4.1. Effect of BA Addition on the Physicochemical Properties of Perilla frutescens Inter-Root Soil
BA is an important secondary metabolite in the synthesis and decomposition of plant substances, which can enter the soil through root secretion. It is a common plant allelopathic substance [
29]. In this study, the addition of BA causes soil acidification (neutral soil with a pH between 6.5 and 7.5; acidic soil, below 6.5) [
30], but the differences between different groups are not significant. This may be because benzoic acid itself is acidic (pH 5.8) and usually adsorbs on soil particles [
31]. Its adsorption capacity decreases with the decrease in pH, and it is also influenced by the surface distribution and adsorption of organic matter. Not only does it affect soil fertility, but it also affects the absorption of soil nutrients by crops, thereby affecting the growth and development of plants and product quality. The organic matter content in soil is usually stable and can only undergo significant changes over a large time scale. In this experiment, there was no significant difference in soil organic matter content among the different treatment groups (
p > 0.05). This is consistent with the research findings of Villarino et al. [
32]. Nitrogen, phosphorus, and potassium are very important nutrients in soil, playing a crucial role in the growth and development of plants. The mechanism of plant nutrient absorption is that plant roots actively absorb nutrients from the soil through their own physiological mechanisms [
33], which require ATP and carrier proteins to assist in transportation. In this study, compared with the CK group, with increased BA addition, the content of total nitrogen (TN), available nitrogen (AN), available phosphorus (AP), and available potassium (AK) increased, indicating that the plant root system is not lacking in nutrients; rather, its ability to absorb and utilize nutrients is reduced. This is consistent with Blum’s report that BA inhibits nutrient absorption in plant roots, leading to growth inhibition [
34]. Based on the results of the perilla root weight experiment, we speculate that due to the addition of BA, the pH of the root soil decreases, and the transportation of substances inside and outside the cell membrane slows down, resulting in weakened plant root absorption functions in relation to nutrients, and even peroxidation reactions. The plant roots become smaller, or tissue cells are damaged, and the absorption of nitrogen, phosphorus, and potassium decreases, which is proportional to the concentration of BA. Usually, plant roots can secrete a large amount of disaccharides such as sucrose, promoting the movement of microorganisms in the soil and selectively shaping the unique microbial community of the root system [
35]. The inhibition of perilla roots by BA leads to an uneven distribution of sucrose in various parts of the plant, resulting in the poor growth and development of perilla plants and decreased seed production.
4.2. Effect of BA Addition on the Inter-Root Soil Enzyme Activities of Perilla frutescens
Soil enzymes mainly come from plant roots and soil organisms and are the main catalysts for the decomposition, turnover, and mineralization of soil organic matter [
36]. They directly participate in various physiological and biochemical reactions in the soil [
37]. Studies have shown that the forms and contents of soil organic matter, nitrogen, phosphorus, and potassium [
38] are all related to soil enzyme activity [
39] and are of great significance for plant growth regulation [
40]. Urease is mainly present in soil bacteria, fungi, and spores, and it is used to catalyze the hydrolysis of urea into ammonia and carbon dioxide [
41]. Phosphatase is a key enzyme in the soil phosphorus cycle that is capable of catalyzing the conversion of insoluble inorganic phosphorus into effective phosphorus in the form of PO
43−, which is absorbed and utilized by plants. In this study, compared with the CK group, the addition of BA significantly increased the activities of urease and phosphatase (
p < 0.05). However, with increasing BA addition, there was no significant difference between the groups (
p > 0.05), indicating that BA promotes increased soil urease activity and converts soil organic nitrogen into available nitrogen that plants can use [
42], which is consistent with the increase in soil AN content in this experiment. The addition of BA significantly increased phosphatase activity in the rhizosphere soil of
Perilla frutescens (
p < 0.05), and it was positively correlated with the amount of BA added. This indicates that the addition of BA can improve soil phosphatase activity, promote the conversion of soil organic phosphorus into inorganic phosphorus [
43], and increase the content of available phosphorus in the soil, which is consistent with the increase in soil AP content in this experiment.
