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Hydrogeological investigation for assessment of the sustainability of low-arsenic aquifers as a safe drinking water source in regions with high-arsenic groundwater in Matlab, southeastern Bangladesh

Identifieur interne : 000053 ( PascalFrancis/Corpus ); précédent : 000052; suivant : 000054

Hydrogeological investigation for assessment of the sustainability of low-arsenic aquifers as a safe drinking water source in regions with high-arsenic groundwater in Matlab, southeastern Bangladesh

Auteurs : Mattias Von Brömssen ; Lars Markussen ; Prosun Bhattacharya ; KAZI MATIN AHMED ; Mohammed Hossain ; Gunnar Jacks ; Ondra Sracek ; Roger Thunvik ; M. Aziz Hasan ; M. Mainul Islam ; M. Mokhlesur Rahman

Source :

RBID : Pascal:15-0030907

Descripteurs français

English descriptors

Abstract

Exploitation of groundwater from shallow, high prolific Holocene sedimentary aquifers has been a main element for achieving safe drinking water and food security in Bangladesh. However, the presence of elevated levels of geogenic arsenic (As) in these aquifers has undermined this success. Except for targeting safe aquifers through installations of tubewells to greater depth, no mitigation option has been successfully implemented on a larger scale. The objective of this study has been to characterise the hydrostratigraphy, groundwater flow patterns, the hydraulic properties to assess the vulnerability of low-arsenic aquifers at Matlab, in south-eastern Bangladesh, one of the worst arsenic-affected areas of the country. Groundwater modelling, conventional pumping test using multilevel piezometers, hydraulic head monitoring in piezometer nests, 14C dating of groundwater and assessment of groundwater abstraction were used. A model comprising of three aquifers covering the top 250 m of the model domain showed the best fit for the calibration evaluation criteria.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

