RAPID: Collaborative Research: Tracking the Flood Pulse of a Record Discharge of the Brazos River in the Gulf of Mexico
RAPID:合作研究:追踪墨西哥湾布拉索斯河创纪录流量的洪水脉冲
基本信息
- 批准号:1828920
- 负责人:
- 金额:$ 1.49万
- 依托单位:
- 依托单位国家:美国
- 项目类别:Standard Grant
- 财政年份:2018
- 资助国家:美国
- 起止时间:2018-03-01 至 2020-08-31
- 项目状态:已结题
- 来源:
- 关键词:
项目摘要
The transport and fate of sediment carried by rivers to the coastal ocean is of great ecological and societal importance. River input is the primary source of land-derived sediment to the marine environment. These particles have significant impacts on the health of coastal ecosystems and the geology and bathymetry of coastal oceans and shipping channels. They directly and indirectly affect fisheries and navigation. This research focuses on the movement of sediments carried into the Gulf of Mexico, via the Brazos River, during the unprecedented rainfall and flooding event that occurred during Hurricane Harvey. The Brazos River ranks as the second largest contributor of nutrients and organic matter to the Gulf of Mexico, after the Mississippi River. Unlike the Mississippi, however, most sediment delivered to the Gulf of Mexico from the Brazos is carried during flooding events like that which accompanied Hurricane Harvey. Little is known about the fate of this sediment. It is not clear if it is retained in the coastal zone, where the nutrients and chemicals it carries affect the coastal environment, or is carried offshore and deposited in the deep waters of the Gulf of Mexico. Through intensive sampling of sediments just offshore the mouth of the Brazos River and further offshore in the Gulf of Mexico in what is known as the Texas Mud Blanket, this project will determine the principal repository of sediments delivered to the western Gulf of Mexico by a major Texas river. The overall goal of this research is to investigate the hypothesis that flood-borne sediment from the Brazos River is initially deposited in the coastal zone and subsequently mobilized and carried offshore with a large fraction of it being deposited in the Texas Mud Blanket. The work builds on the analysis of sea-bottom sediment samples collected in 2017 during flooding associated with Hurricane Harvey. This new program will include two sampling cruises to augment already collected data. The first cruise will entail acquisition of ~25 cores that will indicate sediment deposition and transport in the near-shore region near the Brazos River mouth. Preliminary work indicates that much of the initial deposition of Brazos River sediment occurred east of the original sampling region. The second cruise in will collect additional Brazos region cores and expand sampling into the Texas Mud Blanket, with the goal of documenting changes in Brazos sediment deposition from the Hurricane Harvey flooding. During both cruises, complementary hydrography data will be collected. This includes water column velocities and suspended sediment loads. Provenance of individual layers, within the sediment samples and box cores, will be determined by digital photos and x-radiographs of intact core slabs that show sediment fabric and structures. To differentiate Gulf of Mexico from Brazos River sediments, sub-samples of collected cores will be geochemically analyzed and profiled for short-lived-radioisotope geochronology, water content, grainsize distribution, and mercury and carbonate content. These indicators will help identify the origin of the sediments deposited in the system.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.
