{"title":"植被生长对土壤微观结构和水力机械性能的影响","authors":"Alessandro Fraccica, Enrique Romero, Thierry Fourcaud","doi":"10.1680/jgeot.23.00163","DOIUrl":null,"url":null,"abstract":"Literature studies are evidencing the counterposed effects of vegetation on soil hydraulic behaviour. Besides, root effects at the microscale are rarely quantified for direct correlations with phenomenological observations due to the complexity of adopting up-scaling factors. This study explores the microstructural causes behind the observed changes in vegetated compacted clayey sand's hydraulic and volume change behaviour. To this aim, laboratory experiments were carried out on compacted samples seeded with <i>Cynodon dactylon</i>. Significant changes in soil water-saturated permeability, water retention and shrinkage upon drying were observed after root growth. Laboratory measurements were complemented with quantification of root morphological features and observations at the microscale at different soil hydraulic states. X-ray scans and mercury intrusion porosimetry allowed covering seven orders of magnitude of pore sizes, shedding light on soil fabric changes at the soil-root interface and the clay aggregate scale. The effects of roots on the soil pore size distribution consisted of multi-physics phenomena: fissure generation, void clogging, and soil aggregation due to roots’ chemical interaction. Furthermore, a good correlation was found between the normalised volume of roots and the micro-pores volume. This new expression was included in a framework to predict soil water retention behaviour considering the aggregated structure and soil-root hydro-chemical interactions.","PeriodicalId":501472,"journal":{"name":"Géotechnique","volume":"8 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2024-03-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Effects of vegetation growth on soil microstructure and hydro-mechanical behaviour\",\"authors\":\"Alessandro Fraccica, Enrique Romero, Thierry Fourcaud\",\"doi\":\"10.1680/jgeot.23.00163\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Literature studies are evidencing the counterposed effects of vegetation on soil hydraulic behaviour. Besides, root effects at the microscale are rarely quantified for direct correlations with phenomenological observations due to the complexity of adopting up-scaling factors. This study explores the microstructural causes behind the observed changes in vegetated compacted clayey sand's hydraulic and volume change behaviour. To this aim, laboratory experiments were carried out on compacted samples seeded with <i>Cynodon dactylon</i>. Significant changes in soil water-saturated permeability, water retention and shrinkage upon drying were observed after root growth. Laboratory measurements were complemented with quantification of root morphological features and observations at the microscale at different soil hydraulic states. X-ray scans and mercury intrusion porosimetry allowed covering seven orders of magnitude of pore sizes, shedding light on soil fabric changes at the soil-root interface and the clay aggregate scale. The effects of roots on the soil pore size distribution consisted of multi-physics phenomena: fissure generation, void clogging, and soil aggregation due to roots’ chemical interaction. Furthermore, a good correlation was found between the normalised volume of roots and the micro-pores volume. This new expression was included in a framework to predict soil water retention behaviour considering the aggregated structure and soil-root hydro-chemical interactions.\",\"PeriodicalId\":501472,\"journal\":{\"name\":\"Géotechnique\",\"volume\":\"8 1\",\"pages\":\"\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2024-03-21\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Géotechnique\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1680/jgeot.23.00163\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Géotechnique","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1680/jgeot.23.00163","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
摘要
文献研究证明了植被对土壤水力行为的反作用。此外,微观尺度上的根系效应很少被量化以直接与现象观测结果相关联,这是因为采用上规模因素非常复杂。本研究探讨了观察到的植被压实粘土砂的水力和体积变化行为变化背后的微观结构原因。为此,我们对播种了 Cynodon dactylon 的压实样本进行了实验室实验。根系生长后,土壤水饱和渗透性、保水性和干燥收缩率都发生了显著变化。除了实验室测量之外,还对不同土壤水分状态下的根系形态特征进行了量化,并在微观尺度上进行了观察。通过 X 射线扫描和汞侵入孔隙度测定法,可以覆盖七个数量级的孔隙大小,从而揭示土壤-根系界面和粘土团粒尺度上的土壤结构变化。根系对土壤孔径分布的影响包括多种物理现象:裂缝产生、空隙堵塞以及根系化学作用导致的土壤聚集。此外,研究还发现根系的归一化体积与微孔体积之间存在良好的相关性。考虑到聚合结构和土壤-根系的水化学相互作用,这种新的表达式被纳入了预测土壤保水性能的框架中。
Effects of vegetation growth on soil microstructure and hydro-mechanical behaviour
Literature studies are evidencing the counterposed effects of vegetation on soil hydraulic behaviour. Besides, root effects at the microscale are rarely quantified for direct correlations with phenomenological observations due to the complexity of adopting up-scaling factors. This study explores the microstructural causes behind the observed changes in vegetated compacted clayey sand's hydraulic and volume change behaviour. To this aim, laboratory experiments were carried out on compacted samples seeded with Cynodon dactylon. Significant changes in soil water-saturated permeability, water retention and shrinkage upon drying were observed after root growth. Laboratory measurements were complemented with quantification of root morphological features and observations at the microscale at different soil hydraulic states. X-ray scans and mercury intrusion porosimetry allowed covering seven orders of magnitude of pore sizes, shedding light on soil fabric changes at the soil-root interface and the clay aggregate scale. The effects of roots on the soil pore size distribution consisted of multi-physics phenomena: fissure generation, void clogging, and soil aggregation due to roots’ chemical interaction. Furthermore, a good correlation was found between the normalised volume of roots and the micro-pores volume. This new expression was included in a framework to predict soil water retention behaviour considering the aggregated structure and soil-root hydro-chemical interactions.