Ultra-slow capillary rise on hydrogel surfaces
Pith reviewed 2026-05-18 18:29 UTC · model grok-4.3
The pith
Capillary rise on agarose hydrogels proceeds ultra-slowly because liquid must flow through the gel's internal pores.
A machine-rendered reading of the paper's core claim, the machinery that carries it, and where it could break.
Core claim
The ultra-slow advance of the meniscus is governed by fluid transport through the porous hydrogel network rather than by the usual balance of capillary pressure, gravity, and bulk viscous resistance; a model built on this transport reproduces the observed dynamics across agarose concentrations and liquid viscosities.
What carries the argument
Fluid transport through the porous hydrogel network, which supplies liquid to the advancing contact line and thereby sets the observed ultra-slow speed.
If this is right
- Rise speed scales with gel concentration through the resulting change in permeability.
- Permeability at the gel-liquid interface can be extracted directly from the shape of the meniscus trajectory.
- The same description holds when the viscosity of the liquid inside the gel is varied.
- The method yields a spatially resolved permeability map without damaging the sample.
Where Pith is reading between the lines
- The same porous-transport limit may appear in other soft, permeable materials such as biological tissues or polymer scaffolds.
- Deliberately tuning pore size or connectivity could be used to control capillary-driven flows in hydrogel devices.
- The approach could be combined with local surface modifications to map how permeability varies across a single gel sample.
- Independent measurements of internal flow velocity inside the gel during rise would provide a direct test of the model's rate prediction.
Load-bearing premise
That fluid permeation through the gel pores is the dominant rate-limiting process and is not overridden by surface viscoelasticity or other hydrogel effects.
What would settle it
If the rise speed on a hydrogel whose pores have been blocked but whose surface wettability is unchanged remains just as ultra-slow as on the open-pore gel.
read the original abstract
Capillary rise occurs when a thin tube contacts a liquid, which rises against gravity due to the capillary force. This phenomenon is present in a wide range of everyday and industrial settings and provides the means to measure the physical properties of liquids. Here, we report on the unusual ultra-slow capillary rise on a solid-like material of agarose hydrogels. The observed meniscus motion cannot be described with classical capillary rise models, and we develop a new model based on the fluid transport through the porous hydrogel network. Our model is in good agreement with the experimental data for agarose gels made with five different concentrations and with two different viscosities of the liquid flowing inside the gel. Our results provide a non-invasive technique to directly estimate the permeability of hydrogel interfaces with high spatial resolution, which is important in the implementation of hydrogels in advanced biomedical applications.
Editorial analysis
A structured set of objections, weighed in public.
Referee Report
Summary. The manuscript reports ultra-slow capillary rise of liquid menisci on agarose hydrogel surfaces that deviates from classical capillary-rise dynamics. The authors argue that the motion cannot be captured by standard models and instead develop a new model based on fluid permeation through the porous hydrogel network. They report quantitative agreement between this model and experiments performed on gels prepared at five different agarose concentrations and with two different liquid viscosities. The work concludes that the approach supplies a non-invasive, spatially resolved method for estimating hydrogel permeability, with relevance to biomedical applications.
Significance. If the porous-transport mechanism is shown to be dominant and the model is not over-fitted, the result would supply a physically grounded description of capillary dynamics on soft porous interfaces together with a practical permeability-measurement technique. The breadth of the experimental matrix (five concentrations, two viscosities) constitutes a positive feature that could strengthen the empirical case once fitting details and controls are supplied.
major comments (3)
- [Abstract] Abstract: the statement that the observed meniscus motion 'cannot be described with classical capillary rise models' is central to the motivation for the new porous-transport model, yet the manuscript provides no quantitative comparison (e.g., fits of the Lucas-Washburn equation or variants with adjusted contact angle, viscosity, or effective radius) demonstrating systematic failure across the full data set. Without such explicit exclusion, the necessity of the new model remains unestablished.
- [Abstract] Abstract and model section: the assumption that fluid transport through the porous hydrogel network is the dominant mechanism is load-bearing for the central claim, but the text does not report measurements or timescale comparisons that quantitatively rule out alternative hydrogel-specific effects such as viscoelastic relaxation or surface swelling. These controls are required to substantiate the physical basis of the model.
- [Abstract] Abstract: the reported 'good agreement' with data for five concentrations and two viscosities is presented without any description of the fitting procedure, error bars on the data or model curves, or criteria for data inclusion/exclusion. This omission prevents assessment of whether the agreement is robust or achieved through post-hoc parameter adjustment.
minor comments (2)
- Notation for permeability and porosity should be defined at first use and kept consistent between the model equations and the experimental analysis.
- Figure captions should explicitly state the number of independent runs, the fitting method, and any scaling used so that the agreement can be evaluated directly from the figures.
Simulated Author's Rebuttal
We thank the referee for their careful and constructive review of our manuscript. We have addressed each major comment point by point below, making revisions to the text, adding quantitative comparisons, and expanding the methods and discussion sections where appropriate to strengthen the justification for the porous-transport model.
read point-by-point responses
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Referee: [Abstract] Abstract: the statement that the observed meniscus motion 'cannot be described with classical capillary rise models' is central to the motivation for the new porous-transport model, yet the manuscript provides no quantitative comparison (e.g., fits of the Lucas-Washburn equation or variants with adjusted contact angle, viscosity, or effective radius) demonstrating systematic failure across the full data set. Without such explicit exclusion, the necessity of the new model remains unestablished.
