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Azotobacter

Azotobacter is a of Gram-negative, aerobic, heterotrophic renowned for their ability to fix atmospheric non-symbiotically, converting dinitrogen gas into biologically available through the . These free-living soil microbes belong to the family within the class and are characterized by their pleomorphic morphology, ranging from rod-shaped to spherical forms measuring 1.0–3.8 μm, with peritrichous flagella enabling motility in most . Discovered in 1901 by Dutch Martinus Willem Beijerinck, who isolated the A. chroococcum, the comprises at least seven recognized , including A. vinelandii, A. beijerinckii, A. paspali, A. armeniacus, A. salinestris, A. nigricans, and A. chroococcum. Azotobacter species thrive in neutral to slightly alkaline soils (optimal 7.0–7.5) and aerobic environments, where they utilize carbon sources like glucose for energy while tolerating oxygen levels that would inactivate in other diazotrophs through rapid respiratory protection. To endure environmental stresses such as , high temperatures (up to 35°C), or limitation, they form thick-walled cysts—a dormant stage that enhances survival in diverse habitats including soils, sediments, water bodies, and plant rhizospheres. Ecologically, Azotobacter contributes 20–30 kg of fixed per hectare annually under optimal conditions, bolstering the global and supporting without relying on host plants. Beyond nitrogen fixation, Azotobacter exhibits multifaceted benefits in as a , producing plant growth-promoting substances such as (IAA), , and siderophores that enhance nutrient uptake, root development, and tolerance to abiotic stresses. These also solubilize phosphates, suppress pathogens through , and stabilize via exopolysaccharide production, leading to increases of 15–40% in various studies. Commercially, Azotobacter-based inoculants represent a sustainable alternative to synthetic fertilizers, with the global —including these products—valued at USD 2.53 billion in 2024, underscoring their role in promoting eco-friendly farming practices.

Taxonomy and Classification

Discovery and History

The Azotobacter was discovered in 1901 by Martinus Willem Beijerinck, who isolated the Azotobacter chroococcum from samples, marking it as the first identified free-living, aerobic bacterium capable of fixing atmospheric . Beijerinck's involved enriching suspensions in a nitrogen-free medium containing as the carbon source, followed by purification on solid media, which selectively promoted the growth of these oligonitrophilic microbes. This breakthrough expanded the known scope of biological beyond in roots, demonstrating that free-living organisms could independently convert N₂ into usable forms under aerobic conditions. In the early , subsequent studies refined isolation techniques for Azotobacter, building on Beijerinck's enrichment approach with serial dilutions in -free liquid media to obtain pure cultures from diverse . Confirmation of their -fixing ability relied on demonstrating biomass accumulation and total gains in closed cultures lacking combined , quantified via chemical analyses such as the , which measured and organic content. These methods established Azotobacter as robust diazotrophs, with researchers like Jacob G. Lipman describing additional , such as Azotobacter vinelandii in 1903 from , further validating the genus's widespread distribution and ecological role. Sergei Winogradsky advanced the understanding of Azotobacter in the 1930s through detailed morphological and ecological investigations, culminating in his publication on the genus's biology. Winogradsky confirmed the aerobic nature of in Azotobacter by studying its respiratory protection mechanisms against oxygen inactivation of , and he introduced the term "cysts" for its dormant, resistant forms, highlighting adaptations for survival in variable soil environments. His work emphasized simple carbon substrates like as natural energy sources, bridging microbiological classification from anaerobic fixers like Clostridium—which he had discovered in 1893—to aerobic, free-living ones. The identification of Azotobacter represented a pivotal shift in microbiological classification of nitrogen fixers, transitioning focus from obligatory symbiotic (e.g., Rhizobium) and anaerobic free-living forms to aerobic heterotrophs that thrive in oxygenated soils without plant hosts. This progression underscored the diversity of diazotrophic strategies, influencing and agricultural research by revealing non-symbiotic contributions to the .

