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Moisture equivalent was proposed by Lyman Briggs and McLane (1910) as a measure of field capacity for fine-textured soil materials. Moisture equivalent is defined as the percentage of water which a soil can retain in opposition to a centrifugal force 1000 times that of gravity. It is measured by saturating a sample of soil 1 cm thick, and subjecting it…
The analysis highlights Overview, Related Topics and Entities as prominent areas in the source structure around Moisture equivalent.
Source areas are shown by the number of related topics found in each part of the analysis. Use smaller areas too: they can reveal specialized angles and content gaps.
Smaller areas are not necessarily less important. They contain fewer connections in this analysis and can be useful for finding specialized angles or coverage gaps.
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moisture equivalent soil lyman briggs water field capacity mclane centrifugal force 1000 times gravity james 1910 shantz 1912 wilting soils
TTTA extracted structured relationships around Moisture equivalent. The table shows each extracted connection, where it came from and its confidence.
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The concept neighborhoods around Moisture equivalent bring nearby vocabulary together. In this analysis, examples include Moisture, Water and Capacity. Use the clusters to find adjacent concepts and terminology that may deserve separate research.
Bridges highlight paths between different parts of the Moisture equivalent map and can reveal research angles that are easy to miss in a flat list.
TTTA analyzes the structure around Moisture equivalent to surface related topics, entities, relationships, concept neighborhoods and bridge connections. Use the map to explore areas such as Overview, Related Topics & Entities, including less central topics that may reveal useful research gaps. Automatically extracted connections are research leads rather than rewritten encyclopedia content.
Source: Wikipedia — Moisture equivalent · EN edition · Analysis: TopicsToTalkAbout