Shucheng Sunab,
Yu Xiaoa,
Dong Liangc,
Zhigang Shao*a,
Hongmei Yua,
Ming Houa and
Baolian Yia
aFuel Cell System and Engineering Laboratory, Dalian Institute of Chemical Physics, Chinese Academy of Sciences, 457 Zhongshan Road, Dalian 116023, PR China. E-mail: zhgshao@dicp.ac.cn; Fax: +86-411-84379185; Tel: +86-411-84379153
bGraduate University of the Chinese Academy of Sciences, Beijing 100039, PR China
cSunrise Power Co., Ltd., Dalian 116025, China
First published on 8th January 2015
Water starvation could be one of the reasons for proton exchange membrane (PEM) water electrolyzer degradation. In this paper, the water starvation phenomena of a unit cell in a PEM electrolyzer stack are investigated. The voltage, current density and temperature distribution are investigated in situ with a segmented electrolyzer. The results show that the voltage of the middle and outlet regions is higher than the inlet voltage, which illustrates that water starvation could occur simultaneously in different regions of the electrolyzer. The water stoichiometries have an important effect on the voltage distribution, current density distribution and temperature distribution at 0.5 A cm−2 and 60 °C. The electrochemical impedance spectra of different segments show that the cell resistance and charge transfer resistance gradually increase along the water flow direction when the water stoichiometry is 3. According to the flow regime map, the critical water stoichiometry for electrolysis is further discussed.
Improving water management in PEM is one of the most interesting topics for improving the efficiency and extending the operation of electrolyzer.
It is well known that the membrane humidification in electrolyzer is provided by the high flow of pumped water. When the flow rate of the circulating water (Q) is too high, the pressure drop increases and thus damages the membrane electrode assembly (MEA) by high hydraulic pressure.5,6 However, when the total water supplied to electrolyzer MEA is lower than the total water consumed in the single water electrolyzer, the water starvation would occur, namely the overall starvation.7 On the contrary, the local starvation would occur,8 which often results from uneven water distribution, inappropriate porous current collectors,9 high current density and high pressure operation.10
Water starvation often causes the inhomogeneous water distribution, which would lead to the inhomogeneous distribution of the voltage and current. Moreover, water starvation can cause the local drying of the membrane and “hot spots” in the electrolyzer, which would lead to the electrolyzer failure. Also, it has been shown that the conductivity of PEMs is directly related to the hydration state.10,11 As the water content in the membrane decreases, the higher ohmic losses can happen.
There are many studies on the subject focused on the novel oxygen evolution reaction (OER) electrocatalyst12,13 and metal cations poisoning.14,15 However, no publication is available concerning the characters of PEM electrolyzer under the water starvation. By means of investigating the behaviors under the water starvation, this work will help to identify the cause of the performance degradation and optimize the water amount for a water electrolyzer operation.
In this paper, the water stoichiometry (ξ) indicates the ratio of the circulated water amount to the consumed water amount for electrolysis at a definite current density, and the critical water stoichiometry (ξ*) is namely the ratio, above which a PEM water electrolyzer just operate stably. The behaviors of a PEM electrolyzer under water starvation were in situ investigated. Potential sensors, mini-size thermocouples and segmented electrolyzer were adopted to identify the voltage, temperature and current density distribution under different water stoichiometry. At last, the superficial velocities of gas–liquid two-phase flow were calculated, and the critical water stoichiometry was further explained.
Fig. 1 showed the schematic of test station. The DC power source (KIKUSUI PAT60-133T) provided an voltage on the water electrolyzer. The value of the DC voltage was in the range of 0–2.4 V for the paper.
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Fig. 1 Schematic diagram of test station for PEM water electrolysis. (1) water tank; (2) power supply; (3) water electrolyzer; (4) micropump; (5) circulating water pump; (6) heat exchanger. |
The water electrolyzer was kept at 60 °C and atmospheric pressure during operation. The electrolyzer temperature was controlled by adjusting the temperature of the circulating water through the cathode bipolar plate. The deionized water (Milli-Q, 18.2 MΩ cm) was fed into the anode side of the electrolyzer by a micropump (SYLTECH 510 Prep Hd, USA). Water starvation was made intentionally by adjusting the water flow rate, so that the behaviors of the single electrolyzer under water starvation could be investigated. The produced oxygen was evacuated from the anode upside of electrolyzer, whereas the produced hydrogen and water were evacuated from the cathode upside of electrolyzer.