Species and Phylogeny

The genus Azotobacter belongs to the family , order Pseudomonadales, and phylum , within the class . This classification reflects its position among aerobic, free-living nitrogen-fixing bacteria in the gamma-proteobacterial lineage, distinguished by their ability to form cysts and tolerate environmental stresses. Currently, the comprises seven recognized : A. armeniacus, A. beijerinckii, A. chroococcum (the , first described in 1901), A. nigricans, A. paspali, A. salinestris, and A. vinelandii (widely used as a for genetic studies), along with the A. chroococcum subsp. isscasi. These species are delineated primarily by differences in colony pigmentation, cyst formation, and growth optima, with A. chroococcum and A. vinelandii serving as reference strains in taxonomic validations. Phylogenetic relationships within Azotobacter have been elucidated through 16S rRNA gene sequencing, which clusters the tightly with other members and confirms its gamma-proteobacterial affiliation, showing sequence similarities exceeding 98% among species. Whole-genome sequencing has further refined these analyses, revealing conserved synteny in core genes while highlighting species-specific expansions in accessory genomes related to environmental adaptation. A 2025 pangenomic study of 30 strains across four Azotobacter species (A. chroococcum, A. vinelandii, A. beijerinckii, and A. salinestris) demonstrated substantial genetic diversity, with the comprising 18,267 genes, including core clusters for enzymes like (nifHDK) that are universally present yet vary in regulatory elements across species. This analysis underscores the genus's evolutionary plasticity, with accessory genes contributing to functional specialization in and stress response.

Biological Characteristics

Morphology and Reproduction

Azotobacter species are characterized by polymorphic cells that typically appear as rods or spheres, measuring 2–10 μm in length and 1–2 μm in width. Vegetative cells are often oval or coccoid and exhibit motility through peritrichous flagella, enabling movement in aqueous environments. These cells possess a large size relative to many , which supports their role in producing copious amounts of extracellular . A distinctive feature of Azotobacter is the formation of cysts, which serve as dormant, resistant structures developed under adverse conditions such as limitation or environmental . Each cyst arises from a single vegetative through a differentiation process that results in a spherical form with contracted and a thick, multi-layered wall. The cyst wall consists of an outer exine layer, which is rough and densely layered, and an inner intine layer, which is homogeneous and viscous, providing protection against and oxygen exposure. Within the central body of the cyst, (PHB) granules accumulate as a carbon reserve, while alginate, an exopolysaccharide, forms a critical structural component of the , enhancing resistance to drying. Reproduction in Azotobacter occurs asexually through binary fission, where vegetative cells divide to produce two identical daughter cells, with no evidence of . Cyst formation represents a survival strategy rather than a reproductive , though cysts can germinate back into vegetative cells under favorable conditions like the presence of , nutrients, and a carbon source such as glucose. involves the enzymatic breakdown and rupture of the exine layer, allowing the central body to expand and emerge as a motile vegetative cell within 4–8 hours, accompanied by the initiation of , RNA and protein synthesis, and eventual . This process ensures the resumption of active and growth.

Physiology and Metabolism

Azotobacter species are obligate aerobic heterotrophs that rely on molecular oxygen for efficient to generate the high ATP levels necessary for their metabolic processes. This respiratory dependence enables rapid growth but poses challenges due to the oxygen sensitivity of certain enzymes, which the bacteria mitigate through respiratory protection mechanisms that consume oxygen near the cell surface, maintaining microoxic conditions internally. These utilize a variety of carbon sources, primarily sugars such as glucose and , as well as acids like succinate and benzoate, to support heterotrophic growth and energy production. While capable of limited CO₂ fixation through anaplerotic pathways to replenish metabolic intermediates, this is minimal compared to their reliance on substrates. Azotobacter also synthesizes exopolysaccharides, notably alginate in species like A. vinelandii, which serves as a protective capsule and carbon reserve, with production enhanced under conditions of excess carbon and limited oxygen. Nutritionally, Azotobacter requires trace metals such as or as cofactors for key enzymes, facilitating metal uptake via siderophores to support metabolic functions. These exhibit tolerance to moderately high concentrations (up to 5% NaCl in some isolates) and thrive in neutral to slightly alkaline soils (optimal 7.0–7.5; growth tolerated from 6 to 9 in some isolates), allowing adaptation to diverse edaphic conditions. Certain species, such as A. chroococcum, produce melanin-like pigments through the oxidation of or precursors, forming dark-brown, water-soluble compounds that provide protection against ultraviolet radiation by absorbing harmful wavelengths and act as antioxidants to scavenge . These pigments contribute to cellular resilience under environmental stress, including brief roles in modulating oxygen exposure during metabolic shifts.

