BIOC40H3 Chapter Notes - Chapter 4: Hydraulic Conductivity, Hydrostatics, Tracheid

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In sandy soils, the spaces between particles are so large that water tends to drain from them and remain only on the particle surfaces and at interstices between particles. In clay soils, the channels are small enough that water is retained against the forces due to gravity. The moisture holding capacity of soil is called field capacity. Field capacity is water content of soil after it is saturated with water and excess has been drained away. Clay soils or soils with high humus content have large field capacity. Sand particles are larger and have less surface area per gram. Clay particles are smaller and have more surface area per gram. Negative hydrostatic pressure in soil water lowers soil water potential. The osmotic potential ( s) of soil water is usually neglible because solute concentrations are low i. e. -0. 02mpa. For soils with substantial concentrations of salt s can be significant i. e. -0. 2 mpa or lower.

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