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Understanding your site: soils, climate,
rootstocks and management strategies
Cornelis (Kees) van Leeuwen
Bordeaux Sciences Agro - UMR EGFV
Institut des Sciences de la Vigne et du Vin
1
Outline
• Define terroir
• Major environmental factors involved in
terroir expression are :
– Temperature
– Water status
– Nitrogen status
• Measurement of terroir parameters
• Managing terroir
2
I – define terroir
3
44
• Terroir is a sense of place
• « Terroir can be defined as an interactive cultivated
ecosystem (agrosystem), in a given place, including
climate, soil and the vine » (Seguin, 1983; 1986; 1988)
• Human factors are also important, because terroir is
managed
• These have a historical dimension (trial and error)
• Science can explain terroir
• Science can help to maximize terroir management
Terroir is pluri-disciplinary
Terroir is a cultivated ecosystem
CO2
waterradiation
water nutrients
(in particular N)
temperature
viticultural techniques
quality and typicity
vinification et aging
plant material
5
66
• Saying a soil is « a clay-loam calcareous soil on Tertiary
hard limestone bedrock » is not measurable
• Idem for a « mediterranean climate »
• Soil act on:
– Water uptake
– Offer of nutrients and in particular nitrogen
– Temperature in the root zone
• Climate acts on:
– Air temperature
– Water uptake
– Radiation
We have to break down each factor in
« measurable » effects
II - Major environmental factors
7
Average temperature April – September
2001 – 2005, Bordeaux
Bois, 2007
Air temperature
Timing of phenology
Grape ripening possibilities
Photo credit: I. Garcia de Cortazar 8
Warm soils Cool soils
Stony soil
Soil with
water logging
Shallow soil
Loamy soil
9
Soil temperature
1010
• Air temperature can be studied at several scales
– Macro
– Meso
– Micro
– These scales interact (nested effect)
• Air temperature has a major effect in viticulture
– Drives potential for grape growing
– Drives cultivar distribution
– Drives wine style (cool climate vs warm climate wines)
– Vintage effect
• Soil temperature has a more limited effect
– Cultivar distribution inside a region
– Harvest dates
Temperature acts on phenology and grape
ripening
Vine water status
• Vine water status depends on:
– Soil Water Holding Capacity (SWHC)
– Climatic parameters (ET0 and rainfall)
0
50
100
150
200
250
01/04/1993
11/04/1993
21/04/1993
01/05/1993
11/05/1993
21/05/1993
31/05/1993
10/06/1993
20/06/1993
30/06/1993
10/07/1993
20/07/1993
30/07/1993
09/08/1993
19/08/1993
29/08/1993
08/09/1993
18/09/1993
28/09/1993
Bilanhydriqueetprécipitations(mm)
Précipitations (mm) Bilan hydrique 1993
SWHC
Water balance
Rainfall
11
12
Water deficit
induces :
• Early shoot growth
cessation
• Reduced berry size
• Low malate
• High anthocyanins
Van Leeuwen et al., 2009 JISVV
13
• No relationship has been established between specific
soil components (Mg++, K+, Fe3+, oligo elements…) and
wine quality
• However, nitrogen does have an effect on vine vigor and
berry composition
• When vines does not receive nitrogen fertilization, vine N
uptake depends on soil parameters:
– Soil organic matter content and C/N ratio
– Soil temperature
– Soil aeration
– pH
– Soil moisture content
• Vine nitrogen uptake is soil related
Soil minerals
14
Moderate to low nitrogen increases
quality in red wine production
• Plots with similar
water status
• Variable N uptake
• Low N:
• Lower vigor, yield
and berry weight
• Lower acidity
• Higher sugar and
anthocyanins
Trégoat et al., 2002
Low
N
(4A)
High
N
(4B)
N-tester values 446 525
Assimilable must nitrogen (mg N/L) 63 134
Shoot growth cessation (day of the
year)
