Hydrogeochemistry

@misc{babintseva1978hydrogeochemical1,
    author = "Babintseva, T. N. et al",
    title = "Hydrogeochemical conditions of the oil and gas reserves of the Tunguska basin",
    year = "1978",
    howpublished = "Geology of Oil and Gas, v. 3, p. 30-36",
    note = "talkorigins\_source = {true}; raw\_reference = {Babintseva, T. N. et al., 1978, Hydrogeochemical conditions of the oil and gas reserves of the Tunguska basin: Geology of Oil and Gas, v. 3, p. 30-36.}"
}

@incollection{blanc1994hydrogeochemistry,
    author = "Blanc, G. and Stille, P. and Vitali, F.",
    title = "Hydrogeochemistry in the Lau Backarc Basin",
    year = "1994",
    booktitle = "Proceedings of the Ocean Drilling Program",
    url = "https://doi.org/10.2973/odp.proc.sr.135.123.1994",
    doi = "10.2973/odp.proc.sr.135.123.1994",
    openalex = "W2185135865",
    references = "doi10100797814684275788, doi1010160012821x76901515, doi1010160012821x9190189o, doi1010160016703781900041, doi101029eo067i021p00489, doi101029jb082i023p03391, doi101038338496a0, doi1011300091761319910190303haitlb23co2, doi104319lo19792420356, openalexw2995351396"
}

@article{asnachinda1997hydrogeochemistry,
    author = "Asnachinda, Pongpor",
    title = "Hydrogeochemistry of the Chiang Mai Basin, northernThailand",
    year = "1997",
    journal = "Journal of Asian Earth Sciences",
    url = "https://doi.org/10.1016/s0743-9547(97)00017-2",
    doi = "10.1016/s0743-9547(97)00017-2",
    number = "2-3",
    openalex = "W2050448573",
    pages = "317-326",
    volume = "15",
    references = "doi101007978364241714670760, doi1010160022169483902500, doi101016002216949190158e, doi101111j174565841972tb02912x, doi101130dnaggnao281, doi103133wsp2323, doi107186bgsm09197712, openalexw2788326797, openalexw3025350344, openalexw634325841"
}

Hydrogeochemical status of the Purna alluvial basin, Maharashtra has been interpreted on the basis of 158 groundwater samples collected from dug wells (60) i.e., shallow aquifer and bore wells (98) i.e., deep aquifer each during pre- and post-monsoon periods of the year 2009. The samples were analyzed for their physicochemical parameters i.e., pH, EC, TDS, Ca, Mg, Na, K, TH, Al, Cl, SO4, NO3 and HCO3. The mean values of cation concentration show a trend of Na>Ca>Mg>K, while anions are in order of HCO3>Cl>SO4>NO3 from both deep and shallow aquifers. The plot of chemical data on Piper’s trilinear diagram reveals that majority of the groundwater samples fall in the fields of alkalis exceeding alkaline earths, weak acids exceeding strong acids, carbonate hardness exceeding 50%, and no cation and anion pairs exceeding 50%. The cationic and anionic triangular fields of the diagram show that sodium-potassium type (Na+K) of water is dominant in the cationic, and bicarbonate type (HCO3) in the anionic category. The analytical data also reveal the existence of six groundwater facies in the area, i.e., (i) Ca-Mg-HCO3, (ii) Na-Cl, (iii) Na-HCO3, (iv) Ca-Cl, (v) Na-Ca-HCO3 (mixed type) and, (vi) Ca–Mg-Cl (mixed type). Ca-Mg-HCO3 facies is predominant in the northern, northeastern, eastern, southeastern and northwestern peripheries of the alluvial basin. Na-Cl and Na-HCO3, facies are confined to certain parts of the eastern and central regions, as well as in a few small patches along the Purna river channel. These areas are represented by moderate to high salinity. Na-Cl-SO4 facies is limited to a small patch situated in the central part of the basin representing excess concentrations of sodium and chloride. Water of Na-Ca-HCO3 (mixed type) is the most dominant covering most of the area on both sides of the Purna main channel in the eastern, central and western regions. Two small patches having Ca-Mg-Cl type of water has also been identified in the basin area.

