Supplementary Information Multiphysics of Ionic Polymer Metal Composites Actuator Zicai Zhu1,2, Kinji Asaka3, Longfei Chang1,2, Kentaro Takagi4 and Hualing Chen1,2* 1 State Key Laboratory of Mechanical Structure Strength and Vibration, Xi’an Jiaotong University, Xi’an, 710049, PRC 2 School of Mechanical Engineering, Xi’an Jiaotong University, Xi’an, 710049, PRC 3 Health Research Institute, National Institute of Advanced Industrial Science and Technology (AIST), Ikeda, Osaka 563-8577, Japan 4 Nagoya University, Furo-cho, Chikusa-ku, Nagoya 464-8603, Japan * To whom correspondence should be addressed. E-mail: hlchen@mail.xjtu.edu.cn A. Blocking effect of electrode In Fig. 5, the moment balance equation is, F1 tw te M1 2M 2 M 0 . (A1) Where te and tw are the thickness of the electrode and the total IPMC respectively. As te<<tw , the moment M2 in electrodes can be ignored. Then we have, F1tw M1 M 0 . (A2) Using the linear strain xx in Eq.Error! Reference source not found., M1 can be figured out as, M 1 ENW xx hydy. (A3) Where ENW is the effective elastic modulus of the wet substrate membrane, h is the width of the cantilever. And the strains are continuous at the contact surface between the electrode and the substrate, so we get, F1 M 1 tw . hte EPd ENW I1 2 (A4) Where EPd is the effective elastic modulus of the electrode, I1 is the area moment of inertia of the substrate. The deformation under the bending moment M0 will be much larger than that under the moment M1 because of the blocking force F1. The electrode effect is equivalent to an external mechanical load, the blocking moment F1tw. M ext F1tw 6hte EPd xx ydy tw (A5) Then the corresponding elastic stress is, eB M ext y I1 (A6) B. Electrostatic stress According to the effective electrical field theory, the total electric field influenced the local electrostatic stress in an ionic cluster is the sum of three electric fields, Ee induced by electrons in the electrodes, Eout induced by the redistributed ionic charges excluded the local cluster and Ein induced by the ionic charges in the local cluster. The directions of Ee and Eout are along the thickness, so they cause the cation migration and have little contribution to the local electrostatic stress. Then the electrostatic stress in a cluster is mainly decided by the ionic charges in it. Based on the RVE model, the total charge of cations in a cluster is, 4 1 Q cI F VS VW cI F r 3 1 3 wV (A7) If the cations distribute uniformly in the pore as in Fig. 6(a), the volume density of the positive charges is, Q 1 cI F 1 VW wV (A8) If the cations distribute uniformly on the liquid/solid surface as in Fig 6(b), the surface density of the positive charges is, Q r 1 cI F 1 2 4 r 3 wV (A9) For the fixed anion charges, the total charge is, Q c F VS VW 0 c F 4 r 3 1 1 3 1 V wV (A10) So the surface density of the negative charges is, Q r 1 c F 1 2 4 r 3 1 V wV (A11) For the electric charge system composed of positive charges in Eq. (A8) and negative charges in Eq. (A11), the total electrical energy of the charge system is, W 4 r 3 2 r 2 3 r 2 3 W 5 2 (A12) 2 3 Q 2 Q Q Q 4 W r 5 2 1 Where W is the dielectric constant of water. Using the electric energy we can calculate the electric force on the outer surface of the electric charge system, i.e. the liquid/solid surface. 2 2 Q 1 3Q W Fer Q Q 2 2 r Q ,r 4W r 5 (A13) And the electrical stress is, 2 2 c Fer r0 2 F 2 wV 3 1 3 2 c pe1 cI cI 1 4 r 2 9W wV 0 wV 5 1 V 2 1 V 2 2 (A14) For the electric system composed of positive charges in Eq.(A9) and negative charges in Eq. (A11), the electrical stress is, 2 2 r 2 F 2 wV 3 1 c pe 2 0 1 c I 18W wV 0 wV 1 V 2 (A15) C. Model simplification Dimensionless method is used to simplify coefficients for the comparison. A few characterized parameters are presented for the dimensionless model as follows: Length scale: ls Time scale: ts RT F 2c RT d II F 2 c . . Voltage scale: Vs RT . F Pressure scale: Ps RT . VW Concentration scale: cs c . For the water based IPMC, the voltage scale is about 25.85mV, the pressure scale is about 138.57MPa, while the others are dependent on the IPMC properties. Furthermore three ratios are also presented, Initial water number: cW 0 c Ratio of diffusion coefficients dWW d II Ratio of hydraulic permeability coefficient KPs dWW The ratio of hydraulic permeability coefficient means the ratio of the convection flux to the diffusion flux induced by the same pressure gradient. For Nafion based IPMC, usually the concentration and mobility of water are larger than that of cation in IPMC, then and are both larger than 1, and the convection flux is no less than the pressure induced diffusion flux, is no less than 1. Using *Vs , cI cI *c , cW cW *c , p p* Ps , xi xi*ls and t t *t s (the variable with a superscript * is the corresponding dimensionless