Yujia
Gao†
a,
Dongxu
Lin†
ab,
Pengyi
Liu
a,
Tingting
Shi
*a and
Weiguang
Xie
*a
aSiyuan Laboratory, Guangzhou Key Laboratory of Vacuum Coating Technologies and New Energy Materials, Guangdong Provincial Engineering Technology Research Center of Vacuum Coating Technologies and New Energy Materials, Department of Physics, Jinan University, Guangzhou 510632, China. E-mail: wgxie@email.jnu.edu.cn
bSUSTech Energy Institute for Carbon Neutrality, Department of Mechanical and Energy Engineering, Southern University of Science and Technology, Shenzhen 518055, China
First published on 9th November 2023
In recent years, significant progress has been made in the application of perovskite materials in the field of photovoltaics. However, their stability is still affected by the presence of water molecules. Investigating the interaction mechanism between water and perovskites is of great importance for enhancing their stability and advancing commercialization. This review, based on theoretical calculations, summarizes the mechanisms underlying the interaction between water and perovskites. These mechanisms encompass water molecule diffusion, perovskite decomposition induced by a high concentration of water, phase transitions, as well as the dual impact of water on defects. Furthermore, it discusses the influence of water on the quality and performance of perovskite devices in experimental settings. By comprehensively elucidating the theoretical mechanisms governing the interaction between water molecules and perovskites, this review offers both a theoretical foundation and practical guidance for enhancing the stability and optoelectronic performance of perovskite photovoltaic devices, while also facilitating further exploration of the underlying mechanisms.
Currently, most of the existing reviews on the influence of water on perovskite materials predominantly approach the subject from an experimental perspective. These reviews encompass the effects of water on perovskites, including degradation mechanisms,18–20 impacts on thin film quality and device performance,19,21,22 as well as strategies to enhance humidity stability.23–26 However, comprehensive summaries regarding theoretical computational investigations on the subject are scare. With this goal in mind, we primarily summarize the theoretical and computational studies on the physical and chemical processes between perovskites and water. Scheme 1 summarizes the main interactions between water and perovskites, along with the resulting outcomes of these interactions. Generally, the dominant interaction between perovskites and water is the hydrogen bonding between water molecules and organic cations as well as the inorganic framework, and the consequences of this interaction are closely related to the amount of water or the molar ratio of water to perovskites. In the case of trace amounts of water, water molecules tend to adsorb on the perovskite surface and undergo short-range diffusion, while in the presence of a large amount of water, excess water molecules diffuse to deeper positions and cause structural distortion of perovskites. The presence of surface defects promotes water adsorption and diffusion, but during the fabrication process, water can passivate defects and enhance film quality. Furthermore, a certain amount of water affects the energy barriers for the phase transition of the FA-system and Cs-system, thus influencing the material's phase transition behavior. In this review, we discuss the interaction mechanisms between water and perovskite ions as well as defects, and explore the effects of these mechanisms on perovskite materials.
In terms of the model for water on the perovskite surface, it is necessary to consider different surfaces, primarily encompassing two types as illustrated in Fig. 1. One is the AX-terminated surface represented by the blue and orange regions, and the other is the MX2-terminated surface represented by the green region. When studying the interaction between a single water molecule and the perovskite surface, the specific adsorption site needs to be taken into account. For AX-terminated surfaces, the potential adsorption sites for H2O can be chosen as near A+ or X−. For MX2-terminated surfaces, the potential adsorption sites for H2O can be chosen as near M2+, the M–X bond, or above A+. Previous studies have employed the calculation of adsorption energy, Eads = Esurface − H2O − (Ebare-surface + EH2O), to determine the most favorable adsorption configurations. For both AX-terminated and MX2-terminated surfaces, the specific Eads with different atomic species at each site are shown in Table 1. For AX-terminated surfaces, when considering the polarity of the MA+ species in the MA+-system, the lowest adsorption energy is obtained when a single H2O molecule is positioned near X− above the surface with the –NH3 moiety of MA+ pointing towards the surface.27,28 For MX2-terminated surfaces, the lowest adsorption energy is obtained when a single water molecule is positioned above M2+ with the –CH3 moiety of the surface MA+ pointing towards the surface. In both cases, when A, M, and X are different ions, the adsorption energies are negative, indicating that water readily adsorbs onto the perovskite surface.29
The lowest Eads (eV) | ||
---|---|---|
AX-terminated | MAI | −0.48 |
FAI | −0.32 | |
CsI | −0.19 | |
MABr | −0.48 | |
MX2-terminated | PbI2 | −0.51 |
SnI2 | −0.44 | |
PbBr2 | −0.50 |
