Difference between revisions of "In situ monitoring of eutrophication"
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Oceanographic [[nutrient]] measurements are commonly made using traditional methods by collecting water samples with subsequent analysis in the laboratory. Besides the risk of quality degradation of the sample the amount of samples and temporal resolution is also limited. | Oceanographic [[nutrient]] measurements are commonly made using traditional methods by collecting water samples with subsequent analysis in the laboratory. Besides the risk of quality degradation of the sample the amount of samples and temporal resolution is also limited. | ||
Nutrient analyzers are used in situ to measure nutrients such as nitrate, nitrite, ammonia, phosphate, silicate. Most in situ nutrient sensors analyzers use wet chemical techniques based on laboratory methods. Alternatives include nitrate analysis using UV-absorbance. | Nutrient analyzers are used in situ to measure nutrients such as nitrate, nitrite, ammonia, phosphate, silicate. Most in situ nutrient sensors analyzers use wet chemical techniques based on laboratory methods. Alternatives include nitrate analysis using UV-absorbance. | ||
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| + | Hanson, A.; Moore, C. (2001). Real-time nutrient surveys in coastal waters: new submersible chemical analyzer speeds real-time nutrient profiling. Sea Technol. 42(9): 10-14 | ||
==Sensors== | ==Sensors== | ||
Revision as of 11:38, 27 November 2013
Introduction
In situ monitoring is the observation and / or measurement of events in its original place (Latin: situs). Oceanographic instruments containing different types of sensors are used to monitor eutrophication in coastal waters. Sensors detect and respond to electrical or optical signals and convert the physical, chemical or biological parameter into a signal which can be measured electrically.
Oceanographic instruments
In this section we focus only on the instruments[1] that measure parameters that are important in the frame of the OSPAR Eutrophication Monitoring Programme: [2]
CTD
The CTD[3][4] - Conductivity, Temperature and Depth - is the standard oceanographic tool for continuously measurement of physical properties of sea water. The instrument contains a cluster of sensors for measuring conductivity, temperature and depth. Depth and salinity are derived from measurements of pressure and electrical conductivity. The CTD is mostly attached to a frame with water-collecting Niskin bottles (CTD rosette). From the deck the rosette is lowered on a cable down to the seafloor and once in the water data are transferred via a conducting cable connecting the CTD to a computer on a ship. The Niskin bottles are closed at predefined depths to target water samples for further analysis. Other sensors to measure chemical or biological parameters such as dissolved oxygen, chlorophyll fluorescence (phytoplankton concentrations) and water light transmission can be added to the cluster.
Expendable bathythermograph
The eXpendable BathyThermograph (XBT) is a free-fall temperature probe providing a profile of measured temperature against depth calculated from a fall-rate model (not by measuring pressure). The XBT is dropped from a ship and measures the temperature (thermistor) as it falls through the water. Two very small copper wires transmit the temperature data to the ship. The depth is calculated from the elapsed time and the expected fall rate. By plotting temperature as a function of depth, scientists obtain a temperature profile of the ocean.
Thermosalinograph
A ThermoSalinoGraph (TSG) are automated instruments which continuously measure the sea surface temperature and conductivity along the track and on board of the ship using a water intake system (in flow-through systems). Conductivity and thermistor cells provide the measurements and salinity is derived from these parameters. The TSG is manually turned on once the ship leaves the port. Water flows through the tubes of the instrument which is located in the hull of the vessel. The position of the ship is given by a GPS. A computer collects all data and processes them. Optionally other types of sensors can be added to the instrument for a wider range of measurements.
Continuous Plankton Recorder[5]
The Continuous Plankton Recorder (CPR) is an instrument used to sample and to continuously collect plankton over a long distance at a depth of approximately 10 meters. Water passes through the CPR and plankton are filtered onto a slow-moving band of silk (270 micron mesh size) and covered by a second silk. The silk and plankton are then spooled into a storage tank containing formalin. The silk is divided into samples representing 10 nautical miles of tow. Analysis is done in two ways:
- Determination of the Phytoplankton Colour Index (PCI): the PCI is an in situ measure of ocean colour and a semi quantitative estimate of phytoplankton biomass. The colour of the silk is evaluated against a standard colour chart and given a 'green-ness' value based on the visual discoloration of the CPR silk produced by green chlorophyll pigments.
- Microscopic analysis: individual phytoplankton and zooplankton taxa are identified and counted.
Nutrient analyzers
Oceanographic nutrient measurements are commonly made using traditional methods by collecting water samples with subsequent analysis in the laboratory. Besides the risk of quality degradation of the sample the amount of samples and temporal resolution is also limited. Nutrient analyzers are used in situ to measure nutrients such as nitrate, nitrite, ammonia, phosphate, silicate. Most in situ nutrient sensors analyzers use wet chemical techniques based on laboratory methods. Alternatives include nitrate analysis using UV-absorbance.
