Embedded Files
Limnological campaigns - Periodic water quality monitoring
Prepared by Xavier Lazzaro (IRD/BOREA)
Viviana Cruz Hernández. William Lanza Aguilar (IE/UMSA)
& Javier Maldonado Alfaro (IIGEO/UMSA)
Material and methods
To evaluate the spatial evolution of water quality in the areas of influence of wastewater from El Alto through the Katari watershed, limnological sampling and measurement campaigns are carried out at representative stations. These stations are located in various sectors of the northeastern region (Chúa, Huatajata, Paco Island (Suriqui), Quehuaya, Cumana Bay, Puerto Pérez, Cojata Island, Huarina), the central region (Katari river mouths, Sehuenca and Cohana, Cumana lagoon, Cohana bay), and the region south of Cohana bay (Pariti and Sicuya islands, littoral cattails (Totora), Chojasivi and Katari channel, coastline towards the Taraco peninsula) (see map).
These campaigns are repeated throughout the most representative periods of the year, i.e. during the dry season (May - October) and rainy season (November - April), as well as during the transitions between rainy and dry, and dry and rainy seasons. The two periods of greatest risk of deterioration are the rainy season (with the greatest contribution of multiple pollution: domestic, industrial and mining) and the transition to the dry season when (with increased evaporation and reduced river flows) there is a concentration of pollutants and nutrients that favor the growth of microalgae.) These campaigns have two objectives: (1) To quantify the seasonal and interannual variability of the parameters, repeating these campaigns throughout the three years of the pilot (2019-2021). (2) Identify a water quality monitoring network, selecting the most representative stations for the study of eutrophication processes, the location of eutrophication gradients and areas with higher risks of proliferation (called efflorescence or 'bloom') of phytoplankton microalgae. In fact, blooms can cause massive die-offs of fish, frogs and waterfowl, as occurred in April-May 2015 when Carteria sp., a green microalgae, proliferated in the northern and central regions of Lago Menor, up to the tip of the Taraco peninsula.
Figure 1 - Study site of the permanent Observatory of Lake Titicaca, centered on the shallow northeastern and central regions of Minor Lake. The orange (Northern region) and yellow circles (Cohana) represent some of the stations of the limnological monitoring network including the location of the HydroMet Buoy ('Mi Boya').
This periodic monitoring is carried out on the basis of measurement and collection campaigns with a frequency of 5-10 days (the frequency of the Sentinel-2 satellites) at a network of limnological stations located in representative areas particularly vulnerable to eutrophication. These stations are located along transects (gradients) from pollution sources (e.g. the mouth of the Katari River in Cohana Bay) towards the open water, or along the coastline in front of point sources (e.g. villages, activity centers...) or diffuse sources (e.g. agricultural and livestock fields...) of pollution. Its objective is to identify areas in a state of eutrophication, so that the institutions responsible for management and restoration policies can implement mitigation measures.
Probe measurements
Physicochemical and biological water quality measurements are performed at each limnological station using submersible probes (FluoroProbe BBE, YSI EXO2 and Biospherical C-OPS); see table below:
The FluoroProbe bbe
Instrument features - The FluoroProbe bbe is a highly sensitive measuring instrument for chlorophyll-a analysis with determination of four microalgae classes. During the measurements individual profiles of green algae, blue-green algae (or cyanobacteria), diatoms + dinoflagellates and cryptophytes are taken.
This makes it possible to analyze the occurrence and distribution of, for example, cyanobacteria in situ without recourse to the laboratory. Possible interferences due to 'yellow substances' (major component of the dissolved organic matter in the water, consisting of molecules that are mainly leached from decomposing detritus and organic matter) are eliminated by an integrated CDOM (Colored Dissolved Organic Matter) correction factor.
The in vivo chlorophyll-a measurement can be affected by particulate matter in the water body. Therefore, a correction is essential when turbidity is too high. The FluoroProbe bbe with the optional transmission sensor provides automatic turbidity correction using the latest bbe++ software extension. Turbidity correction with the FluoroProbe makes the determination of chlorophyll-a even more reliable.
The FluoroProbe bbe can quickly and reliably determine the chlorophyll-a content of different kinds of microalgae down to a depth of 100 m. The measurement data can be visualized and displayed on a screen. The measurement data can be displayed in real time on a PC or stored in the probe for further evaluation.
Measurement principle - The fluorescence of algae (emission at a wavelength of about 700 nm) due to excitation by visible light depends mainly on the presence of chlorophyll-a, the main pigment responsible for photosynthesis in the plant world. The presence of other pigments is typical of different kinds of algae. The interactions between these different pigment systems with chlorophyll-a result in a special excitation spectrum for the taxonomic classes of algae.
The special patterns of this algal fluorescence - the so-called fingerprints - are used in bbe fluorometers for the quantification of the different algal classes. The excitation light sources are LEDs with different wavelengths. The fingerprints of four algae classes and the yellow substances are already stored in the FluoroProbe. Special user-defined fingerprints can also be added.
Units - Measurements are expressed in µg chl-a/L, in a range of 0 - 200 µg chl-a/L.
