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Carbon arc production of heptagon-containing fullerene[68]


A carbon heptagon ring is a key unit responsible for structural defects in sp2-hybrized carbon allotropes including fullerenes, carbon nanotubes and graphenes, with consequential influences on their mechanical, electronic and magnetic properties. Previous evidence concerning the existence of heptagons in fullerenes has been obtained only in off-line halogenation experiments through top-down detachment of a C2 unit from a stable fullerene. Here we report a heptagon-incorporating fullerene C68, tentatively named as heptafullerene[68], which is captured as C68Cl6 from a carbon arc plasma in situ. The occurrence of heptagons in fullerenes is rationalized by heptagon-related strain relief and temperature-dependent stability. 13C-labelled experiments and mass/energy conservation equation simulations show that heptafullerene[68] grows together with other fullerenes in a bottom-up fashion in the arc zone. This work extends fullerene research into numerous topologically possible, heptagon-incorporating isomers and provides clues to an understanding of the heptagon-involved growth mechanism and heptagon-dependent properties of fullerenes.


Cage-closed all-carbon structures, including fullerenes and carbon nanotubes, are typically composed of hexagon and pentagon carbon rings1,2. Experimentally, however, heptagon rings are also incorporated into carbon frameworks making the experimentally available carbon allotropes (for example, fullerenes and carbon nanotubes, as well as graphenes) defective species3,4,5,6,7,8,9,10. Although unambiguous identification of heptagons in the family of all-carbon allotropes remains an open question, numerous theoretic studies have focused on the heptagon-involved defect because of its key responsibility for changing geometric structures and properties of the experimentally available carbon allotropes11,12,13,14,15,16,17,18,19.

The possible existence of heptagons in carbon nanotubes was first proposed by Iijima3 in 1992. A heptagon-incorporating fullerene, named a heptafullerene in this work, was originally proposed by Taylor20. Heptafullerene[72], which has been predicted by Akasaka and Nagase21 from 431,240 isomeric possibilities, is more stable than the Isolated Pentagon Rule22 satisfying isomer in form of endofullerene Ca@C72. A bare heptafullerene[62] with Cs-symmetry23, as well as the exohedral heptagon-containing C68X4 (X=H, F, Cl)24, has been calculated to be more stable than all the classical non-heptagon isomers. Very recently, a number of smaller heptafullerenes (C46–C58) have also been suggested to be viable18,25,26. However, experimental confirmation of the existence of heptagons in the family of fullerenes is still a challenge for chemists and physicists.

It is possible chemically to manipulate a few of the carbons on a fullerene surface to modify the carbon cages into heptafullerene derivatives, such as C58F18 (ref. 27) and C84Cl32 (ref. 28). Such work has provided a breakthrough in the synthesis of heptafullerene derivatives by a top-down chemical method. Clearly, such synthetically produced halides of heptafullerenes (C58 and C84) are not species directly retrieved from an in situ carbon-clustering process. Thus, these species do not establish the finite existence of unmodified heptafullerenes.

Here we perform an experiment, using graphite arc-discharge, which is well known for bottom-up growth of the whole family of sp2-hybrided carbon allotropes2,29,30, to capture a heptafullerene[68] in situ as a heptagon-containing C68Cl6 (hepta-C68Cl6).


Carbon arc production and purification

C68Cl6 was produced in a Krätschmer–Huffman reactor of a graphite arc-discharge under 0.0395 atm CCl4 and 0.1974 atm helium29,31. After separation and purification by multistage high performance liquid chromatography (HPLC), 1.6 mg of the C68Cl6 of 99% purity was obtained from 150 g soot products of the CCl4-involving graphite arc-discharge (Methods; Supplementary Figs S1–S3).

Crystallographic structure

Single, black crystals suitable for X-ray diffraction were grown by solvent evaporation of a mixed solution of carbon disulfide and chloroform (2:1 in volume) of C68Cl6, (Supplementary Figs S4 and S5; Supplementary Tables S1–S6 and Supplementary Methods). The molecular structure of C68Cl6 revealed by X-ray crystallography is shown in Figure 1. It has 22 hexagons, 13 pentagons and 1 heptagon on the surface of the molecular cage. Of these, four pentagons are contiguous to form two pairs of doubly fused pentagons, in which the carbon atoms at the fusion are bonded to chlorine to relieve the unfavourable local strain. As well as the four chlorine atoms associated with these pentagon fusions, two further chlorines are bonded, one at each of two pentagon–hexagon–hexagon vertexes. The resultant sp2-hybridized 62-atom open-cage cluster is in good accord with the so-called Local aromaticity principle32.