260 269
Yield (kg/vine) 1.8 2.2
Berry weight (g) 1.67 1.84
Grape sugar (g/L) 247 227
Anthocyanin (mg/L) 1490 1250
Total Phenolics Index 54 43
Total acidity (g tartrate/L) 4.7 5.4
Malic acid (g/L) 2.0 2.4
Merlot
15
Low nitrogen decreases aroma
expression in white wine production
0 N 60 N
P-4MMP (ng eq/L) 405 (a) 715 (b)
P-4MMPOH (ng eq/L) 760 (a) 2059 (b)
P-3MH (ng eq/L) 3358 (a) 14812 (b)
Total polyphenol
index
0.28 (a) 0.21 (b)
Glutathione 17.9 (a) 120 (b)
Choné et al. 2006
Sauvignon blanc
Vine nitrogen status
• Nitrogen impacts on :
– Yield and vigor
– Grape and wine composition
• Vine nitrogen status varies with :
– Soil type
– Climatic conditions of the vintage (turn over of organic matter)
– Fertilization and vineyard floor management
16
III – Measurement of terroir
parameters
17
Soil mapping
18
Soil mapping assited by geophysics
• Very precise soil maps can be made after measuring
soil resistivity with electric tomography
19
Climate
20
21
Critical climatic parameters
• Temperatures ->
phenology
• Rainfall -> water status
• ET0 -> water status
• Solar radiation ->
photosynthesis, color
accumulation
Classic weather
station (many
parameters)
Miniaturized
weather station
(temperature
only)
Measurement and fine scale mapping of
air temperatures
• Weather stations become smaller and more
affordable : increased density of measurements
• Spatial modelling using environmental co-variables
Saint-Emilion – Pomerol area 22
Phenology
23
Measure phenology
• Timing of phenology depends on temperature
and grapevine variety
• Timing of phenology is a key factor in terroir
expression
• Precise assessment of phenological stages is
important
• « 50% » date: bud break, flowering, veraison
• This knowledge helps to orientate variety
choices
24
25
Predicting phenology
• Vine phenology is temperature driven
• Phenology can be predicted with process-
based models, using temperature as input
data
• Examples: Winkler, Huglin
New model for predicting phenology:
Grapevine Flowering Veraison model (GFV)
• Timing of phenology can be accurately modelled from air
temperatures
• GFV model : temperature summation, base 0°C, starting at
DOY 90 (1st of March)
c) Chardonnay
Observation (DOY)
100 120 140 160 180 200 220 240
Prediction(DOY)
100
120
140
160
180
200
220
240
Flowering modeling
(Parker et al., 2011) Classification of the timing of veraison
(Parker et al., 2013) 26
Variety F*
Chasselas 2342
Pinot noir 2507
Sauvignon blanc 2517
Chardonnay 2541
Riesling 2584
Syrah 2598
Merlot 2627
Cabernet-Sauvignon 2641
Cabernet franc 2655
Grenache 2750
Ugni blanc 2777
Validation GFV model on a trial with 52
varieties
27
Flowering
Difference
observation -
model in days
(relative values)
Difference
observation -
model in days
(absolute values)
Most
extreme
difference
(days)
2012 1.5 2.0 5.7 Mourvèdre
2013 6.2 6.2 12.7 Rousanne
2014 2.7 3.3 10.1 Tempranillo
2015 0.7 2.2 6.9 Roussanne
average 1.7 3.4
Veraison
Difference
observation -
model in days
(relative values)
Difference
observation -
model in days
(absolute values)
Most
extreme
difference
(days)
2012 0.4 3.2 16,5 Tannat
2013 8.2 8.2 14,4 Tempranillo
2014 0.4 2.2 7,2 Carignan
2015 3,3 4.1 12,7 Xynomavro
average 3.1 4.4
Water
28
29
Soil based measurements are poor estimators of
water status in vines because of deep rooting
• Soil water potential :
– Tensiometers
– Watermark device (gypsum block)
• Available soil water :
– Neutron moisture probe
– Time Domaine Reflectometry (TDR)
– Capacitance probe
30
Water potentials
• It is possible to measure water potential
in vine organs
• Tool : pressure chamber
• Easy to measure
• Good precison, covers a wide range of
water deficits