Furthermore, for the M-site cations, common examples include Pb2+, Sn2+, and other metal cations. Calculations have revealed that the interaction between H2O and M-site cations differs from the hydrogen bonding interaction with the A-site. H2O interacts with the M-site ions through a combination of covalent and ionic interactions. Due to the closer electronegativity between Pb and I, the ionic interaction between H2O–MAPbI3 is stronger than H2O–MASnI3.27 Guo Xie et al. conducted a comparative analysis of the impact of H2O on MASnI3 and MAPbI3, and found that H2O has a significant influence on the Sn–I bonds on the surface of MASnI3, suggesting that, in a H2O atmosphere, MAPbI3 is more stable than MASnI3.29 This conclusion contradicts the stability analysis based solely on adsorption energy, emphasizing the necessity in practical research to consider multiple factors rather than relying on a single energy-based indicator to assess structural stability. On MI2-terminated surfaces, the O of H2O forms an O–M bond with the M2+ acceptor due to its lone pair of electrons. Other factors such as light illumination also influence the interaction between H2O and M2+. Lu Ying-Bo et al. found that above-band-gap light illumination of MAPbI3 induces a significant photo-induced lattice expansion effect, increasing the electron density around Pb2+ and enhancing the bonding interaction between H2O and Pb2+.35
Lastly, regarding the X-site anions, on AX-terminated surfaces, the H of H2O forms an H–X hydrogen bond with the adjacent X−.31 On MX2-terminated surfaces, Shuxia Tao suggests a covalent interaction between H2O and X−,27 while Bin Hu suggests that the interaction between I− on the (011) surface and the H of H2O is close to an ionic bond.29 The electronic density of the H–I bond is 0.05, indicating a relatively weak covalent interaction, and the H and I− form an antibonding state. However, regardless of the specific bonding analysis, the conclusions regarding Br− and I− are consistent, indicating that the interaction with Br− is weaker than with I−.27,36 Due to the weaker adsorption characteristics of H2O on Br−, experimental studies have improved the humidity stability of solar cells by partially replacing I− with Br−.37 Weiguang Zhu et al. investigated the dissolution and degradation mechanisms of isomorphous Cs2SnCl6 and Cs2SnI6 in direct contact with water. Cs2SnI6 undergoes direct dissolution in water, decomposing into CsI and SnI4, leading to the formation of an intermediate hydrolysis product, Sn(OH)4. In comparison to Cs2SnI6, Cs2SnCl6 exhibited greater stability and formed a smaller quantity of amorphous phase due to their different interaction with water molecules. The authors attribute this behavior to the smaller ionic radius of chloride, with chloride having a higher ionic potential than iodide, thereby forming stronger atomic bonds.38
Fig. 2 (a) Imaginary typical structure of three-layer (001) surface containing water named O1F1S1. The colored regions in the surface divisions of MAI-terminated (left) and PbI2-terminated (right) represent the possible locations of water molecules and are named O, F, and S, respectively. Reproduced with permission (left figure).39 Copyright 2015, American Chemical Society. (b) An illustration showing water adsorbed in the (i) O (O5) region, with water residing in the inner regions ((ii) F5 and (iii) F4S1). Reproduced with permission.39 Copyright 2015, American Chemical Society. (c) Snapshots of the key steps for a few water molecules absorbed on MAI-terminated (i) and PbI2-terminated surfaces (ii). Reproduced with permission.40 Copyright 2016, Royal Society of Chemistry. |
Firstly, regarding MAPbI3, whether a single water molecule can diffuse from its surface to the interior was investigated through computational simulations, and the answer to this question is affirmative. Specifically, it was observed that the energy of the system when H2O is in region F is lower than when it is in region O, indicating that H2O tends to stay energetically favorable on MAPbI3. Simultaneously, the diffusion barrier from region O to F is merely 0.04 eV, suggesting a highly facile process with minimal resistance. This behavior can be attributed to the unique structural characteristics of MAPbI3, featuring a large framework composed of Pb and I atoms with relatively spacious interstices, despite the presence of organic MA+ molecules. Furthermore, H2O diffuses from region F to region S, with a diffusion barrier of 0.31 eV, slightly higher than the barrier from O1 to F1, yet still relatively small, thereby providing the opportunity for water molecules to diffuse from region F to region S. Additionally, compared to water molecules in region F, those in region S exhibit a lower system energy. During this process, H2O needs to overcome the [PbI6]4− framework. Throughout this entire process, due to the interaction between O in H2O and HN in MA+, the orientation of MA+ in regions F and S changes as water molecules diffuse.38 Koocher Nathan et al. discovered through simulations that on the PbI2-terminated surface, as the –NH3 groups in MA+ in region S are directed towards the surface, water molecules begin to stay within the plane. O interacts with the HN in MA+ in region S through hydrogen bonding, while the two HW atoms interact with the surface I−. The penetration of H2O increases the cavity size, weakening the octahedral rotation due to the interaction between O and HN, thereby opening adjacent hollow spaces.28 This indicates that water adsorption beneath the surface has a collective influence on neighboring structures. Once H2O fully enters region S, strong hydrogen bonds form between O and HN, and the barrier for this process is smaller than that for the reverse process, indicating that once H2O molecules penetrate the hollow sites, they cannot easily leave.