Figure 1: Structure of C68Cl6 molecule.

ORTEP structure (a) and Schlegel diagram (b) of C68Cl6 (ORTEP=Oak ridge thermal ellipsoid plot).

Mass spectrometric analysis

The molecular composition of C68Cl6 is confirmed by mass spectrometry (MS) (Supplementary Fig. S3). Multistage mass spectrometric experiments show progressive dechlorination of C68Cl6 and the eventual formation of bare C68, with the implication that heptafullerene[68] itself has a finite lifetime in the gas phase (Fig. 2).

Figure 2: Multistage mass spectrometry.

(MSn, n=1–3). Progressive dechlorination produces C68Clm (m=0–6) (m is indicated in blue). The species picked for next stage of fragmentation, by collision with helium buffer gas in ion trap, is marked by an asterisk. m/z, mass to charge ratio.

13C-Labelling experiments

To establish that the retrieved C68 species indeed grows together with other fullerenes in the CCl4-involving graphite arc-discharge conditions, a series of 13C-labelled experiments were conducted in a glass chamber (inner diameter (I.D.) 194 mm) with reactants (graphite and CCl4) having different 13C contents: (A) Exp. A with normal graphite and CCl4 (about 1.1 atm % 13C); (B) Exp. B with 1.1 atm % 13C graphite and 99 atm % 13CCl4; (C) Exp. C with 21.8 atm % 13C-rich graphite and 1.1 atm % 13CCl4. The products were analysed by HPLC–MS technology to record the mass spectra for individual components (Supplementary Figs S6–S11). A total of 13 chlorinated polycyclic aromatic hydrocarbons (chloro-PAHs), 6 bare fullerenes, and 7 chlorofullerenes were detected in the crude products of the 13C-labelled experiments (Supplementary Figs S6–S11; Supplementary Table S7). Note that more species were detected when crude products were preliminarily concentrated by HPLC). Typical mass spectra of some selected products are shown in Figure 3, including smaller chloro-PAHs (C12Cl8, C18Cl10 (isomer 2) and C20Cl10 (isomer 1)), typical fullerenes (#1812C60, #8149C70 and #19150C76), and chlorofullerenes (#1809C60Cl8, #271C50Cl10 and hepta-C68Cl6). Note that the nomenclature specified by the Fowler–Manolopoulos spiral algorithm33 has been used to distinguish classical non-heptagonal isomers. The mass spectrum of each product clearly shows the featured mass-to-charge (m/z) pattern (Fig. 3; Supplementary Figs S6–S11). The m/z pattern can be clearly defined by the isotopic 12C/13C content of the corresponding cluster (Supplementary Methods for details) and thus reflects the footprint of the parental carbon sources involved. Table 1 lists the estimated 13C percentage of the selected carbon clusters according to the corresponding mass spectra recorded.

Figure 3: Mass spectra of representative products from the 13C-labelled experiments.

The products are exemplified by (a) chlorofullerenes (#1809C60Cl8, #271C50Cl10 and hepta-C68Cl6), (b) fullerenes (#1812C60, #8149C70 and #19150C76) and (c) chloro-PAHs [C12Cl8, C18Cl10 (2) and C20Cl10 (1)]. Spectra are coloured green, red and blue for Expts. (A), (B) and (C), respectively. m/z, mass to charge ratio.

Table 1 The 13C percentage estimated from mass spectra of selected carbon clusters produced in 13C-labelled experiments.


A classical cage-closed all-carbon structure (fullerene or carbon nanotube) typically contains a number of hexagons and exactly 12 pentagons. However, because of the incorporation of a heptagon, the number of pentagons in the present C68 is increased to 13. Two pairs of them are adjacent, in violation of the isolated pentagon rule22, rendering the bare C68 highly reactive and elusive. As a result of passivization by six chlorine atoms for the most reactive carbon atoms at the pentagon fusions and the aromaticity-unsatisfied sites, the elusive C68 has been stabilized as chlorofullerene C68Cl6.

