Earthworms accelerate soil porosity turnover under watering conditions

Endogeic earthworms significantly modify soil aggregation and porosity, which in turn control water flow in soil. This study aimed to determine how the earthworm casting activity influences soil porosity and its dynamics. The main hypothesis was that the deposition of belowground water-stable casts increases soil porosity and its water stability. First we quantified cast production by the endogeic earthworm species Metaphire posthuma under laboratory conditions for 15 days. Secondly, casts and the bulk soil were analysed for structural stability to water and were packed in soil and subjected to wetting under various conditions and energy levels. The shape and size of pores were measured by image analysis. Almost all casts (98%) were produced belowground. M. posthuma produced approximately five times its own weight per day. Casts were depleted in C and were more easily disaggregated by water than the bulk soil. Although casts initially led to larger soil porosity (on average 50%), their structure was unstable. As a consequence, water inputs led to a faster decrease in soil porosity in the presence of casts. Large pores in between casts were rapidly replaced by small elongated and rounded pores. These results suggest that cast lifespan and associated porosity are of primary importance in the regulation of soil porosity turnover and the ecological functions that are under its control. Our findings suggest that in the field, the low stability of casts is likely to lead to a rapid compaction of the soil after rainfall events. However, high levels of cast production may prevent soil porosity from being broken down. Soil structural porosity thus depends on the balance between the production and degradation of casts. Improvements to the soil structure will occur when the former predominates.

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Bibliographic Details
Main Authors: Bottinelli, N., Henry des Tureaux, Thierry, Hallaire, V., Mathieu, J., Benard, Y., Tran Duc Toan, Jouquet, Pascal
Format: Journal Article biblioteca
Language:English
Published: Elsevier 2010-04
Subjects:earthworms, soil pore system,
Online Access:https://hdl.handle.net/10568/40486
https://doi.org/10.1016/j.geoderma.2010.01.006
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spelling dig-cgspace-10568-404862023-12-08T19:36:04Z Earthworms accelerate soil porosity turnover under watering conditions Bottinelli, N. Henry des Tureaux, Thierry Hallaire, V. Mathieu, J. Benard, Y. Tran Duc Toan Jouquet, Pascal earthworms soil pore system Endogeic earthworms significantly modify soil aggregation and porosity, which in turn control water flow in soil. This study aimed to determine how the earthworm casting activity influences soil porosity and its dynamics. The main hypothesis was that the deposition of belowground water-stable casts increases soil porosity and its water stability. First we quantified cast production by the endogeic earthworm species Metaphire posthuma under laboratory conditions for 15 days. Secondly, casts and the bulk soil were analysed for structural stability to water and were packed in soil and subjected to wetting under various conditions and energy levels. The shape and size of pores were measured by image analysis. Almost all casts (98%) were produced belowground. M. posthuma produced approximately five times its own weight per day. Casts were depleted in C and were more easily disaggregated by water than the bulk soil. Although casts initially led to larger soil porosity (on average 50%), their structure was unstable. As a consequence, water inputs led to a faster decrease in soil porosity in the presence of casts. Large pores in between casts were rapidly replaced by small elongated and rounded pores. These results suggest that cast lifespan and associated porosity are of primary importance in the regulation of soil porosity turnover and the ecological functions that are under its control. Our findings suggest that in the field, the low stability of casts is likely to lead to a rapid compaction of the soil after rainfall events. However, high levels of cast production may prevent soil porosity from being broken down. Soil structural porosity thus depends on the balance between the production and degradation of casts. Improvements to the soil structure will occur when the former predominates. 2010-04 2014-06-13T14:47:46Z 2014-06-13T14:47:46Z Journal Article Bottinelli, N.; Henry des Tureaux, Thierry; Hallaire, V.; Mathieu, J.; Benard, Y.; Toan, Tran Duc; Jouquet, Pascal. 2010. Earthworms accelerate soil porosity turnover under watering conditions. Geoderma, 156(1-2):43-47. doi: http://dx.doi.org/10.1016/j.geoderma.2010.01.006 0016-7061 https://hdl.handle.net/10568/40486 https://doi.org/10.1016/j.geoderma.2010.01.006 en Copyrighted; all rights reserved Limited Access Elsevier
institution CGIAR
collection DSpace
country Francia
countrycode FR
component Bibliográfico
access En linea
databasecode dig-cgspace
tag biblioteca
region Europa del Oeste
libraryname Biblioteca del CGIAR
language English
topic earthworms
soil pore system
earthworms
soil pore system
spellingShingle earthworms
soil pore system
earthworms
soil pore system
Bottinelli, N.
Henry des Tureaux, Thierry
Hallaire, V.
Mathieu, J.
Benard, Y.
Tran Duc Toan
Jouquet, Pascal
Earthworms accelerate soil porosity turnover under watering conditions
description Endogeic earthworms significantly modify soil aggregation and porosity, which in turn control water flow in soil. This study aimed to determine how the earthworm casting activity influences soil porosity and its dynamics. The main hypothesis was that the deposition of belowground water-stable casts increases soil porosity and its water stability. First we quantified cast production by the endogeic earthworm species Metaphire posthuma under laboratory conditions for 15 days. Secondly, casts and the bulk soil were analysed for structural stability to water and were packed in soil and subjected to wetting under various conditions and energy levels. The shape and size of pores were measured by image analysis. Almost all casts (98%) were produced belowground. M. posthuma produced approximately five times its own weight per day. Casts were depleted in C and were more easily disaggregated by water than the bulk soil. Although casts initially led to larger soil porosity (on average 50%), their structure was unstable. As a consequence, water inputs led to a faster decrease in soil porosity in the presence of casts. Large pores in between casts were rapidly replaced by small elongated and rounded pores. These results suggest that cast lifespan and associated porosity are of primary importance in the regulation of soil porosity turnover and the ecological functions that are under its control. Our findings suggest that in the field, the low stability of casts is likely to lead to a rapid compaction of the soil after rainfall events. However, high levels of cast production may prevent soil porosity from being broken down. Soil structural porosity thus depends on the balance between the production and degradation of casts. Improvements to the soil structure will occur when the former predominates.
format Journal Article
topic_facet earthworms
soil pore system
author Bottinelli, N.
Henry des Tureaux, Thierry
Hallaire, V.
Mathieu, J.
Benard, Y.
Tran Duc Toan
Jouquet, Pascal
author_facet Bottinelli, N.
Henry des Tureaux, Thierry
Hallaire, V.
Mathieu, J.
Benard, Y.
Tran Duc Toan
Jouquet, Pascal
author_sort Bottinelli, N.
title Earthworms accelerate soil porosity turnover under watering conditions
title_short Earthworms accelerate soil porosity turnover under watering conditions
title_full Earthworms accelerate soil porosity turnover under watering conditions
title_fullStr Earthworms accelerate soil porosity turnover under watering conditions
title_full_unstemmed Earthworms accelerate soil porosity turnover under watering conditions
title_sort earthworms accelerate soil porosity turnover under watering conditions
publisher Elsevier
publishDate 2010-04
url https://hdl.handle.net/10568/40486
https://doi.org/10.1016/j.geoderma.2010.01.006
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