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Biophys J, June 2002, p. 2833-2846, Vol. 82, No. 6
and
*Department of Chemistry, University of California, Davis,
California 95616 USA and
Institute
of Problems of Chemical Physics, Russian Academy of Sciences,
142432 Chernogolovka, Moscow, Russia
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ABSTRACT |
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Some proton pumps, such as cytochrome c oxidase (CcO), translocate protons across biological membranes at a rate that considerably exceeds the rate of proton transport to the entrance of the proton-conducting channel via bulk diffusion. This effect is usually ascribed to a proton-collecting antenna surrounding the channel entrance. In this paper, we consider a realistic phenomenological model of such an antenna. In our model, a homogeneous membrane surface, which can mediate proton diffusion toward the channel entrance, is populated with protolytic groups that are in dynamic equilibrium with the solution. Equations that describe coupled surface-bulk proton diffusion are derived and analyzed. A general expression for the rate constant of proton transport via such a coupled surface-bulk diffusion mechanism is obtained. A rigorous criterion is formulated of when proton diffusion along the surface enhances the transport. The enhancement factor is found to depend on the ratio of the surface and bulk diffusional constants, pKa values of surface protolytic groups, and their concentration. A capture radius for a proton on the surface and an effective size of the antenna are found. The theory also predicts the effective distance that a proton can migrate on the membrane surface between a source (such as CcO) and a sink (such as ATP synthase) without fully equilibrating with the bulk. In pure aqueous solutions, protons can travel over long distances (microns). In buffered solutions, the travel distance is much shorter (nanometers); still the enhancement effect of the surface diffusion on the proton flow to a target on the surface can be tens to hundreds at physiological buffer concentrations. These results are discussed in a general context of chemiosmotic theory.
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INTRODUCTION |
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Proton translocation across biomembranes is a key
step in biological energy conversion in mitochondria and
chloroplasts. The translocation is carried out by proton pumps,
membrane enzymes that utilize redox energy (or light energy in
photosynthetic systems) to move protons from one side of the membrane
to the other, thereby creating electrochemical gradients. Later, the
free energy stored in proton gradients is utilized in synthesis of ATP
or other energy-requiring processes (Skulachev, 1988
;
Cramer and Knaff, 1990
)
Proton pumps, such as cytochrome oxidase (CcO) (Wikström,
1998
), are very efficient
they are capable of pumping more
than 103 H+ per second (Babcock and
Wikström, 1992
). The corresponding time scale for overall
processing of a single proton is as short as 1 ms. Moreover, some
proton-transfer reactions during the catalytic cycle of CcO occur on
even a shorter time scale of 0.1 ms, and the reprotonation of some
protolytic sites of the enzyme from the bulk is believed to occur even
faster (Karpefors et al., 1999
, 2000
; Kotelnikov et al., 2001
).
Similar time scales of proton transfer reactions have been reported for
bacteriorhodopsin (Heberle, 2000
).
The high rate of proton pumping raises the question about the maximum
possible rate of supply of protons by the organelle's medium to the
pump, given the fact that the concentration of available protons is
limited and the diffusion occurs with only a finite speed (e.g., in the
bulk free protons diffuse with coefficient Db ~ 10
4
cm2s
1, see review in Gutman and
Nachliel, 1997
). Although the diffusion control has not been
directly implicated in proton pumps, such a diffusion-limited kinetics
does seem to occur in a number of proton-conducting channels
(DeCoursey and Cherny, 1999
). The absence of the
diffusion bottleneck in CcO is ascribed to a proton-collecting antenna
surrounding the entrance of the proton-conducting channel, which
enhances the proton influx from the solution to the channel entrance
(Gutman and Nachliel, 1997
; Brandsburg-Zabary et
al., 2000
). Hence, the rate of proton supply is modified by the
properties of the surface of the protein, or that of the surrounding
membrane. The lateral membrane diffusion has been also suggested to
occur in other proton-conducting systems (DeCoursey and Cherny,
1999
). The relevant question then is how to correctly estimate
such a diffusion-limited and surface-enhanced rate of proton supply
from the medium to the entrance of the proton-conducting channel.