The most prominent feature in the captured C68 is the occurrence of a heptagon, which represents a new type of building unit for constructing cage-closed all-carbon architectures. In contrast to previously reported non-heptagonal fullerenes, heptafullerene[68] contains a heptagon having about 10% more space than a hexagon, and this presumably delivers easier pass through of foreign atoms, such as helium or nitrogen, to produce endofullerenes for potential technical applications. Indeed, first-principle density functional theory (DFT) calculations (Supplementary Fig. S12; Supplementary Table S10 and Supplementary Methods) predict that the activation energy for a helium atom penetrating into a fullerene cage decreases dramatically from 225.1 kcal mol−1 for Ih-C60 to 128.4 kcal mol−1 for hepta-C68Cl6. This easier penetration of helium into hepta-C68Cl6 is also supported by mass spectrometric evidence (Supplementary Fig. S13). The heptagon is surrounded by four pentagons and three hexagons. One of the carbon atoms in the heptagon is shared by two adjacent pentagons and subsequently transformed from sp2- to sp3-hybridization to release the strain of the doubly fused pentagons. Of interest is the decreased π-orbital axis vector (POAV) angle34 of 6.0–10.4° (average 8.2°) at the fusions of the remaining two pairs of sp2-hybridized pentagon–heptagon junctions (Fig. 1b). These POAV angles are even smaller than those in the stable buckminsterfullerene Ih-C60 (11.64°), rendering heptafullerene[68] a heptagon-related planarity. Such kinds of decreased POAV angle have also been seen in the recently reported C84Cl32 molecule, in which the POAV angles at the carbon atoms of the heptagon are in the range of 3.2–5.8° (average 5.2°)28. As the heptagon-related planarity facilitates strain relief in a curved surface of a cage, the existence of a heptagon may be expected to bring extra stabilization for the carbon cage involved. However, DFT calculations reveal substantial accommodation of the highest occupied molecular orbital electron densities around the cycloheptatriene-like ring of hepta-C68Cl6 (Supplementary Fig. S14; Supplementary Table S11 and Supplementary Methods), implying a readiness for electrophilic additions at the heptagon area. DFT calculations also suggest that the C–Cl bond pertaining to the cycloheptatriene-like ring of hepta-C68Cl6 is subject to nucleophilic substitution by taking advantage of local aromaticity of the 6-electron π-conjugated C7+ tropylium-like ring in the corresponding hepta-C68Cl5+ intermediate (Supplementary Fig. S15; Supplementary Table S12 and Supplementary Methods). Thus, the cycloheptatriene-like ring of hepta-C68Cl6 is a double-edged sword, conveying unique reactivity to this heptagon-incorporating fullerene derivative, making it subject to both electrophilic addition and nucleophilic substitution.

Theoretical studies predict that the hepta-C68 has an energy comparable to that of the most stable isomers of classical C68 that lack a heptagon. At room temperature, the hepta-C68 is the third most stable of the C68 isomers, with an energy ~2.5 kcal mol−1 higher than the most stable one. At a temperature above 2,100 K, however, the heptagon-incorporating C68 becomes the most abundant species as entropic factors have a decisive role in their relative Gibbs free energies and relative concentrations/abundances (Supplementary Tables S8 and S9). In agreement with this prediction about the temperature-dependent stability, several theoretical studies have suggested the prevalence of heptagons in the world of the cage-closed all-carbon allotropes11,12,13,14,15,16,17,18,19,20,21,23,24,25,26,35,36. Experimental corroboration of such a prevalence of heptagons heavily depends on the in situ capture of heptafullerene in the carbon clustering venue for the growth of the whole family of fullerenes. However, the previously reported heptafullerene derivatives (hepta-C58F18 and hepta-C84Cl32) were synthesized by an off-line top-down method through chemical detachment of a C2 unit from a stable fullerene (C60 or C86)27,28. This top-down approach is similar to the so-called open-cage method in which the hexagons/pentagons of fullerene cages (typically C60) are modified to give so-called open-cage fullerenes containing rings with twelve-, sixteen-, or eighteen-membered-rings and beyond37,38,39. By fluorination of C60 at 550 °C, therefore, it is not surprising that two carbon atoms at a hexagon–pentagon fusion of C60 have been removed to form stable derivatives of heptafullerene[58], C58F18 or C58F17CF3 (ref. 27). Very recently, the chlorinated heptafullerene[84] C84Cl32 has also been synthesized from C86 by chlorination at 250 °C (ref. 28). These cases, however, are inappropriate for establishing the survival of bare heptafullerenes in a bottom-up clustering process during growth of the whole fullerene family.