As the number of water molecules increases, how does the diffusion model differ from that of a single water molecule? For MAPbI3, simulation studies have found that under high humidity conditions, whether on the MAI-terminated or PbI2-terminated surfaces, water molecules exhibit strong adsorption at all sites, with hydrogen bonding interactions forming between water molecules.
Firstly, for the MAI-terminated surface, similar to the case of a single water molecule, when water molecules are located in region O, as depicted in Fig. 2(b)(i), the hydrogen bonding interaction between water and MAPbI3 is weak, and there is no significant structural change after water adsorption. Subsequently, water molecules diffuse to region F, as shown in Fig. 2(b)(ii), where the interaction between water and MAPbI3 strengthens, leading to disruption of the perovskite structure in region F. Occasionally, certain water molecules can further diffuse to region S, disrupting the structure of region S, as shown in Fig. 2(b)(iii). From an energy perspective, compared to region O, H2O tends to stay in region F. The changes in MA+ positions and the distortion of Pb–I bonds in region F increase with increasing n. The oxygen atom (O) of H2O forms strong bonding with the remaining exposed Pb, breaking the Pb–I bonds until the structure of region F is completely disrupted. Driven by the high coverage of water molecules, they can further diffuse from region F to S, causing greater distortion of Pb–I bonds.39 Similarly, Lei Zhang et al. using ab initio molecular dynamics (AIMD) simulations, found that the presence of H2O on the MAI surface within MAPbI3 not only altered the orientation of MA+ but also led to larger fluctuations in Pb–Pb distances and dihedral angles, as illustrated in Fig. 2(c)(i). This indicates that the MAI surface lacks chemical stability due to interactions with water molecules. Furthermore, by extracting snapshots from the AIMD trajectories, it was observed that over time, the ordered structure of the outermost layer of the MAI-terminated surface was disrupted, resulting in a relatively wide diffusion range of water molecules on the surface.40
For the PbI2-terminated surface, some simulation results differ from the MAI-terminated case. Although H2O exhibits strong interactions with the surface's Pb2+, the PbI2-terminated surface does not undergo decomposition, as illustrated in Fig. 2(c)(ii). This might be attributed to the PbI2-terminated surface possessing the shortest and consequently strongest Pb–I bonds. A few individual water molecules may enter region S, forming hydrogen bonds with MA+ and becoming trapped within the cavity for the remaining simulation time. However, during this process, the inorganic framework of the perovskite undergoes only slight deformation while maintaining its integrity. Yet, when a certain quantity of water molecules accumulates in region S, the perovskite lattice elongates perpendicular to the surface. This suggests that higher water concentrations could weaken the interlayer binding strength in halide perovskites, thereby promoting the decomposition of MAPbI3.40 As the quantity of water molecules further increases, decomposition also occurs on the PbI2-terminated surface. Claudia Caddeo et al.'s simulation results of water and MAPbI3 interactions reveal that at a 75% water coverage rate on the MAI surface, an I atom is attracted and lifted from the surface by surrounding H2O molecules.41 This forms a hydrogen bond network between water molecules and surface I atoms, causing each molecule's hydrogen bond donor count to approach its ideal value.42 Consequently, Pb–I bond rupture occurs, enabling two water molecules to infiltrate the crystal interior, marking the first step of water degradation.
