Bert Sara Di, Tomasella Martina, Duddek Patrick, Natale Sara, Petruzzellis Francesco, Carminati Andrea, Zini Luca, D'Amico Lorenzo, Tromba Giuliana, Nardini Andrea
Physics of Soils and Terrestrial Ecosystems, Department of Environmental Systems Science, Institute of Terrestrial Ecosystems, ETH Zürich, Zurich, Switzerland.
Dipartimento di Scienze della Vita, Università di Trieste, Trieste, Italia.
Plant Cell Environ. 2025 May;48(5):3448-3458. doi: 10.1111/pce.15369. Epub 2025 Jan 8.
Drought impacts trees in varied temporal and spatial patterns, suggesting that heterogeneity of below-ground water stores influences the fate of trees under water stress. Karst ecosystems rely on shallow soil overlying bedrock that can store available water in primary pores. A contribution of rock moisture to tree water status has been previously demonstrated, but actual mechanisms and rates of rock-to-root water delivery remain unknown. We report accurate measurements of hydraulic properties of two rock types (Breccia and Dolostone), of typical Karst red soil, and of roots of a common Karst tree species grown under different rock-soil combinations. Experimental data were used to build a water exchange model that supported the hypothesis that roots can extract water from porous and highly conductive rocks (Breccia), but not from more compact ones (Dolostone), especially when plants grow in rocky substrate or experience water stress, and thus have low root hydraulic conductivity and low rates of water extraction from rocks. Our data support the hypothesis that rocks represent important water stores for plants growing in rock-dominated habitats. Heterogeneous rock properties translate into different rates of water delivery to root systems, underlying complex patterns of tree mortality under severe drought stress.
干旱以不同的时间和空间模式影响树木,这表明地下蓄水的异质性会影响水分胁迫下树木的命运。喀斯特生态系统依赖于覆盖在基岩上的浅层土壤,这些土壤可以在原生孔隙中储存可用水分。先前已经证明了岩石湿度对树木水分状况的影响,但岩石向根系输水的实际机制和速率仍然未知。我们报告了对两种岩石类型(角砾岩和白云岩)、典型喀斯特红壤以及在不同岩石 - 土壤组合下生长的常见喀斯特树种根系的水力特性进行的精确测量。实验数据被用于构建一个水分交换模型,该模型支持以下假设:根系能够从多孔且高导水的岩石(角砾岩)中提取水分,但不能从更致密的岩石(白云岩)中提取,特别是当植物生长在岩石基质中或经历水分胁迫时,此时根系水力传导率较低且从岩石中提取水分的速率也较低。我们的数据支持了这样的假设,即岩石是生长在以岩石为主的栖息地中的植物的重要水源。岩石性质的异质性导致向根系输水的速率不同,这是严重干旱胁迫下树木死亡复杂模式的基础。