In contrast, the present heptafullerene[68] molecule was captured in situ and directly isolated from the pristine products of a carbon arc, which is a typical venue for bottom-up growth of carbon allotropes such as fullerenes29, carbon nanotubes2 and graphenes30. Powerful evidence to establish the bottom-up process comes from the 13C-labelled Exp. C: the reactant of 21.8 atm % 13C-rich graphite is an inhomogeneous mixture with a 90 atm % 13C-rich carbon powder filled into a hollow graphite rod with regular 1.1 atm % 13C content (Methods), but the produced hepta-C68Cl6 and other fullerene species (for example, #1812C60, #8149C70, #19150C76, #1809C60Cl8, and #271C50Cl10) show an almost homogeneous 13C percentage of 20.4 atm % (rather than the separated 1.1 or 90 atm % value) in the corresponding mass spectra (Fig. 3; Supplementary Figs S9 and S10). This evidence, in accordance with previous literature40,41,42, clearly confirms that fullerenes grow from atomization of a carbon or small carbon clusters such as C2 derived from graphite in the carbon arc process. Moreover, our 13C-labelled experiments also ascertain that the bare heptafullerene[68] grows together with other fullerenes in the arc zone at high temperature and subsequently is captured by chlorine atoms produced from CCl4 in the carbon arc conditions.

In the present CCl4-involving graphite arc-discharge conditions, there are two carbon sources for the growth of carbon clusters, that is, the reactive carbon species from graphite (C-source I) and CCl4 (C-source II). The former C-source I has a gradual density distribution with enhanced concentration at the arc zone but decreased beyond, whereas the latter CCl4 source II is assumed to disperse in association with temperature distribution in the reaction chamber. The density of C-source I (or II) versus the distance from the arc centre (that is, the radius) in the reactor can be simulated based on mass conservation equation (Supplementary Figs S16–S20; Supplementary Tables S13, S14 and Supplementary Methods). Accordingly, the carbon clusters produced at a certain region in the reactor can be quantified to grow from a mixture of carbon sources with an exclusive proportion of C-source I versus C-source II. In the present 13C-labelled experiments, we conducted the syntheses of carbon clusters in a glass chamber (I.D. 194 mm) starting with the graphite and CCl4 having different 12C/13C ratios, that is, Exp. A with normal graphite and CCl4 (1.1 atm % 13C), Exp. B with 1.1 atm % 13C graphite and 99 atm % 13CCl4, and Exp. C with 21.8 atm % 13C-rich graphite and 1.1 atm % 13CCl4. The products formed at a certain region inside the reactor would deliver an exclusive 12C/13C isotopic ratio that can be determined from the isotopic pattern recorded in the corresponding mass spectra (for example, Fig. 3). For example, the mass spectrum of hepta-C68Cl6 itself shows the isotopic percentage of 13C being ~1.6% 13C in Exp. B and ~20.4% 13C in Exp. C. Sequentially, the region for the growth of the carbon cluster product can be located simply according to the relationship of the 13C isotopic percentage of products/reactants versus the location in the reactor for Exp. B or C (Supplementary Figs S6–11, S16–20; Supplementary Tables S7, S13, S14 and Supplementary Methods).

Figure 4 shows the simulated curves of 13C content of reactive carbon sources (C-source I plus II) versus the distance from the arc centre in the reactor for Expts B and C (detailed calculations regarding mass conservation equation are described in Supplementary Methods). According to the simulated curves and the estimated 13C content in the hepta-C68Cl6 produced from the 13C-labelled experiments (Expts B and C), it can be concluded that the carbon framework of hepta-C68Cl6 grows in the arc zone about 2–3 mm from the arc centre. Interestingly, as shown in the corresponding mass spectra (Fig. 3; Supplementary Figs S6, S7, S9 and S10), isotopic percentages of 13C in other representative fullerene species (for example, #1812C60, #8149C70, #19150C76, #1809C60Cl8, and #271C50Cl10) are approximately the same as those of hepta-C68Cl6 itself, that is, ~1.1% 13C in Exp. A, ~1.6% 13C in Exp. B, and ~20.4% 13C in Exp. C, implying that the heptafullerene[68] grows together with the other fullerenes in the same zone. Conformity of the reaction area with the experimentally obtained 13C contents of fullerenes in both Exp. B and Exp. C validates the model of the mass conservation equation. Although the precision remains to be established, the proposed reaction zone might be informative for improving the yields of fullerenes in the carbon arc. As an example, we designed a synthetic experiment using a hollow anode (I.D. 4 mm) to replace a solid anode under otherwise identical arc-discharge conditions. Very interestingly, the yields of fullerene species such as #1812C60, #8149C70 and #1809C60Cl8 were improved twofold (Supplementary Fig. S21 and Supplementary Methods), probably due to increase of the reaction venue at ~2 mm from the arc centre.

