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(1)

BFM Benthic

Arthur Capet, Paolo Lazzari, Cosimo Solidoro

OGS, Trieste, Italy

(2)

Why a benthic module ?

Processes/Mechanism you need the benthic for :

Retention

(part of) primary production mineralized locally

Seasonal inertia

Delayed remin. reshapes production seasonal

cycle

Inter-annual inertia

Delayed response to water policies

Denitrification

Net N removal (except N

2

fixation)

P sequestration

Solid P sequestration (Feedbacks!!)

Biology

Filtration, irrigation, turbation, consolidation,

(3)

Why a benthic module ?

Processes/Mechanism you need the benthic for :

Retention

(part of) primary production mineralized locally

Seasonal inertia

Delayed remin. reshapes production seasonal

cycle

Inter-annual inertia

Delayed response to water policies

Denitrification

Net N removal (except N

2

fixation)

P sequestration

Solid P sequestration (Feedbacks!!)

Biology

Filtration, irrigation, turbation, consolidation,

(4)

Why a benthic module ?

Processes/Mechanism you need the benthic for :

Retention

(part of) primary production mineralized locally

Seasonal inertia

Delayed remin. reshapes production seasonal

cycle

Inter-annual inertia

Delayed response to water policies

Denitrification

Net N removal (except N

2

fixation)

P sequestration

Solid P sequestration (Feedbacks!!)

Biology

Filtration, irrigation, turbation, consolidation,

(5)

Why a benthic module ?

Processes/Mechanism you need the benthic for :

Retention

(part of) primary production mineralized locally

Seasonal inertia

Delayed remin. reshapes production seasonal

cycle

Inter-annual inertia

Delayed response to water policies

Denitrification

Net N removal (except N

2

fixation)

P sequestration

Solid P sequestration (Feedbacks!!)

Biology

Filtration, irrigation, turbation, consolidation,

(6)

Why a benthic module ?

Processes/Mechanism you need the benthic for :

Retention

(part of) primary production mineralized locally

Seasonal inertia

Delayed remin. reshapes production seasonal

cycle

Inter-annual inertia

Delayed response to water policies

Denitrification

Net N removal (except N

2

fixation)

P sequestration

Solid P sequestration (Feedbacks!!)

Biology

Filtration, irrigation, turbation, consolidation,

(7)

Why a benthic module ?

Processes/Mechanism you need the benthic for :

Retention

(part of) primary production mineralized locally

Seasonal inertia

Delayed remin. reshapes production seasonal

cycle

Inter-annual inertia

Delayed response to water policies

Denitrification

Net N removal (except N

2

fixation)

P sequestration

Solid P sequestration (Feedbacks!!)

Biology

Filtration, irrigation, turbation, consolidation,

(8)

Hypoxia in the Adriatic

We knows that

1.

It happened in the Northern Adriatic shelf

(9)

Hypoxia in the Adriatic

We knows that

1.

It happened in the Northern Adriatic shelf

(10)

BFM benthic module

Previously in BFM, 4 levels of complexity :

0.

No benthic-pelagic coupling

1.

Simple return

2.

Benthic Organisms + intermediate diagenetic model

(11)

0. No benthic-pelagic coupling

Bath Tub

I

No sediment layer

I

Sinking OM accumulates in the lower layer

I

All mineralisation process are driven by pelagic formulations

Delocalisation of OM remineralization, and pelagic rates

instead of benthic rates.

(12)

1. Simple Benthic return

Benthic stocks for Organic Matter

I

Sinking OM accumulates in the sediments

I

Fixed mineralisation rates provide Oxygen and nutrient

fluxes

I

No burial (except from the standing equilibrium benthic

stock when mineralisation = sedimentation)

I

No benthic losses (e.g. denitrification, P sequestration) : All

mineralised fluxes are sent back to the water column

(13)

2. Benthic Organisms + Simple Benthic return

Benthic food web includes (all heterotrophs)

H1

: Aerobic bacteria

H2

: Anaerobic bacteria

Y1

: Epibenthic predators ∼ Megabenthos, acts on surface

Y2

: Deposit feeders, feeds on Benth. Detritus + small Benth.

Organisms

Y3

: Filter feeders, feeds on Pelagic OM and Phy.