The above question is complicated by the fact that the nature of the
protons participating in the process is not always known with
certainty. For instance, under physiological conditions, the
concentration of free protons in the organelles is of an order of
10
7 to 10
8M. Hence, in a typical organelle
with dimension of 1 µm, there will be only an order of one free
proton or less(!) on average. The splitting of water is energetically
unfavorable, hence the involved protons must belong to buffer molecules
that contain acidic or basic groups. These buffer molecules can be both
mobile and immobile, i.e., fixed on the surface of membrane proteins and on the membrane itself (Gutman and Nachliel, 1997
;
Brandsburg-Zabary et al., 2000
). The presence of fixed
and mobile buffers changes the effective concentration and mobility of
the protons (Junge and McLaughlin, 1987
).
The question of how the membrane surface can modify the proton
transport is also of interest in a more general context of chemiosmotic
coupling (Nicholls and Ferguson, 1992
; Ferguson, 1995
). Previously, it has been suggested that the diffusion of protons along the membrane may play a major role in translocation of
protons between the generators, such as CcO or bacteriorhodopsin, and
consumers, such as ATP synthase (Scherrer, 1995
;
Teissié, 1996
; Gabriel and Teissié,
1996
; Nachliel et al., 1996
; Antonenko and Pohl, 1998
; Krasinskaya et al., 1998
).
Long-distance migration of protons along membranes has been observed in
purple membranes and reconstituted bacteriorhodopsin (Heberle
and Dencher, 1992
; Alexiev et al., 1994
,
1995
; Heberle et al.,
1994
; Scherrer et al., 1994
; Nachliel et
al., 1996
; Riesle et al., 1996
). Long-range proton diffusion has also been observed along lipid (Gabriel et al., 1994
) and stearic acid monolayers (Slevin and
Unwin, 2000
; Slevin and Unwin proposed a similar model to what
is discussed in this paper, and analyzed it numerically. They found
that, for stearic acid monolayers, the surface diffusion coefficient is 1.2 × 10
5 cm2s
1). The
effect of the surface on the proton transport depends on its
properties
diffusion coefficient, nature of the lipid head groups,
their pKa, concentration, etc. (Scherrer,
1995
; Teissié, 1996
). Because these
properties are not easily defined, since the proposal of the
chemiosmotic theory, there has been a continuing debate about whether
the surface participates in the proton transport.
To formulate an exact criterion of when and how the surface can affect
the proton transport is also a nontrivial theoretical problem. Various
aspects of the effect of reduced dimensionality have been discussed by
many authors in a general context of diffusion-controlled ligand-receptor binding (Adam and Delbrück, 1968
;
Berg and Purcell, 1977
; Berg and Blomberg,
1976
; Hardt, 1979
, 1981
; Schranner and Richter, 1978
;
Berg, 1985
). It has been recognized that, when diffusion
is limited to one or two dimensions, for example, DNA molecule or a
membrane, the rate of finding the target can be significantly increased.
In our previous paper (Georgievskii et al.,
2002
), a phenomenological model was developed that
describes diffusion of protons near the entrance of a proton-conducting
channel. The transport of protons occurs both through the bulk and
along the membrane surface, which can exchange protons with the bulk.
There are two regimes of the proton transport. In the first regime, the
exchange between the bulk solution and the membrane is so fast that a
local equilibrium is always established between the surface and bulk concentrations at neighboring points. This case is most likely to occur
in a typical biological environment. In the second regime, the exchange
is slow, so that the local equilibrium is not established. A rigorous
solution of the model was obtained with no restrictions on the exchange kinetics.
In this paper, we present a detailed analysis and application of the fast exchange regime to the relevant experimental studies of proton migration along biological membranes. The plan of the paper is as follows. In the next section the model is presented and the fast exchange approximation is introduced. In the following section, the solution of the model is described and simplified derivation for the fast exchange regime is given in Appendix A. The concept of the capture radius is introduced in the next to last section. In the last section, we discuss the results and parameters of our model, and give numerical estimates for pure unbuffered and buffered aqueous solutions and the rate expression derived in this paper. The concept of proton lifetime on the surface, for which an explicit formula is derived in Appendix B, the extension of the theory to buffered solutions, and the capture radius are also discussed in the last section.
