PMCCPMCCPMCC

Search tips
Search criteria 

Advanced

 
Logo of nihpaAbout Author manuscriptsSubmit a manuscriptHHS Public Access; Author Manuscript; Accepted for publication in peer reviewed journal;
 
Am J Physiol. Author manuscript; available in PMC 2010 June 2.
Published in final edited form as:
PMCID: PMC2879881
NIHMSID: NIHMS204084

Exchange of potassium and strontium in adult bone

Abstract

The kinetics of exchange of strontium (85Sr) and potassium (42K) were studied in the midtibial cortical bone of 37 adult dogs. After injection of these two tracer cations and tracer-labeled albumin into the tibial nutrient artery, two types of observations were made: 1) collection of sequential venous samples to provide the outflow indicator-dilution curves and to calculate the extraction and retention at early times; and 2) detection of energy-selected gamma emissions via a detector over the tibia to give the time course of content of 42K and 85Sr in the tibia. Extractions of K+ and Sr2+ were 50 and 60% during a single transcapillary passage. More Sr2+ than K+ was retained in the first minutes. Their rates of washout over a 3-h period were similar. The interpretation is that the rate of uptake at extravascular sites is faster for Sr2+ than for K+, as is the rate of release, and that the extravascular volume of distribution for Sr2+ (adsorption sites in the interstitium or on bone) is much larger than that for K+ (intracellular).

Keywords: bone-seeking isotopes, indicator-dilution curves, tracer kinetics, transcapillary passage, transport mechanism, residue function, fractional escape rate

talmage and meyer (30) expanded the original concept of Howard (9) to include the postulate that the extracellular fluid space of bone is compartmentalized by a layer of osteocytic cells lining the surfaces of bone. The identity of the cells making up this hypothetical membrane is unknown. The idea is that this layer acts as a membrane that maintains a concentration gradient between the fluid space adjacent to the bone mineral and the interstitial fluid (ISF), which is in equilibrium with the blood. Neuman (24) and Neuman and Neuman (23) have estimated, in the chick calvarium in vitro, that the potassium concentration in bone extracellular fluid is inexplicably high.

Because any compartmentalization of potassium is likely to be regulated at barriers to exchange, this implies the high probability of compartmentalization of calcium. It seems important, therefore, to compare and contrast the rate of exchange of potassium with that of calcium or its near analogue, strontium (2, 6, 13). The multiple indicator-dilution technique allows the examination of both capillary permeability and cellular uptake rates and is suitable for studying potassium and strontium simultaneously in that paired comparisons can be made. The uptake by bone of numerous bone-seeking isotopes is impeded by the capillary membrane, which acts only as a passive barrier (5, 1012). Sucrose, which is inert and is not transported across cell membranes, serves well in such studies as a second reference substance for extracellular distribution, and albumin still serves as the primary reference, being limited to the vascular space. With these aids, it was our goal to estimate the relative amounts of retention of K+ and Sr2+ by the dog tibia and to examine the transport rates and retention in the light of the possible existence of a specialized bone membrane.

The purpose of this study, therefore, was to compare the transcapillary extractions of potassium and strontium and their retention at brief times (2–3 min) and over the fllrst 3 h after injection and to try to interpret the observations in terms of membrane barriers and accessible volumes of distribution.

METHODS

Animal preparation

The animals studied were adult, male mongrel dogs weighing between 14 and 28 kg. All were given heparin (1,500 U) and anesthetized with intravenous pentobarbital sodium (30 mg/kg). The nutrient artery of the tibia was cannulated with a 0.58-mm ID cannula (Intramedic PE-50) for the injection tracers, as previously described (5). Stopping nutrient artery flow decreases clearance of 85Sr from the tibia1 diaphysis by about one-third (3). The cognate bed of the nutrient artery was perfused in some animals by collateral flow at about two-thirds of the normal flow (3), and in others the artery was continuously perfused at chosen rates with blood from the dog taken before any tracers were injected (17). The ipsilateral femoral vein was cannulated with a T cannula (5.3-mm ID), and tributary veins just proximal to the site were ligated to prevent tracer from bypassing the cannula via collaterals. For the collection of sequential samples from the T cannula for outflow dilution curves, the vein was clamped proximal to the T; by collection of the total outflow for 3 min and then unclamping, approximately 99% of the tracer could be accounted for as the sum of tracer in the outflow plus that retained in the bone (10).

