4.7 Article

Impact of heavy traffic on soil macroporosity of two silty forest soils: Initial effect and short-term recovery

期刊

GEODERMA
卷 217, 期 -, 页码 10-17

出版社

ELSEVIER
DOI: 10.1016/j.geoderma.2013.10.025

关键词

Compaction; Porosity; Micromorphology

资金

  1. GIP Ecofor Soere F-ore-T network
  2. Feder

向作者/读者索取更多资源

Processes and rate of macroporosity changes following heavy traffic in forest ecosystems are seldom studied. The aim of this study was to determine the ability of forest soils to regenerate their macroporosity naturally. The study was performed on 2 silty temperate-forest soils classified as sensitive to compaction located in north-eastern France. Macroporosity was measured in control and trafficked plots at 3 depths (0-7, 15-30 and 30-45 cm) over 2-3 years. Soil macroporosity characteristics (shape, size and orientation) were assessed on polished sections through 2D-image analysis and micromorphic observations. Immediately after heavy traffic, macroporosity decreased by 96 to 49% from 0 to 45 cm in depth. Natural regeneration of macroporosity occurred in the upper 7 cm of soil, while the soil below remained compacted. Small and medium macropores (0.05-0.8 mm(2)) dominated by rounded and irregular pores regenerated completely. Large macropores (>0.8 mm(2)) originally dominated by vughs, mammilated vughs and channels rarely regenerated and were gradually replaced by horizontally oriented planar pores. Our results suggest that initial stages of natural macroporosity recovery are likely due to plant-root penetration and physical processes (shrink-swell, freeze-thaw), whereas recovery due to fauna activities appears later. (C) 2013 Elsevier B.V. All rights reserved.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.7
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据