Y4

: Meiobenthos: Large aggregation. Small → No effect on

sed. mix.

Y5

: Infaunal predators “hunt” in the sediments for prey of

their size

I

Vertical distribution of OM

and organism activity.

I

No diagenetic modelling

(fixed rates, no losses)

I

Later version of ERSEM

(Blackford, 2002) includes

Microphytobenthos

(diatoms)

(14)

2. Benthic Organisms + Simple Benthic return

Benthic food web includes (all heterotrophs)

H1

: Aerobic bacteria

H2

: Anaerobic bacteria

Y1

: Epibenthic predators ∼ Megabenthos, acts on surface

Y2

: Deposit feeders, feeds on Benth. Detritus + small Benth.

Organisms

Y3

: Filter feeders, feeds on Pelagic OM and Phy.

Y4

: Meiobenthos: Large aggregation. Small → No effect on

sed. mix.

Y5

: Infaunal predators “hunt” in the sediments for prey of

their size

I

Vertical distribution of OM

and organism activity.

I

No diagenetic modelling

(fixed rates, no losses)

I

Later version of ERSEM

(Blackford, 2002) includes

Microphytobenthos

(diatoms)

(15)

3. Benthic Organisms + Diagenetic model

I

Now includes pore water dissolved state variables : O

2

,

NO

3

, NH

4

, PO

4

, SiO + Reduction Equivalent

I

No vertical resolution, but analytical resolution for three

(variables) layer : Oxic, Suboxic, Anoxic.

I

Bioturbation and bioirrigation derive from benthic

organisms

(16)

3. Benthic Organisms + Diagenetic model

I

Now includes pore water dissolved state variables : O

2

,

NO

3

, NH

4

, PO

4

, SiO + Reduction Equivalent

I

No vertical resolution, but analytical resolution for three

(variables) layer : Oxic, Suboxic, Anoxic.

Figure:

Example for phosphate dynamics.

I

Bioturbation and bioirrigation derive from benthic

organisms

(17)

3. Benthic Organisms + Diagenetic model

I

Now includes pore water dissolved state variables : O

2

,

NO

3

, NH

4

, PO

4

, SiO + Reduction Equivalent

I

No vertical resolution, but analytical resolution for three

(variables) layer : Oxic, Suboxic, Anoxic.

I

Bioturbation and bioirrigation derive from benthic

organisms

(18)

3. Benthic Organisms + Diagenetic model

I

Oxygen consumption (miner., nitrif. and oxid. of reduction

equivalents) determines oxygen penetration depth.

I

Oxygen penetration modifies the nutrient dynamics.

I

The sulphide horizon depth derives from the nitrate module

and controls the adsorption properties of Phopshate

(19)

Table

CalcBenthicFlag

RetentionSeasonal

iner

tia

Inter

annual

iner

tia

Denitr

ification

P

retention

V

ar

ia

bility

of

P,N

diagenesis

Biology

0

X

X

X

X

X

X

X

1

V

V

X

X

X

X

X

2

V

V

X

X

X

X

V

3

V

V

X

V

V

V

V

(20)

Table

CalcBenthicFlag

RetentionSeasonal

iner

tia

Inter

annual

iner

tia

Denitr

ification

P

retention

V

ar

ia

bility

of

P,N

diagenesis

Biology

0

X

X

X

X

X

X

X

1

V

V

X

X

X

X

X

1b

V

V

V

V

X

V

X

2

V

V

X

X

X

X

V

3

V

V

X

V

V

V

V

OMEXDIA

V

V

V

V

V

VV

X

(21)

B1B

p

anox

part of anoxic mineralization (ie. producing ODU)

p

denit

part of denitrification mineralization (ie. using NO

x

)

p

nit

part of produced ammonium nitrified within the sediments

p

sid

ratio between potential and effective dissolution

(saturation)

(22)

B1B

p

anox

part of anoxic mineralization (ie. producing ODU)

p

denit

part of denitrification mineralization (ie. using NO

x

)

p

nit

part of produced ammonium nitrified within the sediments

p

sid

ratio between potential and effective dissolution

(saturation)

(23)

B1B

p

anox

part of anoxic mineralization (ie. producing ODU)

p

denit

part of denitrification mineralization (ie. using NO

x

)

p

nit

part of produced ammonium nitrified within the sediments

p

sid

ratio between potential and effective dissolution

(saturation)