• Equipment is affordable for a
winegrowing estate
•  Water potential measurement has
become the technique of reference
31
Stem water potential is great tool to
monitor vine water status
-2,0
-1,8
-1,6
-1,4
-1,2
-1,0
-0,8
-0,6
-0,4
-0,2
0,0
Juin Juillet Août Septembre Octobre
Potentieltige(MPa)
2004
2005
2007
-2,0
-1,8
-1,6
-1,4
-1,2
-1,0
-0,8
-0,6
-0,4
-0,2
0,0
Juin Juillet Août Septembre Octobre
Potentieltige(MPa)
Sol graveleux
Sol sableux avec nappe d'eau
Sol argileux
To assess the dynamics of vine
water status during a vintage
To assess the dynamics of
vine water status as a
function of soil type
Van Leeuwen et al., 2009 JISVV
Or to monitor vine water
status in order to optimize
irrigation strategy
32
Carbon isotope discrimination: an easy to-use
reliable indicator of vine water status
• Ambient CO2 contains 98.9% of 12C and 1.1% of 13C
• During photosynthesis 13C, heavier than 12C, is
discriminated
• This isotope discrimination is reduced when stomata
are closed (water deficit)
• => 13C/12C ratio in metabolites from photosynthesis
indicates vine water status
• 13C/12C (called δ13C) is expressed in ‰ against a
standard
– Range in grape sugar from -27 (no water deficit) to -20
(severe water deficit)
Van Leeuwen et al. 2001; Gaudillère et al. 2002
33
δ13C is highly correlated with stem water potential and
with the level of photosynthesis
Corrélation entre le potentiel tige mesuré le 31 août 2010 et le δ
13
C
mesuré sur les sucres du moût à maturité
R2
= 0,84
-28
-27
-26
-25
-24
-23
-22
-21
-20
-19
-2 -1,8 -1,6 -1,4 -1,2 -1 -0,8 -0,6 -0,4
Potentiel tige (MPa)
δ13
C(p.1000)
Corrélation entre le niveau de photosynthèse mesuré le 31 août 2010 en
début d'après-midi et le δ13
C mesuré sur les sucres du moût à maturité
R2
= 0,67
-28
-27
-26
-25
-24
-23
-22
-21
-20
-19
0 2 4 6 8 10 12 14
Photosynthèse (μmole*m-2
*s-1
)
δ13
C(p.1000)
van Leeuwen and Destrac,
Saint-Emilion, 2010,
unpublished data
34
Thresholds for water deficit
δ
13
C
Midday Stem
Water Potential
(MPa)
Midday Leaf
Water Potential
(MPa)
Pre-dawn Leaf
Water Potential
(MPa)
No water deficit < -26 > -0.6 > -0.9 > -0.2
Weak water deficit -24.5 to -26 -0.6 to -0.9 -0.9 to -1.1 -0.2 to -0.3
Moderate to weak water deficit -23 to -24.5 -0.9 to -1.1 -1.1 to -1.3 -0.3 to -0.5
Moderate to severe water deficit -21.5 to -23 -1.1 to -1.4 -1.3 to -1.4 -0.5 to -0.8
Severe water deficit > -21.5 < -1.4 < -1.4 < -0.8
-20 -21 -22 -23 -24 -25 -26 -27
35
Advantage of the δ13C technique
• Easy to measure (specialized labs)
• Integrated measurement of vine water status
during the fruit ripening period
• Many plots can be sampled
• Validation of irrigation strategies
• Not for day to day irrigation management
Mapping vine water status with δ13C
Water statusSoil type δ13C
Mapping vine water
status (10 analyses / ha);
SOVIVINS
36
Nitrogen
37
38
Assessment of nitrogen status is easy with
plant based indicators
• Leaf blade N
• Petiole N
• Grape juice Yeast Available Nitrogen (YAN)
• Leaf blade color (SPAD)
Mapping vine nitrogen status with Yeast
Available Nitrogen
• Yeast Available
Nitrogen (YAN) is
a good indicator
of vine nitrogen
status
Map of YAN (10 analyses / ha)
39
Brief summary
• Several factors are involved in terroir expression:
• Climate : temperature, impact on water status (ET0 and
rainfall)
• Soil : soil temperature, impact on vine water status and
impact on vine nutrient status (in particular N)
• These factors interact with plant material (variety and root
stock), training system and vineyard floor management
• These factors can be measured at fine resolution
• How can terroir be managed at the block level to maximize
yield and quality?