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A02 01      @0 JHYDA7
A03   1    @0 J. hydrol. : (Amst.)
A05       @2 518
A06       @3 p. c
A08 01  1  ENG  @1 Hydrogeological investigation for assessment of the sustainability of low-arsenic aquifers as a safe drinking water source in regions with high-arsenic groundwater in Matlab, southeastern Bangladesh
A09 01  1  ENG  @1 Arsenic in hydrological processes-Sources, speciation, bioavailability and management
A11 01  1    @1 VON BRÖMSSEN (Mattias)
A11 02  1    @1 MARKUSSEN (Lars)
A11 03  1    @1 BHATTACHARYA (Prosun)
A11 04  1    @1 KAZI MATIN AHMED
A11 05  1    @1 HOSSAIN (Mohammed)
A11 06  1    @1 JACKS (Gunnar)
A11 07  1    @1 SRACEK (Ondra)
A11 08  1    @1 THUNVIK (Roger)
A11 09  1    @1 AZIZ HASAN (M.)
A11 10  1    @1 MAINUL ISLAM (M.)
A11 11  1    @1 MOKHLESUR RAHMAN (M.)
A12 01  1    @1 BHATTACHARYA (Prosun) @9 ed.
A12 02  1    @1 NAIDU (Ravi) @9 ed.
A12 03  1    @1 POLYA (David A.) @9 ed.
A12 04  1    @1 MUKHERJEE (Abhijit) @9 ed.
A12 05  1    @1 BUNDSCHUH (Jochen) @9 ed.
A12 06  1    @1 CHARLET (Laurent) @9 ed.
A14 01      @1 KTH-International Groundwater Arsenic Research Group, Department of Sustainable Development, Environmental Science and Engineering, KTH Royal Institute of Technology Teknikringn 76 @2 100 44 Stockholm @3 SWE @Z 1 aut. @Z 3 aut. @Z 5 aut. @Z 6 aut. @Z 8 aut. @Z 9 aut.
A14 02      @1 Department of Soil and Water Environment, Ramböll Sweden AB, Box 4205 @2 102 65 Stockholm @3 SWE @Z 1 aut. @Z 2 aut.
A14 03      @1 Department of Geology, University of Dhaka, Curzon Hall Campus @2 Dhaka 1000 @3 BGD @Z 4 aut. @Z 9 aut. @Z 11 aut.
A14 04      @1 NGO Forum for Drinking Water Supply and Sanitation, Block-E @2 Lalmatia, Dhaka @3 BGD @Z 5 aut. @Z 10 aut.
A14 05      @1 Department of Geology, Faculty of Science, Palacký University, 17. Listopadu 12 @2 771 46 Olomouc @3 CZE @Z 7 aut.
A15 01      @1 KTH-International Groundwater Arsenic Research Group, Department of Sustainable Development, Environmental Science and Engineering, KTH Royal Institute of Technology @2 100 44 Stockholm @3 SWE @Z 1 aut.
A15 02      @1 Cooperative Research Centre for Contamination Assessment and Remediation of the Environment Building X, University of South Australia @2 Mawson Lakes Campus, SA 5095 @3 AUS @Z 2 aut.
A15 03      @1 School of Earth, Atmospheric & Environmental Sciences and Williamson Research Centre for Molecular Environmental Science, The University of Manchester @2 Manchester M13 9PL @3 GBR @Z 3 aut.
