BIO
201: Botany
PLANT METABOLISM
SOIL NUTRIENTS
Carbon (C), Hydrogen (H) & Oxygen (O) are not considered nutrients
Yet, they of great importance to plants since they are in large quantities in environment
MACRONUTRIENTS – mineral nutrients needed in large quantities, essential for plant growth
element (symbol): % of plant – common form
Nitrogen (N): 1.5% - NO3- or NH4+
Potassium (K): 1.0% - K+
Calcium (Ca): 0.25% - Ca2+
Phosphorus (P): 0.2% - H2PO4-
Sulfur (S): 0.2% - SO4=
Magnesium (Mg): 0.2% - Mg2+
MICRONUTRIENTS - Mineral nutrients needed in small quantities
include Boron, Manganese, Zinc, Molybdenum, Copper, Chlorine, Iron
many have unknown importance
Some nutrients can be recycled:
moved from older parts to young parts.
eg.: N, P, Mg, K
Some nutrients needed continuously from soil:
* mechanism of uptake is active transport into epidermal cells from soil
* then transport up stem though xylem
Form of uptake:
1) simple ions: K+, Mg2+, Fe3+
2) as oxidized ions: PO43-, SO42-, NO3-
once taken up must be reduced: NO3- à NH4+
CATION EXCHANGE SYSTEM
Ability of soil to exchange & hold ions
* large soil particles (-) charged;
* attract and hold (+) charged
Plants take up lose cations (+)
* replaced with H+ in soil
* cation exchange frees up ions from soil particles
* soil recharged through decomposition
Movement of soil nitrogen
Organic nitrogen ---------------> NH4+ -------------> NO3-
mineralization nitrification
Ammonia (NH4+) rapidly used by bacteria and plants
Nitrate (NO3-) easily lost from soil (negatively charged)
Sands & silts - have low cation exchange capacity
contain very few charged soil particles
results in leaching
loams, clays, mucks - have high capacity
FERTILIZERS
Organic – from decomposition of organic matter
* slow release, long lasting, more natural
Inorganic – chemically produced, commonly from petroleum
* fast release, quick acting, typically artificial source
* measured as:
Nitrogen (NH4 or NO3) : Phosphate (PO4) : Potash (K2O)
fertilizer containers with percentage of each: 8-10-5