A small volume of solution (0.25–1.0 ml) containing three radionuclides was injected into the nutrient artery, an intravascular reference tracer, albumin, and a pair of permeable tracers, either 14C-labeled sucrose and 42K or 42K and 85Sr. The doses were 10 or 15 μCi for the 51Cr- or 99mTc-labeled albumin, respectively, and 5–20 μCi for 14C-labeled sucrose, 42K, and 85Sr. The injection was given over several seconds by slow manual injection to avoid raising the pressure unnaturally in the nutrient arterial system. Blood samples were collected every 5 s for 3 min from the femoral vein. In dogs with pump perfusion of the nutrient artery, the injection of isotopes was given as a short pulse over a few seconds.

Fractional tracer content of the tissue [R(t)] was monitored for 3 h by a 2-in. thallium-activated sodium iodide crystal placed over the subcutaneous surface of the tibial diaphysis. The recorded activity of the fractional tracer content at time t [C*(t)] was divided by C*(0), the maximum value obtained after removal of the injection syringe and completion of the flush, so that

R(t)=C(t)C(0)
(1)

[Injection was an impulse input in all washout studies of 42K and 85Sr and would have exactly the form of residue function as defined by Zierler (33).] For the measurement of flow, in some experiments only, 15 μCi of 25I-labeled antipyrine (I-Ap) was injected quickly into the nutrient artery, and the area under the curve of R(t) was used to estimate the blood flow per unit volume of bone (3, 14). The I-Ap is washed out to a low level in 15–30 min. A detector placed over the opposite tibia indicated that recirculation was negligible.

At the end of 3 h the tibia was removed, cleansed of soft tissue, and weighed. The hematocrit (Hct) was either measured in the venous blood samples or, when the nutrient artery was perfused with blood, in the blood used for perfusion. When the nutrient artery was perfused, it was assumed that there was no additional collateral flow. With nutrient artery perfusion, the plasma flow (Fs; ml·100 g bone–1·min–1) equaled pump flow × (1 – Hct)/(wt of tibia). Flow values in these studies were similar to those used by Martin et al. (20) in an isolated tibial preparation and were well within the range for tibial diaphyseal cortical flow values observed by Morris and Kelly (21). When I-Ap washout was used, which provided FI-Ap, (ml·100 g bone–1·min–1), this was translated to plasma flow because the hydrophilic tracers sucrose, K+, and Sr2+ do not enter erythrocytes as I-Ap does, and thus Fs = FI-Ap (1 – Hct).

Isotopic activity of samples

For samples with 42K, 14C-labeled sucrose, and 51Cr-labeled albumin, the samples were counted in two channels of a gamma well counter (Nuclear Chicago, model C-120-1); then, after 8 days or more were allowed to pass for the decay of the 42K, the samples were counted again, as a check on accuracy, in a two-channel liquid scintillation system (Nuclear Chicago, Mark II) for the beta activity of 14C and 51Cr. For external detection, two channels were set up for the gamma peaks of the pairs of tracers. In three preliminary experiments, maximum values of instantaneous extraction (Emax) were calculated from the transport functions [h(t)'s] for potassium from both whole blood and plasma: the Emax estimates were 0.76 vs. 0.77, 0.44 vs. 0.38, and 0.54 vs. 0.58. These differences were not significant. Therefore, for venous samples of gamma emitters, either whole blood, accounting for the hematocrit, or plasma samples could be used; the results were as accurate with one method as with the other.

