生物炭
壤土
导水率
钙质的
土壤水分
渗透(HVAC)
粒径
化学
土壤科学
环境科学
农学
材料科学
植物
热解
复合材料
生物
有机化学
物理化学
作者
Alaa Ibrahim,Adel R. A. Usman,Mohammad Ibrahim Al-Wabel,Mahmoud E. A. Nadeem,Yong Sik Ok,Abdulrasoul Mosa Al-Omran
标识
DOI:10.1080/03650340.2016.1193785
摘要
A laboratory column experiment was conducted to investigate the effects of 400°C biochar at application rate of 15 g kg−1 (21.9 t ha−1) with different particle sizes (<0.5 mm (S1), 0.5–1 mm (S2) and 1–2 mm (S3)) and application depths (0–2 cm depth (D0), 4–6 cm depth (D5) and 8–10 cm depth (D10)) on hydro-physical properties of sandy loam soil. The results indicated that applying biochar decreased the waterfront and saturated hydraulic conductivity of sandy loam soil. The cumulative evaporation was the highest and amounted to 40.9 mm in the non-treated soil, but it recorded the lowest amount of 32.2–35.5 mm in the biochar-treated soil. Applying biochar caused significant increases in the amount of conserved and retained water with the highest amount of water conserved in soil treated with S2 biochar at D5. Moreover, the cumulative water infiltration through the soil was significantly reduced by S1 and S2 biochars at D0. The values of saturated hydraulic conductivity for biochar treatments were significantly lower than those for the control, with the lowest values for S1 at D0 and D5. These results suggest positive improvement for the hydro-properties of coarse-textured soils following biochar addition, especially with finer particles of biochar.
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