An in situ benthic chamber system for improved temporal and spatial resolution measurement of sediment oxygen demand

IF 2.1 3区 地球科学 Q2 LIMNOLOGY
Kara J. Gadeken, Grant Lockridge, Kelly M. Dorgan
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引用次数: 0

Abstract

In shallow coastal systems, sediments are exposed to dramatic and complex variability in environmental conditions that influences sediment processes on short timescales. Sediment oxygen demand (SOD), or consumption of oxygen by sediment-dwelling organisms and chemical reactions within sediments, is one such process and an important metric of aquatic ecosystem functioning and health. The most common instruments used to measure SOD in situ are batch-style benthic chambers, which generally require long measurement periods to resolve fluxes and thus do not capture the high temporal variability in SOD that can be driven by dynamic coastal processes. These techniques also preclude linking changes in SOD through time to specific features of the sediment, for example, shifts in sediment faunal activities which can vary on short time scales and can also be affected by ambient oxygen concentrations. Here we present an in situ semi-flow through instrument to repeatedly measure SOD in discrete areas of sediment. The system isolates patches of sediment in replicate benthic chambers, and measures and records oxygen decrease for a short time before refreshing the overlying water in the chamber with water from the external environment. This results in a sawtooth pattern in which each tooth is an incubation, providing an automated method to produce direct measurements of in situ SOD that can be directly linked to an area of sediment and related to rapid shifts in environmental conditions.

一种用于改进沉积物需氧量时空分辨率测量的原位底栖室系统
在浅海海岸系统中,沉积物暴露于影响沉积物过程的短时间尺度环境条件的剧烈而复杂的变化中。沉积物需氧量(SOD),即沉积物生物对氧气的消耗和沉积物内的化学反应,就是这样一个过程,也是衡量水生生态系统功能和健康的重要指标。用于就地测量SOD的最常用仪器是批式底栖箱,这种仪器通常需要很长的测量周期来解析通量,因此无法捕获可由动态海岸过程驱动的SOD的高时间变异性。这些技术还排除了将SOD随时间变化与沉积物的特定特征联系起来的可能性,例如,沉积物动物活动的变化可能在短时间尺度上发生变化,也可能受到环境氧浓度的影响。在这里,我们提出了一种原位半流通过仪器,反复测量沉积物离散区域的SOD。该系统在复制底栖生物室中隔离沉积物,并在短时间内测量和记录氧气减少,然后用外部环境中的水刷新室中的上覆水。这就产生了锯齿状图案,其中每个牙齿都是一个孵育,提供了一种自动化的方法来直接测量原位SOD,这种方法可以直接与沉积物区域联系起来,并与环境条件的快速变化有关。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
4.80
自引率
3.70%
发文量
56
审稿时长
3 months
期刊介绍: Limnology and Oceanography: Methods (ISSN 1541-5856) is a companion to ASLO''s top-rated journal Limnology and Oceanography, and articles are held to the same high standards. In order to provide the most rapid publication consistent with high standards, Limnology and Oceanography: Methods appears in electronic format only, and the entire submission and review system is online. Articles are posted as soon as they are accepted and formatted for publication. Limnology and Oceanography: Methods will consider manuscripts whose primary focus is methodological, and that deal with problems in the aquatic sciences. Manuscripts may present new measurement equipment, techniques for analyzing observations or samples, methods for understanding and interpreting information, analyses of metadata to examine the effectiveness of approaches, invited and contributed reviews and syntheses, and techniques for communicating and teaching in the aquatic sciences.
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