河流携带沉积物到沿海海洋的运输和归宿具有重要的生态和社会重要性。河流输入是海洋环境中陆源沉积物的主要来源。这些颗粒对沿海生态系统的健康以及沿海海洋和航道的地质和水深测量具有重大影响。它们直接和间接影响渔业和航运。这项研究的重点是在飓风哈维期间发生的前所未有的降雨和洪水事件期间,通过布拉索斯河带入墨西哥湾的沉积物的运动。布拉索斯河是墨西哥湾第二大营养物和有机物贡献者,仅次于密西西比河。 然而,与密西西比河不同的是,从布拉索斯河输送到墨西哥湾的大部分沉积物是在飓风哈维期间发生的洪水事件中携带的。 人们对这种沉积物的命运知之甚少。 目前尚不清楚它是否保留在沿海地区,其携带的营养物和化学物质会影响沿海环境,或者被带到近海并沉积在墨西哥湾的深水中。通过对布拉索斯河河口近海和墨西哥湾更远的德克萨斯泥毯区域的沉积物进行密集采样,该项目将确定由主要沉积物输送到墨西哥湾西部的沉积物的主要储存库。德克萨斯河。 这项研究的总体目标是调查这样的假设:布拉索斯河的洪水沉积物最初沉积在沿海地区,随后被移动并带到近海,其中很大一部分沉积在德克萨斯州泥毯中。 这项工作建立在对 2017 年飓风哈维洪水期间收集的海底沉积物样本分析的基础上。 这个新计划将包括两次采样巡航,以补充已经收集的数据。第一次航行将需要采集约 25 个岩心,这些岩心将表明布拉索斯河口附近近岸区域的沉积物沉积和运输情况。 初步工作表明,布拉索斯河沉积物的大部分初始沉积发生在原始采样区域以东。 第二次航行将收集更多的布拉索斯地区岩心,并将采样范围扩大到德克萨斯州泥毯,目的是记录飓风哈维洪水导致布拉索斯沉积物沉积的变化。 在两次航行期间,将收集补充的水文学数据。这包括水柱速度和悬浮沉积物负荷。沉积物样本和盒状岩心内各层的来源将通过显示沉积物结构和结构的完整岩心板的数码照片和 X 射线照片来确定。 为了区分墨西哥湾和布拉索斯河沉积物,将对收集的岩心子样本进行地球化学分析和剖面分析,以了解短寿命放射性同位素地质年代学、含水量、粒度分布以及汞和碳酸盐含量。 这些指标将有助于确定系统中沉积物的来源。该奖项反映了 NSF 的法定使命,并通过使用基金会的智力价值和更广泛的影响审查标准进行评估,被认为值得支持。
项目成果
期刊论文数量(0)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
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Zhaohui 'Aleck' Wang其他文献
Zhaohui 'Aleck' Wang的其他文献
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{{ truncateString('Zhaohui 'Aleck' Wang', 18)}}的其他基金
Collaborative Research: Deciphering drivers and variability in salt marsh lateral carbon export
合作研究:破译盐沼横向碳输出的驱动因素和变异性
- 批准号:
2242115 - 财政年份:2023
- 资助金额:
$ 1.49万 - 项目类别:
Standard Grant
Developing a Reagentless In situ Sensor for Measurements of Dissolved Inorganic Carbon in Seawater
开发用于测量海水中溶解无机碳的无试剂原位传感器
- 批准号:
2221931 - 财政年份:2022
- 资助金额:
$ 1.49万 - 项目类别:
Continuing Grant
Collaborative Research: How are estuarine carbon and alkalinity dynamics influenced by macrobiota?
合作研究:河口碳和碱度动态如何受到宏观生物群的影响?
- 批准号:
2148953 - 财政年份:2022
- 资助金额:
$ 1.49万 - 项目类别:
Continuing Grant
NSFOCE-BSF: Collaborative Research: The Role and Mechanisms of Nuclei-induced Calcium Carbonate Precipitation in the Coastal Carbon Cycle: A First In-depth Study
NSFOCE-BSF:合作研究:核诱导碳酸钙沉淀在沿海碳循环中的作用和机制:首次深入研究
- 批准号:
1635388 - 财政年份:2016
- 资助金额:
$ 1.49万 - 项目类别:
Standard Grant
Collaborative Research: The Paradox of Salt Marshes as a Source of Alkalinity and Low pH, High Carbon Dioxide Water to the Ocean: A First In-depth Study of A Diminishing Source
合作研究:盐沼作为碱度和低 pH 值、高二氧化碳水进入海洋的来源的悖论:首次深入研究日益减少的来源
- 批准号:
1459521 - 财政年份:2015
- 资助金额:
$ 1.49万 - 项目类别:
Standard Grant
Developing an In-situ Sensor for Continuous Measurements of Total CO2 on Mobile Platforms
开发用于在移动平台上连续测量总二氧化碳的原位传感器
- 批准号:
1233654 - 财政年份:2013
- 资助金额:
$ 1.49万 - 项目类别:
Continuing Grant
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