40
III – Managing terroir
41
• Best sites allow ripening to occur in the window 10 September
– 10 October (NH)
• Great variation in temperature requirements among varieties
allow obtaining ripeness inside this window in a wide range of
climates
Managing temperatures through variety
choice
42
Parker, 2012
Modelled sugar ripeness (200 g/L):
50 days between Pinot noir and
Zinfandel
• Knowledge on local temperature variability can be used to :
– fit variety choice to local climatic conditions
– adapt to climate change
Managing temperatures through site
selection
43Saint-Emilion - Pomerol Douro Valley (Jones, 2012)
Managing the timing of ripeness by
adapting variety choice to soil temperature
• Bordeaux has a marginal climate for ripening
Cabernet-Sauvignon
– Best results for Cabernet-Sauvignon on warm soils
Warm soil (gravel) :
Cabernet-Sauvignon 44
Cool soil (deep, loamy) :
Merlot
Managing drought by adapting plant
material and training system
• In dry climates use :
– drought resistant rootstocks
– drought resistant varieties
– adapted training systems
– soils with at least medium Soil Water Holding Capacity
– irrigation
45
44-53M, Ramsey,
1103P, 1447P, 110R,
140Ru
Grenache Dry farmed vineyard in Spain
Managing nitrogen status through vineyard
floor management and fertilization
46
Yeast Available Nitrogen (YAN) during grape ripening
0
50
100
150
200
250
03-sept 08-sept 13-sept 18-sept 23-sept 28-sept 03-oct 08-oct 13-oct
YAN(mg/L)
Cover crop
+N fertlization
Controll
Hamieau, 2014
Conclusion
• Terroir is all about interactions between the vine and its local
environment
• Impact of environmental factors (soil, climate) should be
broken down in measurable factors (water, temperature, light)
to be understood
• Some terroir factors matter more than others
• Tools have been developped to measure and map major
terroir factors
• This knowledge should be used to manage terroir through
– Plant material
– Management strategies
• This allows to maximizing terroir expression in a given site
47
Continuing education at Bordeaux
Sciences Agro
48
49
Extension in Burgundy from 13-17 March 2017
6-10 March 2017

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2017 Oregon Wine Symposium | The Myth of Terroir and Understanding Your Site: Soils, Rootstalks, Varieties and Management Strategies

  • 1. Understanding your site: soils, climate, rootstocks and management strategies Cornelis (Kees) van Leeuwen Bordeaux Sciences Agro - UMR EGFV Institut des Sciences de la Vigne et du Vin 1
  • 2. Outline • Define terroir • Major environmental factors involved in terroir expression are : – Temperature – Water status – Nitrogen status • Measurement of terroir parameters • Managing terroir 2
  • 3. I – define terroir 3
  • 4. 44 • Terroir is a sense of place • « Terroir can be defined as an interactive cultivated ecosystem (agrosystem), in a given place, including climate, soil and the vine » (Seguin, 1983; 1986; 1988) • Human factors are also important, because terroir is managed • These have a historical dimension (trial and error) • Science can explain terroir • Science can help to maximize terroir management Terroir is pluri-disciplinary
  • 5. Terroir is a cultivated ecosystem CO2 waterradiation water nutrients (in particular N) temperature viticultural techniques quality and typicity vinification et aging plant material 5
  • 6. 66 • Saying a soil is « a clay-loam calcareous soil on Tertiary hard limestone bedrock » is not measurable • Idem for a « mediterranean climate » • Soil act on: – Water uptake – Offer of nutrients and in particular nitrogen – Temperature in the root zone • Climate acts on: – Air temperature – Water uptake – Radiation We have to break down each factor in « measurable » effects
  • 7. II - Major environmental factors 7
  • 8. Average temperature April – September 2001 – 2005, Bordeaux Bois, 2007 Air temperature Timing of phenology Grape ripening possibilities Photo credit: I. Garcia de Cortazar 8
