Organic solid waste is disposed of using typical composting methods. Composting and vermicomposting use two biological mechanisms to turn organic waste into nutrient-dense organic manure. The traditional composting process is primarily dependent on microbial activity; however, in vermicompost, the breakdown is performed by the earthworm, which also interacts with microbes and promotes nutritional compositions. In addition, the enzyme present on the earthworm increases digestion and strongly promotes nutritional composting. In conventional waste disposal, composting procedures were used. First, garbage was collected, then shredding was done and finally aerobic decomposition, maturation and curing was done in solid waste disposal beds. This produces stable compost and improves soil fertility. Composting produces CO
2, water vapour and heat as organic matter decomposes through mineralization and humification
(Bernal et al., 2009; Epstein, 1997;
Tuomela et al., 2000). Earthworms such as
Eudrilus eugeniae work with bacteria in vermicomposting to accelerate the decomposition of organic waste. Following a brief pre-composting stage, earthworms devour and fragment waste, boosting microbial activity, nutrient mineralization and humus production. The resulting vermicompost is dark, granular, odourless and high in nutrients, beneficial bacteria, enzymes and plant growth-promoting compounds. The step wise composting process was shown in Fig 1a. In this study, we focused on the differences in macronutrient content between vermicompost and normal compost created from black tea waste and floral waste gathered from hotels, tea stores, flower markets and temples. The physicochemical characteristics of compost and vermicompost products were studied using products made with varying amounts of black tea waste (BTW) and floral waste (FW). Fig 2a depicts the pH and electrical conductivity findings of the treatments after traditional composting and vermicomposting. The results confirmed that the pH and EC values differed between compost and vermicompost, indicating earth worm activity. The vermicompost’s strong black color indicated significant humification and substrate stabilization. The pH of compost without earthworms varied from 6.82 in T1 (100% clay soil) to 7.24 in T3. The pH levels in vermicompost including
E. eugeniae ranged from 6.92 in T1 to 7.46 in T5. The higher pH seen in vermicompost than compost could be attributable to improved microbial breakdown, ammonification and mineralization of organic components by earthworm activity. Earthworms shred organic substrates and enhance microbial communities in the stomach and surrounding substrate, resulting in the production of ammonia and humic chemicals, which buffer the pH toward neutral. The pH of mature vermicompost ranges from near-neutral to slightly alkaline, indicating that the organic material has stabilized and matured enough to be used in agriculture. T5 had the highest pH of the treatments, indicating that increased quantities of floral debris assisted in the humification and breakdown processes.
Electrical conductivity (EC) increased gradually in all treatments after vermicomposting. Compost without earthworms showed EC values that ranged from 1.2 dS/m in T1 to 1.8 dS/m in T5. In contrast, vermicompost with
E. eugeniae showed higher EC values, ranging from 1.4 d/Sm in T1 to 2.4 dS/m in T5. The higher EC in vermicompost indicates that soluble mineral salts such as nitrogen, phosphorous, potassium, calcium and magnesium are more easily liberated during the breakdown process. Earthworm activity increases biodegradation by increasing aeration, enzymatic activity and microbial biomass, hence improving the conversion of complex organic compounds into plant-available nutrients. The greatest EC found in T5 indicates that treatments with bigger floral waste fractions had higher breakdown efficiency and nutrient release. The dark black colour of the vermicompost indicated that the substrate had undergone advanced humification and attained greater stability (
Moorthi and Nagarajan, 2011). The total organic carbon (TOC%) values from the compost and vermicomposting products are displayed in Fig 2b. We discovered that, depending on the composition ratio, the test sample’s TOC content gradually decreased. Vermicompost prepared with
Eudrilus eugeniae displayed a more notable decrease in TOC values (T1 to T5), whereas compost without earthworms had TOC values of about 48±3.2%. Vermicompost consistently had lower TOC levels than typical compost in all treatments, with the T1 showing a value of about 38±3.3% and the T5 recording 22±3.9%. The difference was statistically significant (p=0.003). The results revealed that the vermicompost method significantly composted organic matter while also rapidly decomposed and mineralized waste materials due to the combined activities of earthworms and microorganisms. Initially, Earthworm species mechanically split the substrate, increasing the surface area and making more phases available for microbial colonization, which enhances enzymatic breakdown and organic carbon oxidation. Microbial respiration breaks down carbonaceous compounds into simpler molecules, which are then released as CO
2. The decrease in TOC indicates the organic waste material’s stability and maturation. T5 (BTW 20% + FW 80%) had the lowest TOC value of all the treatments, indicating increased decomposition efficiency and organic matter transformation. The produced vermicompost’s are intense black colour and fine texture demonstrated advanced humification and stability
(Garg et al., 2006; Kaushik and Garg, 2004) all showed similar reductions in TOC during vermicomposting, attributing the carbon loss to microbial mineralization and earthworm-assisted decomposition.