@article{srivastava2015hydrogeochemistry,
    author = "Srivastava, Ashok K. and Parimal, Pravin S.",
    title = "Hydrogeochemistry of Purna Alluvial Basin, Central India",
    year = "2015",
    journal = "Journal of the Geological Society of India",
    abstract = "Hydrogeochemical status of the Purna alluvial basin, Maharashtra has been interpreted on the basis of 158 groundwater samples collected from dug wells (60) i.e., shallow aquifer and bore wells (98) i.e., deep aquifer each during pre- and post-monsoon periods of the year 2009. The samples were analyzed for their physicochemical parameters i.e., pH, EC, TDS, Ca, Mg, Na, K, TH, Al, Cl, SO4, NO3 and HCO3. The mean values of cation concentration show a trend of Na\>Ca\>Mg\>K, while anions are in order of HCO3\>Cl\>SO4\>NO3 from both deep and shallow aquifers. The plot of chemical data on Piper’s trilinear diagram reveals that majority of the groundwater samples fall in the fields of alkalis exceeding alkaline earths, weak acids exceeding strong acids, carbonate hardness exceeding 50\%, and no cation and anion pairs exceeding 50\%. The cationic and anionic triangular fields of the diagram show that sodium-potassium type (Na+K) of water is dominant in the cationic, and bicarbonate type (HCO3) in the anionic category. The analytical data also reveal the existence of six groundwater facies in the area, i.e., (i) Ca-Mg-HCO3, (ii) Na-Cl, (iii) Na-HCO3, (iv) Ca-Cl, (v) Na-Ca-HCO3 (mixed type) and, (vi) Ca–Mg-Cl (mixed type). Ca-Mg-HCO3 facies is predominant in the northern, northeastern, eastern, southeastern and northwestern peripheries of the alluvial basin. Na-Cl and Na-HCO3, facies are confined to certain parts of the eastern and central regions, as well as in a few small patches along the Purna river channel. These areas are represented by moderate to high salinity. Na-Cl-SO4 facies is limited to a small patch situated in the central part of the basin representing excess concentrations of sodium and chloride. Water of Na-Ca-HCO3 (mixed type) is the most dominant covering most of the area on both sides of the Purna main channel in the eastern, central and western regions. Two small patches having Ca-Mg-Cl type of water has also been identified in the basin area.",
    url = "https://doi.org/10.1007/s12594-015-0264-x",
    doi = "10.1007/s12594-015-0264-x",
    number = "6",
    openalex = "W601681475",
    pages = "673-685",
    volume = "85",
    references = "doi101007s100400050176, doi101007s100400070220y, doi101007s1266500900598, doi101007s126650100472z, doi101016jjksus200910005, doi101016s0883292700000780, doi101029tr025i006p00914, doi1012019780429265693, doi101306eg0820303011, doi105897jgrp9000066"
}

@inproceedings{andsuydam2016mapping,
    author = "Suydam, Seth and Marsac, Kara and Navarre-Sitchler, Alexis K.",
    title = "MAPPING HYDROGEOCHEMISTRY OF THE DENVER-JULESBURG BASIN",
    year = "2016",
    booktitle = "Geological Society of America Abstracts with Programs",
    url = "https://doi.org/10.1130/abs/2016am-283158",
    doi = "10.1130/abs/2016am-283158",
    openalex = "W2532732504"
}

Hydrogeochemical conditions of the West and East Messoyakhsk fields are discussed in the article. These conditions of the complex hydrogeological Mesozoic basin are important in the formation and preservation of oil and gas deposits. The geological structure is characterized by the presence of a large number of disjunctive dislocations. The fields belong to the Elysion geodynamic water drive system - the Omsk-Gydansk structural zone. This determined the conditions and intensity of oil and gas generation.

