Research Article

Synergistic Effect of Biochar and Indigenous Plant Growth-Promoting Rhizobacteria (PGPR) on Soil Fertility and Crop Productivity in Arid Regions of Iraq

Ibrahim Ayad jihad١ Eatidal Akram Farhan2 Aseel Ehsan Mahmoud٣ Alaa Saleh Mahdi٤ Maryam Mansoor Mathkoor٥ Mustafa Mudhafar٦ and Qais R. Lahhob7

1Department of chemistry and biochemistry, Al-Zahraa college of medicine, University of Basrah, Iraq; 2Department of chemistry and biochemistry, Al-Zahraa college of medicine, University of Basrah, Iraq; ٣Department of Medical Physics , Faculty of Medical Applied Sciences,University of kerbala, 56001, kerbala, Iraq; 4Department of pharmaceutics, collage of pharmacy, Al-Bayan university ; ٥Department of therapeutic nutrition technologies, Al Taff university college, 56001, Kerbala, Iraq; ٦Centre for Research on Environment and Renewable Energy, University of Kerbala, Karbala 56001, Iraq; 7Collage of Pharmacy, National University of Science and Technology, Dhi Qar, 64001, Iraq.

Abstract | In arid lands soil degradation, salinity, and low fertility are major issues that limit agricultural production. Biochar, a carbon-rich material produced from biomass pyrolysis, and native plant suggest the words rhizobacteria/plant growth-promoting rhizobacteria (PGPR) are both promising amendments to improve soil condition and plant performance. The purpose of this project was to understand the combined action of bio applicable and locally isolated PGPR (Bacillus subtilis and Pseudomonas fluorescens) to promote the soil fertility and wheat yield in saline-alkaline soils in Basrah. A randomized complete block design (RCBD) field experiment was arranged with four treatments: control, biochar alone, PGPR alone, and a combination of biochar and PGPR. These combinations have shown that when applied together, they significantly improved SOC, available nitrogen and phosphorus, and microbial biomass carbon in addition to wheat yield and WUE throughout the experiment. The treatment gave a 28.4% increase in soil organic carbon (SOC), 35.6% increase in available phosphorus, and 42.3% increase in grain yield as compared to the control (p < 0.05). Increases in those parameters were probably influenced by the rhizosphere priming effect and nutrient cycling, as biochar provided a stable carbon framework for microbial colonization coupled with PGPR activity. Thus, the co-application of biochar and indigenous PGPR may provide a cheap method for improving soil fertility and crop productivity under arid conditions. Its long-term impact and wider geographical extension in different agroecological sets deserve further studies.


Received | 23 May 2025; Accepted | September 30, 2025; Published | June 30, 2026

*Correspondence | Qais R. Lahhob, Department of chemistry and biochemistry, Al-Zahraa college of medicine, University of Basrah, Iraq; Email: [email protected]

Citation | Jihad, I.A., E.A. Farhan, A.E. Mahmoud, A.S. Mahdi, M.M. Mathkoor, M. Mudhafar and Q.R. Lahhob. 2026. Synergistic effect of biochar and indigenous plant growth-promoting rhizobacteria (pgpr) on soil fertility and crop productivity in arid regions of Iraq. Pakistan Journal of Agricultural Research, 39(2): 179-186.

DOI | https://dx.doi.org/10.17582/journal.pjar/2026/39.2.179.186

Keywords | Biochar; Plant Growth-Promoting Rhizobacteria ; Saline-Alkaline Soil; Soil Fertility; Wheat Productivity; Sustainable Agriculture.

Copyright: 2026 by the authors. Licensee ResearchersLinks Ltd, England, UK.

This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/).



Introduction

Arid and semi-arid environments, which make up more than 70% of arable land in Iraq, severely impact agriculture due to desertification, low soil organic matter, elevated salinity, and limited water availability (Hussain et al., 2020). Climate change and intensive farming are aggravating these issues, with lower yields of the key crop wheat (Triticum aestivum L.) leading to food insecurity concerns (Iqbal et al., 2023; Farooq et al., 2020). Soil degradation contributes to nutrient deficiency, reduced water holding capacity, and salinization of a limited resource, which ultimately threatens agriculture’s sustainability (Ahmed et al., 2022).