Lu Ying-Bo et al. discovered that under light illumination, the lattice of MAPbI3 undergoes expansion due to the photo-induced lattice expansion effect, resulting in an increase in the Pb–I–Pb angles. This expansion reduces the hydrogen bonding interactions between the organic and inorganic components. It is well-known that the hydrogen bonding interactions between the [PbI6]4− framework and the MA molecules maintain the unique structure of MAPbI3.35,43 Therefore, when water molecules penetrate into the interior of MAPbI3 under light illumination, they encounter weaker resistance compared to non-illuminated conditions. In experimental studies, Nurul Ain Manshor et al. compared the air stability of MAPbI3 stored at >70% humidity under dark and light conditions.44 It was found that exposure to humidity in the dark also led to slight decomposition of the perovskite into its initial precursors. When exposed to light, the thin film exhibits a degradation rate over 10 times higher in the presence of humidity. This further underscores that the larger voids within the perovskite structure are also one of the contributing factors enabling water molecules to penetrate the interior of the perovskite.
Dong Xu et al. investigated the neighbor interactions in MAPbI3 using natural bonding orbital (NBO) analysis and identified two main types of neighboring interactions: (1) (interaction between the lone pair of I atom and the antibonding orbital of H–N bond) and (2) (interaction between the lone pair of I atom and the antibonding orbital of H–C bond).45 The stability energy of stereoelectronic interaction (1) is approximately 19 kcal mol−1, which is significantly higher than the stability energy of interaction (2). Upon encountering a water molecule, the weaker donor–acceptor interaction (2) within the MAPbI3 molecule is disrupted, and the two stereoelectronic interactions (1) are weakened, with the stability energy decreasing from ∼19 kcal mol−1 to ∼13 kcal mol−1. Furthermore, two additional interactions are established between MAPbI3 and water molecules: (3) and (4) . The stability energy of the donor–acceptor interaction (4) between the lone pair of O atom in water and the antibonding orbital of N–H bond in the organic MA unit is 21.8 kcal mol−1, which is significantly higher than the stability energy between PbI3 and MA units. As a result, the presence of a water molecule decreases the stability of MAPbI3. Although one water molecule weakens the interactions between [PbI6]4− and MA units in MAPbI3, the structure of MAPbI3 is not completely destroyed. However, when two water molecules encounter a MAPbI3 molecule, the hydrogen bonds between [PbI6]4− and MA units are almost broken. The interaction (4) between the MA unit and H2O is much stronger than the interaction between [PbI6]4− and MA units, resulting in the complete decomposition of MAPbI3. Kakekhani Arvin et al. suggested that the polarization of water's lone pair induces more electron charge density closer to the proton-like H*N, leading to its interaction with the HN group on MA+.32 This interaction, in addition to hydrogen bonding, has a small covalent component manifested as a slight charge transfer from water to MA+. For a relatively low concentration of H2O:MA = 0.25, the water is oriented such that most of the highest occupied molecular orbital (HOMO) lone pairs interact with the H*N, lowering the system's energy, while hydrogen bonding exists between H2O and nearby I− anions. At this point, water causes some distortions in the lattice structure. When the ratio of H2O:MA ranges from 0 to 1, each H2O molecule binds to the –HN on MA+. Initially, each H2O perturbs (distorts) the inorganic framework to maximize hydrogen bonding attraction with I− and minimize electrostatic repulsion between O-2p lone pairs and I−. At H2O:MA = 1, as shown in Fig. 3(a), two water molecules form hydrogen bonds with each other, creating a connecting chain of (H2O–MA–H2O–H2O–MA), while the fourth water molecule interacts with two adjacent MA+ ions. At high water concentrations (H2O:MA > 1), due to continuous distortion of water molecules in the presence of MAPbI3, the system reaches an energetically favorable point for Pb bonding upon embedding. This results in the structure with broken octahedra becoming the actual ground state when sufficient water is present. Adequate water molecules form strong bonds with the ionic components of MAPbI3 and stabilize this distorted structure through a network of hydrogen bonds with other H2O molecules, as shown in Fig. 3(b). Experimental observations also indicate that MAPbI3 films are stable in dry air with humidity at or below 15%. However, in air with humidity as high as 60%, degradation can occur. During the degradation process, water initially decomposes MAPbI3 into crystalline MAI and PbI2, followed by the transformation of crystalline MAI into its amorphous form.
