UK Biochar Research Centre, School of Geosciences, University of Edinburgh, Crew Building, Alexander Crum Brown Road, Edinburgh EH9 3FF, UK.
UK Biochar Research Centre, School of Geosciences, University of Edinburgh, Crew Building, Alexander Crum Brown Road, Edinburgh EH9 3FF, UK.
Sci Total Environ. 2020 Apr 20;714:136857. doi: 10.1016/j.scitotenv.2020.136857. Epub 2020 Jan 22.
Biochar can significantly alter water relations in soil and therefore, can play an important part in increasing the resilience of agricultural systems to drought conditions. To enable matching of biochar to soil constraints and application needs, a thorough understanding of the impact of biochar properties on relevant soil parameters is necessary. This meta-analysis of the available literature for the first time quantitatively assess the effect of not just biochar application, but different biochar properties on the full sets of key soil hydraulic parameters, i.e., the available water content (AWC), saturated hydraulic conductivity (K), field capacity (FC), permanent wilting point (PWP) and total porosity (TP). The review shows that biochar increased soil water retention and decreased K in sandy soils and increased K and hence decreased runoff in clayey soils. On average, regardless of soil type, biochar application increased AWC (28.5%), FC (20.4%), PWP (16.7%) and TP (9.1%), while it reduced K (38.7%) and BD (0.8%). Biochar was most effective in improving soil water properties in coarse-textured soils with application rates between 30 and 70 t/ha. The key factors influencing biochar performance were particle size, specific surface area and porosity indicating that both soil-biochar inter-particle and biochar intra-particle pores are important factors. To achieve optimum water relations in sandy soils (>60% sand and <20% clay), biochar with a small particle size (<2 mm) and high specific surface area and porosity should be applied. In clayey soil (>50% clay), <30 t/ha of a high surface area biochar is ideal.
生物炭可以显著改变土壤中的水分关系,因此可以在提高农业系统对干旱条件的恢复力方面发挥重要作用。为了使生物炭适应土壤限制和应用需求,需要彻底了解生物炭特性对相关土壤参数的影响。本研究首次通过荟萃分析定量评估了生物炭应用的影响,以及不同生物炭特性对全套关键土壤水力参数(即可用水含量 (AWC)、饱和导水率 (K)、田间持水量 (FC)、永久萎蔫点 (PWP) 和总孔隙率 (TP))的影响。综述表明,生物炭增加了沙质土壤的水分保持能力,降低了 K 值,并减少了粘质土壤的 K 值和径流量。平均而言,无论土壤类型如何,生物炭的应用都会增加 AWC(28.5%)、FC(20.4%)、PWP(16.7%)和 TP(9.1%),同时降低 K 值(38.7%)和 BD(0.8%)。生物炭在 30 至 70 吨/公顷的施用量下,对改善粗质地土壤的土壤水分特性最为有效。影响生物炭性能的关键因素是粒径、比表面积和孔隙率,表明土壤-生物炭颗粒间和生物炭内的孔隙都是重要因素。为了在沙质土壤(>60%砂和<20%粘土)中实现最佳水分关系,应使用粒径小(<2 毫米)、比表面积和孔隙率高的生物炭。在粘质土壤(>50%粘土)中,<30 吨/公顷的高表面积生物炭是理想的选择。