A15 04      @1 Department of Geology and Geophysics, Indian Institute of Technology Kharagpur @2 Kharagpur, WB 721302 @3 IND @Z 4 aut.
A15 05      @1 Faculty of Engineering and Surveying, University of Southern Queensland @2 Toowoomba, Queensland 4350 @3 AUS @Z 5 aut.
A15 06      @1 ISTerre-OSUG, CNRS, J. Fourier University of Grenoble-I, BP 53 @2 38041 Grenoble @3 FRA @Z 6 aut.
A20       @1 373-392
A21       @1 2014
A23 01      @0 ENG
A43 01      @1 INIST @2 13239 @5 354000502687550080
A44       @0 0000 @1 © 2015 INIST-CNRS. All rights reserved.
A45       @0 1 p.1/4
A47 01  1    @0 15-0030907
A60       @1 P
A61       @0 A
A64 01  1    @0 Journal of hydrology : (Amsterdam)
A66 01      @0 GBR
C01 01    ENG  @0 Exploitation of groundwater from shallow, high prolific Holocene sedimentary aquifers has been a main element for achieving safe drinking water and food security in Bangladesh. However, the presence of elevated levels of geogenic arsenic (As) in these aquifers has undermined this success. Except for targeting safe aquifers through installations of tubewells to greater depth, no mitigation option has been successfully implemented on a larger scale. The objective of this study has been to characterise the hydrostratigraphy, groundwater flow patterns, the hydraulic properties to assess the vulnerability of low-arsenic aquifers at Matlab, in south-eastern Bangladesh, one of the worst arsenic-affected areas of the country. Groundwater modelling, conventional pumping test using multilevel piezometers, hydraulic head monitoring in piezometer nests, 14C dating of groundwater and assessment of groundwater abstraction were used. A model comprising of three aquifers covering the top 250 m of the model domain showed the best fit for the calibration evaluation criteria.
C02 01  2    @0 001E01N02
C02 02  2    @0 001E01O04
C02 03  2    @0 001E01N03
C02 04  2    @0 226A02
C02 05  2    @0 226B04
C02 06  2    @0 226A03
C03 01  2  FRE  @0 Arsenic @5 01
C03 01  2  ENG  @0 arsenic @5 01
C03 01  2  SPA  @0 Arsénico @5 01
C03 02  2  FRE  @0 Aquifère @5 02
C03 02  2  ENG  @0 aquifers @5 02
C03 03  2  FRE  @0 Eau potable @5 03
C03 03  2  ENG  @0 drinking water @5 03
C03 03  2  SPA  @0 Agua potable @5 03
C03 04  2  FRE  @0 Eau souterraine @5 04
C03 04  2  ENG  @0 ground water @5 04
C03 04  2  SPA  @0 Agua subterránea @5 04
C03 05  2  FRE  @0 Exploitation @5 05
C03 05  2  ENG  @0 exploitation @5 05
C03 05  2  SPA  @0 Explotación @5 05
C03 06  2  FRE  @0 Holocène @2 NX @5 06
C03 06  2  ENG  @0 Holocene @2 NX @5 06