Catalase (CAT) is a type of oxidoreductase produced by microorganisms or plants, which is an important enzyme in soil. It can use hydrogen peroxide as a substrate to quickly convert waste generated by soil metabolism into harmless or less toxic substances, while releasing oxygen, reducing the toxicity of hydrogen peroxide accumulation to soil microorganisms and plant roots [
44] and enhancing plant antioxidant capacity; moreover, its activity can reflect the soil respiration intensity [
45]. Peroxidases have a strong removal effect on some pollutants or their derivatives in soil, eliminating the toxic effects of pollutants by converting them into other products. Peroxidases can utilize hydrogen peroxide and oxygen in other organic peroxides formed in soil due to microbial activity and the action of certain oxidase enzymes to oxidize soil organic matter, catalyze the oxidation reaction of various aromatic compounds (phenol, substituted phenols, aniline, polycyclic aromatic hydrocarbons, etc.), catalyze the oxidation–reduction reaction between hydrogen peroxide (H
2O
2) and iron minerals, oxidize colorless substrates of 3,3′, 5,5′-tetramethylbenzidine (TMB) to blue products (TMBox), and release effluents [
46]. Hydrogen peroxide is a very active oxidant, and the decrease in the activity of catalase and peroxidase leads to the accumulation of excessive hydrogen peroxide in the soil, causing damage to soil microorganisms and plants [
47]. In this study, the activities of catalase and peroxidase significantly decreased in the group treated with BA (
p < 0.05), but with increasing BA concentrations, there was no significant difference between the groups (
p > 0.05), indicating that the addition of BA led to a decrease in the activity of catalase and peroxidase in the root soil, damage to the antioxidant system of perilla, damage to its own immune system, and the poor development or toxicity of perilla roots, leading to decay. The difference between the two enzyme activity groups was not significant, indicating that there is no significant linear relationship between the amount of BA added and the activity of antioxidant enzymes. Further research is needed to investigate the reasons behind this.
4.3. Effects of BA Addition on the Structure and Function of Inter-Root Soil Microbial Communities of Perilla frutescens
Soil microorganisms play a crucial role in plant nutrition and health [
48], and microbial community diversity is closely related to crop growth and development [
49]. The results of this study found that, when compared with the CK group, the Chao1 and ACE indices of bacteria and fungi in the group with added BA were positively correlated with BA concentration. This may be due to the additional carbon source provided by exogenous BA, which stimulates the growth of in situ soil microbial communities and increases the richness of bacteria and fungi. This result is consistent with previous research. For example, Qu et al. studied the effects of two phenolic acids on soil microbial populations and found that phenolic acids can selectively enhance specific microbial populations in the soil [
50]. On the other hand, it may also be related to pH changes, which increase the efficiency of organic carbon conversion to biomass carbon and alter nutrient utilization efficiency, physiological metabolic activity, and competition among microbial populations, directly or indirectly affecting the microbial diversity of soil [
51]. Rousk et al. proposed that low pH values can reduce microbial indicators of soil quality, such as fungi, bacteria, and microbial biomass and, to a lesser extent, reduce microbial activity without affecting metabolism [
52]. Fungi in soil have a strong tolerance for acidification, and Moran et al.’s research has shown that fungal biomass is not affected by pH values [
53]. Therefore, the changes in fungal biomass are not as significant as those in bacteria, and the abundance of some acidophilic microbial populations changes significantly, disrupting the distribution balance between bacterial and fungal communities. In this study, the addition of BA reduced soil pH, resulting in weak acidity in the soil, indicating that higher concentrations of hydrogen ions inhibited microbial proliferation, which is consistent with the findings of Sui et al. [
54]. Therefore, BA can disrupt the ecological balance of soil microorganisms in the rhizosphere of
Perilla frutescens, resulting in changes in microbial evenness. As the concentration of BA increases, the complexity and stability of soil microbial communities gradually decrease.
