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首页> 外文期刊>Progress in Physical Geography >Variability of throughfall volume and solute inputs in wooded ecosystems
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Variability of throughfall volume and solute inputs in wooded ecosystems

机译:树木繁茂的生态系统中穿透量和溶质输入量的变异性

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Throughfall is a critical component of the hydrological and biogeochemical cycles of wooded ecosystems with a characteristically large degree of temporal and spatial variability. The highly variable nature of throughfall is of importance to scientists and natural resource managers concerned with the effects of water and solute inputs to the subcanopy, including understory vegetation, soil moisture, soil solution chemistry, and the fate of atmospheric dryfall. The purpose of this study is to critically review and evaluate the present state of knowledge pertaining to the temporal and spatial variability of throughfall volume and solute inputs in wooded ecosystems. The authors are optimistic that this review will facilitate the advancement of science by exposing gaps in our current understanding and mitigating the duplication of unwarranted research efforts. Several key areas where current knowledge is weak are: (1) the effect of meteorological conditions on the variability of throughfall volume; a data gap exists concerning the effects of precipitation type (eg, rain, snow, snow-to-rain, rain-to-snow), incident rain drop size, intensity, duration, wind speed and direction, and wind run on the throughfall variability; (2) the effect of meteorological conditions on the variability of throughfall solute inputs; (3) the role of canopy structure on precipitation partitioning into throughfall and stemflow and the variability of throughfall volume and solute inputs; (4) effects of epiphytes on the spatial variation of throughfall volume and solute inputs; (5) the physics and fluid dynamics of water flow over vegetative surfaces and its impact on throughfall yield and chemical enrichment; and (6) intraspecific variation of throughfall water and solute inputs. Future research projects undertaken with the specific aim of addressing the deficiencies identified will improve our understanding of interactions among the biosphere-atmosphere-lithosphere and promote better stewardship of forest and water resources.
机译:穿透力是树木繁茂的生态系统的水文和生物地球化学循环的重要组成部分,其特征是时空变化很大。通透性的高度可变性对于关注水和溶质输入到亚冠层的影响的科学家和自然资源管理者来说非常重要,其中包括地下植被,土壤水分,土壤溶液化学和大气干旱的命运。这项研究的目的是批判性地审查和评估与森林生态系统中穿透量和溶质输入的时空变化有关的知识的现状。作者们乐观地认为,本综述将通过揭露我们目前的理解差距并减轻不必要的研究工作的重复,从而促进科学的发展。当前知识薄弱的几个关键领域是:(1)气象条件对穿透量变化的影响;存在与降雨类型(例如,雨,雪,雪到雨,雨到雪),入射雨滴大小,强度,持续时间,风速和风向以及风向贯穿降雨的影响有关的数据缺口变化性; (2)气象条件对穿透性溶质输入量变化的影响; (3)冠层结构对降水划分为通流和茎流的作用以及通流量和溶质输入量的可变性; (4)附生植物对穿透量和溶质输入量空间变化的影响; (5)营养面水流的物理和流体动力学及其对贯通产量和化学富集的影响; (6)穿透水和溶质输入的种内变化。为解决所发现的不足而开展的未来研究项目将增进我们对生物圈-大气-岩圈之间相互作用的理解,并促进更好地管理森林和水资源。

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