Evidence map›Paper›PMID 39241359›Full record

ArticleJournal of hazardous materials2024

Identification of key factors and mechanism determining arsenic mobilization in paddy soil-porewater-rice system.

Shuqiong Kong, Dawei Cai, Yixian Shao, Xiaguo Wei, Zhihao Yi, Robert A Root, Jon Chorover

Abstract read
In one paragraph

Article in Journal of hazardous materials, 2024. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 2 papers.

0numbers the graph read from it
0cells of the map it votes in
2citing 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

2 citing papers in PubMed.

  1. Article
  2. Review
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

7 authors.

Shuqiong KongMOE Key Laboratory of Groundwater Quality and Health, China University of Geosciences, Wuhan, Hubei 430078, China; School of Environmental Studies, China University of Geosciences, Wuhan, Hubei 430078, China. Electronic address: ksq@cug.edu.cn.
Dawei CaiCollege of Environmental Sciences and Engineering, Peking University, Beijing 100871, China.
Yixian ShaoZhejiang Institute of Geological Survey, Hangzhou, Zhejiang 311200, China.
Xiaguo WeiMOE Key Laboratory of Groundwater Quality and Health, China University of Geosciences, Wuhan, Hubei 430078, China; School of Environmental Studies, China University of Geosciences, Wuhan, Hubei 430078, China.
Zhihao YiMOE Key Laboratory of Groundwater Quality and Health, China University of Geosciences, Wuhan, Hubei 430078, China; School of Environmental Studies, China University of Geosciences, Wuhan, Hubei 430078, China.
Robert A RootDepartment of Environmental Science, University of Arizona, Tucson, AZ 85721, United States. Electronic address: rroot@email.arizona.edu.
Jon ChoroverDepartment of Environmental Science, University of Arizona, Tucson, AZ 85721, United States. Electronic address: chorover@arizona.edu.

Funding

TRANSPORT OF TRACE METALS IN A POLLUTED AQUIFERP42ES004940 · NIEHS · UNIVERSITY OF ARIZONA · PI Jon D Chorover · 1990 to 2026
$68.1M
SOUTHWEST ENVIRONMENTAL HEALTH SCIENCES CENTERP30ES006694 · NIEHS · UNIVERSITY OF ARIZONA · PI DEAN BILLHEIMER · 1994 to 2026
$36.7M
NIEHS NIH HHS P30 ES006694NIEHS NIH HHS P42 ES004940
6 · The paper itself

Abstract

Arsenic (As) mobilization in paddy fields poses significant health risks, necessitating a thorough understanding of the controlling factors and mechanisms to safeguard human health. We conducted a comprehensive investigation of the soil-porewater-rice system throughout the rice life cycle, focusing on monitoring arsenic distribution and porewater characteristics in typical paddy field plots. Soil pH ranged from 4.79 to 7.98, while porewater pH was weakly alkaline, varying from 7.2 to 7.47. Total arsenic content in paddy soils ranged from 6.8 to 17.2 mg/kg, with arsenic concentrations in porewater during rice growth ranging from 2.97 to 14.85 μg/L. Specifically, arsenite concentrations in porewater ranged from 0.48 to 7.91 μg/L, and arsenate concentrations ranged from 0.73 to 5.83 μg/L. Through principal component analysis (PCA) and analysis of redox factors, we identified that arsenic concentration in porewater is predominantly influenced by the interplay of reduction and desorption processes, contributing 43.5 % collectively. Specifically, the reductive dissolution of iron oxides associated with organic carbon accounted for 23.3 % of arsenic concentration dynamics in porewater. Additionally, arsenic release from the soil followed a sequence starting with nitrate reduction, followed by ferric ion reduction, and subsequently sulfate reduction. Our findings provide valuable insights into the mechanisms governing arsenic mobilization within the paddy soil-porewater-rice system. These insights could inform strategies for irrigation management aimed at mitigating arsenic toxicity and associated health risks.

Indexed as

ArsenicOryzaSoil PollutantsWater Pollutants, ChemicalAgricultureEnvironmental MonitoringHydrogen-Ion ConcentrationOxidation-ReductionSoilArsenicSoilSoil PollutantsWater Pollutants, ChemicalArsenicPorewaterPrincipal component analysisRedox

Identifiers

PMID39241359
PMCPMC11451535

What OpenQuestion holds

Textmetadata
LicenceTDM
Read underepoch 390

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.