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首页> 外文期刊>Wetlands >VEGETATION PATTERNS RESULTING FROM SPATIAL AND TEMPORAL VARIABILITY IN HYDROLOGY, SOILS, AND TRAMPLING IN AN ISOLATED BASIN MARSH, NEW HAMPSHIRE, USA
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VEGETATION PATTERNS RESULTING FROM SPATIAL AND TEMPORAL VARIABILITY IN HYDROLOGY, SOILS, AND TRAMPLING IN AN ISOLATED BASIN MARSH, NEW HAMPSHIRE, USA

机译:美国新罕布什尔州一个孤立的盆地沼泽水文,土壤和足迹的时空变异导致的植被格局

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This study investigated the role of hydrology, soils, and trampling in determining the distribution of vegetation in an isolated wetland from 1996 to 1999. Grassy Pond, in Litchfield, New Hampshire, is a seasonally flooded basin marsh situated in sandy soils. It is a depressional wetland consisting of three connected basins; it has no surface-water inlets or outlets. This acidic, low-nutrient wetland contains several rare species and represents an uncommon ecosystem type in New England. A network of wells and piezometers monitored from 1996 to 1999 established that the wetland receives an average of 95.4% of its growing season inputs from precipitation and the rest from shallow ground water flowing through the wetland; as a result, it experiences large fluctuations in water levels. Vegetation in the wetland fell into five major elevation zones. Variation in plant diversity within each zone, and differences between adjacent zones, result in part from differences in depth of organic layer, trampling by hikers, all-terrain vehicles, and native wildlife, and the extent of water-level fluctuations. Several of the low basin species are more likely to be found in trampled areas. Shrub invasion of the open basin areas is prevented by trampling in some areas and by high water levels in others. Variability in hydrology resulted in temporal, as well as spatial, variability in the plant community, as dry years yielded significantly greater diversity, including a large increase in tree seedlings. Both hydrologic variability and trampling are external factors that explain a significant portion of the variation in vegetation on a large scale and connect this geographically isolated wetland to the surrounding landscape. On a smaller scale, however, autogenic forces related to soil formation and plant species interactions may be more important in explaining the plant diversity in the wetland.
机译:这项研究调查了水文,土壤和践踏在确定孤立的湿地中植被分布方面的作用(从1996年到1999年)。新罕布什尔州利奇菲尔德的草塘是季节性被洪水淹没的盆地沼泽,位于沙质土壤中。这是一个洼地湿地,由三个相连的盆地组成。它没有地表水入口或出口。这种酸性,低营养的湿地包含几种稀有物种,代表了新英格兰罕见的生态系统类型。从1996年至1999年监测的井网和测压计网络确定,湿地平均收到其生长季节投入的95.4%,来自降水,其余部分来自流经湿地的浅层地下水;结果,它的水位波动很大。湿地上的植被分为五个主要海拔区。每个区域内植物多样性的变化以及相邻区域之间的差异,部分原因是有机层深度的差异,远足者,全地形车辆和本地野生动物践踏的原因以及水位波动的程度。在被践踏的地区更可能发现几种低流域物种。通过在某些地区践踏和在其他地区高水位,可以防止灌木丛侵入开放流域。水文学的变化导致植物群落的时间和空间变异,因为干旱年份产生的多样性大大增加,其中包括树木幼苗的大量增加。水文变异性和践踏都是外部因素,可以解释植被大规模变化的很大一部分,并将这一地理上孤立的湿地与周围景观联系起来。但是,在较小规模上,与土壤形成和植物物种相互作用有关的自生力可能在解释湿地植物多样性方面更为重要。

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