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Grundwasserchemismus im Bezirk Neubrandenburg. Teil 3. Jodid im Grundwasser

Grundwasserchemismus im Bezirk Neubrandenburg. Teil 3. Jodid im Grundwasser The iodide contents in 389 ground‐water‐tapping plants of the county are compared with the geological character of the aquifer, the carbonate and non‐carbonate hardness and the nitrate and chloride contents of the waters. 54% of the plants have I‐concentrations of 3 … 7 μg/l. In the air‐covered ground‐water (hardness quotient<2.8) 2 … 50 μg/l I are found, whereas in the confined ground‐water (hardness quotient >2.8) 2 … 50 μg/l I are contained. In general, the I‐content increases with the carbonate hardness, a connection with till existing. Therefore, ground‐waters of the Miocene have relatively low salt‐ and I‐contents. Geogenic salt influences in the form of NaCl increase the I‐contents to 50 … 100 μg/l. Anthropogenic influences in the residential area and due to waste increase the Cl−‐ and I−‐concentrations. There were not detected any dependences between the I‐ and NO3‐contents. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Acta hydrochimica et hydrobiologica Wiley

Grundwasserchemismus im Bezirk Neubrandenburg. Teil 3. Jodid im Grundwasser

Deibel, K.
Acta hydrochimica et hydrobiologica , Volume 18 (1) – Jan 1, 1990
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References (7)

Publisher
Wiley
Copyright
Copyright © 1990 Wiley Subscription Services, Inc., A Wiley Company
ISSN
0323-4320
eISSN
1521-401X
DOI
10.1002/aheh.19900180117
Publisher site
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Abstract

The iodide contents in 389 ground‐water‐tapping plants of the county are compared with the geological character of the aquifer, the carbonate and non‐carbonate hardness and the nitrate and chloride contents of the waters. 54% of the plants have I‐concentrations of 3 … 7 μg/l. In the air‐covered ground‐water (hardness quotient<2.8) 2 … 50 μg/l I are found, whereas in the confined ground‐water (hardness quotient >2.8) 2 … 50 μg/l I are contained. In general, the I‐content increases with the carbonate hardness, a connection with till existing. Therefore, ground‐waters of the Miocene have relatively low salt‐ and I‐contents. Geogenic salt influences in the form of NaCl increase the I‐contents to 50 … 100 μg/l. Anthropogenic influences in the residential area and due to waste increase the Cl−‐ and I−‐concentrations. There were not detected any dependences between the I‐ and NO3‐contents.

Journal

Acta hydrochimica et hydrobiologica – Wiley

Published: Jan 1, 1990

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