C03 06  2  SPA  @0 Holoceno @2 NX @5 06
C03 07  2  FRE  @0 Profondeur @5 07
C03 07  2  ENG  @0 depth @5 07
C03 07  2  SPA  @0 Profundidad @5 07
C03 08  2  FRE  @0 Ecoulement @5 08
C03 08  2  ENG  @0 flow @5 08
C03 09  2  FRE  @0 Hydraulique @5 09
C03 09  2  ENG  @0 hydraulics @5 09
C03 09  2  SPA  @0 Hidraúlica @5 09
C03 10  2  FRE  @0 Modèle @5 10
C03 10  2  ENG  @0 models @5 10
C03 10  2  SPA  @0 Modelo @5 10
C03 11  2  FRE  @0 Essai débit @5 11
C03 11  2  ENG  @0 pump tests @5 11
C03 11  2  SPA  @0 Ensayo bombeo @5 11
C03 12  2  FRE  @0 Datation @5 12
C03 12  2  ENG  @0 dating @5 12
C03 12  2  SPA  @0 Fechado @5 12
C03 13  2  FRE  @0 Etalonnage @5 13
C03 13  2  ENG  @0 calibration @5 13
C03 13  2  SPA  @0 Contraste @5 13
C03 14  2  FRE  @0 Irrigation @5 14
C03 14  2  ENG  @0 irrigation @5 14
C03 14  2  SPA  @0 Irrigación @5 14
C03 15  2  FRE  @0 Pompage @5 15
C03 15  2  ENG  @0 pumping @5 15
C03 15  2  SPA  @0 Bombeo @5 15
C03 16  2  FRE  @0 Pollution @5 16
C03 16  2  ENG  @0 pollution @5 16
C03 16  2  SPA  @0 Polución @5 16
C03 17  2  FRE  @0 Topographie @5 17
C03 17  2  ENG  @0 topography @5 17
C03 17  2  SPA  @0 Topografía @5 17
C03 18  2  FRE  @0 Gestion ressource eau @5 18
C03 18  2  ENG  @0 water resource management @5 18
C03 18  2  SPA  @0 Gestión recurso agua @5 18
C03 19  2  FRE  @0 Approvisionnement eau @5 21
C03 19  2  ENG  @0 water supply @5 21
C03 19  2  SPA  @0 Conducción de agua @5 21
C03 20  2  FRE  @0 Hydrogéologie @5 22
C03 20  2  ENG  @0 hydrogeology @5 22
C03 20  2  SPA  @0 Hidrogeología @5 22
C03 21  2  FRE  @0 Simulation numérique @5 23
C03 21  2  ENG  @0 digital simulation @5 23
C03 21  2  SPA  @0 Simulación numérica @5 23
C03 22  2  FRE  @0 Ressource eau @5 24
C03 22  2  ENG  @0 water resources @5 24
C03 22  2  SPA  @0 Recurso agua @5 24
C03 23  2  FRE  @0 Politique eau @5 25
C03 23  2  ENG  @0 water policy @5 25
C03 24  2  FRE  @0 Bangladesh @2 NG @5 61
C03 24  2  ENG  @0 Bangladesh @2 NG @5 61
C07 01  2  FRE  @0 Quaternaire sup @2 NX
C07 01  2  ENG  @0 upper Quaternary @2 NX
C07 01  2  SPA  @0 Cuaternario sup @2 NX
C07 02  2  FRE  @0 Quaternaire @2 NX
C07 02  2  ENG  @0 Quaternary @2 NX
C07 02  2  SPA  @0 Cuaternario @2 NX
C07 03  2  FRE  @0 Cénozoïque @2 NX
C07 03  2  ENG  @0 Cenozoic @2 NX
C07 03  2  SPA  @0 Cenozoico @2 NX
C07 04  2  FRE  @0 Phanérozoïque @2 NX
C07 04  2  ENG  @0 Phanerozoic @2 NX
C07 04  2  SPA  @0 Fanerozoico @2 NX
C07 05  2  FRE  @0 Asie @2 564
C07 05  2  ENG  @0 Asia @2 564
C07 05  2  SPA  @0 Asia @2 564
N21       @1 047

