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1 ding to a 3'-(dT)(20)-18 bp DNA substrate by sedimentation equilibrium.
2 gin-1 associates as a dimer when analyzed by sedimentation equilibrium.
3 ight scattering, sedimentation velocity, and sedimentation equilibrium.
4 r interference or absorbance measurements at sedimentation equilibrium.
5 f a dimerizing system in chemical as well as sedimentation equilibrium.
6 nce profiles acquired during the approach to sedimentation equilibrium.
7 ized by isothermal titration calorimetry and sedimentation equilibrium.
8 association of the peptides were measured by sedimentation equilibrium.
9 ansmembrane helices during the time-scale of sedimentation equilibrium.
10 7 +/- 4) kDa, a value confirmed by low-speed sedimentation equilibrium.
11 tistically different from values acquired by sedimentation equilibrium.
12 nd compared to values measured previously by sedimentation equilibrium.
13 detection, fluorescence quench titration, or sedimentation equilibrium.
14 l electrophoresis, isoelectric focusing, and sedimentation equilibrium.
15 with the equilibrium constant determined by sedimentation equilibrium.
16 the application to expedite the approach to sedimentation equilibrium.
17 his hypothesis was examined rigorously using sedimentation equilibrium.
18 n moiety in the protein/detergent complex by sedimentation equilibrium; (2) measurement of the appare
19 ed by disassociation constants determined by sedimentation equilibrium: 6.62 x 10(-6) M (rbetaA3), 0.
20 an be verified by sedimentation velocity and sedimentation equilibrium after correction for bound det
23 acentrifugation, sedimentation velocity, and sedimentation equilibrium analyses of the native dirigen
29 ree paramyxovirus F proteins was analyzed by sedimentation equilibrium analysis in detergent and buff
32 r organization in solution, we carried out a sedimentation equilibrium analysis of arrestin at both c
33 of this protein in solution, we carried out sedimentation equilibrium analysis of ATIC over a broad
37 nce chemical shift perturbation mapping, and sedimentation equilibrium analysis show that KIX binds a
40 applied a method described previously, using sedimentation equilibrium analysis to calculate the cont
41 esidue long N-terminal fragment was shown by sedimentation equilibrium analysis to form a dimer with
46 on protein, a novel dye-label technique, and sedimentation equilibrium analysis, we directly and conc
50 a single predominant oligomeric species, and sedimentation equilibrium analysis-derived mass values i
56 analytical size-exclusion chromatography and sedimentation equilibrium analytical ultracentrifugation
57 he core of the protein were studied by using sedimentation equilibrium analytical ultracentrifugation
59 e have used alanine-scanning mutagenesis and sedimentation equilibrium analytical ultracentrifugation
62 ducing single-alanine substitutions and used sedimentation equilibrium analytical ultracentrifugation
67 into stable monomers in solution as shown by sedimentation equilibrium and CD and formed an intrachai
72 have been measured in the absence of DNA by sedimentation equilibrium and gel filtration chromatogra
74 chemical and biophysical analyses, including sedimentation equilibrium and scanning transmission elec
77 f the octylglucoside-solubilized receptor by sedimentation equilibrium and sedimentation velocity ana
78 cterized and compared using a combination of sedimentation equilibrium and sedimentation velocity in
79 d S3/S4 half-operator oligonucleotides using sedimentation equilibrium and sedimentation velocity mea
80 Using analytical ultracentrifugation in both sedimentation equilibrium and sedimentation velocity mod
81 have established that C-tau is a monomer by sedimentation equilibrium and sedimentation velocity ult
83 tion constant (Ka) of 2-4 x 10(8) M-1, using sedimentation equilibrium and size exclusion chromatogra
91 ar UV CD spectroscopy, thermal denaturation, sedimentation equilibrium and velocity, and intrinsic fl
94 echniques, including sedimentation velocity, sedimentation equilibrium, and dynamic light scattering
95 ircular dichroism, dynamic light scattering, sedimentation equilibrium, and fluorescence experiments
96 eport the results of sedimentation velocity, sedimentation equilibrium, and gel-filtration experiment
98 n explored by analytical gel chromatography, sedimentation equilibrium, and oxygen binding experiment
99 he techniques of intensity light scattering, sedimentation equilibrium, and radiation inactivation we
100 forms a very stable trimer as determined by sedimentation equilibrium, and the concentration depende
101 assembly in these mutants were monitored by sedimentation equilibrium, and the conformational states
102 s, as measured by sedimentation velocity and sedimentation equilibrium, and the tryptic cleavage patt
103 now shown unambiguously by light scattering, sedimentation equilibrium, and titration calorimetry tha
104 chemical methods including light scattering, sedimentation equilibrium, and titration calorimetry, we
105 the "Smc2/4 complex," which upon analysis by sedimentation equilibrium appears to reversibly self-ass
