proteins were determined by equilibrium ultracentrifugation ... formed at different rotor speeds was required to give reason- .... h cell depth, parallel to axis of revolution ... molecular weight distribution(MWD) of a sample can also be ..... CM
MOLECULAR WEIGHT DISTRIBUTIONS OF PROTEINS BY EQUILIBRIUM ULTRACENTRIFUGATION AND GEL FILTRATION CHROMATOGRAPHY by CHING-YUNG MA B.Sc,
University of Hong Kong, 1970
M.Sc, University of Hong Kong, 197^ A thesis submitted i n p a r t i a l f u l f i l m e n t of the requirements f o r the degree of Master of Science i n the Department of FOOD SCIENCE Faculty of A g r i c u l t u r a l Sciences We accept t h i s thesis as conforming to the required standard
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i.
ABSTRACT The molecular weight d i s t r i b u t i o n s (MWDs) of some proteins were determined by equilibrium u l t r a c e n t r i f u g a t i o n and g e l f i l t r a t i o n chromatography
(GPC).
A l i n e a r program-
ming technique was used to compute MWDs from equilibrium data.
The l i g h t - s c a t t e r i n g second v i r i a l c o e f f i c i e n t ( B ) LS
of one protein, ovalbumin, was determined and was used to correct f o r the non-ideal behavior of the polymers. F o r unimodal systems, good MWDs were obtained from single experiment without correction f o r non-ideality.
For more complex
systems, combination of data from several experiments performed at d i f f e r e n t rotor speeds was required to give reasonable d i s t r i b u t i o n s ; and correction f o r B
L S
brought about
further improvement i n the smoothness and accuracy of the MWDs. GFC was found to be a rapid and convenient method f o r MWD determination, having better resolving power than the l i n e a r programming technique. The advantages and l i m i t ations of these two methods were discussed.
ii
TABLE OF CONTENTS PAGE INTRODUCTION
1
THEORY
8
A.
EQUILIBRIUM SEDIMENTATION
8
1. Basic Equations
8
2. S c h o l t e ^ Method f o r Determining MWD B.
11
3. Correction f o r Non-ideality
14-
GEL FILTRATION CHROMATOGRAPHY (GFC) 1. Basic Theory 2. Determination of MWD by GFC
16 16 17
MATERIALS AND METHODS
19
A.
CHEMICALS
19
B.
ULTRACENTRIFUGATION
19
1. Instrumentation a. Centrifuge;, and o p t i c a l system b. Rotor and c e l l 2. Equilibrium U l t r a c e n t r i f u g a t i o n
19 19 21 21
GEL FILTRATION CHROMATOGRAPHY
23
C.
27
RESULTS A.
B
L S
DETERMINATION BY THE METHOD OF ALBRIGHT
AND WILLIAMS , B. SCHOLTE'S METHOD FOR MWD DETERMINATION 1. Unimodal Systems a. Ovalbumin b. Other proteins
27 27 27 27 33
iii
PAGE 2. Bimodal Systems
,
39
a. Ovalbumin/y-globulin
39
b. Ovalbumin/RNase
39
3. Trimodal Systems a. Ovalbumin/y-globulin/apoferritin
39 39
b. Trypsin inhibitor/bovine serum albumin/ catalase C.
MWD DETERMINATION BY GFC
46 46
DISCUSSION
58
LITERATURE CITED
68
iv.
LIST OF FIGURES FIGURE
PAGE
1.
Record of a UV trace from an equilibrium experiment using double-sector c e l l .
2.
Plot of A C / C
3.
Plot of (AC/xG)'
k.
P l o t of ( M ^ ) "
vs. C .
31
5.
MWD of ovalbumin by Scholte's method, with data from four A .
35
6.
MWD of ovalbumin by Scholte's method, with data from one A .
36
7.
MWD
of human y - g l o b u l i n , RNase and t r y p s i n
38
vs. A .
n
29
vs.
1
1
2k
A.
Q
30
i n h i b i t o r by Scholte's method. 8.
MWD
of ovalburain/y-globulin mixture by
kl
Scholte's method. 9.
MWD
of ovalbumin/RNase mixture by S c h o l t e ^
kj
method. 10.
MWD
of ovalbumin/y-globulin/apoferritin
kS
. mixture by Scholte's method. 11.
MWD of t r y p s i n inhibitor/bovine serum albumin/ catalase mixture by Scholte's method.
kQ
12.
C a l i b r a t i o n curve of Sephadex G-200.
k9
13.
E l u t i o n pattern of t r y p s i n i n h i b i t o r on
50
Sephadex G-200.
v.
FIGURE 14.
PAGE E l u t i o n pattern of ovalburain/V-globulin
50
mixture on Sephadex .G-200. 15.
E l u t i o n pattern of ovalbumin/RNase mixture
52
on Sephadex G-200\ 16.
