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9th April 2014 Kari Austnes 1 Critical limits for acidification of surface waters vs boundary values in the Water Framework Directive (WFD) – a Norwegian case study 24th CCE workshop and 30 th task force meeting

9th April 2014Kari Austnes1 Critical limits for acidification of surface waters vs boundary values in the Water Framework Directive (WFD) – a Norwegian

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Page 1: 9th April 2014Kari Austnes1 Critical limits for acidification of surface waters vs boundary values in the Water Framework Directive (WFD) – a Norwegian

Kari Austnes 19th April 2014

Critical limits for acidification of surface waters vs boundary values in the Water Framework Directive (WFD) – a Norwegian case study

24th CCE workshop and 30th task force meeting

Page 2: 9th April 2014Kari Austnes1 Critical limits for acidification of surface waters vs boundary values in the Water Framework Directive (WFD) – a Norwegian

Kari Austnes 2

Objective

• Two sets of management regulations related to acidification of surface waters− LRTAP: Acid deposition below the critical load (CL) for

protection of the ecosystems− WFD: Ecological indicators (quality elements) above

certain boundary values for achieving good ecological status (with respect to acidification)

• Both use acid neutralising capacity (ANC) as chemical criterion linking water chemistry to biological effects− Do they set the same requirements?− Not directly comparable – CL calulated based on both

criteria for comparison

9th April 2014

Page 3: 9th April 2014Kari Austnes1 Critical limits for acidification of surface waters vs boundary values in the Water Framework Directive (WFD) – a Norwegian

Kari Austnes 3

Critical loads for surface waters

• SSWC and FAB the commonly used models• Both use ANClimit as link chemistry-biology

− The criterion we want to compare with the ANC criterion in the WFD

• SSWC: CL(A) = BC0 - ANClimit

− BC0: Flux of (non-marine) base cations from the catchment in pre-acidification times

− ANClimit • Minimum ANC to avoid harmful effects

on selected biota• Originally a fixed limit at 20 eq/l 95% probability of no damage

9th April 2014Lien et al. (1996)

Page 4: 9th April 2014Kari Austnes1 Critical limits for acidification of surface waters vs boundary values in the Water Framework Directive (WFD) – a Norwegian

Kari Austnes 4

The variable ANClimit

• Less sensitive systems higher biodiversity higher ANClimit needed to keep the diversity intact

• The variable ANClimit varies with the original base cation concentration− [ANC]limit,var = k*CL = k*Q*[BC*]0/(1+k*Q)

− ANC-range: 0-50 eq/l

• Organic acid adjustment− Organic acids contribute to the strong acid anion

concentration larger buffer needed at higher organic acid concentration

− [ANC]limit,oaa,var = k*Q*([BC*]0-1/3*m*[TOC])/(1+k*Q) (m=10.2, k=0.2)

− CL=Q*([BC*]0- [ANC]limit,oaa,var -3.4*[TOC])9th April 2014

Page 5: 9th April 2014Kari Austnes1 Critical limits for acidification of surface waters vs boundary values in the Water Framework Directive (WFD) – a Norwegian

Kari Austnes 5

The WFD and boundary values

• Ecological status of surface waters based on a set of quality elements− Biological and physicochemical

• Boundary values set for different quality elements (e.g. ANC) with respect to different pressures (e.g. acidification)− Five status classes from high to bad− Good status environmental target the

good/moderate (G/M) boundary essential− The boundary values represent deviation from a

reference status (natural conditions)• Different sets of boundary values for different types of

water bodies (e.g. small, lowland, humic lakes)9th April 2014

Page 6: 9th April 2014Kari Austnes1 Critical limits for acidification of surface waters vs boundary values in the Water Framework Directive (WFD) – a Norwegian

Kari Austnes 6

WFD boundary values (Norway)

• Lake types for acidification classification defined by Ca- and TOC-concentration− Boundary values vary according to buffering capacity and

humic acid content as the ANClimit,oaa,var

− Discrete boundary values (ANClimit,oaa,var continuous)

• 1st classification manual (2009)− 6 types: 2 Ca classes (split at 1 mg/l), 3 TOC classes− Reference value median of reference lakes− G/M boundary

• Brown trout status vs ANC • Benthic invertebrate vs ANC (adj)• Expert judgement• ANC-range: 20-40 eq/l

9th April 2014

Hesthagen et al. (2008)

Page 7: 9th April 2014Kari Austnes1 Critical limits for acidification of surface waters vs boundary values in the Water Framework Directive (WFD) – a Norwegian

Kari Austnes 7

WFD boundary values (Norway) cont.

• 2nd classification manual (2014)− Revised reference values

• Pre-industrial ANC from MAGIC many lakes pre-industrial ANC below G/M boundary large range within the same lake type

• Lower Ca-class (<1 mg/l) split into four

9th April 2014

• Median of MAGIC-results used

− Revised G/M boundary values• Re-analysis of brown trout data for new lake types• Boundaries adjusted downwards to take delayed biological

recovery into account (Wright, 2013)

• Expert judgement• ANC-range: 0-30 eq/l

Wright and Cosby (2012)

Ca<1, TOC<2

Page 8: 9th April 2014Kari Austnes1 Critical limits for acidification of surface waters vs boundary values in the Water Framework Directive (WFD) – a Norwegian

Kari Austnes 8

Background – variability across Norway

9th April 2014

Page 9: 9th April 2014Kari Austnes1 Critical limits for acidification of surface waters vs boundary values in the Water Framework Directive (WFD) – a Norwegian