Hanson, A.; Moore, C. (2001). Real-time nutrient surveys in coastal waters: new submersible chemical analyzer speeds real-time nutrient profiling. Sea Technol. 42(9): 10-14
Sensors
In this section we focus only on sensors that measure parameters that are important in the frame of the OSPAR Eutrophication Monitoring Programme: [6]
Temperature
The simplest mechanical way to measure temperature is by using a mercury-in-glass thermometer. They are commonly used to measure sea surface temperature by placing it in a bucket of sea water. Electrical temperature sensors such as the Resistance Temperature Detectors (RTDs) and the thermistors are more frequently used on a CTD. A thermistor is a type of resistor composed of a small piece of electrically semiconductor material (metallic oxides) such as a resistor which exhibits a large change in resistance proportional to a small change in temperature (negative temperature coefficient). RTDs are sensors used to measure temperature by correlating the resistance of the RTD element (pure metals usually platinum) with temperature (positive temperature coefficient).
Salinity
Salinity is a measure of the quantity of salt in a volume of sea water and can be measured in situ using a conductivity sensor on a CTD. The sensor measures the electrical conductivity (electrical current: ions in solution that flow through the sea water (dissolved salts conduct more electricity than water without salts)) at a known temperature and pressure and this conductivity is converted to salinity using a formula.
Turbidity
Turbidity is a measure of water clarity or transparency caused by suspended particles from organic (algae, plankton) or inorganic (fine silts or clays) origin. The more turbid the water the less light is transmitted. A common simple and cheap device for manually measuring ocean turbidity is the Secchi disk which consists of a circular disk (20-30 cm in diameter). The disc is being lowered into the water and the depth at which the disc is no longer visible, is a measure of the clarity of the water and is known as the Secchi depth and is related to water turbidity. The Secchi disk readings do not provide an exact measure of transparency (for example: interpretation of different observers) and are often replaced by the use of turbidity sensors. Turbidity sensors designed for extended in situ measurements are based on nephelometric or optical-backscatter principles where the scattering and absorbing effects of the suspended particles on light are measured [7]. Nephelometers measure the concentration of suspended particles in a liquid by employing a light beam 90 degrees from the light detector. Particle density is then a function of the light reflected into the detector from the particles. Optical-backscatter sensors (OBS) measure the same properties as nephelometers but the angle between the light source and the detector is less than 90 degrees.
Dissolved oxygen
Phytoplankton chlorophyll a
An important consequence of the enrichment of nutrients (eutrophication) is the growth of algae and other phytoplankton. These algae contain chlorophyll, an important biochemical component that is responsible for photosynthesis. Chlorophyll a is the most abundant form of chlorophyll within photosynthetic organisms and gives plants their green color. The amount of chlorophyll found in a water sample is used to estimate the concentration of phytoplankton (biomass). The chlorophyll (a colored algal pigment) absorbs red and blue light and reflects green light. For in situ monitoring fluorescence sensors or fluorometers are used to induce chlorophyll fluorescence by shining a beam of light of the proper wavelength into the water and then measuring the higher wavelength light which is emitted [8]. The chlorophyll fluoresces at a wavelength of 650-750 nm when excited by radiation at a wavelength of 400-470 nm [9]. In situ measurements are only rough approximations of chlorophyll a concentrations and need to be enhanced through laboratory (extraction) methods.
More information
- Temperature sensors
- Salinity sensors
- Turbidity sensors
- Fluorescence sensors
- Optical backscatter point sensor (OBS)
- Continuous Plankton Recorder (CPR)
See also
References
- ↑ Oceanographic Instrumentation, Australian Oceanographic Data Centre, Data Management Group DMG DOC No: 4/98[1]
- ↑ OSPAR Commission (2005), Agreement on the Eutrophication Monitoring Programme (Reference Number: 2005-4)[2]
- ↑ http://www.whoi.edu/instruments/viewInstrument.do?id=1003[3]
- ↑ http://noc.ac.uk/research-at-sea/nmfss/nmep/ctd[4]
- ↑ CPR sampling: the technical background, materials and methods, consistency and comparability Batten, S.D.; Clark, R.; Flinkman, J.; Hays, G.; John, E.; John, A.W.G.; Jonas, T.; Lindley, J.A.; Stevens, D.P.; Walne, A. (2003) . Progress in Oceanography 58(2-4): 193-215.
- ↑ OSPAR Commission (2005), Agreement on the Eutrophication Monitoring Programme (Reference Number: 2005-4)[5]
- ↑ Rasmussen, P.P., Gray, J.R., Glysson, G.D., and Ziegler, A.C., 2009, Guidelines and procedures for computing time-series suspended-sediment concentrations and loads from in-stream turbidity-sensor and streamflow data: U.S. Geological Survey Techniques and Methods book 3, chap. C4, 53 p.
- ↑ YSI, Technical Notes, The Basics of Chorophyll Measurement[6]
- ↑ Fluorescence sensors
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