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Ecohydrology Bearings - Invited Commentary The ecohydrology of roots in rocks

机译:生态水文方位-特邀评论岩石根系的生态水文

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摘要

Large portions of the world are characterized by shallow soil underlain by weathered bedrock or cemented soil horizons. The implications of this substrate condition for ecohydrological processes have not been systematically explored, but misrepresentation in models could have profound consequences for climate prediction and global vegetation modelling. An issue of particular uncertainty is the characterization of water storage for these regions. A limited number of case studies have shown that plant water uptake is not restricted to shallow soils but can involve uptake from rock layers below. The mechanisms governing root-rock interactions are only beginning to be investigated. Research is needed to further characterize the dynamics of water recharge and depletion in weathered bedrock, to develop a better understanding of plant adaptations and rooting patterns required for effective use of bedrock-stored water, and to explore consequences for below-ground competition.
机译:世界上大部分地区的特征是,浅层土壤被风化的基岩或水泥地层覆盖。这种底物条件对生态水文过程的影响尚未得到系统地探讨,但是模型中的错误表达可能会对气候预测和全球植被建模产生深远的影响。特别不确定的问题是这些区域的储水特征。有限的案例研究表明,植物对水的吸收不仅限于浅层土壤,还可能涉及地下岩层的吸收。控制根-岩相互作用的机制才刚刚开始研究。需要进行研究以进一步表征风化基岩中补给和枯竭的动态,以更好地了解有效利用基岩储水所需的植物适应性和生根模式,并探讨地下竞争的后果。

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