Rainfall monitoring and distribution trends during crop period of 2022 and 2023
 
The analysis of rainfall patterns in this study provided the necessary climatic context for evaluating the eight treatments (T1-T8) outlined in the Methods section. Understanding the spatial and temporal variations in rainfall during the crop period is crucial for assessing the effectiveness of water conservation treatments in semi-arid environments. The comparative regression analysis of monthly rainfall (Fig 1) from June to December in 2022 and 2023 demonstrated a consistently declining rainfall trend in both years and linear regression equations derived for each dataset are depicted in Fig 1. The equations revealed a negative correlation in both years during the latter half, with a steeper rainfall deceleration in 2022. The higher intercept of the 2022 model indicates that the June rainfall is more than 2023. Rainfall peaked at 260 mm in August 2022 and 178 mm in September 2023. Both years showed declining rainfall from October, reaching near zero by November 2023, with 2022 maintaining higher levels until December. The year 2023 was generally drier than that of 2022. The 2023 reduction may be attributed to El Niño conditions weakening monsoon intensity 
(Wang et al., 2001), whereas 2022 likely experienced neutral or La Niña conditions enhancing rainfall 
(Ashok et al., 2001). Local factors, such as land-use change and urbanization, may influence rainfall variability. Despite similar seasonal patterns, reduced rain volumes and gradual peak formation indicate interannual climate variability effects.
Effect of in situ rainwater conservation practices on yield, morphological traits and energy indices of groundnut under semi-arid conditions
 
The evaluation of eight conservation treatments (T1-T8) showed improvements in groundnut yield, haulm, RWUE and energy indices (Table 1). T8 (subsoiling + furrow diking), T6 (subsoiling + conservation furrow) and T7 (subsoiling + broad bed and furrow) outperformed the control (T1). T8 achieved the highest pod yield at 361.2 kg ha
-1, a 288% increase over T1 of 93 kg ha
-1. T6 and T7 yielded 313 and 281.6 kg ha
-1, respectively 
(Li et al., 2020; Liang et al., 2019). For haulm yield, T8 recorded at 2420 kg ha
-1, T6 at 2299 kg ha
-1 and T3 at 1744.5 kg ha
-1 and T1 recorded at 1445 kg ha
-1. RWUE was highest in T8 at 0.888 kg ha
-1 mm
-1, compared to T1 at 0.228 kg ha
-1 mm
-1. T7 and T6 showed values of 0.769 and 0.692 kg ha
-1 mm
-1, respectively 
(Kugedera et al., 2022; Tefera et al., 2024). The treatment effects were significant at p≤ 0.05. Superiority of T8 stemmed from enhanced infiltration and root development 
(Singh et al., 2019; Olayinka et al., 2021; Veeramani et al., 2025). The yield distribution (Fig 2) showed that T8 contributed 20.3% of the total production, T7 at 17.6% and T6 at 15.9%, whereas T1 contributed 5.2% 
(Kumar et al., 2020; Rockström et al., 2010). T8 achieved the highest plant height (40 cm), density (26 plants m
-2) and root length (13 cm) (Fig 3). T6 showed the highest plant density (28 plants m
-2), whereas T7 had the longest root length (14 cm). T1 showed the poorest performance (17 plants m
-2, 32 cm height, 8 cm root length). Statistical analysis confirmed significant differences in CV for plant density (12.5%), height (9.8%) and root length (11.4%).
       
The assessment of energy inputs and outputs across the treatments (T1-T8) showed the impact of rainwater conservation on groundnut yield and energy efficiency (Table 1). The energy input for field operations ranged from 2352 to 4081 MJ ha
-1, with land preparation requiring the most energy. Treatments with extensive mechanization (T2, T7, T8 and T6) required higher energy inputs (7387-7687 MJ ha
-1) owing to the larger machinery. T8 achieved the highest energy output (47,717 MJ ha
-1), followed by T7 (43,536 MJ ha
-1) and T6 (34,254 MJ ha
-1), whereas T1 had the lowest (26,500 MJ ha
-1). Superior performance of T8 resulted from the combination of subsoiling and furrow diking, which improved soil structure and moisture retention during critical growth stages, consistent with the findings of 
Rockström  et al., (2010) and 
Tadesse et al., (2020). Conservation treatments enhance vegetative growth and moisture management. The energy ratios were highest in T8 (6.4%), T7 (5.9%) and T3 (5.8%), with T1 having the lowest ratio at 4.5%. T6 showed the lowest specific energy (20.6 MJ kg
-1) compared to T1 (63.3 MJ kg
-1). T8 achieved the highest energy productivity (0.048 kg MJ
-1) and net energy return (40,286 MJ ha
-1). These results demonstrate that integrated subsoiling and furrow-based strategies optimize biological and energy productivity in rainfed semi-arid systems 
(Oweis et al., 2012; Yadav et al., 2017).
 
Assessment of carbon footprint and carbon intensity indices in relation to crop yield
 
Pod CF values ranged from 524.8 ± 11.44 kg CO
2-eq ha
-1 (T1) to 864.5±58.35 kg CO
2-eq ha
-1 (T2) (Table 2). The shell CF varied between 209.9±4.58 (T1) and 345.8±23.34 (T2), while the haulm CF ranged from 501.6 to 794.7 kg CO‚ -eq ha
-1. The total biomass CF was lowest in T1 (532.3±49.2) and highest in T2 (863.3±62.8), with high-yield treatments (T6-T8) maintaining high CF values. The high CF under T2, despite moderate yield increases, indicates that early intensification leads to disproportionate emissions. High-yield treatments showed higher absolute CF but demonstrated better carbon efficiency per-unit yield. Similar patterns occur in cereal-legume systems, where intensification increases emissions while improving efficiency 
(Burney et al., 2010). Regression analysis showed a strong positive relationship between CF and yield components (Fig 4). As the yield increased, there was a notable reduction in carbon intensity (CI) values (Table 3). Specifically, the CI for pods decreased from 5.70±0.71 kg CO
2-eq kg
-1 in T1 to 2.32±0.19 kg CO
2-eq kg
-1 in T8, while the CI for shells declined from 14.25±1.77 to 5.79±0.47 kg CO
2 -eq kg
-1 across all treatments. Similar downward trends were observed for the CI of haulm and biomass. Regression models indicated negative linear correlations between CI and yield parameters (Fig 5). The shell yield showed the steepest reduction (slope = -0.062), followed by pods (-0.011), while biomass and haulm had gentler slopes, indicating the role of reproductive yield in decreasing CI. High R² values (>0.87) indicate that yield performance predicts CI outcomes, consistent with legume systems 
(Goglio et al., 2018). While yield intensification increases CF, it reduces CI, creating a productivity-emission trade-off. T6-T8 achieved the highest yields and lowest CI values, suggesting that productivity gains diluted maintenance emissions 
(Goglio et al., 2018; Nemecek et al., 2015). The positive CF-yield correlation across pods, shell, haulm and biomass indicates that higher yields require increased inputs, elevating emissions (
Lal, 2020). Pod CI decreased from 5.70 kg CO
2-eq kg
-1 in T1 to 2.32 kg CO
2-eq kg
-1 in T8, showing 60% reduced emissions. Shell yield showed the steepest CF regression slope, whereas pod yield showed the largest CI reduction. These findings indicate that optimizing inputs for higher yields enables carbon-efficient agriculture 
(Tilman et al., 2011; Burney et al., 2010).