  • 9. Warm soils Cool soils Stony soil Soil with water logging Shallow soil Loamy soil 9 Soil temperature
  • 10. 1010 • Air temperature can be studied at several scales – Macro – Meso – Micro – These scales interact (nested effect) • Air temperature has a major effect in viticulture – Drives potential for grape growing – Drives cultivar distribution – Drives wine style (cool climate vs warm climate wines) – Vintage effect • Soil temperature has a more limited effect – Cultivar distribution inside a region – Harvest dates Temperature acts on phenology and grape ripening
  • 11. Vine water status • Vine water status depends on: – Soil Water Holding Capacity (SWHC) – Climatic parameters (ET0 and rainfall) 0 50 100 150 200 250 01/04/1993 11/04/1993 21/04/1993 01/05/1993 11/05/1993 21/05/1993 31/05/1993 10/06/1993 20/06/1993 30/06/1993 10/07/1993 20/07/1993 30/07/1993 09/08/1993 19/08/1993 29/08/1993 08/09/1993 18/09/1993 28/09/1993 Bilanhydriqueetprécipitations(mm) Précipitations (mm) Bilan hydrique 1993 SWHC Water balance Rainfall 11
  • 12. 12 Water deficit induces : • Early shoot growth cessation • Reduced berry size • Low malate • High anthocyanins Van Leeuwen et al., 2009 JISVV
  • 13. 13 • No relationship has been established between specific soil components (Mg++, K+, Fe3+, oligo elements…) and wine quality • However, nitrogen does have an effect on vine vigor and berry composition • When vines does not receive nitrogen fertilization, vine N uptake depends on soil parameters: – Soil organic matter content and C/N ratio – Soil temperature – Soil aeration – pH – Soil moisture content • Vine nitrogen uptake is soil related Soil minerals
  • 14. 14 Moderate to low nitrogen increases quality in red wine production • Plots with similar water status • Variable N uptake • Low N: • Lower vigor, yield and berry weight • Lower acidity • Higher sugar and anthocyanins Trégoat et al., 2002 Low N (4A) High N (4B) N-tester values 446 525 Assimilable must nitrogen (mg N/L) 63 134 Shoot growth cessation (day of the year) 260 269 Yield (kg/vine) 1.8 2.2 Berry weight (g) 1.67 1.84 Grape sugar (g/L) 247 227 Anthocyanin (mg/L) 1490 1250 Total Phenolics Index 54 43 Total acidity (g tartrate/L) 4.7 5.4 Malic acid (g/L) 2.0 2.4 Merlot
  • 15. 15 Low nitrogen decreases aroma expression in white wine production 0 N 60 N P-4MMP (ng eq/L) 405 (a) 715 (b) P-4MMPOH (ng eq/L) 760 (a) 2059 (b) P-3MH (ng eq/L) 3358 (a) 14812 (b) Total polyphenol index 0.28 (a) 0.21 (b) Glutathione 17.9 (a) 120 (b) Choné et al. 2006 Sauvignon blanc
  • 16. Vine nitrogen status • Nitrogen impacts on : – Yield and vigor – Grape and wine composition • Vine nitrogen status varies with : – Soil type – Climatic conditions of the vintage (turn over of organic matter) – Fertilization and vineyard floor management 16
  • 17. III – Measurement of terroir parameters 17
  • 19. Soil mapping assited by geophysics • Very precise soil maps can be made after measuring soil resistivity with electric tomography 19
  • 21. 21 Critical climatic parameters • Temperatures -> phenology • Rainfall -> water status • ET0 -> water status • Solar radiation -> photosynthesis, color accumulation Classic weather station (many parameters) Miniaturized weather station (temperature only)
  • 22. Measurement and fine scale mapping of air temperatures • Weather stations become smaller and more affordable : increased density of measurements • Spatial modelling using environmental co-variables Saint-Emilion – Pomerol area 22
  • 24. Measure phenology • Timing of phenology depends on temperature and grapevine variety • Timing of phenology is a key factor in terroir expression • Precise assessment of phenological stages is important • « 50% » date: bud break, flowering, veraison • This knowledge helps to orientate variety choices 24
