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Marine applications of an autonomous indicator-based pH sensor.

机译:基于指示器的自主pH传感器在海洋中的应用。

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摘要

Currently, the lack of accurate in situ pH measurements limits our understanding of natural pH variability. In order to predict future pH changes in the oceans, quality high temporal resolution pH data are needed. This work used the newly developed Submersible Autonomous Moored Instrument for pH (SAMI-pH), a fully autonomous, in situ spectrophotometric pH sensor, to study oceanic pH variability. The three main goals of this research were to: determine the field performance of the new SAMI-pH, establish the utility of combining SAMI-pH data with in situ pCO2 data to characterize the entire inorganic carbon cycle and establish pH variability, and what drives it, in a coral reef.Autonomous pH and pCO2 sensors were deployed in tandem in Monterey Bay, CA from June to August 2007. The results showed that the pH-pCO 2 combination can provide information about data quality and can be used to model calcium carbonate (CaCO3) saturation states. The pH and pCO2 can be combined with a salinity-derived AT to model both long and short-term DIC variability. The SAMI-pH was also used to examine pH variability on Media Luna coral reef, Puerto Rico for two month periods over three seasons in 2007 and 2008. pH on the reef was at a minimum of 7.89 pH units during the fall and at a maximum of 8.17 pH units during the winter. Half of this seasonal variability was driven by temperature, with the remaining changes due to organic carbon and CaCO 3 production. CO2 gas fluxes showed that the reef was a source of CO2 during the summer and fall, and a sink during the winter. Annually, the reef was a source of CO2, with a flux of 1.19 mol m-2 year-1. Calcium carbonate saturation states were modeled with pH and pCO2 and showed seasonal values between 2.7--5.4 for aragonite and 4.0--7.0 for calcite. Both data sets showed that the SAMI-pHs performed well in extended field tests, including high fouling environments, making it possible to determine combined temporal pH and pCO2 variability in unprecedented breadth and detail.
机译:当前,缺乏准确的原位pH测量值限制了我们对自然pH变异性的理解。为了预测未来海洋中的pH值变化,需要高质量的高时间分辨率pH值数据。这项工作使用了新开发的用于pH的潜水式自动系泊仪器(SAMI-pH),这是一种全自动的原位分光光度pH传感器,用于研究海洋pH的可变性。这项研究的三个主要目标是:确定新型SAMI-pH的现场性能,建立将SAMI-pH数据与原位pCO2数据相结合以表征整个无机碳循环并确定pH变异性的效用,以及驱动因素2007年6月至2007年8月,在加利福尼亚州蒙特利湾串联配置了自动pH和pCO2传感器。结果表明,pH-pCO 2组合可提供有关数据质量的信息,可用于对钙进行建模碳酸盐(CaCO3)饱和状态。 pH和pCO2可以与盐度衍生的AT结合使用,以模拟长期和短期DIC变异性。 SAMI-pH还用于检查波多黎各Media Luna珊瑚礁在2007年和2008年的三个季节中两个月期间的pH变异性。在秋天,礁石上的pH至少为7.89 pH单位,最大为冬季的pH值为8.17。这种季节性变化的一半是由温度驱动的,其余的变化是由于有机碳和CaCO 3的产生。 CO2气体通量表明,在夏季和秋季,礁石是CO2的来源,而在冬季则是礁石的下沉。每年,珊瑚礁都是CO2的来源,其通量为1.19 mol m-2 year-1。用pH和pCO2对碳酸钙饱和态进行建模,文石的季节性值介于2.7--5.4和方解石的4.0--7.0之间。两种数据集均表明,SAMI-pH在扩展的现场测试(包括高污垢环境)中表现良好,从而有可能以前所未有的广度和细节确定组合的pH和pCO2的可变性。

著录项

  • 作者

    Cullison, Sarah Elizabeth.;

  • 作者单位

    University of Montana.;

  • 授予单位 University of Montana.;
  • 学科 Chemical Oceanography.Chemistry Analytical.Biogeochemistry.
  • 学位 Ph.D.
  • 年度 2010
  • 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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