@article{doi103166004450108201722835,
    author = "Salnikova, Yu. I. and Абдрашитова, Р. Н. and Бешенцев, В. А.",
    title = "HYDROGEOCHEMICAL CONDITIONSOF WESTERN AND EASTERN MESSOYAKHSK DEPOSITS",
    year = "2017",
    journal = "Oil and Gas Studies",
    abstract = "Hydrogeochemical conditions of the West and East Messoyakhsk fields are discussed in the article. These conditions of the complex hydrogeological Mesozoic basin are important in the formation and preservation of oil and gas deposits. The geological structure is characterized by the presence of a large number of disjunctive dislocations. The fields belong to the Elysion geodynamic water drive system - the Omsk-Gydansk structural zone. This determined the conditions and intensity of oil and gas generation.",
    url = "https://doi.org/10.31660/0445-0108-2017-2-28-35",
    doi = "10.31660/0445-0108-2017-2-28-35",
    openalex = "W2901446380"
}

@inproceedings{bachurin2018hydrogeochemistry,
    author = "Bachurin, B. A. and Fetisova, N. F.",
    title = "HYDROGEOCHEMISTRY OF TEHNOGENESIS OF THE KIZEL COAL BASIN",
    year = "2018",
    booktitle = "The Geological Evolution of the Water-Rock Interaction",
    url = "https://doi.org/10.31554/978-5-7925-0536-0-2018-332-335",
    doi = "10.31554/978-5-7925-0536-0-2018-332-335",
    openalex = "W2906119184",
    pages = "332-335"
}

The object of our research is hydrogeochemical conditions of the Mesozoic hydrogeological basin within Yamalo-Nenets oil and gas bearing region. The Mesozoic basin includes the Aptian-Albian-Cenomanian, Neocomian and Jurassic hydrogeological complexes. These complexes contain thermal and mineralized water. The water exchange in the basin in question is significantly hampered; this is reflected in hydrogeochemical conditions. The article presents the distribution maps of water types in three complexes of the Mesozoic basin, maps of changes in the magnitude of mineralization and the content of the most valuable microcomponents (iodine and bromine). It has been established that with the depth (from the Aptian-Albian-Cenomanian to the Jurassic complex) the area of distribution of sodium bicarbonate-type water increases. Further directions of groundwater research in the region are noted.

@article{doi103166004450108201951022,
    author = "Бешенцев, В. А. and Salnikova, Yu. I. and Абдрашитова, Р. Н. and Vorobjeva, S. V.",
    title = "Hydrogeochemical conditions of oil and gas areas in Yamalo-Nenets oil and gas producing region (Part 1)",
    year = "2019",
    journal = "Oil and Gas Studies",
    abstract = "The object of our research is hydrogeochemical conditions of the Mesozoic hydrogeological basin within Yamalo-Nenets oil and gas bearing region. The Mesozoic basin includes the Aptian-Albian-Cenomanian, Neocomian and Jurassic hydrogeological complexes. These complexes contain thermal and mineralized water. The water exchange in the basin in question is significantly hampered; this is reflected in hydrogeochemical conditions. The article presents the distribution maps of water types in three complexes of the Mesozoic basin, maps of changes in the magnitude of mineralization and the content of the most valuable microcomponents (iodine and bromine). It has been established that with the depth (from the Aptian-Albian-Cenomanian to the Jurassic complex) the area of distribution of sodium bicarbonate-type water increases. Further directions of groundwater research in the region are noted.",
    url = "https://doi.org/10.31660/0445-0108-2019-5-10-22",
    doi = "10.31660/0445-0108-2019-5-10-22",
    openalex = "W2984668689"
}

The object of our research is hydrogeochemical conditions of the Mesozoic hydrogeological basin within Yamalo-Nenets oil and gas bearing region. The Mesozoic basin includes the Aptian-Albian-Cenomanian, Neocomian and Jurassic hydrogeological complexes. These complexes contain thermal and mineralized water. The water exchange in the basin in question is significantly hampered; this is reflected in hydrogeochemical conditions. The article presents the distribution maps of water types in three complexes of the Mesozoic basin, maps of changes in the magnitude of mineralization and the content of the most valuable microcomponents (iodine and bromine). It has been established that with the depth (from the Aptian-Albian-Cenomanian to the Jurassic complex) the area of distribution of sodium bicarbonate-type water increases. Further directions of groundwater research in the region are noted.

