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- Q5073758 subject Q7464107.
- Q5073758 subject Q8759368.
- Q5073758 subject Q8784062.
- Q5073758 abstract "Soil is essential to most animals on the earth. It is a relatively thin crust where an even smaller portion contains much of the biological activity. Soil consists of three different phases. A solid phase (≈ 50%) that contains mainly minerals of varying sizes as well as organic compounds. The rest is pore space. This space contains the liquid and gas phases.In order to understand porosity better a series of equations have been used to express the quantitative interactions between the three phases of soil. Macropores or fractures play a major role in infiltration rates in many soils as well as preferential flow patterns, hydraulic conductivity and evapotranspiration. Cracks are also very influential in gas exchange, influencing respiration within soils. Modeling cracks therefore helps understand how these processes work and what the effects of changes in soil cracking such as compaction, can have on these processes.".
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- Q5073758 wikiPageWikiLink Q7464107.
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- Q5073758 wikiPageWikiLink Q8759368.
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- Q5073758 wikiPageWikiLink Q8784062.
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- Q5073758 comment "Soil is essential to most animals on the earth. It is a relatively thin crust where an even smaller portion contains much of the biological activity. Soil consists of three different phases. A solid phase (≈ 50%) that contains mainly minerals of varying sizes as well as organic compounds. The rest is pore space.".
- Q5073758 label "Characterisation of pore space in soil".