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Beckman Institute, University of Illinois at Urbana-Champaign, Urbana, Illinois
Correspondence: Address reprint requests to Klaus Schulten, Tel.: 217-244-1604; Fax: 217-244-6078; E-mail: kschulte{at}ks.uiuc.edu.
| ABSTRACT |
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| INTRODUCTION |
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Computational studies have suggested that CNTs can be designed as molecular channels to transport water. A (6,6) single-walled CNT, with a diameter of 8.1 Å, has been studied recently by molecular dynamics (MD) simulations (Hummer et al., 2001
). The simulations revealed that the CNT was spontaneously filled with a single file of water molecules and that water diffused through the tube concertedly at a fast rate. The motion of water through CNTs can be described by a continuous-time, single-file random-walk model (Berezhkovskii and Hummer, 2002
).
Microporous alumina layers with CNTs embedded within the pores can be produced by chemical vapor deposition and fluxes of electrolytes through these layers have been observed (Miller et al., 2001
). Chemical groups can be attached to the CNTs by electrochemical derivatization, which can alter their transport properties (Miller et al., 2001
). The findings suggest applications for CNTs as nanofluidic devices, e.g., filters.
In living cells exist analogous water channels. Most notable are aquaporins (AQPs), a family of membrane channel proteins, that are abundantly present in nearly all life forms (Borgnia et al., 1999
). Biological water channels are much more complex than CNTs, with irregular surfaces and highly inhomogeneous charge distributions. CNTs can serve as prototypes for these biological channels, that can be investigated more easily by MD simulations due to their simplicity, stability, and small size. But pristine CNTs are electrically neutral, and unable to reproduce some important features of biological channels. For example, MD simulations have revealed that water molecules in the AQP channels adopt a bipolar orientation which is induced electrostatically and is linked to the exclusion of proton conduction in AQP channels (Tajkhorshid et al., 2002
). However, one may modify CNTs through the introduction of charges to mimic AQP water channels. Below we describe how we have modeled accordingly several types of CNTs with representative charge distributions by means of MD simulations. We have investigated, in particular, the effect of charges on water conduction and water orientation. We also investigated proton conduction through the CNTs using the theory of network thermodynamics (Brünger et al., 1983
; Schulten and Schulten, 1985
, 1986
).
| METHODS |
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-helix has a net dipole moment whose magnitude corresponds to a charge of
0.50.7 e at each end of the helix (Branden and Tooze, 1991
-helices with one-half of the CNT length; in ntP0N, the net dipole moment mimics that of a single
-helix with the same length as the CNT. In these modified CNTs, we assign the charges to only a few carbon atoms rather than distributing them over many, in an attempt to mimic charged groups in biological channels such as AQPs, which usually have strong localized interaction with water molecules inside the channels. In the following, the simulations on nt0, ntP0N, ntNPN, and ntPNP are referred to as sim0, simP0N, simNPN, and simPNP, respectively.
All simulations were performed at constant temperature (300 K) and pressure (1 atm), and by using the PME method (Essmann et al., 1995
) for full electrostatics. Each of the four systems described above was simulated for 10 ns, with coordinates recorded every 1 ps. The first 200-ps of each simulation was discarded, and the rest of the trajectory was used for analysis. Version 2.5 of the program NAMD2 (Kalé et al., 1999
) was used for the simulations, with a performance of
12.6 h per ns on 16 processors of an IA-64 Linux cluster.
During the simulations, translation of the CNTs due to thermal fluctuation was observed. However, their aggregation remained very stable and the CNTs translated only collectively. All of the CNTs were empty initially, but filled up with water molecules within 200 ps. Water did not enter the gaps between CNTs, because in the chosen arrangement, the gaps were too narrow to accommodate water molecules (distance of 2.5 Å from gap center to nearest carbon atom).