Format Inist (serveur)

NO : PASCAL 15-0030907 INIST
ET : Hydrogeological investigation for assessment of the sustainability of low-arsenic aquifers as a safe drinking water source in regions with high-arsenic groundwater in Matlab, southeastern Bangladesh
AU : VON BRÖMSSEN (Mattias); MARKUSSEN (Lars); BHATTACHARYA (Prosun); KAZI MATIN AHMED; HOSSAIN (Mohammed); JACKS (Gunnar); SRACEK (Ondra); THUNVIK (Roger); AZIZ HASAN (M.); MAINUL ISLAM (M.); MOKHLESUR RAHMAN (M.); BHATTACHARYA (Prosun); NAIDU (Ravi); POLYA (David A.); MUKHERJEE (Abhijit); BUNDSCHUH (Jochen); CHARLET (Laurent)
AF : KTH-International Groundwater Arsenic Research Group, Department of Sustainable Development, Environmental Science and Engineering, KTH Royal Institute of Technology Teknikringn 76/100 44 Stockholm/Suède (1 aut., 3 aut., 5 aut., 6 aut., 8 aut., 9 aut.); Department of Soil and Water Environment, Ramböll Sweden AB, Box 4205/102 65 Stockholm/Suède (1 aut., 2 aut.); Department of Geology, University of Dhaka, Curzon Hall Campus/Dhaka 1000/Bangladesh (4 aut., 9 aut., 11 aut.); NGO Forum for Drinking Water Supply and Sanitation, Block-E/Lalmatia, Dhaka/Bangladesh (5 aut., 10 aut.); Department of Geology, Faculty of Science, Palacký University, 17. Listopadu 12/771 46 Olomouc/Tchèque, République (7 aut.); KTH-International Groundwater Arsenic Research Group, Department of Sustainable Development, Environmental Science and Engineering, KTH Royal Institute of Technology/100 44 Stockholm/Suède (1 aut.); Cooperative Research Centre for Contamination Assessment and Remediation of the Environment Building X, University of South Australia/Mawson Lakes Campus, SA 5095/Australie (2 aut.); School of Earth, Atmospheric & Environmental Sciences and Williamson Research Centre for Molecular Environmental Science, The University of Manchester/Manchester M13 9PL/Royaume-Uni (3 aut.); Department of Geology and Geophysics, Indian Institute of Technology Kharagpur/Kharagpur, WB 721302/Inde (4 aut.); Faculty of Engineering and Surveying, University of Southern Queensland/Toowoomba, Queensland 4350/Australie (5 aut.); ISTerre-OSUG, CNRS, J. Fourier University of Grenoble-I, BP 53/38041 Grenoble/France (6 aut.)
DT : Publication en série; Niveau analytique
SO : Journal of hydrology : (Amsterdam); ISSN 0022-1694; Coden JHYDA7; Royaume-Uni; Da. 2014; Vol. 518; No. p. c; Pp. 373-392; Bibl. 1 p.1/4
LA : Anglais
EA : Exploitation of groundwater from shallow, high prolific Holocene sedimentary aquifers has been a main element for achieving safe drinking water and food security in Bangladesh. However, the presence of elevated levels of geogenic arsenic (As) in these aquifers has undermined this success. Except for targeting safe aquifers through installations of tubewells to greater depth, no mitigation option has been successfully implemented on a larger scale. The objective of this study has been to characterise the hydrostratigraphy, groundwater flow patterns, the hydraulic properties to assess the vulnerability of low-arsenic aquifers at Matlab, in south-eastern Bangladesh, one of the worst arsenic-affected areas of the country. Groundwater modelling, conventional pumping test using multilevel piezometers, hydraulic head monitoring in piezometer nests, 14C dating of groundwater and assessment of groundwater abstraction were used. A model comprising of three aquifers covering the top 250 m of the model domain showed the best fit for the calibration evaluation criteria.
CC : 001E01N02; 001E01O04; 001E01N03; 226A02; 226B04; 226A03
FD : Arsenic; Aquifère; Eau potable; Eau souterraine; Exploitation; Holocène; Profondeur; Ecoulement; Hydraulique; Modèle; Essai débit; Datation; Etalonnage; Irrigation; Pompage; Pollution; Topographie; Gestion ressource eau; Approvisionnement eau; Hydrogéologie; Simulation numérique; Ressource eau; Politique eau; Bangladesh
FG : Quaternaire sup; Quaternaire; Cénozoïque; Phanérozoïque; Asie
ED : arsenic; aquifers; drinking water; ground water; exploitation; Holocene; depth; flow; hydraulics; models; pump tests; dating; calibration; irrigation; pumping; pollution; topography; water resource management; water supply; hydrogeology; digital simulation; water resources; water policy; Bangladesh
EG : upper Quaternary; Quaternary; Cenozoic; Phanerozoic; Asia
SD : Arsénico; Agua potable; Agua subterránea; Explotación; Holoceno; Profundidad; Hidraúlica; Modelo; Ensayo bombeo; Fechado; Contraste; Irrigación; Bombeo; Polución; Topografía; Gestión recurso agua; Conducción de agua; Hidrogeología; Simulación numérica; Recurso agua
LO : INIST-13239.354000502687550080
ID : 15-0030907