Genetic Features

The genomes of Azotobacter species typically consist of a single circular ranging from 4 to 5.5 million base pairs (Mbp) in size, with A. vinelandii possessing a chromosome of approximately 5.4 Mbp that encodes around 5,000 genes. This genomic architecture supports the bacterium's complex metabolic capabilities, including and environmental adaptation. Key genetic elements include the nif gene cluster, which encodes the structural and regulatory components of the nitrogenase enzyme essential for biological nitrogen fixation; this major cluster in A. vinelandii spans multiple operons and includes at least 15 nif-specific genes. Azotobacter genomes also feature CRISPR-Cas systems for defense against foreign DNA, with multiple CRISPR arrays and associated cas genes identified across species such as A. chroococcum and A. vinelandii. Additionally, these bacteria contain multiple rRNA operons—typically six per genome—to facilitate rapid protein synthesis under varying growth conditions. Azotobacter species often harbor plasmids, which can be large (up to >200 megadaltons in A. chroococcum) and contribute to ; for instance, A. chroococcum NCIMB 8003 contains six plasmids totaling over 600 kilobase pairs alongside its . These extrachromosomal elements exhibit genetic instability, with curing observed under environmental stresses like nutrient limitation or oxidative conditions, potentially as a mechanism to alleviate metabolic burden. Recent pangenomic analyses of 30 Azotobacter strains reveal a genome of about 1,600 genes shared across , with the accessory genome enriched in genes acquired via that enhance stress resistance, such as those for heavy metal tolerance and response. These mobile elements underscore the genus's adaptability to diverse soil environments.

Ecology and Distribution

Natural Habitats

Azotobacter species are predominantly found in neutral to alkaline soils with a range of 7.0 to 8.5, particularly those rich in , and are rarely isolated from acidic soils below 6.0. These thrive in fertile, well-aerated environments that support their aerobic , with population densities typically ranging from 10³ to 10⁶ colony-forming units (CFU) per gram of in such areas. Their cysts, which form under conditions, exhibit remarkable longevity, remaining viable in dry soils for up to 24 years. Globally, Azotobacter is ubiquitous in arable soils, freshwater and water bodies, and sediments, with detections in 30% to 80% of sampled soils worldwide. The genus has a broad distribution, including polar regions such as tundra. This widespread occurrence underscores its adaptability to diverse edaphic conditions, though abundance is higher in cultivated lands than in uncultivated or barren areas. Azotobacter species are commonly associated with the of various crops, including , , and , where they exist as non-symbiotic fixers benefiting from root exudates without forming mutualistic partnerships. In these microhabitats, populations can be denser compared to bulk , contributing to localized nutrient cycling in agricultural ecosystems.

Environmental Adaptations

Azotobacter species exhibit remarkable adaptations to through the formation of cysts, which are dormant structures consisting of a central surrounded by a multilayered that provides protection against loss. These cysts enable survival in dry soils for extended periods, up to 24 years, by maintaining cellular integrity under low moisture conditions. Vegetative cells, in contrast, are more sensitive to but gain protection through the production of extracellular polymeric substances () that facilitate formation, retaining hydration and shielding cells from environmental stress. Regarding temperature tolerance, Azotobacter cysts withstand a broad range, including extremes from -80°C during to up to 45–48°C, while vegetative cells are limited to optimal growth around 20–30°C and survive short exposures to 45–48°C before formation is induced for further protection. These adaptations allow Azotobacter to persist in fluctuating microenvironments. Stabilizing proteins like confer resistance to both high and low temperatures. In biotic interactions, Azotobacter displays antagonistic activity against plant pathogens through the production of antibiotics, such as compounds structurally similar to anisomycin, which inhibit fungal growth and reduce disease incidence in the rhizosphere. Additionally, it forms symbiotic-like associations with plant roots, enhancing phosphate solubilization by secreting organic acids that convert insoluble phosphates into bioavailable forms, thereby supporting plant nutrition without forming true symbioses. Azotobacter responds to pollutants by accumulating like , maintaining viability through EPS-mediated that sequesters ions without disrupting cellular functions, as evidenced by strains tolerating high Cr(VI) concentrations via mechanisms. It also degrades hydrocarbons, assimilating crude oil components as carbon sources during , which aids survival in contaminated soils. Recent research from 2023 highlights how carbon and amendments influence Azotobacter population dynamics in paddy soils; for instance, glucose addition as a carbon source significantly stimulates Azotobacter growth and enhances cycling, while balanced N inputs modulate community abundance under varying CO2 levels.

