Geochemistry of ground water the Yurubcheno-Tokhomo hydrocarbon accumulation zone

Результат исследований: Материалы для журнала

Выдержка

In this study the chemical analysis of groundwater in Yurubcheno-Tokhomo hydrocarbon accumulation zone (YTHAZ) was carried out. The analysis revealed that fresh, brackish, saline waters and brines of various chemical types occur in the study area. Water salinity increases with the depth, but this dependency is not observed in Vendian and Riphean oil and gas deposits. The most mineralized brines occur in the salt-bearing hydrogeological formation. On the basis of the data on the geochemistry of groundwater, the possibilities of their further practical application were determined.

Язык оригиналаАнглийский
Номер статьи07033
ЖурналE3S Web of Conferences
Том98
DOI
СостояниеОпубликовано - 7 июн 2019
Событие16th International Symposium on Water-Rock Interaction, WRI 2019 and 13th International Symposium on Applied Isotope Geochemistry, 1st IAGC International Conference - Tomsk, Российская Федерация
Продолжительность: 21 июл 201926 июл 2019

Отпечаток

Brines
Geochemistry
Groundwater
Bearings (structural)
geochemistry
Hydrocarbons
hydrocarbon
Riphean
Vendian
groundwater
Saline water
chemical analysis
Deposits
Salts
salt
oil
Chemical analysis
Gases
gas
Water

ASJC Scopus subject areas

  • Environmental Science(all)
  • Energy(all)
  • Earth and Planetary Sciences(all)

Цитировать

Geochemistry of ground water the Yurubcheno-Tokhomo hydrocarbon accumulation zone. / Trifonov, Nikolay.

В: E3S Web of Conferences, Том 98, 07033, 07.06.2019.

Результат исследований: Материалы для журнала

@article{2d35ec01647d489195d98843e85c6a78,
title = "Geochemistry of ground water the Yurubcheno-Tokhomo hydrocarbon accumulation zone",
abstract = "In this study the chemical analysis of groundwater in Yurubcheno-Tokhomo hydrocarbon accumulation zone (YTHAZ) was carried out. The analysis revealed that fresh, brackish, saline waters and brines of various chemical types occur in the study area. Water salinity increases with the depth, but this dependency is not observed in Vendian and Riphean oil and gas deposits. The most mineralized brines occur in the salt-bearing hydrogeological formation. On the basis of the data on the geochemistry of groundwater, the possibilities of their further practical application were determined.",
author = "Nikolay Trifonov",
year = "2019",
month = "6",
day = "7",
doi = "10.1051/e3sconf/20199807033",
language = "English",
volume = "98",
journal = "E3S Web of Conferences",
issn = "2555-0403",
publisher = "EDP Sciences",

}

TY - JOUR

T1 - Geochemistry of ground water the Yurubcheno-Tokhomo hydrocarbon accumulation zone

AU - Trifonov, Nikolay

PY - 2019/6/7

Y1 - 2019/6/7

N2 - In this study the chemical analysis of groundwater in Yurubcheno-Tokhomo hydrocarbon accumulation zone (YTHAZ) was carried out. The analysis revealed that fresh, brackish, saline waters and brines of various chemical types occur in the study area. Water salinity increases with the depth, but this dependency is not observed in Vendian and Riphean oil and gas deposits. The most mineralized brines occur in the salt-bearing hydrogeological formation. On the basis of the data on the geochemistry of groundwater, the possibilities of their further practical application were determined.

AB - In this study the chemical analysis of groundwater in Yurubcheno-Tokhomo hydrocarbon accumulation zone (YTHAZ) was carried out. The analysis revealed that fresh, brackish, saline waters and brines of various chemical types occur in the study area. Water salinity increases with the depth, but this dependency is not observed in Vendian and Riphean oil and gas deposits. The most mineralized brines occur in the salt-bearing hydrogeological formation. On the basis of the data on the geochemistry of groundwater, the possibilities of their further practical application were determined.

UR - http://www.scopus.com/inward/record.url?scp=85067316443&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=85067316443&partnerID=8YFLogxK

U2 - 10.1051/e3sconf/20199807033

DO - 10.1051/e3sconf/20199807033

M3 - Conference article

AN - SCOPUS:85067316443

VL - 98

JO - E3S Web of Conferences

JF - E3S Web of Conferences

SN - 2555-0403

M1 - 07033

ER -