首页> 外文期刊>Journal of Agricultural Science >Actual and Relative Soil Air Permeability as Soil Physical Quality Index
【24h】

Actual and Relative Soil Air Permeability as Soil Physical Quality Index

机译:实际和相对的土壤空气渗透率作为土壤物理质量指标

获取原文
获取外文期刊封面目录资料

摘要

Developing indices to evaluate soil physical quality can facilitate diagnosis and decision-making. In this context, intrinsic soil air permeability (Kair) is a physical parameter very sensitive to structural changes due to soil management. However, it is important to establish a standard Kair, considering a reference soil physical state. Thus, the present study proposes to create an index called relative soil air permeability (Kairr), taking as reference the physical state of maximum bulk density, obtained by normal Proctor test. Kairr is the ratio between compacted soil air permeability (Kairc) and actual soil air permeability (Kair). Kairr was evaluated using disturbed and undisturbed samples of a Latossolo and a Planossolo. The experimental design was completely randomized, with four treatments (T1-Latossolo 0-0.1 m; T2-Latossolo 0.1-0.2 m; T3-Planossolo 0-0.1 m and T4-Planossolo 0.1-0.2 m) and eight replicates. Kairr was equal to 0.1032 and 0.3547 in the Latossolo and to 0.4115 and 0.1923 in the Planossolo, in the 0-0.1 and 0.1-0.2 m layers, respectively. These characteristic values observed in both soils and layers are due to the management adopted in the area. In Latossolo, the use of medium harrow has made the 0.1-0.2 m layer more restrictive to air movement, whereas the Planossolo showed lower values of relative soil air permeability in the 0-0.1 m layer due to animal grazing, which has greater impact on the superficial portion of the soil.
机译:制定评估土壤物理质量的指标可以促进诊断和决策。在这种情况下,土壤固有空气渗透率(Kair)是对土壤管理引起的结构变化非常敏感的物理参数。但是,考虑参考土壤的物理状态,建立标准的Kair非常重要。因此,本研究建议创建一个称为相对土壤空气渗透率(Kairr)的指数,以通过正常Proctor试验获得的最大容重的物理状态作为参考。 Kairr是压实土壤空气渗透率(Kairc)与实际土壤空气渗透率(Kair)之比。使用Latossolo和Planossolo的不受干扰和不受干扰的样本对Kairr进行了评估。实验设计是完全随机的,有四个处理(T1-Latossolo 0-0.1 m; T2-Latossolo 0.1-0.2 m; T3-Planossolo 0-0.1 m和T4-Planossolo 0.1-0.2 m)和八次重复。在Latossolo中的Kairr等于0.1032和0.3547,在Planossolo中的Kairr等于0.4115和0.1923,分别在0-0.1和0.1-0.2 m的层中。在土壤和土壤层中观察到的这些特征值归因于该地区采用的管理方法。在Latossolo,中耙耙的使用使0.1-0.2 m的层对空气运动的限制更大,而Planossolo在0-0.1 m的层中由于动物放牧而显示出较低的相对土壤空气渗透率值,这对动物的放牧有更大的影响。土壤的表层部分。

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