4.1. Soil physicochemical properties
The study yielded significant findings, particularly concerning bulk density, particle density, total porosity, electrical conductivity, pH levels, organic carbon, organic matter, oxidizable carbon, phosphorus levels, and potassium levels. The most notable improvements were evident in soils modified with activated biochar compared to non-amended soil. However, it is noteworthy that a slight increase in electrical conductivity and pH in biochar-treated soil could be attributed to the presence of salts from the biochar's ash content, as noted by Liang et al.52 and Saeed et al.53 Biochar has been noticed to stimulate microbial activity, promoting the decomposition of organic residues and thereby influencing the turnover of soil organic matter54. The introduction of biochar in soil alters its physical properties, fostering improved water infiltration and reducing the risk of water runoff, consequently increasing the saturation percentage10. The observed increase in organic carbon and oxidizable carbon content signifies a positive impact on soil health and fertility, as organic carbon plays a primary role in nutrient retention, water-holding capacity, improved microbial activity, and overall soil structure. This finding aligns with the notion that biochar acts as a stable organic carbon pool and C/N ratios in the soil, thereby influencing overall carbon dynamics55,56. The biochar enhances the nutrient level, including nitrogen, available phosphorus, and potassium, in the soil by increasing the cation exchange capacity of soil particles57.
The soil's SEM-EDX examination reveals that carbon, oxygen, magnesium, silicon, potassium, calcium, aluminium, and iron are the elements with the largest concentrations, followed by trace amounts of sodium and titanium. About 98% of the earth's crust is made up of oxygen, silicon, iron, aluminium, calcium, potassium, and sodium. The other 2% is made up of other elements. Additionally, feldspar and quartz dominate the continental crust58. Silica particles (also known as SiO2) contain a high Si and O concentration, indicating quartz material (almost 50% by weight). Also, most of the pure silica particles come from natural sources59. Furthermore, potassium and sodium belong to the feldspar group (sometimes known as alkali feldspars). The constituents of the soil under present study mostly include iron-bearing particles, silicified quartz, and feldspar. However, all of the samples (from 0 T/ha, 5 T/ha, 10 T/ha biochar supplemented soil) showed carbon content because of the peat formation60, but highest carbon content detected in 10 tons ha–1 supplemented soil might be due to addition of recalcitrant carbon from the biochar10. The biochar application in soil improves its structure which helps to enhance its water retention capability61. The presence of fine particles in biochar may lead to the decrease of saturated hydraulic conductivity62.
4.2. Influence of biochar supplementation on maize growth
Insufficient water availability led to reduced root and shoot biomass, and comparative growth rate in plants. This decline may be due to various factors, such as, limited water uptake due to limited soil moisture accessibility, root and shoot cell damage by oxidative stress, resource distribution by prioritizing functions over root and shoot development and loss of nutrient absorption63. Conversely, when biochar was applied into the soil, it significantly improved root and shoot, dry and fresh weight under water stress conditions. This improvement maybe due its advantageous effects, such as its ability to hold moisture in the soil, increasing nutrient availability through improved cation exchange capacity (CEC), promoting healthier root growth through a supportive soil structure, reducing soil compaction, mitigating oxidative stress, and fostering beneficial soil microbial communities64. These mutual benefits create a more helpful atmosphere for roots to access water and nutrients and shoots to continue photosynthesis and growth, eventually resulting in increased root and shoot mass even when facing water stress challenges.
Water stress led to decrease in leaf live and dehydrated mass weight, as well as a decline in leaf area in which are the consequences of limited water availability, which hinders the plant's ability to maintain turgor pressure, cell expansion, and overall leaf growth. Moreover, water stress can induce oxidative stress in leaves, damaging their growth and functioning65,66. On the flip side, when the biochar is applied in soil, it triggered an intensification in leaf live and dehydrated mass weight, as well as an expansion in leaf area under water stress conditions67. This improvement is accredited to several valuable effects of biochar, including enhanced soil moisture retention, improved nutrient availability, and reduced oxidative stress7. Biochar's capacity to reduce water stress ultimately results in healthier and more vigorous leaves, with increased biomass and leaf area even in the face of water restrictions.
There has been decline in net assimilation rate (NAR) of plants due to water stress which is primarily associated to the plant's fight to preserve optimal photosynthesis rates due to limited water availability. As a result, reduced photosynthetic activity hampers carbon assimilation, leading to decreased biomass production and, consequently, lower NAR68. Although, biochar application to soil can significantly boost the net assimilation rate (NAR) of plants under water stress. This enhancement is driven by biochar’s capacity to enhance soil water retention, promote nutrient availability, and make conditions favorable for leaf development, eventually leading to increased carbon assimilation and subsequently higher NAR, even under hydric stress69.