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MODEL |
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We consider the following idealized model. A half-space filled with a solution of protons (free or attached to buffer molecules) is limited by a membrane. The membrane is populated with protolytic groups and can exchange protons with the bulk. The protons can diffuse both in the bulk and on the surface of the membrane. The diffusion coefficients on the surface and in the bulk are different. There is a specific finite lifetime of the protons on the surface, during which protons can migrate along the surface. The protons are dynamically exchanged between the surface and the bulk. On the surface of the membrane, there is a sink (or a source) of the protons of molecular size through which protons are removed (supplied) to the system. (For simplicity we will talk about the removal of the protons from the system. The results for the reversed process are identical in the approximation considered in this paper.) We model this sink of the protons as an absorbing spot on the surface, such that, after a proton gets to this spot, it is immediately removed from the system. Thus, the absorbing conditions are ideal, and there is no reverse reaction with the sink. The absorbing spot models the entrance of the proton channel, through which protons are pumped out of the system. The questions in which we are interested are: 1) what is the maximum (diffusion-limited) rate at which protons can be collected (pumped out) from such a system, and 2) at what distance from the absorbing spot the equilibrium concentration both in the bulk and on the surface will be established. The former question is related to the efficiency of proton pumps and the latter to the discussion of the nature of chemiosmotic coupling between the source and the sink of the protons on the membrane. The effects of the finite size of the organelle on the results can be easily incorporated and will be discussed in the paper.
In a system of a finite size, after some transient period, a quasi-stationary flow and a distribution of the concentration of protons are established. In our idealized infinite model, these conditions can be described as completely stationary by assuming that there is a compensating source of the protons at infinity such that the equilibrium is maintained at an infinitely large distance from the sink.
The stationary proton concentration in the bulk,
n(x, y, z), obeys the three-dimensional
diffusion equation
|
(1) |
1s
1) and deprotonated with a monomolecular
rate of desorption koff (in units of
s
1). The rate of protonation is proportional to
0
, where
(x, y) is the
stationary surface density of protons captured at a given point
(x, y) at the surface, and
0 is the
concentration of the protolytic groups on the surface. We will consider
the case when the surface protolytic groups are far from saturation,
0, a regime that is practically the most
important one. Then the proton flux from the bulk to the surface is
given by the equation
|
(2) |
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The second assumption of the model is that there exists a long-range
connectivity between the protonatable groups on the surface (as
described, e.g., in the percolation model [Rupley and Careri, 1991
; Gutman and Nachliel, 1995
,
1997
]), resulting in a
Brownian proton migration along the surface. The stationary
concentration of the protons on the surface satisfies the
two-dimensional diffusion equation,
|
(3) |
n/
z at
z = 0 is a source of protons on the surface.
The proton channel entrance, which serves as a sink for both the bulk
and surface protons, is modeled by a circle of radius r0 on the membrane surface. Eqs. 1-3
supplemented by the absorbing boundary condition inside the channel
entrance and the equilibrium condition at infinity were solved in our
previous paper (Georgievskii et al., 2002
).
Qualitatively, there are two regimes of proton transport, depending on
the rate with which protons are exchanged between the surface and the
bulk. In the fast-exchange regime, each of the two Langmuir terms in
the right-hand side of Eq. 2 is much larger than the total diffusional
flux on the surface, the term on the left-hand side. Then the surface
density and the local bulk density of the protons in every point on the
surface are essentially in equilibrium and are related as
|
(4) |
|
(5) |


1, where M = mole/liter = NA × 10
3
cm
3 and NA is the Avogadro number.
Because
0 is the number of groups per unit surface,
L0 has a dimension of length. The physical
meaning of L0 is the height of a column in the
bulk equilibrium solution that contains the same number of protons as a
spot on the surface with the same area as the column's cross-section.
Eq. 5 is written for a pure (unbuffered) solution. In the presence of a
buffer, it is modified as discussed in the Discussion, Buffers.
Eq. 4 is a modified boundary condition to Eq. 1 (replacing Eq. 2) and
it provides a direct coupling between the surface and bulk diffusion.
The analysis shows (Georgievskii et al., 2002
) that the
formal condition for the local equilibrium described by Eq. 4 is
expressed in terms of two length parameters characterizing the system.
The first parameter,
|
(6) |
|
(7) |
|
(8) |
Ls, whereas the
opposite case, Lsb
Ls, corresponds to the slow exchange regime. In
this paper, we will consider in more detail the case of the fast
exchange because it is most relevant to the proton transport in
biological systems.
