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Hydro-geomorphological influences on plant patch density and distribution in bedrock shoal habitats of the Cahaba River, AL.

机译:水力地貌学对阿拉巴马州卡哈巴河基岩浅滩生境中植物斑块密度和分布的影响。

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摘要

There is a growing body of research that examines bedrock channels. Despite this, biotic-abiotic interactions remain a topic mostly addressed in alluvial systems. This research seeks to identify patch-scale hydro-geomorphic factors operating at the patch-scale in bedrock shoals of the Cahaba River (AL) that help determine the distribution of the emergent aquatic macrophyte, Justicia americana..;Macrophyte patch density (number of stems/m2) and percent bedrock void surface area (rock surface area/m2 occupied by joints, fractures, and potholes) were measured (n = 24) using stem counts and underwater photography, respectively. One-dimensional hydrologic modeling (HEC-RAS 4.1.0) was completed for one cross-section within a shoal to examine whether velocity and channel depth are controlling variables for macrophyte patch density. A Pearson's Correlation test between bedrock surface void area and stem density demonstrated a statistically significant positive correlation (r=.665, p=0.01). Results of an independent t-test between the velocity and depth model outputs for within and outside plant patches showed a significant difference in average velocity (p =0.011) and depth ( p = 0.001) between the two types of locations across discharges, ranging from 7 m3/sec to 226 m3/sec. These results suggest that the amount of void space present in bedrock surfaces and localized depth and velocity help control the macrophyte patch density, and by extension, the distribution of macrophytes in bedrock shoal complexes. The utility of geomorphology in explaining patch-scale habitat heterogeneity in this study demonstrates potential to use geomorphology to explain macrophyte habitat heterogeneity at reach and system-scales and highlights the need for more research that helps understand biotic-abiotic interactions in bedrock fluvial systems.
机译:研究基岩通道的研究越来越多。尽管如此,生物-非生物相互作用仍然是冲积系统中主要解决的话题。这项研究旨在找出在卡哈巴河(AL)基岩浅滩的斑块规模上起作用的斑块规模水文地貌因素,这些因素有助于确定新兴水生大型植物Justicia americana的分布。杆数和水下摄影分别测量(n = 24)和基岩空隙表面积百分比(节理,裂缝和坑洼所占的岩石表面积/ m2)(n = 24)。针对浅滩中的一个横截面完成了一维水文建模(HEC-RAS 4.1.0),以检查速度和通道深度是否是大型植物斑块密度的控制变量。基岩表面空隙面积与茎密度之间的皮尔逊相关检验显示出统计学上显着的正相关(r = .665,p = 0.01)。在植物内部和外部的速度和深度模型输出之间进行的独立t检验结果表明,两种放电位置之间的平均速度(p = 0.011)和深度(p = 0.001)有显着差异。 7立方米/秒至226立方米/秒这些结果表明,基岩表面中存在的空隙空间的数量以及局部深度和速度有助于控制大型植物的斑块密度,进而控制大型植物在基岩浅滩复合体中的分布。在这项研究中,地貌学在解释斑块规模生境异质性方面的实用性表明了利用地貌学在远景和系统规模上解释大型植物生境异质性的潜力,并强调需要开展更多的研究来帮助理解基岩河流系统中的生物-非生物相互作用。

著录项

  • 作者

    Vaughn, Ryan.;

  • 作者单位

    The University of Alabama.;

  • 授予单位 The University of Alabama.;
  • 学科 Geomorphology.;Biology General.;Biology Ecology.
  • 学位 M.S.
  • 年度 2014
  • 页码 63 p.
  • 总页数 63
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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