Effect of Soil Application of Humic Acid on Nitrogen Availability and Nitrifying Bacteria in the Rhizosphere of Sorghum (Sorghum bicolor L.)

N
Nihad A. Abbas1,*
H
Hajir Sajad Alassfar1
Z
Zainab Gatea Abed2
S
Saja Nadhim Hussein1
Q
Qais Ataallah Al-Amiri3
A
Asmaa Hussein Allawi Al-Dulaimi4
1Department of Soil Sciences and Water Resources, College of Agriculture, University of Al-Qadisiyah, Iraq.
2University Presidency, University of Al-Qadisiyah, Iraq.
3College of Arts, University of Babylon, Babylon, 51002, Iraq.
4Department of Soil Sciences and Water Resources, College of Agriculture, Wasit University, Iraq.

Background: Humic acid improves soil fertility, nutrient availability and microbial activity. This study evaluated the effects of different humic acid levels on nitrogen availability and nitrifying bacteria in rhizosphere and outside of rhizosphere soils of sorghum.

Methods: A pot experiment was conducted at the College of Agriculture, University of Al-Qadisiyah, Iraq, during the autumn season of 2025. were planted with Sorghum bicolor (L.) Moench on 15 July 2025. Six levels of humic acid (0, 2, 4, 6, 8 and 10 ml L-1) were applied using a completely randomized design (CRD) with three replicates. Sorghum plants were grown in plastic pots containing 20 kg of soil. Available ammonium (NH4+), nitrate (NO3-), numbers of nitrosomonas and nitrobacter, chlorophyll content and plant height were evaluated after 60 and 90 days of planting.

Result: The highest humic acid level (10 ml L-1) significantly increased nitrogen availability and nitrifying bacterial numbers in both rhizosphere and outside of rhizosphere soils. The highest concentrations of ammonium and nitrate reached 49.81 and 55.13 mg kg-1 soil, respectively, in the rhizosphere after 60 days of planting. The same treatment recorded the highest numbers of nitrosomonas and nitrobacter, reaching 19.03 × 105 and 11.26 × 105 cells g-1 soil, respectively. Chlorophyll content and plant height were also significantly improved, reaching 55.7 SPAD units and 96.2 cm after 90 days of planting.

Humic acid is an organic soil amendment high in organic matter that improves soil fertility through its effects on soil physical, chemical and biological properties. It stimulates root growth, nutrient uptake, enzymatic activity and chlorophyll formation, resulting in improved plant growth and productivity (Nardi et al., 2002; Cimrin and Yilmaz, 2005; El-Ghamry et al., 2009; Akıncı, 2011; Ameri and Tehranifar, 2012; Yildiz et al., 2023; Manna and Siddique, 2025).
       
Recent studies have shown that humic substances can be influence the activity of microorganisms responsible for nitrification and nitrogen mineralization, resulting in improved balance among forms of nitrogen in soil and increased nitrogen availability for plants (Jin et al., 2024).
   
The rhizosphere is a biologically active zone in which nitrogen transformations are strongly influenced by root exudates and microbial activity. Root-derived carbon compounds stimulate microbial numbers and accelerate nitrogen cycling processes compared with soil outside the rhizosphere (Hu et al., 2021; Miao et al., 2026).
      
Although the beneficial effects of humic acid on soil fertility and plant growth have been widely reported, further studies are needed to better understand its effects on nitrogen availability and nitrifying bacteria populations in both rhizosphere and outside-rhizosphere soils under sorghum cultivation (Hu et al., 2021; Jin et al., 2024; Miao et al., 2026). Therefore, this study aimed to evaluate the effects of different humic acid levels on ammonium, nitrate, nitrosomonas and nitrobacter numbers, as well as chlorophyll content and plant height of sorghum.
The experiment was conducted in lathhouse of the Department of Soil Sciences, College of Agriculture, University of Al-Qadisiyah, Al-Diwaniyah, Iraq. during the autumn season of 2025. Plastic pots containing 20 kg of air-dried soil were planted with Sorghum bicolor (L.) Moench on 15 July 2025. Five seeds were planted per pot and thinned to one plant after 15 days. Potassium sulfate (100 kg K2O ha-1), triple superphosphate (200 kg P2O5  ha-1) and urea (320 kg N ha-1) in two additions, the first 15 days after planting and the second 30 days after the first additions, according to the experimental design. Standard irrigation, weed control and pest management practices were carried out uniformly for all treatments. Soil analyses were conducted according to Jackson (1958); Black (1965a, 1965b) and Page et al., (1982). Soil samples were collected at 60 and 90 days after planting. Soil adhering to the roots was considered rhizosphere soil, whereas soil collected away from the roots was considered outside of rhizosphere soil. At each sampling period, soil samples were collected from each of the three replicates of every treatment (H0-H5) for both rhizosphere and outside of rhizosphere soil. nitrosomonas and nitrobacter numbers were estimated using the MPN method, chlorophyll content was measured using a SPAD meter and plant height was measured at the flowering stage. Nutritional content of humic acid (according to the manufacturer) 20% Humicacids and fulvic acid , 25% organic matter, 5% N, 0% P and 10% K. The main physical, chemical and biological characteristics of the soil before planting are presented in Table (1). The humic acid levels and their corresponding treatment symbols used in the experiment are presented in Table (2).