Biochar is a carbon-rich product made from pyrolysis of biomass (Jin et al., 2021; Tariq et al., 2021). Biochar can alter soil characteristics such as improve soil structure and water holding capacity and is also documented to improve nutrient holding capacity (Jin et al., 2021; Lal et al., 2020). In addition to soil benefits, biochar is porous in nature, therefore biochar can promote microbial activity and carbon stabilization leading to potential improvements in nutrient cycling through microbial activity (Gul et al., 2021; Tian et al., 2021). Phizorigc plant growth promoting rhizobacteria (PGPR), specifically Bacillus subtilis and Pseudomonas fluorescens, can assist promote natural plant growth through nitrogen binding, phosphate solubilization and production of phytohormone while suppressing the and minimizing abiotic stress from salinity and drought (Backer et al., 2020; Sharma et al., 2021). The absence of one of these sources in soil will lessen effectiveness of the other. The rhizosphere priming effect indicates that biochar will optimize microbial activation by giving them long-term feedstock to build carbohydrate found in the biochar. Essentially selecting the right PGPR will help with conversion of biochar into nutrient available to crops. The nutrient cycling hypothesis specifically states that when plants and PGPR work together and accumulate carbon at a higher rate in biochar-amended soils, so the %NC and AP that is determined from the nutrients conversion that is facilitated/transformed through microbially mediated processes. The property of both biochar and PGPR working together to together in terrestrial ecosystems can make them work better together is most effectively seen in arid ecosystem with are characterized by the soils physical and/or chemical limitations of crop evolutionary history (Nadeem et al., 2020).

Research on these amendments in high temperature saline-alkaline arid soils of Iraq has been scant (Ahmed et al., 2022; Khan et al., 2022). This research will look at the combined impacts of biochar and indigenous PGPR on soil fertility and wheat productivity in Basrah, Iraq. This study aims to evaluate the impact of treatments on soil fertility indicators (i.e., SOC, nitrogen, phosphorus, and microbial biomass),the impacts of the treatments on wheat growth and yield and toinvestigate any possible synergistic impacts in arid settings.

Materials and Methods

Study area

The experiment was performed in Basrah, Iraq situated at 30.5° North and 47.8° East, in a hot desert region with extreme climatic conditions that are common to arid areas. The location experiences a low average yearly precipitation (<150 mm) and has a high mean temperature averaging ~35°C, with summer maxima reaching ~45°C (Hussain et al., 2020). The soil is a sandy loam (>60% sand, 25% silt, and 15% clay) with low organic carbon (0.8%), slightly alkaline (pH 7.8), and an electrical conductivity (EC) of 2.1 dS m-¹ indicating moderate salinity (Ahmed et al., 2022; Jadah, & Al-Rubaye, 2025). The weather or climatic conditions, combined with the properties of the soil and high evaporation rate, along with reliable water scarcity, create numerous constraints to crop production, thus representing the perfect location for trialling amendments to soils with biochar and PGPR (Rehman et al., 2022). The experimental field site was chosen as a representative field of degraded agricultural lands throughout southern Iraq which have nearly 100 % vegetation cover and a history of conventional wheat cropping.

Experimental design

A field experiment was conducted during the 2023–2024 growing season using a randomized complete block design (RCBD) for robust statistical analysis and to account for spatial variation. Four treatments were tested and include (1) control (no amendments), (2) biochar added at 10 t ha-¹, (3) PGPR, with Bacillus subtilis and Pseudomonas fluorescens added at 10⁸ CFU g-¹ added, and (4) a combination of biochar plus PGPR. Each treatment was replicated four times resulting in 16 experiments, each measuring 4 m × 4 m. There were 1 m buffer zones separating each treatment to prevent cross-contamination to ensure treatment independence (Sharma et al., 2021). The RCBD method was demographic of variability in the field due to the potential for soil heterogeneity, with treatments assigned randomly with a random number generator to reduce bias (Wang et al., 2020). Crops were irrigated via drip irrigation to maintain consistent soil moisture, with rates of water application based on crop_ET requirements for wheat under arid conditions (Farooq et al., 2020).