The dosages injected were calibrated by counting aliquots of the injectate, whose volume in the injection syringe was measured. The venous outflow dilution curves were normalized to h(t), the fraction of dose reaching the femoral vein per unit time, by

h(t)=C(t)Fvq0
(2)

where C(t) is the tracer concentration (in counts/min) in the outflowing blood, Fv is femoral vein flow, and q0 is total counts from the injectate per minute. From the curves hR(t) for the reference tracer albumin and hD(t) for a permeating tracer, one can compute an apparent instantaneous extraction

E(t)=hR(t)hD(t)hR(t)
(3)

as demonstrated by Crone (4). In the ideal situation, when this extraction represents a unidirectional flux out of the blood into an extravascular region, one can calculate a permeability-surface area product (PSc) for the barrier that encloses the blood in the exchange region by the Crone-Renkin formula (4, 27)

PSc=Fsloge(1Emax)

or

PScFs=loge(1Emax)
(4)

where Fs is plasma flow and Emax is an estimate chosen from E(t) (the instantaneous apparent fractional extraction of a permeating species), usually the maximum smoothed value occurring during the upslope or peak of hR(t). We have reason to doubt that this formula is adequate for the estimation of PSc in these studies; we suspect that return flux of tracer from the extravascular region to the bloodstream reduces the apparent extractions and leads to underestimation of PSc by Eq. 4 (1, 7). If permeation is a purely passive process in bone, as it appears from the data of Lemon et al. (17), the ratio of PSc's would be expected to be equal to the ratio of free-diffusion coefficients, given that the passages are uncharged and that there is no steric hindrance and no binding of solutes to endothelial surfaces. For reference, the diffusion coefficients are DK+ = 1.99 × 10–5, Dsr = 1.33 × 10–5, and Dsuc = 0.52 × 10–5 cm2/s in water at 25°C (19, 28). The permeant tracers, 85Sr and 42K, will be retained in bone longer than the reference tracer, labeled albumin. This retention at any specific time (T) after injection can be estimated from the venous outflow dilution curve

Enet(t)=0T[hR(t)hD(t)]dt0ThR(t)dt
(5)

The fraction of the injected dose remaining in the tissues is also provided by the detection of gamma emissions over the tibia, giving R(t), as in Eq. 1. When the reference tracer curve is complete, i.e., when all the albumin has washed out and hR(t) = 0 at times greater than 2 or 3 min, then Enet) = R(t) for the permeating tracer.

Blood flow, FI-Ap (ml·100 g bone–1·min–1), was estimated from the I-Ap residue function or washout curve, R(t), with the use of a modification of the height-area method of Zierler (14, 33)

FI-Ap=100λρb1R(T)0TR(t)dt
(6)

where R(t) = C*(t)/C*(0), so that 1 represents the activity over the tibia initially when all the dose was introduced; λ is the tissue-blood partition coefficient for antipyrine (11); and ρb is the specific gravity of the bone (11). T was chosen to be 15 min when R(T) was 10% or less.

The fractional escape rate (FER) is the ratio of the rate at which the tracer is leaving the tissue to the amount stiIl residing within the tissue at each time, t

FER=ΔRΔtR(t)
(7)

The FER may also be written as d loge R(t)/dt, which makes it obvious that the FER is equivalent to a rate constant at each time t, by measurement of the local logarithmic slope, such as taking the slope at each time on a semilogarithmic plot.

RESULTS

A typical outflow dilution curve is shown in Fig. 1 for albumin, sucrose, and potassium injected into a nonperfused nutrient artery. The return flux of sucrose is earlier than that for potassium, even though its estimated permeability-surface area product, PSc is less; this indicates its smaller volume of distribution in the extravascular region. However, even at 3 min, the Enet for sucrose is still about 15%, which indicates that there is a barrier to washout. For K+ the retention is about 40% at t = 3 min, which is less than that for highly cellular organs but is still quite high in comparison with sucrose and therefore indicates a process of sequestration (cellular uptake or binding) in the extravascular region.

FIG. 1
Outflow dilution curves from femoral vein obtained after injection of 51Cr-labeled albumin, 14C-labeled sucrose, and 42K into tibial nutrient artery at time zero. Fractional extraction for K+ is higher than that for sucrose. Return of tracer from interstitial ...

Tramcapillary extractions of K+ and Sr2+

MAXIMAL INSTANTANEOUS EXTRACTION

In 12 such experiments (Table 1), the mean Emax for 42K was 0.58 ± 0.10 and for sucrose 0.32 ± 0.10. The mean ratio of K+ and sucrose permeability coefficients (PK/Psuc) of 2, 28 was substantially less than the ratio of their free-diffusion coefficients, which is 3.8. We interpret this difference as being caused by substantial underestimation of PSc for potassium; this occurred in spite of its greater retention, which reduces the return flux. This interpretation presumes that the return flux is not slowed because of the positive charge, an inference made from the study of Lemon et al. (17). They showed that there is no difference between the extraction of Sr2+ and that of F; these have the same diffusion coefficients but opposite charges.