Using the cylindrical symmetry of the problem and the coupling
condition 4, we rewrite Eq. 3 as
|
(9) |
n(r, z), n'z =
n/
z at z = 0, and
Lsb is given by Eq. 6. A simplified method to
solve the coupled Eq. 1 and 9 with appropriate boundary conditions is
presented in Appendix A. The solution to these equations is the function n(r, z) given by Eqs. A1, A6, A8, and
A14. The function n(r)
n(r, z = 0) necessary to calculate the surface
proton flux in the next section is given by Eq. A15.
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THE RATE CONSTANT |
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The total rate of proton transport to the channel consists of two
proton fluxes, k = kb + ks. The bulk proton flux
kb through the channel is given by
|
(10) |
|
(11) |
The mechanism of proton transport to the proton channel is different
for different values of Lsb. If
Lsb
r0, the proton transport occurs mainly via absorption of protons from the bulk solution by the channel entrance, i.e., kb
ks. In this situation, one can neglect the
surface diffusion and replace Eq. 3 with
n'z = 0, r > r0. This is the standard model for proton
transfer. The rate constant of such a process is given by
(Crank, 1990
)
|
(12) |
r0. The distribution of the surface
density is given by the equation
|
(13) |
1.1229 (see Eq. A13), and
eq is the equilibrium concentration of protons on the
surface,
|
(14) |
|
(15) |
Lsb
r0, the expression for the rate has the same
form as Eq. 15, but, in the logarithmic factor, the length
Lsb is replaced with Ls.
In a different context, Berg (1985)For the purpose of comparison, the above equation is rewritten in the
form equivalent to the bulk rate, Eq. 12,
|
(16) |
|
(17) |
r0. The effect of the surface diffusion can now
be measured directly by comparing the effective radius of the channel
R0 with the actual radius
r0.
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THE CAPTURE RADIUS |
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The above-introduced effective radius of the channel R0 is a more or less formal parameter, which is useful for comparison with the usual bulk diffusion. It should not be confused with the actual size of the area on the membrane surface from which protons are collected to the channel in the process of the coupled surface-bulk diffusion. The size of such an area is described in terms of the capture radius, Rc. The latter is defined as the distance from which a proton once on the surface will be absorbed by the channel.
The capture radius Rc can be also understood as
a distance between a generator and a consumer of protons on the surface
of the membrane at which the exchange between the two occurs mainly via
the surface, before equilibrating with the bulk. The coupling between
the source and the sink in this case is said to be local. The opposite
case of delocalized coupling is realized when the source and the sink
are each in equilibrium with the bulk. The rate of absorption by the
consumer in this case will neither depend on the rate of proton
generation (assuming infinite volume), nor on the distance between the
generator and the consumer (Ferguson, 1995
).
The probability of capture by the channel via the surface diffusion is
described by the function,
|
(18) |
(r) from the equilibrium value
eq is due to absorption by the channel, and is a measure
of the probability that the proton will be absorbed by the channel from
a specified position. At the boundary of the absorbing channel,
= 0 and the probability is exactly one. At an infinitely large
distance from the channel,
=
eq and the
probability of absorption is zero.
From Eq. A15, we find that
|
(19) |
|
(20) |
1, because we assume Lsb
r0). Thus, the constant
C0 ~ 1, Eq. A13, is essentially
irrelevant in the above expression for Rc. It is
recalled that, here, we treated the case Lsb
Ls. In a general case, as shown by
Georgievskii et al. (2002)
|
(21) |
|
(22) |
r0 and r0 < r
Rc.
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DISCUSSION AND CONCLUSIONS |
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Summary
The surface can enhance the flow of protons to a target, such as
the entrance of a proton channel, via its low-pK protonatable groups
capable of catching protons from the bulk and then shuttling them along
the surface. If there are only a few such groups, then, quantitatively,
the enhancement can be expressed in terms of so-called virtual
bimolecular rate constants introduced by Gutman and coworkers (Yam et al., 1988
). When there are many such groups, and
the connectivity between them is established, the transport to the
target on the surface is a combined surface-bulk diffusion. The model
discussed in this paper refers to the latter type of proton transfer.