Links to Exploration step

Pascal:15-0030907

Le document en format XML

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<name sortKey="Aziz Hasan, M" sort="Aziz Hasan, M" uniqKey="Aziz Hasan M" first="M." last="Aziz Hasan">M. Aziz Hasan</name>
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<name sortKey="Mainul Islam, M" sort="Mainul Islam, M" uniqKey="Mainul Islam M" first="M." last="Mainul Islam">M. Mainul Islam</name>
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<title xml:lang="en" level="a">Hydrogeological investigation for assessment of the sustainability of low-arsenic aquifers as a safe drinking water source in regions with high-arsenic groundwater in Matlab, southeastern Bangladesh</title>
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<title level="j" type="main">Journal of hydrology : (Amsterdam)</title>
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<term>Bangladesh</term>
<term>Holocene</term>
<term>aquifers</term>
<term>arsenic</term>
<term>calibration</term>
<term>dating</term>
<term>depth</term>
<term>digital simulation</term>
<term>drinking water</term>
<term>exploitation</term>
<term>flow</term>
<term>ground water</term>
<term>hydraulics</term>
<term>hydrogeology</term>
<term>irrigation</term>
<term>models</term>
<term>pollution</term>
<term>pump tests</term>
<term>pumping</term>
<term>topography</term>
<term>water policy</term>
<term>water resource management</term>
<term>water resources</term>
<term>water supply</term>
</keywords>
<keywords scheme="Pascal" xml:lang="fr">
<term>Arsenic</term>
<term>Aquifère</term>
<term>Eau potable</term>
<term>Eau souterraine</term>
<term>Exploitation</term>
<term>Holocène</term>
<term>Profondeur</term>
<term>Ecoulement</term>
<term>Hydraulique</term>
<term>Modèle</term>
<term>Essai débit</term>
<term>Datation</term>
<term>Etalonnage</term>
<term>Irrigation</term>
<term>Pompage</term>
<term>Pollution</term>
<term>Topographie</term>
<term>Gestion ressource eau</term>
<term>Approvisionnement eau</term>
<term>Hydrogéologie</term>
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<div type="abstract" xml:lang="en">Exploitation of groundwater from shallow, high prolific Holocene sedimentary aquifers has been a main element for achieving safe drinking water and food security in Bangladesh. However, the presence of elevated levels of geogenic arsenic (As) in these aquifers has undermined this success. Except for targeting safe aquifers through installations of tubewells to greater depth, no mitigation option has been successfully implemented on a larger scale. The objective of this study has been to characterise the hydrostratigraphy, groundwater flow patterns, the hydraulic properties to assess the vulnerability of low-arsenic aquifers at Matlab, in south-eastern Bangladesh, one of the worst arsenic-affected areas of the country. Groundwater modelling, conventional pumping test using multilevel piezometers, hydraulic head monitoring in piezometer nests,
<sup>14</sup>
C dating of groundwater and assessment of groundwater abstraction were used. A model comprising of three aquifers covering the top 250 m of the model domain showed the best fit for the calibration evaluation criteria.</div>
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<s0>hydraulics</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="2" l="SPA">
<s0>Hidraúlica</s0>
<s5>09</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE">
<s0>Modèle</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="ENG">
<s0>models</s0>
<s5>10</s5>
</fC03>
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<s0>Modelo</s0>
<s5>10</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE">
<s0>Essai débit</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="ENG">
<s0>pump tests</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="SPA">
<s0>Ensayo bombeo</s0>
<s5>11</s5>
</fC03>
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<s0>Datation</s0>
<s5>12</s5>
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<s0>dating</s0>
<s5>12</s5>
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<fC03 i1="12" i2="2" l="SPA">
<s0>Fechado</s0>
<s5>12</s5>
</fC03>
<fC03 i1="13" i2="2" l="FRE">
<s0>Etalonnage</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="2" l="ENG">
<s0>calibration</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="2" l="SPA">
