When water gets into the soil, it pours into pores. Pores are spaces in the soil that come in different sizes. The bigger the pore, the more water it holds.
Because there is an equilibrium between large pores and small pores. That results in equilibrium between water adsorbed and air capacity
pores
true
The voids present between the soil particles are called pore space and the size of these pores depends on whether the ore is between the soil particles or between the soil aggregates. In general, in cultivated lands, soil particles do not exist as single grains and therefore, there are only voids within the soil aggregates or peds and voids between the aggregates. As clay particles play a major role in the formation of soil aggregates by way of binding the soil particles, the particles within the aggregates are micro pores and between the aggregates are macro pores. Depending on the amount of clay particles, the proportion of micro to macro pores may vary and in most cases the soils containing more clay particles favour aggregation and thereby the micro pores and total porosity.
Water contained in pores of soil or rock is groundwater..
When water gets into the soil, it pours into pores. Pores are spaces in the soil that come in different sizes. The bigger the pore, the more water it holds.
Because there is an equilibrium between large pores and small pores. That results in equilibrium between water adsorbed and air capacity
pores
true
The voids present between the soil particles are called pore space and the size of these pores depends on whether the ore is between the soil particles or between the soil aggregates. In general, in cultivated lands, soil particles do not exist as single grains and therefore, there are only voids within the soil aggregates or peds and voids between the aggregates. As clay particles play a major role in the formation of soil aggregates by way of binding the soil particles, the particles within the aggregates are micro pores and between the aggregates are macro pores. Depending on the amount of clay particles, the proportion of micro to macro pores may vary and in most cases the soils containing more clay particles favour aggregation and thereby the micro pores and total porosity.
Soil water is water suspended in soil, groundwateris water collected inside the pores of rock formations.
No special substances; for the soil aeration are important: soil density, soil porosity, dimensional distribution of pores, granulation, humidity, the presence of the worm Lumbricus terrestris.
False
Saturated Zone .
in pores or holes in the soil and the underlying rock layers
water held underground in the soil or in pores and crevices in rock :]-LLC