THE SIZE OF INFLUENZA VIRUS
THE SIZE OF INFLUENZA VIRUS
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DOI:
10.1084/jem.79.3.267
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发表时间:
1944-03-01
影响因子:
15.3
通讯作者:
Stanley, W. M.
中科院分区:
文献类型:
--
作者:
Stanley, W. M.
The sedimentation behavior of influenza virus in dilute solns. of electrolyte was found to be quite variable. At times the virus activity appeared to sediment at a rate comparable with that of particles about 80 to 120 m[mu] in diam., at other times at a rate comparable with that of particles about 10 m[mu] in diam., and at still other times the bulk of the activity appeared to sediment at a rate comparable with that of the larger particles and the residual activity at a rate comparable with that of the smaller particles. However, in the presence of sucrose density gradient, the virus activity was always found to sediment with a rate comparable to that of particles about 80-120 m.[mu] in diam.; hence it appeared that the variable sedimentation behavior in dilute electrolyte soln. was due to convection or mechanical disturbances during centrifugation. About 30% of the high molecular wt. protein present in the allantoic fluid of chick embryos infected with the F 12 strain of influenza virus was found to consist of a component having a sedimentation constant of about 30 S, and hence a probable particle diam. of about 10 m[mu]. The residual protein of high mol. wt. was present in the form of a component having a sedimentation constant of about 600 S, and hence a probable particle diam. of about 70 m[mu]. The proportion of the 30 S component in allantoic fluid of chick embryos infected with the PR8 strain of influenza virus was found to be considerably less. The 600 S and 30 S components of F 12 allantoic fluid were purified and separated by differential centrifugation. The purified prepns. of the 600 S component were found to possess a specific virus activity from 100 to over 10,000 times that of the purified prepns. of the 30 S component, the difference in activity apparently depending only on the degree of frac-tionation of the 2 components. The purified 30 S component was found to sediment normally in the presence of 12% sucrose; the small residual virus activity of such prepns. was found to sediment in the presence of a sucrose density gradient with a rate comparable to that of much heavier particles. It is concluded that influenza virus activity is not associated with material having a particle diam. of about 10 m[mu], but is associated solely with material having a sedimentation constant of about 600 S and hence a probable particle diam. of about 70 m[mu].