The YSI EXO2 Multi-Parameter Sonde
Features - This multi-parameter water quality sonde includes 7 sensor ports (including a center wiper port = a brush), a depth sensor and a battery compartment (4 alkaline D-cell batteries). It is the best-in-class platform for the highest quality data. The dynamic range of the EXO2's smart sensors provides comprehensive multi-parametric water quality data, while SmartQC ensures proper calibrations and best sensor performance. You can be confident in the extended deployments thanks to EXO2's rugged materials and unmatched anti-fouling technology. Depth range: 0 to 250 m.
Parameters - The 6 Smart sensors installed measure:
- Conductivity (in µS/cm) / Temperature (in ºC).
- Dissolved oxygen (in % saturation and mg/L)
- fDOM (fluorescent dissolved organic matter, in RFU = Relative Fluorescence Unit)
- pH and ORP (oxido-reduction potential, in mV)
- Total algae: chlorophyll-a + phycocyanin (in RFU)
- Turbidity (in NTU = Nephelometric Turbidity Unit)
Memory capacity - 512 MB, >1,000,000 recorded readings.
The Biospherical Inc. C-OPS Spectroradiometer
Features - The C-OPS ('Compact Optical Profiling System') is a state-of-the-art optical profiling system for determining apparent optical properties in aquatic systems. It consists of a 7-cm diameter radiometer that measures downward water irradiance, pressure/depth and dual-axis inclinations. This submersible radiometer (EdZ) is equipped with up to 19 optical filter microradiometers, selected from 8 different wavelengths: UV-B ﴾305 and 313 nm﴿, UV-A ﴾320, 340, 380 and 395 nm﴿, and visible or PAR ﴾412 and 400-700 nm﴿. They are mounted on a unique free-falling, kite-like backplate. To avoid boat or dock shadow influences, the structure can be optimized for slow descent rates for work in very shallow (e.g., 3 m) and coastal waters, or for faster descent rates for open ocean observations. In the lake, we use a rate of 30 cm/s. The C-OPS is so light that it can be deployed by hand by almost anyone, and the system can be operated from small or large boats.
The submersible C-OPS is complemented by an airborne radiometer (Ed0) of the same characteristics installed on top of a mast, in order to simultaneously measure solar irradiance (incident energy) and downward energy absorbed vertically in the water column. The two radiometers are powered by a Deckbox battery connected to the PC for data transmission.
Parameters - From the exponential decay curve of the incident solar radiation with depth, the C-OPS allows the calculation of the extinction coefficient Kd (in m-1), using the formula: Iz = Io exp (-Kd z), where Iz is the incident energy at depth z, Io is the subsurface incident energy (just below the water surface). The light extinction depth z1% is the depth at which 1% of the subsurface light is received; it is calculated by the formula: z1% = -log10 (0.01)/Kd.
Units - For each wavelength: in microwatts/(cm2 nm-1) for irradiance; for PAR (Photosynthetically Active Radiation) between 400 and 700 nm: in µE/(cm-1 s-1).
Collection of water samples and planktonic organisms
Water samples are collected from different depths using a Van Dorn (horizontal) or Niskin (vertical) bottle. Before lowering it into the water, the mechanism is assembled so that the two lids are opened during the descent. When the bottle reaches the desired depth, a weight (called a 'messenger') is dropped on the cable, which when it percusses the mechanism closes the two lids to isolate the sample, then it can be brought back on board. The water sample can be used to collect samples of nutrients (nitrogen, phosphorus) or phytoplankton micro-algae.
The Niskin bottle (vertical) is an improvement of the Nansen bottle. It is the subject of a patent filed by Shale Niskin in March 1962. The bottle has two openings and the messenger does not cause the bottle to tip over as in the Nansen bottle.
The Van Dorn bottle (horizontal) consists of a transparent tube. It allows sampling at different water depths. The horizontal design of the bottle makes it ideal for sampling in stratified water areas with prevailing currents or very shallow water (< 1 m depth).
To collect zooplankton (animal plankton) samples, it can be used:
A conical net for zooplankton (diameter Ø = 30 cm, with 60 µm mesh opening) to collect from a certain depth to the surface. The volume (V, in m3 ) filtered is calculated with the formula: V = z . (r2 * 3.14) where z = depth (in m), r = net opening section = Ø / 2 (in m).
A Schindler trap allows a volume of water (usually 5 or 10 L) to be collected at a given depth. Like the Niskin and Van Dorn bottles, it has a mechanism that can be triggered at a certain depth by means of a 'messenger'.
Water transparency measurement:
The Secchi disk, was created in 1865 by Angelo Secchi. It is a smooth white circular disk 30 cm in diameter used to measure the transparency or turbidity in bodies of water. The disk is mounted on a line, and is slowly lowered into the water. The depth at which the disk is no longer visible is taken as a measure of the transparency of the water. This measure is known as the Secchi depth and is related to the turbidity of the water. Since its invention, the disk has also been used in a modified, smaller design, 20 cm (8 inches) in diameter, with alternating black and white quadrants, to measure transparency in freshwater lakes and reservoirs....
Page updated
Google Sites
Report abuse