The rising global demand for agricultural products is driven by population growth, leading to increased production rates that have resulted in topsoil depletion, diminished organic matter levels, and diminished soil ecological functions. Soil microbes play a crucial role in maintaining these functions, providing stability to the soil environment and enhancing resilience to disturbances. Poor land management practices have also contributed to problems such as groundwater contamination, plant disease outbreaks, and air pollution. The increasing recognition of the significance of sustainable and nutritious food reflects a growing awareness among the populace of the importance of environmental conservation (Abdul Rahman et al., 2021; Aguilar-Paredes et al., 2023; Vincze et al., 2024). Therefore, environmentally-friendly approaches to sustainable agriculture are gaining increasing popularity. De Corato proposes that sustainable agroecosystems demonstrate high levels of resilience, adaptability, and diversity (De Corato, 2020). These elements are interconnected, as diversity promotes adaptability, which is a crucial component in the resilience of agricultural ecosystems. The diversity of soil microbiota is essential for nutrient recycling and the formation of soil structure, and it plays a vital role in sustainable agriculture. Instead of solely focusing on the taxonomic diversity of soil microorganisms, the emphasis should be on their functional diversity (Gupta et al., 2022; Aguilar-Paredes et al., 2023). It is essential to have a thorough understanding of the function of microbes in agroecosystem processes, particularly in relation to crop growth and soil fertility, in order to achieve sustainable agricultural practices.

Soil microorganisms play a vital role in agricultural ecosystems by contributing to the decomposition of soil organic matter, maintaining soil fertility, facilitating nutrient cycling for plants, and supporting overall productivity (Etesami and Adl, 2020b). They are essential for the transformation and movement of nutrients from the soil to plants. The structure and composition of microbial communities in the soil are often used as a key indicator of soil quality (Jacoby et al., 2017). Moreover, soil microorganisms are indispensable for maintaining soil functions, including carbon and nitrogen cycles, as well as the metabolism of organic matter (Paul and Frey, 2023). The diversity of soil microbes serves as a significant indicator for evaluating ecosystem function (Luo et al., 2018). Numerous studies have highlighted the vital role of soil microbes as environmental indicators of soil quality, as they contribute to preserving the biological activities of soils, enhancing soil nutrient cycling, and promoting the formation of soil structure (Sharma et al., 2011; Schloter et al., 2018). However, the soil microbiome is constantly challenged by various environmental stresses, which can significantly alter its composition, diversity, and overall functionality (Chu, 2018; Etesami, 2018; Abdul Rahman et al., 2021).

Environmental stresses can have profound impacts on the soil microbiome (Khoshru et al., 2020; Abdul Rahman et al., 2021). These stresses can disrupt the delicate balance of the soil ecosystem, leading to shifts in microbial community structure, changes in metabolic activities, and reduced ecosystem services (Jansson and Hofmockel, 2020; Abdul Rahman et al., 2021; Vincze et al., 2024). For example, drought stress increases Gram-positive bacteria (e.g., Actinobacteria) while decreasing Gram-negative bacteria (e.g., Proteobacteria), reducing nutrient cycling and soil moisture (Ward et al., 2009; Barnard et al., 2013; Meisner et al., 2018; Flórián et al., 2019; Denardin et al., 2020). Salinity disrupts plant water relations and nutrient uptake, lowering microbial biomass and activity, with fungi being more vulnerable than bacteria (Zhang et al., 2019; Etesami and Adl, 2020a). Heavy metals like cadmium and lead select for tolerant taxa but impair microbial metabolism, leading to decreased diversity (Song et al., 2021b). Flooding compacts soil, reducing oxygen for aerobic organisms and favoring anaerobic bacteria, while altering pH and nutrient status (Bai et al., 2000; Graff and Conrad, 2005; Furtak et al., 2020; Grzyb et al., 2020). Temperature stress shifts microbial community structures, often decreasing alpha diversity and increasing beta diversity, impacting nutrient cycling and organic matter decomposition (Goicoechea et al., 2010; Frater et al., 2018; Jerbi et al., 2020). Agrochemicals in conventional farming reduce microbial diversity, disrupt soil health, and impact enzyme activities (Milošević and Govedarica, 2002; Santos et al., 2006; Kremer and Means, 2009). Changes in soil pH also influence microbial composition, with higher pH generally increasing bacterial diversity (Jones et al., 2009b; Malik et al., 2018; Smercina et al., 2019). Overall, these stresses lead to significant shifts in microbial community dynamics and soil health.

