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Ref. No. [UMCES] CBL 2015-010

ACT VS15-03

for a period of 12 weeks. Instruments were removed from the water only after the test period

was complete.

Instrument Setup

– Prior to deployment, all instruments were set up at the field site by a trained

ACT staff member following established protocols that had been developed in collaboration with

the manufacturers at the training session that occurred in December, 2012 (at the beginning of

the ACT laboratory test). Manufacturers that did not conduct an in-person training session sent

written protocols and video demonstration of desired handling procedures. As appropriate, and

where requested by the manufacturer, submitted test instruments were initially calibrated by

ACT staff using a common batch of commercial, non-dyed, NIST traceable buffers at a pH of

7.02 and 10.06. (Each sensor was calibrated with buffer from its own bottle, but they were all

from the same LOT and shipment). All calibrations occurred in a constant temperature bath at

20.0

o

C (except at HI which was done at 25°C). Any deviation from this temperature was noted

and used to adjust the stated pH values of the buffers as defined on the bottles.

After calibration and prior to deployment (again where appropriate for each instrument)

instruments were exposed to additional certified reference solutions. At Moss Landing, Hawaii,

CBL instruments were exposed to batches of Seawater CRMs produced by the CO2-QC facility

at Scripps Institution of Oceanography. (CRMs were batched into a single container before

distributing into individual calibration cups for each sensor. Three cuvettes were filled

immediately upon mixing the batch and again at the end of pouring out the solution to measure

pH and ensure consistency of each aliquot.) For the freshwater test in Lake Michigan

instruments were exposed to NIST buffers prepared by ACT personnel using salts obtained from

Kenneth Pratt (NIST) or lake water CRMs as appropriate for the instrument. Both the buffers

and the CRMs were characterized by spectrophotometric analysis by ACT personnel. All pre-

deployment instrument measurements of the reference buffers were in a water bath at a constant

temperature (20

o

C, except at HIMB which were at 25

o

C) and all solutions and instruments were

pre-equilibrated at this temperature.

For the deployment, instruments were programmed to record data based on a time

interval that allowed for a 30 day (or 90 day for HI) deployment. Intervals were selected such

that there was a common 30 (or 60) minute interval achieved by all instruments. This schedule

allowed us to coordinate our reference sampling for all instruments. Internal clocks were set to

local time and synchronized against the time standard provided b

y www.time.gov .

In high flow

coastal environments, clock drift could lead to significant bias.

Instrument Deployment

– A photograph of each individual instrument and the entire instrument

rack was taken just prior to deployment and just after recovery to provide a qualitative estimate

of biofouling during the field tests. Instruments were set-up as self-recording on a deployment

rack and arranged so that a single representative field sample could be collected within 1 meter

of any individual sampling inlet. The deployment frames were arranged so that all of the

instruments remain at a fixed depth of 1 m below the water surface (using a float system or fixed

dock in environments not affected by tidal changes or strong wave action). Two calibrated

SeaBird CTD packages and four RBR Solo thermistors were attached to the mooring at each test

site in order to accurately characterize the temperature and salinity heterogeneity surrounding the

mooring. In these dynamic coastal regions it was critical to understand the spatial and temporal

dynamics of the water column in order to interpret pH measurements appropriately.

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