The theory developed allows one to evaluate the maximum
(diffusion-limited) rate at which a proton pump can translocate protons across a membrane. The model is phenomenological. It assumes that the
protons are collected by a proton channel in the membrane, and that
they can diffuse both along the surface and from the bulk toward the
entrance of the channel. There is a dynamic proton exchange between the
surface and the bulk, which is described by the Langmuir
adsorption/desorption kinetics. Such a coupling results in a nontrivial
coupled surface and bulk proton diffusion in the system. The surface
was assumed to be infinite, homogeneous, and characterized by a surface
proton diffusion coefficient, Ds, pKa of the surface protolytic groups,
pK
0 (the number of
groups per unit surface), and the parameters of the Langmuir
kinetics
the first-order rate constant of desorption,
koff, and the second-order rate constant of
adsorption, kon. The radius of the proton sink
on the surface is r0. The bulk protons are
characterized by the bulk diffusion coefficient
Db and the equilibrium bulk density
n0.
In this phenomenological description, we do not specify the precise
nature of the protonatable groups on the surface, but rather
characterize them by their pKa, their density
0, and the proton diffusion coefficient
Ds. The protonatable groups on the surface of
the protein (Gutman and Nachliel, 1997
), and the
protonatable lipid head groups of the membrane both can play the role
of the proton-transmitting elements on the surface (Scherrer,
1995
; Teissié, 1996
). In this section,
quantitative estimates will be made with the use of parameters from
Table 2, where the values of
pKa and
0 are characteristic of carboxylates
on the surface of proteins such as cytochrome c oxidase and
bacteriorhodopsin, and are in the range of values for protonatable
lipid head groups studied by Scherrer (1995)
.
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Modeling the channel entrance as a plain sink of a given radius r0 with free proton diffusion in its vicinity may look, at a first glance, as an oversimplification. Indeed it has been suggested that the entrance of protein proton channels may be surrounded by negative charges that provide a guiding electrostatic potential, which extends to some distances, leading to both directed and enhanced bulk diffusion toward the channel entrance. The range of action of the attracting potential, however, may be expected to be only of the order of the Coulomb cage radius, say, 7-14 Å. Because the phenomena described by the present model typically occur on a much larger scale, as we demonstrate below, this external "short-range" potential can be described in our phenomenological model by simply increasing the effective radius of the channel from a few angstroms to 10-15. The rate of surface transport, as we saw, only weakly, logarithmically, depends on the channel radius. Thus, the increase of the effective size of the channel may be insignificant. However, the relative contribution of the bulk and the surface transport may be indeed affected, because the bulk contribution is proportional to r0. This uncertainty in r0 should be kept in mind when estimates are made using this theory.
Within the model developed, the theory also allowed us to formulate a criterion of when the coupling between a source and a sink on the membrane surface is localized, i.e., the transport between the two occurs before the protons generated by the source are fully equilibrated with the bulk.
Both the issue of diffusion-limited transport and the range of delocalization of the surface protons are of interest in a general context of chemiosmotic theory of energy transduction.
The rate
In this paper, we treated the case of the fast exchange between
the surface and the bulk, a regime in which the surface and bulk
protons are in local equilibrium. Formally, the condition for the fast
exchange is Lsb
Ls.
The study of the opposite case of the slow exchange
(Georgievskii et al., 2002
),
Lsb
Ls, yields the expression for the rate similar to the one obtained here.
In the regime where the surface diffusion dominates the transport, in
both cases of the fast and slow exchange between the surface and the
bulk, the rate can be written in the form
|
(23) |
The effect of the surface on the maximum rate of absorption by the
channel is described in terms of the effective radius of the channel,
R0, as defined in Eq. 17. When
R0 is much larger than the actual radius of the
channel, r0, the surface-modified diffusion enhances the rate by a factor of
R0/r0. Analytical results
could be obtained in the regime where the surface dominates proton
transport, R0/r0
1, and the protonation of the surface is far from saturation,
eq
0. The latter condition makes
the coupling between the bulk and the surface linear.
Because the surface diffusion coefficient typically is not expected to
be much different from that of the bulk (the reported values for
Ds/Db are in the range of
10
3 to 1 [Heberle et al., 1994
;
Scherrer et al., 1994
; Slevin and Unwin,
2000
]), but the surface density can be much higher than the
equivalent bulk density (the measure is given by the equilibrium constant L0, see Eqs. 4 and 5), the surface can
provide an extremely high output of protons. For example, using
Ds = 10
5
cm2s
1 and other parameters from Table 2, we
obtain
dw = 4 µs by Eq. 8,
L0 = 170 µm by Eq. 5,
Lsb = 17 µm by Eq. 6,
Ls = 660 Å by Eq. 7,
Rc = 17 µm by Eq. 20, and
R0 = 2 µm by Eq. 17. Thus, the enhancement effect would be
R0/r0 ~ 104, provided that the surface available for the proton
diffusion was infinite.