TABLE 1
Emax and PS/F values from indicator-dilution curves of 42K and [14C]sucrose

[In a similar set of experiments that made use of albumin, sucrose, and strontium, Davies et al. (5) observed that PSr/Psuc was 1.91 ± 0.35 (SD; n = 11), which was also less than the ratio of free-diffusion coefficients, 2.56. If potassium and strontium were compared on the basis of these results, the prediction of PK/PSr would be 2.28/2.56, or 0.89, again less than the ratio of free-difision coefficients, which is 1.50. However, this determination is quite indirect.]

Paired comparisons of K+ and Sr2+ were made in seven experiments (Fig. 2 and Table 2). The critical points are that 1) the h(t)'s for Sr2+ were consistently lower than those for K+; 2) the maximal values of the instantaneous extraction E(t), Emax were greater for Sr2+; and 3) the retention at 3 min was greater for Sr2+. The ratios of apparent permeabilities from Eq. 4, PK/PSr, averaged 0.83, which is much less than the ratio of free-diffusion coefficients, DK/DSr, of 1.5. This leads one to suspect that the estimates of the PSc's from Eq. 4 are erroneous, for the reduction in ratio is what one would expect when the conditions of Eq. 4 are not fulfilled (there should be no return flux) and the return flux of K+ would be proportionally greater for K+ than for Sr2+, because retention of Sr2+ is greater.

FIG. 2
Dilution and fractional extraction curves for 42K and 85Sr. 42K crosses downslope of reference curve before 85Sr crosses reference curve; note that E(t) goes to zero earlier for K+. This was true in all 7 expts. Similarly, the retention, Enet (t), of ...
TABLE 2
Emax, Enet, and PS/F values from indicator-dilution curves of K+ and Sr2+ by perfusion of nutrient artery region via collaterals

To verify that these low ratios of PK/PSr were not simply a result of inadequacy of perfusion in the tibia with unperfused nutrient arteries, we performed a series of unpaired experiments with continuous perfusion of the nutrient artery with blood. The results are listed in Table 3, and the observed Emax's for K+ and Sr2+ are given in Fig. 3. As expected from the Crone-Renkin equation (Eq. 4, the continuous lines for PSc's at 0.5, 1.0, and 2.0 ml/100 g–1·min–1), the Emax's did diminish at higher flows. However, just as with the paired experiments, the ratios of PK/PSr at any chosen flow, Fs, are seen to be lower than the ratio of DK/DSr; the PSc's averaged 0.83 ± 0.25 (n = 9) for K+ and 0.99 ± 0.32 (n = 7) for Sr2+, the unpaired ratio PK/PSr, being 0.84. Thus all three series of experiments gave estimates of PK/PSr in the range 0.83–0.89 on a total of 28 observations for K+ and 25 for Sr2+. Perfusing the nutrient artery at normal rates therefore made no difference in the relative extractions, and this reaffirms the impression that the extraction data should not be interpreted by means of the simplest capillary exchange model (Eq. 4), which does not account for return flux of tracer to the blood.

FIG. 3
K+ and Sr2+ extraction at different values of plasma flow during perfusion of tibial bone with blood. All points but one fall between curves for Eq. 3 and PSc values of 0.5 and 2.0. Curves were given by Eq. 3.
TABLE 3
Comparison of extraction for 42K and 85Sr by pump perfusion of tibial nutrient artery with blood

net extractions at T = 3 min. The forms of Enet(t) for K+ and Sr2+ are illustrated in Fig. 2 for a tibia perfused via its own collateral circulation. They are similar to those obtained with pump-perfused nutrient arteries. The retention of Sr2+ is consistently greater than that of K+. The data for a particular time, T = 3 min, for the net extraction Enet(t) (Eq. 5) are provided for autoperfused midtibias in Table 2 (a paired comparison between K+ and Sr2+) and for pump-perfused nutrient arteries in Table 3 (unpaired comparison). The values for Enet (T = 3 min) for K+ were not different in the two sets, the overall mean for K+ being 0.30 ± 0.10 (n = 16) and that for Sr2+, 0.45 ± 0.09 (n = 14).

