magnet, and high saturation.

(Novita et al., 2023)

 

Based on research that has been done, the mineral content in iron sand in rivers has a more unique diversity than the mineral content in iron sand in coastal areas. This can occur because the iron sand in the river has mixed with various minerals during the transportation process by water.

Hematite Nanostructure (α-Fe2O3)

Hematite (α-Fe2O3) has properties that are difficult to corrode so it is suitable for applications such as gas sensors, catalysts, lithium-ion batteries, and pigments, it can also be used in the manufacture of permanent magnets. At high temperatures, the α-Fe (Edianta et al., 2021; Gandha et al., 2016; Miftahul Khoiroh et al., 2013; Rostami et al., 2021; Suhendi et al., 2021; Susilawati et al., 2022). (hematite) phase is the most stable phase compared to other phases. This crystal structure is rhombohedral (trigonal) with a crystal type such as corundum (α-Al2O3), has a space group "R-3 c" lattice parameters a = b = 5.036 Å, c = 13.747 Å, α= = 90° (Figure 1). It is antiferromagnetic under ~260 K (Morin transition temperature), and weak ferromagnetic between 260 K and 950 K (Neel temperature). Many factors, such as pressure, particle size, and magnetic field intensity influence its magnetic properties. Fasahematite has curie temperatures above 800 ºC and below 1000 ºC (Song & Pistorius, 2019).

Figure 1.  (a) Corundum structure of hematite (α-Fe2O3); (b) Rhombohedral shape of hematite crystal lattice (α-Fe2O3)

To produce α-Fe 2O3 nanoparticles is carried out using several methods, including the sol-gel method, from which the particle size of α-Fe2O3  between 10 – 20 nm, the hydrothermal method with a particle size of 30 nm, the ball miling method, with a particle size of 99.14 μm  – 93.34 μm, and the coprecipitation method, with a particle size of 22.8899 nm (Dewi & Adi, 2018; Fahlepy et al., 2019; Gandha et al., 2017; Malik & Putra, 2018; Tadic, Panjan, et al., 2019)

Various nanostructures have been studied on hematite by varying the synthesis process. The nanostructures formed during the synthesis and fabrication process also depend on different factors such as synthesis methods, types of precursors, stabilizers, substrates, and not to mention their parameters, for example, temperature and time variations in the synthesis process. Nanostructures are useful for a wide range of applications due to their unique structure and optical and electrical behavior. The nanostructure of α-Fe2O3is nanorods, as shown in Figure 2, micro-cubes, nanowires, nanotubes, nanoflakes, flower-shaped hematite, nanoparticles, and nanorod arrays (W. R. W. Ahmad et al., 2017, 2019; Atabaev, 2015; Emi̇L-Kaya et al., 2022; Gurudayal et al., 2014; X. Li et al., 2015).

Figure 2. Nanostructure of α-Fe2O3; (a) microcubes, (b) nanowires, (c) nanotubes, (d) nanoflakes, (e) nanorods, (f) microstructure orientation, (g) sea-urchin shaped, and (h) worm-shaped.

Hematite nanostructure synthesis

Coprecipitation

Iron sand is separated by impurities using neodymium magnets. The result is then dissolved into HCl, with the reaction:

Fe2O3 + 6HCl2FeCl3 + 3H2O

 

Stirred and heated at 80oC using a magnetic stirrer at a speed of 350 rpm for 2 hours. Precipitation is carried out by dripping ammonium hydroxide (NH4OH) dissolved to pH 6 and forming a precipitate by the reaction:

2FeCl3 + 3H2O + 6NH4OH 2Fe (OH)3 + 6NH4Cl + 3H2O

 

The resulting precipitate is washed with equates and dried in a memmert oven at 100°C for 19 hours, with the reaction:

 

2Fe (OH)3+6NH4OH+3H2O→ 2FeOOH+6NH4Cl+5H2O

 

The dried sample is ground and then calcined. The synthesis process using the coprecipitation method can be seen in Figure 3. The weakness of the coprecipitation method is that the grain size distribution of nanoparticles tends to be large, as well as the polydisversiveness of small particles. Nanoparticles are easily agglomerated the synthesis of nano-hematite using the coprecipitation method has been reported in various studies. A comparison of the results of each study that has been conducted can be seen in Table 3.

 

https://ars.els-cdn.com/content/image/1-s2.0-S2214785321015704-ga1_lrg.jpg

Figure 3. Flow of the coprecipitation method(Kushwaha &; Chauhan, 2021)

 

Table 3. Comparison of research results using the coprecipitation method

Coprecipitation Variation

Particle Size and Shape

Physical, Mechanical, and Chemical Characteristics

Influence of Process Parameters

Ref.