Fig. 3 (a) and (b) Ground state water structure for different H2O:MA concentrations. Color code is O (red), H (white), C (black), N (green), I (brown), and Pb (dark gray). Reproduced with permission.32 Copyright 2019, American Institute of Physics. (c) Water molecule bound to the PbI2-terminated perovskite slab showing the formation of the Pb–O bond. (d) Water molecule infiltrated within the MAPI crystal showing the formation of the H–O link between the methylammonium and water. Red is O, white is H, pink is I, dark gold is Pb, cyan is C, and blue is N. Reproduced with permission.41 Copyright 2017, American Chemical Society. |
In contrast to liquid water, the case of water vapor is different. In the gas phase, individual water molecules placed in front of the surface are attracted to the crystal, with their oxygen eventually binding to the surface Pb atoms, forming polar Pb–O connections. Once the molecule is anchored in this manner, it does not undergo extensive diffusion on the nanosecond timescale at room temperature, thus water cannot disrupt the [PbI6]4− framework, as depicted in Fig. 3(c). Therefore, it can be concluded that water, as isolated molecules, gradually infiltrates and diffuses without disrupting the crystal until hydrated phases are formed. Conversely, as illustrated in Fig. 3(d), when water accumulates on the surface, irreversible lattice degradation may occur.41 These simulation results are consistent with the experimental observations by Aurélien M. A. Leguy et al. In their experiments, it was observed that when MAPbI3 single crystals and films were exposed to water vapor at room temperature, hydrated crystalline phases were formed.46 Importantly, this transition can be reversed under dry conditions. In contrast, when exposed to liquid water, MAPbI3 degrades and forms PbI2, which is an irreversible process. Under such conditions, degradation is highly efficient, and only minimal amounts of liquid, such as condensed droplets on the film surface or rapid immersion in water, have been observed.46,47 Similarly, Jong Un-Gi et al., through calculations, found that water interacts with PbX6 and MA through hydrogen bonding, with the interaction of water intercalation gradually increasing as X changes from I to Br and then Cl, while the hydration interaction remains nearly unchanged. Water-induced hydrogen bonding interactions significantly affect vacancy-mediated ion migration, as water intercalation in halide perovskites reduces the activation barrier. These results indicate that the degradation of perovskite solar cells (PSCs) following exposure to humidity arises from a multi-step process: the formation of water intercalation and hydrated compounds, followed by the decomposition of these compounds.36
Fig. 4 Representative geometrical structures of the formation of (a) [PbI2(H2O)4] and (b) [PbI(H2O)5]+ complexes. Reproduced with permission.30 Copyright 2015, American Chemical Society. |
Accelerated degradation of the perovskite structure invariably leads to deterioration in device performance. Pezhman Darvishzadeh et al. modeled the variation of open circuit voltage (VOC) over time, demonstrating that ion migration and PbI2 defects are the primary causes for the degradation of VOC exposed to humidity.53 Sohrabpoor Hamed et al. also concluded that the defect profile plays a pivotal role in the instability of the device.54
Yun-Hyok Kye et al. investigated the defect processes in MAPbI3, water-intercalated MAPbI3_H2O, and monohydrated phase MAPbI3·H2O.56 They considered the formation energies of isolated and clustered vacancy defects with different charge states under iodine-rich and iodine-poor conditions. The study found that the formation of VPbI2 from its isolated vacancy defect is spontaneous. However, due to the significantly lowered kinetic barrier for I− migration upon hydration, the concentration of VI should be reduced to prevent this formation, which can be achieved by imposing iodine-rich conditions. In hydrated compounds, the formation of individual point defects VI and VMA is easier than that of VMAI. Therefore, during decomposition, I2 or CH3NH2 or HI can be formed instead of MAI. Unlike in pristine MAPbI3, all vacancy defects lead to the creation of deep transition energy levels in hydrated compounds. This is attributed to electrostatic interactions with water molecules, suggesting the degradation of halide lead perovskites when exposed to humidity.