<s0>Contraste</s0>
<s5>13</s5>
</fC03>
<fC03 i1="14" i2="2" l="FRE">
<s0>Irrigation</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="2" l="ENG">
<s0>irrigation</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="2" l="SPA">
<s0>Irrigación</s0>
<s5>14</s5>
</fC03>
<fC03 i1="15" i2="2" l="FRE">
<s0>Pompage</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="2" l="ENG">
<s0>pumping</s0>
<s5>15</s5>
</fC03>
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<s0>Bombeo</s0>
<s5>15</s5>
</fC03>
<fC03 i1="16" i2="2" l="FRE">
<s0>Pollution</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="ENG">
<s0>pollution</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="SPA">
<s0>Polución</s0>
<s5>16</s5>
</fC03>
<fC03 i1="17" i2="2" l="FRE">
<s0>Topographie</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="2" l="ENG">
<s0>topography</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="2" l="SPA">
<s0>Topografía</s0>
<s5>17</s5>
</fC03>
<fC03 i1="18" i2="2" l="FRE">
<s0>Gestion ressource eau</s0>
<s5>18</s5>
</fC03>
<fC03 i1="18" i2="2" l="ENG">
<s0>water resource management</s0>
<s5>18</s5>
</fC03>
<fC03 i1="18" i2="2" l="SPA">
<s0>Gestión recurso agua</s0>
<s5>18</s5>
</fC03>
<fC03 i1="19" i2="2" l="FRE">
<s0>Approvisionnement eau</s0>
<s5>21</s5>
</fC03>
<fC03 i1="19" i2="2" l="ENG">
<s0>water supply</s0>
<s5>21</s5>
</fC03>
<fC03 i1="19" i2="2" l="SPA">
<s0>Conducción de agua</s0>
<s5>21</s5>
</fC03>
<fC03 i1="20" i2="2" l="FRE">
<s0>Hydrogéologie</s0>
<s5>22</s5>
</fC03>
<fC03 i1="20" i2="2" l="ENG">
<s0>hydrogeology</s0>
<s5>22</s5>
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<fC03 i1="20" i2="2" l="SPA">
<s0>Hidrogeología</s0>
<s5>22</s5>
</fC03>
<fC03 i1="21" i2="2" l="FRE">
<s0>Simulation numérique</s0>
<s5>23</s5>
</fC03>
<fC03 i1="21" i2="2" l="ENG">
<s0>digital simulation</s0>
<s5>23</s5>
</fC03>
<fC03 i1="21" i2="2" l="SPA">
<s0>Simulación numérica</s0>
<s5>23</s5>
</fC03>
<fC03 i1="22" i2="2" l="FRE">
<s0>Ressource eau</s0>
<s5>24</s5>
</fC03>
<fC03 i1="22" i2="2" l="ENG">
<s0>water resources</s0>
<s5>24</s5>
</fC03>
<fC03 i1="22" i2="2" l="SPA">
<s0>Recurso agua</s0>
<s5>24</s5>
</fC03>
<fC03 i1="23" i2="2" l="FRE">
<s0>Politique eau</s0>
<s5>25</s5>
</fC03>
<fC03 i1="23" i2="2" l="ENG">
<s0>water policy</s0>
<s5>25</s5>
</fC03>
<fC03 i1="24" i2="2" l="FRE">
<s0>Bangladesh</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="24" i2="2" l="ENG">
<s0>Bangladesh</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC07 i1="01" i2="2" l="FRE">
<s0>Quaternaire sup</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="01" i2="2" l="ENG">
<s0>upper Quaternary</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="01" i2="2" l="SPA">
<s0>Cuaternario sup</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="02" i2="2" l="FRE">
<s0>Quaternaire</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="02" i2="2" l="ENG">
<s0>Quaternary</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="02" i2="2" l="SPA">
<s0>Cuaternario</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="03" i2="2" l="FRE">
<s0>Cénozoïque</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="03" i2="2" l="ENG">
<s0>Cenozoic</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="03" i2="2" l="SPA">
<s0>Cenozoico</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="04" i2="2" l="FRE">
<s0>Phanérozoïque</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="04" i2="2" l="ENG">
<s0>Phanerozoic</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="04" i2="2" l="SPA">
<s0>Fanerozoico</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="05" i2="2" l="FRE">
<s0>Asie</s0>
<s2>564</s2>
</fC07>
<fC07 i1="05" i2="2" l="ENG">
<s0>Asia</s0>
<s2>564</s2>
</fC07>
<fC07 i1="05" i2="2" l="SPA">
<s0>Asia</s0>
<s2>564</s2>
</fC07>
<fN21>
<s1>047</s1>
</fN21>
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<server>
<NO>PASCAL 15-0030907 INIST</NO>
<ET>Hydrogeological investigation for assessment of the sustainability of low-arsenic aquifers as a safe drinking water source in regions with high-arsenic groundwater in Matlab, southeastern Bangladesh</ET>
<AU>VON BRÖMSSEN (Mattias); MARKUSSEN (Lars); BHATTACHARYA (Prosun); KAZI MATIN AHMED; HOSSAIN (Mohammed); JACKS (Gunnar); SRACEK (Ondra); THUNVIK (Roger); AZIZ HASAN (M.); MAINUL ISLAM (M.); MOKHLESUR RAHMAN (M.); BHATTACHARYA (Prosun); NAIDU (Ravi); POLYA (David A.); MUKHERJEE (Abhijit); BUNDSCHUH (Jochen); CHARLET (Laurent)</AU>