If the proton diffusion on the surface around the channel entrance is restricted by a finite area, such as a cluster of protonatable groups of dimension Lmax and Lmax < Rc, then the enhancement factor is less than R0/r0. In this case, a proton, once adsorbed by the cluster with a high probability, will be dragged into the channel before returning to the bulk. The cluster, therefore, will act as an absolutely absorbing disk for which the rate of absorption is given by Eq. 12 where r0 should be replaced with Lmax. The effective radius of the channel, Reff, will be equal to Lmax, and the enhancement effect will be Lmax/r0.
In the opposite limit of Lmax > Rc the surface proton flow is independent of Lmax, and Reff is gradually approaching R0 somewhere between R0 and Rc. This behavior is schematically depicted in Fig. 1. One can see, therefore, that the length parameter Rc is a critical parameter that determines the rate, although formally the rate depends only logarithmically on it.
|
Above, we gave estimates of the effective radius of the channel and the surface enhancement effect for a pure unbuffered solvent. Buffers can change these estimates dramatically. However, the surface is still predicted to dominate the transport up to a high buffer concentration (see Buffers subsection).
In Fig. 2, the proton flux into the
channel due to the surface-diffusion mechanism is shown as a function
of the surface-diffusion constant. Within the assumed range of
Ds, the rate of proton supply to a channel may
vary from 105 up to 4 × 107
s
1. In cytochrome c oxidase, the rates of
internal proton transfer in different redox states of the enzyme were
estimated in the previous work from this group (Kotelnikov et
al., 2001
) to be (102-104)
s
1, so that, even at the lowest diffusional mobility on
the surface, the calculated rate of proton delivery is still
sufficiently high to prevent a bottleneck in CcO turnover. Further, in
the work cited, the proton channel was represented by a single
protonatable group that was in the fast equilibrium with the bulk at
the apparent protonation rate of 5 × 1011
M
1s
1, which is an order of magnitude higher
than that expected for a diffusion-controlled protonation from the
bulk. From Fig. 2, it is seen that, at the lowest diffusion constant,
the flux is 105 s
1, which corresponds to the
apparent bimolecular protonation rate from the bulk of 1012
M
1s
1 at pH = 7. Thus, the results
shown in Fig. 2 are consistent with our previous findings.
|
The high surface rate is due to a relatively high concentration of protons on the surface, their high mobility, and, most importantly, to the reduced dimensionality of diffusion. The latter results in practical independence of the rate of absorption on the actual radius of the channel. In contrast, the bulk diffusion to the channel is limited by the small size of the channel and a relatively low bulk density of protons.
An increased effective radius of the channel,
R0, is equivalent to the effect of a
proton-collecting antenna (Gutman and Nachliel, 1997
).
In the antenna model, special properties of the groups surrounding the
entrance to the channel are required (high mobility, overlap of their
Coulomb wells, etc.). We find that, in fact, any surface area
surrounding the channel that conducts protons can already significantly
increase the output of protons through the channel. That is, if the
enhancement of the infinite surface is significant,
R0/r0
1, a patch of
a similar surface with dimensions of Lmax < Rc can also serve as an enhancement factor of
the output of the channel. In this case, the proton conducting patch of
the surface is exactly equivalent to the antenna model of Gutman
and Nachliel (1997
; see also the Capture Radius subsection). In
contrast, when Lmax > Rc, only a part of the proton-collecting
collecting cluster will work as a collecting antenna, see Fig. 1. The
main point here is that no special properties, such as an extremely fast exchange between the groups of the antenna, are in fact required. The two-dimensional nature of the antenna can significantly relax the
requirements on the transport and the collecting properties of the
groups making up the antenna.
It is well recognized that the effect of the surface can be significant
only if the dwell time on the surface is relatively large. In this
case, the proton can migrate a long distance on the surface during its
dwell time, Ls
r0,
and Ls is often tacitly assumed to be the
natural length that determines the size of the region on the surface
from which protons can migrate to a target. We find, however, that such
a region, in fact, can be much larger than Ls,
and is equal to Lsb instead when
Lsb
Ls. Moreover, we find that this is a typical situation. When the exchange between the
surface and the bulk is fast (in the sense discussed in Model section
and below in the Parameters and Assumptions subsection), the proton can
many times desorb and be readsorbed by the surface, staying, on
average, close to the surface, and hence make use of the reduced
dimensionality of the space in which its migration occurs.