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Fig. 2 Schematic sketch of the detailed places of voltage sensors: (a) three voltage sensors on the surface of anode catalyst layer; (b) two voltage sensors on the surface of cathode diffusion layer. |
The RHE was connected with normal reaction region through proton exchange membrane. The anode and cathode voltage sensors used in this study was made of platinum and copper wires with insulating paint outside, respectively. The diameter of the wires was 0.08 mm. At the end of each voltage sensor being placed on the measured regions, the insulating paint was removed for about 2 mm. Thus, the local voltages could be indicated by the voltage sensors. Because the high purified hydrogen (99.99%) was fed into the anode and cathode side at a flow rate of 50 ml min−1, respectively, the potential of RHE and cathode was assumed to be stable and zero. However, the potential difference between the cathode and the RHE existed, which was used as a modified coefficient of the cathode reference. The mean value of the inlet and outlet potential of the cathode side could be taken as a reference potential. The local voltages of inlet region, middle region and outlet region on anode (hereinafter referred as inlet, middle and outlet, respectively) against the reference were measured and recorded automatically.
The MEA was specially designed as displayed in Fig. 3. The anode electrode was segmented, the active area of each segment was 4.5 cm2, and the total active area was 49.5 cm2. The segments were numbered from 1 to 5 along the direction of water flow. Segment 1 and 5 were individual segment, whereas each of segment 2, 3 and 4 included three segments, respectively, as shown in Fig. 3. The cathode effective area was 160 cm2 with normal structure. The preparation process of MEA was the same as our previous paper.16 A carbon paper (Toray, Φ 145) and eleven porous titanium disks (Φ 24) electroplated Pt were used as the current collector for cathode and anode of MEA, respectively. Fig. 4 showed the specially made anode current collecting end plate, in which eleven titanium blocks electroplated Pt were embedded corresponding to the segmented MEA. Eleven copper sticks were connected with eleven titanium blocks. The organic glass end plate was carved into parallel channels, the cross-section of the channel was rectangle (0.4 mm × 0.8 mm) and 0.0032 cm2 in area, and the number of the flow channels was 80. In the electrolyzer set-up, the water flow was vertical upward in the parallel flow field. When current distribution was investigated, the electrolysis current was kept at 24.75 A, and the current density was 0.5 A cm−2 with regard to the total effective area of anode.
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Fig. 3 Structure of the segmented MEA ((a) segmented anode; (b) proton exchange membrane; (c) cathode; (d) plastic frame). |
Fig. 6 shows the voltage difference between outlet and inlet corresponding to Fig. 5. When the water stoichiometry decreases from 8 to 3, the voltage difference is almost constant (ca. −12 mV). However, when the water stoichiometry varies from 3 to 1.5, the voltage difference between outlet and inlet dramatically increases, which approximately increases from −10 mV to 22 mV. The phenomena display that at low water stoichiometry (ξ < 3), the water supply could not meet the demand for the overall MEA, and the water amount decreases down the water flow direction. The water content in the membrane has a more significant effect on ohmic resistance.18,19 Therefore, Fig. 5 and 6 show the membrane water content near the water outlet is quite insufficient for operation at 0.5 A cm−2 when ξ < 3, which increases the outlet voltage to a large extent, and thus it causes the increase of the total voltage.
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Fig. 6 The voltage difference between outlet and inlet relating to Fig. 7. |
In order to observe obviously the voltage distribution in electrolyzer, the water stoichiometry (ξ = 2.5) was selected.
Fig. 7 displays the voltage distribution inside PEM water electrolyzer under different current densities at fixed water stoichiometry of 2.5 (with regard to the current density 0.1, 0.3, 0.5, 0.6 and 0.8 A cm−2, respectively), and the water flow rate corresponds to 0.23, 0.68, 1.13, 1.35 and 1.8 ml min−1, respectively. It can be seen that the voltage distribution becomes more non-homogeneous with the increase of current density. For the current densities from 0.1 to 0.5 A cm−2, the voltages of middle and outlet are only slightly lower than that of inlet, which is attributed to the slightly lower temperature at water inlet. However, when the current density is above 0.5 A cm−2, the voltages of middle and outlet are obviously higher than that of inlet, and that of outlet is the highest. We can obviously see the phenomenon in Fig. 8, which is a plot of the voltage difference between outlet and inlet corresponding to Fig. 7. As shown in Fig. 8, when the current density is above 0.5 A cm−2, the voltage difference between outlet and inlet increases dramatically. The outlet voltage is even 33 mV higher than that of inlet at 0.8 A cm−2.
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Fig. 7 Voltage distribution under different current densities at fixed water stoichiometry of 2.5 (with regard to the current densities 0.1, 0.3, 0.5, 0.6 and 0.8 A cm−2, respectively). |
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Fig. 8 Voltage difference between outlet and inlet relating to Fig. 7. |
This may be attributed to the insufficient amounts of water supplied to the anode. Water amount at anode inlet is the most highest in membrane and decreases along the water flow direction when water stoichiometry is 2.5. Therefore, the drying of membrane near the water outlet occurs at high current density (ca. above 0.5 A cm−2), which will lead to the increase in the local ohmic resistance.
As the water stoichiometry is equal to or less than 3, the temperature distribution becomes more heterogeneous. It indicates that the water amount is insufficient to remove the produced heat, the local hot spot in the electrolyzer would be produced, which is likely to cause the local degradation of the MEA.