FeCl precursor3and NH4OH precipitator

Hexagonal crystal structure, polygonal morphology, average particle size 10-25 nm. The surface area of the particle is about 17.937 m2/g.

The average pore diameter is 85.67 nm, and the total pore volume is 0.2699 cm3/g. It has a band gap of 1.8 eV.

This method promises to narrow the band gap in the iron oxide system.

(Parvathy Namboothiri &; Vasundhara, 2023)

FeCl precursors3and NaOH precipitators

The crystal measures 41.7 nm, the average particle size of 50-150 nm is spherical.

Agglomeration occurs, and it is chemically stable.

Temperature affects the formation of nanophases.

(Gobinath et al., 2015)

FeCl precursor3and NH4OH precipitator

The rhombohedral/hexagonal crystal structure measures 16-44 nm.

Agglomeration occurs, has seven phonon modes, crystals are formed at low temperatures.

The concentration of precursors affects the size, crystallinity, morphology, and formation of clots.

(Fouad et al., 2019)

FeCl precursor3and NH4OH precipitator

The particles are 30 nm in size, shaped like a ball with the formation of clusters, hexagonal crystal structure.

Bandgap energy 2.58 eV.

Nano-hematite powder has a uniform size when calcined at 500oC.

(Farahmandjou &; Soflaee, 2015)

FeCl precursor3and NH4OH precipitator

The smallest particle size is 21 nm, spherical.

It has a band gap of 2.09 eV.

An increase in the concentration of precursors leads to an increase in nanoparticle size.

(Lassoued et al., 2017)

 

Gel Insoles

The sol-gel method is a synthesis method that requires chemical engineering. The term sol-gel comes from two words, namely: 1) sol refers to a precursor solution that will be used as the starting material for the synthesis of Fe2O3 nanoparticles; and 2) gel refers to the form of the final product of synthesized nanoparticles in the form of gels. The sol-gel method is commonly used to synthesize ceramic materials and is not suitable for synthesizing oxide nanoparticles, so additional modifications are needed in using this method. The sol-gel method is a chemical method that has a complex procedure. Many synthesis parameters must be observed (Indrayana, 2019).

 

Table 4. Process Parameters of Gel Soles

Process Stages

Process Objectives

Process Parameters

Chemical Solutions

Forming Gels

Precursor type, Solvent type, Water content, Precursor concentration, Temperature, and pH

Aging

Let the gel sit to change properties

Time, Temperature, Fluid composition, Aging environment

Drying

Removing water from the gel

Drying method (ovaporative, supercritical, and freeze drying), Temperature, Pressure, Time

Calcining

Changes the physical/chemical properties of solids, often resulting in crystallization and densification

Temperature, Time, Gas (inert or reactive)

 

The sol-gel method has several disadvantages, namely: 1) it produces a lot of alcohol during the calcination process, 2) it requires additional heat treatment at high temperatures, and 3) the nanoparticle permeability is high, and the bonding power of nanoparticles is weak (Koo et al., 2019)

Hydrothermal

Hydrothermal is formed from the words hydro which means water and thermal which means heat. So the hydrothermal method is a method that uses water and heat whose properties convert solutions into crystals. The hydrothermal method must be performed in a closed system to prevent solvent loss when heated above its boiling point (Jung et al., 2018; Noviyanti et al., 2012; Ou et al., 2018; Qiongyu Li, 2018a; C. Wang et al., 2018; W. Wang et al., 2018; G. T. Zhu et al., 2018).

Hydrothermal synthesis is widely used in the manufacture of metal oxides. Metal oxide synthesis can occur in two stages. The first stage is hydrolysis of the salt solution to produce metal hydroxide. The second stage is that the hydroxide will be dehydrated to produce the desired metal.

Water is the most effective solvent in dissolving ionic compounds at high temperatures and pressures. Water can also act as a pressure transmission and as a precursor solvent, so the resulting powder can be amorphous or crystalline. The advantages of the hydrothermal method include being able to produce crystalline products that can be achieved at low enough temperatures with a high degree of crystallity, can reduce agglomeration between particles, can produce a relatively uniform particle size distribution, high product purity, relatively cheaper, directly formed powder from solution, shape and particle sizes can be controlled from the initial material and different hydrothermal conditions,  The reactivity of the resulting powder is high, and allows the synthesis of compounds that have oxidation numbers that are difficult to obtain, especially transition groups (Colombo et al., 2015; Fulle et al., 2018; Zarringhadam & Farhadi, 2018).