Nitrogen Fixation

Mechanism and Process

Azotobacter species fix atmospheric dinitrogen (N₂) into (NH₃) through the action of the enzyme complex, a process essential for their growth under nitrogen-limited conditions. This biological (BNF) involves the stepwise reduction of N₂, requiring significant energy input in the form of (ATP) and low-potential electrons. The overall reaction catalyzed by the molybdenum-dependent (Mo-nitrogenase), the primary form in Azotobacter, is represented by the equation: \text{N}_2 + 8\text{H}^+ + 8\text{e}^- + 16\text{ATP} \rightarrow 2\text{NH}_3 + \text{H}_2 + 16\text{ADP} + 16\text{P}_\text{i} This stoichiometry indicates that 16 ATP molecules are hydrolyzed per N₂ molecule reduced, with one molecule of hydrogen (H₂) inevitably produced as a byproduct, reflecting the enzyme's inefficiency but enabling the challenging activation of the inert N₂ triple bond. As obligate aerobes, Azotobacter maintain microaerobic intracellular conditions during to protect the oxygen-sensitive from inactivation. This protection is achieved through elevated rates, where oxygen consumption can increase dramatically—up to 8-10 fold upon nitrogenase derepression—to scavenge incoming O₂ and sustain low cytosolic oxygen levels below 1% air saturation. These high respiratory fluxes, driven by robust cytochrome-based transport chains, not only shield the but also generate the ATP and reducing equivalents needed for BNF. Nitrogen fixation efficiency is notably inhibited by fixed nitrogen sources, with activity ceasing in the presence of ammonium or nitrate, as these trigger repression of nitrogenase synthesis to prevent unnecessary energy expenditure. The expression of nitrogen fixation genes (nif cluster) in Azotobacter is tightly regulated by the nifL and nifA genes, which respond to nitrogen availability and cellular energy status. Under low-nitrogen conditions, the transcriptional activator NifA promotes nif gene expression, while the sensor protein NifL inhibits this activation in the presence of ammonium or high fixed nitrogen, ensuring fixation only when beneficial. In molybdenum-limited environments, Azotobacter switches to an alternative vanadium-dependent nitrogenase (V-nitrogenase), which is less efficient but allows continued BNF, with regulation involving analogous vnfA and possibly nifL-mediated controls. Under combined molybdenum and vanadium limitation, an iron-only nitrogenase (Fe-nitrogenase) is expressed, providing a final, even less efficient alternative.

Nitrogenase Complex

The nitrogenase complex in Azotobacter species, such as A. vinelandii, is composed of two primary metalloproteins: the molybdenum-iron (MoFe) protein, also termed dinitrogenase, and the iron (Fe) protein, known as dinitrogenase reductase. The MoFe protein is an α₂β₂ heterotetramer that houses the iron-molybdenum cofactor (FeMo-co), a [MoFe₇S₉C(R-homocitrate)] cluster serving as the active site for N₂ reduction, along with P-clusters ([Fe₈S₇]) that facilitate electron transfer within the protein. The Fe protein, a homodimer containing a [4Fe-4S] cluster, transfers electrons to the MoFe protein in a process coupled to ATP hydrolysis. An alternative vanadium-iron (VFe) protein, structurally analogous to the MoFe protein but with a [VFe₇S₉C(R-homocitrate)] cofactor, assembles under molybdenum limitation and supports lower-efficiency nitrogen fixation. In the , the protein docks transiently with the MoFe protein in a 1:1 or 2:1 , delivering electrons from its [4Fe-4S] cluster to the P-clusters and ultimately to the FeMo-co for reduction. This is tightly regulated to prevent futile ATP consumption, with the protein's conformational changes upon nucleotide binding enabling efficient and undocking. To protect the oxygen-sensitive from inactivation, Azotobacter employs multiple mechanisms. Respiratory protection involves rapid oxygen consumption by the bd , a high-affinity that maintains low intracellular O₂ levels during uncoupled respiration under diazotrophic conditions. Conformational protection occurs through reversible binding of the Shethna protein (FeSII), an Fe-S protein that associates with the Fe protein in response to , stabilizing the complex and preventing O₂-mediated damage. Additionally, the extracellular , composed primarily of alginate , forms a barrier that excludes O₂, creating microanaerobic niches around the cells. The structural genes for the conventional nitrogenase are organized in the nifHDK , where nifH encodes the protein, nifD the MoFe protein α-subunit, and nifK the β-subunit. Expression of nifHDK is tightly regulated and occurs predominantly in the low-O₂ microenvironments established by respiratory and diffusional barriers, mimicking heterocysts in .