Figure 4: Simulated curves of temperature and 13C content.

Simulated temperature (blue line) and 13C content of carbon sources (black for Exp. B, red for Exp. C) versus distance from the arc centre (radius r) for a reaction period of 600 s. Fullerenes with 13C content of 1.6±0.1% in Exp. B and 20.4±0.1% in Exp. C are produced in an area of r ~2–3 mm at ~2,000–2,500 K (orange background) while a fraction of chloro-PAHs with 13C content of 76.0±0.9 % in Exp. B and 5.0±0.4% in Exp. C are produced in an area of r=~30–33 mm at ~700–730 K (green background).

The temperature for fullerene growth in a carbon arc is still uncertain. At the centre of the arc zone, the temperature could be higher than 4,000 K during the carbon-clustering process43. Beyond the arc zone, the temperature decreases rapidly. The relationship of temperature with the distance from the arc centre can also be simulated by an energy-conservation equation. The simulated temperature curve has been calibrated for good fit to the experimental data at sites of 34, 43 and 52 mm from the arc centre for a reaction time of 300 s (Supplementary Figs S17 and S18). Because fullerenes grow at a region ~2 to 3 mm from the arc centre, the temperature region for fullerene growth can be estimated to be about 2,000–2,500 K from the simulated temperature curve (Fig. 4). This estimate is in line with the above DFT prediction that hepta-C68 is the most abundant isomer at a temperature higher than 2,100 K (Supplementary Tables S8 and S9). It appears that at such a high temperature, Cl–C bonds can not survive and are likely irrelevant to the formation of pristine fullerenes.

However, a drastic difference was observed in the mass spectra of smaller chlorinated carbon clusters, such as C12Cl8, C14Cl8 (1, 2), C16Cl10 (1–3), C18Cl10 (1, 2) and C20Cl10 (1–3) (Fig. 3 and Table 1, as well as Supplementary Figs S8, S11 and Supplementary Table S7). These smaller carbon clusters should have open structures similar to PAHs, because a carbon cluster of less than twenty carbon atoms is too small to give a cage structure. The Exp. B data exemplify that the corresponding mass spectra of these chloro-PAHs (red mass spectra in Fig. 3; Supplementary Fig. S8), very different from those of fullerenes (Supplementary Figs S6 and S7), are a combination of two sets of m/z signals assignable to 13C abundance ratios of approximately ~1.6 and ~76.0 atm % 13C-rich species. Scrutiny of the mass spectra of Exp. C distinguishes two kinds of 13C percentage (average ~5.0 and ~20.4 atm %) for the chloro-PAHs also (Supplementary Fig. S11). Accordingly, two kinds of smaller carbon cluster can be established as growing from different reactive sources: one is produced in the high-temperature zone together with fullerenes and the other is formed in a chlorine-involving process in the region about 30–33 mm from the arc centre at ~700–730 K (Fig. 4). The latter result is in accord with the fact that the smaller chlorinated PAHs can be produced from CCl4 under pyrolysis conditions at around 600–1,000 K (refs 44, 45), and, therefore, differentiates it from the formation mechanism of fullerene species. Such a formation difference between fullerenes and chloro-PAHs also corroborates that the parent heptafullerene[68] and other fullerenes grow in the high-temperature zone, independently of chlorine, and subsequently are captured/stabilized by chlorine on cooling outside the arc zone. The survival of heptafullerene in the carbon clustering process is thus clarified.

On the basis of its crystallographic structure, the connectivity of hepta-C68 also supports a hitherto unidentified mechanism for fullerene growth, namely the Heptagon road, in which the insertion of a C2 cluster and the generation of heptafullerene have been suggested46. In the same carbon arc process, we have also been able to capture and isolate #4169C66 and #8149C70 (ref. 47). From a structural point of view, these two carbon clusters might be possible preceding/subsequent intermediates bridged by the heptafullerene[68]. The scheme shown in Figure 5 suggests a possible route for the formation of #8149C70 by the Heptagon road involving C2-insertion growth from #4169C66 to #8144C70, as well as two Stone–Wales transformations from #8144C70 to #8149C70. It should be noted that this is just a possible implication simply inferred from the structures. Powerful evidence to elucidate the authentic mechanism is needed and further theoretical and experimental studies are now in hand.

Figure 5: Heptagon Road.

Possible growth of fullerene from #4169C66 to #8149C70 through hepta-C68 by the Heptagon Road and two Stone–Wales transformations.