107 en measured under a variety of conditions by sedimentation equilibrium at pH 7.5 and 4 and 20 degrees
108 ll design for analytical ultracentrifugation-sedimentation equilibrium (AUC-SE), ideal for studying s
109 nfirmed by analytical ultracentrifugation to sedimentation equilibrium by which a 1:1 complex was obt
110 d on results from sedimentation velocity and sedimentation equilibrium centrifugation as well as anal
111 of the self-association state of hDlg using sedimentation equilibrium centrifugation, matrix-assiste
114 tracentrifugation data confirmed this, where sedimentation equilibrium curve fits gave a mean molecul
120 tein concentrations, and good global fits to sedimentation equilibrium data require a positive value
124 vely, in agreement with their sequences, and sedimentation equilibrium data supported these determina
127 he recombinant protein by gel filtration and sedimentation equilibrium demonstrate a dimer-tetramer s
128 ons, static light scattering, and analytical sedimentation equilibrium, demonstrate that Ud NS1A ED f
132 l allowance for thermodynamic nonideality in sedimentation equilibrium distributions reflecting solut
135 he approach to equilibrium in a short-column sedimentation equilibrium experiment followed by a high-
137 rization of C167PM has been characterized in sedimentation equilibrium experiments (K(d) approximatel
138 e prolonged stability needed in conventional sedimentation equilibrium experiments and it can increas
140 ce optical data acquisition system, allowing sedimentation equilibrium experiments at loading concent
147 ce the number of SCR domains compared to CR2 Sedimentation equilibrium experiments gave a mean molecu
148 sedimentation velocity and density gradient sedimentation equilibrium experiments in CsCl with UV de
152 iments and it can increase the efficiency of sedimentation equilibrium experiments of previously unch
155 In contrast, sedimentation velocity and sedimentation equilibrium experiments show that full-len
157 dI is found to form a homodimer of 16.7 kDa; sedimentation equilibrium experiments show that the dime
160 slinking, size-exclusion chromatography, and sedimentation equilibrium experiments shows that the mos
162 6 E7 and Ad5 E1A oligomerization properties, sedimentation equilibrium experiments were performed wit
172 ive site by means of sedimentation velocity, sedimentation equilibrium, fluorescence solute quenching
174 his investigation indicates the potential of sedimentation equilibrium for the quantitative character
178 lation) have been studied using short-column sedimentation equilibrium in the analytical ultracentrif
180 t average molar mass (M(w)) determined using sedimentation equilibrium in the analytical ultracentrif
181 I = 0.10 M) using sedimentation velocity and sedimentation equilibrium in the analytical ultracentrif
182 tail analytical solutions of expressions for sedimentation equilibrium in the analytical ultracentrif
183 A combination of sedimentation velocity and sedimentation equilibrium in the analytical ultracentrif
184 0 Da as determined by neutron scattering and sedimentation equilibrium, in good agreement with the se
186 conformation is remarkably changed, and the sedimentation equilibrium indicates that the protein is
189 timate for SCF-sKit interaction, obtained by sedimentation equilibrium, is about 17 nm at 25 degrees
190 e assembly process have been dissected using sedimentation equilibrium measurements and DNaseI footpr
192 of dynamin II by analytical ultracentrifuge sedimentation equilibrium measurements at high ionic str
210 polysomes were separated from other mRNAs by sedimentation equilibrium or sedimentation velocity.
211 ants, SN228 and SR228, was also evaluated by sedimentation equilibrium over this same temperature ran
212 reduce the systematic errors in the measured sedimentation equilibrium profiles by more than an order
214 the monomer-monomer interface is stabilized, sedimentation equilibrium results demonstrated that the
221 nzyme have been obtained by using analytical sedimentation equilibrium, sedimentation velocity studie
227 nergy scale and free energy differences from sedimentation equilibrium studies for point mutants of t
255 d CaM were determined by CD spectrometry and sedimentation equilibrium: their affinities were Cys(-)-
256 tions, isothermal titration calorimetry, and sedimentation equilibrium to determine whether scRPA can
258 However, a thermodynamic investigation using sedimentation equilibrium ultracentrifugation in deterge
263 Clostridium thermoaceticum was determined by sedimentation equilibrium ultracentrifugation to be 300,
264 mples of enzyme were subjected to analytical sedimentation equilibrium ultracentrifugation to obtain
265 -domain interactions were investigated using sedimentation equilibrium ultracentrifugation, cross-lin
269 ein-surfactant complexes are investigated by sedimentation equilibrium via analytical ultracentrifuga
271 techniques, and additional studies in which sedimentation equilibrium was used show that the binding
274 ere a systematic study of K(a) determined by sedimentation equilibrium, which showed that it varied b