Kari Austnes 9

The G/M boundary

9th April 2014

• Markedly higher values with the 1st WFD manual

• Both reflect the Ca and TOC patterns

• Not directly comparable to ANClimit,oaa,var TOC incorporated in the ANClimit,oaa,var value

• CL calculation used for comparison

Page 10: 9th April 2014Kari Austnes1 Critical limits for acidification of surface waters vs boundary values in the Water Framework Directive (WFD) – a Norwegian

Kari Austnes 10

Critical load: Compare ANClimit,oaa,var and G/M boundary

9th April 2014

• Markedly lower CL with G/M boundary based on the 1st manual

• Negative CL aiming for the unachievable

Page 11: 9th April 2014Kari Austnes1 Critical limits for acidification of surface waters vs boundary values in the Water Framework Directive (WFD) – a Norwegian

Kari Austnes 11

Exceedance 2007-2011: Comparison

9th April 2014

• Fairly similar results

• More realistic G/M boundary values in the 2nd manual

• Drawing on experience from the LRTAP work

• WFD requirements slightly lower

Page 12: 9th April 2014Kari Austnes1 Critical limits for acidification of surface waters vs boundary values in the Water Framework Directive (WFD) – a Norwegian

Kari Austnes 12

Differences CLA_oaa and CLA_WFD2

9th April 2014

• CLA_oaa mainly lower than CLA_WFD2

• Largest differences when CLA_oaa is lower than CLA_WFD2

• Largest relevant differences found on the west coast

Grid cells with CLA>90 meq/m2/yr removed from the analysis – not relevant - no risk of acidification

Page 13: 9th April 2014Kari Austnes1 Critical limits for acidification of surface waters vs boundary values in the Water Framework Directive (WFD) – a Norwegian

Kari Austnes 13

Differences: Humic acid content

• For both criteria CL decreases with increasing TOC

• Large range in deviation at low TOC− Different TOC-approach

less important

• At TOC>8 mg/l CLA_oaa is always lower− G/M boundary no

differentiation at TOC>5 mg/l (with respect to TOC)

− Too low G/M at high TOC?

9th April 2014

• Marked changes at class boundaries− Larger differences at the

lower end

Page 14: 9th April 2014Kari Austnes1 Critical limits for acidification of surface waters vs boundary values in the Water Framework Directive (WFD) – a Norwegian

Kari Austnes 14

Differences: Buffering capacity

9th April 2014

• G/M boundary increases with increasing Ca

• ANClimit,oaa,var increases with increasing BC0

• Fairly similar pattern reflect the same effect

• Lower CLA_WFD2 mainly at Ca0.75-1.25 mg/l

• Lower CLA_oaa along the whole range− Majority Ca<0.75 mg/l − Most grid cells with

Ca>0.75 mg/l high TOC

• Marked changes at class boundaries− Larger differences at the

lower end

Page 15: 9th April 2014Kari Austnes1 Critical limits for acidification of surface waters vs boundary values in the Water Framework Directive (WFD) – a Norwegian

Kari Austnes 15

Differences: Summary

• Exceedance− CLA_oaa stricter at very low Ca− CLA_WFD2 stricter at Ca0.75-1 mg/l− Differences in TOC approach mainly relevant at high TOC

• Discrete G/M boundaries problematic− Artificial trend within classes− High uncertainty around the class boundaries

9th April 2014

Page 16: 9th April 2014Kari Austnes1 Critical limits for acidification of surface waters vs boundary values in the Water Framework Directive (WFD) – a Norwegian

Kari Austnes 16

TOC increases – then what?

• WFD− Boundaries dynamic for their actual purpose, i.e. to

assess ecological status with respect to acidification• Increase in TOC type changes stricter requirement

(higher ANC G/M boundary)• But - only three TOC classes: Marked changes

needed, and no effect of TOC increase above 5 mg/l

• LRTAP− In theory critical loads based on ANC limit constant

• In practice revised as calculations and data improve

− Using ANClimit,oaa,var introduces a non-constant factor (TOC) not taken into account• Increasing TOC lower CL higher exceedance 9th April 2014

Page 17: 9th April 2014Kari Austnes1 Critical limits for acidification of surface waters vs boundary values in the Water Framework Directive (WFD) – a Norwegian

Kari Austnes 17

TOC increase: Effects on critical loads

9th April 2014

• Rough test− TOC increase in line

with long-term monitored lakes

− Increase from 1995-present

− Different factor in different regions: 1.0-1.9

• Small changes only− Most pronounced in

regions with higher TOC increase

Page 18: 9th April 2014Kari Austnes1 Critical limits for acidification of surface waters vs boundary values in the Water Framework Directive (WFD) – a Norwegian

Kari Austnes 18

TOC increase: Effects on exceedances

9th April 2014

• Relatively small differences so far

• Larger impact in other countries?

Page 19: 9th April 2014Kari Austnes1 Critical limits for acidification of surface waters vs boundary values in the Water Framework Directive (WFD) – a Norwegian

Kari Austnes 19

Conclusions

• WFD requirements far more in line with the LRTAP requirements in the 2nd manual for WFD classification

• Still some differences− WFD requirements somewhat lower overall− The upper TOC class should probably be split− Major differences at very low Ca – difficult to say which

criterion is more correct

• Discrete WFD boundaries give higher uncertainty• CLA_oaa decreases with increasing TOC

− Small changes so far, but may call for revision if continued TOC increase

9th April 2014