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利用双同位素示踪技术,在大鼠灌注模型中对口服补液溶液(大米和葡萄糖基)在正常及分泌性肠道中的水和电解质转运进行研究。

Studies of water and electrolyte movement for oral rehydration solutions (rice- and glucose-based) across a normal and secreting gut using a dual isotope tracer technique in a rat perfusion model.

作者信息

Wall C R, Bates M S, Cleghorn C J, Ward L

机构信息

Children's Nutrition Research Centre, Royal Children's Hospital, Brisbane, Queensland, Australia.

出版信息

Aliment Pharmacol Ther. 1997 Jun;11(3):581-7. doi: 10.1046/j.1365-2036.1997.00171.x.

DOI:10.1046/j.1365-2036.1997.00171.x
PMID:9218086
Abstract

AIMS

To establish a model to measure bidirectional flow of water from a glucose oral rehydration to solution (G-ORS) and a newly developed rice-based oral rehydration solution (R-ORS) using a dual isotope tracer technique in a rat perfusion model. To measure net water, sodium and potassium absorption from the ORS.

METHOD

In vivo steady-state perfusion studies were carried out in normal and secreting (induced by cholera toxin) rat small intestine (n = 11 in each group). To determine bidirectional flow of water from the ORS the animals were initially with tritium, and deuterium was added to the perfusion solution. Sequential perfusate and blood samples were collected after attainment of steady-state conditions and analysed for water and electrolyte content.

RESULTS

There was significant increase in net water absorption from the R-ORS compared to the G-ORS in both the normal (P < 0.02) and secreting intestine (P < 0.05). Water efflux was significantly reduced in the R-ORS group compared to the G-ORS group in both the normal (P < 0.01) and the secreting intestine (P < 0.01). There was an increase in sodium absorption in the R-ORS group compared to the G-ORS. The G-ORS produced a significantly greater blood glucose level at 75 min compared to the R-ORS (P < 0.03) in the secreting intestine.

CONCLUSIONS

This study demonstrates the improved water absorption from a rice-based ORS in both the normal and secreting intestine. Evidence that the absorption of water may be influenced by the osmolality of the ORS was also demonstrated.

摘要

目的

利用双同位素示踪技术在大鼠灌注模型中建立一个模型,以测量葡萄糖口服补液盐溶液(G-ORS)和新开发的大米基口服补液盐溶液(R-ORS)的双向水流。测量口服补液盐溶液中的净水分、钠和钾吸收量。

方法

在正常和分泌型(由霍乱毒素诱导)大鼠小肠中进行体内稳态灌注研究(每组n = 11)。为了确定口服补液盐溶液的双向水流,动物最初用氚标记,然后将氘添加到灌注溶液中。在达到稳态条件后收集连续的灌注液和血液样本,并分析其水分和电解质含量。

结果

在正常小肠(P < 0.02)和分泌型小肠(P < 0.05)中,与G-ORS相比,R-ORS的净水分吸收均显著增加。在正常小肠(P < 0.01)和分泌型小肠(P < 0.01)中,与G-ORS组相比,R-ORS组的水流出量均显著降低。与G-ORS相比,R-ORS组的钠吸收增加。在分泌型小肠中,与R-ORS相比,G-ORS在75分钟时产生的血糖水平显著更高(P < 0.03)。

结论

本研究表明,在正常和分泌型小肠中,大米基口服补液盐溶液的水分吸收均有所改善。同时也证明了水分吸收可能受口服补液盐溶液渗透压影响的证据。

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