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Methods of Soil Resampling to Monitor Changes in the Chemical Concentrations of Forest Soils
Published on: November 25, 2016
Acid rain: neutralization within the hubbard brook ecosystem and regional implications
Summary
Acidic precipitation is neutralized by soil reactions, primarily with aluminum salts and organic matter. Acidified lakes and streams are mainly found in low-order watersheds in New England.
Area of Science:
- Environmental Chemistry
- Soil Science
- Hydrology
Background:
- Acid precipitation poses a significant environmental threat, altering water and soil chemistry.
- Understanding neutralization processes is crucial for managing acidified ecosystems.
Purpose of the Study:
- To investigate the primary mechanisms neutralizing strong acids from precipitation in soil.
- To identify the regional distribution of acidified and aluminum-rich surface waters.
Main Methods:
- Analysis of soil and water samples to determine chemical composition.
- Assessment of neutralization reactions involving basic aluminum salts and biologic matter.
- Regional mapping of water bodies in relation to watershed characteristics.
Main Results:
- Approximately 75 percent of acid neutralization occurs in the soil zone.
- Rapid reactions with basic aluminum salts and biologic matter are key neutralization processes.
- Acidified and aluminum-rich lakes and streams are predominantly located in low-order watersheds.
Conclusions:
- Soil plays a critical role in mitigating acid precipitation impacts through chemical neutralization.
- Watershed order is a significant factor influencing the occurrence of acidified surface waters.
- Findings highlight the vulnerability of low-order watersheds to acid deposition in regions like New England.
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