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27 Cards in this Set

  • Front
  • Back
soil texture is determined by the relative amounts of 3 groups of soil particles
sand,silt,clay
soil gives plants the following which are essentioal to sustain plant life
support nutrients and water(snw)
water is retained in or moves through the pore spaces as a result of
the size, number and continuity of the pores, textural, structural, and organic matter
organic
living or once was living
a given volume of soil contains 4 parts
organic matter
living matter
water
air
Physically describes soil by the feel
texture
course soil
larger amount of sand
texture of flour
silt
loam
mearly equal amounts of sand, silt, and clay
microscope must be used to see
silt
electron microscope must be used to see
clay particles
a lab procedure used to find proportions of soil seperates in a soil is called
mechanical analysis
textural triangle used to
determine soil texture after mechanical analysis
3 sides of the triangle represent the
% of sand, silt, and clay
intersection on triangle points to of the 3 lines from each side of the triangle determine how
the soi texture will be classified
the arrangement of soil seperates or individual soil particles in units
soil structure
(individual soil particles)into units
soil aggregates
process that causes aggregates
welting, drying periods, freezing/thawing, decaying, organic matter, activity of roots and small animals, absorbed nurtients, soil tillage(wdpftdoma(of)r(and)saanst)
bulk density
how soil retains water, the weight per unit volume of soil
the volume includes both
solids and pore space
bulk density used in determing
soil porosity
lose porous soils have
lower bulk density than tight compacted soil.
tight compacted soil has
bulk density that increase with compaction
bulk density indicates(4)
how easy soil will till, how easily water will infilarate, how it will hold water, and its suitability for growing plants
space between soil particle is_________and consists of__________
1) the pore space
2)consists of varying amounts of water and air
soil poristy depends on
soil texture and structure
the characteristics causes
bulk density to be lighter for sands