Table 1: Some chemical, physical and biological characteristics of the soil before planting.



Table 2: Humic acid levels used in the study and their symbols.

Effect of humic acid on ammonium and nitrate concentration in soil
 
The results presented in Table (3) showed significant differences among humic acid levels in all rhizosphere and outside of rhizosphere soils during the two sampling periods. All humic acid treatments significantly increased ammonium and nitrate concentrations compared with the control treatment.

Table 3: Effect of humic acid on N-NH4+ mg kg-1 and on N-NO3- mg kg-1 ion concentration of rhizosphere soil and outside it for periods 60 and 90 days of planting.


       
The highest ammonium concentration is recording in treatment H5 during all study periods. After 60 days from planting, ammonium concentrations reached 49.81 and 54.33 mg kg-1 soil in rhizosphere and outside of rhizosphere soils, respectively, compared with 22.22 and 25.54 mg kg-1 soil in treatment H0, representing increases of 124.16% and 112.72%, respectively. After 90 days, H5 recorded 41.77 and 45.56 mg kg-1 soil compared with 17.49 and 19.32 mg kg-1 soil in the control treatment, with increases of 138.82% and 135.81%, respectively.
       
Similarly, nitrate concentrations increased significantly with increasing humic acid levels. Treatment H5 recorded the highest nitrate concentrations, reaching 55.13 and 57.42 mg kg-1 soil after 60 days and 44.33 and 49.36 mg kg-1 soil after 90 days in rhizosphere and outside of rhizosphere soils, respectively. These values were significantly higher than these of the control treatment, with increases ranging from 112.35% to 131.44%.
       
The increase in ammonium and nitrate concentrations with increasing humic acid levels indicates improved nitrogen availability and enhanced nitrogen transformation processes in soil. Humic acid promotes microbial activity and improves soil fertility by stimulating nitrogen mineralization and nitrification processes, In addition, humic acid improves soil structure, increases cation exchange capacity (CEC) and enhances nutrient retention, thereby reducing ammonium losses and maintaining a continuous supply of substrate for nitrification thereby increasing nitrogen availability for plant uptake.
       
These results agree with those reported by Nelson and Huber (2001), who indicated that humic substances improve nitrogen availability by enhancing soil fertility and nutrient retention. Tan (2003) also reported that humic acid stimulates nitrogen transformation processes and improves nutrient uptake by plants. Similarly, Patra et al., (2009) observed increased ammonium and nitrate concentrations following humic acid application due to enhanced microbial activity. Al-Taweel and Abo-Tabikh (2019, 2020) found that humic acid stimulated nitrogen mineralization and increased nitrogen availability in soil, while Jarallah and Rahi (2020) reported that enhanced nitrification activity promoted nitrate accumulation in agricultural soils.
       
Furthermore, Nitrogen concentrations generally decreased at 90 days compared with 60 days, which may be attributed to increasey plant uptake and nitrogen losses through biological and chemical transformation processes. Nitrate concentrations were generally higher than ammonium concentrations, reflecting the nitrifying of activity microorganisms responsible for the conversion of ammonium to nitrate (Okabe et al., 2010; Jarallah and Rahi, 2020). The simultaneous increase in ammonium and nitrate concentrations suggests that humic acid enhanced the overall nitrogen cycle by stimulating both nitrogen mineralization and nitrification processes.
       
