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Quality of Drinking Water
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Quality of Groundwater
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On Index
The tables below show the results of measurements of bacteria in drinking water in the Norðurþing, Thingeyjarsveit and Skútustaðahreppur.
This graph shows conductivity in drinking water. The conductivity was not measured in Reykjahlíð in 2015.
Conductivity is measured in Siemens pr. meter or S/m.
This graph show acidity in drinking water. Acidity is measured in pH.
This graph shows the temperature in five springs by Lake Mývatn. Where the graph shows 0 for the springs it means measurements are missing.
This graph shows water conductivity at 25°C in µS/cm.
This graph shows the concentration of arsenic (As) in springs by Lake Mývatn. Where the graph shows 0.05 the concentration was below that number.
Environmental limits I for arsenic 0.4 µg/L
This graph shows the concentration of silicon dioxide (SiO2) in springs by Lake Mývatn.
This graph shows the concentration of chromium in springs by Lake Mývatn. Where no values are shown measurements are missing.
Environmental limits I: Very little or no danger of effects. Guideline limits for chromium are 0.3 µg/L
Environmental limits II: Little danger of effects. Guideline limits for chromium are 0.3-5 µg/L
This graph shows the temperature of groundwater in Þeistareykir and Kelduhverfi.
This graph shows the conductivity of water at 25°C from springs and boreholes in Þeistareykir and Kelduhverfi.
This graph shows the concentration of silicon dioxide in groundwater in Þeistareykir and Kelduhverfi.
This graph shows the concentration of arsenic in groundwater in Þeistareykir and Kelduhverfi.
Environmental limits I for arsenic 0.4
This graph shows the concentration of chromium in groundwater in Þeistareykir and Kelduhverfi.
Environmental limits I for chromium 0.3
Environmental limits II for chromium 0,3-5
Water facilities make sure that inhabitants and businesses have clean drinking water. It is important to secure the quality of that water. The concentration of nutrients and minerals needs to be monitored in cold water in power plant areas and planned areas for power plants.
In this index, the water supply and distribution system of water in Húsavík will be monitored:
Quality of groundwater in springs and underground streams from geothermal power plants will be monitored. Measurements from the following places will be published:
Mývatnssveit
Þeistareykir and Kelduhverfi
The following chemicals and parameters have been chosen to show results:
Chromium is an element with the chemical formula Cr. Chromium is categorised as a heavy metal which means it is a metal with a high mass. A number of chemicals belong to that group but exogenous ones are considered to be arsenic, lead, cadmium, cobalt, chromium, mercury, nickel, tin and vanadium. These metals are found in nature in air, soil, water and in small quantities in organisms. Many of those metals play a major role in metabolic pathways and it is necessary for organisms to pick them up in small quantities. Most heavy metals can cause toxicity if the quantities get bigger. Chemical samples are taken once per year and if the amount of chromium in water gets higher because of geothermal processing it can be because of oxidisation in the machinery.
Arsenic is an element with the chemical formula As. Arsenic is most often considered a heavy metal because of its density even though, in fact, it is a metalloid. The concentration of arsenic and other chemicals in geothermal water is higher than in groundwater because of the interaction of water and rock at high temperatures in the geothermal system. In geothermal processing, chemicals are released into water and air. In the waste water from geothermal power stations and geothermal areas there is a higher concentration of dissolved chemicals than in drinking water and arsenic is one of those chemicals.
Silicic acid is a chemical compound of the elements silicon (Si) and oxygen (and hydrogen) (SiO2 or H4O4Si) and is the dissolved form of silica. The word silicon is commonly used for both the element and the chemical compound. The concentration of silicon and more chemicals in geothermal water is high because of the interaction of water and rock at high temperature in the geothermal system. In geothermal processing, chemicals are released into water and air. In the waste water from geothermal power stations and geothermal areas there is a higher concentration of dissolved chemicals than in drinking water and silicic acid is one of those chemicals. By monitoring the concentration of silicon in water, any geothermal effects can be seen.
Temperature and conductivity of the water in monitored areas in Mývatnssveit, Þeistareykir and Kelduhverfi is measured once per year as well as a sample being taken. The places where the samples are taken can be streams, monitored holes or springs (hot, tepid and cold). If the conductivity measurements go up, it would be an indication of higher chemical concentration in the water and therefore increased effects of the geothermal energy. The concentration in geothermal water is higher than groundwater because of the interaction of water and rock at high temperature in the geothermal system. The same applies if temperature rises in water in sampling areas which would be an indication of increased effects of geothermal energy.
Data showing the quality of drinking water and groundwater in springs and underground from geothermal power stations in the above-mentioned sampling areas will be published yearly.
Data from the central area will be compared.
The project manager is responsible for acquiring the data and publishing it according to the publishing schedule.
Data will be collected from Heilbrigðiseftirlits Norðurlands eystra (Public Health Authority) and Landsvirkjun/ÍSOR