Authors: We agree that an explicit quantitative comparison is needed to establish the failure of classical models. In the revised manuscript we have added a dedicated subsection in the Results section together with a new supplementary figure that reports Lucas-Washburn fits (and variants allowing adjusted contact angle, viscosity, and effective radius) to the entire experimental data set. These fits show systematic over-prediction of the rise dynamics by several orders of magnitude for all five agarose concentrations and both viscosities, thereby justifying the necessity of the porous-transport model. revision: yes
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Referee: [Abstract] Abstract and model section: the assumption that fluid transport through the porous hydrogel network is the dominant mechanism is load-bearing for the central claim, but the text does not report measurements or timescale comparisons that quantitatively rule out alternative hydrogel-specific effects such as viscoelastic relaxation or surface swelling. These controls are required to substantiate the physical basis of the model.
Authors: We acknowledge that dedicated experimental controls would be ideal. In the revised manuscript we have added a paragraph in the model section that compares the observed capillary-rise timescales (hours) with literature values for agarose viscoelastic relaxation (seconds to minutes) and shows that surface-swelling kinetics cannot reproduce the measured dependence on gel concentration and liquid viscosity. While we have not performed new dedicated experiments to exclude these alternatives, the consistency of the porous-transport model across the full experimental matrix supports its physical basis; we would be happy to discuss additional controls if the referee considers them essential. revision: partial
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Referee: [Abstract] Abstract: the reported 'good agreement' with data for five concentrations and two viscosities is presented without any description of the fitting procedure, error bars on the data or model curves, or criteria for data inclusion/exclusion. This omission prevents assessment of whether the agreement is robust or achieved through post-hoc parameter adjustment.
Authors: We thank the referee for highlighting this omission. The revised manuscript now includes an expanded Methods section that details the fitting procedure (least-squares optimization with fixed versus free parameters), the criteria used for data inclusion, and the sources of uncertainty. Error bars have been added to all experimental data points in the figures, and model curves are shown with shaded uncertainty bands derived from parameter covariance. These additions allow readers to evaluate the robustness of the reported agreement. revision: yes
Circularity Check
No significant circularity; model derived from independent physical mechanism and validated externally
full rationale
The paper derives a new model for ultra-slow meniscus motion from the physical mechanism of fluid permeation through the porous hydrogel network rather than classical capillary rise. This derivation is presented as following from the assumed dominant transport process and is then compared to independent experimental datasets across five gel concentrations and two liquid viscosities. No equations or steps reduce a prediction to a fitted parameter by construction, no self-citations are invoked as load-bearing uniqueness theorems, and the agreement is reported with external data runs that are not statistically forced by the model inputs themselves. The central claim therefore retains independent content beyond its starting assumptions.
Axiom & Free-Parameter Ledger
Lean theorems connected to this paper
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IndisputableMonolith/Cost/FunctionalEquation.leanwashburn_uniqueness_aczel unclear?
unclearRelation between the paper passage and the cited Recognition theorem.
the damped flow rate through the porous hydrogel material was modelled using Darcy’s law... z(t)∼2κγcosθ/ηR² t = U t
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IndisputableMonolith/Foundation/RealityFromDistinction.leanreality_from_one_distinction unclear?
unclearRelation between the paper passage and the cited Recognition theorem.
Our model is in good agreement with the experimental data for agarose gels made with five different concentrations
What do these tags mean?
- matches
- The paper's claim is directly supported by a theorem in the formal canon.
- supports
- The theorem supports part of the paper's argument, but the paper may add assumptions or extra steps.
- extends
- The paper goes beyond the formal theorem; the theorem is a base layer rather than the whole result.
- uses
- The paper appears to rely on the theorem as machinery.
- contradicts
- The paper's claim conflicts with a theorem or certificate in the canon.
- unclear
- Pith found a possible connection, but the passage is too broad, indirect, or ambiguous to say the theorem truly supports the claim.
Reference graph
Works this paper leans on
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[2]
Ziege, R. et al. Adaptation of Escherichia coli Biofilm Growth, Morphology, and Mechanical Properties to Substrate Water Content. ACS Biomater. Sci. Eng. 7, 5315–5325 (2021). 26. Moore, M. J. et al. The dance of the nanobubbles: detecting acoustic backscatter from sub-micron bubbles using ultra-high frequency acoustic microscopy. Nanoscale 12, 21420–21428...
work page 2021
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[3]
Latikka, M. et al. Ferrofluid Microdroplet Splitting for Population‐Based Microfluidics and Interfacial Tensiometry. Adv. Sci. 7, 2000359 (2020). 43. Rigoni, C., Beaune, G., Harnist, B., Sohrabi, F. & Timonen, J. V. I. Ferrofluidic aqueous two-phase system with ultralow interfacial tension and micro-pattern formation. Commun. Mater. 3, 26 (2022). 44. Reys...
discussion (0)
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