  • 25. 25 Predicting phenology • Vine phenology is temperature driven • Phenology can be predicted with process- based models, using temperature as input data • Examples: Winkler, Huglin
  • 26. New model for predicting phenology: Grapevine Flowering Veraison model (GFV) • Timing of phenology can be accurately modelled from air temperatures • GFV model : temperature summation, base 0°C, starting at DOY 90 (1st of March) c) Chardonnay Observation (DOY) 100 120 140 160 180 200 220 240 Prediction(DOY) 100 120 140 160 180 200 220 240 Flowering modeling (Parker et al., 2011) Classification of the timing of veraison (Parker et al., 2013) 26 Variety F* Chasselas 2342 Pinot noir 2507 Sauvignon blanc 2517 Chardonnay 2541 Riesling 2584 Syrah 2598 Merlot 2627 Cabernet-Sauvignon 2641 Cabernet franc 2655 Grenache 2750 Ugni blanc 2777
  • 27. Validation GFV model on a trial with 52 varieties 27 Flowering Difference observation - model in days (relative values) Difference observation - model in days (absolute values) Most extreme difference (days) 2012 1.5 2.0 5.7 Mourvèdre 2013 6.2 6.2 12.7 Rousanne 2014 2.7 3.3 10.1 Tempranillo 2015 0.7 2.2 6.9 Roussanne average 1.7 3.4 Veraison Difference observation - model in days (relative values) Difference observation - model in days (absolute values) Most extreme difference (days) 2012 0.4 3.2 16,5 Tannat 2013 8.2 8.2 14,4 Tempranillo 2014 0.4 2.2 7,2 Carignan 2015 3,3 4.1 12,7 Xynomavro average 3.1 4.4
  • 29. 29 Soil based measurements are poor estimators of water status in vines because of deep rooting • Soil water potential : – Tensiometers – Watermark device (gypsum block) • Available soil water : – Neutron moisture probe – Time Domaine Reflectometry (TDR) – Capacitance probe
  • 30. 30 Water potentials • It is possible to measure water potential in vine organs • Tool : pressure chamber • Easy to measure • Good precison, covers a wide range of water deficits • Equipment is affordable for a winegrowing estate •  Water potential measurement has become the technique of reference
  • 31. 31 Stem water potential is great tool to monitor vine water status -2,0 -1,8 -1,6 -1,4 -1,2 -1,0 -0,8 -0,6 -0,4 -0,2 0,0 Juin Juillet Août Septembre Octobre Potentieltige(MPa) 2004 2005 2007 -2,0 -1,8 -1,6 -1,4 -1,2 -1,0 -0,8 -0,6 -0,4 -0,2 0,0 Juin Juillet Août Septembre Octobre Potentieltige(MPa) Sol graveleux Sol sableux avec nappe d'eau Sol argileux To assess the dynamics of vine water status during a vintage To assess the dynamics of vine water status as a function of soil type Van Leeuwen et al., 2009 JISVV Or to monitor vine water status in order to optimize irrigation strategy
  • 32. 32 Carbon isotope discrimination: an easy to-use reliable indicator of vine water status • Ambient CO2 contains 98.9% of 12C and 1.1% of 13C • During photosynthesis 13C, heavier than 12C, is discriminated • This isotope discrimination is reduced when stomata are closed (water deficit) • => 13C/12C ratio in metabolites from photosynthesis indicates vine water status • 13C/12C (called δ13C) is expressed in ‰ against a standard – Range in grape sugar from -27 (no water deficit) to -20 (severe water deficit) Van Leeuwen et al. 2001; Gaudillère et al. 2002
  • 33. 33 δ13C is highly correlated with stem water potential and with the level of photosynthesis Corrélation entre le potentiel tige mesuré le 31 août 2010 et le δ 13 C mesuré sur les sucres du moût à maturité R2 = 0,84 -28 -27 -26 -25 -24 -23 -22 -21 -20 -19 -2 -1,8 -1,6 -1,4 -1,2 -1 -0,8 -0,6 -0,4 Potentiel tige (MPa) δ13 C(p.1000) Corrélation entre le niveau de photosynthèse mesuré le 31 août 2010 en début d'après-midi et le δ13 C mesuré sur les sucres du moût à maturité R2 = 0,67 -28 -27 -26 -25 -24 -23 -22 -21 -20 -19 0 2 4 6 8 10 12 14 Photosynthèse (μmole*m-2 *s-1 ) δ13 C(p.1000) van Leeuwen and Destrac, Saint-Emilion, 2010, unpublished data
