首页> 外文期刊>The Science of the Total Environment >Effects of biochar application during different periods on soil structures and water retention in seasonally frozen soil areas
【24h】

Effects of biochar application during different periods on soil structures and water retention in seasonally frozen soil areas

机译:不同时期施用生物炭对季节性冻土地区土壤结构和水分保持的影响

获取原文
获取原文并翻译 | 示例
           

摘要

Currently, little is knownabout soil improvement by biochar in seasonally frozen soil areas. It is not clear whether the effects of biochar application on soil physical properties differ based on application period. Therefore, the purpose of this study was to explore the effects of biochar on soil structure and water retention in cold regions during different application periods. Three biochar applications during different periods were set up through field trials (A: in the early stage of freezing, B: in the middle period of thawing and C: addition of half of the biochar in the early stage of freezing and other half in the middle period of thawing), including four biochar application rates (3, 6, 9 and 12 kg.m(-2)), and no biochar was applied as a control (CK). The results showed that the selection of the biochar application period had a significant effect on the soil structure, but there was no significant difference in the stability of the soil structure. Biochar significantly increased the total porosity (TP) and the content of aggregates with diameters >0.25 mmin the soil, and all 9 kg.m(-2) biochar treatments showed the best structural stability index. The improvement of the soil structure led to the enhancement of the water storage capacities. The plant available water content (PAWC) increased from 0.0638 to 0.0927-0.1767 cm(3).cm(-3), and this result was significantly related to the increases in soil TP and large aggregates (LAs: >2 mm). The optimum field capacity (FC= 0.372 cm(3).cm(-3)) was obtainedwhen the appliedamountwas 9 kg.m(-2). This was beneficial for the stable storage of soil moisture. However, compared with the CK, none of the treatments in area B increased the liquid water content in the field soil. In summary, we suggest that treatment C9 is the most suitable method for application in seasonally frozen soil areas. (C) 2019 Elsevier B.V. All rights reserved.
机译:目前,关于季节性冻土地区通过生物炭改善土壤的了解甚少。尚不清楚生物炭施用对土壤物理性质的影响是否因施用期而异。因此,本研究的目的是探讨生物炭在不同施用时期对寒冷地区土壤结构和保水性的影响。通过田间试验建立了三个不同时期的生物炭应用(A:在冷冻初期,B:在融化中期,C:在冷冻初期添加一半的生物炭,在冷冻初期添加一半)。融化中期),包括4种生物炭施用量(3、6、9和12 kg.m(-2)),并且没有生物炭用作对照(CK)。结果表明,生物炭施用时期的选择对土壤结构有显着影响,但土壤结构的稳定性没有显着差异。生物炭显着增加了土壤中的总孔隙度(TP)和直径> 0.25 mm的骨料含量,所有9 kg.m(-2)生物炭处理均显示出最佳的结构稳定性指数。土壤结构的改善导致蓄水能力的提高。植物有效水分含量(PAWC)从0.0638增加到0.0927-0.1767 cm(3).cm(-3),并且此结果与土壤TP和大型聚集体(LAs:> 2 mm)的增加显着相关。当施加量为9 kg.m(-2)时,可获得最佳场容量(FC = 0.372 cm(3).cm(-3))。这有利于土壤水分的稳定储存。但是,与CK相比,B区的任何处理都没有增加田间土壤中的液态水含量。总而言之,我们建议处理C9是最适合用于季节性冻土地区的方法。 (C)2019 Elsevier B.V.保留所有权利。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号