Evidence map›Paper›PMID 37058571›Full record

ArticleScience advances2023

Water transport in reverse osmosis membranes is governed by pore flow, not a solution-diffusion mechanism.

Li Wang, Jinlong He, Mohammad Heiranian, Hanqing Fan, Lianfa Song, Ying Li, Menachem Elimelech

Open access · goldAbstract read
In one paragraph

Article in Science advances, 2023. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 39 papers.

0numbers the graph read from it
0cells of the map it votes in
39citing papers in PubMed
23.9field-weighted citation impact, top 1% of its field
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

39 citing papers in PubMed, 208 citations in OpenAlex.

  1. Review
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  8. In Situ Ptychographic X-ray Computed Tomography of Fully Hydrated Polyamide Membranes.Langmuir : the ACS journal of surfaces and colloids · 2026
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  13. Wearable solar fluidic system.Science advances · 2025
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  17. Article
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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

7 authors at 3 institutions in 1 country.

Li WangDepartment of Chemical and Environmental Engineering, Yale University, New Haven, CT 06520-8286, USA.ORCID 0000-0002-5542-6696
Jinlong HeDepartment of Mechanical Engineering, University of Wisconsin-Madison, Madison, WI 53706-1572, USA.
Mohammad HeiranianDepartment of Chemical and Environmental Engineering, Yale University, New Haven, CT 06520-8286, USA.ORCID 0000-0002-2227-4948
Hanqing FanDepartment of Chemical and Environmental Engineering, Yale University, New Haven, CT 06520-8286, USA.
Lianfa SongDepartment of Civil, Environmental, and Construction Engineering, Texas Tech University, Lubbock, TX 79409-1023, USA.ORCID 0000-0002-9684-1896
Ying LiDepartment of Mechanical Engineering, University of Wisconsin-Madison, Madison, WI 53706-1572, USA.ORCID 0000-0002-1487-3350
Menachem ElimelechDepartment of Chemical and Environmental Engineering, Yale University, New Haven, CT 06520-8286, USA.ORCID 0000-0003-4186-1563
Yale University · USUniversity of Wisconsin–Madison · USTexas Tech University · US

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

We performed nonequilibrium molecular dynamics (NEMD) simulations and solvent permeation experiments to unravel the mechanism of water transport in reverse osmosis (RO) membranes. The NEMD simulations reveal that water transport is driven by a pressure gradient within the membranes, not by a water concentration gradient, in marked contrast to the classic solution-diffusion model. We further show that water molecules travel as clusters through a network of pores that are transiently connected. Permeation experiments with water and organic solvents using polyamide and cellulose triacetate RO membranes showed that solvent permeance depends on the membrane pore size, kinetic diameter of solvent molecules, and solvent viscosity. This observation is not consistent with the solution-diffusion model, where permeance depends on the solvent solubility. Motivated by these observations, we demonstrate that the solution-friction model, in which transport is driven by a pressure gradient, can describe water and solvent transport in RO membranes.

Identifiers

PMID37058571
PMCPMC10104469
OpenAlexW4365504460

What OpenQuestion holds

Textmetadata
LicenceCC BY
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.