4.7 Article

Root reinforcement and extracellular products reduce streambank fluvial erosion

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SCIENCE OF THE TOTAL ENVIRONMENT
卷 896, 期 -, 页码 -

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ELSEVIER
DOI: 10.1016/j.scitotenv.2023.165125

关键词

Streambank fluvial erosion; Extracellular polymeric substances; Plant roots; Stream hydrodynamics; Recirculating flume; Organic matter

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This study assessed the combined contributions of roots and soil microorganisms to soil resistance against fluvial erosion. The results showed that the combination of roots and organic carbon inputs significantly reduced soil erosion rates. This indicates that root-biochemical interactions play an important role in influencing channel migration rates due to reductions in streambank erodibility.
A detailed understanding of the factors that impact bank erodibility is necessary to effectively model changes in channel form. This study evaluated the combined contributions of roots and soil microorganisms to soil resistance against fluvial erosion. To do this, three flume walls were constructed to simulate unvegetated and rooted streambanks. Unamended and organic material (OM) amended soil treatments with either no-roots (bare soil), synthetic (inert) roots, or living roots (Panicum virgatum) were created and tested with the corresponding flume wall treatment. OM stimulated the production of extracellular polymeric substances (EPS) and appeared to increase the applied stress required to initiate soil erosion. Synthetic fibers alone provided a base reduction in soil erosion, regardless of the flow rate used. When used in combination, synthetic roots and OM-amendments reduced erosion rates by 86 % or more compared to bare soil; this reduction was identical to the live rooted treatments (95 % to 100 %). In summary, a synergistic relationship between roots and organic carbon inputs can significantly reduce soil erosion rates due to fiber reinforcement and EPS production. These results indicate that root-biochemical interactions, like root physical mechanisms, play an important role in influencing channel migration rates due to reductions in streambank erodibility.

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