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The BIFoR FACE facility: ecohydrological responses of a mature deciduous woodland to elevated carbon dioxide Rob MacKenzie on behalf of the nascent BIFoR team

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Page 1: The BIFoR FACE facility: ecohydrological responses of a ... Hydrology 2015... · BIFoR FACE top-level research questions 1. Does elevated CO 2 increase the carbon storage in mature

The BIFoR FACE facility: ecohydrological responses of a mature deciduous woodland to elevated carbon dioxide

Rob MacKenzie on behalf of the nascent BIFoR team

Page 2: The BIFoR FACE facility: ecohydrological responses of a ... Hydrology 2015... · BIFoR FACE top-level research questions 1. Does elevated CO 2 increase the carbon storage in mature

Mature forests are a carbon sink – because of elevated CO2, nitrogen deposition, &

changing climate

(Odum’s 1-D steady-state is inapplicable for finite patches with varying boundary conditions)

Page 3: The BIFoR FACE facility: ecohydrological responses of a ... Hydrology 2015... · BIFoR FACE top-level research questions 1. Does elevated CO 2 increase the carbon storage in mature

BIFoR FACE top-level research questions

1. Does elevated CO2 increase the carbon storage in mature woodlands?

2. Do other macro- or micro-nutrients limit the uptake of carbon?

3. What aspects of biodiversity and ecosystem structure-and-function alter?

4. How can lessons learnt be generalised to other woodlands and forests? (Global Network of second-generation Forest FACE experiments)

Norby, R. J., …, A. R. MacKenzie, R. Thomas…, Model-data synthesis for the next generation of forest FACE experiments, New Phytologist, 2015, DOI: 10.1111/nph.13593

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CO2

Free-Air Carbon Dioxide Enrichment (FACE) Methodology

Aim to run experiment for 10 years +

“The ecological equivalent of the Large Hadron Collider”

Wind 30 m diameter

24

-27

m, d

epen

din

g o

n

loca

l can

op

y h

eigh

t

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Aquatic systemsSoil horizons

Microbial pathogens

Feeding insects

Parasitic insects

Birds and free moving

insectivores

Litter Layer

Tree roots and rhizosphere symbiotic

microbes

Leaf fall

Leaf decomposition

Nutrient flow through soil

Nutrient fixation

Detritivores(Invertebrate and microbial )

Trees, shrubs and ground plants

Bed Rock

Nutrient flow through water

systems(invertebrates and microbial)

Nutrient emissions in VOCs

VOCs - parasite attractants

Leaf damage

Tissue damage

Anti-herbivore defence

Anti-microbial defence

Pollinator insects

Tertiary and quaternary

feeding animals

FACE 2.0 …SEX AND DEATH

Plant-pathogen molecular interactions - Current tree pathogens - Which pathogens will

emerge or cause most devastation in the changing environment?

Plant-insect interactions and chemical ecology

Rhizosphere microbiology, nutrient fixation and cycling

Plant Physiology - Tree growth - photosynthesis and

respiration (Which trees will be the winners under increased CO2?

- Trees role in C and N cycles

Animal behaviour

Litter layer: Invertebrate detritivores and nutrient cycling

Aquatic zoology and animal behaviour

Page 6: The BIFoR FACE facility: ecohydrological responses of a ... Hydrology 2015... · BIFoR FACE top-level research questions 1. Does elevated CO 2 increase the carbon storage in mature
Page 7: The BIFoR FACE facility: ecohydrological responses of a ... Hydrology 2015... · BIFoR FACE top-level research questions 1. Does elevated CO 2 increase the carbon storage in mature
Page 8: The BIFoR FACE facility: ecohydrological responses of a ... Hydrology 2015... · BIFoR FACE top-level research questions 1. Does elevated CO 2 increase the carbon storage in mature

Laser Scanning

Image from Eric Casella, Forest Research

3D reconstruction of trees to measure volume of wood

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The BIFoR FACE facility

FACE – 3 no-infrastructure controls (ambient air);

3 ambient-air FACE rings &

3 treatments of +150 ppmv CO2

Fieldwork compound – cabins & CO2 reservoir

a decadal experiment to study the response of a mature temperate deciduous forest ecosystem to elevated CO2.

1 km

Page 10: The BIFoR FACE facility: ecohydrological responses of a ... Hydrology 2015... · BIFoR FACE top-level research questions 1. Does elevated CO 2 increase the carbon storage in mature

BIFoR FACE: ring structure

30m

24-27m, depending on local canopy height

Page 11: The BIFoR FACE facility: ecohydrological responses of a ... Hydrology 2015... · BIFoR FACE top-level research questions 1. Does elevated CO 2 increase the carbon storage in mature
Page 12: The BIFoR FACE facility: ecohydrological responses of a ... Hydrology 2015... · BIFoR FACE top-level research questions 1. Does elevated CO 2 increase the carbon storage in mature

Core Measurements at Mill Haft

Underway – Dendrometers

– LAI - via hemispherical photography

– Leaf gas exchange

– Stream Monitoring (Discharge,Water temperature, pH, Turbidity, Dissolved oxygen, Nitrate & Nitrite, Dissolved organic carbon

– Eddy covariance flux measurements (CO2,H2O, CH4)

– Phenocam

– Meteorology above & below canopy

– Plant tissue sampling

– Invertebrate sampling

– Litter traps

– Soil sampling

Pending – Soil gas fluxes

– Minirhyzotrons

Page 13: The BIFoR FACE facility: ecohydrological responses of a ... Hydrology 2015... · BIFoR FACE top-level research questions 1. Does elevated CO 2 increase the carbon storage in mature

Gauging stations

10 min measurements of: • Discharge • Water temperature • pH • Turbidity • Dissolved oxygen • NO3 • Dissolved organic carbon (incl. different fractions)

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Data transferred via telemetry system to online server. Allows for continuous real-time viewing through web browser.

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Evidence of sub-daily NO3 cycles

2 days

Page 16: The BIFoR FACE facility: ecohydrological responses of a ... Hydrology 2015... · BIFoR FACE top-level research questions 1. Does elevated CO 2 increase the carbon storage in mature

FACE ring hydrological monitoring 12 dataloggers distributed between six rings

Dendrometer

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Depth-variable response of soil moisture to rain event

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0

50

100

150

200

250

50 100 150 200 250

90% distance (m) Peak (m) Flux Footprint Estimates

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Preliminary Flux results

400

200

0

He

at F

lux (

W/m

2)

01/05/2015 03/05/2015 05/05/2015 07/05/2015

Date & Time

300

200

100

0

Win

d D

ir (ºN)

8

6

4

2

Wsp

d (

m/s

)

-10

-5

0

5

10

CO

2 (µ

mo

l s-1 m

-2)

-100x10-3

-50

0

50

100

CH

4 (µ

mo

l s

-1 m

-2)

Wind Direction Wind Speed

Latent Heat (E) Sensible Heat (H)

CO2 CH4 (5pnt mean)

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Diurnal Cycles

-4

-2

0

2C

O2 (µ

mo

l s

-1 m

-2)

06:0001/01/1904

12:00 18:00

Time of Day

200

150

100

50

0

He

at F

lux (W

/m2)

Respiration

Net photosynthesis

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BIFoR Field Facility: Timeline

2014 2015 2016

Baseline

FACE design FACE build

FACE operation

Other field activities (by agreement)

2014 2026

FC SIS 2015-2020 HadGEM 3 JULES 4.0

HadGEM 13?? JULES 14.0??

FC SIS 2020-25

IPCC AR6 IPCC AR7

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BIFoR summer intensive 2015