Table (3) shows that ammonium and nitrate concentrations increased with increasing humic acid levels during all study periods, with the highest values recorded in treatment H5. Nitrogen concentrations decreased at 90 days compared with 60 days and were generally lower in the rhizosphere than outside of rhizosphere soil, which may be due to greater biological activity and nitrogen utilization in the root zone. Nitrate concentrations were generally higher than ammonium concentrations due to nitrification processes mediated by nitrosomonas and nitrobacter.
 
Nitrosomonas and Nitrobacter bacteria count × 105 cells g-1 soil
 
The results presented in Table (4) showed significant increases in nitrosomonas and nitrobacter numbers with increasing humic acid levels in all rhizosphere and outside of rhizosphere soils during the two sampling periods (60 and 90 days after planting). In general, bacterial populations increased progressively with increasing humic acid application and remained consistently higher in the rhizosphere than in the non-rhizosphere throughout the study period, indicating the favorable microbial environment associated with root activity.

Table 4: Effect of humic acid on the numbers of nitrosomonas and nitrobacter (´105 cells g-1 soil) in rhizosphere and outside of rhizosphere soils during the study periods (60 and 90 days after planting).


       
Treatment H5 recorded the highest nitrosomonas numbers, reaching 19.03 and 5.94 × 105 cells g-1 soil in rhizosphere and outside of rhizosphere soils, respectively, after 60 days, compared with 1.50 and 1.22 × 105  cells g-1 soil in the control treatment. After 90 days, the corresponding values reached 12.63 and 1.85 × 105 cells g-1 soil compared with 0.43 and 0.20 × 105 cells g-1 soil in the control treatment.
       
A similar response was observed for nitrobacter. Treatment H5 produced the highest populations, reaching 11.26 and 5.46 × 105 cells g-1 soil in the rhizosphere and non-rhizosphere, respectively, after 60 days. After 90 days, the corresponding values decreased to 1.88 and 1.65 × 105 cells g-1 soil, while the control treatment consistently recorded the lowest bacterial numbers throughout the experiment.
       
The gradual increase in nitrifying bacterial numbers with increasing humic acid levels demonstrates the beneficial role of humic substances in stimulating soil microbial activity. This effect can be due to improved organic carbon availability, enhanced nutrient retention, better soil structure and more favorable physicochemical conditions, all of which promote microbial growth and metabolic activity. In addition, humic acid enhances root development and root exudation, providing a continuous supply of readily available carbon compounds that stimulate the proliferation and activity of beneficial microorganisms, particularly within the rhizosphere.humic acid also acts as a source of biologically active organic compounds that provide energy and nutrients for soil microorganisms, thereby stimulating microbial proliferation and enhancing the abundance of nitrifying bacteria in the rhizosphere.
       
The consistently higher numbers of nitrosomonas and nitrobacter in the rhizosphere compared with the outside of rhizosphere may be attributed to the greater availability of root exudates, amino acids, sugars and other organic compounds released by plant roots. These compounds serve as important energy sources for soil microorganisms and create a biologically active environment that favors nitrifying bacteria responsible for nitrogen transformations (Innes et al., 2004; Meyhew, 2004).
       
The increase in nitrosomonas and nitrobacter populations indicates enhanced nitrification activity and improved nitrogen cycling efficiency in soil. As nitrosomonas oxidizes ammonium to nitrite and nitrobacter subsequently converts nitrite to nitrate, the increased abundance of these bacteria contributes to greater nitrogen availability for plant uptake. Furthermore, improved soil aeration and aggregation following humic acid application may have enhanced oxygen availability within soil pores. Since nitrification is an aerobic process, these conditions favor the activity of nitrifying bacteria and improve nitrogen transformation efficiency. Similar findings have been reported by Rui et al., (2024); Chen et al., (2024); Jin et al., (2024); Ma et al., (2024) and Qin et al., (2025). Guo et al., (2025); Han et al., (2025).
       
The reduction in bacterial numbers after 90 days compared with 60 days may be associated with the gradual depletion of readily available nutrients, increased competition among soil microorganisms and plant roots and age-related changes in root exudation during plant development, as well as the reduced availability of easily degradable carbon substrates as plant growth progressed, resulting in reduced microbial activity during the later growth stage. Similar explanations have been reported by Smalla et al., (2001); Bezbaruah and Zhang (2004) and Saito et al., (2007). Overall, the present findings are consistent with those of Tsuchiya et al., (2011); Okabe et al., (2012); Wu et al., (2017), confirming the positive role of humic acid in enhancing nitrifying bacterial populations and improving biological nitrogen transformations in soil.
 