In recent years, the use of silicon (Si) has emerged as a promising strategy to mitigate the adverse effects of environmental stresses on the soil microbiome. Silicon is the second most abundant element in the Earth’s crust and has been shown to play a crucial role in soil parameters such as nutrient and water availability, as well as aggregate stability (Schaller et al., 2020, Schaller et al., 2021a, Schaller et al., 2022; Barbosa et al., 2024). It enhances plant growth, stress tolerance, and overall ecosystem resilience (Etesami and Jeong, 2018; Etesami and Jeong, 2020; Etesami et al., 2022a; Etesami and Jeong, 2023). Numerous studies have demonstrated that the application of Si can significantly alter the composition and diversity of the soil microbial community, even under stressful conditions (Leonard, 2019; Deng et al., 2021; Song et al., 2021b; Ahmad et al., 2024; Leite et al., 2024). However, the practical mechanisms through which Si can affect the soil microbiome are not well defined and are at the beginning of the research stages, requiring further investigation. Some of the potential mechanisms may include changes in soil pH, nutrient availability, and plant-microbe interactions (Etesami and Jeong, 2018; Etesami and Adl, 2020a; Putra et al., 2020; Etesami et al., 2021). Additionally, Si-induced changes in crop physiology and root exudation patterns can also have cascading impacts on the soil microbiome (Fan et al., 2016; Putra et al., 2020; Etesami et al., 2022a; Etesami and Glick, 2024). The aim of this review paper was to synthesize the current understanding of the effects of various environmental stresses on the soil microbiome and to explore the potential of Si as a mitigating agent in enhancing the resilience of the soil microbial community. Given the critical role of the soil microbiome in maintaining ecosystem function and agricultural productivity, and the growing challenges posed by environmental stresses, this review paper is essential in providing a comprehensive overview of the latest research and insights that can inform sustainable soil management practices and contribute to the development of more resilient and productive agricultural systems.

Microorganisms are among the most abundant living organisms on Earth, accounting for approximately 17% of global biomass (Bar-On et al., 2018). Soil is considered the most complex habitat, harboring an immense abundance of microbial life, estimated to comprise around 4-5 × 10³⁰ microbial cells. The soil microbiome consists mainly of soil archaea, bacteria, viruses, and fungi (Dubey et al., 2019). Mendes et al. (2013) estimate that 10⁸–10⁹ bacteria, 10⁷–10⁸ viruses, and 10⁵–10⁶ fungal cells occupy just one gram of soil. The soil microbiome plays a vital role in various aspects of crop growth, soil health and fertility, nutrient cycling, decomposition of organic matter, bioremediation of pollutants, and ecosystem functioning. These microorganisms are essential components of terrestrial ecosystems, contributing to overall ecosystem functioning and services (Sharma et al., 2011; Sahu et al., 2017; Banerjee and van der Heijden, 2023; Vincze et al., 2024). Soil also provides habitats for crop pathogenic microorganisms and opportunistic human pathogenic microorganisms (Mendes et al., 2013). Research related to soil microbiota has gained significant attention due to its pivotal role in the global carbon cycle and climate change and its importance for sustainable agricultural practices.

