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Time-series electrochemical studies in the lower Delaware Bay and at the 9 degrees 50' north East Pacific Rise hydrothermal vent field.

机译:在特拉华湾下部和东太平洋上升北坡9度50'热液喷口处进行的时间序列电化学研究。

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摘要

The research conducted in here is an effort towards meeting the needs of the ocean observing community by designing, and applying voltammetric instruments in conjunction with other sensors on autonomous platforms. These studies were conducted in the Delaware Bay and at the 9°50'N East Pacific Rise hydrothermal vent site. Data collected by these instruments were then used towards gaining a better understanding of primary production in these systems.;Dissolved oxygen and other physical and biological factors were monitored in the lower Delaware Bay using an autonomous buoy. Six weeks of data from the summer of 2007 provide insight into the processes occurring in the lower bay. Dissolved oxygen concentrations vary at both tidal and diel periodicities and are super-saturated for most of the summer, with day time maxima of up to 390 muM (140% saturation). Extended periods of high wind speed reduce the dissolved oxygen concentration to saturation, after which it can take up to 4 days for the system to recover. Reaeration and net oxygen production rates (primary productivity respiration) were calculated using the measured dissolved oxygen concentrations, wind speed, and tidal currents. Oxygen production was modeled using the Delta method and a primary productivity and respiration model. The lower Delaware Bay is net autotrophic, producing oxygen at a rate of 2.8 muM d-1. These results demonstrate the need for time series studies in marine systems, where complex physical and biogeochemical processes would be over-looked by discrete, infrequent observations. When combined with modeling techniques, time series studies provide a tool to investigate processes occurring in natural systems.;Chemistry and temperature were monitored during 6 deployments of an in situ electrochemical analyzer between December, 2004 and January, 2007 in diffuse flow sites at the 9°50'N East Pacific Rise hydrothermal vent site. Au/Hg micro-electrodes and temperature loggers were placed near the mussel Bathymodiolus thermophilus, and the tubeworms Riftia pachyptila and Tevnia jerichonana to monitor the conditions in which these organisms reside, and to investigate the physical and chemical processes occurring at these diffuse flow sites. Results reveal that temperature can be used as a proxy for chemistry, as long as the site is well characterized. Additionally, a site needs to be observed for at least one tidal cycle to monitor the full range of conditions an organism living there experiences. Data were also used in conjunction with previous lab based studies to calculate the rates of sulfide and oxygen uptake near mussels and tubeworms. Additionally, the results suggest that Bathymodiolus and Riftia are found in similar habitats, and that Tevnia favor low O2, high H2S uptake environments.
机译:这里进行的研究是通过在自主平台上设计并应用伏安法仪器以及其他传感器来满足海洋观测界的需求。这些研究是在特拉华湾和东太平洋上升9°50'N热液喷口处进行的。然后使用这些仪器收集的数据来更好地了解这些系统中的初级生产。使用自动浮标在特拉华湾下部监测溶解氧和其他物理和生物因素。从2007年夏季开始的六周数据可以深入了解下海湾发生的过程。溶解的氧气浓度在潮汐和diel周期都变化,并且在整个夏季的大部分时间里都是过饱和的,白天最大最大值为390μM(饱和度为140%)。延长的高风速会使溶解的氧气浓度降低到饱和状态,此后系统最多可能需要4天才能恢复。使用测得的溶解氧浓度,风速和潮流计算出通气量和净氧气产生率(初级生产力呼吸)。使用Delta方法以及主要的生产力和呼吸作用模型对氧气产量进行建模。较低的特拉华湾为净自养性,以2.8μMd-1的速度产生氧气。这些结果表明,需要在海洋系统中进行时间序列研究,在该系统中,离散,不频繁的观测将忽略复杂的物理和生物地球化学过程。当与建模技术相结合时,时间序列研究提供了一种研究自然系统中发生的过程的工具。2004年12月至2007年1月,在9个扩散流场中的6个现场电化学分析仪部署期间,对化学和温度进行了监测。 °50'N东太平洋上升热液喷口。将金/汞微电极和温度记录仪放置在贻贝嗜热巴斯德杯和,虫Riftia pachyptila和Tevnia jerichonana附近,以监测这些生物的生存条件,并调查在这些扩散流场发生的物理和化学过程。结果表明,只要能很好地表征温度,就可以将其用作化学反应的代表。另外,需要观察一个地点至少一个潮汐周期,以监测生活在那里的生物体所经历的全部条件。数据还与先前基于实验室的研究结合使用,以计算贻贝和块茎附近的硫化物和氧气吸收率。此外,这些结果表明,在相似的栖息地中发现了水Bath和裂谷,特维尼亚有利于低O2,高H2S吸收环境。

著录项

  • 作者

    Moore, Tommy S.;

  • 作者单位

    University of Delaware.;

  • 授予单位 University of Delaware.;
  • 学科 Physical Oceanography.
  • 学位 Ph.D.
  • 年度 2008
  • 页码 137 p.
  • 总页数 137
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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