Effect of humic acid on chlorophyll content and plant height of sorghum
 
The results presented in Table (5) showed significant differences among treatments, with chlorophyll content and plant height increasing progressively with increasing humic acid levels. Treatment H5 recorded the highest chlorophyll content, reaching 52.4 and 55.7 SPAD units after 60 and 90 days from planting, respectively, compared with 35.4 and 37.2 SPAD units in the control treatment, represented increased of 48.02% and 49.73%, respectively.

Table 5: Effect of humic acid levels on chlorophyll content and plant height during the study periods (60 and 90 days after planting).


       
Similarly, treatment H5 produced the greatest plant height, reaching 71.1 and 96.2 cm after 60 and 90 days from planting, respectively, compared with 48.7 and 70.2 cm in the control treatment, with increases of 45.99% and 37.03%, respectively.
       
The improvement in chlorophyll content and plant height may be attributed to the role of humic acid in enhancing nutrient availability and uptake, particularly nitrogen, magnesium and iron, which are directly associated with chlorophyll synthesis and plant growth. Increased chlorophyll content improves photosynthetic efficiency and promotes biomass accumulation, while the growth-regulating effects humic substances stimulate root development and stem elongation (Helaly, 2021; Chen et al., 2022; Zandonadi et al., 2025; Nabi et al., 2025; Al-Musawi et al., 2025). Similar findings were reported by Abu-Ria et al. (2024); Abdulmajeed et al., (2025) and Al-Bayaty and Raheem (2026).
Humic acid application significantly increased ammonium and nitrate availability, enhanced nitrosomonas and nitrobacter populations and improved chlorophyll content and plant height of sorghum. The highest application level (10 ml L-1) consistently produced the greatest values for all measured parameters in both rhizosphere and outside of rhizosphere soils. These results demonstrate the effectiveness of humic acid in improving nitrogen transformation, microbial activity and soil fertility, thereby supporting sorghum growth under the conditions of this study.
None.
 
Disclaimers
 
The views expressed in this article are those of the authors. The authors are responsible for the accuracy of the information presented.
 
Informed consent
 
Not applicable. This study did not involve human participants or experimental animals.
The authors declare no conflict of interest.

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Effect of Soil Application of Humic Acid on Nitrogen Availability and Nitrifying Bacteria in the Rhizosphere of Sorghum (Sorghum bicolor L.)

N
Nihad A. Abbas1,*
H
Hajir Sajad Alassfar1
Z
Zainab Gatea Abed2
S
Saja Nadhim Hussein1
Q
Qais Ataallah Al-Amiri3
A
Asmaa Hussein Allawi Al-Dulaimi4
1Department of Soil Sciences and Water Resources, College of Agriculture, University of Al-Qadisiyah, Iraq.
2University Presidency, University of Al-Qadisiyah, Iraq.
3College of Arts, University of Babylon, Babylon, 51002, Iraq.
4Department of Soil Sciences and Water Resources, College of Agriculture, Wasit University, Iraq.

Background: Humic acid improves soil fertility, nutrient availability and microbial activity. This study evaluated the effects of different humic acid levels on nitrogen availability and nitrifying bacteria in rhizosphere and outside of rhizosphere soils of sorghum.

Methods: A pot experiment was conducted at the College of Agriculture, University of Al-Qadisiyah, Iraq, during the autumn season of 2025. were planted with Sorghum bicolor (L.) Moench on 15 July 2025. Six levels of humic acid (0, 2, 4, 6, 8 and 10 ml L-1) were applied using a completely randomized design (CRD) with three replicates. Sorghum plants were grown in plastic pots containing 20 kg of soil. Available ammonium (NH4+), nitrate (NO3-), numbers of nitrosomonas and nitrobacter, chlorophyll content and plant height were evaluated after 60 and 90 days of planting.

Result: The highest humic acid level (10 ml L-1) significantly increased nitrogen availability and nitrifying bacterial numbers in both rhizosphere and outside of rhizosphere soils. The highest concentrations of ammonium and nitrate reached 49.81 and 55.13 mg kg-1 soil, respectively, in the rhizosphere after 60 days of planting. The same treatment recorded the highest numbers of nitrosomonas and nitrobacter, reaching 19.03 × 105 and 11.26 × 105 cells g-1 soil, respectively. Chlorophyll content and plant height were also significantly improved, reaching 55.7 SPAD units and 96.2 cm after 90 days of planting.