Yun-Hyok Kye et al. also calculated the thermodynamic transition levels ε(q1/q2) between defect states of different charge states q1 and q2. Fig. 5(a) depicts the potential transition levels along with the relative positions of MAPbI3_H2O and MAPbI3·H2O with respect to MAPbI3. Water molecules inserted through the membrane surface extract electrons, causing the valence band maximum (VBM) to shift to lower energies and the conduction band maximum (CBM) to higher energies, consequently altering the bandgap from the original phase to the water-intercalated and monohydrated phases. Evidently, in the case of MAPbI3, all vacancy defects possess shallow transition levels, while in the context of hydrated compounds, vacancies exhibit deep trap behavior. This can promote charge carrier recombination, leading to the degradation of solar cell performance. Specifically, in MAPbI3, VI and VMA act as shallow donors and acceptors, as evidenced by their respective transition levels ε(1+/0) and ε(0/1−) near the CBM and VBM. In the case of hydrated compounds, transition levels are situated deep within the bandgap, with the transition level for VMA not far from the valence band. Notably, VPb in MAPbI3 lacks a transition level within the band (ε(0/2−)), but in hydrated compounds, it could possess two deep transition levels, ε(0/1−) and ε(1−/2−). Both VMAI (with two transition levels) and VPbI2 (with two/four transition levels in pristine/hydrated MAPbI3) exhibit such characteristics.
Fig. 5 (a) Band alignment and thermodynamic transition levels in MAPbI3, water-intercalated MAPbI3_H2O, and monohydrate MAPbI3·H2O, where deep-lying Pb 5d levels are used as a reference for the VBM and CBM of each phase. Reproduced with permission.56 Copyright 2018, American Chemical Society. (b) Minimum energy level of π*2p of O2 absorbed at the interstitial space on a PbI2-terminated surface as a function of water content. Reproduced with permission.59 Copyright 2019, John Wiley and Sons. |
Water not only influences defect formation but also passivates defects. Water molecules passivate deep-level defects by forming hydrogen bonds with I atoms in the perovskite structure.57 Wenke Zhou et al. verified the defect passivation effect of water molecules on MAPbI3 thin films using thermal admittance spectroscopy. Initially, the authors measured control MAPbI3 perovskite films without water treatment and identified deep-level defects at 0.295 eV, typically associated with Pb–I anti-site defects. After appropriate water treatment, the deep-level position shifted closer to the conduction band, indicating effective passivation of Pb–I anti-site defects by water molecules. Upon further drying the water, the defect level position deepened. This outcome suggests that an appropriate amount of water can effectively passivate deep-level defects, and the process is reversible.
Apart from 3D perovskites, H2O can also passivate defects in 2D perovskites. Xinlu Guo et al., through DFT calculations, discovered that a suitable number of water molecules can preferentially occupy VI defects in Dion–Jacobson (DJ) phase perovskites, reducing trap centers, forming hydrogen bonds with surrounding atoms, enhancing the structural stability, and making them more robust. Concurrently, experimental observations showed that devices prepared under humid conditions exhibit improved photovoltaic performance and stability.58 However, compared to 3D perovskites, there has been limited research on the interaction of water and defects in 2D perovskites, and theoretical investigations in this context are particularly lacking. Conducting research on issues related to 2D perovskites could significantly promote the advancement of this field.
Light- and oxygen-induced degradation of MAPbI3 is a primary factor limiting the lifespan of PSCs. Yixin Ouyang et al. revealed through calculations that due to the weak affinity between oxygen and MA, as well as the capture of iodine vacancies, O2 cannot spontaneously diffuse from the surface into the internal lattice of MAPbI3.59 The slow diffusion properties lead to photodegradation concentrating on the perovskite surface. Induced by the MAPbI3 surface, the degenerate π*2p energy level of O2 slightly splits into two bands. When H2O approaches O2, the π*2p energy level of O2 decreases, moving it closer to the valence band of MAPbI3. The pronounced polarization effect of water enhances oxygen's electron affinity, causing a reduction in the O2 energy level. Changes in H2O content also impact this process. With more H2O molecules progressively surrounding adsorbed O2, the oxygen state shifts further downward. For O2 adsorbed at hollow sites on the PbI2-terminated surface, the transition of oxygen states is significantly influenced by water content. As illustrated in Fig. 5(b), as water content increases, more charge is transferred from surface I atoms to O2 due to water molecules. This results in a deceleration of the reduction in the O2 energy level. H2O acts as a bridge on VMA points, facilitating the transmission of changes between I atoms and absorbed O2. In conclusion, stable perovskite thin films necessitate crystal surfaces terminated with defect-free MAI.
