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Temporal changes in soil properties at an upland Scottish site between 1956 and 1997
J D Miller1, E I Duff, D Hirst
1Macaulay Land Use Research Institute, Aberdeen, UK.
The Science of the Total Environment
|March 3, 2001
Summary
Soil sampling frequency was analyzed to detect temporal property changes. Current protocols, like the Environmental Change Network
Area of Science:
- Soil Science
- Environmental Monitoring
Background:
- Soil properties change over time, necessitating appropriate sampling strategies.
- Archived soil samples can be affected by storage, impacting chemical analysis.
- Understanding temporal soil changes is crucial for environmental management.
Purpose of the Study:
- To determine the optimal soil sampling frequency for detecting significant temporal changes.
- To evaluate the impact of storage on soil chemistry data.
- To assess the adequacy of current monitoring protocols.
Main Methods:
- Analysis of historical soil data (1956, 1977, 1997) from Glensaugh Research Station.
- Statistical analysis of soil chemistry, including pH, exchangeable cations (Ca, Mg, H), and base saturation.
- Application of statistical techniques to Environmental Change Network (ECN) data to estimate detectable change.
- Calculation of required sampling intervals based on observed temporal change rates.
Main Results:
- Storage significantly affected soil pH and chemistry, particularly in organic soils.
- Temporal changes observed include decreasing exchangeable Ca and Mg, and increasing exchangeable H.
- Percent base saturation declined due to reduced exchangeable base cations.
- Sampling intervals vary by soil horizon and chemical property.
Conclusions:
- Current Environmental Change Network (ECN) sampling protocols (5- and 20-year intervals) are likely appropriate for detecting changes in podzolic soils at this site.
- Site-specific data are essential for refining soil monitoring strategies.
- Long-term soil monitoring requires careful consideration of analytical methods and potential storage effects.