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Ref. No. [UMCES] CBL 2016-011

ACT VS16-02

26

Individual response slopes and intercepts of instrument measurement versus reference DO

for each of the laboratory trials at a fixed temperature and salinity level are summarized in Table 4.

Slope responses are somewhat variable across temperature with no uniform trend. The response

slopes did decrease slightly across salinity levels, averaging 1.22, 1.11, and 1.01 for salinity trials

of 0, 10, and 35, respectively.

Table 4.

Summary of regression statistics for the PME miniDOT versus reference sample response curves

for each of the nine laboratory trials.

Test ID

R2

y Intercept

Slope

LT15S00

0.921

-2.203

1.660

LT15S10

0.913

-1.470

1.312

LT15S35

0.996

-0.426

1.062

LT04S00

1.000

-0.110

0.991

LT04S10

0.999

-0.021

0.983

LT04S35

1.000

-0.042

0.960

LT30S00

1.000

0.053

1.018

LT30S10

0.997

-0.125

1.042

LT30S35

1.000

0.089

1.005

Results of the 56 day long-term stability and thermal stress challenge for the PME

miniDOT are shown in figure K. The instrument was maintained in a well circulated tank and

oxygen content manipulated by alternately varying water temperature set point between 15 and

25

o

C several times per week of deployment. The data completion result for the stability test was

100%. The time series of instrument readings at 15min intervals is plotted against discrete values

for Winkler reference samples (

top panel

) along with the time series of the difference between

instrument and reference measurements (

bottom panel

).

The overall mean difference between

measurements was

0.034 (s.d. = 0.107) mg/L for 77 comparisons (out of a potential total of 77).

There was a small but statistically significant trend in accuracy over time (slope = -0.002 mg/L/d;

r2 = 0.11; p=0.003) indicating very modest performance drift over the 56 days.

Results for a sensor response time assessment of the PME miniDOT are shown in figure L.

The top panel depicts the time series of 5s instrument reads during transfers between adjacent high

(9.6 mg/L) and low (2.0 mg/L) DO water baths, maintained commonly at 15

o

C. The bottom panel

(

lower left

) depicts results fit with a 3 parameter exponential decay function: DO

rel

= DO

relMin

+ a

e

-

bt

and indicated τ calculated from fit. Data for low DO to high DO transitions (

lower right

) were

treated similarly but normalized to steady state value in subsequent high DO tank and subsequently

fit with an analogous 3 parameter exponential rise function: DO

rel

= DO

relMin

+ a(1-

e

-bt

) with

indicated τ being directly calculated from fit.

The calculated τ

90

was 90 s during high to low

transitions and 63 s for low to high transitions covering a DO range of approximately 8 mg/L at a

constant 15

o

C.