In addition, hydrothermal also has a drawback, that is, the initial solubility must be known, hydrothermal slurry is corrosive, and the use of high-pressure vessels will be dangerous in case of accidents (Mercier et al., 2018; D. F. Putri et al., 2019).

 

https://ars.els-cdn.com/content/image/1-s2.0-S0022369720302705-fx1_lrg.jpg

Figure 4. The process of synthesis of hydrothermal methods with various precursors( Kongsat et al., 2021)

 

Good crystals can be obtained by adding a mineralizer. Mineralizer serves to increase the polarity of water to increase the solubility of a dissolved substance. Compounds used as mineralizers should not be seen in reactions, and commonly used compounds are alkaline bases, NaOH, and KOH (Noviyanti et al., 2018).

 

Table 5. Comparison of research results using hydrothermal methods

Hydrothermal Variations

Particle Size and Shape

Physical, Mechanical, and Chemical Characteristics

Influence of Process Parameters

Ref.

Anionic, cationic, and nonionic surfactants. Temperature 180oC.

Spherical particle shapes with a diameter ranging from 15-205 nm.

Single-domain magnetic behavior, coercivity of 225 Oe, high stability, and thermal conductivity of 0.4787 W/mK.

The type and concentration of surfactants can affect the colloidal stability and thermal stability of nanoparticle suspensions.

(Kongsat et al., 2021)

PVP surfactants and NaAc precipitants.

Temperature 200oC.

The average particle size is 40 nm with a spherical shape.

The highest capacitance is 340.5 F/g at a current density of 1 A/g, remanent magnetization is 0.02 emu/g, coercivity is 66.8 Oe, and a long cycle life.

The concentration of the precursor affects the quality of the size and dispersion of the resulting hematite

(M. Zhu et al., 2012)

Fe sulfate heptahydrate solution Fe2 (SO4)3.7H2O

Temperature 160oC.

Spherical in shape, and the average size is 8 nm.

It is superparamagnetic with blocking temperature T B = 52 K and irreversibility temperature T irr = 103 K. Magnetization Ms = 3.98 emu/g and magnetic moment mp = 657 B.

The magnetization properties of hematite nanoparticles are influenced by the crystallinity and surface of the nanoparticles.

(Tadic et al., 2014)

Fe (III) nitrate solution.

Temperature 100oC.

The average particle size is 20-60 nm.

A low pH produces a positive potential value, while a pH of 7 produces a negative value

The size of the synthesized particles increases with the reaction time. Particle size affects colloidal behavior to absorption and aggregation processes.

(Colombo et al., 2015)

Hierarchical nanostructures with various glycine-free and glycine-assisted morphologies.

The diameter of the particles is on average 20-80 nm, spherical in shape.

Ferromagnetic, coercivity Hc = 3725 Oe.

Glycine in hydrothermal reactions can increase the coercivity value up to 3 times.

(Trpkov et al., 2018)

Precursors of iron and sodium acetate.

Temperature 180oC.

The size of 50 nm irregular nanoparticles, such as plates with a thickness of 10 nm and a diameter of 50-80 nm, a 3D ellipsoid with a length of 3.5 nm and a diameter of 1.5 m

Coerciveness of irregular nanoparticles Hc = 73 Oe, nanoplates Hc = 689 Oe, and 3D ellipsoid Hc = 2688 Oe. Indicates a low level of cytotoxicity.

The anisotropic form influences the increase in coercivity in hematite nanoplates, their structure and morphology.

(Tadic, Trpkov, et al., 2019)

 

Sonication

The sonication method is the easiest and most effective method for large-scale production with precise size control, high morphology, and crystallinity. In research using ultrasonic sonochemical methods obtained polyhedron monodispersa hematite nanoparticles with uniform shape, particle size of about 14nm at a temperature of 500oC (Khalil et al., 2017). Shock waves in the sonification method can separate the agglomeration of a particle (agglomeration) and due to the influence of sonification (ultrasonic) can produce nanoscale crystal sizes. This method uses ultrasonic bath with high frequencies such as 20 kHz - 10 MHz to break down metal ions in molecules so that it is expected that the crystal growth process can take place quickly and can avoid oxidation of metal ions resulting in the formation of amorphous particles (Candani et al., 2018; Firnando & Astuti, 2015).

