Shi X, Summers R W, Schedl H P, Chang R T, Lambert G P, Gisolfi C V
Department of Exercise Science and Internal Medicine, University of Iowa, Iowa City 52242.
J Appl Physiol (1985). 1994 Sep;77(3):1178-84. doi: 10.1152/jappl.1994.77.3.1178.
These experiments examined relationships between initial osmolality and carbohydrate (CHO) composition of an infused solution and osmolality and water and CHO absorption in a test segment. A triple-lumen tube with a 10-cm mixing segment and a 40-cm test segment was passed into the duodenojejunum. The infusion port was approximately 10 cm beyond the pyloric sphincter. Perfusion solutions were hypotonic (186 mosmol/kg; solution A), isotonic (283 mosmol/kg; solution B), and hypertonic (403 mosmol/kg; solution C). All solutions contained 18 meq Na+ and 3 meq K+. In the mixing segment, osmolality increased 83 mosmol/kg and decreased 90 mosmol/kg for solutions A and C, respectively. Corresponding changes in the test segment were an increase of 60 mosmol/kg and a decrease of 34 mosmol/kg. The osmolality of solution B did not change. In the test segment, mean osmolality and water and total solute fluxes were not significantly different among solutions, but solution C produced 27% greater fluid absorption than did solution A. When net fluid movement from mixing and test segments was determined, solution A produced 17% greater fluid absorption than did solution C. The mean increases in plasma and urine volumes over the 80-min test period were not significantly different. In the test segment, water flux correlated with CHO and Na+ fluxes but not with osmolality. In conclusion, 1) significant differences in solution osmolality were eliminated within the proximal duodenum and 2) perfusing 6% CHO solutions with osmolalities ranging from 186 to 403 mosmol/kg did not produce significant differences in fluid homeostasis (plasma volume) at the end of an 80-min test period.
这些实验研究了输注溶液的初始渗透压与碳水化合物(CHO)组成之间的关系,以及渗透压、水和CHO在测试段的吸收情况。将一根带有10厘米混合段和40厘米测试段的三腔管插入十二指肠空肠。输注端口位于幽门括约肌约10厘米以外。灌注溶液为低渗(186毫摩尔/千克;溶液A)、等渗(283毫摩尔/千克;溶液B)和高渗(403毫摩尔/千克;溶液C)。所有溶液均含有18毫当量的Na⁺和3毫当量的K⁺。在混合段,溶液A和C的渗透压分别增加了83毫摩尔/千克和降低了90毫摩尔/千克。测试段的相应变化分别为增加60毫摩尔/千克和降低34毫摩尔/千克。溶液B的渗透压没有变化。在测试段,各溶液之间的平均渗透压、水和总溶质通量没有显著差异,但溶液C产生的液体吸收比溶液A多27%。当确定混合段和测试段的净液体移动时,溶液A产生的液体吸收比溶液C多17%。在80分钟的测试期间,血浆和尿量的平均增加没有显著差异。在测试段,水通量与CHO和Na⁺通量相关,但与渗透压无关。总之,1)近端十二指肠内消除了溶液渗透压的显著差异;2)在80分钟的测试期结束时,灌注渗透压范围为186至403毫摩尔/千克的6%CHO溶液在液体稳态(血浆量)方面没有产生显著差异。