Previous Page  6 / 59 Next Page
Information
Show Menu
Previous Page 6 / 59 Next Page
Page Background

Ref. No. [UMCES] CBL 2016-015

ACT VS16-06

6

the Stern-Volmer equation. For most lifetime-based optical DO sensors, this Stern-Volmer

relationship

(Tzero/T) – 1) versus O 2 pressure

is not strictly linear (particularly at higher oxygen

pressures) and the data must be processed using analysis by polynomial non-linear regression.

Fortunately, the non-linearity does not change significantly with time so that, as long as each

sensor is characterized with regard to its response to changing oxygen pressure, the curvature in the

relationship does not affect the ability of the sensor to accurately measure oxygen for an extended

period of time.

Xylem EXO2 DO sensor specifications:

Units

% Saturation mg/L

Temperature

Operating

Storage

-5to+50°C

-20to+80°C

Range

0to500% airsaturation

0to50mg/L

Accuracy

0-200%: ±1% reading or 1%air sat., whichever

is

greater; 200-500%:: ±5% reading 0-20 mg/L:

±1%

ofreadingor0.1mg/L;20-50mg/L;±5%reading

Response

T63<5sec

Resolution

0.1%airsat

0.01mg/L

SensorType

Optical,luminescencelifetime

Variables that could affect dissolved oxygen measurements include temperature, salinity,

and barometric pressure. Temperature and salinity are compensated for during instrument

calibration and field use with the use of additional sensors and/or instrument software settings.

Barometric pressure relates to the pressure of oxygen in the calibration environment, and barometric

pressure changes due to a change in altitude or local weather. Generally the effect of barometric

pressure is overcome by proper sensor calibration to a standard pressure. However, if the user

measures dissolved oxygen in something besides per cent saturation, then the EXO2 DO sensor can

store a local barometric reading put into the KOR software (DO % local) or the EXO2 handheld

can take a live barometric reading with its internal barometer (ODO % EU).

ODO % Sat = Raw DO reading corrected with temperature and local barometric pressure at the

time of calibration. (Local pressure/760 mmHg x 100 = % Sat.)

ODO % Local = Raw DO reading corrected with temperature and % Sat output fixed to 100%

regardless of barometric pressure entry. (The entered local barometric pressure is

used by KOR software for mg/L calculations.)