| RESULTS |
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Water diffusion and orientation
Water molecules entering the CNTs form single files and move concertedly. Such water movement has been characterized by a continuous-time random-walk model (Berezhkovskii and Hummer, 2002
). The key parameter in this model, the hopping rate k (a hop is the translocation of the water file by a distance of the separation of adjacent water molecules), has been determined in our simulations and is provided in Table 2. According to the continuous-time random-walk model, the number p of permeation events (a water molecule crossing from one end to the other end of a CNT) per CNT, per ns, can be calculated from k (see Eq. A1 in the Appendix). Alternatively, p can be counted from the trajectories. Both the predicted and directly observed p-values from the simulations are listed in Table 2, where one can see that they are in agreement. The same pristine CNT (nt0) was studied in (Berezhkovskii and Hummer, 2002
; Hummer et al., 2001
; Kalra et al., 2003
) by MD using the AMBER force field, which gave mean hopping times (
= 1/k) of 13 ps for a single CNT in water (Berezhkovskii and Hummer, 2002
; Hummer et al., 2001
) and 20 ps for a layer of CNT arrays (Kalra et al., 2003
). In sim0 we observed a larger
-value (37 ps), which may be due to the difference in the force fields (AMBER vs. CHARMM) used. Indeed, it was pointed out in Hummer et al. (2001)
that the observed water behavior in CNTs is sensitive to the force field parameters. In comparison with biological channels, the conduction rate in sim0 (5.9 water permeation events per CNT per ns) is more than five times larger than that observed in simulations of AQPs (de Groot and Grubmüller, 2001
; Tajkhorshid et al., 2002
). This difference is due to the difference in the electrostatic environment in CNTs and AQPs. Indeed, among the four types of CNTs, the pristine CNT (nt0) has the fastest water conduction; in ntNPN, which resembles AQPs more closely, the water molecules exhibited remarkably lower mobility, with no permeation event and only a few hops of water observed in 10 ns.
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be the dipole of water molecule j, and let µjz be its z-component; then Dz is the sum of µjz divided by the sum of
for all water molecules inside a CNT. A Dz value of +1 or -1 would indicate a perfectly aligned water file along the z-axis. Histograms of Dz from sim0 and simP0N are provided in Fig. 3, where one can see that the Dz values are clustered near ±1, and few are close to zero. The distribution of Dz is symmetric for sim0 (solid curve) and asymmetric for simP0N (dashed curve). In simP0N, negative Dz values, corresponding to the water orientation in ntP0N of Fig. 2, exhibited a wider distribution than positive Dz values, mainly due to the interaction between the water molecules and the charged carbon atoms.
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The resistance of a proton channel
When an electromotive force (EMF) V, e.g., a voltage, is applied across a proton channel, a steady electric current J of protons through the channel will be induced. For small EMF, a linear (Ohmic) voltage-current relationship can be expected, i.e.,
![]() | (1) |
At the atomic level, a continuously conducting proton channel cycles periodically between states that are the intermediates of the conduction process. We first consider a simple case where only a single unbranched cycle exists, with states S1
S2
...
SN
S1. We assume that when the channel undergoes one full cycle and returns to the initial state, the net effect is one proton being transferred from one side to the other. It has been proven that the resistance of such a proton channel can be calculated from equilibrium, i.e., no EMF, properties (Brünger et al., 1983
) and is
![]() | (2) |
B denotes the rate constant of the transition A
B in equilibrium. PAKA
B is the number of transitions from state A to state B in unit time in equilibrium, which is also equal to the number of transitions from B to A due to detailed balance, i.e., PAKA
B = PBKB
A. Equation 2 shows that the total resistance has additive terms or subresistances, rAB = (kT/e)(1/PAKA
B), that are associated with each jump A
B between two adjacent states in the cycle. If the number of transitions between two adjacent states i and j, PiKi
j, is much smaller than others, its associated subresistance rij is the dominant component of the total resistance, and the jump between states i and j is the rate-limiting step of proton conduction.
For branched cycles, Kirchhoff's law can be applied to calculate the resistance of the complete network, in analogy to its use for electric circuits (Brünger et al., 1983
; Schulten and Schulten, 1985
, 1986
).
