Jesse Smithyman* and
Zhiyong Liang
High-Performance Materials Institute, Florida State University, 2005 Levy Ave, Tallahassee, FL 32310, USA. E-mail: jessesmithyman@gmail.com; liang@eng.fsu.edu; jrs03n@my.fsu.edu; Tel: +1-954-547-3081
First published on 26th June 2014
The response to humidity changes from the open-circuit potential (OCP) of a coaxial electrode polymer electrolyte cell was characterized. The OCP response showed a dependency on both the rate of change of the humidity and on the rate of water diffusion within the electrolyte, suggesting the Gibbs free energy due to ionic concentration gradients as the source of the OCP response. This is supported through the estimation of the membrane potential using the Nernst equation and the good agreement between the experimental and theoretical results. The method exploits the hygroscopic properties of the polymer electrolyte and utilizes changes in the relative humidity (RH) of the surrounding environment to induce a concentration gradient between the electrodes. The establishment of the concentration gradient is achieved through the use of a solid-state electrochemical cell with a coaxial electrode structure, enabling the exposure of only one of the electrodes to the environment. These results have implications for applications such as energy harvesting and self-powered sensors and additionally may provide a novel approach to studying the thermodynamic properties of polymer electrolytes.
This local concentration change occurs due to the hygroscopic nature of the polymer electrolyte and its ability to rapidly exchange H2O molecules with the surrounding environment as the relative humidity changes. The occurrence of this absorption/desorption at only one of the electrodes is critical to the establishment of the concentration gradient and is achieved through the use of a coaxial electrode cell architecture. The coaxial architecture ensures that the inner electrode is shielded from the surrounding environment, thereby causing the water absorption/desorption to occur only at the outer electrode.
Unlike the rapid action potentials of excitable animal cells which contain non-responsive refractory periods, the OCP of the coaxial cell was still responsive to humidity changes during its slow return towards the resting potential. This is demonstrated by the oscillations in the RH prior to its stabilization at the target humidity due to the PID control mechanism used for its regulation. These oscillations produce peaks in the RH that are also captured by the OCP during its return to equilibrium for both an increase or decrease in humidity, as shown in Fig. 1a and b.
The repeatability of the OCP response was investigated by performing three iterations of a 10% increase, 10% decrease cycling of the RH at three different humidity levels: 35–45%, 45–55% and 55–65%. Following each step change, the humidity was kept constant for at least 1 hour to allow the cell's OCP to return to a quasi-equilibrium/resting potential prior to each humidity step change. Fig. 1 is provided as a representative sample of the results from the cycling tests. The original data for all tests are provided in the ESI.†
The coordinates (x, y) of both the RH and OCP peaks were obtained using the Peak Analyzer function in the OriginLab software program. Two quantities were calculated from the peak data in order to compare the data sets and analyze the characteristics of the OCP response. The first is a calculation of the time difference between the RH peak and the corresponding OCP peak to quantify the lag between the data sets. The calculation of the time between peaks (Δt) is defined here as the time (i.e. x-coordinate) of the OCP peak (tOCP) subtracted from the RH peak (tRH) peak time, as shown in eqn (1):
| Δt = tRH − tOCP | (1) |
The second quantity calculated from the peak data is the magnitude (absolute value) of the OCP response. The peak magnitude, or change in the OCP (ΔOCP), is the absolute value of the difference between the peak potential (OCPpeak) and the potential prior to the humidity change (OCPinitial), as shown in eqn (2):
| ΔOCP = OCPpeak − OCPinitial | (2) |
A thermodynamic estimate of the potential generated from the humidity induced salinity difference can be calculated through the use of the Nernst relationship as shown in eqn (3):
![]() | (3) |
and
are the water activities at the outer and inner electrodes, respectively. The water activity at each electrode can be represented through the humidity data to provide a theoretical prediction of the potential based purely on the thermodynamics of the Gibbs free energy of the salinity difference generated from an increase of decrease of the water activity at on electrode. It should be noted that eqn (3) corresponds to a polarity where the inner electrode is positive and could be written alternatively as the negative of the current form for the alternate polarity.
Since the system was allowed to reach equilibrium prior to each test, the initial humidity will provide an accurate representation of the water activity at the inner electrode up until the point when water diffusion to/from the outer electrode reaches the inner electrode and increases/decreases the local water concentration. To estimate the peak potential induced by the humidity change, the water activity at the outer electrode can be represented by the peak humidity. The thermodynamic prediction of ΔOCP based on the Nernst relationship is shown in eqn (4) with the results plotted along with the ΔOCP data in Fig. 2.
