The mass per unit volume of soil particles, usually expressed in grams per cubic centimetre.
soil texture is heavily influenced by particle density
lower levels of organic matter, less aggregation and more compaction
soil texture refers to particle sizes. whereas soil structure refers to particle arrangements
Silt.
soil ferility
soil texture is heavily influenced by particle density
Concerning the second Question: "Can you find bulk density with just this info?"Purely on mathematical insight and analysis:Yes, you should be able to find the bulk density of dry soil, given the 'dry overall' and the 'particle' densities.When wet, there is not enough 'given'Also some should be known about the (or your) definition of porosity
bulk density depend on that material from which soil formed. so maximum bulk density depend on particle density of that mineral. Therefore,we can only tapped the soil upto perticle density. so maximum bulk density may be occur at equal to paricle density.
Bulk density is the dry mass of the solids (M sub t) / total volume (V sub t) Particle density is bulk density (P sub b) / 1 minus total porosity (1-theta).
lower levels of organic matter, less aggregation and more compaction
the longer the soil partical the coarser it will be
Particle Density is how deep in volume something is for example: the density of water and sand.
The bigger the particle size, the more drainage the soil would have. The smaller the particle sizer, the less drainage the soil would have. ITS EASY
soil texture refers to particle sizes. whereas soil structure refers to particle arrangements
Silt.
soil ferility
large particle soil