The resistance of nt0
Since CNTs do not donate or accept protons, we are only concerned with the configuration of water molecules inside CNTs. In this study, we adopt the symbolic diagram introduced in Brünger et al. (1983)
; Schulten and Schulten (1985
, 1986
) to denote the single file water configurations in nt0, as illustrated in Fig. 5 a. We note that, at any moment, each water molecule in the CNT has at least one inactive H atom (as marked by an arrow in Fig. 5 a) which does not participate in any H-bond. We define the skeleton of a water molecule as its O atom plus one inactive H atom. In our diagram, the skeleton is not shown, and only the H atom(s) not included in the skeleton are explicitly represented for the water molecule. We use a two-index code to denote the configuration of a water molecule in the CNT, the first and second indices representing the protonation state on the left and right sides of the oxygen atom, respectively. Each index is either X, meaning protonated, or O, meaning not protonated. Therefore, in our diagram, a water molecule can have four possible proton configurations: XO represents an H2O molecule whose dipole moment points to the left, which may donate a proton to its left or accept a proton from its right; OX represents an H2O molecule whose dipole moment points to the right; XX represents an H3O+ ion, which may donate a proton to either side; and OO represents an OH- ion, which may accept a proton from either side.
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i (i = 1, ...,N) represents the state in which the ith water molecule is an H3O+, i.e., XX. Similarly,
i (i = 1, ...,N) represents the (N + 1 - i)th water molecule being an OH-, i.e., OO.
i (i = 1, ...,N - 1) represents the state in which the ith and (i + 1)th water molecules have opposite orientations and thus are not connected by an H-bond, i.e., XO OX or OX XO.
Assuming the water chain to be initially in state E1, to conduct a proton from the left to the right, the system must first reach E2 through either E1
1
N
E2 or E1
1

N
E2, then come back to the initial state through E2
N-1
1
E1.
1
N is the process of translocating an H3O+ ion (or an excess proton) along the water chain;
1
N is the process of translocating an OH- ion (or a hole) from the right to the left, which is equivalent to transferring a proton from the left to the right (Brünger et al., 1983
). Note that the translocation of either an excess proton or a hole involves only the forming and breaking of the O-H bonds, and does not require large movement of the water molecules. E2
N-1
1
E1 is the process of reorienting the water chain through successive rotations of water molecules (Brünger et al., 1983
). The translocation of an excess proton and the reorientation of the water chain are often referred to as the hop and turn steps, respectively (Pomès and Roux, 1998
).
Applying Eq. 2 and Kirchhoff's law, the total resistance of the network in Fig. 5 b is according to Brünger et al. (1983)
and Schulten and Schulten (1985
, 1986
)
![]() | (3) |
![]() |
![]() |
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corresponds to the rate of spontaneous reorientation of the water chain in equilibrium; 1/
and 1/
correspond to the rates of spontaneous transfer of an excess proton and a hole from one side to the other side of the channel, respectively.
At neutral pH, a water molecule has equal probability to be protonated, i.e., to become an H3O+, or deprotonated, i.e., to become an OH-. We assume that the translocation rate of a hole along the water chain is also the same as that of an excess proton. In this case, the two pathways E1
1
N
E2 and E1
1
N
E2 have the same reaction rate, i.e., 
= 
, and Eq. 3 becomes:
![]() | (4) |

can be obtained from the spontaneous reorientation (flipping) rate observed in the simulations. In sim0, no reorientation event was observed in the twelve CNTs during 10 ns. Therefore, 
should be at least of the order of 100 ns. We assume 
200 ns = 2 x 10-7 s in this study. A much faster flipping rate (one per 23 ns) was observed in a single CNT during a 66-ns simulation (Hummer et al., 2001
), corresponding to a smaller 
. We note that in the mentioned study, the single CNT was immersed in bulk water, whereas in our simulations, the CNTs formed a tightly packed bundle which partitions bulk water into two layers separated by a 15-Å water-free layer. For comparison, we also built a system of a single CNT immersed in bulk water as in Hummer et al. (2001)
, and indeed observed one reorientation event in a 10-ns simulation on this system. Despite the uncertainty in the flipping rate, even if our large 
value is adopted, 
, as will be shown below, is still negligible when compared with 
. Therefore, the choice of 
will not have a large effect on the calculated resistance of nt0.
To calculate 
, we need to estimate the probability Pi of each state i and the transition rate Ki
j between adjacent states i and j. In equilibrium, E1 and E2 are by far the most populated states, so we have
. Previous studies have shown that an excess proton can hop through the water chain requiring little activation energy (Pomès and Roux, 1998
). Therefore we assume that each water molecule in the CNT has the same probability (Pprot) to be protonated, i.e.,
![]() | (5) |
2 x 10-9.