MWD of t r y p s i n i n h i b i t o r , determined by GFC.
53
17.
MWD of ovalbumin/y-globulin mixture, deter-
5^
mined by GFC. 18.
MWD of ovalburain/RNase mixture, determined by GFC.
55
vii
LIST
OF
TABLES PAGE
TABLE 1.
Data f o r B^
s
determination by the method of
28
Albright and Williams. 2.
Results of B
L S
determination by the method
32
of Albright and Williams. 3.
Table f o r the calculation of MWD of ovalbumin
34
by Scholte*s method. 4.
Average molecular weights of ovalbumin calculated from MWD data.
5.
Data f o r c a l c u l a t i o n of MWD of ovalbumin/ y-globulin/mixture
,
37
40
by Scholte*s method.
6.
Data f o r c a l c u l a t i o n of MWD of ovalbumin/ RNase mixture by Scholte*s"method.
42
7.
Data f o r c a l c u l a t i o n of MWD of ovalbumin/
44
y - g l o b u l i n / a p o f e r r i t i n mixture by Scholte*s method. 8.
Data f o r c a l c u l a t i o n of MWD of t r y p s i n inhibitor/bovine serum albumin/catalaise
47
mixture by Scholte*s method. 9.
Average molecular weights and molecular weight r a t i o s of some proteins, determined from MWDs.
57
vii.
LIST OF SYMBOLS A
c e l l area,
B
second v i r i a l c o e f f i c i e n t (or
B|,
(1-VP)W /2RT 2
l i g h t - s c a t t e r i n g second v i r i a l c o e f f i c i e n t
s
C
concentration on volume-based scales (g/l)
Q
o r i g i n a l concentration of solution
C
concentration of the i - t h species concentration at the c e l l bottom CL, m concentration at the meniscus (C)^
i d e a l equilibrium concentration
d
G(s) K
i n t e g r a l d i s t r i b u t i o n function of sedimentation coefficient
a y
K
f r a c t i o n of g e l volume available to the substance
d
distribution coefficient
M
molecular weight molecular weight of the i - t h species
M
app
apparent weight average molecular weight
M
app
apparent weight average molecular weight at zero speed
M
n
true number average molecular weight true weight average molecular weight
M
true z-average molecular weight z
P
pressure
R
molar gas constant
T VV e
absolute temperature elution volume inner volume
viii.
V
o
void volume t o t a l bed volume
U(x,l) f^
C/C
o
weight f r a c t i o n of i - t h species i n an equilibrium mixture
f:(W)) normalized d i f f e r e n t i a l d i s t r i b u t i o n function of molecular weight g(s)
normalized d i f f e r e n t i a l d i s t r i b u t i o n function of sedimentation c o e f f i c i e n t
h
c e l l depth, p a r a l l e l to axis of revolution
r
r a d i a l distance from the centre of r o t a t i o n
r^
r a d i a l distance from the c e l l bottom
rm m
r a d i a l distance from the meniscus
s
sedimentation c o e f f i c i e n t
Q
l i m i t i n g sedimentation c o e f f i c i e n t
s
v
p a r t i a l s p e c i f i c volume of solute, cm-Vg
y^
a c t i v i t y c o e f f i c i e n t of the i - t h species
s
A
correction term f o r B
.
experimental errors
A
(l-v )o) (r -r )/2RT 2
P
2
L S
determination
2
b
m
chemical potential of the i - t h species t o t a l potential of the i - t h species reference (r
2 b
-r
2 :
chemical potential of the i - t h species
)/(r
2 b
-r
2 m
)
p
density of solution,
g/cm
ul
angular v e l o c i t y , radians per second
ACKNOWLEDGEMENTS
I would l i k e to express my deepest gratitude to Dr. S. Nakai f o r i n i t i a t i n g t h i s project and h i s valuable advice and encouragement throughout the course of the study, and i n the preparation of the t h e s i s . I l i k e to thank Dr. Th. G. Scholte f o r providing me the computer program used i n t h i s work.
1.
INTRODUCTION Equilibrium u l t r a c e n t r i f u g a t i o n has been considered a c l a s s i c a l method f o r determining the molecular weight of macromolecules i n s o l u t i o n . mentation-diffusion
At the establishment of s e d i -
equilibrium a f t e r prolonged r o t a t i o n at
moderate speed, the v a r i a t i o n i n concentration (or concentration gradient) along a solution column i n an ultracentrifuge c e l l can be measured o p t i c a l l y .
From these data, the molecular
weight can be calculated from the following
equationsi
or
Where M i s the molecular weight of the solute; R, the
universal
gas constant; T, the absolute temperature; v, the p a r t i a l s p e c i f i c volume of the solution; p,
the density of the solv- '
ent; c, the concentration of the solution; co, the angular v e l o c i t y of the rotor and r , the r a d i a l distance from the centre of r o t a t i o n .