The longer retention of Sr2+ probably explains why the extractions for Sr2+ were as high as those for K+ despite the lower diffusion coefficient. The mechanism is that retention in the tissue retards return flux of Sr2+ and causes the curve of E(t) to be higher than it would be if there were more return flux. This improves the accuracy of estimating PSc from E(t) by Eq. 4, but it does not mean that the estimates of PSc are wholly accurate for Sr2+, for they could well be significantly underestimated, and probably are. However, the important feature is the dramatic difference between K+ and Sr2+ in retention at 3 min, for both of these ions have significant volumes of distribution in bone (6).

Retention of Sr2+ and K+ over 3-h periods, R(t)

The retention of K+ and Sr2+ at longer times was examined by recording simultaneously for 3 h the intraorgan content, R(t), for 42K and 85Sr in six dogs with collateral-perfused nutrient artery regions. R(t) at zero time is the peak count recorded over the tibia and is 100%. Washout of K+ was more rapid during the first minute after injection of the tracers, as expected from the curves of Enet(t). After the first minutes, however, the rate of washout, the FER's (Table 4), became similar for K+ and Sr2+. The similarity in FER's during the period from the end of the 1st min to the 30th min, from the 30 to 60th min, and from the 60 to 150th min is shown in Table 4. The corollary of this similarity is that the greater retention of Sr2+ during the 1st min continues throughout the period of observation. The curves of Fig. 4 are approximately parallel, Sr2+ being higher, and only two of the curves show a tendency for RSr(t) and RK(t) to approach each other. Because of the larger retention for Sr2+, the parallelism shows directly that the absolute rate of loss for Sr2+ is greater than that for K+. The generality that is being demonstrated is that an FER is equal to a conductance for escape of tracer divided by its volume of distribution in the tissue; since the volume for Sr2+ is larger than that for K+, the conductance must be larger also.

FIG. 4
Residue functions (washout curves) for tracer potassium and strontium from dog tibia after introduction into the nutrient artery. Data obtained at 0.5-min intervals for the first 5 min and at 2-min intervals thereafter. Ordinate is on a logarithmic scale; ...
TABLE 4
Fractional escape rates of K+ and Sr2+

The scales used in Fig. 4 need comment. The use of the logarithmic ordinate is common practice for tracer washout curves when the abscissa is a linear function of time. On such plots, these curves tend to be concave upward, indicating that the washout curves are not monoexponential. The geometric progression of times in the abscissas in Fig. 4 is also a log scale, which serves to shorten the length of the plots. A monoexponential curve, exp(–t/16), is shown in the upper left panel to illustrate how far from monoexponential the R(t)'s are. It is interesting that the plots give nearly straight lines; the straight lines drawn through the data have the general form

R(t)=R(t0)(tt0)m
(8)

where t0 is an arbitrary time on the straight line and –m is the slope on the log-log plot. These slopes, from the data of Fig. 4, were similar for K+ and Sr2+, ranging from 0.08–0.25 (these extremes were both Sr2+) and averaging 0.13 ± 0.05 (n = 12). Note that this is purely an empiric descriptive approach, which cannot be entirely interpreted as providing physiological insight.

The curves of Fig. 4 exhibit one feature that may be meaningful. Those for K+ tend to be straight, whereas those for Sr2+ are bowed upward rather slightly but quite consistently. This difference may reflect some physiological feature of the system such as the nature of the process retaining Sr2+ in the tibia, e.g., diffusion into a surface region.

The residue curves were also recorded in the same dogs with pump-perfused nutrient arteries (Fig. 5). The Enet's are given in Table 3. The retentions at 60 min averaged 11.5 ± 2.2% (n = 3) for K+ and 21.9 ± 11.4% (n = 7) for Sr2+. As in Fig. 4, all of these curves showed rapid washout in the first minute and then slower, more prolonged washouts. At 120 min, the R(t)'s averaged 8.8 ± 4.0% (n = 3) for K+ and 17.7 ± 9.5% (n = 7) for Sr2+, still twice as much Sr2+ retained as K+.

