胆囊的运输功能。

International review of physiology Pub Date : 1980-01-01
R A Frizzell, K Heintze
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引用次数: 0

摘要

在餐间期,胆囊的吸收功能负责浓缩胆汁酸钠盐。这完全归因于其以等渗比例吸收NaCl(和NaHCO3)和水的能力,从而使肝胆汁的体积减少了80%- 90%。采用几种胆囊的研究结果与中性NaCl(和NaHCO3)吸收的存在是一致的,这是由于在粘膜处存在耦合的(一对一)NaCl进入过程。活性钠离子从细胞向浆膜溶液的挤压似乎为细胞Cl-积累提供了能量,从而为经上皮Cl-运输提供了能量。Cl-从细胞出口到浆液溶液的机制尚不清楚,需要进一步研究。兔胆囊为表征NaCl共转运提供了理想的制备材料,也是进一步研究这一机制的首选组织。电生理研究支持非导电NaCl共输的概念,也表明偏离严格中性盐吸收过程可能与Na+和/或Cl-通过粘膜运动的额外(扩散)途径的存在有关,从而消除了这些离子吸收运动之间中性耦合的机制约束。在这些条件下,观察到显着的浆膜阳性经上皮PD,并且一部分Cl-吸收可能与Na+的吸收电偶联。通过渗透耦合电解质运输,水被被动吸收。在上皮内产生的高渗区域,在外侧细胞间隙水平,为渗透水流提供动力。鉴于胆囊的高渗透性,解释吸水率所需的高渗程度可能比最初预期的要小,并且可能难以通过实验检测。最近关于体液和药理学对电解质和水运输的影响的研究表明,液体吸收的速度可能受到生理调节。例如,分泌素刺激富含HCO3的胆汁分泌,也抑制胆囊对这种富含HCO3的液体的重吸收,并以这种方式加速十二指肠管腔的中和。旨在确定胆囊吸收功能的生理控制的调查应该为未来的研究提供一个令人兴奋的途径。
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Transport functions of the gallbladder.

The absorptive functions of the gallbladder are responsible for concentrating the Na+ salts of bile acids during interprandial periods. This can be attributed entirely to its ability to absorb NaCl (and NaHCO3) and water in isotonic proportions, thus reducing the volume of hepatic bile by 80%--90%. The results of studies employing gallbladders of several species are consistent with the presence of neutral NaCl (and NaHCO3) absorption that is due to the presence of a coupled (one-for-one) NaCl entry process at the mucosal membrane. Active Na+ extrusion from cell to serosal solution appears to provide the energy for cellular Cl- accumulation, and thus for transepithelial Cl- transport. The mechanism of Cl- exit from the cell to serosal solution is uncertain andrequires further study. Rabbit gallbladder provided an ideal preparation for the characterization of NaCl cotransport and continues to be the tissue of choice for further study of this mechanism. Electrophysiological studies support the concept of nonconductive NaCl cotransport and also suggest that departures from the process of strictly neutral salt absorption may be related to the presence of additional (diffusional) pathways for Na+ and/or Cl- movement across the mucosal membrane so that the mechanistic constraint of neutral copuling between the absorptive movements of these ions is removed. Under these conditions, a significant serosa-positive transepithelial PD is observed and a fraction of Cl- absorption may be electrically coupled to that of Na+. Water is absorbed passively by virtue of osmotic coupling to electrolyte transport. A region of hypertonicity generated within the epithelium, at the level of the lateral intercellular space, provides the driving force for osmotic water flow. In view of the high osmotic water permeability of the gallbladder, the degree of hypertonicity required to account for the rate of water absorption is probably smaller than originally anticipated and is likely to be difficult to detect experimentally. Recent studies of the effects of humoral and pharmacological agents on electrolyte and water transport suggest that the rate of fluid absorption may be subject to physiological regulation. For example, secretin, which stimulates a HCO3--rich biliary secretion, also inhibits the reabsorption of this HCO3--rich fluid by the gallbladder, and in this manner may expedite the neutralization of the duodenal lumen. Inquires aimed at defining the physiological control of the absorptive functions of the gallbladder should provide an exciting avenue for future studies.

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