Sha'afi R I, Rich G T, Sidel V W, Bossert W, Solomon A K
J Gen Physiol. 1967 May;50(5):1377-99. doi: 10.1085/jgp.50.5.1377.
A study has been made of water entry into human red blood cells under an osmotic pressure gradient. The measurements were made using a rapid reaction stop flow apparatus, whose construction, calibration, and performance are described in detail. Red cell volume changes were determined from 90 degrees scattered light. The permeability coefficient for water entry under a relative isosmolar concentration of 1 to 1.5 was found to be 0.22 +/- 0.01 cm(4)/sec osmol, which agrees well with our previously published value. The experiments were also designed to measure the thickness of the unstirred layer around the6 red cells. This was found to be 5.5 +/- 0.8 micro under the present experimental conditions. It is concluded that our previously measured permeability coefficient for water entrance under a diffusion gradient does not require correction on account of the unstirred layer.
对在渗透压梯度下水分进入人体红细胞的情况进行了一项研究。测量是使用快速反应停流装置进行的,该装置的构造、校准和性能已详细描述。红细胞体积变化由90度散射光测定。在相对等渗浓度为1至1.5时,水分进入的渗透系数为0.22±0.01 cm⁴/(秒·渗透压),这与我们之前发表的值非常吻合。实验还旨在测量红细胞周围未搅动层的厚度。在当前实验条件下,发现其厚度为5.5±0.8微米。得出的结论是,我们之前测量的在扩散梯度下水分进入的渗透系数,无需因未搅动层而进行校正。