  • 34. 34 Thresholds for water deficit δ 13 C Midday Stem Water Potential (MPa) Midday Leaf Water Potential (MPa) Pre-dawn Leaf Water Potential (MPa) No water deficit < -26 > -0.6 > -0.9 > -0.2 Weak water deficit -24.5 to -26 -0.6 to -0.9 -0.9 to -1.1 -0.2 to -0.3 Moderate to weak water deficit -23 to -24.5 -0.9 to -1.1 -1.1 to -1.3 -0.3 to -0.5 Moderate to severe water deficit -21.5 to -23 -1.1 to -1.4 -1.3 to -1.4 -0.5 to -0.8 Severe water deficit > -21.5 < -1.4 < -1.4 < -0.8 -20 -21 -22 -23 -24 -25 -26 -27
  • 35. 35 Advantage of the δ13C technique • Easy to measure (specialized labs) • Integrated measurement of vine water status during the fruit ripening period • Many plots can be sampled • Validation of irrigation strategies • Not for day to day irrigation management
  • 36. Mapping vine water status with δ13C Water statusSoil type δ13C Mapping vine water status (10 analyses / ha); SOVIVINS 36
  • 38. 38 Assessment of nitrogen status is easy with plant based indicators • Leaf blade N • Petiole N • Grape juice Yeast Available Nitrogen (YAN) • Leaf blade color (SPAD)
  • 39. Mapping vine nitrogen status with Yeast Available Nitrogen • Yeast Available Nitrogen (YAN) is a good indicator of vine nitrogen status Map of YAN (10 analyses / ha) 39
  • 40. Brief summary • Several factors are involved in terroir expression: • Climate : temperature, impact on water status (ET0 and rainfall) • Soil : soil temperature, impact on vine water status and impact on vine nutrient status (in particular N) • These factors interact with plant material (variety and root stock), training system and vineyard floor management • These factors can be measured at fine resolution • How can terroir be managed at the block level to maximize yield and quality? 40
  • 41. III – Managing terroir 41
  • 42. • Best sites allow ripening to occur in the window 10 September – 10 October (NH) • Great variation in temperature requirements among varieties allow obtaining ripeness inside this window in a wide range of climates Managing temperatures through variety choice 42 Parker, 2012 Modelled sugar ripeness (200 g/L): 50 days between Pinot noir and Zinfandel
  • 43. • Knowledge on local temperature variability can be used to : – fit variety choice to local climatic conditions – adapt to climate change Managing temperatures through site selection 43Saint-Emilion - Pomerol Douro Valley (Jones, 2012)
  • 44. Managing the timing of ripeness by adapting variety choice to soil temperature • Bordeaux has a marginal climate for ripening Cabernet-Sauvignon – Best results for Cabernet-Sauvignon on warm soils Warm soil (gravel) : Cabernet-Sauvignon 44 Cool soil (deep, loamy) : Merlot
  • 45. Managing drought by adapting plant material and training system • In dry climates use : – drought resistant rootstocks – drought resistant varieties – adapted training systems – soils with at least medium Soil Water Holding Capacity – irrigation 45 44-53M, Ramsey, 1103P, 1447P, 110R, 140Ru Grenache Dry farmed vineyard in Spain
  • 46. Managing nitrogen status through vineyard floor management and fertilization 46 Yeast Available Nitrogen (YAN) during grape ripening 0 50 100 150 200 250 03-sept 08-sept 13-sept 18-sept 23-sept 28-sept 03-oct 08-oct 13-oct YAN(mg/L) Cover crop +N fertlization Controll Hamieau, 2014
  • 47. Conclusion • Terroir is all about interactions between the vine and its local environment • Impact of environmental factors (soil, climate) should be broken down in measurable factors (water, temperature, light) to be understood • Some terroir factors matter more than others • Tools have been developped to measure and map major terroir factors • This knowledge should be used to manage terroir through – Plant material – Management strategies • This allows to maximizing terroir expression in a given site 47
  • 48. Continuing education at Bordeaux Sciences Agro 48
  • 49. 49 Extension in Burgundy from 13-17 March 2017 6-10 March 2017