Fig. 6 (a) Lattice evolution of α- and δ-FAPbI3 with increasing H2O concentration and an indication of phase transition path. Reproduced with permission.64 Copyright 2022, John Wiley and Sons. (b) Schematic diagrams of high-T CsPbI3 (left, orthorhombic structure with three-dimensionally connected corner-sharing octahedra) to low-T CsPbI3 (right, orthorhombic structure with one-dimensional chains of edge-sharing octahedra) phase transformation triggered by moisture. (c) Illustrative energy diagram of CsPbI3 (thick red line) comparison with common moisture induced modification (faint red line) of the energy scheme. Reproduced with permission.69 Copyright 2021, Elsevier. |
Similar to FAPbI3, CsPbI3 is also prone to undergo a phase transition from the high-temperature (high-T) γ phase to the low-temperature (low-T) δ phase under atmospheric conditions,66–68 as shown in Fig. 6(b). Zhenni Lin et al. employed molecular dynamics simulations and found that when a thin layer of water contacts the metastable perovskite surface, the large solvation enthalpy of I− and its associated low formation energy of vacancies enhance the halide vacancies at the water–perovskite interface. These halide vacancies can be considered as defect sites that lower the activation energy barrier (PT barrier) between the metastable γ- and stable δ- of CsPbI3, as illustrated in Fig. 6(c), effectively catalyzing the phase transition.
Further increasing the relative humidity (RH) results in an exponential increase in vacancy equilibrium concentration. Based on this, it can be predicted that elevated RH levels lead to an exponential increase in the nucleation rate of δ phase CsPbI3.69 Moreover, Kyoung E. Kweon et al. utilized DFT calculations to study the water-induced effects of H2O molecules and their dissociation species (H+/OH−) during the γ- to δ-transition of CsPbI3. They discovered that the reaction energy barrier is significantly lowered when H2O or OH- is present within CsPbI3, while the influence of H+ on kinetics can be neglected.70 Corresponding phenomena have also been experimentally observed and quantitatively validated the computational conclusions. Daniel B. Straus et al. experimentally observed the vapor-induced transformation of γ-CsPbI3 to δ-CsPbI3 through synthetic variations and in situ PXRD measurements.71 Similarly, for CsPbBr3, Jiayu Di et al. found through calculations that the presence of water during crystal growth reduces the formation energy of γ-CsPbBr3 and promotes the reaction in that direction.72 This can explain recent observations that atmospheric humidity accelerates the phase transition kinetics without significantly altering the transition enthalpy.
Fig. 7 (a) Schematic illustration of H2O in regulating the crystallization process. Reproduced with permission.75 Copyright 2022, Springer Nature. (b) The PDOSs for three surfaces. Reproduced with permission.40 Copyright 2016, Royal Society of Chemistry. (c) Illustration of the perovskite–moisture interaction, leading to electron transfer, hydration, and degradation. Reproduced with permission.81 Copyright 2019, American Chemical Society. |
Andrew M. Rappe et al. discovered that when the H2O:MA ratio typically ranges from 0 to 1, and the addition of water generally leads to an increase in the bandgap.32,80 This gap variation is caused by structural deformation and lattice expansion. Generally, the introduction of water reduces the connectivity of the primary structure of MAPbI3, weakening bonds, narrowing bands, and increasing the bandgap. When the ratio of H2O:MA falls within the range of 1 to 2, water molecules exhibit a “chemical” effect in determining the bandgap. At higher water concentrations such as H2O:MA = 2, the orbitals of water more significantly contribute to the VBM and CBM due to increased covalency with the inorganic framework's I− and Pb2+. This is a consequence of the fractured octahedra, leading to direct binding of water with the inorganic framework (i.e., Pb2+).
