Markfort Corey D, Hondzo Miki
St. Anthony Falls Lab., Dep. of Civil Engineering, Univ. of Minnesota-Twin Cities, Minneapolis, MN, USA.
J Environ Qual. 2009 Jun 23;38(4):1766-74. doi: 10.2134/jeq2008.0197. Print 2009 Jul-Aug.
Dissolved oxygen (DO) is probably the most important parameter related to water quality and biological habitat in aquatic environments. In situ DO sensors are some of the most valuable tools used by scientists and engineers for the evaluation of water quality in aquatic ecosystems. Presently, we cannot accurately measure DO concentrations under variable temperature and pressure conditions. Pressure and temperature influence polarographic and optical type DO sensors compared to the standard Winkler titration method. This study combines laboratory and field experiments to compare and quantify the accuracy and performance of commercially available macro and micro Clark-type oxygen sensors as well as optical sensing technology to the Winkler method under changing pressure and temperature conditions. Field measurements at various lake depths revealed sensor response time up to 11 min due to changes in water temperature, pressure, and DO concentration. Investigators should account for transient response in DO sensors before measurements are collected at a given location. We have developed an effective model to predict the transient response time for Clark-type oxygen sensors. The proposed procedure increases the accuracy of DO data collected in situ for profiling applications.
溶解氧(DO)可能是与水生环境中的水质和生物栖息地相关的最重要参数。原位溶解氧传感器是科学家和工程师用于评估水生生态系统水质的一些最有价值的工具。目前,我们无法在可变温度和压力条件下准确测量溶解氧浓度。与标准的温克勒滴定法相比,压力和温度会影响极谱型和光学型溶解氧传感器。本研究结合了实验室和现场实验,以比较和量化市售的宏观和微观克拉克型氧传感器以及光学传感技术在变化的压力和温度条件下相对于温克勒方法的准确性和性能。在不同湖泊深度的现场测量表明,由于水温、压力和溶解氧浓度的变化,传感器响应时间长达11分钟。在给定位置收集测量数据之前,研究人员应考虑溶解氧传感器的瞬态响应。我们已经开发出一种有效的模型来预测克拉克型氧传感器的瞬态响应时间。所提出的程序提高了原位收集的用于剖面测量应用的溶解氧数据的准确性。