Biochar and PGPR preparation

Biochar was made from locally available (and prevalent agricultural waste in Iraq) date palm (Phoenix dactylifera L.) by step-wise pyrolyzing it at 450 °C in an oxygen-limited environment consuming organic material to maximize carbon stability and surface area (Jin et al., 2021). The process lasted a total of 4 hours and produced a biochar product with a high fixed carbon content (>70%) and low ash content (<10%) by an assessment of proximate analysis (Tariq et al., 2021). The biochar was ground to a <2 mm particle size to improve uniform incorporation and surface contact with the soil and then was incorporated into the upper 15 cm of soil using a rotary tiller for even distribution (Lal et al., 2020). The chosen PGPR strains (Bacillus subtilis and Pseudomonas fluorescens) were isolated and selected from the rhizosphere of wheat grown in arid soils sourced from Basrah, Iraq, through standard microbiological protocols (Bano et al., 2023). The rhizosphere (0–20 cm) soil samples were serially diluted in 3 steps and spread plated using the standard nutrient agar growth medium in order to isolate single colonies of bacteria. Bacterial colonies were confirmed by 16s rRNA sequencing to demonstrate strain specificity and functionality (Liu et al., 2022). The PGPR strains were cultured in nutrient broth until a concentration of 10⁸ CFU g-¹ was achieved before applying as a seed coating to wheat (cv. IPA 99) with a carboxymethyl cellulose (CMC) binder to improve attachment (Peng et al., 2021).

Soil and plant sampling

Soil sampling occurred (0 to 20 cm) at pre-soil and post-harvest. This soil sampling includes SOC, available phosphorus, available nitrogen, microbial biomass carbon, water, bulk density, porosity, and aggregate stability (Zhang et al., 2020; Khan et al., 2022). The wheat grain yield and water use efficiency (WUE) was measured agronomically at the harvest (Iqbal et al., 2023), as shown in the Figure 1.

 

Statistical analysis

The data were analyzed using analysis of variance (ANOVA) in SPSS (version 26) and treatment means were evaluated using Tukey’s Honestly Significant Difference (HSD) test at P < 0.05 level of significance to detect treatment differences (Khan et al., 2020; Silva et al., 2024). To assess the association between soil fertility parameters (e.g., SOC, available nutrients) and crop productivity indicators (e.g., grain yield, WUE), the Pearson’s correlation analysis was performed. The Shapiro-Wilk test and Levene’s test were employed to check normality and homogeneity of variances, respectively, and hence both assumptions were satisfied.

Ethical approval

There were no ethical procedures as there were no humans or animal subjects in this study.

Results

Soil fertility parameters

The biochar + PGPR treatment caused a major increase in soil fertility (Table 1). Soil organic carbon (SOC) rose 28.4% (0.80% to 1.03% SOC), available phosphorus rose 35.6%, and available nitrogen rose 22.1% (P < 0.05). A high microbial biomass carbon level (245.6 mg kg-¹) indicates high amounts of microbial activity (Gul et al., 2021; Jin et al., 2021; Liu et al., 2022). The priming effect of biochar in the rhizosphere may occur since biochar acts as a stable carbon matrix for the PGPR in the soil and may improve microbial activity by providing the microbes with a porous environment that enhances organic matter mineralization and nutrient release (Peng et al., 2021). This may be related to the large surface area of biochar (typically > 200 m² g-¹) that promotes microbial attachment to the biochar and microbial protection against some environmental stresses (e.g., desiccation in arid soils) (Tian et al., 2021).

