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How we did the work We studied two rivers (Belelle and Mandeo) and two
intertidal zones (Ortigueira’s ria and Cobas beach). Dates: November and March Students involved: 1st ESO (12-13 year-olds), 2nd ESO
(12-13 year-olds), 3rd ESO (14-15 year-olds), 4th ESO (15-16 year-olds) and 1st Bach (16-17 year-olds)
Subjects: Biology, Chemistry and Science for the Contemporary World
We worked on the field, in the lab and in class. We organised some conferences about these subjects.
Rivers
Aspects observed: Parts of the course Flora and fauna Chemical data Anthropogenic
action Pollution
Uses: energy, agriculture, recreation
Parts of the rivers’ course
High course
- The river has more inclination and carries little water.
- Due to the inclination the water is very oxygenated.
Middle course
- Higher flow; affluents; riparian forest.
Low course
- Forms part of the estuary.
The course of the rivers is divided in three parts:
Parts of the rivers studied We only observed and collected data in the middle course and
the low course of the rivers. In the middle course the water is more dynamic and has more
disolved oxygen, so it is cleaner. This is the part where the water for human supply (consumption) comes from.
The low course of the river• The low course is less dynamic and the quantity of disolved oxygen is
lower.• The low course may be under the influence of tides.
Flora: the riparian forest The riparian forest is one of the most outstanding
features of the river bank. It follows the river course. It’s important for the conservation of the river course. Common trees: European alder, sycamore plane,
hazelnut tree, bay laurel and oak.
Flora: the riparian forest
Sycamore plane Acer pseudoplatanus
Hazelnut treeCorilus avellana
Alder Alnus glutinosa
FAUNA
Chysomela menthastri
on mint leaf
Mint beetleTemporary frog
Calopterix virgo Salamander
Erithacus rubeculaEuropean robin
Lutra lutraEuropean otter
Gerris lacustris
Chemical data We measured temperature, pH, conductivity and
dissolved oxygen in the middle course and the low course of the river.
Chemical dataPart of the river
Temperature pH Conductivity Dissolved oxygen
Belelle river Middle course
9.6 ºC 6.64 190 µS/cm 8.5 ppm
Low course 10.1 ºC 7.15 251µs /cm 8.3 ppm
Conclusions: The highest pH and conductivity are found in the low course due to the influence of tides.
Portable digital Multiline P3 WTW
Anthropogenic action
It’s noticeable all along the course of the riverIt has been present for a long time because water is very useful and necessary, as some constructions we found on the way bear witness to. Nowadays, there is still pressure due to the same reasons
Some constructions in the river bank
UsesThe uses that we could observe were: household consumption, irrigation, farming usage, power generation, recreational uses
Waterwheel
Irrigation
Recreation
Uses
Hydroelectrical plant
Public washing place
Detour for consumption
Recreational uses
Agriculture and livestock
High tide line: supralittoral zoneThe high tide line features species like:
Armeria flowers
Xantoria and Crythmun maritimun
Crythmun marking the high tide line
Specific fauna
LimpetAnemone
Balanus sp.
Monodonta sp. Litorina litoralis
Carcinus maenas
Pollicipes cornucopia
Clams / Cardium edule
Martesterias glaciaris
Holoturia
Intertidal zone: occasional fauna
Cormoran
Seagull colony
Purple sandpiper
Rat
Anas platyrhynchos
Larus argentatus
Dolphin family - Calderon
In the lab: seawater study
The aim of the study was:
To separate the seaweed’s pigments by paper chromatography.
To extract iodine from seaweed.
To measure the density of seawater.
A sample of seawater and seaweed was taken to the lab.
Density of sea water. Results
Mass
(g)
Volume(cm3)
Density
(g/cm3)
25,51 25 1.020
25,49 25 1.019
25,47 25 1.019
Density (g/cm3) 1.019
The density of sea water in Cobas beach is 1019 kg/m3
Changes and pollution
Private property, law isn’t respected. No public walking path
Rats: waste waters
Discarded fishing gear