The rhizosphere, the region surrounding plant roots, serves as a critical interface for interactions between plants and the soil microbiome. It acts as a biological hotspot where complex interactions among plants, microbes, and other organisms take place. Plant roots secrete organic compounds that nourish and support the activity of microorganisms in the rhizosphere (Massalha et al., 2017). Rhizosphere soil contains 10⁸–10¹¹ cultivable cells in one gram of soil, corresponding to approximately 10⁴ microbial species (Saleem et al., 2019). Among the microbes associated with plants, bacteria and fungi are crucial components of the plant microbiome, playing complementary roles in enhancing plant growth, nutrient acquisition, abiotic and biotic stress tolerance, and overall ecosystem functioning (Etesami and Maheshwari, 2018; Begum et al., 2019). The diversity and composition of the bacterial community in the rhizosphere vary among crop plants, showing greater disparities among plant types like legumes, forbs, and grasses (Vincze et al., 2024). The rhizosphere microbiome consists of a variety of bacterial groups belonging to phyla such as Actinobacteria, Acidobacteria, Ascomycota, Bacteroidetes, Basidiomycota, Euryarchaeota, Deinococcus-Thermus, Firmicutes, and Proteobacteria (Yadav et al., 2018). Among the bacterial phyla, Proteobacteria and Acidobacteria are the most abundant bacterial groups in rhizosphere soil, playing key roles in carbon and nutrient cycling (Islam et al., 2020). They promote plant growth (Gahan and Schmalenberger, 2014; Smercina et al., 2019), suppress plant pathogens, fix nitrogen (N₂), decompose recalcitrant organic matter, and produce beneficial compounds such as antibiotics and auxins (Bhatti et al., 2017; Ebrahimi-Zarandi et al., 2023) ( Figure 1 ). Plant growth-promoting rhizobacteria (PGPR), such as those from the Rhizobiaceae family, form symbiotic relationships with plants, directly improving nutrient availability, root growth, and stress tolerance while indirectly suppressing pathogens. PGPR can reduce fertilizer use by 50% while enhancing plant nutrient uptake and yield. Rhizosphere and endophytic bacteria can also produce plant hormones like auxin, gibberellin, and cytokinin, which regulate plant development, while also lowering plant ethylene levels to mitigate stress (Etesami, 2018; Etesami and Maheshwari, 2018; Etesami and Adl, 2020b; Etesami et al., 2023). Nitrogen-fixing diazotrophs, a group of PGPR, serve as a major nitrogen source in soils, accounting for 30-50% of the total nitrogen in crop fields (Rosenblueth et al., 2018; Smercina et al., 2019). The presence of these bacteria is crucial for plant health, facilitating growth and nutrient uptake. These bacteria can also enhance the resilience of plants against biotic and abiotic stresses, making them essential for sustainable agricultural practices. Archaea also contribute to soil function by playing roles in carbon, nitrogen, and sulfur cycling. Ammonia-oxidizing Thaumarchaeota are particularly abundant and versatile in soil environments. However, the nitrification carried out by archaea can lead to nitrate leaching and greenhouse gas emissions (Ren et al., 2018; Baker et al., 2020; Wang et al., 2020b).

Fungi exhibit high plasticity and can thrive in diverse environmental conditions. They act as decomposers, producing extracellular enzymes to convert organic matter to CO₂, and can mitigate metal toxicity by absorbing heavy metals (Islam et al., 2020). Fungi are recognized as biological controllers, helping to manage phytopathogenic fungal diseases (Iqbal et al., 2021; Yan and Khan, 2021). Additionally, fungal communities are pivotal in nutrient cycling and uptake (Khan et al., 2010; Vergara et al., 2017). Mycorrhizal fungi form symbiotic relationships with crop roots, enhancing nutrient and water uptake and increasing tolerance to biotic and abiotic stresses (Sun et al., 2018; Islam et al., 2020; Abdul Rahman et al., 2021) ( Figure 2 ). They also play a critical role in solubilizing and enhancing the availability of phosphorus, a key nutrient for plant growth (Begum et al., 2019; Abdul Rahman et al., 2021).

A diverse and balanced soil microbiome is essential for sustaining soil fertility, productivity, and resilience to environmental stresses. Disruption of the soil microbiome can result in soil degradation, reduced crop yields, and heightened susceptibility to pests and diseases. Therefore, understanding and managing the soil microbiome is crucial for sustainable agriculture and for preserving the ecosystem services provided by soils.

Soil microbiomes are highly sensitive to various abiotic factors that can significantly influence their composition and functions (Abdul Rahman et al., 2021) ( Figure 3 ). Soil pH is a primary driver, as beneficial microbes and plants prefer a neutral pH range of 6-7 (Sullivan et al., 2017). Changes in soil acidity or alkalinity often lead to shifts in the microbial community, with acidic soils reducing the diversity of nitrogen-fixing bacteria (Smercina et al., 2019), and different bacterial groups exhibiting varying pH tolerances (Jones et al., 2009b; Malik et al., 2018; Smercina et al., 2019). Soil temperature also plays a crucial role, as it affects the growth and activity of mesophilic, psychrophilic, and thermophilic microbes (Frater et al., 2018; Keenleyside, 2019; Jerbi et al., 2020). Increased temperatures can favor certain pathogens and alter mycorrhizal associations (Goicoechea et al., 2010; Frater et al., 2018; Jerbi et al., 2020). Soil aeration is another important factor, as hypoxic or waterlogged conditions disrupt aerobic microbes and nitrogen fixation (Smercina et al., 2019), prompting diazotrophs to employ various strategies to maintain nitrogen fixation under oxygen stress (Smercina et al., 2019). The soil’s physico-chemical properties—such as soil texture, structure, and organic matter content—play a crucial role in shaping microbial communities and their functions (Gupta and Roper, 2010; Smercina et al., 2019; Mosaffaei et al., 2020; Scudeletti et al., 2021). Soil compaction and depth can negatively affect fungal populations. Soil moisture levels significantly influence soil microbial respiration, biomass, and community structure (Sorensen et al., 2013; Yan et al., 2019; Grzyb et al., 2020; Siebielecet al., 2020). Excess soil moisture can be particularly harmful to aerobic microbes, as it limits oxygen availability (Yan et al., 2019; Sales Da Silva et al., 2020; Siebielec et al., 2020).