 

Table 1: Effect of treatments on soil fertility parameters

Treatment

SOC (%)

Available P (mg kg-¹)

Available N (mg kg-¹)

Microbial biomass C (mg kg-¹)

Control

0.80a

12.5a

45.3a

150.2a

Biochar

0.95b

15.8b

50.1b

180.4b

PGPR

0.87a

16.2b

52.4b

200.6c

Biochar + PGPR

1.03c

17.0c

55.3c

245.6d

 

The nutrient cycling hypothesis proposes that biochar typically has a high cation exchange capacity (CEC, typically 20–50 cmol kg-¹), which can store very important cations, such as NH₄and K, and that PGPR organisms have enzymes (e.g., phosphatases and nitrogenases), that can solubilize phosphorus and fix nitrogen and increase the availability of nutrients in the soil (Zhang et al., 2020). Biochar is also capable of furthering the stabilization of labile nutrients by sorbing organic compounds and leading a reduction of nutrient leaching, thus providing a microenvironment suitable for PGPR populations to inhabit (DeLuca et al., 2023). For example, biochar has oxygen-containing functional groups such as carboxyl (–COOH) and hydroxyl (–OH) to retain nutrients, and could lead to the reduced loss of nutrient from sandy loam soils with low inherent CEC (Li et al., 2023).

Additionally, biochar-amended soils can support different microbial community dynamics where some beneficial taxa such as Bacillus and Pseudomonas appear to gain favour and can support nitrogen fixation and produce siderophores as well as tolerate salinity stress via the production of extracellular polysaccharides (Bashan et al., 2021; Bano et al., 2023). PGPR also secrete extracellular enzymes, such as ureases and proteases, which will mineralize organic nitrogen and further increases in the amount of available nitrogen (Backer et al., 2020). These type of synergistic interactions will work most effectively in arid environments of low organic matter and high salinity levels with limited microbial activity and therefore nutrient availability (Hussain et al., 2020). The improved performance from the BC + PGPR treatment is likely because of the complementary roles of BC as a physical scaffold, and PGPR as a biological catalyst in order to improve soil fertility at larger-scale than either of the amendments alone (Silva et al., 2024).

 

Crop productivity

Wheat grain yield was increased by 42.3% in the biochar + PGPR treatment (4.23 t ha-¹ vs. 2.98 t ha-¹; P < 0.05; Figure 3). WUE increased from 1.02 kg m-³ to 1.45 kg m-³ suggesting improved nutrient and water uptake (Farooq et al., 2020; Li et al., 2023). The rhizosphere priming effect likely enhanced root exudation which stimulated the efficiency of PGPR activity and nutrient uptake (Peng et al., 2021). This effect is attributable to biochar as a porous material that enhances soil retention of water and also provides a better microenvironment for root growth and microbial activity which will increase the production of root exudates (Jin et al., 2021). Rhizodeposits from crops are enriched in sugars and organic acids and are carbon sources for PGPR and increase the metabolic activity of PGPR and nutrient mobilization (Liu et al., 2022). The nutrient cycling hypothesis suggests that the CEC (20–50 cmol kg-¹) and water-holding capacity of biochar (which could be up to 50% larger than control soils) would provide PGPR with additional assistance decomposing organic matter that contained soluble phosphorus and gaseous nitrogen substrates to further increase soil nutrient availability for wheat (Zhang et al., 2020) (Table 2).

 

Table 2: Effect of treatments on wheat productivity

Treatment

Grain yield (t ha-¹)

WUE (kg m-³)

Chlorophyll content (SPAD)

Control

2.98a

1.02a

35.6a

Biochar

3.45b

1.18b

39.2b

PGPR

3.62b

1.24b

40.5b

Biochar+PGPR

4.23c

1.45c

44.8c

 

 

