Song Haoab,
Bingchu Yang*ab and
Yongli Gaoabc
aInstitute of Super Microstructure and Ultrafast Process in Advanced Materials, College of Physics and Electronics, Central South University, 605 South Lushan Road, Changsha 410012, P. R. China. E-mail: bingchuyang@csu.edu.cn
bHunan Key Laboratory for SuperMicrostructure and Ultrafast Process, Central South University, 932 South Lushan Road, Changsha 410012, P. R. China
cDepartment of Physics and Astronomy, University of Rochester, Rochester, NY 14534, USA
First published on 7th June 2016
The fracture behavior of two-dimensional polycrystalline molybdenum disulfide (MoS2) films is essential to device performance and has attracted tremendous attention in recent years. Here, we investigate the mixed intergranular and transgranular fracture behaviors of CVD-grown polycrystalline MoS2 atomic layers using multiple techniques. The underlying mechanism is proposed to be that micro-cracks initially nucleate at grain boundary junctions and propagate along with the grain boundaries, resulting in intergranular fracture behavior. On the other hand, as-existed sulfur vacancies serve as crack nuclei and propagate along energy preference directions through Mo–S bond breaking, resulting in transgranular fracture behavior. Lattice shrinking induced compressive, rather than tensile strain is residual in fractured MoS2 microflakes, which enlarges the corresponding bandgap by ∼200 meV. Our work deepens the understanding of the fracture behaviors of polycrystalline MoS2 atomic layers and demonstrates a promising method to engineer the strain in MoS2-like atomically-thin materials to further tune their physical properties.
As is well known, fracture behavior is widely present in nature from the macro- to nano-scale.9 The fracture behavior of bulk materials has been widely investigated, however, research focused on 2D materials is relatively scarce. Given the atomically thin structure and excellent mechanical properties, the fracture behavior of 2D materials would be a fascinating topic. For example, the fracture strength of CVD-grown polycrystalline MoS2 (90–99 GPa) is only slightly smaller than the intrinsic one (130 ± 10 GPa), despite the existence of grain boundaries.10,11 It was very recently reported in the literature that monolayer MoS2 suffers from significant aging effects including extensive fracture behavior even under ambient conditions (room temperature and atmospheric pressure).12 However, the range of studies have left a confusing picture regarding the definite fracture behavior and mechanism, and the influence on the physical properties of the fractured crystals.
In this article, the fracture behavior of CVD-grown polycrystalline MoS2 atomic layers is systematically investigated by multiple means, including Optical Microscopy (OM), X-ray Photoemission Spectroscopy (XPS), Scanning Electron Microscopy (SEM), Atomic Force Microscopy (AFM), Raman and Photoluminescence (PL) techniques. Measurements on single crystalline MoS2 were also carried out to provide a baseline case. A quenching-induced mixed intergranular and transgranular fracture behavior was observed through SEM and AFM characterization. The corresponding photoluminescence (PL) characteristic peaks rigidly blue-shift by ∼200 meV, which is ascribed to combined effects of compressive strain and oxidation induced p-type doping. While an E12g mode splitting demonstrates a resulting strain in the fractured MoS2 microflakes, the E12g and A1g modes shift towards opposite directions, implying fracture induced structural changes. Since all the layered TMDCs have extremely similar structures, the conclusions acquired in this work are expected to be adaptable for other TMDCs.
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1) and by 5 min of air plasma spurting to remove organic matter. A nitrogen (N2, 5N purity) gas flow was introduced to purge the quartz tube at 150 standard cubic centimeters per minute (sccm) for 20 min. Then, the 2nd heating zone was rapidly heated up to 800 °C at a constant heating rate of 20 °C min−1 and maintained at this temperature for 15 min with a decreased N2 gas flow of 100 sccm. The sulfur powders were maintained at a temperature slightly below the melting point of ∼120 °C during the reaction process, so that sulfur vapor could be carried by the N2 gas flow to the reaction zone slowly. Subsequently, for a fractured sample, the furnace was switched off and the sample withdrawn for faster cooling from 800 °C to 500 °C with a N2 gas flow. For a normal sample, a slow cooling process from 800 °C to room temperature was controlled using a PID temperature program and the sample protected with a N2 gas atmosphere.