Drought can significantly impact microbial growth, activity, and community composition, favoring the proliferation of drought-tolerant taxa like Actinobacteria and Firmicutes that can produce spores and osmolytes to withstand desiccation (Ward et al., 2009; Barnard et al., 2013; Meisner et al., 2018; Flórián et al., 2019; Denardin et al., 2020). Conversely, flooding and waterlogged conditions promote the dominance of anaerobic bacteria while suppressing aerobic microbes and fungal communities (Bai et al., 2000; Graff and Conrad, 2005; Furtak et al., 2020; Grzyb et al., 2020). The reduced oxygen availability and changes in soil pH and nutrient status during submergence induce major shifts in the microbial community structure (Rosenblueth et al., 2018; Sánchez-Rodríguez et al., 2018; Hartman and Tringe, 2019). Heavy metal contamination significantly affects soil microbiomes, with Firmicutes, Proteobacteria, and Actinobacteria often dominating polluted soils. Arbuscular mycorrhizal fungi can colonize nutrient-poor, metal-laden environments, but high levels of metals like cadmium can hinder key life cycle stages, such as sporulation and mycelium expansion (Fomina et al., 2005; Abdu et al., 2017; Ma et al., 2021; Etesami and Glick, 2023). Heavy metals inhibit soil enzyme activities, reducing biological activity and potentially leading to the selection of metal-resistant microbial strains (Song et al., 2021b). Microbes adapt to metal toxicity through strategies like producing metal-chelating organic acids and developing metal-tolerant enzymes (Khan et al., 2000; Fomina et al., 2005; Seneviratne et al., 2017).

The extensive use of chemical fertilizers and pesticides in agriculture can be detrimental to the ecosystem and human health. Heavy metal contamination is a widespread issue in agricultural fields and farms as a result of these chemical inputs (Ali et al., 2019; Alengebawy et al., 2021; Nadarajah et al., 2021). However, the impact on the soil microbiome is complex and varied. Soil microbes are highly sensitive to fertilization practices, and their reactions to organic and inorganic fertilizers have received considerable attention (Hartmann et al., 2015; Fu et al., 2017). Fertilization can influence soil microbial diversity by altering the nutrient concentration in the soil (Bell et al., 2015). The long-term use of mineral fertilizers, especially nitrogen, can decrease microbial biomass and shift community composition, potentially due to soil acidification and metal contaminants (Holík et al., 2019; Wu et al., 2020). Emerging nano-fertilizer technologies can also impact the soil microbiome, with both positive and negative effects reported (Rajput et al., 2018; Gupta and Prakash, 2020). Pesticides, including herbicides, insecticides, and fungicides, are widely used to control weeds, pests, and pathogens. However, these chemicals can have detrimental impacts on soil microbes, reducing microbial abundance, diversity, and key functional processes like nitrogen fixation (Milošević and Govedarica, 2002; Santos et al., 2006; Kremer and Means, 2009). The specific effects depend on the pesticide type, dose, and interactions with other soil factors. Organic pesticides are generally less harmful than synthetic ones, but concerns remain about their environmental impacts (Bahlai et al., 2010; Biondi et al., 2012). It is important to note that the environmental stresses mentioned can have an indirect impact on the soil microbiome through their effects on plants. Plants play a significant function in shaping the composition and diversity of the soil microbiome in the rhizosphere through mechanisms such as altering root architecture, releasing root exudates, and forming symbiotic relationships (Abdul Rahman et al., 2021). Overall, the environmental stresses chemicals pose risks to the soil microbiome and ecosystem health. Across these stresses, the ability of the soil microbiome to adapt and maintain functional diversity is crucial for sustaining soil health and ecosystem processes in the face of environmental change.

