Dissolved Ion Concentrations Flashcards
Different dissolved ion concentrations: direct water from precipitation and snowmelt results in
A lower ion concentration, as rivers are more dilute.
Reasons for different dissolved ion concentrations: (7)
Weathering, Rock type, Major cations - Ca2+, Mg2+, Na+, K+, Major anions - HCO3 -, SO4 2-, NO3 -, Vegetation, Soils, Human intervention.
Acidic waters, pH <3, tend to arise from
Oxidised sulfide-rich rocks, which generates sulfuric acid.
Alkaline waters, pH 12, tend to arise from
Weathering of ultra mafic rocks.
Seasonal variation: Stream discharge; (2)
Increased in April & Nov/Dec.
More water = more leaching of weathered material.
Seasonal variation: Rainstorms;
Displace water that has been in contact with rocks for a while, results in initial increase in ion concentrations.
Seasonal variation: Nutrient demand by vegetation;
Ammonium ion (NH4 +) -
Input exceeds output all year because of the breakdown of proteins from plants.
Seasonal variation: Nutrient demand by vegetation;
Potassium & nitrate -
Input exceeds output in summer, but not in winter. Lower demand for the ions in winter.
In summer, plant growth results in their extraction.