The as-synthesized samples were systematically characterized using Optical Microscopy (CaiKang DMM-200C), confocal Raman and photoluminescence techniques (WITec alpha 300R), Scanning Electron Microscopy (FEI Helios 600i), X-ray Photoemission Spectroscopy (thermo fisher ESCALAB 250xi) and Atomic Force Microscopy (Agilent 5500). Raman and PL spectra/mapping were obtained under a 532.0 nm laser light at ambient conditions. To ensure reproducibility of the data, we followed a careful alignment and optimization protocol. In addition, the laser power was maintained below 1 mW to avoid local heating and oxidation, and to obtain a satisfactory signal-to-noise ratio while retaining an acceptable data acquisition duration and avoiding drift. The 520.0 cm−1 phonon mode of the Si substrate was used for calibration of the Raman shift. The emitted stoke Raman signal was collected using a Zeiss 100× objective (N.A = 0.9) and dispersed using a 1800 lines per mm grating for Raman measurements and a 600 lines per mm grating for PL measurements. XPS measurements were performed using monochromatic aluminium Kα X-rays with a light spot size of approximately 1 mm2. The binding energy was calibrated by assigning the corresponding C 1s peak to 284.5 eV. The acceleration voltage for SEM was 10 kV to minimize charge effects. AFM measurements were obtained in the contact mode for morphology characterization.
Given that the thermal expansion coefficient of MoS2 (10−5/°C) is roughly 1000 times larger than that of silicon dioxide (5.6 × 10−8/°C), CVD-grown MoS2 on a SiO2/Si substrate always suffers from a tensile strain induced by interactions between the MoS2 and SiO2.14 Thus, a lower cooling rate is essential to enable the thermal strain to be sufficiently released for MoS2 directly deposited on a SiO2/Si substrate. The cooling rate for the normal sample was linear and was 7.5 °C min−1 in the range from 800 °C to 500 °C, controlled by the furnace temperature programming, as shown in the inserted plot in Fig. 1a. Such a small cooling rate enables the thermal strain in the as-synthesized MoS2 microflakes to be sufficiently released. For the fractured sample, the furnace was powered off following 15 min of growth and the sample was slid far away from the growth zone for quenching. The plot of the temperature measured using an infrared radiation thermometer vs. the cooling duration for the fractured sample was perfectly fitted with the standard non-stationary heat exchange equation of T = 148.5 + 624.0
exp(−t/2.2) and is the insert in Fig. 1b. The cooling rate is as high as ∼300 °C min−1 at the beginning of the quenching phase. Very recently, it has been established that the same cooling rate led to fracture of CVD-grown hexagonal boron nitride.15 Therefore, we believe that the drastic cooling-down process prevents the thermal tensile strain from being sufficiently relieved in the as-synthesized polycrystalline MoS2 atomic layers, which is an important cause of fracture behavior.
It is noteworthy that intense oxidation treatment can induce cracks in either CVD-grown or mechanically exfoliated MoS2 crystals.16,17 To check whether oxidation induces fracture in our investigation, ex situ XPS measurements were carried out. Fig. 1c and d display the Mo 3d and S 2p core level spectra of XPS for the normal and fractured samples, respectively. The doublet peaks located at ∼233.3 and 230.2 eV below the Fermi level were assigned to Mo 3d3/2 and 3d5/2 of Mo4+.18 In addition, the doublet peaks of the S 2p1/2 and 2p3/2 core levels are located at ∼164.2 and ∼163.0 eV, respectively, which is in agreement with values for MoS2 systems. The atomic stoichiometric ratio between the sulfur and molybdenum elements was estimated from the respective integrated peak areas of the XPS to be ∼2.0 for the normal sample and ∼1.8 for the fractured sample, manifesting that the fractured sample contains some sulfur vacancies. A weak peak (indicated by a blue frame) centered at ∼236.1 eV for the fractured sample was assigned to Mo6+ 3d3/2. Thus, the XPS results indicate that oxidation induced fracture could not be excluded but was minor, attributed to residual oxygen in the furnace.
