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Differences in soil moisture in two Middle Eastern oak forests: Comparing the effects of trees and soil composition

机译:两种中东栎林的土壤水分差异:比较树木和土壤成分的影响

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The incidence of large rain events in Mediterranean ecosystems vary among years. Summer aridity is interpreted as a resetting event, eliminating previous soil-moisture dynamics. The dynamics of soil moisture and retention are critical to tree survival, particularly in dry regions. This study examines the long-term soil water content (theta(V)) dynamics in two distinct locations within the forest, under the canopy and forest clearing, within two diverse oak forests: subhumid mixed oak forests (MG) and semiarid monospecific oak woodlands (YE). Plots were established at small-scale catchments and soil water contents were measured during 2010-2013, at three depths in the two different locations. Cumulative rainfall was used as an independent proxy for theta(V) analysis. A novel bell-bilogistic mathematical model of wetting, saturation, and drying arms was developed. We aimed to study the theta(V) distribution differences between soil profiles giving the large climatic gradient between the two forested sub basins, the differences in vegetation traits along with soil attributes. We further aimed at determining the role of an individual tree in regulating soil-moisture dynamics. We hypothesized the occurrence of distinct responses between sites in all soil-moisture indices with higher theta(V) at the wetter site. We tested the hypothesis that seasonal cumulative rainfall dictates the variations in soil-moisture regimes throughout contiguous years. Annual rainfall was higher than long-term average throughout the study. Soil profiles under the canopies at both sites were consistently wetter. Infiltration and depletion constants were higher at MG whereas maximum soil moisture was higher at YE. Homogenous recharge patterns were seen at MG although YE evinced more variation. Oaks had no effect on recharge at MG compared with the forest clearing. Soil properties primarily affected the wetting arm whereas vegetation composition regulated the drying arm. Mixed-stands characterized by ever-green and deciduous species may maintain favourable soil-moisture conditions, in comparison with other mixed stand morphologies. The increasing role of slacking forces in infiltration process may alter the interaction between trees and herbaceous vegetation.
机译:地中海生态系统中大雨事件的发生率每年都不同。夏季干旱被解释为重置事件,消除了以前的土壤水分动态。土壤水分和固位力的变化对树木的生存至关重要,特别是在干旱地区。这项研究研究了在两个不同的栎林中的森林中两个不同位置,冠层和森林砍伐下的长期土壤水分(theta(V))的动态:两个湿润的橡树林(MG)和半干旱单种栎林(YE)。在小规模流域建立了样地,并在2010-2013年期间在两个不同地点的三个深度测量了土壤含水量。累积降雨量被用作theta(V)分析的独立代理。开发了一种新颖的钟形生物学模型,用于润湿,饱和和干燥臂。我们旨在研究土壤剖面之间的θ(V)分布差异,从而给出两个森林次流域之间较大的气候梯度,植被特征以及土壤属性的差异。我们进一步旨在确定一棵单独的树在调节土壤水分动态中的作用。我们假设在所有土壤水分指数中,在较湿润的位置具有较高的theta(V)的位置之间会出现不同的响应。我们检验了以下假设:季节性累积降雨决定了整个连续年中土壤水分状况的变化。在整个研究中,年降水量高于长期平均水平。两个站点的冠层下的土壤剖面始终湿润。 MG的入渗和耗水常数较高,而YE的最大土壤水分较高。尽管YE表现出更多的变化,但在MG处发现了同质的补给模式。与森林砍伐相比,橡树对MG的补给没有影响。土壤特性主要影响润湿臂,而植被组成调节干燥臂。与其他混交林形态相比,以常绿和落叶树种为特征的混交林可以保持良好的土壤水分条件。松弛力在渗透过程中的作用日益增强,可能会改变树木与草本植物之间的相互作用。

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