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    等密度针阔叶材微观孔隙结构对其压缩吸能行为的影响机制

    Influence of micro-pore structure on compressive energy absorption behavior in isodensity hardwood and softwood

    • 摘要:
      目的 木材作为一种天然多孔材料,在防护领域具有重要应用潜力,但其复杂的多级孔隙结构与各向异性导致现有基于人工材料的吸能理论适用性有限,限制了其在减震领域中的精准设计与高值利用。为此,本研究选取密度相同的典型针叶材与阔叶材,系统比较二者微观孔隙构造对其压缩吸能行为的影响,以期为减震木材的科学遴选、结构设计与性能优化提供理论依据。
      方法 以密度均为0.335 g/cm3的杉木(针叶材)和轻木(阔叶材)为研究对象,首先采用压汞法和显微观察系统表征其多级孔隙结构及解剖特征;随后通过准静态压缩实验测试二者在顺纹与横纹方向的力学响应,获取应力−应变曲线,并计算能量吸收与力学指标;同时结合超景深三维显微系统动态观察压缩过程中的微观破坏演变过程及形貌变化。
      结果 (1)研究表明,尽管杉木与轻木密度相同,总孔隙率相近,但其细胞结构与孔隙分布在多个尺度上存在显著差异。杉木以管胞为主要组成(占比约95%),早晚材渐变,管胞横截面多呈长方形或多边形;轻木为散孔材,木纤维占比约75%,横截面接近正六边形。(2)孔隙分析显示,杉木孔径分布更分散,大孔Ⅱ更多,轻木则孔径较小,分布集中、微孔更多。(3)力学测试表明:顺纹压缩时,轻木呈现较平稳的平台阶段,杉木则出现明显应力塌陷;横纹压缩时二者均单调递增呈“应变硬化”,杉木的压缩强度高于轻木。(4)能量吸收分析进一步揭示,轻木在顺纹方向吸能更优且过程平稳,杉木则在横纹方向表现更佳,该差异主要源于细胞形态、材质均匀性及化学组成等因素。(5)破坏形貌观察发现,顺纹压缩下杉木沿木射线与早晚材界面产生贯通裂纹,轻木破坏相对完整;横纹压缩时,杉木早材管胞与轻木导管分别成为主要变形薄弱部位。
      结论 木材的微观孔隙构造对其压缩吸能行为具有决定性影响。在相同密度下,轻木因纤维截面近似正六边形、材质均匀且微孔丰富,在顺纹压缩中表现出更优的吸能平稳性与总量;杉木则因管胞腔径差异小,早晚材呈梯度分布及较高木质素含量,在横纹压缩中具备更好的能量吸收能力。因此,在实际工程应用中,应根据具体载荷方向与缓冲需求,选择具有相应孔隙特征的木材。本研究从微观结构角度揭示了木材的压缩吸能机制,不仅可为防护领域中的木材选材与结构设计提供理论指导,也可为仿生设计高性能多孔吸能材料提供参考。

       

      Abstract:
      Objective Wood, as a natural porous material, holds significant potential in protective applications. However, its complex hierarchical pore structure and anisotropy limit the applicability of existing energy absorption theories developed for synthetic materials, thereby hindering precise design and high-value utilization in shock absorption. To address this, this study compares two representative wood species—softwood and hardwood—with equal-density, systematically investigating how their microstructural pore architectures influence compressive energy absorption behavior. The findings aim to provide theoretical foundations for scientific selection, structural design, and performance optimization of shock-absorbing wood materials.
      Method Cunninghamia lanceolata (softwood) and Ochroma pyramidale (hardwood), both with a density of 0.335 g/cm3, were selected as experimental materials. Mercury intrusion porosimetry and microscopic observation were employed to characterize their hierarchical pore structures and anatomical features. Quasi-static compression tests were conducted along longitudinal and transverse grain directions to obtain stress–strain curves and calculate energy absorption and mechanical parameters. Additionally, a 3D ultra-depth-of-field microscopy system was used to dynamically observe microstructural failure evolution and morphological changes during compression.
      Result (1) Despite similar densities and total porosities, significant differences in cellular structure and pore distribution across multiple scales were observed. Cunninghamia lanceolata consisted predominantly of tracheids ( ~ 95%), with gradual earlywood-to-latewood transition and rectangular or polygonal cross-sections; Ochroma pyramidale, a diffuse-porous hardwood, contained ~ 75% fibers with nearly regular hexagonal cross-sections. (2) Pore size analysis revealed that Cunninghamia lanceolata exhibited a broader pore size distribution with more macropores (Type II), whereas Ochroma pyramidale showed smaller, more concentrated pores and a higher proportion of micropores. (3) Mechanical testing indicated that under longitudinal compression, Ochroma pyramidale displayed a stable plateau phase, while Cunninghamia lanceolata exhibited pronounced stress collapse. Under transverse compression, both species showed monotonic “strain hardening” behavior, with Cunninghamia lanceolata demonstrating higher compressive strength. (4) Energy absorption analysis further demonstrated that Ochroma pyramidale performed better in longitudinal compression with smoother energy absorption, whereas Cunninghamia lanceolata excelled in transverse compression. These differences primarily stem from variations in cell morphology, material homogeneity, and chemical composition. (5) Failure morphology observations revealed that longitudinal compression induced through-cracks along rays and earlywood–latewood interfaces in Cunninghamia lanceolata, while Ochroma pyramidale maintained relatively intact structure. Under transverse compression, earlywood tracheids in Cunninghamia lanceolata and vessels in Ochroma pyramidale became the primary sites of deformation and failure.
      Conclusion The microstructural pore architecture of wood decisively governs its compressive energy absorption behavior. At equal-density, Ochroma pyramidale achieves superior energy absorption capacity and stability in longitudinal compression due to its near-hexagonal fiber cross-sections, material uniformity, and abundant micropores. In contrast, Cunninghamia lanceolata exhibits better transverse energy absorption owing to minimal tracheid lumen diameter variation, graded earlywood–latewood distribution, and higher lignin content. Therefore, in practical engineering applications, wood selection should be guided by specific loading direction and cushioning requirements. This study elucidates the compressive energy absorption mechanisms of wood from a microstructural perspective, offering theoretical guidance for material selection and structural design in protective applications and providing insights for bio-inspired development of high-performance porous energy-absorbing materials.

       

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