Table 3 Impacts of biochar amendment in soil on the carbon sequestration potential
Biochar synthesis conditions | Type of studies | Soil type | Biochar application rate | Carbon sequestration potential | References |
---|---|---|---|---|---|
Corn silage, 500 °C | Lab-scale | Forests and agricultural soils | 1% (w/w) | No impact on forest soil, but reduced CO2 emission from the agricultural soil | |
Swine manure, 600–800 °C | Lab-scale | Rice paddy field | 2% (w/w) | Significant reduction of CO2 emission after biochar treatment | |
Reed straw, 400 °C (nZVI-biochar) | Lab-scale | Saline-alkali soil | 0.15–0.45% (w/w) | Significant reduction of CO2 emission after nZVI-biochar treatment | |
Corn cob, 250 °C | Lab-scale | Acidic sandy soil | ∼0.84% (w/w) | Reduction of CO2 emission by 11.8% | |
Rice husk, 700 °C | Lab-scale | Soil from university campus | 2% (w/w) | Reduction of CO2 emission by 80.29% | |
Rice husk, 700 °C (H3PO4-biochar) | Lab-scale | Soil from university campus | 2% (w/w) | Reduction of CO2 emission by 91.60% | |
Rice husk, 700 °C (H3PO4–nZVI-biochar) | Lab-scale | Soil from university campus | 2% (w/w) | Reduction of CO2 emission by 88.28% | |
Hard wood, 200–600 °C (Steam & CO2 activation) | Lab-scale | Topsoil (silt loom) | 0.75% (w/w) | Reduction of CO2 emission by 18% | |
Wood sawdust, 450 °C | Lab-scale | Surface soil | 3.2% (w/w) | Negative priming effects was observed with biochar treatment (−0.22 to –23.56 mg-CO2–C/g -soil-C) | |
Peanut shells, 400–500 °C | Lab-scale | Soil from an experimental field | ~1.4% (w/w) | Reduced CO2 emission by 23.61% | |
Rice straw, 500 °C | Lab-scale | Saline–Alkaline Soil (sandy loam) | ~0.77% (w/w) | Reduction of CO2 emission by 35.19% with addition of biochar as well as straw and urea | |
Wheat straw, 450 °C | Lab-scale | Irragric Anthrosols | ∼1.1% (w/w) | Biochar application decreased CO2 emission by an average of 23% | |
Rice husk, 300 °C | Lab-scale | Soil of Bungor Series | ∼0.54% (w/w) | Cumulative CO2 emission reduced by 139.41% compared to control | |
Wheat straw, 500–600 °C | Pot experiments | Clay loom soil | 50–95% (w/w) | CO2 emissions reduced by 8.05–31.46%. Higher CO2 emissions observed at higher biochar dose. | |
Corn stover, 550 °C | Pot experiments | Garden top soil | 3% (w/w) | CO2 emissions reduced by 15% compared to control soil | |
Pine wood, 500–700 °C | Pot experiments | Olton clay loam soil | 1% (w/w) | Reduced CO2 emission by 66.9–72.4% | |
Corn stalks, 400 °C | Microcosms | Coastal saline soil | 16 tons/hectare | Corn stalks-derived biochar showed higher GWMP (−3.84 to −3.17 tonne CO2-eq/hectare/tonne C) than control treatment (−0.11 tonne CO2-eq/hectare/tonne C). | |
Rice straw | Mesocosm | Rice paddy field | 6 tons/hectare | CO2 uptake increased by 43.5% and decreased the GWP by 375.6 g CO2-eq/m2/season | |
Multiple feedstocks, 280 °C | Pot experiments | Alkaline clay and acidic sandy soil | 4 tons/hectare | Biochar with N fertilizer addition reduced CO2 emission by 7–12% | |
Corn straw, 360 °C | Microcosm | Agricultural soil | 9 tons/hectare | Reduced CO2 emission by 11% | |
Farm wastes and wood residues, 500–550 °C | Field-scale | Andisol | 11 tons/hectare | Biochar amendment reduced CO2 fluxes. But, no significant differences in CO2 emission rates among different types of biochar treatments | |
Corn cobs, 500–550 °C | Field-scale | Haplic Acrisols | 0–30 tons/hectare | Specific maintenance respiration (qCO2) reduced by 66–73% | |
Maize straw. 350–550 °C | Field-scale | sandy-loam soil | 30 tons/hectare | Reduced CO2 emission by 33% | |
Corn straw, 450 °C | Field-scale | Sandy loam soil | 20 tons/hectare | Biochar addition enhanced SOC levels and reduced CO2 emissions |