BioArgo:一个全球规模的化学传感器网络,用于观察海洋中的碳、氧和氮循环

K. Johnson
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引用次数: 2

摘要

本讲座将集中讨论分布在全球海洋的化学传感器网络的发展和运作。由光合作用和呼吸作用驱动的无机碳、pH、溶解氧和硝酸盐浓度的日、季、年际变化是海洋代谢的基本示踪剂。这种新陈代谢对地球气候具有根本的控制作用,因为海洋表层有机物的产生可以将大气中的二氧化碳含量降低约200ppm。随着海洋表面变暖,这些元素循环速率在未来有可能发生变化[1]。然而,目前还没有能够在全球范围内直接观测海洋代谢的现有观测系统。特别是,由于大部分海洋的昂贵和偏远,从船上取样化学物质是行不通的。在全球范围内,海洋生产力只能通过卫星海洋颜色观测间接地感知。要直接观测海洋代谢,需要使用配备化学传感器的机器人平台的全球尺度传感器网络[2]。用于监测海洋热含量的Argo网络(http://www.argo.ucsd.edu)就是这样一个系统的模型。在整个海洋中有超过3000个Argo剖面浮标。它们每隔5至10天从2000米的深度上升,在上升过程中测量温度和盐度,然后将数据传输到近地轨道通信网络。这个循环在每个浮子的5年寿命中重复进行。BioArgo系统目前正致力于建立一个配备pH值、氧气、硝酸盐和生物光学传感器的互补网络[3]。目前,从北极到南极的所有主要海洋盆地(http://argo.jcommops.org/maps.html,向右滚动到生物地图),有200多艘携带氧气的分析浮标和40多艘携带硝酸盐的分析浮标在运行。这些传感器在四年的时间周期内表现出卓越的稳定性和精度[4-7]。实验pH传感器现在在剖面浮子上运行,在一年的周期内精度和稳定性接近0.001 pH。这些结果证明了建立全球化学传感器网络的可行性。本讲座将回顾用于开发具有多年稳定性的化学传感器的方法和全球观测系统的发展。
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BioArgo: A global scale chemical sensor network to observe carbon, oxygen, and nitrogen cycles in the ocean
This talk will focus on the development and operation of a global scale, chemical sensor network that is distributed throughout the world's ocean. The daily, seasonal and interannual changes in the concentrations of inorganic carbon, pH, dissolved oxygen and nitrate that are driven by photosynthesis and respiration are basic tracers of ocean metabolism. This metabolism has a fundamental control on the earth's climate, as production of organic matter in the surface ocean acts to lower atmospheric carbon dioxide by about 200 ppm. It is possible that these rates of elemental cycling will change in the future as the surface ocean warms [1]. However, there are no existing observing systems that allow ocean metabolism to be observed directly at a global scale. In particular, sampling chemistry from ships does not work because of the expense and remoteness of most of the ocean. At the global scale, ocean productivity can only be sensed indirectly from satellite ocean color observations. Global scale sensor networks using robotic platforms equipped with chemical sensors are required to directly observe ocean metabolism [2]. The Argo network (http://www.argo.ucsd.edu), which is used to monitor the heat content of the ocean, is a model for such a system. There are >3000 Argo profiling floats throughout the ocean. They rise from 2000 m depth at 5 to 10 day intervals measuring temperature and salinity during the ascent and then transmit the data to low earth orbit communications networks. This cycle is repeated for the 5 year life of each float. The BioArgo system is now working to build a complementary network equipped with pH, oxygen, nitrate and biooptical sensors [3]. More than 200 profiling floats with oxygen and >40 floats with nitrate are now operating from the Arctic to the Antarctic in all of the major ocean basins (http://argo.jcommops.org/maps.html, scroll right to the Bio map). These sensors have demonstrated exceptional stability and precision over time periods now reaching four years [4-7]. Experimental pH sensors are now operating on profiling floats with a precision and stability near 0.001 pH over an annual cycle. These results demonstrate the feasibility of establishing a global chemical sensor network. This talk will review the methods used to develop chemical sensors with multi-year stability and the development of a global observing system.
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