Pullout Behaviour and Influencing Mechanisms of Desert Plant Roots in Clayey Sand During Thawing

In cold and arid regions, the mechanical properties and influencing mechanisms of the root-soil interface during the thawing stage remain poorly understood. This study focuses on <i>Alhagi sparsifolia</i> root-clayey sand composites to investigate the effects of temperature (-10 °C to 25 °C), initial soil water content (4-12%), and naturally varying root diameter (4.50-5.05 mm) on root pullout behaviour, and integrates endoscopic macro-observation, environmental scanning electron microscopy (ESEM), soil water migration tests, and nuclear magnetic resonance (NMR) techniques to reveal the dominant influencing mechanisms. Key findings reveal the following: (1) An increase in soil water content from 4% to 12%, and a temperature rise from -10 °C to 25 °C led to a maximum reduction in the average peak pullout force (F<sub>T</sub>) of roots exceeding 95%. (2) There is a non-monotonic relationship between root diameter and pull-out force, which can be attributed to two distinct failure modes: a newly observed failure mode known as root bark peeling, occurring under high soil moisture conditions (≥8%), and a commonly observed failure mode referred to as partial soil detachment, occurring under low soil moisture conditions (≤6%). (3) The coupling effects of temperature and water content reveal that the increase in temperature predominantly contributes to strength loss (>63%) during the ice-water phase transition (-10 °C to 0 °C), while soil water content primarily influences root pullout behaviour in the liquid water stage (5 °C to 25 °C). (4) As the temperature rises, in soils with low water content (4-6%), the reinforcing effect of roots appears to stabilize at -1 °C, whereas in soils with high water content (8-12%), stabilization occurs only beyond 5 °C. These findings enhance the understanding of root-soil interactions in thawing environments and provide a theoretical basis for soil bioengineering techniques aimed at slope stabilization in cold and arid regions.

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Publication Details

Journal
Plants
Published
2025-09-16
DOI
https://doi.org/10.3390/plants14182876
Primary Topic
Tree Root and Stability Studies
Type
article
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article

Pullout Behaviour and Influencing Mechanisms of Desert Plant Roots in Clayey Sand During Thawing

Qinglin Li, Peizhong Feng, Guang Yang, Xiaofei Yang et al.
Plants
Tree Root and Stability Studies
article

Pullout Behaviour and Influencing Mechanisms of Desert Plant Roots in Clayey Sand During Thawing

Qinglin Li, Peizhong Feng, Guang Yang, Xiaofei Yang, Miao Zhang, Wenjuan Chen, Yu Song
article en

Abstract

In cold and arid regions, the mechanical properties and influencing mechanisms of the root-soil interface during the thawing stage remain poorly understood. This study focuses on <i>Alhagi sparsifolia</i> root-clayey sand composites to investigate the effects of temperature (-10 °C to 25 °C), initial soil water content (4-12%), and naturally varying root diameter (4.50-5.05 mm) on root pullout behaviour, and integrates endoscopic macro-observation, environmental scanning electron microscopy (ESEM), soil water migration tests, and nuclear magnetic resonance (NMR) techniques to reveal the dominant influencing mechanisms. Key findings reveal the following: (1) An increase in soil water content from 4% to 12%, and a temperature rise from -10 °C to 25 °C led to a maximum reduction in the average peak pullout force (F<sub>T</sub>) of roots exceeding 95%. (2) There is a non-monotonic relationship between root diameter and pull-out force, which can be attributed to two distinct failure modes: a newly observed failure mode known as root bark peeling, occurring under high soil moisture conditions (≥8%), and a commonly observed failure mode referred to as partial soil detachment, occurring under low soil moisture conditions (≤6%). (3) The coupling effects of temperature and water content reveal that the increase in temperature predominantly contributes to strength loss (>63%) during the ice-water phase transition (-10 °C to 0 °C), while soil water content primarily influences root pullout behaviour in the liquid water stage (5 °C to 25 °C). (4) As the temperature rises, in soils with low water content (4-6%), the reinforcing effect of roots appears to stabilize at -1 °C, whereas in soils with high water content (8-12%), stabilization occurs only beyond 5 °C. These findings enhance the understanding of root-soil interactions in thawing environments and provide a theoretical basis for soil bioengineering techniques aimed at slope stabilization in cold and arid regions.

PlantsVol. 14(18)
Shihezi University (CN), Xinjiang Production and Construction Corps (CN)
Openalex Percentile: Top 74%
Tree Root and Stability Studies
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