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The Calcium, Magnesium, Potassium, and Sodium Budgets for a Small Forested Ecosystem
This study tracked calcium, magnesium, potassium, and sodium in Hubbard Brook watersheds. Net losses of these cations suggest significant geochemical weathering in the northern hardwood ecosystem.
Area of Science:
- Ecosystem analysis
- Biogeochemistry
- Environmental science
Background:
- Hubbard Brook Experimental Forest ecosystems are characterized by northern hardwoods, humid continental climate, and acid metamorphic rock.
- Understanding cation balance is crucial for assessing ecosystem health and geochemical processes.
Purpose of the Study:
- To investigate the balance of calcium (Ca++), magnesium (Mg++), potassium (K+), and sodium (Na+) in six watersheds.
- To quantify cation input via precipitation and output via streamwater runoff.
- To estimate geochemical weathering rates based on cation budgets.
Main Methods:
- Weekly sampling of precipitation and stream water from June 1963 to May 1965.
- Cation analysis using atomic absorption spectrophotometry.
- Calculation of cation budgets based on input (precipitation) and output (runoff) volumes and concentrations.
Main Results:
- Precipitation and runoff volumes varied between years, with peak runoff in April.
- Cation concentrations in precipitation were variable but generally low; dry fallout contribution was negligible.
- Streamwater cation concentrations were low and relatively constant, with significant inverse relationships for Na+ and discharge in some watersheds.
Conclusions:
- Net losses of Ca++, Mg++, and Na+ were observed, indicating significant geochemical weathering.
- The K+ budget appeared to be near balance, suggesting minimal net loss or gain.
- These findings provide conservative estimates of weathering rates in the northern hardwood ecosystem.
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