Chapter 37: Soil and Plant Nutrition Flashcards
soil
composite of organic and inorganic matter that accumulated in layers over time
defining features of soil
texture and compositions
soil horizons
stratified soil layers
a horizon
topsoil; mineral particles, living organisms and humus; most important for plant growth
b horizon
less organic matter and less weathered that horizon a
c horizon
mainly partially broken-down rock
clay
soil texture that retains too much water and not enough oxygen
sandy
soil texture that is unable to retain enough water for plant growth and to access soil minerals
loam
ideal/most fertile topsoil; equal amounts of sand, silt, and clay
soil solution
water and dissolved minerals retained in pores between soil particles
topsoil composition
inorganic and organic chemical components; mostly particles are negatively charged
leaching
anion plant nutrients that cannot bind to soil particles are lost from the soil
cation exchange
cations (K+, Ca+, Mg+) that adhere to negatively charged soil particles are displaced by H+ to be absorbed in the soil solution and taken up by the roots
soil pH
affects mineral availability; slightly acidic soils are usually preferred
Humus
prevents packing of clay particles by forming a crumbly soil
Macronutrients
Carbon, oxygen, hydrogen, nitrogen, potassium, calcium, magnesium, phosphorus, sulfur