Water Retention, Air Exchange and Pore Structure Characteristics after Three Years of Rice Straw Biochar Application to an Acrisol

被引:20
|
作者
Obour, Peter Bikon [1 ,2 ]
Danso, Eric Oppong [3 ]
Yakubu, Adam [3 ]
Abenney-Mickson, Stephen [4 ]
Sabi, Edward Benjamin [5 ]
Darrah, Yvonne Kugblenu [6 ]
Arthur, Emmanuel [1 ]
机构
[1] Aarhus Univ, Dept Agroecol, Fac Sci & Technol, POB 50, DK-8830 Tjele, Denmark
[2] Univ Illinois, Dept Nat Resources & Environm Sci, 1102 S Goodwin Ave,MC-047, Urbana, IL 61801 USA
[3] Univ Ghana, Sch Agr, Forest & Hort Crops Res Ctr, POB LG 1195, Legon, Accra, Ghana
[4] Cent Univ, Sch Engn & Technol, DS 2310, Accra, Ghana
[5] Univ Ghana, Sch Engn Sci, Dept Agr Engn, POB LG 77, Legon, Accra, Ghana
[6] Univ Ghana, Sch Agr, Soil & Irrigat Res Ctr, POB LG 1195, Legon, Accra, Ghana
关键词
HYDROLOGICAL PROPERTIES; OXYGEN DIFFUSION; SOIL; PERMEABILITY; FLOW;
D O I
10.2136/sssaj2019.07.0230
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Biochar has been suggested as soil amendment for improving soil structure and associated functions for agricultural production. We investigated the impact of rice straw biochar application on soil water retention (SWR), air movement through soil, and soil pore characteristics of a tropical sandy clay loam field. A field experiment was conducted at the University of Ghana's Forest and Horticultural Crops Research Centre, Kade, Ghana, which comprised three treatments: soil without biochar (B0), and soil amended with 15 and 30 Mg ha(-1) of biochar (B15 and B30, respectively). Three years after biochar application, we sampled intact 100 cm(3) soil cores and measured SWR, air permeability (k(a)) and gas diffusivity (D-p/D-0), and quantified pore characteristics: tortuosity (t), effective pore diameter (d(B)) and the number of air-filled pores in a given soil cross-section (n(B)) at selected matric potentials. At all matric potentials (-10 to -15000 hPa), B30 considerably reduced SWR compared to B0, whereas the B15 had similar SWR as B0. Biochar did not significantly affect the plant available water (PAW). The B30 significantly increased k(a) at -30 hPa relative to B15. At a given air-filled porosity, the B30 tended to have larger D-p/D-0 values compared to B0. Despite these improvements in soil air transport, the effect of the biochar treatment was marginal on soil t, d(B) and n(B). We suggest that, probably higher biochar application rates and longer time are needed to significantly improve PAW and soil pore structure characteristics, which control air and gas transport through the soil.
引用
收藏
页码:1664 / 1671
页数:8
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