生物炭在粗质土壤中比在细质土壤中更能降低植物残体的早期矿化率--人工土壤法

IF 5.8 2区 农林科学 Q1 SOIL SCIENCE Soil Pub Date : 2024-05-06 DOI:10.5194/egusphere-2024-1143
Thiago M. Inagaki, Simon Weldon, Franziska B. Bucka, Eva Farkas, Daniel P. Rasse
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引用次数: 0

摘要

摘要由于土壤条件的多变性,量化生物碳对不同土壤质地中碳的持久性的影响非常复杂。利用具有精确质地和矿物成分的人工土壤,我们可以将生物炭的影响与土壤颗粒大小的影响区分开来。我们可以证明,在不同质地的土壤(粘度从 5% 到 41%)中,施用生物炭能显著降低植物残体的早期碳矿化率,但在沙质土壤中更为明显。这一发现表明,生物炭可以弥补粘土的不足,促进碳在土壤系统中的持久性。这份简短的报告对了解土壤质地和生物炭应用之间的相互作用大有裨益。
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Biochar reduces early-stage mineralization rates of plant residues more in coarse than fine-texture soils – an artificial soil approach
Abstract. Quantifying the impact of biochar on carbon persistence across soil textures is complex, owing to the variability in soil conditions. Using artificial soils with precise textural and mineral composition, we could disentangle the effects of biochar from the effects of soil particle size. We can show that biochar application significantly reduces early-stage carbon mineralization rates of plant residues in various soil textures (from 5 to 41 % clay) but more significantly in sandy soils. This finding suggests that biochar can compensate for the lack of clay in promoting C persistence in soil systems. This short report significantly contributes to understanding soil texture and biochar application interactions.
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来源期刊
Soil
Soil Agricultural and Biological Sciences-Soil Science
CiteScore
10.80
自引率
2.90%
发文量
44
审稿时长
30 weeks
期刊介绍: SOIL is an international scientific journal dedicated to the publication and discussion of high-quality research in the field of soil system sciences. SOIL is at the interface between the atmosphere, lithosphere, hydrosphere, and biosphere. SOIL publishes scientific research that contributes to understanding the soil system and its interaction with humans and the entire Earth system. The scope of the journal includes all topics that fall within the study of soil science as a discipline, with an emphasis on studies that integrate soil science with other sciences (hydrology, agronomy, socio-economics, health sciences, atmospheric sciences, etc.).
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