A p l o t of the logarithm of concentration
against the square of the r a d i a l distance
should give a
s t r a i g h t l i n e , with the slope d i r e c t l y r e l a t e d to the molecu l a r weight. High polymeric substances are mixtures of a large number of molecules which are chemically i d e n t i c a l but d i f f e r e n t i n molecular weight.
are
Various average molecular
2.
weights such as number-average
(MJJ),
weight-average (M^) end
z-average (M_) molecular weights can be calculated from the sedimentation equilibrium data by either one of the several procedures available (1,2, 3t 4 0 •
However, these molecular
weight averages can only give ,limited information t o the f r a c t i o n a l d i s t r i b u t i o n of the component molecules over the whole range of molecular weights.
In p r i n c i p l e , the entire
molecular weight distribution(MWD) of a sample can also be determined from sedimentation equilibrium experiments. Shortly a f t e r the construction of the f i r s t
ultra-
centrifuge by Svedberg and h i s associates i n the early 1920*s (5i 6 ) , Rinde (7) developed a method f o r determining the d i s t r i b u t i o n of r a d i i of the c o l l o i d a l gold sols from equil i b r i u m data. He derived the following equationi
Here, G
Q
i s the i n i t i a l concentration of the s o l u t i o n , A and
£ are functions of the rotor speed and the r a d i a l distance respectively, and f(M) i s the d i f f e r e n t i a l MWD function. A f t e r t h i s pioneering work, many attempts have been made to solve Rinde's equation f o r f(M).
In some cases (1,
8, 9 ) , s p e c i f i c models such as the most probable d i s t r i b u t i o n were used.
Wales and h i s co-workers (10, 11, 12, 13) avoided
these models and used osmotic pressure second v i r i a l i e n t , B__, to correct f o r non-ideality.
coeffic-
Sundelbf (14), pro-
OS-
, posed a method which was based on Fourier convolution theorem.
3.
Refinements of t h i s method were reported by Provencher (15) who showed that the basic equation f o r MWD
determination
(Eq. 3) i s a Fredholm i n t e g r a l equation of the f i r s t
kind.
He recommended a method by which the equation can be solved by a combination of quadrature and l e a s t squares.
A l l these
methods were found to be unsatisfactory and experimental errors may lead to negative weight f r a c t i o n s f o r some of the polymeric components. Recently, some new and elegant methods have been devised to solve the problem. Donmelly (16, 17) showed that the concentration d i s t r i b u t i o n of the polymeric solutes at sedimentation equilibrium i s i n the form of a Laplace transform.
He substituted a function
Making use of Eq. (10) we have M
l-V)^ r
1C
2
l (
1
a/ain
±
y i
\
The logarithm of y\ i s expressed i n power of C^ i n the form l n y
1
=
M ^B k=l i
i k
C
(18)
k +
and M. (l-i7. f>) to rQ. Z
~
fe B
ache
ik
a
r
e
i
v
e
r
v
dC.
q
dC.
= -3F' i i|»ik-3? +M
c
0 : and (3) a further constraint can be added to s p e c i f y 2^fv= i"V;: It should be noted that non-negative f ^ and the unity of 2 fy. are e s s e n t i a l features of a i
MWD.
13.
The set of f ^ obtained from the chosen set of not unique.
is
Seholte suggested the use of four molecular
x weight series spaced from each other "by a factor of 2*. Thus, =1
(36a)
=4
(36b)
(four s e r i e s ) =1
(36c)
f. (one series)
m i ^ f j L (four series) l^fjA
Eq. ( 3 6 c ) i s therefore also a solution, but w i l l give a more smooth MWD
since more points are included.
A f t e r the f ^ have been obtained, a continuous can be constructed using Seholte*s procedures. *a i f
=
1
=
j f < f
M
)
d
M
MWD
Note that
C< M
=
*
M)
A In M2 [Mf(M)] i
±
(37)
I f the i n t e r v a l between successive molecular weights i s Jr.
2*, then A In M = £ln 2 = 0 . 6 9 3 A
and
Since
^[Btf (M)]
±
= 4/0.693
%. f . (four series) = k
1 1
(39)
(Eq. 3 6 c ) , i t follows that
f ./0.693 = 4/0.693
•>l
(38)
(40)
1
Thus, [Mf ( M ) ^
= f5/0.693
(41)
Hence, the MWD curve i s constructed by p l o t t i n g Mf(M) v s . In M, and the area under the curve i s 1.
14. From the computed MWD functions, the various average molecular weights can also be calculated from the following relationsi (42) M
= f°°Mf (M)dM w
(43)
•'O
(44)
o
3» Correction f o r Non-ideality For monodisperse non-ideal
solutions at sedimentation
equilibrium, Williams and co-workers (34) derived the following i
1
equationsi "ap* = V 1
where M
a p p
app
+
(
V
2
> m (C
°b
+
)
+