eutech-instruments ecoscan do 6 do meter User Manual
Instruction Manual
DO 6
66
14.1.4 Air
Calibration
Understanding the principle of air calibration is easy, once you know that it is
partial pressure that the probe is responding to. When the probe is in air, it is
measuring the partial pressure of oxygen in air. If water is air saturated, then
the partial pressure of oxygen in the water will be the same as it is in air.
Therefore, all you need to know is the temperature of the air in which the probe
is placed. By consulting solubility tables for oxygen at the particular barometric
pressure and salinity of the water being measured, the corresponding
concentration (mg/L or ppm) can be found for air saturated water at the air
calibration temperature, and the meter can be set accordingly. Because most
meters are temperature compensated, they will still give correct readings in
mg/L even though the actual water temperature may be different to the air
calibration temperature.
partial pressure that the probe is responding to. When the probe is in air, it is
measuring the partial pressure of oxygen in air. If water is air saturated, then
the partial pressure of oxygen in the water will be the same as it is in air.
Therefore, all you need to know is the temperature of the air in which the probe
is placed. By consulting solubility tables for oxygen at the particular barometric
pressure and salinity of the water being measured, the corresponding
concentration (mg/L or ppm) can be found for air saturated water at the air
calibration temperature, and the meter can be set accordingly. Because most
meters are temperature compensated, they will still give correct readings in
mg/L even though the actual water temperature may be different to the air
calibration temperature.
Note: The closer the air calibration temperature to the water temperature, the
more accurate is the calibration.
more accurate is the calibration.
14.1.5 Applications
Oxygen is essential for fish, invertebrate, plant, and aerobic bacteria respiration.
DO levels below 3 ppm are stressful to most aquatic organisms. Levels below 2
or 1 ppm will not support fish. Fish growth and activity usually require 5 to 6
ppm of DO, an important consideration for Aqua-culture industry.
DO levels below 3 ppm are stressful to most aquatic organisms. Levels below 2
or 1 ppm will not support fish. Fish growth and activity usually require 5 to 6
ppm of DO, an important consideration for Aqua-culture industry.
Low DO indicates a demand on the oxygen of the system. Natural organic
material such as leaves accumulate in the stream and create an oxygen
demand as it is decomposed. Organic materials from human activities also
create an oxygen demand in the system. Micro-organisms consume oxygen as
they decompose sewage, urban and agricultural run-off, and discharge from
food-processing plants, meat-packing plants and diaries. There is an optimum
DO level for this process and if DO level falls too low, the micro-organisms die
and the decomposition ceases. If DO level is too high, more power is used than
necessary for aeration and the process becomes costly.
material such as leaves accumulate in the stream and create an oxygen
demand as it is decomposed. Organic materials from human activities also
create an oxygen demand in the system. Micro-organisms consume oxygen as
they decompose sewage, urban and agricultural run-off, and discharge from
food-processing plants, meat-packing plants and diaries. There is an optimum
DO level for this process and if DO level falls too low, the micro-organisms die
and the decomposition ceases. If DO level is too high, more power is used than
necessary for aeration and the process becomes costly.