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Mineral intake independent from gastric irritation or pica by cell-dehydrated rats
Abstract Gavage of 2 M NaCl (IG 2 M NaCl), a procedure to induce cell-dehydration—and water and 0.15 M NaCl intake in a two-bottle choice test—is also a potential gastric irritant. In this study, we assessed whether mineral intake induced by IG 2 M NaCl is associated with gastric irritation or produ...
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Published in: | Physiology & behavior 2011-10, Vol.104 (5), p.659-665 |
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Main Authors: | , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | Abstract Gavage of 2 M NaCl (IG 2 M NaCl), a procedure to induce cell-dehydration—and water and 0.15 M NaCl intake in a two-bottle choice test—is also a potential gastric irritant. In this study, we assessed whether mineral intake induced by IG 2 M NaCl is associated with gastric irritation or production of pica in the rat. We first determined the amount of mineral solution (0.15 M NaCl, 0.15 M NaHCO3 , 0.01 M KCl and 0.05 mM CaCl2 ) and water ingested in response to IG 2 M NaCl in a five-bottle test. Then, we used mineral solutions (0.01 M KCl and 0.15 M NaHCO3 ), whose intakes were significantly increased compared to controls, and water in three-bottle tests to test the gastric irritation hypothesis. The IG 2 M NaCl induced KCl and NaHCO3 intake that was not inhibited by gavage with gastric protectors Al(OH)3 or NaHCO3 . IG 2 M NaCl or gavage of 0.6 N acetic acid induced mild irritation, hyperemia, of the glandular part of the stomach. A gavage of 50% ethanol induced strong irritation seen as pinpoint ulcerations. Neither ethanol nor acetic acid induced any fluid intake. Neither IG 2 M NaCl nor acetic acid induced kaolin intake, a marker of pica in laboratory rats. Ethanol did induce kaolin intake. These results suggest that IG 2 M NaCl induced a mineral fluid intake not selective for sodium and independent from gastric irritation or pica. |
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ISSN: | 0031-9384 1873-507X |
DOI: | 10.1016/j.physbeh.2011.07.010 |