PGPRs such as Bacillus subtilis and Pseudomonas fluorescens produce natural plant hormones called auxins and gibberellins that promote root elongation and branching, respectively; thus, in arid conditions, this enhances nutrient and water uptake (Khan et al., 2020). As shown in the Figure 2 the present case, biochar + PGPR treatment combination had increased chlorophyll content (44.8 SPAD units vs. 35.6 in control), thereby providing a metabolic advantage for photosynthesis and consequently, biomass accumulation (Liu et al., 2022). There will be significant limitations to crop growth potential in arid soils where water and nutrients are limited to crops, however biochar will hold moisture in the soil and provide some relief from drought stress while PGPR will produce siderophores, and enzymes that relieve stress (e.g., ACC deaminase), thus enhancing crop resilience to salinity affected soil and heat stress (Nadeem et al., 2020; Farooq et al., 2020). The improved performance of the combination treatment could be attributed to biochar’s improvement of soil physical parameters, which would improve water retention, and the positively affect plant physiology that PGPR have on plants; thus, constituting a beneficial system to optimise crop productivity in the arid and barren soils of Iraq (Silva et al., 2024).

 

Table 3: Effect of treatments on soil physical properties

Treatment

Bulk density (g cm-³)

Porosity (%)

Aggregate stability (%)

Control

1.60a

39.5a

55.2a

Biochar

1.50b

43.2b

62.8b

PGPR

1.58a

40.1a

57.1a

Biochar + PGPR

1.40c

45.5c

68.4c

 

Soil physical properties

The biochar + PGPR treatment lowered bulk density by 12.5% (1.40 g cm-³ vs. 1.60 g cm-³) and increased total porosity by 15.2% (Table 3) and thereby can improve root growth and water infiltration, similar to studies conducted that used biochar soils (Zhang et al., 2020; Li et al., 2023). Biochar’s highly porous structure, more than 200 m² g-¹ for surface area, affects soil formation by improving inter-particle bonding and reducing compaction, in turn creating additional pore space for water movement and root growth (Peng et al., 2021; Tian et al., 2021). The conditional hydrology of the soil is determined by hydraulic conductivity and the improvement from the biochar treatment will improve the amount of hydraulic conductivity, which improves the capacity for moisture and water management which is particularly important in arid areas were low moisture conditions reduce growing conditions for crops (Lal et al., 2020). The sorption dynamics of biochar are affected through water-holding capacity which can increase up to 50%, depending on conditions, which can reduce drought stress to some degree with scarce water conditions and is related to the highly specific surface area and oxygen-containing groups on the biochar (e.g., carboxyl, hydroxyl) (Gul et al., 2021). In addition, biochar also fosters the development of stable soil aggregates through physical entanglement and the adsorptive characteristics of organic matter, which can improve soil structure and reduce erosion risks in sandy loam soils common for Iraq (Sharma et al., 2021). PGPRs improve soil structure through the production of exopolysaccharides that are biological adhesives that extend to bind soil particles into stable aggregates also resulting in improved soil cohesion (Bashan et al., 2021) and this synergism between biochar and PGPR is most evident in the biochar + PGPR treatment. Biochar provides a long-term matrix to stimulate microbial activity and the exopolysaccharides from PGPR enhance the stability of aggregates, resulting in a 68.4% increase in stability, versus a 55.2% increase observed in control (Table 3) and also shown in Figure 3. These improvements provide a more favorable environment for roots that maximizes nutrient and water uptake, which is critical to provide for wheat productivity in arid settings (Iqbal et al., 2023).

 

