Sadowska Urszula, Zaleski Tomasz, Kuboń Maciej, Latawiec Agnieszka, Klimek-Kopyra Agnieszka, Sikora Jakub, Gliniak Maciej, Kobyłecki Rafał, Zarzycki Robert
Department of Machinery Exploitation, Ergonomics and Production Processes, Faculty of Production Engineering and Energetics, University of Agriculture in Krakow, Balicka 116 B, 30-149 Krakow, Poland.
Department of Soil Science and Agrophysics, University of Agriculture in Krakow, Al. Mickiewicza 21, 30-120 Krakow, Poland.
Materials (Basel). 2023 Feb 20;16(4):1737. doi: 10.3390/ma16041737.
Soils enriched with biochar are recommended as a cultivation grounds, especially in case they contain significant amount of sand. However, the interactions between biochar and plants, as well as the influence of the biochar on water retention, cultivation and air properties of soils, are still not obvious. The present study aimed to determine the impact of various biochar doses on soils used for soya cultivation, in comparison to soils maintained as black fallow soil, on their water retention and productivity, for the period of two years. Sunflower husk biochar (BC1) and biochar of leafy trees (BC2), in doses of 0, 40, 60, 80 t·ha, were used for field experiments. The water retention was investigated with porous boards in pressure chambers by a drying method. No differences in the hydrological properties of the soils that were differently managed (black fallow soil, crop) were observed following biochar application. Addition of BC1, in the amounts of 40, 60, and 80 t·ha, caused an increase in the plant available water capacity (AWC) by 15.3%, 18.7%, and 13.3%, respectively, whereas the field capacity (FC) increased by 7.4%, 9.4%, and 8.6% for soils without biochar. Application of BC2 analogously resulted in higher AWC, by 8.97, 17.2%, and 33.1%, respectively, and higher FC by 3.75, 7.5%, and 18.3%, respectively. Increasing the doses of BC1 and BC2, both on black fallow soils and soils enriched with soya, caused a rise in total porosity (TP) and drainage porosity (DP), and a decrease in soil bulk density (SBD). Biochar with a higher total area and higher porosity (BC1) applied to soils with soya cultivation resulted in lower reductions in AW and FC than BC2 in the second year of investigation.
富含生物炭的土壤被推荐用作耕地,特别是当它们含有大量沙子时。然而,生物炭与植物之间的相互作用,以及生物炭对土壤保水、耕作和空气性质的影响,仍然不明显。本研究旨在确定与保持为黑休耕地的土壤相比,不同剂量的生物炭对用于大豆种植的土壤在两年期间的保水能力和生产力的影响。采用向日葵壳生物炭(BC1)和阔叶树生物炭(BC2),剂量分别为0、40、60、80吨·公顷,进行田间试验。通过干燥法在压力室中用多孔板研究保水能力。施用生物炭后,未观察到不同管理方式(黑休耕地、作物地)土壤的水文性质有差异。施用40、60和80吨·公顷的BC1,分别使植物有效含水量(AWC)增加了15.3%、18.7%和13.3%,而对于未添加生物炭的土壤,田间持水量(FC)分别增加了7.4%、9.4%和8.6%。施用BC2同样使AWC分别提高了8.9%、17.2%和33.1%,使FC分别提高了3.7%、7.5%和18.3%。增加BC1和BC2的剂量,无论是在黑休耕土壤还是富含大豆的土壤上,都会导致总孔隙度(TP)和排水孔隙度(DP)增加,土壤容重(SBD)降低。在调查的第二年,将具有较高总面积和孔隙度的生物炭(BC1)施用于大豆种植土壤时,与BC2相比,AW和FC的降低幅度较小。