ee ee te HES ee te oN.

61
i ae f ndependently verified by observing the overlapping of

|

ayversian systems in bone of known age and remodeling

a

id for thnttion of bone generations shown in [igure 51. (See
ng
i the valuefeection on the generation distribution of remodeli

LL

ute. A truly random process would produce a distribu-

semuewelin

# bone in’

4

TT

TTT

TT

Toa

TTT

|

q
4

4
—

Lil

(1) It follows from postulates 1(b), 1(c); and 1(d)
hat the area under the curveof the specific activity of
some ex the body between the time of injection and infinite

svstem vbtime|is equal to the area under the curve of specific

7

mentation (b) This area is simply q/nk, where q is the activitye

at bone. cae and nk is the rate of excretory plasma clearanc
n the last xpressed as grams of calcium per day(liters per day
.
mentationtimes the calcium content per liter).

go. Ther

ToT

2

» Derived Relationships

onelucive activity of the blood plasma versus time.

;

0

L

on rate ibne.)
dent

Por

s JF
>

[_

5

4

=

-

>

r~

uJ
=

[—
L.

-

a

_

4

o

Lo

oO

z
o

4

4
-j

L

re

=o
i

Ol

fe

4

I

=

[7

4

(c) This requirement of area together with the early

jon ¢ateftetention. curve determines the time constant of thefinal

onds uporbesponential which is characteristic of age-invariant
at region fsystems. If the system is age-invariant, then a tracer

"following a single injection must eventually reach tranmds upon
sient. equilibrium: a state in which the tracer concentra-

nentatioWein differ in different compartments, but all decrease
erimentee proportion to the same exponential function of
ed by the!itime.'
4. Vew Associations

(1),

(a) Observation and theory show that the removal
of tracer activity from bone by diminution (diffusion) ~

d 5 days ean be represented quite closely by the power function.
pposition’ At short and intermediate times after tracer intake,
given in power function retention in bone existingat the timeof

in years.pintake can result from diffusion of tracer in cylindrical
dl year,’ geometry around canaliculi.“ In bone formed shortly
tion. For; aftcr intake and in existing bone at long times after
~alizationt intake, power function retention can result from the

nly the’ decrease of the coefficient of diffusion with local bone
ne. This, @xe.

> rate off

(b) On the other hand, in an age-invariant system

-diminu-f the removal of tracer activity by resorption of bone

bone. Inf could not produce power function or multi-exponential

pears tof retention unless there were an extremely wide distribu-

nsfer be-g tion of the turnover times of bonein different parts of
J the skeleton. Bone turnover times that differed by four
Porfive orders of magnitude in different locations would
be required to produce the sort of power function or

multi-exponential function that is observed for skeletal
of boneg Tetention, The ratio between the fastest and the slowest
re of thet turnover by apposition-resorption is probably not

‘ould bef ®reuter than four or six. Therefore, the effect. of resorp-

tion -hould be associated only with the final one or
found a poxsibly two exponential terms. The earlier terms (or

the power funetion part of retention) should be associ-

Oo,

+L

0

|

05

!

Lo

}

plo Et

1.5

2

25

TIME AFTER ADOLESCENCE — AT

Fia. 51—The distribution of generations within a region of
bone that has been remodeling at the rate A in locations
governed entirely by chance (osteons) for a period of time T
since the original formation of the skeleton (assumed to occur at the age of adolescence). Figures from Table 28. These
predictions, if verified, could be used to verify the applicability
of the assumption of randomnessin local regions of remodeling.

ated with diminution. In viewof the little data on this
point, we assume that the diminution of activity from

hotspots and from the diffuse component is the same

so that the specific activities of individual hotspots

and the diffuse component decrease in parallel with

the power function part of the whole-body retention

curve.

4, Bone Model
(a) Let us assume that there are twoclasses of bone,
cortical bone and trabecular bone, each with its own
rate of turnover by apposition-resorption. Let the rate
of cortical turnover be
(in units of time~'). Then

let the rate of trabecular turnover be oA. ¢ probablyis
of the order of 4 to 6. Let the fraction of the skeleton
that is trabecular be 7, and the fraction that is cortical
be 1 — 7 (fraction by calcium content). + is probably
about 0.2.

(b) Then it is easy to show that when an injected

tracer has finally equilibrated within this skeletal system, practically no activity remains in the trabeculae.
The skeletal activity is almost wholly in the slowlyturning-over cortex so that it is the turnover time of

dad

Select target paragraph3