Soil microbial and chemical properties

The biochar + PGPR treatment dramatically increased bacterial counts and slightly decreased soil pH (from 7.8 to 7.4) and electrical conductivity (EC, from 2.1 to 1.8 dS m-¹), potentially reducing salinity stress conditions in arid soils (Li et al., 2023; Bano et al., 2023). Biochar’s highly porous structure, with a variety of pore sizes (ranging from micro pores to macro pores), acts as a habitat for colonization by microbes, allowing them to be protected from environmental stressors, such as desiccation and high salinity, while improving nutrient cycling (Jin et al., 2021; Gul et al., 2021). The microbial community dynamics model suggests that biochar increases microbial diversity, as it provides helps deliver a carbon-rich matrix to support multi-species PGPR colonization, such as species of Bacillus subtilis or Pseudomonas fluorescens. Multi-species PGPR can also produce phytohormones (e.g., auxins, gibberellin) and also siderophores to help support plant tolerance to stress (Peng et al., 2021). Multi-species PGPR can also secrete extracellular enzyme, such as phosphatases and ureases that can help mineralize organic phosphorus and nitrogen and add to the pool of readily available nutrients (Liu et al., 2022). The decline in soil pH and EC occurred due to biochar’s buffering capacity with its functional groups (e.g. carboxyl, phenolic) and surface area which can neutralize alkaline ions and PGPR can generate organic acids (e.g. gluconic acid) that will counter soil alkalinity especially in dry areas (Li et al., 2023). In addition, biochar decontaminates salts (e.g., adsorptions) and lowers soil solution salinity which decreases osmotic stress creating a favorable environment for microbes and plants as shown in Figure 4 (Tariq et al., 2021). The interaction between biochar and PGPR may also promote microbial biomass and activity since biochar produces stable carbon, and PGPR produce secondary metabolites that enhance the chemical properties of soils and normalized plant tolerance/resilience to saline-alkaline soils in Iraq (Ahmed et al., 2022).

Discussion

The biochar and PGPR treatment had an effect on soil fertility and wheat productivity, and reflects the rhizosphere priming effect , which enhances microbial activity, stimulating nutrient mineralisation (Gul et al., 2021; Peng et al., 2021). The nutrient cycling hypothesis describes enhancements to nutrient availability, as biochar has a high cation exchange capacity (CEC) which retains nutrients, while PGPR also solubilises phosphorus and fixes atmospheric nitrogen to increase nutrient uptake (Liu et al., 2022). The sorption dynamics of biochar reduce nutrient leaching, stabilise labile nutrients, and therefore creates a localised and beneficial microhabitat persistence of PGPR which produce enzymatic products as phosphatases and nitrogenases (DeLuca et al., 2023). According to microbial community dynamics model, biochar may change the structure of microbial diversity away from detrimental taxa towards beneficial taxa (for example, Bacillus and Pseudomonas), that enhance nutrient cycling and stress tolerance (Bano et al., 2023).

These processes are essential in a semi-arid country like Iraq, where agriculture is limited by salinity in soils and a lack of water (Hussain et al., 2020; Ahmed et al., 2022). As is documented in the literature, biochar improves root establishment and water infiltration by reducing soil bulk density and increasing porosity, while addressing the limitations associated with growing crops in an arid region (Sharma et al., 2021; Tian et al., 2021). Furthermore, the lowering of pH and EC will work towards addressing salinity stress levels and improve uptake of nutrients, consistent with similar studies in other arid regions (Gul et al., 2021; Zhang et al., 2020). Future study will need to explore various metrics on the costs of biochar production, its potential PGPR application, as well as the impact associated with longer-term planting of crops (for instance, barley or date palms) (Iqbal et al., 2023; Silva et al., 2024).

Conclusions and Recommendations

In this study concluded Bio compression of biochar and native PGPR has a tremendous effect on fertility of the soil, soil structure and wheat yield in the arid regions of Iraq. It enhances the soil organic carbon, nutrient density, and yield of grains and decreases bulk density, salinity and moisture stress. An environmentally friendly solution to enhance soil health, promote food security, and uptake resistance to land degradation is the use of locally made date-palm biochar and native PGPR in promoting climate-intelligent, low-cost, and scalable agriculture.

Acknowledgments

Our sincere thanks go to the University of Basrah and the Iraqi Ministry of Agriculture (Grant No. AG2023-015) for their generous financial and logistical support, without which this research would not have come to fruition. Special thanks are due to the Department of Soil Science at the University of Basrah, which provided access to laboratory facilities, field equipment, and technical support during the experiment implementation. We would also like to acknowledge the support of the Agricultural Research Directorate in Basrah for selecting sites and constructing irrigation infrastructure.

