Saturday, February 4, 2006 we conducted the second session of the karst springs of Fornovolasco levies. We found both sources that the cave where we accompanied the speleogita slightly in the middle, which is positive for the different flow rates during sampling sessions. These days we can compare the data of chemical and physical analysis and begin to draw comparative charts.
Then the analyst can write a report on water quality.
0 comments:
Post a Comment