Figure 5. Synthesis process sonication method(Fuentes-García et al., 2020)

 

Applications of Hematite (α-Fe2O3) Nanoparticles

Hematite nanoparticles (α-Fe2O3) have potential applications in various fields of advanced nanotechnology, such as electronics, optical devices, photonics, and microwave absorbers. Much research has focused on hematite nanoparticles (α-Fe2O3) both undoped and doped as solar photoelectrochemical cell (PEC) materials (Bai et al., 2022; Dhiman et al., 2020; Kamil et al., 2022; Y. Li et al., 2021; Silva et al., 2020).

Hematite nanoparticles (α-Fe2O3) are also suitable for photocatalytic applications because they are environmentally friendly, cost-effective, and have chemical stability over a wide pH range. The size of the diameter and porosity of the hematite nanorod (ALP, 2023; S. A. Putri et al., 2021; Suchi Ramadhani Putri et al., 2022). α-Fe2O3 also affect the magnetization properties. Furthermore, hematite nanorods (α-Fe2O3) (Rifai et al., 2021; S., 2019; Simbolon et al., 2021; Sinuhaji et al., 2021) are also applied to gas sensors and Lithium-ion batteries, where it has been proven that the working principle of electrochemical and gas sensors is highly dependent on the size of the diameter and surface area of the Branauer Emmet-Teller (BET) (A. Ahmad et al., 2019; Hung et al., 2016; Indra & Noerochim, 2016; Liu et al., 2020; Ma et al., 2020; Qin et al., 2022).

Hematite nanoparticles (α-Fe2O3) can also be applied as microwave absorbers on aircraft walls. By utilizing the potential of natural sand in East Java, a prototype of a microwave absorbing coating based on Mhexaferite BaFe12-xZnxO19 has been successfully made, by making it a coating for paint composite materials on the interior walls of the aircraft. The use of hematite nanoparticles as microwave absorbers is also supported by the results of research conducted by Rianna et al using natural iron sand (Efhana et al., 2013; Rianna et al., 2023).

Barium hex ferrite is an ideal material to dampen electromagnetic interference (EMI) caused by malfunctions in electronic equipment. One of the ingredients for making Barium hexaferrite is hematite (α-Fe2O3) (Susanto et al., 2014). Barium hexaferrite has been widely studied because it has many advantages, including its relatively cheap price, high curie temperature, resistance to corrosion, good physical properties, and its manufacture is relatively easy (Dermayu Siregar & Humaidi, n.d.; Hayati et al., 2016; Widanarto et al., 2015).

Hematite nanoparticles as water and sewage treatment have been reported in research by Kefeni et al. Based on the research that has been done, hematite nanoparticles have succeeded in removing Al, Mg, Mn, Zn, Ni, Ca, and Na metals. The adsorption and precipitation properties possessed by hematite can help in the process of cleaning water from heavy metals and other solutes. This is also reinforced by the findings of Aal et al which show that hematite nanoparticles can absorb Cu, Ni, Co, Cd, and Pb ions (Abd El Aal et al., 2019; Kefeni et al., 2018).

In the medical field, hematite nanoparticles also show no less unique abilities, one of which is their use as a delivery drug. Hematite nanoparticles can be coated with drug compounds to be then directed to specific locations in the body using external magnetic fields. External magnetic fields can also generate heat through magnetic hysteresis in magnetic hyperthermia therapy to damage cancer cells. In addition, the unique magnetic properties that hematite nanoparticles possess can help in medical imaging techniques such as magnetic resonance (MRI) by increasing image contrast (Beato-López et al., 2020; Mabrouk et al., 2020; Pham et al., 2016; Surowiec et al., 2017).

 

Figure 6. Applications and methods of synthesis of hematite nanoparticles(Kokila et al., 2022)

 

CONCLUSION

Based on the literature that has been described, it can be concluded that iron sand can be further utilized in producing a variety of minerals, especially hematite. The characteristics of iron sand used can be influenced by the location where iron sand is found. In addition, the synthesis method plays an important role in determining the physical, mechanical, and chemical properties of hematite nanoparticles from iron sand. The structure of hematite nanoparticles, especially at the level of crystallinity and surface morphology has an impact on the performance and application of hematite nanoparticles. Hematite nanoparticles have demonstrated their capabilities in a wide range of applications, including water and environmental treatment, catalysts, and energy storage.

 

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Novita, Ramlan, Marzuki Naibaho, Masno Ginting, Syahrul Humaidi, Tulus Na Duma (2024)

 

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