FIG. 5
Residue functions—curves of tracer content, R(t)'s—are plotted against Fs × t (plasma flow × time). Fs, is plasma flow produced by pumping blood of known hematocrit through tibia1 nutrient artery.

DISCUSSION

There are differences in the behaviors of Sr2+ and K+. This finding is not very surprising, for the kinetics of Sr2+ exchange appear to be virtually identical to those of Ca2+ (16), and the divalent cation is the key one in bone crystal structure. K+ is the normally abundant intracellular cation, which is high in concentration in the free ionic state in cells. For example, Hinke (8) showed that its concentration was 150–200 mM in barnacle muscle cells, and Lee and Fozzard (15) found it to be at a level of 134.9 mM in cardiac muscle cells. Neuman et al. (25) found that K+ was not taken up in hydroxyapatite crystals; later, Triffitt et al. (32) demonstrated in rats that it was completely exchangeable. Contrarily, Sr2+ and Ca2+ certainly are not completely exchangeable, and the exchange rates of the crystals in bone probably take years, as was found for radium deposited in bones.

The comments bring out the conundrum posed by our data: Sr2+ is more rapidly extracted from the blood in a single passage than K+ and most probably cannot enter its whole volume of distribution; K+ has a higher diffusion coefficient but a lower initial extraction, but then the fraction that has entered the extravascular region in bone is retained about as well as the Sr2+, despite the fact that its immediate volume of distribution is smaller. How can these apparent conflicts be resolved?

Perhaps a better quantitative approach to the problem might be obtained by using complex multiunit capillary-ISF-cell-bone matrix (and surface) models to account for the possible fluxes. The multiunit models of Rose et al. (29) and of Levin et al. (18), however, are probably not wholly suitable; they do account for cellular uptake and return flux but do not account for surface binding with diffusion into and out of a bone matrix. Even so, the main features of the processes for K+ and Sr2+ appear to be at least qualitatively explicable in terms of a capillary-ISF-cell system.

The increased initial extraction of Sr2+ compared with K+ is not explicable on the basis of a tightly limiting capillary barrier, for K+ should have a higher permeability in any passive diffusional permeation process. Therefore, the explanation must be beyond the membrane: if both K+ and Sr2+ had a high permeability so that return flux from the ISF to blood was rapid, the E(t) for Sr2+ would become higher than that for K+ if it is taken up more quickly than K+ at some site in the ISF. Cellular uptake of K+ is usually quite rapid; in the heart, the sarcolemmal exchange constant (PScell) is about 2 ml·g–1·min–1, which is many times higher than the flow in bones. But explaining the observations requires that the rate of unidirectional uptake of Sr2+ be higher than that of K+; and if this is not likely to occur in the cells, then an alternative is adsorption of Sr2+ at superficial sites on bone matrix. This idea has the virtue that surface-binding processes are rapid, more so than membrane transport processes. Of course, these events need not all take place on bone surface; Sr2+, Ca2+, La3+ all bind to cell surfaces on the glycocalyx.

If that explains the more rapid extraction of Sr2+ than of K+, how can the similarity of the washout rates in Figs. 4 and and55 be explained? In general, escape from a cell has a rate constant equal to the permeability-surface area product (PScell) divided by the intracellular volume of distribution (Vcell). The values of the FER (in Table 4) for t = 30–60 min for K+ are about 4 × 10–3/min, whereas for the heart, where the perfusion is about 100-fold higher, the rate at t = 30–60 min observed by Tancredi et al. (31) was only about 15 × 10–3/min, about four times higher in a highly cellular tissue. Thus the FER for K+ is quite compatible with loss from an intracellular capacitance.

One might take this one step further. Because the FER is dominated by PScell/Vcell for K+, PScell can be estimated. Taking the cell space to be about 4% of bone volume (22) and with a K+ concentration of 5 mM in plasma and 150 mM in the available cellular water (80% of the cell), the Vcell for K+ would be 0.8 × 0.04 × (150/5) = 0.96 ml K+ space/ml bone. Then PScell = Vcell × FER = 0.96 × 4 × 10–3 = 3.84 × 10–3 ml·ml bone–1 min−1. This again is compatible with K+ permeabilities in myocardium when one considers the relatively small volume of cells in bone, 4%, as compared with the heart, 80% (26). It should be emphasized that these represent studies in a mature dog.