The activationless nature of proton hops also implies that the transition rates
are all close in value, and we assume that they all have the same value Khop. We further assume that the transition rates
and
are also identical to Khop, which means that a protonated water molecule (H3O+) at the end of the CNT has roughly equal probability to pass the excess proton to the next water molecule in the CNT and to bulk water. Altogether, the values are
![]() | (6) |
![]() | (7) |
1 ps (Pomès and Roux, 1998
1/ps = 1012/s, resulting in 
5 x 10-4 s.
Our estimate for 
is three orders-of-magnitude larger than 
, so 
can be neglected in Eq. 4, and the resistance of nt0 is
![]() | (8) |
i (i.e., small Pprot), the spontaneous transfer of a proton from one side to the other side of the channel is a much rarer event compared with the spontaneous reorientation of the water chain, and thus is the rate-limiting step for proton conduction at neutral pH. Since most of the above analysis does not involve specific properties of CNTs, the conclusions for nt0 may be generalized to other nonpolar single file water channels.
Small proton conduction in ntNPN
The description of proton conduction in nt0 can also be adopted to ntNPN, as illustrated in the corresponding diagram of protonation states in Fig. 6 a. However, in this case the water molecule in the center of the CNT needs to be treated differently from the remaining water molecules. Since both of its H atoms are involved in H-bonds with adjacent water molecules, it has no inactive H atom. Therefore, we define the skeleton of this water molecule as only its O atom and represent both of its H atoms in the diagram. Furthermore, since its O atom is strongly interacting with the positive charges of the CNT, it cannot accept an excess proton, although it may donate a proton. Therefore, this central water molecule can have three configurations: XX represents an H2O molecule; XO or OX represents an OH- ion.
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To evaluate the energy of each state in the proton conduction pathway, we define three types of faults, each coming with an energy penalty. When a water molecule becomes an H3O+ or OH-, it forms a so-called Bjerrum fault (ß) (Brünger et al., 1983
; Schulten and Schulten, 1985
, 1986
). When two adjacent water molecules do not have an H-bond in between, they are associated with a rotation fault (
) (Brünger et al., 1983
; Schulten and Schulten, 1985
, 1986
). Furthermore, in ntNPN, due to the internal electrostatic field generated by the CNT, each water molecule has a favorable orientation; if adopting the opposite orientation, the water molecule forms an orientation fault (
). In nt0, there exist faults ß and
with significant energy penalties, but no fault
, since there is no internal electrostatic field preferring one water orientation over the other.
The number of faults for each state is shown in Fig. 6 b, where one can see that some states are associated with three faults (either 1ß + 2
or 1ß + 1
+ 1
). In contrast, in nt0, each state is associated with at most one fault (either ß or
). If we assign to the faults ß,
, and
energies 20 kT, 8 kT, and 10 kT, respectively, and assume that the energy of faults is approximately additive, then the proton conduction pathway in ntNPN involves an energy barrier that is
20 kT higher than that in nt0. Therefore, ntNPN is expected to have a much lower conductivity for protons than nt0.
| DISCUSSION |
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Single-walled CNTs have delocalized
-electrons and exhibit semiconducting or metallic electrical conduction (Dresselhaus et al., 1996
). An external electric field can alter the electronic structure of a CNT and, hence, induce a nonzero charge distribution in the CNT wall. Therefore, even though pristine CNTs are electrically neutral, they can interact with other charged atoms through field-induced polarization. However, such polarization has not been accounted for in our present simulations. While our current approach could serve the purpose of modeling biological channels, it may not accurately describe the interaction between CNT and water. An improved force field that takes into account the polarizability of CNTs is desirable in future modeling. The choice of water model (Guillot, 2002
) is also worth further investigation.
AQP channels adopt a bipolar water orientation which is held responsible for proton blockage (Tajkhorshid et al., 2002
). We have demonstrated that a bipolar water orientation can be reproduced in a simple model CNT (ntNPN) and conclude that ntNPN like AQPs also blocks proton conduction. We have demonstrated, through a network thermodynamic description of proton conduction, that this is indeed the case. Our description assigns a high activation barrier to the proton conduction process in ntNPN. However, we observed low water conduction in ntNPN. Fortunately, ntPNP appears to function better in this respect. ntPNP has the opposite charge distribution as ntNPN, and, therefore, its water orientations are opposite to those in ntNPN (see Fig. 4), implying that they also effectively block proton conduction.
