Preconditions to Technogenic Metamorphization of Nadym River Water Ionic Composition in Conditions of Global Climate Change
https://doi.org/10.31857/S2587556620010069
Abstract
The hydrochemical regime changes of Nadym River near city of Nadym from the start of regular observations in 1955 till 2016 in conditions of anthropogenic impact and global climate change was reviewed. Shown, that the relations between the major ion concentrations (ions of sodium and potassium, calcium, magnesium, chlorides, sulfates and bicarbonates) and water discharge from 1980 are getting weaker down to insignificant. Likewise, disturbances the natural ratio between the major ions, which most pronounced in a strong positive trend of the sulfate ions content in river water, are arise. The data on the long-term dynamics of the main ions in the main phases of the hydrological regime (spring high water, summer-autumn and winter low water) are presented. The probable causes of the observed preconditions to technogenic metamorphization of Nadym River ionic composition are considered: impact of untreated sewage discharge, atmospheric transport of anthropogenic and natural sulfur compounds, and pollution by mineralized formation waters. It has been suggested that the sulfates increased during all phases of the hydrological regime, including the winter low water, is associated with contamination of ground waters as a result of filtration and leakage of drilling waste from slurry barns. Probably, it occurs due to the degradation of their natural waterproofing layer of permafrost rocks under the influence of global climate change.
Keywords
Nadym River,
ionic composition of river water,
technogenic metamorphization,
anthropogenic
impact,
global climate change
Supporting agencies: The study was financially supported by the grant received from the RFBR, no. 18-05-60165.
About the Authors
A. O. Danilenko
Hydrochemical Institute
Russian Federation
Rostov-on-Don
Russian Federation
Rostov-on-Don
L. S. Kosmenko
Hydrochemical Institute
Russian Federation
Rostov-on-Don
Russian Federation
Rostov-on-Don
O. S. Reshetnyak
Hydrochemical Institute,
Southern Federal University
Russian Federation
Rostov-on-Don
Russian Federation
Rostov-on-Don
M. Y. Kondakova
Hydrochemical Institute
Russian Federation
Rostov-on-Don
Russian Federation
Rostov-on-Don
References
1. Novikov D.A. Geochemistry of groundwater in oil and gas deposits of the Nadym-Tazovsky interfluve. Extended Abstract of Cand. Sci. (Geol.-Min.) Dissertation. Tomsk: Inst. of Petroleum Geology and Geophysics, SB RAS, 2002. 248 p.
2. Alekin A.O. Obshchaya gidrokhimiya (Khimiya prirodnykh vod) [Hydrochemistry (Chemistry of Natural Waters)]. Leningrad: Gidrometeorol. I–vo Publ., 1948. 208 p.
3. Gosudarstvennyi doklad “O sostoyanii i ispolzovanii mineral’no-syr’evykh resursov Rossiiskoi Federatsii v 2015 godu” [State Report on the Status and Using Mineral Resources of the Russian Federation in 2015]. Kiselev E.A., Ed. Moscow, 2016. 344 p.
4. Brekhuntsov A.M. Historical development of the West Siberian petroleum province and hydrocarbon resources replacement issues at the present stage. Neftegaz. Geol., 2010, no. 3, pp. 20–25. (In Russ.).
5. Opekunov A.Yu., Opekunova M.G., Kukushkin S.Yu., Ganul A.G. Environmental assessment in the oil and gas production areas of the Yamalo-Nenets Autonomous District. Vestn. S.-Peterb. Gos. Univ., Ser. 7: Geol., Geogr., 2012, no. 4, pp. 87–101. (In Russ.).
6. Gnusin N.P. Forecast of increase in sulphate ions runoff on the Soviet Union territory until 2000. In Gidrokhimicheskie materialy. Metody khimicheskogo analiza i protsessy samoochishcheniya prirodnykh vod [Hadrochemical Materials. Methods of Chemical Analysis and Processes of Natural Waters Self-Purification]. Leningrad: Gidrometeorol. I–vo Publ., 1970, vol. LIII, pp. 125–130. (In Russ.).
7. Resursy poverkhnostnykh vod SSSR. Аltai i Zapadnaya Sibir’. Nizhnii Irtysh i Nizhnyaya Ob’ [Surface Water Resources of the USSR. Altai and Western Siberia. Lower Irtysh and Lower Ob]. Leningrad: Gidrometeoisdat Publ., 1973, vol. 15, no. 3, 424 p.
