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Ref. No. [UMCES] CBL 2016-016

ACT VS16-07

5

Lake Michigan, the temperature ranged from 21.0

o

C at the surface to 4.1

o

C in the hypolimnion,

with corresponding DO concentrations of 8.6 and 12.6 mg/L, respectively. Two profiling trials

were conducted at each location. The first trial involved equilibrating test instruments at the

surface (3m) for ten minutes and then collecting three Niskin bottle samples at one minute

intervals. Following the third sample, the rosette was quickly profiled into the hypolimnion were

samples were collected immediately upon arrival and then each minute for the next 6 minutes. The

second trial was performed in the reverse direction. For Muskegon Lake, the Troll 9000

overestimated DO when transitioning rapidly from the hypolimnetic equilibration into the warmer

and high DO surface water. Conversely when equilibrate in the surface water the Troll RDO

underestimated DO levels when rapidly transitioned into the colder, low DO hypolimnion. The

range in measurement differences between instrument and reference was 0.04 to 0.41 mg/L for cast

2 and -0.35 to 0.23 mg/L for cast 3. (Note: cast 1 was aborted and redone as cast 3). For Lake

Michigan, the Troll 9000 underestimated DO when transitioning rapidly from surface equilibration

into a colder, high DO hypolimnion. Conversely when equilibrate in the hypolimnion the Troll

RDO overestimated DO levels when rapidly transitioned into the warmer, lower DO surface

waters. The range in measurement differences between instrument and reference was -0.59 to 0.07

mg/L for cast 1 and -0.11 to 0.54 mg/L for cast 2. In both cases the Troll RDO appeared to

approach equilibrium by the seventh minute and the offsets declined to around 0.10 – 0.15 mg/L.

BACKGROUND AND OBJECTIVES

Instrument performance verification is necessary so that effective existing technologies can

be recognized and so that promising new technologies can be made available to support coastal

science, resource management and ocean observing systems. To this end, the NOAA-funded

Alliance for Coastal Technologies (ACT) serves as an unbiased, third party testbed for evaluating

sensors and sensor platforms for use in coastal environments. ACT also serves as a comprehensive

data and information clearinghouse on coastal technologies and a forum for capacity building

through workshops on specific technology topics (visit

www.act-us.info

).

As part of our service to the coastal community, ACT conducted a performance verification

of commercially available, in situ dissolved oxygen (DO) sensors through the evaluation of

objective and quality assured data. The goal of ACT’s evaluation program is to provide technology

users with an independent and credible assessment of instrument performance in a variety of

environments and applications. To this end, the data and information on performance

characteristics were focused on the types of information users most need.

The fundamental objectives of this Performance Verification were to: (1) highlight the

potential capabilities of particular in situ DO sensors by demonstrating their utility in a range of

coastal environments; (2) verify the claims of manufacturers on the performance characteristics of

commercially available DO sensors when tested in a controlled laboratory setting, and (3) verify

performance characteristics of commercially available DO sensors when applied in real world

applications in a diverse range of coastal environments.

INSTRUMENT TECHNOLOGY TESTED

The In-Situ Rugged Dissolved Oxygen (RDO

®

) Sensor measures dissolved oxygen (DO)

using the latest advancements in optical measurement technology. By improving upon the