Silicon is the second most abundant element in the Earth’s crust, after oxygen, and plays a crucial role in the growth and development of many plant species, particularly grasses and cereals. Although Si is not considered an essential nutrient for plants, it is now recognized as a beneficial element that can enhance crop tolerance to both biotic and abiotic stresses (Epstein, 1994). In soils, Si exists in various forms, including soluble silicic acid, amorphous silica, and crystalline silicates, and its availability for plant uptake depends on factors such as soil pH, moisture, and the presence of other elements (Epstein, 1994; Ma and Yamaji, 2006). For example, amorphous silica has recently been shown to be an important factor influencing several soil traits, such as nutrient availability (Schaller et al., 2022), and water availability (Schaller et al., 2020; Zarebanadkouki et al., 2022), which depend on soil texture (Zarebanadkouki et al., 2024). It also improves aggregate stability (Barbosa et al., 2024). All of these parameters can significantly affect soil microbial community structure (Lewin et al., 2024). The availability of silicic acid for microbes is influenced by mineralogy and the content of amorphous silica, which serves as the primary source of silicic acid (Schaller et al., 2021a).

Once absorbed, Si can confer numerous benefits to plants, including structural support through deposition in cell walls and other plant tissues, improved tolerance to stresses such as water deficit, salinity, heavy metal toxicity, extreme temperatures, and fungal diseases, regulation of nutrient uptake and utilization, stimulation of antioxidant activity, and enhancement of crop yields and quality (Epstein, 1994; Yongchao et al., 2015; Etesami and Jeong, 2018; Etesami and Jeong, 2020; Etesami et al., 2022a; Etesami and Jeong, 2023). The beneficial effects of Si on plants have led to increased interest in the use of Si-based fertilizers and amendments in sustainable agriculture, but their impact on soil biological properties is still not clear. Understanding the mechanisms by which Si interacts with plants, soil, and microorganisms is crucial for developing effective strategies to optimize Si management and harness its potential for improved crop performance and environmental resilience.

The application of Si has emerged as a promising approach to alleviate the negative impacts of environmental stresses on soil microbiomes ( Table 1 ). Research indicates that Si can significantly stimulate beneficial soil bacteria. For instance, Karunakaran et al. (2013) demonstrated that nanosilica application doubled the total soil bacterial population, enhancing microbial biomass and activity. Specifically, the viability of PGPR, including Bacillus megaterium, B. brevis, P. fluorescens, and Azotobacter vinelandii, increased by over 20% in the presence of nanosilica. Silicon not only boosts bacterial abundance but also alters microbial community diversity and composition. Lin et al. (2020) found that Si application influenced 63.7% of the operational taxonomic units (OTUs) in the soil, highlighting a direct effect on microorganisms independent of crop presence. This alteration has been linked to improved soil biological properties and overall ecosystem functioning, including enhanced carbon/nitrogen cycling genes and metal detoxification in contaminated soils. In various studies, Si application has been shown to enhance microbial populations in crops like tomatoes (Wang et al., 2013) and in environments with heavy metal contamination (Wang et al., 2020a). Moreover, Si-rich amendments, such as rice husk and calcium silicate, have been reported to modify specific microbial communities tied to soil processes like arsenic metabolism (Dykes et al., 2021).