Ecological and Agricultural Importance

Role in Soil Fertility

Azotobacter species play a vital role in the nitrogen cycle by performing asymbiotic biological , converting atmospheric into bioavailable forms that enrich pools in natural ecosystems. These free-living contribute an estimated 20 kg N ha⁻¹ annually, depending on conditions and species abundance, thereby supplementing inputs and reducing dependence on mineralization as the primary source. Beyond nitrogen fixation, Azotobacter enhances overall through the production of siderophores, low-molecular-weight compounds that chelate ferric iron (Fe³⁺), solubilizing it for uptake by soil microbes and preventing iron limitation in aerobic environments. This process not only improves nutrient availability but also indirectly suppresses phytopathogenic by depriving them of iron. Additionally, Azotobacter accelerates the of organic residues via enzymatic activity, promoting the mineralization of complex compounds into and releasing essential nutrients like carbon and , which bolsters quality. In terms of ecological balance, Azotobacter competes effectively with for substrates and space in the soil, helping to mitigate nitrogen losses through and maintain higher soil levels. This competitive interaction, along with its production of compounds, shapes microbial community structure, particularly in rhizospheres, where Azotobacter can comprise a small but influential proportion (e.g., ~0.06%) of the bacterial population, fostering diverse nitrogen-cycling consortia. Recent studies from 2024 underscore the robustness of in Azotobacter vinelandii under aerobic conditions, highlighting its respiratory protection mechanisms that sustain diazotrophy despite oxygen exposure, thereby supporting global pools in oxygen-rich terrestrial environments.

Plant Growth Promotion

Azotobacter species promote growth through multiple indirect mechanisms beyond , primarily via their interactions in the . These free-living colonize roots non-symbiotically, forming biofilms that enhance acquisition and resilience. Key contributions include the production of phytohormones and siderophores, solubilization of essential minerals, antagonism against phytopathogens, and modulation of conditions to favor . One primary mechanism is the synthesis of phytohormones such as (IAA), , and cytokinins, which stimulate root elongation, lateral root formation, and overall biomass accumulation. IAA production by Azotobacter chroococcum and A. vinelandii, for instance, has been shown to increase root length in crops like and , thereby improving nutrient and water uptake efficiency. and cytokinins further support cell division and shoot growth, leading to enhanced plant vigor under normal and stressed conditions. These hormones are excreted into the , directly influencing without requiring host specificity. Azotobacter also facilitates phosphate solubilization by secreting low-molecular-weight organic acids, such as gluconic and 2-ketogluconic acids, which lower the and chelate insoluble like into bioavailable forms. This process converts fixed soil , often comprising 30-50% of total P in organic and insoluble states, into soluble orthophosphate that can readily absorb. Studies with A. vinelandii strains demonstrate solubilization efficiencies up to 43% of phosphate rock, significantly boosting availability and uptake in crops such as , where P-responsive genotypes show improved yields. In terms of biocontrol, Azotobacter produces antifungal compounds, including hydrogen cyanide (HCN), which inhibit the growth of soil-borne pathogens like Fusarium species responsible for wilt and root rot diseases. HCN acts by disrupting fungal respiration and enzyme activity, with A. chroococcum strains exhibiting inhibition against Fusarium oxysporum in vitro. This antagonism reduces disease incidence in host plants, complementing other growth-promoting traits. A 2022 study highlighted synergistic effects when combining Azotobacter nigricans with NPK fertilizers in maize, resulting in 15-20% higher yields through integrated nutrient management and pathogen suppression. Non-symbiotic root colonization by Azotobacter further enhances plant through the production of , which form protective biofilms around and improve aggregation. increase water retention in the by up to 50%, mitigating water stress and maintaining in like and during dry periods. Inoculation with EPS-producing Azotobacter isolates has been shown to elevate accumulation and activity in , leading to 20-30% better survival and growth under conditions compared to uninoculated controls. Recent 2025 studies have demonstrated enhanced growth and yield in crops like , , and through Azotobacter inoculation, further supporting its role in .

