Evidence map›Paper›PMID 28966395›Full record

ArticleJournal of hydrology2016

VULNERABILITY OF LOW-ARSENIC AQUIFERS TO MUNICIPAL PUMPING IN BANGLADESH.

P S K Knappett, B J Mailloux, I Choudhury, M R Khan, H A Michael, S Barua, D R Mondal, M S Steckler, S H Akhter, K M Ahmed and 7 more

Abstract read
In one paragraph

Article in Journal of hydrology, 2016. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 9 papers.

0numbers the graph read from it
0cells of the map it votes in
9citing papers in PubMed
–field-weighted citation impact
1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.

2 · The registry

The trial behind it

Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.

Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

9 citing papers in PubMed.

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4 · The record

Corrections and comments

PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.

5 · Who and what money

Authors and funding

17 authors.

P S K KnappettLamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964.
B J MaillouxDepartment of Environmental Science, Barnard College, New York, NY 10027.
I ChoudhuryDepartment of Geology, University of Dhaka, Dhaka 1000, Bangladesh.
M R KhanDepartment of Geological Sciences, University of Delaware, Newark, DE 19716.
H A MichaelDepartment of Civil and Environmental Engineering, University of Delaware, Newark, DE 19716.
S BaruaDepartment of Geology, Kansas State University, Manhattan, KS 66506.
D R MondalSchool of Earth & Environmental Sciences, Queens College, Queens, NY 11367.
M S StecklerLamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964.
S H AkhterDepartment of Geology, University of Dhaka, Dhaka 1000, Bangladesh.
K M AhmedDepartment of Geology, University of Dhaka, Dhaka 1000, Bangladesh.
B BostickLamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964.
C F HarveyDepartment of Civil & Environmental Engineering, Massachusetts Institute of Technology, Cambridge, MA 02139.
M ShamsudduhaInstitute for Risk & Disaster Reduction, University College London, London WC1E 6BT, UK.
P ShuaiDepartment of Geology and Geophysics, Texas A&M University, College Station, TX 77843.
I MihajlovLamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964.
R MozumderLamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964.
A van GeenLamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964.

Funding

Training CoreP42ES010349 · NIEHS · COLUMBIA UNIVERSITY HEALTH SCIENCES · PI NAVAS-ACIEN, ANA · 2000 to 2020
$53.6M
NIEHS NIH HHS P42 ES010349
6 · The paper itself

Abstract

Sandy aquifers deposited >12,000 years ago, some as shallow as 30 m, have provided a reliable supply of low-arsenic (As) drinking water in rural Bangladesh. This study concerns the potential risk of contaminating these aquifers in areas surrounding the city of Dhaka where hydraulic heads in aquifers >150 m deep have dropped by 70 m in a few decades due to municipal pumping. Water levels measured continuously from 2012 to 2014 in 12 deep (>150m), 3 intermediate (90-150 m) and 6 shallow (<90 m) community wells, 1 shallow private well, and 1 river piezometer show that the resulting drawdown cone extends 15-35 km east of Dhaka. Water levels in 4 low-As community wells within the 62-147 m depth range closest to Dhaka were inaccessible by suction for up to a third of the year. Lateral hydraulic gradients in the deep aquifer system ranged from 1.7×10

Identifiers

PMID28966395
PMCPMC5617134

What OpenQuestion holds

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Registered trials

None linked

Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.