8. GOST R ISO 16269-4–2017. Statistical Methods. Statistical Data Presentation. Part 4. Detection and Treatment of Outliers. Moscow: Standartinform Publ., 2017. 53 p.
9. Savichev O.G., Bernatonis P.V., Bernatonis V.K. Geochemical conditions of the drilling waste’s allocation and utilization in peat-bog geosystems of Siberia. Vestn. Tomsk. Gos. Univ., 2013, no. 375, pp. 183–186. (In Russ.).
10. Gusev E.M., Nasonova O.N., Dzhogan L.Ya., Ayzel G.V. Simulating the formation of river runoff and snow cover in the northern West Siberia. Water Resour., 2015, vol. 42, no. 4, pp. 460–467. doi 10.1134/S0097807815040065
11. Svanidze I.G. The impact of mineralized formation waters on the river valleys landscapes of the southern taiga in Western Siberia (using the example of the South of the Tyumen region). Cand. Sci. (Geogr.) Dissertation. Barnaul: Tyumen State Univ., 2015. 155 p.
12. Kropachev N.M., Rysev V.V., Korikov A.P., Kornev A.N., Mordvintsev M.V., Skachek K.G. Methods of lithological facies modeling of the J1 formation of the Vasyugan formation within the Surgut arch according to seismic survey and drilling data. Tekhnologii Seismorazvedki, 2004, no. 2, pp. 81–91. (In Russ.).
13. Schemes of Integrated Use and Protection of Water Bodies in the Nadym River Basin. Book 1: General Characteristics of the River Basin. 2014. 71 p.
14. Kukushkin S.Yu. Indicators of anthropogenic load on natural-territorial complexes during the development of oil and gas condensate fields of the north of Western Siberia. Cand. Sci. (Geogr.) Dissertation. St. Petersburg: St. Petersburg State Univ., 2016. 200 p.
15. Shtyrlyaeva A.A. The regional correlation and reconstruction of the formation’s condition of the Middle and Apper Jurassic reservoir rocks J1 and J2 by NadymPurskaya and Sredneobskaya oil and gas fields (West Siberian petroleum basin). Vestn. Voronezh. Gos. Univ., Ser. Geol., 2016, no. 2, pp. 40–46. (In Russ.).
16. Maksimova M.P. Effect of technogenesis on hydrosphere. Methods for evaluating chemical anthropogenic river runoff to the sea. Vestn. MGOU. Ser. Estestvennye Nauki, 2012, no. 2, pp. 89–96. (In Russ.).
17. Weiss N., Kaal J. Characterization of labile organic matter in Pleistocene permafrost (NE Siberia), using Thermally assisted Hydrolysis and Methylation (THMGC MS). Soil Biol. Biochem., 2018, vol. 117, pp. 203–213.
18. Moskovchenko D.V. Geochemistry of the West Siberi-an plain landscapes. Extended Abstract of Doct. Sci.(Geogr.) Dissertation. St. Petersburg: Inst. Probl. North-ern Dev., SB RAS, 2010. 394 p.
19. Woo M.-K. Permafrost Hydrology. Berlin: SpringerVerlag, 2012. 564 p.
20. Toropov G.V., Beshentsev V.A. Features of the chemical composition’s formation of natural water in the Urengoy oil and gas production area (the case of the Urengoy oil and gas condensate field). Vestn. Tyumenskogo Gos. Univ., Ser. Nauki o Zemle, 2013, no. 4, pp. 115–124. (In Russ.).
21. Zakharova E.A., Kouraev A.V., Biancamaria S., Kolmakova M.V., Mognard N.M., Zemtsov V.A., Kiprotin S.N., Decharme B. Snow cover and spring flood flow in the Northern part of Western Siberia (the Poluy, Nadym, Pur, and Taz Rivers). J. Hydrometeorol, 2011, vol. 12, pp. 1498–1511. doi 10.1175/JHM-D-11-017.1
22. Novikov D.A. Geochemistry of groundwater in oil and gas deposits of the Nadym-Tazovsky interfluve. Extended Abstract of Cand. Sci. (Geol.-Min.) Dissertation. Tomsk: Inst. of Petroleum Geology and Geophysics, SB RAS, 2002. 248 p.
