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Published byJewel Johnston Modified over 9 years ago
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Controls on Catchment-Scale Patterns of Phosphorous in Soil, Streambed Sediment, and Stream Water Marcel van der Perk, et al… Journal of Environmental Quality, 2007
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Presentation Outline 1)Overview 2)Methods 3)Results 4)Conclusion 5)Discussion/Critique
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1. OVERVIEW
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Goal of Research: Attempt to quantify the unique and joint contribution of… 1)Soil type, soil chemical properties, and land use 2)Soil [P], sediment chemical properties, and point source emissions 3)Sediment chemical properties, water chemistry, and point source emissions Spatial variation of [P] in soil Spatial variation of [P] in streambed sediments Spatial variation of [P] in stream water Independent variablesDependent variables
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1. OVERVIEW Motivation for the goal: Phosphorous is a common limiting nutrient in both aquatic and terrestrial ecosystems Scientists know it is controlled by climate, geology, topography, and anthropogenic influences Yet to be successfully quantified/modeled at basin scale Valid models can be very useful Geochemical dataset available in the watershed promised possibility of “breaking new ground”
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1. OVERVIEW The Watershed Southwest England 976 km 2 (377 mi 2 ) 72% grassland 6% farmable 17% forest 50 STW, mostly small dispersed towns
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2. METHODS
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Geochemical survey (2002) 460-495 samples of each of the major top soil type, Stream water, & streambed sediment Soil-> randomly within every 2 nd square kilometer (systematic random) Streambed-> 1 st to 4 th order streams (systematic) Stream water-> same locations as streambed
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2. METHODS Spatial Data Also made interpolated maps from geochemical survey (conditional simulation) *******all data re-sampled to 25m resolution
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2. METHODS Statistical Analysis Ln transformed if regression residuals not normally distributed Only considered variables in regressions if significant (α=0.05, ANOVA) Multiple linear regression coefficient must be logical Coefficient of Determination (R 2 ) used to partition variation
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2. METHODS Partitioning the Variance
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2. METHODS Partitioning the Variance
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3. RESULTS
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Soil Data
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3. RESULTS Soil Data
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3. RESULTS Result of conditional simulation interpolation Soil Data
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3. RESULTS Streambed Data
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3. RESULTS Streambed Data
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3. RESULTS Stream Water
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3. RESULTS Stream Water
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4. CONCLUSION
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1.Soil Parent Material is major factor controlling catchment-scale spatial variation in soil TP and Olsen P, land cover is important too 2.Streambed [P] are correlated with major elements (adsorption). 3.Streambed [P] better predicted by erosion model and land use than upstream soil tests 4.Illustrates complex cascade of P transfer from soil to streambed to stream water under baseflow conditions (long term accumulation/diff sized storms) 5.Problems with spatial data
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5. DISCUSSION/CRITIQUE
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1.Cluster analysis? 2.GIS techniques 3.Erosion model
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