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.
The highest ammonium concentration is recording in treatment H
5 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 H
0, representing increases of 124.16% and 112.72%, respectively. After 90 days, H
5 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 H
5 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.
Treatment H5 recorded the highest nitrosomonas numbers, reaching 19.03 and 5.94 × 10
5 cells g
-1 soil in rhizosphere and outside of rhizosphere soils, respectively, after 60 days, compared with 1.50 and 1.22 × 10
5 cells g
-1 soil in the control treatment. After 90 days, the corresponding values reached 12.63 and 1.85 × 10
5 cells g
-1 soil compared with 0.43 and 0.20 × 10
5 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 × 10
5 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 × 10
5 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.
Similarly, treatment H
5 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).