Air and/or water, plus a host of microscopic flora and fauna.
particles are of soil so there is no particle in the soil ANSWER: Rock and mineral particles are found in soil.
Loosely packed spoil has spaces between the particles. These space fill with air and water
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.
cohesive soils are those soils where the attraction between the soil particles is very high such as in clay. non-cohesive soils are those soils where there is no firm attraction between the soil particles.
in forests because of the large and small rock particles
particles are of soil so there is no particle in the soil ANSWER: Rock and mineral particles are found in soil.
actually they create some spaces in between the particles of the soil so that air can pass in and out through the particles ans thus maintains the fertility of the soil. Ex- Earthworm.
Air and/or water, plus a host of microscopic flora and fauna.
Clay, silt, and sand are the three types of weathered rock particles found in soil.
Loosely packed spoil has spaces between the particles. These space fill with air and water
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.
its groundwater!
cohesive soils are those soils where the attraction between the soil particles is very high such as in clay. non-cohesive soils are those soils where there is no firm attraction between the soil particles.
Soil organisms live in the space between the soil particles. i am a science genius!! :P
in forests because of the large and small rock particles
pore spaces
Grainy stones.