23. Gosudarstvennyi doklad “O sostoyanii i ispolzovanii mineral’no-syr’evykh resursov Rossiiskoi Federatsii v 2015 godu” [State Report on the Status and Using Mineral Resources of the Russian Federation in 2015]. Kiselev E.A., Ed. Moscow, 2016. 344 p.
24. Opekunov A.Yu., Opekunova M.G., Kukushkin S.Yu., Ganul A.G. Environmental assessment in the oil and gas production areas of the Yamalo-Nenets Autonomous District. Vestn. S.-Peterb. Gos. Univ., Ser. 7: Geol., Geogr., 2012, no. 4, pp. 87–101. (In Russ.).
25. Resursy poverkhnostnykh vod SSSR. Аltai i Zapadnaya Sibir’. Nizhnii Irtysh i Nizhnyaya Ob’ [Surface Water Resources of the USSR. Altai and Western Siberia. Lower Irtysh and Lower Ob]. Leningrad: Gidrometeoisdat Publ., 1973, vol. 15, no. 3, 424 p.
26. Savichev O.G., Bernatonis P.V., Bernatonis V.K. Geochemical conditions of the drilling waste’s allocation and utilization in peat-bog geosystems of Siberia. Vestn. Tomsk. Gos. Univ., 2013, no. 375, pp. 183–186. (In Russ.).
27. Svanidze I.G. The impact of mineralized formation waters on the river valleys landscapes of the southern taiga in Western Siberia (using the example of the South of the Tyumen region). Cand. Sci. (Geogr.) Dissertation. Barnaul: Tyumen State Univ., 2015. 155 p.
28. Schemes of Integrated Use and Protection of Water Bodies in the Nadym River Basin. Book 1: General Characteristics of the River Basin. 2014. 71 p.
29. Shtyrlyaeva A.A. The regional correlation and reconstruction of the formation’s condition of the Middle and Apper Jurassic reservoir rocks J1 and J2 by NadymPurskaya and Sredneobskaya oil and gas fields (West Siberian petroleum basin). Vestn. Voronezh. Gos. Univ., Ser. Geol., 2016, no. 2, pp. 40–46. (In Russ.).
30. Weiss N., Kaal J. Characterization of labile organic matter in Pleistocene permafrost (NE Siberia), using Thermally assisted Hydrolysis and Methylation (THMGC MS). Soil Biol. Biochem., 2018, vol. 117, pp. 203–213.
31. Woo M.-K. Permafrost Hydrology. Berlin: SpringerVerlag, 2012. 564 p.
32. Zakharova E.A., Kouraev A.V., Biancamaria S., Kolmakova M.V., Mognard N.M., Zemtsov V.A., Kiprotin S.N., Decharme B. Snow cover and spring flood flow in the Northern part of Western Siberia (the Poluy, Nadym, Pur, and Taz Rivers). J. Hydrometeorol, 2011, vol. 12, pp. 1498–1511. doi 10.1175/JHM-D-11-017.1
Graphical Abstract
|
|
1. Average annual sulphate-ions concentration in Nadym River | |
| Subject | ||
| Type | Исследовательские инструменты | |
View
(63KB)
|
Indexing metadata ▾ | |
|
2. PDF | |
| Subject | ||
| Type | Исследовательские инструменты | |
Download
(3MB)
|
Indexing metadata ▾ | |
- The water mineralization of the Nadym River is increasing due to rising sulfates concentration.
- These hydrochemical regime alterations create risks of river water technogenic metamorphization. Since 2000, the class of chemical composition has gradually changed from bicarbonate to mixed sulfate-hydrocarbonate or hydrocarbonate-sulfate.
- The alternations are possibly caused by the influx of major ions, primarily sulfates from drill cuttings into seasonal meltwaters.
- This process is fostered by the degradation of permafrost under conditions of rising atmospheric temperatures, seasonal increase in soil and groundwater and surface water temperatures, and an increase in seasonal thaw depth.
Review
For citations:
Danilenko A.O., Kosmenko L.S., Reshetnyak O.S., Kondakova M.Y. Preconditions to Technogenic Metamorphization of Nadym River Water Ionic Composition in Conditions of Global Climate Change. Izvestiya Rossiiskoi Akademii Nauk. Seriya Geograficheskaya. 2020;(1):127-137. (In Russ.) https://doi.org/10.31857/S2587556620010069
Views:
488
Email this article 