Applications and Biotechnology

Biofertilizers and Agriculture

Azotobacter species are widely utilized in formulations as carrier-based inoculants to enhance availability in agricultural systems. These products typically consist of , , or similar carriers with a viable count of 10^8 to 10^9 colony-forming units per gram (CFU/g), ensuring effective and activity in . Such inoculants are commonly applied as seed coatings, where seeds of cereals like and or are treated with a slurry of the to promote direct root association upon . In field applications, Azotobacter biofertilizers have demonstrated efficacy in boosting crop yields by 10-30%, particularly for staples such as and , by facilitating biological and reducing reliance on synthetic inputs. Recent 2025 studies emphasize their role in sustainable farming, highlighting improved nutrient uptake and in diverse agroecosystems through free-living . Inoculation methods include seed coating, soil drenching to deliver the bacteria directly to the zone, and foliar sprays for targeted application during vegetative stages. These approaches are compatible with chemical fertilizers, allowing integrated without significant antagonism, though optimal results occur when combined with balanced NPK applications. Despite their benefits, challenges persist in Azotobacter biofertilizer deployment, including reduced survival in acidic soils where pH below 6.0 inhibits activity and bacterial persistence. Commercial strains require rigorous to maintain viability during and , as suboptimal formulations can lead to inconsistent and diminished efficacy. Azotobacter also produces phytohormones such as auxins, which briefly contribute to enhanced in treated crops. Ongoing research focuses on strain selection and encapsulation techniques to overcome these limitations and broaden applicability in varied soil conditions.

Industrial and Bioremediation Uses

Azotobacter species, particularly A. vinelandii, serve as key microbial platforms for industrial of alginate, a linear derived from their structures. This alginate is valued for its gelling and stabilizing properties in the , where it functions as a thickener in products like and salad dressings. In pharmaceuticals, it acts as a controlled-release agent for systems. Additionally, alginate from Azotobacter cysts is incorporated into wound dressings due to its , moisture-retention capabilities, and promotion of , facilitating faster healing in moist environments. To enhance yields, bioengineered strains of A. vinelandii have been developed through genetic modifications targeting biosynthetic pathways, such as overexpressing epimerases and polymerases, resulting in up to twofold increases in alginate under optimized conditions. These strains are cultivated in large-scale bioreactors with controlled oxygen and limitation to maximize accumulation. In , Azotobacter strains demonstrate efficacy in persistent organic pollutants, including pesticides. For instance, A. chroococcum and related species hydrolyze and mineralize herbicides like , reducing soil concentrations by over 70% within months through enzymatic breakdown. They also contribute to the of hydrocarbons, assimilating crude oil components as carbon sources during , with A. chroococcum isolates achieving up to 50% reduction in in marine and soil environments. Regarding accumulation, Azotobacter employs via extracellular and cell walls, binding (Cd) and lead (Pb) ions with capacities of approximately 33 mg/g dry for lead and comparable for ; exopolysaccharides from A. chroococcum specifically adsorb Pb²⁺ and Cd²⁺, mitigating in contaminated sites. As a biotechnological model, A. vinelandii facilitates of , with its well-characterized nif gene cluster enabling targeted interference systems that repress up to 60% of activity for pathway optimization as of 2024. Genome-scale metabolic models of A. vinelandii guide efforts to transfer robust protection mechanisms to crops, potentially reducing dependency. Furthermore, Azotobacter produces (PHAs), biodegradable bioplastics accumulated as intracellular granules under nutrient imbalance; A. vinelandii yields up to 60% PHA content from agro-waste substrates like apple residues, offering a sustainable alternative to petroleum-based plastics with properties suitable for packaging and medical devices. Recent advances in 2023 highlight enhanced Azotobacter-mediated remediation in contaminated soils via carbon-to-nitrogen (C/N) amendments. supplementation in diesel-polluted soils boosts Azotobacter activity, accelerating degradation by 30-50% through improved and expression. Similarly, balanced C/N ratios with biofertilizers increase immobilization and soil activity, promoting efficiency in metal-laden sites. 2025 studies further confirm high rates, achieving complete removal in soil within 10 days.

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