![]() | (4) |
Fig. 2 shows the accuracy of the Nernst equation and is strong supporting evidence of the underlying mechanism of the Gibbs free energy being responsible for the OCP response. In fact, eqn (4) can be generalized to calculate the humidity at time i, by replacing the ‘peak humidity’ with the humidity at time i and is highly accurate during conditions of minimal kinetic effects (i.e. before diffusion of water reaches the inner electrode). An example for both an increase and decrease in humidity are shown in the ESI (Fig. S12 and S13, and eqn (S1)†).
First, we can see from Fig. 2 that the trend of decreasing ΔOCP with increasing initial RH is a thermodynamic feature of the system under these conditions. Interestingly, the thermodynamic predictions were nearly identical to the peak potentials observed experimentally for the increasing humidity cases, yet a consistent deviation was observed between the experimental and predicted response for the decreasing humidity tests. As seen in Fig. 2, according to eqn (4), the potentials should be higher for decreasing humidity than the peak potentials of the increasing humidity tests. In general, deviations from the thermodynamic predictions are likely to occur due to kinetic effects from the properties of the Nafion electrolyte or due to effects of the test conditions. We believe the later is a possible cause for the consistent deviation observed in the decreasing humidity tests. The chamber decreases the humidity by pumping the chamber air through a desiccant column, which typically results in a slower rate of change of the humidity when compared with the increase of humidity from injection of water vapor from an ultrasonic humidifier. The plots of the first derivative of the humidity data are provided in the ESI† for one cycle from each humidity range and show the consistently slower rate of the RH decrease versus the RH increase. While further studies are required to fully elucidate the effects of various kinetic relationships, some insight can be obtained from the results of the time between peaks (Δt) plotted in Fig. 3.
Fig. 3 shows a strong dependency of Δt on the initial humidity with an additional dependency on whether an increase or decrease in RH occurred from that initial RH. With higher initial humidity of the test, a larger Δt is observed, while when starting from the same initial RH, a decrease in humidity always produced a larger Δt than an increase of similar magnitude (all results in Fig. 2 and 3 are of the same magnitude change). Note that a positive Δt indicates that the OCP peak preceded the RH peak. This preceding peak, or negative lag, of the OCP versus the RH is observable in the original test data shown in Fig. 1b for a 55% to 45% decrease event. Such a response would not be expected under the assumption that the OCP is changing in response to the humidity change. The transport properties of the Nafion electrolyte may provide some explanation for these observations.
Dr Benziger group has shown three important characteristics of water transport through Nafion membranes: (1) the limiting water self-diffusivity in Nafion increases exponentially with water activity,6 (2) water desorption is faster than absorption,7 and (3) water transport is diffusion limited at lower water concentrations, while at high water content the interfacial transport at the membrane/vapor interface becomes the limiting step. Due to the significant increase in water diffusivity with membrane water content, water diffusion to/from the interface is faster during desorption than adsorption.
Immediately upon establishment of the concentration gradient, water diffusion towards regions of lower water content begins in order to minimize the energy of the system. So long as this diffusion has not changed the local concentration at the inner electrode, and absorption/evaporation continues at the outer electrode, the concentration gradient will continue to increase. However, once the diffusion front reaches the inner electrode, the magnitude of the concentration difference begins to decrease, along with the potential difference observed between the electrodes (i.e. causing a peak in the OCP). This would result in the OCP peaking prior to the RH when conditions are such that the rate of the water transport through the electrolyte is limited by interfacial transport (as opposed to diffusion) and the RH step-change is large. Similarly, faster diffusion of water will result in the OCP peaking sooner (i.e. larger Δt), precisely what is observed in the results of Fig. 3.
On multiple occasions during long periods of constant RH, the humidity displayed a series of low-magnitude (∼±0.25% RH) oscillations around the humidity set point over a period of 2–3 hours. The top plot of Fig. 4 shows the OCP and RH data during one such period of low-magnitude oscillations in the RH with the first derivatives of each data set shown in the bottom plot.
After responding to four consecutive peaks in the RH, the OCP showed no corresponding responds to a fifth RH peak. The OCP did however respond to the decrease from the fifth peak as the humidity returned to the RH set point; a response that had not occurred previously for the other declines in RH from the first four peaks. The strong correlation between the first derivatives of the OCP and RH in bottom plot of Fig. 4 provides the explanations for these “inconsistencies”. The OCP change is dependent on the rate of change of the humidity and not the magnitude of the humidity in and of itself. The gradual increase of humidity to the fifth peak produced no significant peaks in the dRH dt−1 as the first four peaks did. However, the decrease from this peak was rapid enough, as observed by the dRH dt−1 peak just before the 85k mark, that a corresponding decrease in the OCP occurred.
