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Do groundwater dynamics drive spatial patterns of tree density and diversity in Neotropical savannas?

机译:地下水动力学是否驱动新热带稀树草原树木密度和多样性的空间格局?

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QuestionsWhat are the temporal and spatial variations of groundwater depth along topographic gradients in Neotropical savannas? Are patterns of tree density and species diversity along topographic gradients in Neotropical savannas controlled by water table depth? Do soil and groundwater nutrient concentrations differ along topographic gradients in Neotropical savannas? LocationFire-protected savannas of central Brazil. MethodsOver 16mo, we monitored temporal and spatial variations in groundwater levels using automated submersible pressure transducers installed in ten wells located along two topographic gradients (five wells per gradient) of 950m and 1703m in length, representing elevations of 47 and 37m a.s.l., respectively. We located the wells according to changes in vegetation physiognomies from woody savannas at high elevations, to open shrubby grasslands at low elevations. Along each topographic gradient we determined soil and groundwater nutrient concentrations as well as richness, density, basal diameter and height of trees within two plots of 14x14m (392m(2)) adjacent to each well. ResultsAlong the two gradients, groundwater levels exhibited larger fluctuations at lower than at higher elevations where the water table was deeper. Richness, density and diversity of trees decreased significantly at lower elevations where soils were waterlogged during the wet season. Soil pH and soil concentrations of carbon, nitrogen and manganese decreased significantly as elevation increased along the topographic gradients, but soil nutrient concentrations of phosphorus, aluminium and iron did not change with elevation. Groundwater samples contained only trace amounts of nutrients and were poorly correlated with elevation along the topographic gradients. ConclusionsIn Neotropical savannas, the minimum distance between the soil surface and water table depth (reached during the wet season) and the relatively large fluctuations in groundwater limit tree density and diversity at low elevations as savanna trees cannot cope with extended waterlogging during the wet season and with low soil water availability during the dry season. Thus, variations of tree density and diversity along topographic gradients are more related to spatial and temporal variations in water table depth than to soil and groundwater nutrient variations in Neotropical savannas
机译:问题在新热带稀树草原中,地下水深度沿地形梯度的时空变化是什么?新热带稀树草原沿地形梯度的树木密度和物种多样性的格局是否受地下水位控制?新热带稀树草原的土壤和地下水养分浓度是否沿地形梯度变化?位置巴西中部的防火大草原。方法在16个月内,我们使用自动潜水压力传感器监测地下水水位的时空变化,该传感器安装在沿两个地形坡度(分别为950m和1703m)的两个地形坡度(每个坡度为5口井)上的10口井中,分别代表海拔47和37m a.s.l.我们根据从高海拔的木质稀树草原到低海拔的开放灌木草原的植被生理学变化来定位井。沿着每个地形梯度,我们确定了每口井附近两个14x14m(392m(2))地块内的土壤和地下水养分浓度以及树木的丰富度,密度,基础直径和高度。结果沿着两个梯度,地下水位的波动比地下水位较深的较高海拔的波动低。在较低的海拔地区,树木的丰富度,密度和多样性在较低的高度显着下降,在潮湿季节土壤被水淹。随着海拔高度沿地形梯度的增加,土壤的pH和碳,氮和锰的浓度显着降低,但是磷,铝和铁的土壤养分浓度并未随海拔的升高而变化。地下水样品仅含有微量的养分,并且与沿地形梯度的海拔高度相关性很弱。结论在新热带稀树草原中,土壤表层与地下水位之间的最小距离(在湿润季节达到)以及相对较大的地下水波动限制了低海拔地区的树木密度和多样性,因为稀疏草原无法应对潮湿季节和更长时期的内涝。干旱季节土壤水分利用率低。因此,树木密度和多样性随地形梯度的变化与地下水位深度的时空变化关系更大,而不是与新热带稀树草原的土壤和地下水养分变化有关

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