In summary, heptafullerene[68] has been made and captured as chlorinated derivatives in a CCl4-involving graphite arc-discharge process. The 13C-labelled synthetic experiments and mass/energy conservation equation simulations reveal that bare heptafullerene can grow in a bottom-up fashion in the arc zone at high temperature and survive in the gas phase during the carbon clustering process. This work, supported by X-ray crystallographic data and theoretical computations, fundamentally establishes that heptagon-incorporating fullerenes should not have been excluded in the classical fullerene family. It thus greatly increases the numbers of members of the fullerene family. The discovery of heptafullerene[68] may be expected to stimulate research activity in the field of all-carbon allotropes involving heptagons, for example: the synthesis of more heptagon-incorporating members in the family of carbon cages, understanding the formation mechanism(s) involving heptagons, and investigations of heptagon-dependent properties of carbon allotropes.


Carbon arc production

The carbonaceous soot containing fullerenes, chlorofullerenes, and smaller carbon clusters was produced under 0.1974 atm He and 0.0395 atm CCl4 in a Krätschmer–Huffman arc-discharge reactor29,31, equipped with two graphite electrodes, a cathode cylinder block [40 mm (diameter)×60 mm], and an anode rod [8 mm diameter×300 mm]. An hourly production of about 3 g of soot was achieved for a power input of 33 V and 100 A.

13C-labelled experiments

The 13C-labelled synthetic experiments were conducted in a glass chamber (I.D. 194 mm) starting with reactants (CCl4 and graphite anode, diameter of 6 mm) having different 13C contents. Exp. A was conducted with normal graphite and CCl4 having the same 13C percentage (about 1.1 atm %), Exp. B with 1.1 atm % 13C graphite and 99 atm % 13CCl4, and Exp. C with 21.8 atm % 13C-rich graphite and 1.1 atm % 13CCl4. The 13C-rich graphite was prepared by filling 90 atm % 13C-carbon powder into a regular 1.1 atm % 13C hollow graphite rod.

Isolation and identification

Hepta-C68Cl6 was extracted by toluene in an ultrasonic bath from the carbonaceous soot and purified by multistage HPLC process sequentially using a pyrenebutyric acid bonded silica column (I.D. 20×250 mm), a Cosmosil Buckyprep column (I.D. 10×250 mm), and a 5PPB column (I.D. 10×250 mm). All preparative HPLC were performed on a Shimadzu LC-6AD HPLC instrument at rt using toluene as eluent. HPLC–MS for the products from the 13C-labelled synthetic experiments was analysed on a Discovery C18 column (I.D. 4.6×250 mm) of SUPELCO eluted by a methanol–ethanol–cyclohexane gradient. Mass spectra were recorded on a Bruker HCT mass instrument. Crystallographic data were collected on an Oxford CCD diffractometer (Supplementary Methods; Supplementary Data 1).

Additional information

How to cite this article: Tan Y-Z. et al. Carbon arc production of heptagon-containing fullerene[68]. Nat. Commun. 2:420 doi: 10.1038/ncomms1431 (2011).


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We thank Professor Yu-Qi Feng from Wuhan University for HPLC support and Professor G. Michael Blackburn from University of Sheffield, UK, for revising the English of the manuscript. This work was supported by the NNSF of China (Grants 21031004, 21021061, 20973137, and 20876127) and the 973 Program [Grants 2007CB815300(1,7) and 2011CB935901].

Author information




S.Y.X., L.S.Z. and R.B.H. conceived and designed the research; Y.Z.T. conducted the isolation and identification and plotted the figures; Z.J.L., R.T.C. and F.Z. participated in the arc-discharge experiments; Jun L. performed the mass/energy conservation equation simulations; X.L. conceived the theoretical work and Jia L. conducted theoretical computations; S.Y.X. and Y.Z.T. analysed the experimental data; S.Y.X., X.L. and Jun L. wrote the paper; All authors discussed the results and commented on the manuscript.

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Correspondence to Su-Yuan Xie or Jun Li.

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The authors declare no competing financial interests.

Supplementary information

Supplementary Figures, Tables, Methods and References

Supplementary Figures S1-S21, Supplementary Tables S1-14, Supplementary Methods and Supplementary References (PDF 14635 kb)

Supplementary Data 1

Crystallographic data for Hepta-C68Cl6 (TXT 25 kb)

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Tan, YZ., Chen, RT., Liao, ZJ. et al. Carbon arc production of heptagon-containing fullerene[68]. Nat Commun 2, 420 (2011).

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