To recover or not to recover – the ”Laurentius-equation”

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To recover or not to recover – the ”Laurentius-equation” Søren Laurentius Nielsen Roskilde University

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To recover or not to recover – the ”Laurentius-equation”. Søren Laurentius Nielsen Roskilde University. Original dataset based on:. 162 transects /stations 23 areas Data from years 1980 – 1991 Data from the then Danish counties. Spearman- Rank Correlation Coefficients – all significant. - PowerPoint PPT Presentation

Transcript of To recover or not to recover – the ”Laurentius-equation”

Page 1: To recover or not to recover – the ”Laurentius-equation”

To recover or not to recover – the ”Laurentius-equation”

Søren Laurentius NielsenRoskilde University

Page 2: To recover or not to recover – the ”Laurentius-equation”

Original dataset based on:

• 162 transects /stations• 23 areas• Data from years 1980 –

1991• Data from the then

Danish counties

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Spearman- Rank Correlation Coefficients – all significant

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Established these relationships:

• Nutrients (N, P) → Phytoplankton biomass• Phytoplankton biomass + suspended matter →

Secchi depth• Secchi depth → Eelgrass depth limit• TN → Eelgrass depth limit

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N and P vs. Phytoplankton biomass2

2

2

ln( ) 1.072ln( ) 4.959 0.391

ln( ) 0.759ln( ) 1.197 0.277

ln( ) 0.806ln( ) 0.344ln( ) 4.666 0.414

phyto

phyto

phyto

B TN R

B TP R

B TN TP R

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2ln( ) 0.367 ln( ) 0.444ln( ) 2.686 0.808sd phytoZ Susp B R

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20.787 0.339 0.606c sdZ Z R

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2ln( ) 0.755ln( ) 6.039 0.547cZ TN R

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• The equations reflect a comparison between locations

• Not a development over time• Later uses imply a place for time substitution• Variation caused by differences among

locations in other factors

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Sediment characteristics suspected

2

0.703 / 12.2

0.703 0.082( / 12.2) / 12.2 0.81c sd

c sd

Z Z C N

Z Z C N C N R

Krause-Jensen et al., Vand & Jord, 2007Krause-Jensen et al., MEPS, 2011

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(it might get quite complicated…)

Krause-Jensen et al., MEPS, 2011

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Causal links:

N - loading

N - concentration

Phyto-plankton

Light Depth limit

Algal mats

Organic matter

Changes insediment

Anoxia

Resus-pension

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Markager S., Carstensen J, Krause-Jensen D, Windolf J, Timmermann K. 2010. Technical report from NERI no. 787. http://www.dmu.dk/Pub/FR787.pdf

Based on empirical analyses of data from Skive Fjord, Horsens Fjord and Odense Fjord

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Kemp et al. 2009

Hysteresis and regime shifts

Duarte et al., Estuaries andCoasts, 2009

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Conceptual modelMarkager S., Carstensen J, Krause-Jensen D, Windolf J, Timmermann K. 2010. Technical report from NERI no. 787. http://www.dmu.dk/Pub/FR787.pdf

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Reasons for the hysteresisCausal links:

N - loading

N - concentration

Phyto-plankton

Light Depth limit

Algal mats

Organic matter

Changes insediment

Anoxia

Resus-pension

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3d dynamic model

Sediment physics

Sediment lability

Benthic fauna

Vegetation

Wave & current energy

Input Output

Hydrodynamic simulation

TD, sediment transport simulation

Ecological simulation

Erosion/deposition

Bio-sedimentation