form), then the transport equation system including Eq. Error! Reference source not found., Error! Reference source not found., Error! Reference source not found. and Error! Reference source not found. can be transformed to, 2 * 1 cI * ; VI * * cI * * * * * * * * * c zc c p n c c p c p I I I dI W W I t * V W c * (A16) VI * * cI p cW *p* W* cW * cW *p* ndW cI * zcI * * VW t N p* pi* i 1 For Nafion based IPMC, usually the concentration and mobility of water are larger than that of cation in IPMC, then and are both larger than 1, and the convection flux is no less than the pressure induced diffusion flux, is no less than 1.The partial molar volume of cations are far less than that of water, so VI VW 1 , then the diffusion terms of cation induced by the pressure can be ignored. Compared the convection flux with diffusion flux induced by the pressure in the water equation, the former is larger than the later ( 1 ) even if we use the smaller hydraulic permeability measured by Evans. And in experiments we can not distinguish the convection from the pressure diffusion flux, it means the hydraulic permeability is obtained from the sum of the two fluxes. So we keep the convection term and ignore the pressure diffusion term in the final form. Then we get a simplified equation as, cI z Fc d II cI I I ndI dWW cW cI K p . RT t cW d c n d c z I FcI c K p . dW II I W WW W t RT (A17) However, the cluster size will change when the water content declines. Smaller radius of the cluster can make the convection flux reduce greatly. Then the pressure diffusion turns to be the dominant mechanism, so the following form is also right in some occasions, cI z Fc d II cI I I ndI dWW cW cW K p . RT t cW d c c K p n d c z I FcI . dW II I WW W W t RT (A18) When 1 , equation (A18) turns to be the case dominated by the pure diffusion mechanism. Although Eq. (A17) and Eq. (A18) are different on the pressure term, numerical results of them are almost the same. D. Cation and water distribution along the thickness varied with time (1) Model B. The concentrations of the cation and water along the thickness varied with time of Model B (ndw=4) are shown in Fig. A1 (Thickness axis 0: Cathode, 2×10-4m: Anode). In Fig. A1(a) cations accumulate near the cathode quickly after applying the electrical stimulation. The highest steady concentration can achieve 40 times of the average. When shorting the electrodes, the cations at the cathode quickly go back to the anode. In Fig. 8(b) water concentration also rises up quickly at the cathode and falls at the anode. The concentration difference between the highest and the lowest is no more than 15% of the average concentration. After the maximum concentration point at the cathode, water concentration decreases with time slowly due to the concentration diffusion. It will take tens of seconds for all the stored water to go back to the anode and recover the initial state. When the electrodes are shorted, the water molecules firstly accumulate near the anode, and then also diffuse back to the initial state. (a) Cation distribution (b) Water distribution Fig. A1 Model B: Concentration distribution along the thickness varied with time (2) Model C. The dynamic process of the cation distribution along the thickness is similar to the result in Fig. A1(a) of Model B. While that of the water distribution is quite different from Fig. A1(b) and is shown in Fig. A2, the water is not highly concentrated in the cathode any more, and the profile of the water concentration is almost linear with the thickness. Fig. A2 Model C: Water distribution along the thickness varied with time (3) Model D. For a specific case ndw=4, nhy=3, the dynamic distribution processes of the cation, the free water and the total water are illustrated in Fig. A3. Compared Fig. A3 (a) with Fig. A1 (a), the steady cation concentration at the cathode of the former is much lower, only about 5 times of the average concentration in the bulk. In Fig. A3 (b) the free water distribution along the thickness shows a contrary trend compared with the distribution of the cation and the later total water. Much free water is driven to the anode after applying the stimulation. In Fig. A3 (c), in the bulk the total water concentration profile still displays a uniform gradient across the thickness and agrees with the experimental results of the neutron imaging. While in the two electrode boundaries, especially in the cathode, the total water concentration shows a sudden change. It is caused by the distribution of the hydrated water concentration that is much high in the cathode and low to zero in the anode. (a) Cation distribution (b) Free water distribution (revised thickness direction) (c) Total water distribution Fig.A3 Model D: Cation and water distribution along the thickness varied with time