The interaction of water molecules alters the geometry and electronic structure of MAPbI3, and undoubtedly influences the material's optical properties. Lei Zhang et al. computed snapshots of the absorption spectra for molecular dynamics (MD) trajectories, and at the beginning of the simulation, the initial structure exhibited optical responses similar to the bulk phase.40 As the simulation progressed and water molecules penetrated the interior layers of the MAI-terminated surface, significant changes in the perovskite structure occurred, resulting in a pronounced decrease in absorption in the visible range, particularly around 550 nm. However, the situation is slightly different on the water-adsorbed PbI2-terminated surface. Initially, the absorption decreases significantly and then remains stable over time, indicating the relative stability of the PbI2-terminated surface. The evolution of the absorption with time suggests that interacting water molecules gradually disrupt the perovskite structure, subsequently diminishing the performance of PSC devices. Ali Kachmar et al. calculated the absorption spectra of MASnI3 before and after water infiltration into the crystal structure, showing that water molecules enhance the absorption of photon energies within the range of approximately 1–2 eV. However, as the photon energy further increases, the absorption coefficient of the monohydrated perovskite system decreases. Moreover, the introduction of water molecules into the system eliminates two distinct peaks in the absorption curve at 2.5 and 3.5 eV. Only at photon energies starting from 4.5 eV (i.e., after the maximum absorption peak) do the absorption coefficients become nearly equal.31
Md Azimul Haque et al. fabricated MAPbI3 microstrips on a flexible substrate and observed a four-order-of-magnitude decrease in the microstrip resistance as the relative humidity levels varied from 10% to 95%. Additionally, the photocurrent response decreased with increasing humidity, and at a relative humidity level of 85%, the perovskite device no longer exhibited a photoresponse. The authors demonstrated a potential scenario for the interaction between perovskite and humidity. As shown on the left side in Fig. 7(c), moderate humidity or short-term exposure to high humidity conditions led to electron transfer from water molecules to the perovskite lattice. However, as depicted on the right side in Fig. 7(c), prolonged exposure to high humidity conditions resulted in degradation through different pathways in the perovskite.81
Thermalization of hot carriers is one of the main sources of efficiency loss in solar cells. Ali Kachmar et al. investigated the thermal electron cooling in both MASnI3 and MASnI3·H2O within the tetragonal phase. In the case of the monohydrated perovskite, the cooling time is less than 1 ps. The overall trend is that the cooling process of hot electrons is faster in the MASnI3·H2O system compared to the MASnI3 system. For energies higher than 2 eV, the cooling time of hot electrons appears to be less influenced by water molecules. This is because, in the case of the monohydrated system, the electron–phonon coupling (coupling between states in the conduction band) is stronger compared to the pristine system.31
We observe that water's influence on perovskites presents both beneficial and detrimental aspects. The advantageous effects predominantly manifest at lower water concentrations, while escalated water concentrations or typical environmental conditions tend to elicit adverse repercussions on perovskite stability. This culminates in material degradation, significantly compromising device performance and ultimately impeding the commercialization trajectory of perovskite devices. Consequently, a more profound exploration of the interactions and mechanisms between water and perovskites is imperative. This endeavor aims to guide experimental endeavors in effectively enhancing perovskite humidity stability, thereby expediting their commercialization endeavors.
By employing these methods, the humidity stability of perovskite optoelectronic devices has been improved to a certain extent. However, further optimization of these approaches is still required to enhance stability under various environmental conditions.
From the perspective of theoretical calculations, there are several challenges in studying the influence of water molecules on perovskites:
(1) Complex interactions: the interactions between perovskites and water involve numerous chemical bonds and forces, making theoretical calculations highly complex. Consideration of factors such as charges, ion radii, bond lengths, and bond angles is necessary, posing significant challenges for computer simulations and theoretical analyses.
(2) Dynamics: the interaction between perovskites and water molecules exhibits high dynamics. Water molecules can form various complexes on the surface and within the perovskite, leading to continuous structural changes. This implies that theoretical calculations need to account for a large number of structural configurations and interactions, increasing computational difficulties.
(3) Time scale: the influence of water on perovskites is a long-time scale process under realistic conditions. Theoretical calculations require simulation over sufficiently long time-scales to capture various possible interactions and structural changes. This may result in computationally intensive tasks that require substantial computing resources.
(4) Temperature: in practical applications, perovskites may be exposed to different temperature conditions. These conditions can affect the interactions between water molecules and perovskites, thereby influencing their stability. When performing theoretical calculations, these factors need to be considered to accurately simulate real-world scenarios.
Footnote |
† These authors contributed equally to this work. |
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