(24)

B1B

p

anox

part of anoxic mineralization (ie. producing ODU)

p

denit

part of denitrification mineralization (ie. using NO

x

)

p

nit

part of produced ammonium nitrified within the sediments

p

sid

ratio between potential and effective dissolution

(saturation)

(25)

B1B

p

anox

part of anoxic mineralization (ie. producing ODU)

p

denit

part of denitrification mineralization (ie. using NO

x

)

p

nit

part of produced ammonium nitrified within the sediments

p

sid

ratio between potential and effective dissolution

(saturation)

(26)

B1B

p

anox

part of anoxic mineralization (ie. producing ODU)

p

denit

part of denitrification mineralization (ie. using NO

x

)

p

nit

part of produced ammonium nitrified within the sediments

p

sid

ratio between potential and effective dissolution

(saturation)

(27)

Meta-modelling

1.

Calibrate (extend) OMEXDIA model from observations

2.

Perturbated Monte Carlo simulations

3.

Derive functions for B1B

OMEXDIA

I

C,N,O,ODU,P,Si

I

100 lev. for 50 cm

I

non-local irr.

I

2 lability (fixed)

I

in-situ

I

Bottom Water

I

Porosity

I

Sed. rate

(28)

Meta-modelling

1.

Calibrate (extend) OMEXDIA model from observations

2.

Perturbated Monte Carlo simulations

3.

Derive functions for B1B

OMEXDIA

I

C,N,O,ODU,P,Si

I

100 lev. for 50 cm

I

non-local irr.

I

2 lability (fixed)

I

in-situ

I

Bottom Water

I

Porosity

I

Sed. rate

(29)

Meta-modelling

1.

Calibrate (extend) OMEXDIA model from observations

2.

Perturbated Monte Carlo simulations

3.

Derive functions for B1B

OMEXDIA

I

C,N,O,ODU,P,Si

I

100 lev. for 50 cm

I

non-local irr.

I

2 lability (fixed)

I

in-situ

I

Bottom Water

I

Porosity

I

Sed. rate

DIC NH3 NO3 PO4 SiDet SIO TOC

0 5 10 15 20 H1 2500 3000 3500 4000050 100 150 200 250 0 5 10 15 0 1 2 3 4 0.000.050.100.15 50 100150 0.40.50.60.7 depth, cm

DIC NH3 NO3 PO4 SiDet SIO TOC

0 5 10 15 20 H2 2400 2800 3200 3600 0 2550751000.02.55.07.5 10.00 3 6 9 0.10 0.15 0.20 0.25050 100 150 2000.20.4 0.60.8 depth, cm

DIC NH3 NO3 PO4 SiDet SIO TOC

0 5 10 15 20 H4 2400 2800 3200 36000255075 100 1250 1 2 3 40 5 10 15 0.0 0.2 0.4 0.6 0100 200 300 4000.45 0.50 0.55 0.60 depth, cm

DIC NH3 NO3 PO4 SiDet SIO TOC

0 5 10 15 20 H6 3000 4000 5000 60000 1002003000123450 50 100 0.2 0.3 0.4 0.5 0.6 0.70 100 200 300 400 5001.01.21.41.6 depth, cm

DIC NH3 NO3 PO4 SiDet SIO TOC

0 5 10 15 20 H7 30004000 050 100 150 200 250 0 5 10 010203040 0.15 0.20 0.25 0.30 0100 200 300 400 1.0 1.2 1.4 1.6 depth, cm

(30)

Meta-modelling

1.

Calibrate (extend) OMEXDIA model from observations

2.

Perturbated Monte Carlo simulations

3.

Derive functions for B1B

−25 −20 −15 −10 −5 0 −30 −20 −10 0

DICflux

−2 −1 0 −3 −2 −1 0

NH3flux

−0.5 −0.4 −0.3 −0.2 −0.1 0.0 −1.00−0.75 −0.50−0.25 0.00

NO3flux

0 5 10 15 20 0 10 20 30

O2totflux

−0.20 −0.15 −0.10 −0.05 0.00 −0.20−0.15−0.10−0.050.00

PO4flux

−5 −4 −3 −2 −1 0 −4 −2 0

SIOflux

Station

0 H1 H2 H4 H6 H7

variable

NonLocal Biodiffusion

(31)

Meta-modelling

1.