At the phylum level, the composition of bacterial communities is relatively similar. Actinobacteria, Proteobacteria, Acidobacteriota, and Chloroflexi are the phyla with a higher relative abundance in the rhizosphere soil of
Perilla frutescens under all treatments. This indicates that the addition of BA did not alter the composition of the relative abundance of the main bacterial phyla in the soil. Dagher et al. found that Proteobacteria are widely distributed in soil, and their abundance is easily affected by environmental factors, playing an important regulatory role in nitrogen cycling and related to the accumulation of plant biomass [
55]. Nguyen et al. proposed Actinobacteria are acidic microorganisms that decompose organic matter to provide plant cells with the necessary nutrients for growth [
56], and these microorganisms have a positive impact on plant disease resistance [
57]; Kalam et al.’s research found that Acidobacteria have genes involved in different metabolic pathways, regulating the geochemical cycle, breaking down macromolecular biopolymers, secreting extracellular polysaccharides, and promoting plant growth [
58]. Actinobacteria and Acidobacteria are acidophilic microorganisms; therefore, their relative abundance is significantly higher under acidic conditions [
59]. In this study, with increasing BA concentration, soil pH significantly decreased from 6.8 to 5.9, and it was found that actinomycetes increased with decreasing pH, which is the main reason for the increase in actinomycetes. However, in this study, it was found that the relative abundance of Acidobacteria was significantly reduced, which may be due to BA stress leading to poor root development in the case of
Perilla frutescens and reduced colonization sites of Acidobacteria. Osiel’s study on the interaction between Acidobacteria and plants found that Acidobacteria have the ability to form flagella, which drive chemotaxis in plant roots [
60].
The results of all of the fungal phyla samples indicate that Ascomycota and
Mortierella are dominant fungal groups in soil, but the effects of different concentrations of BA on the relative abundance of
Mortierella vary. The results of this study indicate that B30 and B60 did not significantly change the relative abundance of
Mortierella, while B90 significantly increased the relative abundance of
Mortierella. The phylum
Aspergillus is one of the most abundant and diverse saprophytic fungi in acidic and alkaline soils, establishing extensive beneficial or pathogenic interactions with hosts [
61]. Liu et al. found that BA can cause
Fusarium wilt disease in cucumber during continuous monoculture [
62]. In addition, Haichar’s study found that BA can promote the biomass and activity of
Ralstonia solanacearum in rhizosphere soil, leading to an outbreak of tobacco bacterial wilt disease [
63]. BA is clearly the key factor to address when adding pathogenic bacteria to cause the plant diseases considered in this article. Although an increasing trend was observed in the case of Ascomycota and other fungal phyla, there was no significant change. Therefore, it can be inferred that the concentration of BA does not have a significant impact on the relative abundance of fungi in the rhizosphere soil of continuously cropped perilla.
At the genus level, there are 10 different bacterial and fungal species in the groups treated with different concentrations of BA:
Gemmatimonas,
Pseudolabrys,
Bradyrhizobium,
Pseudonocardia,
Marmoricola,
Bryobacter,
Streptomyces,
Sphingomonas,
Nocardioides, and
Mycobacterium. There are 4 different fungal microorganisms:
Ascomycota,
Glomeromycota,
Basidiomycota, and
Chytridiomycota. Compared with CK, the addition of BA significantly reduced the relative abundance of these 10 bacterial genera (
p < 0.05). Dias et al. found in their research that
Gemmatimonas is a phosphate-accumulating bacterium that can regulate the accumulation of phosphorus and energy conversion during cellular metabolism, promoting plant development and maturation [
64]. Zhao et al. found in their research that
Bradyrhizobium has various biochemical functions, including biological nitrogen fixation and carbon fixation. It belongs to the family Rhizobiaceae and interacts with the roots of leguminous plants to fix nitrogen in the atmosphere, improving the nitrogen availability of plants. It also has an extremely high agricultural value [
65].
Streptomyces is an important antagonistic microorganism with the ability to produce various antibiotics. Studies have shown that
Streptomyces can promote plant growth and induce overall plant resistance by secreting multiple secondary metabolites. Maila et al. found that
Streptomyces produces iron carriers, VOC, and ACC deaminases in tomatoes; furthermore, dissolving phosphate can promote tomato plant growth and improve its disease resistance [
66]. Song et al. found in their research that
Sphingomonas genus can efficiently decompose aromatic compounds and has the ability to reduce the concentration of allelopathic substances [
67]. Due to the addition of BA, soil pH and nutrient content decrease, inhibiting the growth and development of perilla, which may be the main reason for the decrease in the abundance of the abovementioned bacterial genera.
