A single groundwater sample from station F_1032 showed normal odor, color, conductivity, and pH, but oxygen saturation was low at 25.9%, which may be natural for deep groundwater or indicate localized reducing conditions. Because only one sample was analyzed, no broader conclusions can be drawn without additional sampling and historical data.
Based on the provided data, one monitoring station (F1032) was sampled, yielding one sample that was analyzed for five parameters. The measured values indicate that odor (Geruchsart) and precipitation/color (Niederschlag(Farbe)) were both negative, which is within expected conditions. Electrical conductivity at 25°C was 374 µS/cm, and pH was 7.43, both within the typical range for groundwater.
The only parameter outside the expected range was oxygen saturation (Sauerstoffsättigung), which was 25.9%, below the threshold of 50%. This low oxygen level could be natural for deep groundwater, where oxygen is consumed over long subsurface residence times, or it could indicate localized reducing conditions. Without additional context such as well depth, aquifer type, or historical trends, this single low value should not be interpreted as contamination.
Overall, the sample from station F_1032 shows generally unremarkable water quality except for low oxygen saturation. Since only one sample from one station is available, no broader conclusions about the monitoring network can be drawn. Further sampling rounds and comparison with historical data would be needed to assess whether the low oxygen level is a persistent condition or a transient anomaly.
🤖 This text was generated with the assistance of AI. All quantitative statements are derived directly from the dataset listed under Data Source.