Loading…

Wettability and biogeochemical properties of the drilosphere and casts of endogeic earthworms in pear orchard

The aim of this work was to evaluate the effect of endogeic earthworms on the burrow system (burrow wall 0-3 mm, transitional zone 3-7 mm, bulk soil greater than or equal to 20 mm from the burrow wall) and cast aggregates of a loess soil under pear orchard. This effect was tested by determining wett...

Full description

Saved in:
Bibliographic Details
Published in:Soil & tillage research 2015-01, Vol.145, p.55-61
Main Authors: Lipiec, J., Brzezińska, M., Turski, M., Szarlip, P., Frąc, M.
Format: Article
Language:English
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:The aim of this work was to evaluate the effect of endogeic earthworms on the burrow system (burrow wall 0-3 mm, transitional zone 3-7 mm, bulk soil greater than or equal to 20 mm from the burrow wall) and cast aggregates of a loess soil under pear orchard. This effect was tested by determining wettability and selected biogeochemical properties (organic carbon, potential redox, respiration, denitrification and methanogenic potentials, and ammonium and nitrate N) using soil from each compartment immediately after sampling. Wetting was measured with an apparatus consisting of a sponge connected with a graduated capillary tube and biogeochemical soil properties using standard methods. The mean wetting rate was the lowest in the cast aggregates and burrow walls (0.154 and 0.542 mm super(3) s super(-1)) and the highest in bulk soil (1.016 mm super(3) s super(-1)). Total organic carbon, C sub(org) (range 1.59-2.40%), microbial carbon, C sub(mic) (range 0.567-1.85 mg g super(-1)) and C sub(mic):C sub(org) ratio (range 3.57-7.69%) followed the ranking series: cast aggregates > burrow walls > transition zone > bulk soil with the lowest relative differences between the cast aggregates and burrow walls. The same compartment arrangement was observed for denitrification potential (range 34.7-98.0 mg N sub(2)O-N kg super(-1) day super(-1)), respiration rate (range 11.3-56.0 mg CO sub(2)-C kg super(-1) day super(-1)), metabolic quotient qCO sub(2) (respiration to microbial biomass ratio) (range 0.83-1.56 mu g CO sub(2)-C mg super(-1) C sub(mic) h super(-1)), and methane production (range 4.00-429.9 mg CH sub(4)-C kg super(-1)). Foregoing indicates that C-enriched burrows and cast aggregates are the least wettable and encouraging habitats for the growth and activity of microorganisms. Ammonium N concentrations were not influenced by earthworms, but concentrations of nitrate N and N sub(tot) were significantly greater in the earthworm affected compartments than in the bulk soil. Principal component analysis (PCA) showed high sensitivity of wettability to concentrations of C sub(org) and C sub(mic) and C sub(mic):C sub(org) ratio. The quantitative description of the spatial distribution of the wettability and the biogeochemical properties in the earthworm system may have implications to the understanding of lateral movement of water in the earthworm inhabited soils.
ISSN:0167-1987
DOI:10.1016/j.still.2014.08.010