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生物炭对泥岩坡地土壤物理性质及侵蚀潜力的影响。

Impacts of biochar on physical properties and erosion potential of a mudstone slopeland soil.

作者信息

Hseu Zeng-Yei, Jien Shih-Hao, Chien Wei-Hsin, Liou Ruei-Cheng

机构信息

Department of Environmental Science and Engineering, National Pingtung University of Science and Technology, Pingtung 91201, Taiwan.

Department of Soil and Water Conservation, National Pingtung University of Science and Technology, Pingtung 91201, Taiwan.

出版信息

ScientificWorldJournal. 2014;2014:602197. doi: 10.1155/2014/602197. Epub 2014 Dec 8.

Abstract

Food demand and soil sustainability have become urgent issues recently because of the global climate changes. This study aims to evaluate the application of a biochar produced by rice hull, on changes of physiochemical characteristics and erosion potential of a degraded slopeland soil. Rice hull biochar pyrolized at 400°C was incorporated into the soil at rates of 2.5%, 5%, and 10% (w/w) and was incubated for 168 d in this study. The results indicated that biochar application reduced the Bd by 12% to 25% and the PR by 57% to 92% after incubation, compared with the control. Besides, porosity and aggregate size increased by 16% to 22% and by 0.59 to 0.94 mm, respectively. The results presented that available water contents significantly increased in the amended soils by 18% to 89% because of the obvious increase of micropores. The water conductivity of the biochar-amended soils was only found in 10% biochar treatment, which might result from significant increase of macropores and reduction of soil strength (Bd and PR). During a simulated rainfall event, soil loss contents significantly decreased by 35% to 90% in the biochar-amended soils. In conclusion, biochar application could availably raise soil quality and physical properties for tilth increasing in the degraded mudstone soil.

摘要

由于全球气候变化,粮食需求和土壤可持续性最近已成为紧迫问题。本研究旨在评估稻壳产生的生物炭对退化坡地土壤理化性质变化和侵蚀潜力的影响。在本研究中,将在400°C下热解的稻壳生物炭以2.5%、5%和10%(w/w)的比例掺入土壤中,并培养168天。结果表明,与对照相比,培养后生物炭的施用使容重降低了12%至25%,颗粒密度降低了57%至92%。此外,孔隙度和团聚体大小分别增加了16%至22%和0.59至0.94毫米。结果表明,由于微孔明显增加,改良土壤中的有效含水量显著增加了18%至89%。生物炭改良土壤的导水率仅在10%生物炭处理中发现,这可能是由于大孔隙显著增加和土壤强度(容重和颗粒密度)降低所致。在模拟降雨事件中,生物炭改良土壤的土壤流失量显著减少了35%至90%。总之,施用生物炭可以有效提高退化泥岩土壤的质量和物理性质,以增加耕地。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2c96/4274655/0fc4cf3ad04d/TSWJ2014-602197.001.jpg

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