However, from the perspective of fungal genera, as the concentration of BA increases, the relative abundance of
Mortierella,
Pseudogymnoascus,
Pseudoeurotium, and
Talaromyces all significantly increase (
p < 0.05). Jiang et al. found in their research that
Mortierella is an oily fungus that can accumulate a large amount of highly unsaturated lipids, often causing plant roots to be unable to effectively absorb nutrients and water, leading to plant diseases such as root rot [
68]. Hassan et al. found in their research that
Pseudogymnoascus, as a saprophytic organism, often exhibits a pathogenic lifestyle [
69]; Avontuur et al. found in their research that
Pseudomonas often causes diseases such as root rot, wilt, and leaf mold [
70]. Zhang et al. found that
Talaromyces is an intracellular pathogenic fungus [
71]. The relative abundance of harmful fungal genera significantly increased (
p < 0.05) in this experiment, and the soil environment deteriorated.
The further annotation of fungal functions reveals that the microbial groups in the BA treatment group mostly involve saprophytic organisms, plant pathogens, and animal pathogens. It can be seen that BA significantly increases the abundance of harmful fungi in the rhizosphere soil of Perilla frutescens. The reproduction and accumulation of these pathogenic microorganisms in the soil cause significant decomposition of the organic matter in the soil, leading to plant malnutrition, an increased plant disease index, and decreased crop yield. However, we found that this change is not linearly related to the amount of BA added, indicating that the effect of BA on pathogenic microorganisms in the rhizosphere soil of Perilla frutescens is limited.
4.4. Correlation between Microorganisms and Physicochemical Indicators in Inter-Root Soils
The results of the redundancy analysis indicate that available phosphorus and available nitrogen are the main factors affecting the composition of bacterial communities, while total nitrogen is the main factor affecting the composition of fungal communities. The content of AP, AN, and TN is significantly positively correlated with the relative abundance of the
Bradyrhizobium,
Streptomyces,
Devosia,
Rhodanobacter,
Pseudogymnoascus,
Bryobacter,
Halenospora,
Mortierella,
Peziza,
Fusarium,
Talaromyces, and
Tausonia fungal genera (
p < 0.05), and it is significantly positively correlated with the relative abundance of
Halenospora,
Mortierlla,
Peziza, and
Fusaria. There is a significant negative correlation (
p < 0.05) between the relative abundance of the bacterial genera
Talaromyces and
Tausonia and the fungal genera
Sedogymnoascus,
Cephalotrichum,
Schizothecium, and
Pseudomycohila.
Bradyrhizobium and
Pseudolabrys are well-known nitrogen-fixing agents that have a symbiotic relationship with plant roots [
72]. They first convert nitrogen into organic nitrogen, and subsequently increase nitrogen levels in rhizosphere soil, thus enhancing effective absorption and the utilization of nitrogen by the host [
73].
Bryobacter can help to degrade organic matter in soil and maintain the water balance by slowly releasing stored water [
74].
Streptomyces can produce enzymes, iron carriers, organic acids, and pigments and degrade organic matter and dissolve phosphates. Phosphorus is an important component of functional components such as nucleic acids, nucleotides, and phospholipids. It is an important organic component in plant photosynthesis and respiration, and it is a necessary element for various coenzymes, high-energy phosphate bonds, and oxidative phosphorylation reactions [
75]. It has a regulatory effect on the metabolism of sugars, proteins, and fats in plants. At the same time, rhizosphere microorganisms secrete various metabolites (mainly including sugars, organic acids, and amino acids) to the rhizosphere, recruit functional bacteria such as phosphorus-solubilizing bacteria and potassium-solubilizing bacteria to colonize the plant rhizosphere, and secrete soil enzymes such as phosphatase, urease, and catalase, thereby increasing soil enzyme activity and nutrients in the rhizosphere. In this study, based on the annotation of microbial functions, it was found that the role of functional microorganisms is more concentrated in amino acid metabolism, carbohydrate metabolism, and energy metabolism. RDA analysis further revealed that AP, AN, and TN are the main physicochemical factors affecting the composition and distribution of dominant soil microbial communities. Considering the degree of influence, nitrogen is the most critical factor affecting the distribution of microbial communities, and nitrogen is positively correlated with nitrogen-fixing bacteria in the dominant microbial community, which is consistent with the research results of Morales et al. [
76].