<AF>KTH-International Groundwater Arsenic Research Group, Department of Sustainable Development, Environmental Science and Engineering, KTH Royal Institute of Technology Teknikringn 76/100 44 Stockholm/Suède (1 aut., 3 aut., 5 aut., 6 aut., 8 aut., 9 aut.); Department of Soil and Water Environment, Ramböll Sweden AB, Box 4205/102 65 Stockholm/Suède (1 aut., 2 aut.); Department of Geology, University of Dhaka, Curzon Hall Campus/Dhaka 1000/Bangladesh (4 aut., 9 aut., 11 aut.); NGO Forum for Drinking Water Supply and Sanitation, Block-E/Lalmatia, Dhaka/Bangladesh (5 aut., 10 aut.); Department of Geology, Faculty of Science, Palacký University, 17. Listopadu 12/771 46 Olomouc/Tchèque, République (7 aut.); KTH-International Groundwater Arsenic Research Group, Department of Sustainable Development, Environmental Science and Engineering, KTH Royal Institute of Technology/100 44 Stockholm/Suède (1 aut.); Cooperative Research Centre for Contamination Assessment and Remediation of the Environment Building X, University of South Australia/Mawson Lakes Campus, SA 5095/Australie (2 aut.); School of Earth, Atmospheric & Environmental Sciences and Williamson Research Centre for Molecular Environmental Science, The University of Manchester/Manchester M13 9PL/Royaume-Uni (3 aut.); Department of Geology and Geophysics, Indian Institute of Technology Kharagpur/Kharagpur, WB 721302/Inde (4 aut.); Faculty of Engineering and Surveying, University of Southern Queensland/Toowoomba, Queensland 4350/Australie (5 aut.); ISTerre-OSUG, CNRS, J. Fourier University of Grenoble-I, BP 53/38041 Grenoble/France (6 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Journal of hydrology : (Amsterdam); ISSN 0022-1694; Coden JHYDA7; Royaume-Uni; Da. 2014; Vol. 518; No. p. c; Pp. 373-392; Bibl. 1 p.1/4</SO>
<LA>Anglais</LA>
<EA>Exploitation of groundwater from shallow, high prolific Holocene sedimentary aquifers has been a main element for achieving safe drinking water and food security in Bangladesh. However, the presence of elevated levels of geogenic arsenic (As) in these aquifers has undermined this success. Except for targeting safe aquifers through installations of tubewells to greater depth, no mitigation option has been successfully implemented on a larger scale. The objective of this study has been to characterise the hydrostratigraphy, groundwater flow patterns, the hydraulic properties to assess the vulnerability of low-arsenic aquifers at Matlab, in south-eastern Bangladesh, one of the worst arsenic-affected areas of the country. Groundwater modelling, conventional pumping test using multilevel piezometers, hydraulic head monitoring in piezometer nests,
<sup>14</sup>
C dating of groundwater and assessment of groundwater abstraction were used. A model comprising of three aquifers covering the top 250 m of the model domain showed the best fit for the calibration evaluation criteria.</EA>
<CC>001E01N02; 001E01O04; 001E01N03; 226A02; 226B04; 226A03</CC>
<FD>Arsenic; Aquifère; Eau potable; Eau souterraine; Exploitation; Holocène; Profondeur; Ecoulement; Hydraulique; Modèle; Essai débit; Datation; Etalonnage; Irrigation; Pompage; Pollution; Topographie; Gestion ressource eau; Approvisionnement eau; Hydrogéologie; Simulation numérique; Ressource eau; Politique eau; Bangladesh</FD>
<FG>Quaternaire sup; Quaternaire; Cénozoïque; Phanérozoïque; Asie</FG>
<ED>arsenic; aquifers; drinking water; ground water; exploitation; Holocene; depth; flow; hydraulics; models; pump tests; dating; calibration; irrigation; pumping; pollution; topography; water resource management; water supply; hydrogeology; digital simulation; water resources; water policy; Bangladesh</ED>
<EG>upper Quaternary; Quaternary; Cenozoic; Phanerozoic; Asia</EG>
<SD>Arsénico; Agua potable; Agua subterránea; Explotación; Holoceno; Profundidad; Hidraúlica; Modelo; Ensayo bombeo; Fechado; Contraste; Irrigación; Bombeo; Polución; Topografía; Gestión recurso agua; Conducción de agua; Hidrogeología; Simulación numérica; Recurso agua</SD>
<LO>INIST-13239.354000502687550080</LO>
<ID>15-0030907</ID>
</server>
</inist>
</record>

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