Hypothesis and theory: Do trees “release the tension” in rainwater? Surface tension reduction in throughfall and stemflow from urban trees

IF 2.7 3区 农林科学 Q2 ECOLOGY
Benjamin J. Noren, Nicholas R. Lewis, K. Tonello, Anna Ilek, John T. Van Stan
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Abstract

Knowledge of the processes and impacts associated with the canopy’s partitioning of rainfall into stemflow (water that drains to the base of tree stems) and throughfall (water that drips through gaps and from canopy surfaces) has expanded in recent years. However, the effect of canopy interactions on the fundamental physical properties of rainwater as it travels through the canopy to the soil, particularly surface tension, remains understudied. To discuss specific hypotheses within this context and their relevance to ecohydrological theory, the surface tension of rainwater samples was examined directly. Over a period of 9 months, open rainwater, throughfall and stemflow samples were collected during 20 storms from 12 study trees located in Secrest Arboretum (about 2.5 km outside Wooster, Ohio). Study trees were selected to highlight a range of canopy characteristics, with each tree being from a unique deciduous species. Surface tension was measured using pendant drop goniometry, and measurements were analyzed for variation across study trees and correlation with event air temperature and rain intensity. In general, surface tension was reduced in throughfall and stemflow compared to measurements made for event rainwater, with median surface tension changes of −0.446 mN m−1 and −0.595 mN m−1 for throughfall and stemflow, respectively. The extent of this reduction varied among study trees (with changes as great as −6.5 to −5.5 mN m−1), and storm event characteristics were directly and indirectly correlated with surface tension changes in select cases. Hypothetically, a number of mechanisms may account for the observed reduction (and variation in this reduction) in surface tension, including differences in tree surface properties, canopy microenvironments, and microbiomes, and each warrant further research. Testing these hypotheses may advance broader ecohydrological theory as surface tension changes will influence wetting, absorption, and solute exchange processes within the canopy which, in turn, may affect related surface processes.
假设与理论:树木会 "释放 "雨水中的张力吗?城市树木直流和茎流中表面张力的降低
近年来,关于树冠将降雨划分为茎流(流到树干底部的水)和透雨(从缝隙和树冠表面滴下的水)的过程和影响的知识有所增加。然而,当雨水通过树冠进入土壤时,树冠相互作用对雨水基本物理特性的影响,特别是表面张力,仍然没有得到充分的研究。为了讨论在此背景下的具体假设及其与生态水文理论的相关性,直接检查了雨水样品的表面张力。在9个月的时间里,从secret Arboretum(位于俄亥俄州伍斯特市外约2.5公里)的12棵研究树中收集了20次风暴期间的开放雨水、雨水和茎流样本。研究树的选择是为了突出一系列的冠层特征,每棵树都来自一个独特的落叶物种。利用垂坠角测量法测量表面张力,并分析了测量结果在研究树木之间的变化以及与事件气温和降雨强度的相关性。总的来说,与事件雨水的测量结果相比,穿透雨和茎流的表面张力降低了,穿透雨和茎流的中位表面张力变化分别为- 0.446 mN m - 1和- 0.595 mN m - 1。这种减少的程度在研究树之间有所不同(变化幅度可达- 6.5至- 5.5 mN m - 1),在某些情况下,风暴事件特征与表面张力变化直接或间接相关。假设,许多机制可以解释观察到的表面张力的减少(以及这种减少的变化),包括树木表面特性、冠层微环境和微生物组的差异,每一个都需要进一步的研究。验证这些假设可以推进更广泛的生态水文理论,因为表面张力的变化将影响冠层内的润湿、吸收和溶质交换过程,而这些过程反过来又可能影响相关的表面过程。
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来源期刊
CiteScore
4.50
自引率
6.20%
发文量
256
审稿时长
12 weeks
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