The beneficial effects of Si extend to legume root-microbe symbiosis, where Medicago sativa showed a 44% increase in nitrogen-fixing root nodules upon Si supplementation (Johnson et al., 2017). This improvement may arise from Si stimulating signaling compounds that enhance nodulation or increasing the abundance of nitrogen-fixing bacteria in root nodules. Silicon applications also favor certain bacterial groups capable of producing plant growth-promoting compounds. For example, Pseudomonas species that produce indole-3-acetic acid and solubilize phosphorus were found to increase following Si treatment (Song et al., 2021b). California-based studies showed that Si helped microbial communities thrive in heavy metal-contaminated soils by improving overall soil properties and nutrient availability while mitigating heavy metal toxicity (Zhang et al., 2019). Studies noted shifts in soil biological properties in response to Si addition. For example, one study observed decreased soil acid phosphatase activity, potentially due to increased phosphorus availability. The application of Si altered microbial composition, increasing Proteobacteria while decreasing Acidobacteria and Verrucomicrobia, driven by changes in soil chemistry including pH and nutrient levels (Deng et al., 2021). Silicon fertilization significantly impacts microbial richness and diversity, correlating positively with lower cadmium (Cd) accumulation in rice plants. Analysis revealed that Si treatment prompted microbial adaptations beneficial for nutrient cycling and Cd immobilization, with factors like soil pH and nutrient levels influencing community variations (Peng et al., 2023). In the rhizosphere of rice plants, long-term Si application enhanced microbial diversity and richness, particularly favoring groups like Proteobacteria and Actinobacteriota (Gao et al., 2022). It also reduced the bioavailability of arsenic, demonstrating potential for mitigating toxic influences on plants. Furthermore, Si application has been shown to enhance disease resistance in various crops. For example, in tomato plants, Si treatment reduced the incidence of soil-borne diseases caused by Ralstonia solanacearum, aiding nutrient cycling and microbial community activity (Wang et al., 2013). The type of Si source utilized also influences microbial community structure. For instance, sodium silicate was found to promote beneficial bacterial groups while inhibiting disease-related fungal taxa in cucumber cultivation, thus enhancing growth and defense against Fusarium wilt (Zhou et al., 2018). A field plot study on wheat cultivation found that the application of amorphous silica to the soil not only increased wheat yield during drought (Schaller et al., 2021b) but also altered the microbial community structure, resulting in an increase in beneficial microbes and a reduction in pathogenic microbes (Lewin et al., 2024).

Silicon’s role in modulating microbial communities extends to ginseng cultivation, where it reduced disease severity from Alternaria panax by restructuring soil bacterial community composition (Li et al., 2019a). Additionally, the combination of Si fertilizer with microbial agents significantly improved plant growth and microbial dynamics in lily crops, indicating a synergistic effect (Yu et al., 2022). Results from arsenic-contaminated soils show that Si application can alter bacterial communities, reducing harmful taxa while enhancing beneficial ones, suggesting that Si treatment has significant implications for soil health and arsenic detoxification (Shao et al., 2016). In another investigation, Si significantly increased soil microbial activity and diversity (Shamshiripour et al., 2022). The addition of Si and phosphorus not only improved rice productivity but also enhanced key soil biological properties, such as enzyme activity (Jinger et al., 2020). Nanotechnology has further enhanced potential applications of Si; nano-Si fertilizers notably improved soil properties and microbial diversity in wheat cultivation, suggesting substantial benefits for soil health and productivity (Zhu et al., 2024). Overall, Si’s application can effectively reshape soil microbial communities across various contexts—from agricultural settings to contaminated environments—indicating its utility in enhancing ecosystem resilience to stressors. Understanding the mechanisms by which Si influences soil microbiomes, such as changes in pH, nutrient dynamics, and plant-microbe interactions ( Figure 4 ), is key for harnessing its full potential. Future research should aim to clarify these mechanisms and explore practical applications for sustainable soil management, underscoring Si’s role in promoting agricultural sustainability. Further research is needed to elucidate the precise mechanisms underlying these Si-mediated changes in the soil microbial community and to explore the practical implications for sustainable soil management practices.

The review has highlighted the critical importance of the soil microbiome in maintaining the overall health and functioning of agricultural ecosystems. Soil microorganisms play pivotal roles in nutrient cycling, organic matter decomposition, crop growth promotion, and enhancing tolerance to biotic and abiotic stresses. However, the soil microbiome is constantly challenged by different environmental stresses, such as drought, salinity, heavy metal contamination, and climate change, which can significantly disrupt the delicate balance of the soil ecosystem. In this context, the application of Si has emerged as a promising strategy to mitigate the adverse effects of environmental stresses on the soil microbiome. Silicon can enhance the resilience of the soil microbial community through several mechanisms, including increasing soil pH, improving nutrient availability and uptake, altering root exudation patterns and plant physiology, and directly stimulating the abundance, diversity, and functional potential of key microbial groups. By enhancing the resilience of the soil microbiome, Si application can help maintain the critical ecosystem services provided by soil microorganisms, ultimately contributing to the sustainability and productivity of agricultural systems. Future research aspects include elucidating the precise mechanisms of Si-microbiome interactions under various environmental stresses, evaluating the long-term effects of Si on soil microbiome resilience, optimizing Si application strategies for specific crop-soil systems, integrating Si management with other sustainable soil practices, and assessing the impacts of Si on soil microbiome-mediated ecosystem services. By addressing these future research aspects, we can deepen our understanding of the mechanisms underlying Si-microbiome interactions and leverage this knowledge to develop more effective and resilient agricultural systems that can withstand the challenges posed by environmental stresses.