Standard

Выявление фильтрационных неоднородностей в водоносном горизонте при проведении опытных откачек и измерении естественного электрического поля : численный анализ. / Михайленко, А. А.; Коносавский, П. К.; Титов, К. В.

Engineering and Mining Geophysics 2020. European Association of Geoscientists and Engineers, 2020. стр. 1-7 (Engineering and Mining Geophysics 2020).

Результаты исследований: Публикации в книгах, отчётах, сборниках, трудах конференцийстатья в сборнике материалов конференциинаучнаяРецензирование

Harvard

Михайленко, АА, Коносавский, ПК & Титов, КВ 2020, Выявление фильтрационных неоднородностей в водоносном горизонте при проведении опытных откачек и измерении естественного электрического поля: численный анализ. в Engineering and Mining Geophysics 2020. Engineering and Mining Geophysics 2020, European Association of Geoscientists and Engineers, стр. 1-7, Engineering and Mining Geophysics 2020, Perm, Российская Федерация, 14/09/20. https://doi.org/10.3997/2214-4609.202051171

APA

Vancouver

Author

Михайленко, А. А. ; Коносавский, П. К. ; Титов, К. В. / Выявление фильтрационных неоднородностей в водоносном горизонте при проведении опытных откачек и измерении естественного электрического поля : численный анализ. Engineering and Mining Geophysics 2020. European Association of Geoscientists and Engineers, 2020. стр. 1-7 (Engineering and Mining Geophysics 2020).

BibTeX

@inproceedings{d8ee4ed1ce594f2c9de201641ab01776,
title = "Выявление фильтрационных неоднородностей в водоносном горизонте при проведении опытных откачек и измерении естественного электрического поля: численный анализ",
abstract = "In this paper, we present Self-Potential (SP) signals associated with pumping tests of heterogeneous aquifers. A technique of 3D SP modelling is based on the use of MODFLOW package. We study numerically six models of aquifers: models 1a and 2b when the aquifer consists of two parts of different hydraulic conductivity; models 2a and 2b contained a planar layer with distinct hydraulic conductivity; and models 3a and 3b included a cylindrical inhomogeneity. For model 1 we detected maximum well-boundary distance at 300 m where the boundary is marked. For model 2 starting from about 100 m distance between the well and the outer boundary this boundary is not marked in both the drawdown and SP distributions. For model 3 two boundaries are marked. We obtained a close correlation between drawdowns and SP signals for models 1a, 2a and model 3. We consider these results can serve as a base for tomography of aquifers based on SP data.",
author = "Михайленко, {А. А.} and Коносавский, {П. К.} and Титов, {К. В.}",
note = "Publisher Copyright: {\textcopyright} Engineering and Mining Geophysics 2020. Copyright: Copyright 2021 Elsevier B.V., All rights reserved.; Engineering and Mining Geophysics 2020 ; Conference date: 14-09-2020 Through 18-09-2020",
year = "2020",
month = sep,
day = "14",
doi = "10.3997/2214-4609.202051171",
language = "русский",
series = "Engineering and Mining Geophysics 2020",
publisher = "European Association of Geoscientists and Engineers",
pages = "1--7",
booktitle = "Engineering and Mining Geophysics 2020",
address = "Нидерланды",

}

RIS

TY - GEN

T1 - Выявление фильтрационных неоднородностей в водоносном горизонте при проведении опытных откачек и измерении естественного электрического поля

T2 - Engineering and Mining Geophysics 2020

AU - Михайленко, А. А.

AU - Коносавский, П. К.

AU - Титов, К. В.

N1 - Publisher Copyright: © Engineering and Mining Geophysics 2020. Copyright: Copyright 2021 Elsevier B.V., All rights reserved.

PY - 2020/9/14

Y1 - 2020/9/14

N2 - In this paper, we present Self-Potential (SP) signals associated with pumping tests of heterogeneous aquifers. A technique of 3D SP modelling is based on the use of MODFLOW package. We study numerically six models of aquifers: models 1a and 2b when the aquifer consists of two parts of different hydraulic conductivity; models 2a and 2b contained a planar layer with distinct hydraulic conductivity; and models 3a and 3b included a cylindrical inhomogeneity. For model 1 we detected maximum well-boundary distance at 300 m where the boundary is marked. For model 2 starting from about 100 m distance between the well and the outer boundary this boundary is not marked in both the drawdown and SP distributions. For model 3 two boundaries are marked. We obtained a close correlation between drawdowns and SP signals for models 1a, 2a and model 3. We consider these results can serve as a base for tomography of aquifers based on SP data.

AB - In this paper, we present Self-Potential (SP) signals associated with pumping tests of heterogeneous aquifers. A technique of 3D SP modelling is based on the use of MODFLOW package. We study numerically six models of aquifers: models 1a and 2b when the aquifer consists of two parts of different hydraulic conductivity; models 2a and 2b contained a planar layer with distinct hydraulic conductivity; and models 3a and 3b included a cylindrical inhomogeneity. For model 1 we detected maximum well-boundary distance at 300 m where the boundary is marked. For model 2 starting from about 100 m distance between the well and the outer boundary this boundary is not marked in both the drawdown and SP distributions. For model 3 two boundaries are marked. We obtained a close correlation between drawdowns and SP signals for models 1a, 2a and model 3. We consider these results can serve as a base for tomography of aquifers based on SP data.

UR - http://www.scopus.com/inward/record.url?scp=85099718255&partnerID=8YFLogxK

U2 - 10.3997/2214-4609.202051171

DO - 10.3997/2214-4609.202051171

M3 - статья в сборнике материалов конференции

AN - SCOPUS:85099718255

T3 - Engineering and Mining Geophysics 2020

SP - 1

EP - 7

BT - Engineering and Mining Geophysics 2020

PB - European Association of Geoscientists and Engineers

Y2 - 14 September 2020 through 18 September 2020

ER -

ID: 74982390