Calibrate (extend) OMEXDIA model from observations

2.

Perturbated Monte Carlo simulations

3.

Derive functions for B1B

● ● ● ● ● ModelSSR 100 100.5 101 101.5 100 100.5 101 101.5

S_j (Biodiffusive)

S_j (Non−local)

● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ●● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ●

DIC DICflux NH3 NH3flux

NO3flux O2flux PO4 PO4flux

SiDet SIO SIOflux TOC

10−4 10−2 100 10−4 10−2 100 10−4 10−2 100 10−8 10−6 10−4 10−2 100 102 10−8 10−6 10−4 10−2 100 102 10−8 10−6 10−4 10−2 100 102 10−8 10−6 10−4 10−2 100 102

S_j (Biodiffusive)

S_j (Non−local)

Station

● ● ● ● ● H1 H2 H4 H6 H7

(32)

Meta-modelling

1.

Calibrate (extend) OMEXDIA model from observations

2.

Perturbated Monte Carlo simulations

3.

Derive functions for B1B

● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●●● ●● ●● ● ● ●● ●● ● ●● ● ● ● ● ● ●● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ●●● ●● ● ● ● ● ● ● ● ●● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●●● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ●●●● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ●● ● ●● ● ● ● ● ● ● ● ● ●● ●● ●●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ●● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ●● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ●● ● ●● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ●● ● ●● ● ● ● ● ● ● ● ● ● ●●● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ●●● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ●●●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ●● ● ● ● ● ● ● ● ● ● ●●● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●●● ●● ●● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ●●● ● ● ●● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●●● ● ●● ●● ●● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ●● ●● ● ● ● ● ●● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ●●● ● ● ● ● ● ● ● ●● ● ● ● ●

0.00

0.05

0.10

0.15

0.20

0.25

0

1000 2000 3000 4000

Cmin

pdenit

0

100

200

300

400

bwO2

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bwO2

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(33)

Meta-modelling

1.

Calibrate (extend) OMEXDIA model from observations

2.

Perturbated Monte Carlo simulations

3.

Derive functions for B1B

● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●●● ●● ●● ● ● ●● ●● ● ●● ● ● ● ● ● ●● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ●●● ●● ● ● ● ● ● ● ● ●● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●●● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ●●●● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ●● ● ●● ● ● ● ● ● ● ● ● ●● ●● ●●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ●● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ●● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ●● ● ●● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ●● ● ●● ● ● ● ● ● ● ● ● ● ●●● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ●●● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ●●●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ●● ● ● ● ● ● ● ● ● ● ●●● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●●● ●● ●● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ●●● ● ● ●● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●●● ● ●● ●● ●● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ●● ●● ● ● ● ● ●● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ●●● ● ● ● ● ● ● ● ●● ● ● ● ●

0.00

0.05

0.10

0.15

0.20

0.25

0

1000 2000 3000 4000

Cmin

pdenit

0

100

200

300

400

bwO2

● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●●● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ●●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ●● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ●● ● ●● ● ● ● ● ● ●● ● ●● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ●●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ●● ● ● ● ● ●● ● ● ● ● ● ● ● ● ●● ● ● ●● ● ● ● ● ●● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ●● ● ● ● ● ● ●● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ●●● ●● ● ● ● ● ● ● ● ● ●●● ● ● ● ●● ●● ● ●● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ●●●● ● ● ●● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ●● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ●● ● ● ●● ● ● ● ● ● ●● ●● ● ●● ● ● ● ●● ● ● ● ● ● ●●● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ●●● ● ● ● ● ● ● ● ● ● ●● ● ●● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ●● ●● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●●● ● ● ● ● ● ● ● ●● ●● ● ● ● ●● ● ● ●●●● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ●

0.00

0.05

0.10

0.15

0.20

0.25

0

1000 2000 3000 4000

Cmin

pdenit

0

100

200

300

400

bwO2

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0

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Cmin

pdenit

0

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bwO2

● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ●● ● ● ● ● ● ● ● ● ● ●●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ●● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ●● ● ●● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ●● ●● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ●●● ● ● ● ● ● ● ● ● ●● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ●● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ●● ●● ● ● ● ● ● ●● ● ● ●● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ●● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ●● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ● ●

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Cmin

pdenit

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