The carbon/nitrogen (C/N) ratio is a good indicator of organic waste composting and quality. Fig 2b shows a gradual drop in the C/N ratio across all composting and vermicomposting treatments. In the absence of earthworms, compost’s C/N ratio decreased from 24±3.1 in T1 to 14±3.5 in T5. Vermicomposting with
E. eugeniae led to considerable reductions, from 18±2.3 in T1 to 11±2.6 in T5. Vermicompost consistently had lower C/N ratios than compost and the difference between treatments was statistically significant (p = 0.002). The C/N ratio decreases during vermicomposting, indicating higher decomposition efficiency, nitrogen availability and organic substrate stabilization. Microbial respiration reduces carbon content while enriching nitrogen through earthworm excretory products and microbial biomass, lowering the C/N ratio. Earthworm activity increases organic matter turnover, nitrogen mineralization and nutrient retention in the substrate. A lower C/N ratio is typically associated with mature and stable vermicompost appropriate for agricultural use. The lowest C/N ratio in T5 shows that treatments with higher quantities of floral waste perform better in terms of breakdown and nutrient enrichment. According to (
Senesi, 1989), mature vermicompost has a C/N ratio of 14 to 22, although values below 15 suggest advanced stability and maturity. Higher C/N ratios reported in T1 and T2 compost treatments may be due to the substrate’s higher carbonaceous content and slower breakdown rate.
Edwards et al. (2011) published similar findings, emphasizing the importance of the C/N ratio in determining mineralization and compost maturity during organic waste decomposition.
Fig 3 shows the macronutrient composition of compost and vermicompost made from various combinations of black tea waste (BTW) and floral waste (FW). In comparison to conventional composting, all vermicompost treatments showed significant increases in total nitrogen (TN), total phosphorus (TP) and total potassium (TK). Compost’s total nitrogen (TN%) content increased from 2.1±0.3% in T1 to 4.2±0.3% in T5. Vermicompost made with
Eudrilus eugeniae had higher TN values, ranging from 2.4 ±0.2% in T1 to 4.7±0.3% in T5. The increase in nitrogen concentration during vermicomposting can be due to improved microbial degradation, organic matter mineralization and earthworm secretion of nitrogenous metabolites. Earthworm activity hastens decomposition and boosts microbial communities that transform organic nitrogen into plant-available compounds like ammonium and nitrate. Mucus secretion, earthworm casts and microbial biomass all contribute to nitrogen enrichment in vermicomposts. Similarly, the total phosphorus (TP%) content increased gradually across all treatments. Compost treatments had TP values ranging from 1.5±0.2% in T1 to 3.1±0.4% in T5, whereas vermicompost had considerably greater phosphorus levels (2.0±0.2% in T1 to 3.9±0.3% in T5). The enhanced phosphorus availability in vermicompost may be attributed to phosphate-solubilizing bacteria and phosphatase enzymes present in the earthworm gut and vermicast, which facilitate the conversion of insoluble phosphorus into soluble and plant-available forms.
(Moorthi et al., 2016; Mahaly et al., 2018). The breakdown and humification processes also help to release phosphorus from complicated organic materials.
Total potassium (TK%) content increased significantly during vermicomposting. Compost TK levels varied from 1.9±0.2% in T1 to 3.5±0.3% in T5, while vermicompost had higher values of 2.5±0.2% in T1 to 4.1±0.2% in T5. The rise in potassium concentration may be linked to increased mineralization and microbial decomposition of organic materials, resulting in the release of exchangeable potassium ions from the substrate matrix. Earthworm-mediated fragmentation of organic wastes enhances nutrient mobilization and speeds up nutrient cycling during vermicomposting (
Mahaly et al., 2018).
