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Limestone
marine life during Paleozoic era lead to immense sedimentary layres of limestone across Alberta
results in dissociated carbonate ions, CO3² (basic)
lakes are normally slightly alkaline
soil that has a high potential for neutralizing acids (not incredibly sensitive to acid deposition)
Buffering & Buffering Capacity
neuralization of acids by CO3² (example: present in soil)
chemical systems that resist a change in pH (small amounts)
Low pH in the Environent
acid rain (<5.6) directly damages plant tissues and structures
deviates from optimal soil pH levels reduces plant’s ability to grow by reducing its ability to absorb nutrients through roots
leaching of metals can effect plants and soils
decrease in growth of roots (preventing absorption of calcium)
reduction in soil bacterial
HCO3 - HCO3
example of a buffering formula