Making calculations regarding the basis of the efflux for Sr2+ is not as easy, but it is clear from the upward bowing of the Sr2+ in Fig. 4 that the process is different from that for K+. The shape is compatible with release from a surface. The slight increase in steepness with time of the R(t) in Fig. 4 is of the type seen with the transport in an organ dominated by flow but with a very large volume of distribution. This would apply to Sr2+ if the capillary permeability were high and the rate constant for exchange over a large surface area were also very high.

We conclude, therefore, that K+ and Sr2+ are not greatly limited in their exchanges by the capillary barrier in these experiments but that their extravascular retention is by surface adsorption for Sr2+ and cell uptake for K+.

Acknowledgments

The authors are grateful to Glenn Christensen for his technical assistance and to Rose M. Garmers, Paddy O'Brien, and Karen Connelly for preparation of the manuscript.

This investigation was supported in part by Research Grant AM-15980 from the National Institutes of Health, Public Health Service. Dr. Bassingthwaighte's efforts are supported by National Institutes of Health Grant HL-19139.

REFERENCES

1. Bassingthwaighte JB. A concurrent flow model for extraction during transcapillary passage. Circ. Res. 1974;35:483–503. [PMC free article] [PubMed]
2. Bauer GCH. Kinetics of calcium and strontium metabolism in man. In: Rodahl K, Nicholson JT, Brown EM Jr., editors. Bone as a Tissue. McGraw; New York: 1960. pp. 121–122.
3. Cofield R,H, Bassingthwaighte JB, Kelly PJ. Strontium-85 extraction during transcapillary passage in tibial bone. J. Appl. Physiol. 1975;39:596–602. [PMC free article] [PubMed]
4. Crone C. Does “restricted diffusion” occur in muscle capillaries? Proc. Soc. Exp. Biol. Med. 1963;112:453–455. [PubMed]
5. Davies DR, Bassingthwaighte JB, Kelly PJ. Transcapillary exchange of strontium and sucrose in canine tibia. J. Appl. Physiol. 1976;40:17–22. [PubMed]
6. Day JB, Kelly PJ. Volume of distribution of 85Sr and 42K in cortical bone of normal, hypoparathyroid, and hyperparathyroid dogs (Abstract). Federation Proc. 1979;38:1186.
7. Guller B, Yipintsoi T, Orvis AL, Bassingthwaighte JB. Myocardial sodium extraction at varied coronary flows in dogs: estimation of capillary permeabihty by residue and outflow detection. Circ. Res. 1975;37:359–378. [PMC free article] [PubMed]
8. Hinke JAM. Solvent water for electrolytes in the muscle fiber of the grant barnacle. J. Gen. Physiol. 1980;56:521–542. [PMC free article] [PubMed]
9. Howard JE. The biological mechanisms of transport and storage of calcium. Can. Med. Assoc. J. 1971;104:699–703. [PMC free article] [PubMed]
10. Hughes SPF, Davies DR, Bassingthwaighte JB, Knox FG, Kelly PJ. Bone extraction and blood clearance of diphosphonate in the dog. Am. J. Physiol. 1977;232:H341–H347. Heart Circ. Physiol. 1. [PubMed]
11. Hughes SPF, Lemon GJ, Davies DR, Bassingthwaighte JB, Kelly PJ. Extraction of minerals after experimental fractures of the tibia in dogs. J. Bone Jt. Surg. Am. Vol. 1979;61:857–866. [PMC free article] [PubMed]
12. Kelly PJ, Bassingthwaighte JB. Studies on bone ion exchanges using multiple-tracer indicator-dilution techniques. Federation Proc. 1977;36:2634–2639. [PubMed]
13. Kelly PJ, Maltby B, Lemon GJ, Bassingthwaighte JB. Extraction and retention of 42K, 85Sr, and 47Ca in canine tibial bone (Abstract). Physiologist. 1978;21(4):63.