The structural properties of the fractured polycrystalline MoS2 atomic layers were investigated using SEM and AFM measurements, in detail. A representative large-scale SEM image (Fig. 2a) clearly reveals cracks distributed across the polycrystalline films, consistent with the OM image. Given that the grain boundaries in polycrystalline films are usually not perfectly straight, we assign most of curved cracks to grain boundaries. Note that the cracks always stop at a triple junction of three random boundaries, indicating that grain boundary junctions always serve as crack nuclei, which is ascribed to stress concentration. This is similar to what was observed in graphene.19 Considering the fact that the binding energy along grain boundaries is smaller, we believe that crack nuclei formed at three grain boundary junctions propagate along with the grain boundaries upon thermal stress.19,20 Then, intergranular fracture behavior would occur when the cracks connect with each other or reach the edges of the MoS2 atomic layers. It is worth mentioning that the crack tip (Fig. 2b) did not continue to propagate, and further study is needed to understand the interactions between the crack tip and grain boundaries. Given that the grain boundaries have a significant influence on the physical properties of 2D materials, there is an urgent need to realize lateral grain boundary distributions across a large area and a given sized sample. SEM can be a powerful technique for studying the grain boundaries of 2D materials as long as they occur through a fracture process. The darker area marked by an oval in Fig. 2b is due to folded MoS2 induced by sliding, similar to overlapped grain boundaries.21
The AFM topography image of the fractured polycrystalline MoS2 atomic layers exhibits obvious cracks, as displayed in Fig. 2c. The inserted height profile scan shown as a solid blue line presents the height of the MoS2 microflakes as ∼1 nm, which is compatible with monolayer MoS2. Moreover, the grain boundary width is ∼100 nm, which is larger than the regular ∼1–3 nm and we propose that quenching induced lattice shrinking broadens the grain boundaries. Further investigations are needed to support this postulate. The corresponding AFM friction image clearly exhibits cracks, as shown in Fig. 2d. Interestingly, the included angle of ∼120° between neighboring straight cracks suggests a directional preference of transgranular fracture behavior. The bonding energy along the armchair directions is indeed lower than that of the zigzag directions, which governs that the Mo–S bonds would be preferentially broken along the armchair directions, resulting in the appearance of direction-specific crack propagation.22 Thus, an underlying mechanism is proposed that the above-mentioned sulfur vacancies can serve as crack nuclei and propagate along the highly symmetrical crystallographic directions, resulting in direction-specific transgranular fracture behavior. It is worth mentioning that similar orientation dependent fracture behavior in graphene has also been reported in the previous literature.23–25 We conclude that polycrystalline atomic layers could show mixed intergranular and transgranular fracture behavior, as a high fraction of random boundaries and sulfur vacancies exist.
To investigate the influence of the fracture behavior on the electronic band structure of MoS2 films, we carried out PL spectroscopy/mapping, as depicted in Fig. 3. While the PL spectrum for the normal sample presents two prominent PL peaks centered at ∼637 nm (1.95 eV) and ∼685 nm (1.81 eV), the fractured one presents a much broader PL peak. Two subpeaks located at ∼573 and ∼617 nm are required to fit the broad PL peak, assigned to excitonic peaks A and B, respectively.26,27 Apparently, the excitonic peaks for the fractured sample rigidly blue-shift by 68 nm (∼200 meV) compared to the normal ones. The possibility of charge transfer from the substrate can be firstly ruled out due to the identical underlying substrates (SiO2/Si) for the normal and fractured samples. On the basis of the previous literature, we believe that two reasons are responsible for the blue shift of the PL peaks and this will be discussed in the following paragraph.28,29
Firstly, we believe that a strain is residual in the fractured MoS2 microflakes and changes the electronic band structure. Given that the optical band gap of the MoS2 microflakes decreases at a rate of ∼45 meV per % tensile strain, whereas it increases at a rate of ∼300 meV per % compressive strain, the enlarged bandgap shows that a compressive strain is residual in the fractured MoS2 microflakes.28,30 This clarifies the apparent inconsistencies of the earlier study and it may stem from quenching induced lattice shrinking.31 The lattice distance within the topmost layer can shrink by ∼5% compared to the bulk value, while the Mo–S bond length at high temperature is larger than that at ambient temperature, demonstrating the excellent elastic properties of Mo–S bonds.31,32 Thus, we tentatively propose that the MoS2 lattices will be shrunk more than in the freestanding state, to some degree, along with the occurrence of a fast quenching process.33 Secondly, oxidation can induce a p-type doping effect, which leads to a blue shift of the PL peak since the PL peak A is a combination of competing results from excitons and trions (negatively charged excitons).34 Given that the trions are located at a lower energy of ∼30 meV, the influence of oxidation on the PL blue-shift cannot be excluded but it is minor compared to the strain effect.34 Fig. 3b shows PL intensity mapping of the A peak throughout the fractured MoS2, indicating that the residual compressive strain modulates the energy band throughout the fractured microflakes rather than at a particular few points.
