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What Describes Soil Particle's Resistance to Releasing Water?

5 years ago
last modified: 5 years ago

A key characteristic of a soil particle is its water holding capacity. But in reading some soil science articles, it seems to me that this is not all water available to the plant. There comes a point when the soil particle holds onto water with more force than the plant's roots can take water. What are the scientific terms for this phenomena, and does anyone have graphs that would show how common soil particles that hold water display these effects? I am thinking of soil particles like sawdust, 1/4" bark, peat, and turface.

The reason that this point came to mind is I am doing some experiments with turface, and I noticed that it remains moist after watering for a long time, but the density of that moisture down deep in the turface soil is low. It is not clear to me that a plant's roots would be able to fully use that moisture in the same way that roots can use a medium like peat.

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