The surface depletion rate and the dwell time
The above result can be qualitatively understood if it is
recognized that the actual average time that the proton spends at or
near the surface,
l, is not the same as the inverse of
the desorption rate, k
1/2, and the depletion
time
l, apart from the numerical factor of the order of
one, is
|
(24) |

l ~ 1 s.
The capture radius
The capture radius Rc describes the maximum distance at which a source and a sink on the surface can exchange protons without full equilibration with the bulk. Thus, if the distance between the donor and acceptor is less than Rc, the coupling is localized.
Eq. 19 and a more general Eq. 22 provide expressions for the probability of capture of a proton that was initially localized on the surface at a distance r from the channel. We find that the capture radius Rc is the larger of two lengths, Lsb and Ls.
Recently, the question of the nature of communication between a source
and a sink on the membrane surface has been directly addressed
experimentally by studying two connected ion channels (Antonenko
and Pohl, 1998
). The reported distance of "direct" coupling
between the donor and acceptor is of the order of 100 µm, which is in
a remarkably good agreement with our estimate of
Rc = 17 µm in the Rate subsection above.
Similar distances in the micrometer range are measured by other authors
(Heberle and Dencher, 1992
; Heberle et al.,
1994
; Alexiev et al., 1994
, 1995
; Scherrer et
al., 1994
). Lateral proton movement on a macroscopic scale has
been also observed both in pure aqueous solutions and buffered
solutions (Gabriel et al., 1994
, and references
therein). We note that, according to the present theory,
Rc is a function not only of the properties of
the surface but also those of the buffers (see the Buffers subsection below).
It should be noticed that a distance as long as
Lmax = 100 µm between the source and the
sink requires a very long lifetime even if proton diffusion on the
surface is as fast as in the bulk. For Ds = 10
4 cm2s
1, one obtains
Lmax2/4Ds = 0.25 s. This long time clearly can not be a simple desorption time
dw (= 4 µs by the estimate given in the Rate
subsection). However, it is very close to our estimate of the surface
depletion time,
l ~ 1 s, given in the previous
subsection. Thus, the long distance of direct and local coupling can be
explained by the coupled surface-bulk diffusion considered in this paper.
In contrast to our calculations and the above-cited experimental data,
Gutman and coworkers derived from their experimental results that the
proton-collecting antenna consisted of a few (typically 2-3) surface
groups in a close vicinity of the fluorescein probe (Flu) and its
dimension did not exceed 30 Å (Gutman and Nachliel,
1997
). This disagreement might be a consequence of the way the
experimental data were described. A notable example is the work on
cytochrome c oxidase (Marantz et al., 1998
).
The Flu protonation on the enzyme surface was found to be mediated by one carboxylate (COO

), it is also obtained that the size of the antenna is
comparable to the dimension of the molecule. In other experiments by
Gutman and Nachliel (1997)
, where the antenna dimension was
found to be small, the contributions of distant groups might not be
properly resolved because the kinetic constants for all numerous
proton-transfer reactions were extracted from a single kinetic curve,
the protonation dynamics of the probe.
Parameters and assumptions
The phenomenological parameters of this theory listed in Table 2
are actually not all independent. For instance, the ratio of
on and koff for the
unbuffered solution is expressed in terms of pK
], bacteriorhodopsin [Nachliel and Gutman,
1996
], and cytochrome c oxidase [Marantz et
al., 1998
]). The absolute value of koff is expected to strongly depend on pK
), whereas that of
on on the
bulk diffusion coefficient Db, see Eq. 25.
It is recognized that the surface diffusion coefficient can depend on
both pK
), and the second is for the lateral movement. The first
barrier is always associated only with pK
; Gutman and Nachliel, 1990
,
1997
; Peitzsch
et al., 1995
). If the sites are close enough, the lateral
barrier will be small (due to overlaps of the neighboring wells), and,
for some range of values of pK




on requires a
detailed microscopic model of the surface and solving the diffusion
equation in the Coulomb potential, similar to the approach developed by
Agmon (1988)
for bulk reactions, which is beyond the
scope of the present paper.