Novelty Statement

This study demonstrates the synergistic potential of biochar and indigenous PGPR to enhance soil fertility and wheat productivity in arid Iraq.

Authors’ Contributions

Ibrahim Ayad jihad: Designed the study, Conducted the microbial analysis.

Eatidal Akram Farhan and Aseel Ehsan Mahmoud: Designed the study, Conducted the microbial analysis, Conducted the microbial analysis.

Alaa Saleh Mahdi: Designed the study, Conducted the experiments.

Maryam Mansoor Mathkoor: Conducted the experiments.

Mustafa Mudhafar: Conducted the microbial analysis.

All authors read and approved the final manuscript.

Generative AI and AI-assisted technology statement

In this study do not used any Ai application.

Conflict of Interest

The authors declare that they have no conflict of interest.

References

Abbas, T., A. Hameed, A. Ahmed, M. Shahid, & S.M. Nadeem. 2022. Combined application of biochar and PGPR enhances wheat growth and nutrient uptake under saline conditions. Agric. Water Manag., 265: 107560. https://doi.org/10.1016/j.agwat.2022.107560

Ahmed, S.H., A.H. Al-Falahi, and R.M. Al-Saadi. 2022. Synergistic role of PGPR and biochar in restoring saline soils in Iraq. J. Environ. Manage., 307: 114522. https://doi.org/10.1016/j.jenvman.2022.114522

Backer, R., Rokem, J. S., Ilangumaran, G., Lamont, J., Praslickova, D., Ricci, E., Subramanian, S., and Smith, D.L., 2020. Plant growth-promoting rhizobacteria: Context, mechanisms of action, and roadmap to commercialization of biostimulants for sustainable agriculture. Front. Pl. Sci., 11: 559. https://doi.org/10.3389/fpls.2020.00559

Bano, A., A. Ullah, and A. Nosheen. 2023. Harnessing rhizobacteria to enhance crop production under water deficit conditions. Microbiol. Res., 266: 127239. https://doi.org/10.1016/j.micres.2022.127239

Bashan, Y., de-Bashan, L.E., Prabhu, S.R. and Hernandez, J.P., 2021. Advances in plant growth-promoting bacterial inoculant technology: Formulations and practical perspectives (1998–2021). Pl. Soil, 378(1–2): 1–33. https://doi.org/10.1007/s11104-013-1956-x

DeLuca, T. H., Gundale, M. J., MacKenzie, M. D., and Jones, D. L., 2023. Biochar effects on soil nutrient transformations, microbial dynamics, and plant productivity in agricultural systems. Soil Biol. Biochem., 182: 109021. https://doi.org/10.1016/j.soilbio.2023.109021

Farooq, M., M. Nawaz, A. Hussain, and S.S. Alghamdi. 2020. Drought stress in wheat: Physiological, biochemical and molecular mechanisms. Plant Physiol. Biochem., 151: 78–89. https://doi.org/10.1016/j.plaphy.2020.03.043

Gul, S., J.K. Whalen, B.W. Thomas, and V. Sachdeva. 2021. Changes in microbial community structure and activity following biochar application. Agriculture, Ecosys. Environ., 319: 107566. https://doi.org/10.1016/j.agee.2021.107566

Hussain, I., M. Khan, and S. Ahmad. 2020. Land degradation and soil erosion in arid regions: Causes and management. J. Arid Environ., 180: 104206. https://doi.org/10.1016/j.jaridenv.2020.104206

Iqbal, M.M., A. Khan, & S. Anwar. 2023. Drought tolerance in wheat: Insights from physiological and molecular mechanisms. Plant Physiol. Biochem., 196: 234–246. https://doi.org/10.1016/j.plaphy.2023.01.014

Jin, H., S. Capareda, Z. Chang, J. Gao, Y. Xu, & H. Huang. 2021. Biochar pyrolysis, properties, and applications in sustainable agriculture: A review. Bioresour. Technol., 319: 124210. https://doi.org/10.1016/j.biortech.2020.124210

Jadah, N.A. and T.S. Al-Rubaye. 2025. Evaluation of how laser photostimulation at two wavelengths alters the antimicrobial potential of Streptomycetes spp. Scient. Repor., 15(1): 28882.

