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The effect of environmental forcing on the suspended sediment within the Naomi Wetlands as reflected in turbidity data.

机译:浊度数据反映了环境强迫对Naomi湿地内悬浮沉积物的影响。

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摘要

In recent years, several freshwater diversion structures have been constructed along the lower Mississippi River south of Baton Rouge, Louisiana. These structures divert freshwater and sediment into Louisiana's coastal wetlands in an effort to combat Louisiana's estimated annual wetland loss of 65 km2. The successful operation of these diversions depends upon the stage of the Mississippi River. An increase in river stage generally results in an increase in the suspended sediment load and in the discharge of water through a diversion. The subsequent transport of suspended sediment within an estuary is also influenced by local rainfall, tide, and wind speed and direction. This study examines the relationship between the suspended sediment concentration in the east-central Barataria Basin and the operation of the Naomi Siphon, Mississippi River stage, local rainfall, tide, wind speed, and wind direction.; The Naomi Freshwater Diversion, located southeast of New Orleans, diverts freshwater and suspended sediment into the Barataria Estuary. A 10-year record of monthly turbidity readings (used as a surrogate for suspended sediment concentration) from within the estuary was combined with river stage, rainfall, tide, wind speed, and wind direction data to examine the effect of these forcing factors on the turbidity and concentration of suspended sediment within the estuary.; Results indicate that suspended sediment concentrations are greatest in the areas closest to the siphon when the siphon is discharging and during periods of high river stage. Spoil banks appear to block the flow of sediment-laden sheet flow to the outer regions of the wetland. Sheet flow is diverted into canals and flows off site. Individually, tide affects only the interior wetlands, due to an increase of readily available sediment in this area. Rainfall and wind individually provide a negligible influence on suspended sediment concentrations.; Regression models of the relationship between suspended sediment concentration and the environmental forcing factors were developed. The study also determined that canals are more efficient than bayous for transporting suspended sediment. The canals appear to be funneling suspended sediment out of the wetlands.
机译:近年来,沿着路易斯安那州巴吞鲁日以南的密西西比河下游建造了一些淡水分流结构。这些结构将淡水和沉积物转移到路易斯安那州的沿海湿地,以应对路易斯安那州每年估计的65平方公里的湿地损失。这些改道的成功运作取决于密西西比河的水位。河流水位的增加通常会导致悬浮泥沙量的增加,以及通过引水导致的水量增加。河口内悬浮泥沙的后续运输也受到当地降雨,潮汐,风速和风向的影响。这项研究研究了中东部巴拉塔里亚盆地的悬浮泥沙浓度与Naomi Siphon,密西西比河河段的运行,局部降雨,潮汐,风速和风向之间的关系。位于新奥尔良东南部的纳奥米(Naomi)淡水改道将淡水和悬浮的泥沙分流到巴拉塔里亚河口。将河口内每月浊度读数的10年记录(用作悬浮泥沙浓度的替代物)与河段,降雨,潮汐,风速和风向数据相结合,以检查这些强迫因素对海平面的影响。河口内悬浮泥沙的浊度和浓度。结果表明,在虹吸水排出时和高水位期间,最靠近虹吸管的区域中悬浮泥沙的浓度最大。弃土堆似乎阻止了载有泥沙的片状流向湿地外围的流动。板料流被转移到运河中并流出现场。个别而言,潮汐仅影响内部湿地,这是由于该地区易于获得的沉积物增加。降雨和风对悬浮泥沙浓度的影响可忽略不计。建立了悬浮泥沙浓度与环境强迫因子关系的回归模型。这项研究还确定,运河在运移悬浮泥沙方面比Bayous更为有效。运河似乎正在将悬浮的泥沙漏出湿地。

著录项

  • 作者

    McGraw, Molly J.;

  • 作者单位

    Louisiana State University and Agricultural & Mechanical College.;

  • 授予单位 Louisiana State University and Agricultural & Mechanical College.;
  • 学科 Physical Geography.; Engineering Environmental.
  • 学位 Ph.D.
  • 年度 2005
  • 页码 126 p.
  • 总页数 126
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 自然地理学;环境污染及其防治;
  • 关键词

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