Laboratories of The Rockefeller Institute for Medical Research.
J Gen Physiol. 1935 Jul 20;18(6):967-85. doi: 10.1085/jgp.18.6.967.
The rate of entrance of potassium into Nitella flexilis has been investigated, and it has been shown that (a) at the concentrations studied the rate is independent of the external pH between 6 and 8 but it is possible that at lower concentrations a dependence may be found; (b) that it does not vary much with the external potassium concentration between 0.01 and 0.001 M, but appears to vary more with the potassium concentration below this limit. It has also been shown that the rate is independent of the illumination, in contrast with the penetration of halides into Nitella clavata studied by Hoagland. It has been found that potassium leaves the cells in distilled water, and since this does not seem to be the result of injury, there is apparently a concentration between 0 and 0.0001 M at which potassium neither enters nor leaves the cell. In Valonia increase of external potassium increases the rate of entrance as shown in the increase in moles of potassium in the sap. In Nitella this is true below an external concentration of 0.001 M. In Valonia this increase is paralleled by the increase in entrance of water so that little or no change in concentration occurs, but in Nitella no growth occurred during the experiment and in consequence the concentration of potassium in the sap increased. It has been shown that the potassium content of the raw gelatinous sap is no greater than that of its ultrafiltrate, so that it is not possible to assume that any of the potassium is bound up in the cell in colloidal compounds. It has been pointed out that all the gradients between the sap and the external solution are unfavorable to the entrance of potassium except the potassium bicarbonate gradient. However, on other grounds entrance as potassium bicarbonate is not considered to be very probable. Various modes of entrance are discussed and it has been concluded that the subject must be investigated further before a definite answer can be given.
已研究了钾进入水绵的进入速率,结果表明:(a)在所研究的浓度下,其速率与外部 pH 值在 6 到 8 之间无关,但在较低浓度下可能存在依赖性;(b)在 0.01 到 0.001 M 的外部钾浓度之间,其变化不大,但在该限度以下的钾浓度下变化更大。还表明,与 Hoagland 研究的进入水绵的卤化物的穿透不同,其速率与光照无关。已经发现钾从蒸馏水中离开细胞,由于这似乎不是损伤的结果,显然在 0 到 0.0001 M 的浓度范围内,钾既不进入也不离开细胞。在轮藻中,外部钾的增加增加了进入速率,如汁液中钾摩尔数的增加所示。在水绵中,在外部浓度低于 0.001 M 时是如此。在轮藻中,这种增加与水的进入增加相平行,因此浓度几乎没有变化,但在水绵中,实验过程中没有生长,因此汁液中的钾浓度增加。已经表明,原始凝胶状汁液的钾含量不大于其超滤物的钾含量,因此不能假设任何钾都以胶体化合物的形式结合在细胞中。已经指出,除了碳酸氢钾梯度外,汁液和外部溶液之间的所有梯度都不利于钾的进入。然而,在其他方面,作为碳酸氢钾的进入被认为不太可能。讨论了各种进入方式,并得出结论,在得出明确答案之前,必须进一步研究这个问题。