@article{doi103166004450108201961930,
    author = "Бешенцев, В. А. and Salnikova, Yu. I. and Абдрашитова, Р. Н. and Vorobjeva, S. V.",
    title = "Hydrogeochemical conditions of oil and gas areas in Yamalo-Nenets oil and gas producing region (Part 2)",
    year = "2020",
    journal = "Oil and Gas Studies",
    abstract = "The object of our research is hydrogeochemical conditions of the Mesozoic hydrogeological basin within Yamalo-Nenets oil and gas bearing region. The Mesozoic basin includes the Aptian-Albian-Cenomanian, Neocomian and Jurassic hydrogeological complexes. These complexes contain thermal and mineralized water. The water exchange in the basin in question is significantly hampered; this is reflected in hydrogeochemical conditions. The article presents the distribution maps of water types in three complexes of the Mesozoic basin, maps of changes in the magnitude of mineralization and the content of the most valuable microcomponents (iodine and bromine). It has been established that with the depth (from the Aptian-Albian-Cenomanian to the Jurassic complex) the area of distribution of sodium bicarbonate-type water increases. Further directions of groundwater research in the region are noted.",
    url = "https://doi.org/10.31660/0445-0108-2019-6-19-30",
    doi = "10.31660/0445-0108-2019-6-19-30",
    openalex = "W3011279221",
    references = "doi101016s030917089600036x, doi101017cbo9780511576546, doi101306819a41f816c511d78645000102c1865d, doi103166004450108201722835, doi103166004450108201951022"
}

The article is devoted to the hydrogeochemical conditions of the Mesozoic hydrogeological basin within the Russkoye oil and gas field. The text gives valuable information on the natural conditions, geological structure, geotemperature regime of the bowels of the Earth and the composition of groundwater of the Aptian-Albian-Cenomanian, Neocomian, and Jurassic hydrogeological complexes. The change in the composition of groundwater in the section of the AptianAlbian-Cenomanian complex has been revealed. Vertical inversion zoning that traces the underlying the Neocomian complex is established. We describe the main features of the regional distribution of reservoir pressures. Hydrodynamic schemes of the Aptian-Albian-Cenomanian, Neocomian, and Jurassic hydrogeological complexes are given in the article. These schemes show that the Russkoye gas and oil field is located in the zone of low reservoir pressures. The above vertical inversion zoning and low reservoir pressures are associated with the location of the field within the elisional hydrodynamic water pressure system of the Yamal-Gydan lineaments. The data of the block-fault model of the considered field were used in the course of the study. The block-fault structure predetermined the migration of hydrocarbons and the formation of tectonically screened deposits.

@article{doi103166004450108202052035,
    author = "Бешенцев, В. А. and Salnikova, Yu. I. and Vorobjeva, S. V.",
    title = "Hydrogeological conditions of the Mesozoic hydrogeological basin within the Russkoye gas and oil field",
    year = "2020",
    journal = "Oil and Gas Studies",
    abstract = "The article is devoted to the hydrogeochemical conditions of the Mesozoic hydrogeological basin within the Russkoye oil and gas field. The text gives valuable information on the natural conditions, geological structure, geotemperature regime of the bowels of the Earth and the composition of groundwater of the Aptian-Albian-Cenomanian, Neocomian, and Jurassic hydrogeological complexes. The change in the composition of groundwater in the section of the AptianAlbian-Cenomanian complex has been revealed. Vertical inversion zoning that traces the underlying the Neocomian complex is established. We describe the main features of the regional distribution of reservoir pressures. Hydrodynamic schemes of the Aptian-Albian-Cenomanian, Neocomian, and Jurassic hydrogeological complexes are given in the article. These schemes show that the Russkoye gas and oil field is located in the zone of low reservoir pressures. The above vertical inversion zoning and low reservoir pressures are associated with the location of the field within the elisional hydrodynamic water pressure system of the Yamal-Gydan lineaments. The data of the block-fault model of the considered field were used in the course of the study. The block-fault structure predetermined the migration of hydrocarbons and the formation of tectonically screened deposits.",
    url = "https://doi.org/10.31660/0445-0108-2020-5-20-35",
    doi = "10.31660/0445-0108-2020-5-20-35",
    openalex = "W3100377197",
    references = "doi103166004450108201542024, doi103166004450108201951022, doi103166004450108201961930"
}