The parameters Lsb and Ls
are also related. The rate constant of the diffusion-controlled
protonation of a single surface group from the bulk can be written as
(Crank, 1990
)
|
(25) |
|
(26) |
|
(27) |
It can be seen from the above relations that, to have an enhancement
effect in the transport rate ks, the dwell time
on the surface should be sufficiently large,
dw
r02/Ds, so
that Ls
r0 (see
Eqs. 7 and 8). Indeed, the first factor in Eq. 26 is
1 because both
the reaction radius and the target size are of the same order or
smaller than the separation between the surface groups. Therefore, if
Ls
r0, we obtain
Lsb
r0 as well,
and, according to the results of the Rate Constant section, no
enhancement effect would be obtained in this case. However, typically,
Ls is expected to be large and the condition
Ls
r0 to be satisfied.
In Eq. 27, the first factor is ~103 for the unbuffered
solution. For the reported values of
Ds/Db = 10
3
100 (Heberle et al.,
1994
; Scherrer et al., 1994
) one has
Lsb
Ls, i.e., only
the fast exchange regime is realized (see the Introduction). Thus, for
the unbuffered solutions, we obtain the estimate for Ls using d = 6 Å,
|
(28) |
170 µm, and therefore typically we have
Lsb
Ls.
Our final remark is on the conditions under which the surface and bulk
protons are in local equilibrium, resulting in Eq. 4. It is
qualitatively clear that it should be the case when the exchange rate
between the surface and the bulk is sufficiently high. It is not
immediately obvious, however, what this rate should be compared with
(to determine if it is indeed sufficiently high). The relevant estimate
can be obtained as follows. The formal condition could be directly
derived from Eqs. 2 and 3, where the terms describing the surface-bulk
exchange kinetics must dominate over the surface diffusion term. The
analysis shows that k
|
(29) |
dw
c. Using the definitions in Eqs.
7, 8, and 21, we obtain Lsb
Ls.
It is interesting to note that, because Lsb is
increasing quadratically with Ls, see Eq. 26,
the greater the length Ls is, the better
condition Lsb
Ls is
satisfied. The latter is a condition for the local equilibrium between
the surface and the bulk protons, which requires a fast exchange with
the bulk, i.e., a "short" dwell time. However, with increasing
Ls the dwell time of the proton on the surface
is increasing instead(!). The seeming contradiction is resolved when it
is recognized that, although with increasing Ls
the dwell time
dw does increase, the corresponding time
scale of the diffusion,
c, with which
dw
should be compared, increases even more rapidly due to its quartic
dependence on Ls.
Buffers
The present theory is easily generalized to the case when an
unsaturated buffer is present in the solution,
|
(30) |
Reaction 30 introduces proton generation/consumption in the bulk
(Nunogaki and Kasai, 1988
) with a characteristic time,
|
(31) |
const. Here and below, the primed
parameters refer to the buffered solutions. Using the parameters from
Table 2, we calculate the characteristic diffusion length
|
', Eq. 31, was obtained under the assumption that the
proton diffusion is sufficiently fast in comparison with that of the
buffer molecules and, therefore, [H+]
const. In the
oposite limit of slow proton diffusion, the supply of protons to the
reaction region will be a limiting factor, and reaction 30 can be
neglected as well.
In this situation, the concentration of the protonated buffer
molecules, [HB], plays the role of the concentration of free protons
in the solution. The proton flux F from the bulk to the surface can be written in a way identical to Eq. 2,
|
(32) |
|
(33) |
The diffusion coefficient D'b now
describes the diffusion of the buffer molecules in the solution. The
parameter L'0 for the buffered solution,
which comes into the expression L'sb = L'0(Ds/D'b) (cf. Eq. 6) can be written as
|
(34) |
eq is independent of the buffer. Substituting
Eq. 14 into Eq. 34, one finds
|
(35) |
This situation is different as compared to the pure unbuffered
solution, because the ratio
[H+]eq/[HB]eq can be several
orders of magnitude smaller than one. Hence,
L'sb, the capture radius
R'c (Eq. 21 with primed parameters), and
the effective radius of the channel,
|
(36) |
To discuss this issue quantitatively, we will write the expressions for
L'sb and
L's in the form
|
(37) |
|
(38) |
]
[B
]
is the total concentration of the buffer, and
|
(39) |
|
(40) |
r0.
However, L'sb is rapidly decreasing with