Humic acid is an organic soil amendment high in organic matter that improves soil fertility through its effects on soil physical, chemical and biological properties. It stimulates root growth, nutrient uptake, enzymatic activity and chlorophyll formation, resulting in improved plant growth and productivity (Nardi et al., 2002; Cimrin and Yilmaz, 2005; El-Ghamry et al., 2009; Akıncı, 2011; Ameri and Tehranifar, 2012; Yildiz et al., 2023; Manna and Siddique, 2025).
       
Recent studies have shown that humic substances can be influence the activity of microorganisms responsible for nitrification and nitrogen mineralization, resulting in improved balance among forms of nitrogen in soil and increased nitrogen availability for plants (Jin et al., 2024).
   
The rhizosphere is a biologically active zone in which nitrogen transformations are strongly influenced by root exudates and microbial activity. Root-derived carbon compounds stimulate microbial numbers and accelerate nitrogen cycling processes compared with soil outside the rhizosphere (Hu et al., 2021; Miao et al., 2026).
      
Although the beneficial effects of humic acid on soil fertility and plant growth have been widely reported, further studies are needed to better understand its effects on nitrogen availability and nitrifying bacteria populations in both rhizosphere and outside-rhizosphere soils under sorghum cultivation (Hu et al., 2021; Jin et al., 2024; Miao et al., 2026). Therefore, this study aimed to evaluate the effects of different humic acid levels on ammonium, nitrate, nitrosomonas and nitrobacter numbers, as well as chlorophyll content and plant height of sorghum.
The experiment was conducted in lathhouse of the Department of Soil Sciences, College of Agriculture, University of Al-Qadisiyah, Al-Diwaniyah, Iraq. during the autumn season of 2025. Plastic pots containing 20 kg of air-dried soil were planted with Sorghum bicolor (L.) Moench on 15 July 2025. Five seeds were planted per pot and thinned to one plant after 15 days. Potassium sulfate (100 kg K2O ha-1), triple superphosphate (200 kg P2O5  ha-1) and urea (320 kg N ha-1) in two additions, the first 15 days after planting and the second 30 days after the first additions, according to the experimental design. Standard irrigation, weed control and pest management practices were carried out uniformly for all treatments. Soil analyses were conducted according to Jackson (1958); Black (1965a, 1965b) and Page et al., (1982). Soil samples were collected at 60 and 90 days after planting. Soil adhering to the roots was considered rhizosphere soil, whereas soil collected away from the roots was considered outside of rhizosphere soil. At each sampling period, soil samples were collected from each of the three replicates of every treatment (H0-H5) for both rhizosphere and outside of rhizosphere soil. nitrosomonas and nitrobacter numbers were estimated using the MPN method, chlorophyll content was measured using a SPAD meter and plant height was measured at the flowering stage. Nutritional content of humic acid (according to the manufacturer) 20% Humicacids and fulvic acid , 25% organic matter, 5% N, 0% P and 10% K. The main physical, chemical and biological characteristics of the soil before planting are presented in Table (1). The humic acid levels and their corresponding treatment symbols used in the experiment are presented in Table (2).

Table 1: Some chemical, physical and biological characteristics of the soil before planting.



Table 2: Humic acid levels used in the study and their symbols.

Effect of humic acid on ammonium and nitrate concentration in soil
 
The results presented in Table (3) showed significant differences among humic acid levels in all rhizosphere and outside of rhizosphere soils during the two sampling periods. All humic acid treatments significantly increased ammonium and nitrate concentrations compared with the control treatment.

Table 3: Effect of humic acid on N-NH4+ mg kg-1 and on N-NO3- mg kg-1 ion concentration of rhizosphere soil and outside it for periods 60 and 90 days of planting.


       
The highest ammonium concentration is recording in treatment H5 during all study periods. After 60 days from planting, ammonium concentrations reached 49.81 and 54.33 mg kg-1 soil in rhizosphere and outside of rhizosphere soils, respectively, compared with 22.22 and 25.54 mg kg-1 soil in treatment H0, representing increases of 124.16% and 112.72%, respectively. After 90 days, H5 recorded 41.77 and 45.56 mg kg-1 soil compared with 17.49 and 19.32 mg kg-1 soil in the control treatment, with increases of 138.82% and 135.81%, respectively.
       
