首页> 外文期刊>Wetlands >USE OF INDIVIDUALISTIC STREAMFLOW-VEGETATION RELATIONS ALONG THE FREMONT RIVER, UTAH, USA TO ASSESS IMPACTS OF FLOW ALTERATION ON WETLAND AND RIPARIAN AREAS
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USE OF INDIVIDUALISTIC STREAMFLOW-VEGETATION RELATIONS ALONG THE FREMONT RIVER, UTAH, USA TO ASSESS IMPACTS OF FLOW ALTERATION ON WETLAND AND RIPARIAN AREAS

机译:利用美国犹他州弗里蒙特河沿岸的个体地表径流-植被关系来评估径流变化对湿地和RIPARIA地区的影响

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We analyzed the transverse pattern of vegetation along a reach of the Fremont River in Capitol Reef National Park, Utah, USA using models that support both delineation of wetland extent and projection of the changes in wetland area resulting from upstream hydrologic alteration. We linked stage-discharge relations developed by a hydraulic model to a flow-duration curve derived from the flow history in order to calculate the inundation duration of 361 plots (0.5 X 2 m). Logistic regression was used to relate plant species occurrence in plots to inundation duration. A weighted average of the wetland indicator values of species was used to characterize plots as Aquatic, Wetland, Transitional, or Upland. Finally, we assessed how alterations in the flow duration curve would change the relative widths of these four zones. The wetland indicator values of species and the wetland prevalence index scores of plots were strongly correlated with inundation duration. Our results support the concept that plants classified as wetland species typically occur on sites inundated at least two weeks every two years. The portion of the riparian zone along the high- gradient study reach of the Fremont River that satisfied the vegetation criterion for a regulatory wetland was narrow (2 m wide). Both the unvegetated Aquatic zone (7.8 m) and the Transitional zone (8 m) were substantially wider. The Transitional zone included the maxima of several species and was, therefore, not merely a combination of elements of the Wetland and Upland zones. Multiplicative increases or decreases in streamflow regime produced a wetter, or drier, bottomland vegetation, respectively. Systematic reductions in flow variability reduced the width of both the Wetland and Transitional zones and increased the width of the Upland zone. Our approach is widely applicable to inform water management decisions involving changes in flow regime.
机译:我们使用支持湿地范围描绘和上游水文变化引起的湿地面积变化预测的模型,分析了美国犹他州国会礁国家公园的弗里蒙特河沿岸植被的横向格局。我们将水力模型开发的水位流量关系与从流量历史得出的流量持续时间曲线相链接,以计算361个地块(0.5 X 2 m)的淹没持续时间。使用逻辑回归将地块中植物物种的发生与淹没持续时间联系起来。物种湿地指标值的加权平均值用于将样地定性为水生,湿地,过渡带或高地。最后,我们评估了流量持续时间曲线的变化将如何改变这四个区域的相对宽度。物种的湿地指标值和样地的湿地流行指数得分与淹没持续时间密切相关。我们的结果支持这样一个概念,即被归类为湿地物种的植物通常每两年至少出现在两周被淹没的地点。沿弗里蒙特河高坡度研究河段的河岸带部分满足规范湿地植被标准,很窄(2 m宽)。无植被的水生带(7.8 m)和过渡带(8 m)都明显更宽。过渡带包括几种物种的最大值,因此,不仅是湿地和高地带要素的组合。河流流态的乘数增加或减少分别产生了较湿或较干的底地植被。流量可变性的系统性减小减小了湿地和过渡带的宽度,并增加了高地带的宽度。我们的方法可广泛应用于为涉及流域变化的水管理决策提供信息。

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