Water conduction is two orders-of-magnitude higher in ntPNP than in ntNPN. Apparently the water molecule in the center of ntNPN has very high affinity to the two positively-charged carbon atoms, which significantly reduces the mobility of the water chain in the CNT. Similar positive charges also exist in AQP channels, including the NH2 groups of two Asn residues and the side chain of an Arg residue (Fu et al., 2000
; Murata et al., 2000
; Sui et al., 2001
). However, AQPs permit fast water diffusion, which may be partly due to the conformational fluctuation of the protein. In general, it is not yet clear how water diffusion and permeation in narrow water pores are quantitatively related to their geometry and charge distribution. In view of this, CNTs with different diameters (Noon et al., 2002
), lengths, and charge distributions and their effect on water conduction are worth further investigation, which may shed light on the determinants of water and proton conduction rates in biological water channels.
In addition to serving as models for biological channels, different types of CNTs may also lead to technical applications. For example, chemically-modified CNTs may be designed for various capabilities, such as controlling water orientation or selectively permeating ions or protons. CNTs with high water permeation, but no ion conduction, could be used for desalination of sea water, where a hydrostatic pressure can be applied to push water through the CNTs with salt (ions) left behind.
| APPENDIX |
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In the continuous-time random-walk model (Berezhkovskii and Hummer, 2002
), the channel is always occupied by N water molecules in single file. They move concertedly and cannot pass each other, i.e., exchange positions, inside the channel. The water chain moves in hops (translocations by a distance of exactly one water molecule). In equilibrium, the leftward and rightward hopping rates are the same, denoted as k0, and the bidirectional hopping rate k is 2k0.
A rightward permeation event is defined as a water molecule entering the channel from the left reservoir and exiting to the right reservoir. A leftward permeation event is defined similarly. The moment at which the water molecule exits the channel is taken as the time for a permeation event. The number of permeation events is often used to quantify water conduction through channels by diffusion in MD simulations (de Groot and Grubmüller, 2001
; Tajkhorshid et al., 2002
). This number can be predicted by the continuous-time random-walk model, as described in Berezhkovskii and Hummer (2002)
. Here, we give an alternative derivation.
As shown in Fig. 7, at any time, there exists a boundary in the channel which separates the i water molecules which had entered the channel from the left reservoir and the N - i water molecules coming from the right reservoir. We define such configuration as state i. At any moment, the configuration is in one of the N + 1 states, from state 0 to state N. When a leftward hop occurs, a state i will transit to state i - 1 (see Fig. 7), except for i = 0, in which case a leftward permeation event leaves the system in state 0. Similar transitions will happen for rightward hops.
|
![]() | (A1) |
It is noteworthy that after a permeation event, the water configuration stays in state 0 or state N, which has a relatively high probability for another permeation event in the same direction to happen. Therefore, although the leftward and rightward hops are uncorrelated, the permeation events are expected to cluster in time. Indeed, clusters of unidirectional pulses of permeation events were observed in Berezhkovskii and Hummer (2002)
and Hummer et al. (2001)
.
| ACKNOWLEDGEMENTS |
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The present work was supported by grants from the National Institutes of Health (PHS 5 P41 RR05969), and from the National Science Foundation (CCR 02-10843). The authors also acknowledge computer time provided at the National Science Foundation centers by the grant from the National Resource Allocation Committee (MCA93S028). F.Z. acknowledges a graduate fellowship awarded by the UIUC Beckman Institute at the University of Illinois at Urbana-Champaign.
Submitted on January 31, 2003; accepted for publication February 27, 2003.
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M. O. Jensen, E. Tajkhorshid, and K. Schulten Electrostatic Tuning of Permeation and Selectivity in Aquaporin Water Channels Biophys. J., November 1, 2003; 85(5): 2884 - 2899. [Abstract] [Full Text] [PDF] |
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A. Kalra, S. Garde, and G. Hummer From The Cover: Osmotic water transport through carbon nanotube membranes PNAS, September 2, 2003; 100(18): 10175 - 10180. [Abstract] [Full Text] [PDF] |
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