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粘质沙雷氏菌对某些无机盐的渗透性。

Permeability of Serratia marcescens to some inorganic salts.

作者信息

Zimmerman L

出版信息

J Bacteriol. 1969 Feb;97(2):749-55. doi: 10.1128/jb.97.2.749-755.1969.

Abstract

The physical interactions between Serratia marcescens and solutions of NaCl, CaCl(2), CaI(2), NaI, and Na(2)HPO(4) plus NaH(2)PO(4) were examined. Dilute (0.017 n) salt solutions did not cause cells to lose water, as evidenced by the unchanged weight of centrifugally packed cells. The cells preferentially adsorbed the cations and repelled the anions of most salts in these solutions. Concentrated (1.71 n) salt solutions markedly reduced the weight and water content of centrifugally packed cells, although these cells took up considerable amounts of salts. More than 90% of the water in the packed-cell pellets was available for the solution of NaCl at 4.2 to 4.4% concentration. The observation that salts apparently penetrated the cells freely and yet caused extensive dehydration was not readily compatible with conventional concepts of solute-induced plasmolysis. Alternative hypotheses to explain the data included the following. First, the cells lost weight and water to concentrated salt solutions through a nonosmotic competitive dehydration, causing a shrinkage of the protoplasmic gel. The shrinkage of the cell wall was limited because of the rigidity of its mucopeptide layer; therefore, a space appeared between the cell wall and the cell membrane. Second, cells may have equilibrated their water activity with that of their environment by two mechanisms: (i) the loss of water by plasmolysis or competitive dehydration, and (ii) alterations in cell permeability that admitted previously excluded solutes to the cell interior. Possibly, the correct explanation of the observations reported here involves elements of all three hypotheses, plasmolysis, competitive dehydration, and permeability alterations.

摘要

对粘质沙雷氏菌与氯化钠、氯化钙、碘化钙、碘化钠以及磷酸氢二钠加磷酸二氢钠溶液之间的物理相互作用进行了研究。稀(0.017n)盐溶液不会导致细胞失水,这可通过离心压实细胞重量未变得到证明。细胞优先吸附这些溶液中大多数盐的阳离子并排斥阴离子。浓(1.71n)盐溶液显著降低了离心压实细胞的重量和含水量,尽管这些细胞吸收了大量盐分。在浓度为4.2%至4.4%的氯化钠溶液中,压实细胞沉淀中超过90%的水是可利用的。盐显然能自由穿透细胞但却导致大量脱水这一观察结果,与溶质诱导质壁分离的传统概念不太相符。解释这些数据的其他假设有以下几点。第一,细胞通过非渗透竞争性脱水向浓盐溶液失去重量和水分,导致原生质凝胶收缩。由于其粘肽层的刚性,细胞壁的收缩受到限制;因此,在细胞壁和细胞膜之间出现了一个空间。第二,细胞可能通过两种机制使其水活性与其环境的水活性达到平衡:(i)通过质壁分离或竞争性脱水失去水分,以及(ii)细胞通透性的改变,使先前被排除的溶质进入细胞内部。可能这里所报告观察结果的正确解释涉及所有三个假设的要素,即质壁分离、竞争性脱水和通透性改变。

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