@article{kulakov2020hydrogeochemical,
    author = "Kulakov, Valerii V. and Berdnikov, Nikolay V.",
    title = "Hydrogeochemical processes in the Tunguska reservoir during in situ treatment of drinking water supplies",
    year = "2020",
    journal = "Applied Geochemistry",
    url = "https://doi.org/10.1016/j.apgeochem.2020.104683",
    doi = "10.1016/j.apgeochem.2020.104683",
    openalex = "W3041269275",
    pages = "104683",
    volume = "120",
    references = "doi101016japgeochem201011008, doi101016jscitotenv201809319, doi101016jwatres201110015, doi101016jwatres201610040, doi101111j174565841976tb03638x, doi101134s0016702919120097, doi101134s0097807814020122, doi101134s1819714019020064, doi102166wst19880093, doi102166wst2010463"
}

@article{burenina2022spatiotemporal,
    author = "BURENINA, T. A. and DANILOVA, I. V. and MIKHEYEVA, N. A.",
    title = "Spatio-temporal dynamics evapotranspirationin the Podkamennaya Tunguska river basin",
    year = "2022",
    journal = "Сибирский экологический журнал",
    url = "https://doi.org/10.15372/sej20220502",
    doi = "10.15372/sej20220502",
    number = "5",
    openalex = "W4312725790",
    pages = "507-519",
    volume = "29"
}

Studies of the hydrogeochemical features of groundwater in deep horizons of the West Siberian megabasin are important. They are closely related to applied and fundamental issues of oil and gas hydrogeology and allow studying the processes of formation, accumulation and migration of hydrocarbons. The article deals with our analysis of the hydrogeochemical conditions of the Mesozoic hydrogeological basin within the Ravninnoe oil field. The ion-salt composition of groundwater in deep horizons in the territory is variable. Basically groundwater are of the calcium chloride type (according to V. A. Sulin's classification), but magnesium chloride and sodium bicarbonate types of water are locally distributed. The hydrogeological conditions of the field are manifested in the change in the chemical composition of groundwater and in the vertical hydrochemical zonality. The article describes the features of the regional distribution of reservoir temperatures and reservoir pressures of the Aptian-Albian-Cenomanian, Neocomian and Jurassic hydrogeological complexes. The study of the formation factors of the hydrogeochemical field of these deposits was carried out taking into account paleotectonic, paleogeomorphological and paleohydrogeological reconstructions of the conditions that influenced the accumulation of fluids. Faults are widespread in the deposits of the pre-Jurassic complex, as well as angular unconformities between rocks of different ages, which predetermined the migration of hydrocarbons and the formation of their deposits.