14. Kelly PJ, Yipintsoi T, Bassingthwaighte JB. Blood flow in canine tibial diaphysis estimated by iodoantipyrine-125I washout. J. Appl. Physiol. 1971;31:38–47. [PMC free article] [PubMed]
15. Lee CO, Fozzard HA. Activities of potassium and sodium ions in rabbit heart muscle. J. Gen. Physiol. 1975;65:695–708. [PMC free article] [PubMed]
16. Lemon GJ, Bassingthwaighte JB, Kelly PJ. Influence of parathyroid state on calcium uptake in bone. Am. J. Physiol. 1982;242:E146–E153. Endocrinol. Metab. 5. [PubMed]
17. Lemon GJ, Davies DR, Hughes SPF, Bassingthwaighte JB, Kelly PJ. Transcapillary exchange and retention of fluoride, strontium, EDTA, sucrose, and antipyrine in bone. Calcif. Tissue Int. 1980;31:173–181. [PMC free article] [PubMed]
18. Levin M, Kuikka J, Bassingthwaighte JB. Sensitivity analysis in optimization of time-distributed parameters for a coronary circulation model. Med. Prog. Technol. 1980;7:119–124. [PMC free article] [PubMed]
19. Longsworth LG. Diffusion measurements, at 25°, of aqueous solutions of amino acids, peptides, and sugars. J. Am. Chem. Soc. 1953;75:5705–5709.
20. Martin KJ, Freitag JJ, Conrades MB, Hruska KA, Klahr S, Slatopolsky E. Selective uptake of synthetic amino terminal fragment of bovine parathyroid hormone by isolated perfused bone. J. Clin. Invest. 1978;62:256–261. [PMC free article] [PubMed]
21. Morris MA, Kelly PJ. Use of tracer microspheres to measure bone blood flow in conscious dogs. Calcif. Tissue Int. 1980;32:69–76. [PubMed]
22. Morris MA, Lopez-Curto JA, Hughes SPF, An K-N, Bassingthwaighte JB, Kelly PJ. Fluid spaces in canine bone and marrow. Microvasc. Res. In press.
23. Neuman MW, Neuman WF. On the measurement of water compartments, pH, and gradients in calvaria. Calcif. Tissue Int. 1980;31:135–145. [PubMed]
24. Neuman WF. The milieu interieur of bone: Claude Bernard revisited. Federation Proc. 1969;28:1846–1850. [PubMed]
25. Neuman WF, Tosibara TY, Mulryan BJ. Synthetic hydroxyapatite crystals. I. Sodium and potassium fixation. Arch. Biochem. Biophys. 1962;98:384–390. [PubMed]
26. Polimeni PI. Extracellular space and ionic distribution in rat ventricle. Am. J. Physiol. 1974;227:676–683. [PubMed]
27. Renkin EM. Transport of potassium-42 from blood to tissue in isolated mammalian skeletal muscles. Am. J. Physiol. 1959;197:1205–1210. [PubMed]
28. Robinson RA, Stokes RH. Electrolyte Solutions: The Measurement and Interpretation of Conductance, Chemical Potential and Diffusion in Solutions of Simple Electrolytes. 2nd ed. Butterworth; London: 1970. p. 513.
29. Rose CP, Goresky CA, Bach GG. The capillary and sarcolemmal barriers in the heart: an exploration of labeled water permeability. Circ. Res. 1977;41:515–533. [PubMed]
30. Talmage RV, Meyer RA., Jr. Physiological role of parathyroid hormone. In: Greep RO, Astwood EB, editors. Handbook of Physiology. Endocrinology. VII. Am. Physiol. Soc.; Bethesda, MD: 1976. pp. 343–351. sect. 7.
31. Tancredi RG, Yipintsoi T, Bassingthwaighte JB. Capillary and cell wall permeability to potassium in isolated dog hearts. Am. J. Physiol. 1975;229:537–544. [PMC free article] [PubMed]
32. Triffitt JT, Terepka AR, Neuman WF. A comparative study of the exchange in vivo of major constituents of bone mineral. Calcif. Tissue Res. 1968;2:165–176. [PubMed]
33. Zierler KL. Equations for measuring blood flow by external monitoring of radioisotopes. Circ. Res. 1965;16:309–321. [PubMed]