Similarly, nitrate concentrations increased significantly with increasing humic acid levels. Treatment H5 recorded the highest nitrate concentrations, reaching 55.13 and 57.42 mg kg-1 soil after 60 days and 44.33 and 49.36 mg kg-1 soil after 90 days in rhizosphere and outside of rhizosphere soils, respectively. These values were significantly higher than these of the control treatment, with increases ranging from 112.35% to 131.44%.
       
The increase in ammonium and nitrate concentrations with increasing humic acid levels indicates improved nitrogen availability and enhanced nitrogen transformation processes in soil. Humic acid promotes microbial activity and improves soil fertility by stimulating nitrogen mineralization and nitrification processes, In addition, humic acid improves soil structure, increases cation exchange capacity (CEC) and enhances nutrient retention, thereby reducing ammonium losses and maintaining a continuous supply of substrate for nitrification thereby increasing nitrogen availability for plant uptake.
       
These results agree with those reported by Nelson and Huber (2001), who indicated that humic substances improve nitrogen availability by enhancing soil fertility and nutrient retention. Tan (2003) also reported that humic acid stimulates nitrogen transformation processes and improves nutrient uptake by plants. Similarly, Patra et al., (2009) observed increased ammonium and nitrate concentrations following humic acid application due to enhanced microbial activity. Al-Taweel and Abo-Tabikh (2019, 2020) found that humic acid stimulated nitrogen mineralization and increased nitrogen availability in soil, while Jarallah and Rahi (2020) reported that enhanced nitrification activity promoted nitrate accumulation in agricultural soils.
       
Furthermore, Nitrogen concentrations generally decreased at 90 days compared with 60 days, which may be attributed to increasey plant uptake and nitrogen losses through biological and chemical transformation processes. Nitrate concentrations were generally higher than ammonium concentrations, reflecting the nitrifying of activity microorganisms responsible for the conversion of ammonium to nitrate (Okabe et al., 2010; Jarallah and Rahi, 2020). The simultaneous increase in ammonium and nitrate concentrations suggests that humic acid enhanced the overall nitrogen cycle by stimulating both nitrogen mineralization and nitrification processes.
       
Table (3) shows that ammonium and nitrate concentrations increased with increasing humic acid levels during all study periods, with the highest values recorded in treatment H5. Nitrogen concentrations decreased at 90 days compared with 60 days and were generally lower in the rhizosphere than outside of rhizosphere soil, which may be due to greater biological activity and nitrogen utilization in the root zone. Nitrate concentrations were generally higher than ammonium concentrations due to nitrification processes mediated by nitrosomonas and nitrobacter.
 
Nitrosomonas and Nitrobacter bacteria count × 105 cells g-1 soil
 
The results presented in Table (4) showed significant increases in nitrosomonas and nitrobacter numbers with increasing humic acid levels in all rhizosphere and outside of rhizosphere soils during the two sampling periods (60 and 90 days after planting). In general, bacterial populations increased progressively with increasing humic acid application and remained consistently higher in the rhizosphere than in the non-rhizosphere throughout the study period, indicating the favorable microbial environment associated with root activity.

Table 4: Effect of humic acid on the numbers of nitrosomonas and nitrobacter (´105 cells g-1 soil) in rhizosphere and outside of rhizosphere soils during the study periods (60 and 90 days after planting).


       
Treatment H5 recorded the highest nitrosomonas numbers, reaching 19.03 and 5.94 × 105 cells g-1 soil in rhizosphere and outside of rhizosphere soils, respectively, after 60 days, compared with 1.50 and 1.22 × 105  cells g-1 soil in the control treatment. After 90 days, the corresponding values reached 12.63 and 1.85 × 105 cells g-1 soil compared with 0.43 and 0.20 × 105 cells g-1 soil in the control treatment.
       
A similar response was observed for nitrobacter. Treatment H5 produced the highest populations, reaching 11.26 and 5.46 × 105 cells g-1 soil in the rhizosphere and non-rhizosphere, respectively, after 60 days. After 90 days, the corresponding values decreased to 1.88 and 1.65 × 105 cells g-1 soil, while the control treatment consistently recorded the lowest bacterial numbers throughout the experiment.
       