Khan, N., A. Bano, and M.A. Babar. 2020. The role of PGPR in plant drought tolerance: Current perspective. Environ. Experimen, Bot., 176: 104038. https://doi.org/10.1016/j.envexpbot.2020.104038

Khan, Z., M. Rafiq, and M.J. Akhtar. 2022. Biochar and PGPR alleviate salinity stress in wheat by modifying root architecture and soil microbial activity. Chemosphere., 305: 135373. https://doi.org/10.1016/j.chemosphere.2022.135373

Lal, R., D. Reicosky, and J.D. Hanson. 2020. Improving soil water retention with biochar in arid ecosystems. Catena., 190: 104544. https://doi.org/10.1016/j.catena.2020.104544

Li, Y., Z. Wang, X. Wang, & Y. Liu. 2023. Biochar and compost interaction improves soil nutrients and crop productivity under saline conditions. Chemosph., 310: 136841. https://doi.org/10.1016/j.chemosphere.2022.136841

Liu, X., Y. Liu, J. Wang, & H. Zheng. 2022. Enhancing soil phosphorus availability through phosphate-solubilizing bacteria: A review. Soil Biol. Biochem., 168: 108620. https://doi.org/10.1016/j.soilbio.2022.108620

Nadeem, S.M., Z.A. Zahir, M. Naveed, & M. Ashraf. 2020. Drought mitigation through PGPR and biochar in wheat: Microbial and agronomic perspectives. Biotechnol. Advan., 42: 107579. https://doi.org/10.1016/j.biotechadv.2020.107579

Peng, X., Q. Zhu, and Y. Huang. 2021. Synergistic effects of biochar and beneficial microbes on soil health and crop yield. Sci. Tot. Environ., 763: 144204. https://doi.org/10.1016/j.scitotenv.2020.144204

Rehman, A., M. Imran, A. Bashir, & T. Mehmood. 2022. Biochar and microbial inoculants improve nutrient availability and wheat productivity in sandy loam soils. Ecotoxicol. Environ. Safe., 231: 113181. https://doi.org/10.1016/j.ecoenv.2022.113181

Sharma, S., A. Kharol, and P. Kaushik. 2021. PGPR-mediated mitigation of salinity and drought stress in cereals: A review. Rhizosphere., 18: 100341. https://doi.org/10.1016/j.rhisph.2021.100341

Silva, A.C., P.F. Martins, and R. de Souza. 2024. Synergistic effects of biochar and microbial consortia on wheat productivity under climate stress. J. Clean. Prod., 428: 139267. https://doi.org/10.1016/j.jclepro.2023.139267

Tariq, A., K. Pan, & M. Shahzad. 2021. Biochar application improves soil quality and plant growth in saline soils: A review. Environm. Technol. Innov., 21: 101313. https://doi.org/10.1016/j.eti.2020.101313

Tian, H., Y. Wang, & J. Sun. 2021. Biochar improves soil microbial community structure and wheat productivity in degraded soils. Appl. Soil Ecol., 165: 103968. https://doi.org/10.1016/j.apsoil.2021.103968

Wang, D., L. Liu, Y. Xu, & Y. Huang. 2020. PGPR-mediated root development and nutrient acquisition in wheat under water-limited conditions. Plant Sci., 298: 110583. https://doi.org/10.1016/j.plantsci.2020.110583

Zhang, Y., M. Abid, & X. Li. 2020. Role of biochar in improving nitrogen use efficiency and crop productivity. Agric. Ecosys. Environ., 295: 106891. https://doi.org/10.1016/j.agee.2020.106891