This dependency on the rate of RH change is in line with the proposed mechanisms responsible for the OCP response. The rate of the humidity change will determine the rate of change in the water content at the outer electrode. If this rate is too slow, and the rate of diffusion through the electrolyte is sufficiently high, then the extent of any concentration gradient, and resulting open-circuit potential, will be minimal to non-existent.
The magnitude of the OCP response to the low-magnitude RH changes was also accurately predicted using the Nernst relationship of eqn (4). Fig. 5 plots both ΔOCP and ΔOCPN for the five OCP peaks (four increases and one decrease) from Fig. 4.
![]() | ||
| Fig. 5 Experimental values of the peak potential (ΔOCP) induced from low-magnitude RH changes (∼±0.25%) along with the thermodynamic predictions (ΔOCPN). | ||
The actual extraction or harvesting of this potential energy could occur in a number of ways. While Pattle's hydroelectric pile drove a direct current, others have utilized the phenomena to increase the charge stored in batteries or electrochemical capacitors.3,8,9 While the cell voltage is governed by the thermodynamics, the current output and resulting power produced are determined by the resistance of the cell.2,9 The humidity dependent equivalent series resistance (ESR) the cell is shown in Fig. 6. The ESR of electrochemical cells is dominated by the resistance of the electrolyte, and thus shows the strong humidity dependency expected from Nafion.10
![]() | ||
| Fig. 6 Humidity dependent equivalent series resistance (ESR) of the coaxial cell measured by electrochemical impedance spectroscopy. | ||
The extremely high resistance at low humidity levels would cause significant limitations in the power output and we recommend the use of polymer electrolytes with higher conductivities in low humidity environments to overcome this disadvantage. Nonetheless, we have measured the short-circuit current (Isc) to demonstrate the potential power output of the cell. Fig. 7 shows Isc results while cycling the humidity between 35% and 45% RH.
Multiplying the peak Isc of ∼600 nA for the increase from 35% to 45% RH by the peak OCP of ∼7.5 mV obtained for the same humidity change results in a maximum power of ∼4 nW. With a cell volume of ∼0.035 cm3, the peak volumetric power density is ∼0.13 W m−3. The peak Isc increased to ∼800 nA for the humidity increase from 45% to 55% (not shown), showing the effect of the humidity dependent resistance of Nafion (i.e. larger current due to lower cell resistance at the higher humidity levels). However, as previously discussed and illustrated in Fig. 2, the OCP decreases as you move into higher RH levels, and thus the results for the maximum power calculation for the 45% to 55% RH increase is only a few tenths of a nanowatt greater than that for the 35% to 45% RH change. This highlights the need to use a polymer electrolyte without the drastic increase in resistance at low humidity levels in order to investigate the capabilities and limitations of the energy harvesting performance.
The characteristics of the OCP response will be determined by the difference between the rate of change of the water content at one electrode and that of the opposite electrode. At the outer electrode, this change rate is determined by the rate of the humidity change, the absorption/evaporation rate and the rate at which water diffuses to/from the electrode. Since the coaxial electrode architecture shields the inner electrode from the surrounding environment, the rate of water diffusion through the electrolyte will determine the rate of change of the water content at inner electrode. Clearly, this inherently dynamic system has many contributing factors, including not only the properties of the electrochemical cell, but also the characteristics of the changing environmental conditions. Further systematic experimental and modeling studies will be required to fully describe the influential factors and the extent of each's impact on the cell's performance. Nonetheless, we have successfully demonstrated the concept, and provided initial studies that should prove useful in guiding future studies.
Just as R. E. Pattle introduced six decades ago with salinity concentration gradients from salt and fresh water, a measurable Gibbs free energy can be obtained from concentration gradients induced in ionic polymers by changes in water content at one electrode. One way to induce such local concentration changes is through changes in the relative humidity of the surrounding environment, and use of a coaxial electrode cell. The established electric potential is governed by the thermodynamics described by the Nernst relationship, and subject to various kinetic effects. The availability of this electrical potential to do work presents the possibility to engineer small, lightweight and flexible devices capable of energy harvesting or providing “self-powered” sensory/detection information. While the data was not shown in this report, we have successfully used a number of different sources to induce the open-circuit potential response, including dry gas flows along with changes in their flow rates, opening and closing of doors, and human breath.
In addition to the attraction for applications, the methods presented may prove useful for studying the fundamental properties of polymer electrolytes and the constituent components of such systems similar. Theoretically, a relatively small and finite amount of water molecules should only be needed (to be absorbed or evaporated) in order to induce a measurable energy change of the system. Such an approach may provide a novel route to perform studies on the solvation or transport properties that is complimentary to the traditional bulk measurement methods used to study these systems.
Footnote |
| † Electronic supplementary information (ESI) available. See DOI: 10.1039/c4ra05251j |
| This journal is © The Royal Society of Chemistry 2014 |