Fig. 4a presents Raman spectra for the normal and fractured samples. The E12g mode is related to the in-plane vibration of molybdenum and sulfur atoms while the A1g mode is associated with the out-of-plane vibration of sulfur atoms, as displayed in the inset cartoons.35 The E12g and A1g peaks for the fractured (and normal) sample are located at ∼380.5 and ∼407.1 cm−1 (and 383.6 and 403.6 cm−1), respectively, indicating that the samples retain the trigonal prismatic coordination. However, the frequency difference between the E12g and A1g modes is ∼26.6 cm−1, which is much larger than the normal one (∼20.0 cm−1) and even the bulk one (∼25.0 cm−1).36 The A1g mode for the fractured sample surprisingly blue-shifts by 3.5 cm−1 compared to the normal one, as depicted in Fig. 4a. It has been reported that the A1g mode blue-shifts with an increasing p-type doping level.37,38 Given that the XPS results reveal that both the Mo 3d and S 2p core levels are not obviously shifted for the fractured and normal samples, an influence of p-type doping for the blue-shift of the A1g mode cannot be excluded but seems unlikely.39 It is well known that the A1g vibration blue-shifts with an increasing MoS2 thickness, because the interlayer vdW interactions increase the effective restoring forces acting on the atoms.40 We ascribe the blue shift to the shrinking of the Mo–S bond length, in excellent agreement with the PL results. Likewise, the Raman modes for monolayer MoS2 can significantly blue-shift (phonon stiffens) under hydrostatic pressure, which is attributed to Mo–S bond shrinking.41 In consideration of the same underlying substrate, we also exclude any significant effect of interactions between the underlying substrate and MoS2.42
Fig. 4a shows that the broad E12g peak was fitted with two subpeaks centered at ∼374.7 and ∼381.2 cm−1, which can explain the strain-induced degeneracy lift of the E12g mode. We note that the subpeaks red-shift with increasing of the tensile strain, whereas they blue-shift with increased compressive strain, which is ascribed to phonon softening or stiffing.43,44 For example, the subpeaks are located at ∼376.5 and ∼382.2 cm−1 for a 2% tensile strain, while are centered at 383.7 and 387.3 cm−1 with a 0.54% compressive strain.43,44 In this regard, a significant blue-shift of the A1g peak signifies compressive strain, while a red-shift of the E12g subpeaks does not. We tentatively propose that the opposite progression for the E12g mode is due to structural gliding. Given that the upper sulfur plane seriously shrinks while the lower plane could weakly shrink upon a tensile strain induced by the SiO2 substrate, a structural gliding between the upper and lower sulfur planes would be induced.45 The aforementioned zoomed-in SEM image exhibits a fold area, reflecting the gliding of the MoS2 films. Fig. 4b presents the intensity line mapping of the A1g peak scan using a blue solid line in Fig. 4d, and exhibits an obvious lower intensity corresponding to a crack. Fig. 4c and d reveal an identical color contrast for the fractured sample, demonstrating that the conclusions made from the Raman spectra can represent all the fractured microflakes rather than specific points.
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