Abstract
This paper deals with hydrogeological conditions and geochemistry of swamp waters. It is shown that swamp waters are noted for exceptionally low TDS, low pH value, high content of Fe, organic matter, and increased content of NO 3, NH 4, PO 4. In swamp waters the content of organic substances exceeds that of mineral substances, which makes these waters organogenic. The composition of organic matter is characterized by pronounced predominance of humic matter, while bitumen and hydrocarbons occur in smaller quantities.
| Original language | English |
|---|---|
| Title of host publication | Water-Rock Interaction - Proceedings of the 13th International Conference on Water-Rock Interaction, WRI-13 |
| Pages | 955-958 |
| Number of pages | 4 |
| Publication status | Published - 2010 |
| Event | 13th International Conference on Water-Rock Interaction, WRI-13 - Guanajuato, Mexico Duration: 16 Aug 2010 → 20 Aug 2010 |
Other
| Other | 13th International Conference on Water-Rock Interaction, WRI-13 |
|---|---|
| Country | Mexico |
| City | Guanajuato |
| Period | 16.8.10 → 20.8.10 |
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ASJC Scopus subject areas
- Geology
Cite this
Chemical characteristics of swamp waters : A case study in the Tom River basin, Russia. / Naymushina, O. S.; Shvartsev, S. L.; Zdvizhkov, M. A.; El-Shinawi, A.
Water-Rock Interaction - Proceedings of the 13th International Conference on Water-Rock Interaction, WRI-13. 2010. p. 955-958.Research output: Chapter in Book/Report/Conference proceeding › Conference contribution
}
TY - GEN
T1 - Chemical characteristics of swamp waters
T2 - A case study in the Tom River basin, Russia
AU - Naymushina, O. S.
AU - Shvartsev, S. L.
AU - Zdvizhkov, M. A.
AU - El-Shinawi, A.
PY - 2010
Y1 - 2010
N2 - This paper deals with hydrogeological conditions and geochemistry of swamp waters. It is shown that swamp waters are noted for exceptionally low TDS, low pH value, high content of Fe, organic matter, and increased content of NO 3, NH 4, PO 4. In swamp waters the content of organic substances exceeds that of mineral substances, which makes these waters organogenic. The composition of organic matter is characterized by pronounced predominance of humic matter, while bitumen and hydrocarbons occur in smaller quantities.
AB - This paper deals with hydrogeological conditions and geochemistry of swamp waters. It is shown that swamp waters are noted for exceptionally low TDS, low pH value, high content of Fe, organic matter, and increased content of NO 3, NH 4, PO 4. In swamp waters the content of organic substances exceeds that of mineral substances, which makes these waters organogenic. The composition of organic matter is characterized by pronounced predominance of humic matter, while bitumen and hydrocarbons occur in smaller quantities.
UR - http://www.scopus.com/inward/record.url?scp=84860138992&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=84860138992&partnerID=8YFLogxK
M3 - Conference contribution
AN - SCOPUS:84860138992
SN - 9780415604260
SP - 955
EP - 958
BT - Water-Rock Interaction - Proceedings of the 13th International Conference on Water-Rock Interaction, WRI-13
ER -