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When we drink water, most absorption occurs in the small intestine, but the large intestine (cecum, colon, rectum) continues to absorb water from the remaining contents. Typically, the material entering the large intestine is more solid, indicating that most water has already been absorbed in the small intestine.
According to research cited in “Gut Microbes” by Professor Guanggang Hui from Japan, the redox potential (ORP) varies along the digestive tract:
| Digestive Section | ORP (mV) |
|---|---|
| Stomach | +150 |
| Duodenum & Jejunum | -50 |
| Ileum | -150 |
| Cecum | -200 |
| Rectum | -250 |
In contrast, ordinary tap water has a potential of +450 to +650 mV, while bottled or natural water is around +200 to +400 mV.
Water entering the stomach gradually undergoes redox changes as it passes through the digestive tract. The ORP slowly decreases, reaching about -250 mV in the rectum, where absorption is most effective.
This process, sometimes referred to as the “natural intake principle”, indicates that the oxidation-reduction potential of water is a key factor in how efficiently the body absorbs it.
Some people believe that water molecules must be “small” to be absorbed quickly. However, the critical factor is not molecular size but redox potential.