Among all treatments, T5 (BTW 20% + FW 80%) had the greatest TN, TP and TK contents, indicating better nutrient enrichment and breakdown. The greater nutrient concentrations detected in vermicompost compared to compost show that
E. eugeniae is excellent at converting organic wastes into nutrient-rich biofertilizer. Statistical investigation demonstrated that compost and vermicompost had significantly different TN, TP and TK contents (p= 0.0001).
The enrichment of macronutrients in vermicompost may also be related to the reduction in total organic carbon and the concentration impact caused by organic matter mineralization. Earthworms increase nutritional availability through gut-associated microbial activity, enzyme release and the generation of growth-promoting compounds. The vermicompost’s black granular structure and stable nature supported the substrate’s advanced humification and maturity. (
Domínguez and Edwards, 2011;
Aira et al., 2007; Lazcano and Domínguez, 2011) and it also increases in TNPK contents after vermicomposting.
Fig 4 shows the variations in available nitrogen (AN), phosphorus (AP) and potassium (AK) in compost and vermicompost. Compost nitrogen levels increased from 0.5±0.01% in T1 to 1.9±0.2% in T5, while vermicompost had higher values ranging from 1.1±0.02% to 2.4±0.3%.
Similarly, the available phosphorus rose from 0.3±0.02% to 1.4±0.2% in compost and 0.8±0.02% to 1.9±0.2% in vermicompost. Potassium levels gradually increased from 0.7±0.01% to 1.8±0.2% in compost and 1.0±0.1% to 2.1±0.4% in vermicompost
(Ramesh et al., 2020). Vermicompost has considerably greater accessible nutrient levels than compost.
The enhanced availability of NPK nutrients in vermicompost may be associated with increased mineralization, microbial decomposition, and humification facilitated by earthworm activity. Earthworms fragment the substrate and stimulate microbial populations, thereby accelerating the release of nutrients into plant-available forms. Phosphatase enzymes present in the earthworm gut and vermicast can convert insoluble phosphorus into soluble and plant-available forms, thereby enhancing phosphorus availability (
Mahaly et al., 2018;
Moorthi et al., 2016). T5 (BTW 20% + FW 80%) had the maximum nutritional availability, indicating improved breakdown and nutrient enrichment. previous reports
(Singh et al., 2011 and
Raihing and Vijayalakshmi (2022) also reported similar results and the improved nutrient availability in vermicomposted organic wastes was observed.
Fig 5 depicts differences in calcium (Ca) and magnesium (Mg) content in compost and vermicompost. Compost calcium concentration rose from 1.5±0.2% in T1 to 2.3±0.3% in T5, while vermicompost had higher values ranging from 1.8±0.2% to 2.9±0.3%. Similarly, total magnesium concentration increased from 1.3±0.1% to 2.1±0.2% in compost and from 1.6±0.1% to 2.7±0.3% in vermicompost. Vermicompost consistently had considerably more calcium and magnesium than compost (Ca: p = 0.002; Mg: p = 0.002).
The elevated calcium and magnesium levels in vermicompost may be attributed to earthworm intestinal activity, mineral transformation, and enhanced microbial activity during the decomposition process. (
Moorthi and Nagarajan, 2011;
Mahaly et al., 2018). Earthworm casts have been shown to include higher quantities of exchangeable calcium and magnesium due to better mineral solubilization and organic matter decomposition. The progressive increase of Ca and Mg from T1 to T5 demonstrates successful nutrient mineralization in treatments with greater floral waste fractions. (
Hartenstein and Hartenstein, 1981) found that vermicomposting caused similar increases in calcium and magnesium.
The findings showed that
Eudrilus eugeniae effectively transformed black tea and floral waste into nutrient-rich vermicompost with better physicochemical characteristics and nutrient availability than conventional composting. Vermicomposting increased organic matter stabilization and improved macro- and micronutrient enrichment, indicating that it has the potential to be an environmentally friendly and sustainable organic waste management technique for increasing soil fertility and crop yield.