@article{salnikova2022hydrogeochemical,
    author = "Salnikova, Yu. I. and Beshentsev, V. A.",
    title = "Hydrogeochemical conditions of the Mesozoic hydrogeological basin within the Ravninnoe oil field",
    year = "2022",
    journal = "Oil and Gas Studies",
    abstract = "Studies of the hydrogeochemical features of groundwater in deep horizons of the West Siberian megabasin are important. They are closely related to applied and fundamental issues of oil and gas hydrogeology and allow studying the processes of formation, accumulation and migration of hydrocarbons. The article deals with our analysis of the hydrogeochemical conditions of the Mesozoic hydrogeological basin within the Ravninnoe oil field. The ion-salt composition of groundwater in deep horizons in the territory is variable. Basically groundwater are of the calcium chloride type (according to V. A. Sulin's classification), but magnesium chloride and sodium bicarbonate types of water are locally distributed. The hydrogeological conditions of the field are manifested in the change in the chemical composition of groundwater and in the vertical hydrochemical zonality. The article describes the features of the regional distribution of reservoir temperatures and reservoir pressures of the Aptian-Albian-Cenomanian, Neocomian and Jurassic hydrogeological complexes. The study of the formation factors of the hydrogeochemical field of these deposits was carried out taking into account paleotectonic, paleogeomorphological and paleohydrogeological reconstructions of the conditions that influenced the accumulation of fluids. Faults are widespread in the deposits of the pre-Jurassic complex, as well as angular unconformities between rocks of different ages, which predetermined the migration of hydrocarbons and the formation of their deposits.",
    url = "https://doi.org/10.31660/0445-0108-2022-3-38-56",
    doi = "10.31660/0445-0108-2022-3-38-56",
    number = "3",
    openalex = "W4283593174",
    pages = "38-56",
    references = "doi103166004450108201542024, doi103166004450108201951022, doi103166004450108201961930"
}

@article{zhang2022hydrogeochemistry,
    author = "Zhang, Xiao and Zhao, Rong and Wu, Xiong and Mu, Wenping",
    title = "Hydrogeochemistry, identification of hydrogeochemical evolution mechanisms, and assessment of groundwater quality in the southwestern Ordos Basin, China",
    year = "2022",
    journal = "Environmental Science and Pollution Research",
    url = "https://doi.org/10.1007/s11356-021-15643-2",
    doi = "10.1007/s11356-021-15643-2",
    number = "1",
    openalex = "W3188712699",
    pages = "901-921",
    volume = "29",
    references = "doi101002j153873051948tb01338x, doi101007s100400050102, doi101007s1066100913021, doi101016jjhydrol200802015, doi101016s0009254199000315, doi101029tr025i006p00914, doi10108001621459196310500845, doi101126science1172974, doi101126science17039621088, openalexw3148284522"
}

The impact of forest cover disturbance on evapotranspiration changes within a river basin is highlighted. The dynamics of forest cover disturbance as a result of forest fires in the Nizhnyaya Tunguska River basin for 2001–2020 has been analyzed based on Landsat satellite imagery. It is found that, regarding the spatial aspect, evapotranspiration in the Nizhnyaya Tunguska River basin is differentiated between the test catchments, which differ in climatic conditions and vegetation cover. Concerning the temporal aspect, a decrease in the weighted average evapotranspiration is noted as the burned areas accumulated. It is revealed that the difference in the evapotranspiration decrease in undisturbed and disturbed areas depends both on the overall disturbance of the forest cover in the catchment area and on the area of current year burns, with the effect of fresh burned areas showing if their area is more than 3% of the catchment area.

@article{doi101134s1995425525700659,
    author = "Burenina, T. A. and Korets, M. A.",
    title = "Evapotranspiration in Northern Taiga Forests of the Nizhnyaya Tunguska River Basin Factoring in Their Postfire Dynamics",
    year = "2025",
    journal = "Contemporary Problems of Ecology",
    abstract = "The impact of forest cover disturbance on evapotranspiration changes within a river basin is highlighted. The dynamics of forest cover disturbance as a result of forest fires in the Nizhnyaya Tunguska River basin for 2001–2020 has been analyzed based on Landsat satellite imagery. It is found that, regarding the spatial aspect, evapotranspiration in the Nizhnyaya Tunguska River basin is differentiated between the test catchments, which differ in climatic conditions and vegetation cover. Concerning the temporal aspect, a decrease in the weighted average evapotranspiration is noted as the burned areas accumulated. It is revealed that the difference in the evapotranspiration decrease in undisturbed and disturbed areas depends both on the overall disturbance of the forest cover in the catchment area and on the area of current year burns, with the effect of fresh burned areas showing if their area is more than 3\% of the catchment area.",
    url = "https://doi.org/10.1134/s1995425525700659",
    doi = "10.1134/s1995425525700659",
    openalex = "W7124136115",
    references = "burenina2022spatiotemporal"
}