4.3. Influence on Physiological, biochemical and yield attributes
Water stress typically leads to increased oxidative stress in plant cells, which can result in membrane damage and instability. Dehydrated plants exhibited a reduction in MSI due to membrane lipid peroxidation triggered by the accretion of reactive oxygen species (ROS)70. This is common effect of all abiotic stresses mainly heavy metals, salinity, drought and heat and reported well in the literature66,71,72. In contrast, biochar-mixed soil provided a more favorable environment for plants under water stress. Biochar's ability to enhance water retention and nutrient availability helps maintain cell turgor and reduces oxidative stress73. Consequently, plants grown in biochar-amended soil revealed higher MSI values in contrast to those in non-amended soil under similar water stress situations. This observation highlighted the latent of biochar as a soil amendment to recover the membrane stability of plants and their capability to cope with water scarcity. Also, the membrane stability index (MSI) in maize is lower during the reproductive stage as compared with the vegetative stage, primarily as a consequence of water stress experienced during the reproductive phase74.
The water stress stimulated oxidative stress in plants, resultant in amplified malondialdehyde content as a marker of lipid peroxidation and cellular damage75. However, the application of biochar in soil can significantly alleviate the effects of water stress on MDA levels due to its water retention properties that help maintain soil moisture, reducing the severity of water stress and subsequently lowering oxidative stress. Additionally, biochar's ability to enhance nutrient availability and foster beneficial microbial communities in the rhizosphere can further bolster the plant's resilience to water stress, limiting the accumulation of MDA76. This double act of biochar in extenuating water stress and reducing MDA content underscores its potential as a sustainable soil amendment for enlightening plant health and tolerance to environmental challenges. The levels of malondialdehyde content were higher during the reproductive stage in comparison to the vegetative stage, linked to more severe condition77.
Protein content in plants was seen to be decreased under limited moisture level as the reduced water availability restricts various metabolic processes, including protein synthesis. The hydration-deficiency-related decline in protein content can result in a cooperated capability for plants to carry out essential functions and bear environmental contests78. Though, the biochar application in the soil exhibits a mitigating effect on decrease in protein content. As a result, protein synthesis and metabolic procedures can continue more efficiently to increase protein content under drought situations79. The protein content was higher during the reproductive stage in comparison to the vegetative stage80, possibly due to decrease in photosynthesis at initial stages of crop while the protein content was seen higher at reproductive stage which is possibly due to new stress proteins expression81.
The hydric stress sources oxidative damage in plants, leading to the overrun of reactive oxygen species (ROS), which can damage cellular components82. Subsequently, the superoxidase dismutase, peroxidase, and catalase activity increased as a resistance mechanism to counteract reactive oxygen species and ease cellular damage83. This is an innate behavior of plants to uplift antioxidant enzymes activities as first line of defense against abiotic stresses and is documented well in previous literature66,84,85. Though, the introduction of biochar into the soil moderated the effects of water stress on these antioxidant enzymes. The ability of activated biochar enhances the retention of soil water and lightens the strictness of drought, thus, reducing the need for excessive ROS scavenging by antioxidant enzymes, i.e. SOD, POD, and CAT resulting enzymes in more concentration86. The SOD, POD, and CAT activity has been seemed to be increased in water stress conditions, and application of biochar in soil resulted in growing of these enzymes activity and this increase in activity due to link with better plant and soil relations87. Moreover, biochar's influence on soil nutrient accessibility and microbial communities indirectly influences enzyme activity88. The activity of peroxidase and catalase at reproductive stage was noted to be more than vegetative stage89, where a decrease in the activity of superoxidase dismutase activity has been noted at reproductive stage in parallel to vegetative stage90. The dual action of biochar, in moderating water stress and controlling enzyme activity, highlights its potential as a sustainable soil supplement for enhancing plant flexibility to environmental stressors.
The water stress exerted a negative impact on crop yield parameters such as cob length, cob weight, kernel number, total seeds per cob, grain yield per hectare, stover yield, and apparent water productivity, as reduced soil moisture hinders various physiological processes in plants91. However, the mixture of biochar into soil lessened the negative impacts of water stress on different yield limiting factors. The water retention properties of activated biochar help maintain consistent soil moisture levels, thus mitigating the severity of water stress and supporting essential physiological functions92. Also, biochar improves nutrient availability, soil structure, and endorses beneficial microbial communities, all of which contribute to better crop resilience and higher yield parameters, even in the condition of water stress.
An interesting finding in this study relates to the dosage of activated biochar. It was obvious that the 5 tons/ha biochar amendment yielded more promising outcomes in terms of physiological, biochemical, and yield parameters as compared to the 10 tons/ha biochar amendment. This observation elevates the likelihood of diminishing returns associated with higher biochar doses, potentially attributed to a limitation in nitrogen (N) uptake at the higher dosage level93. In essence, the optimal biochar dosage seems to strike a delicate balance between enhancing plant responses and avoiding nutrient oversaturation, highlighting the importance of fine-tuning biochar application rates for maximal benefits in agricultural practices.