The gradual increase in nitrifying bacterial numbers with increasing humic acid levels demonstrates the beneficial role of humic substances in stimulating soil microbial activity. This effect can be due to improved organic carbon availability, enhanced nutrient retention, better soil structure and more favorable physicochemical conditions, all of which promote microbial growth and metabolic activity. In addition, humic acid enhances root development and root exudation, providing a continuous supply of readily available carbon compounds that stimulate the proliferation and activity of beneficial microorganisms, particularly within the rhizosphere.humic acid also acts as a source of biologically active organic compounds that provide energy and nutrients for soil microorganisms, thereby stimulating microbial proliferation and enhancing the abundance of nitrifying bacteria in the rhizosphere.
       
The consistently higher numbers of nitrosomonas and nitrobacter in the rhizosphere compared with the outside of rhizosphere may be attributed to the greater availability of root exudates, amino acids, sugars and other organic compounds released by plant roots. These compounds serve as important energy sources for soil microorganisms and create a biologically active environment that favors nitrifying bacteria responsible for nitrogen transformations (Innes et al., 2004; Meyhew, 2004).
       
The increase in nitrosomonas and nitrobacter populations indicates enhanced nitrification activity and improved nitrogen cycling efficiency in soil. As nitrosomonas oxidizes ammonium to nitrite and nitrobacter subsequently converts nitrite to nitrate, the increased abundance of these bacteria contributes to greater nitrogen availability for plant uptake. Furthermore, improved soil aeration and aggregation following humic acid application may have enhanced oxygen availability within soil pores. Since nitrification is an aerobic process, these conditions favor the activity of nitrifying bacteria and improve nitrogen transformation efficiency. Similar findings have been reported by Rui et al., (2024); Chen et al., (2024); Jin et al., (2024); Ma et al., (2024) and Qin et al., (2025). Guo et al., (2025); Han et al., (2025).
       
The reduction in bacterial numbers after 90 days compared with 60 days may be associated with the gradual depletion of readily available nutrients, increased competition among soil microorganisms and plant roots and age-related changes in root exudation during plant development, as well as the reduced availability of easily degradable carbon substrates as plant growth progressed, resulting in reduced microbial activity during the later growth stage. Similar explanations have been reported by Smalla et al., (2001); Bezbaruah and Zhang (2004) and Saito et al., (2007). Overall, the present findings are consistent with those of Tsuchiya et al., (2011); Okabe et al., (2012); Wu et al., (2017), confirming the positive role of humic acid in enhancing nitrifying bacterial populations and improving biological nitrogen transformations in soil.
 
Effect of humic acid on chlorophyll content and plant height of sorghum
 
The results presented in Table (5) showed significant differences among treatments, with chlorophyll content and plant height increasing progressively with increasing humic acid levels. Treatment H5 recorded the highest chlorophyll content, reaching 52.4 and 55.7 SPAD units after 60 and 90 days from planting, respectively, compared with 35.4 and 37.2 SPAD units in the control treatment, represented increased of 48.02% and 49.73%, respectively.

Table 5: Effect of humic acid levels on chlorophyll content and plant height during the study periods (60 and 90 days after planting).


       
Similarly, treatment H5 produced the greatest plant height, reaching 71.1 and 96.2 cm after 60 and 90 days from planting, respectively, compared with 48.7 and 70.2 cm in the control treatment, with increases of 45.99% and 37.03%, respectively.
       
The improvement in chlorophyll content and plant height may be attributed to the role of humic acid in enhancing nutrient availability and uptake, particularly nitrogen, magnesium and iron, which are directly associated with chlorophyll synthesis and plant growth. Increased chlorophyll content improves photosynthetic efficiency and promotes biomass accumulation, while the growth-regulating effects humic substances stimulate root development and stem elongation (Helaly, 2021; Chen et al., 2022; Zandonadi et al., 2025; Nabi et al., 2025; Al-Musawi et al., 2025). Similar findings were reported by Abu-Ria et al. (2024); Abdulmajeed et al., (2025) and Al-Bayaty and Raheem (2026).
Humic acid application significantly increased ammonium and nitrate availability, enhanced nitrosomonas and nitrobacter populations and improved chlorophyll content and plant height of sorghum. The highest application level (10 ml L-1) consistently produced the greatest values for all measured parameters in both rhizosphere and outside of rhizosphere soils. These results demonstrate the effectiveness of humic acid in improving nitrogen transformation, microbial activity and soil fertility, thereby supporting sorghum growth under the conditions of this study.
None.
 
Disclaimers
 
The views expressed in this article are those of the authors. The authors are responsible for the accuracy of the information presented.
 
Informed consent
 
Not applicable. This study did not involve human participants or experimental animals.
The authors declare no conflict of interest.

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