Definition: The word "alkaliescence" is a Greek term which originally referred to a phenomenon occurring in rocks where water or other liquids (such as oil) reacts with minerals present in the rock, producing organic compounds that are then transported into the soil. The exact meaning and historical context of this term vary greatly. Some sources attribute its origin to an ancient Roman law known as Alkaliae, which was used to regulate the distribution of water and other substances in rivers and aquifers by creating a system where only certain chemicals could flow through a certain channel. In the New International Version (NIV) Bible, "alkaliescence" is defined as: 1. The process by which soil or rock that has been exposed to water for long periods of time becomes wetter and more productive. 2. The occurrence of organic compounds in the soil after they have been transported into the soil due to water retention, including oils from plants and animal fats. This term dates back over 600 years.
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