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Fig. 11 Electrochemical impedance spectra of different segments under water stoichiometries: a = 10; b = 3. |
Segments | RΩ (Ω cm2) | Rct (Ω cm2) | ||
---|---|---|---|---|
ξ = 3 | ξ = 10 | ξ = 3 | ξ = 10 | |
1 | 0.492 | 0.490 | 0.243 | 0.244 |
2 | 0.504 | 0.490 | 0.252 | 0.244 |
3 | 0.531 | 0.509 | 0.239 | 0.234 |
4 | 0.581 | 0.491 | 0.319 | 0.242 |
5 | 0.720 | 0.500 | 0.360 | 0.246 |
So we can deduce that the water amount for ξ = 10 has a little influence on RΩ and Rct, whereas for ξ = 3, the performance near the exit of electrolyzer has deteriorated at 0.5 A cm−2 and 60 °C. This coincides with the results in Fig. 6 and 9.
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Fig. 12 Flow regime map expressed by superficial velocity of gas (jG) and liquid (jL) presented by Cubaud and Ho.23 Symbols indicate our calculated velocities in the channel of PEM electrolyzer at 0.5 A cm−2 and 60 °C for different segments. |
The flow regime changes depending on the mass flux, quality, or superficial velocity of each phase.5,24 Quality fraction (x) inside the two-phase flow is defined at an arbitrary location along the channel as follows:
![]() | (1) |
The superficial velocities of the gas and liquid (jG and jL) can be calculated as follows:
![]() | (2) |
![]() | (3) |
The x can be calculated by the total mass balance through the anode channel in eqn (3). Table 2 summarizes the detailed definitions of Gcirc, GO2, Gcons and Gdrag. The jG and jL at the channel of different segments can be calculated using eqn (2) and (3).
Parameter | Equation |
---|---|
Gcirc | ![]() |
GO2 | ![]() |
Gcons | ![]() |
Gdrag | ![]() |
ndrag | 0.016T − 2.89556 (ref. 25) |
When the water stoichiometry (ξ) is equal to 10 at 0.5 A cm−2 and 60 °C, segment 3–5 have located in annular area, as shown in Fig. 12b. Although the diffusion impedance exists for ξ = 10 (Fig. 11a), the MEA should be wet under annular flow so that the electrolyzer can operate having no loss in performance (Fig. 9).
However, when ξ = 3, segment 3, 4 and 5 of electrolyzer have obviously located in dry area (Fig. 12a). However, this conflicts with the critical water stoichiometry (ξ*) to some extent. The difference may result from two causes. Firstly, the flow regime map is based on the assumption that the membrane is in contact and in equilibrium with liquid water on both sides of the electrolyzer. Secondly, the electro-osmotic drag coefficient varies within a wide range, depending on the degree of membrane hydration in contact with liquid water.26 For ξ = 3, the water content of membrane is in nonequilibrium with liquid water, and the electro-osmosis drag coefficient (ndrag) should be less than 2.43 (ref. 23) at 0.5 A cm−2 and 60 °C. Moreover, the back-diffusion water from the cathode may compensate for the electro-osmotic dragged water, which would lead to the net water transport from the anode to cathode decrease.27 As a result, Fig. 12 differs from described above results to some extent.
Consequently, the critical water stoichiometry (ξ*) is obtained for a PEM electrolyzer at 60 °C and 0.5 A cm−2, ξ* is about 3. A PEM water electrolyzer could operate normally on condition that the water stoichiometry is more than ξ*. In addition, heat dissipation in a PEM water electrolyzer also becomes a limiting factor under water starvation. This point also proves that the circulating water does not only act as reactant, but functions as cooling water. Therefore, a heat balance between the heat generation capacity and the ability of the heat dissipation must be considered in some cases of a large cell/stack. In addition, low humidity and high temperature may lead to the membrane degradation such as thermal degradation, mechanical stress, and chemical attack28 during the water starvation.
ξ | Water stoichiometry |
ξ* | Critical water stoichiometry |
Q | Flow rate of circulating water, ml min−1 |
a | Cross-sectional area of flow channel, cm2 |
F | Faraday constant = 96![]() |
G | Mass flow flux in channel, kg m−2 s−1 |
nchan | Number of channels in flow field |
ndrag | Electro-osmosis drag coefficient |
Rct | Charge transfer resistance |
Rd | Mass-transport resistance |
GO2 | Mass flux of produced oxygen gas |
Gcons | Mass flux consumed by the anode reaction |
Gdrag | Mass flux of the water dragged by electro-osmosis |
A | Electrode surface area, cm2 |
T | Cell temperature, K |
x | Quality fraction |
ρL | Liquid density, kg m−3 |
ρG | Gas density, kg m−3 |
j | Superficial velocity, m s−1 |
i | Current density, A cm−2 |
M | Molar weight, kg mol−1 |
RΩ | Cell resistance |
Cdl | Double layer capacitance |
Gcirc | Mass flux of circulating water |
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