Viti 1: The Growing Environment Flashcards

1
Q

Photosynthesis in a nutshell:

A

Sunlight energy allows chlorophyll (leaves) to combine water and CO2 to make sucrose, later transformed into glucose and fructose in the vine itself.

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2
Q

Glucose gives…

A

Larger carbohydrates e.g. cellulose (building the vine), tannins, acids and flavour molecules.

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3
Q

Vine temperatures:

A

Dormant below 10 degrees, growth peaks between 22 and 25 degrees. Growth slows above this, as needs outpace its speed of sugar production. Freeze injury begins at -15, serious at -20 and fatal at -25.

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4
Q

Sunlight intensity:

A

Reduces as the angle at which it hits the ground reduces from 90 degrees to 0. Light beams have to travel through greater thickness of atmosphere.

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5
Q

Sites facing east:

A

Rays less scattered in morning as earth has cooled and dust has settled.

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6
Q

Sites facing west:

A

BAD! 1. Sunlight scattered by dust settled after being lifted by warming air. 2. They face damper and cooler weather conditions.

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7
Q

Soils on slopes:

A

Poorer, more coarse and better drained. Moderates vigour. BUT - lifts costs and runs risk of erosion. Isolated hills often best as they avoid descending cold air from main slopes (e.g. hill of Corton, Montagne de Reims).

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8
Q

Forests:

A

Act as windbreaks, store heat and reduce erosion. BUT - increase humidity and decrease temperature of mesoclimate and can harbour birds.

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9
Q

Vigorous canopy can:

A

Reduce flower initiation and berry set (shading), give more acidity (cooling), reduce sugars (humidity and shading) and encourage competition between shoot tips and berries (stunted ripening).

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10
Q

Temperature’s impact on yield:

A

Rate of growth, number of flower clusters produced, their size and the success of setting into berries.

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11
Q

Temperature’s impact on quality:

A

Level of yield, accumulation of sugars, reduction of acidity and development of aromas.

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12
Q

Amerine and Winkler’s heat summation system:

A
  1. Mean temp. for month, subtracting 10 degrees and multiply by number of days in month. Sums are totalled for growing season months to give figures in Growing Degree Days (GDD). 1370, 1370-1650, 1650-1930, 1930-2200 and over 2200. Sunlight, humidity and temp. variability not taken into account - vine growth slows above 30 degrees.
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13
Q

Prevailing Australian heat summation system:

A

Smart and Dry

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14
Q

Rainfall requirements:

A

500mm/year in cool climate, up to 750mm/year in hotter climate.

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15
Q

Calculation for rainfall:

A

1mm of rainfall on 1 square metre is 1 litre.

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16
Q

Substance responsible for ‘green’ flavours:

A

Pyrazines

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17
Q

Regions of higher latitude:

A

Longer days, longer ripening window.

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18
Q

Sunshine’s impact on vine:

A

Bud viability, flower initiation, berry ripening, cane maturation and rate of photosynthesis.

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19
Q

Sunshine hours needed for ripe fruit:

A

A minimum of 1250 hours. Amount of available sunshine will decrease by up to 10% if near to town or city (pollution).

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20
Q

Berry scorching most likely:

A

After leaf stripping or spray application.

21
Q

Annual temp. and altitude:

A

Mean annual temp. decreases 0.6 deg with every 100 metre rise above sea level. Loss of 105 GDD a year.

22
Q

Soil fertility:

A

TOSMAWA! Texture, organic matter content, structure, mineral content, air and water availability and acidity/alkalinity.

23
Q

Soil particles:

A

Diameter measured in mm. CSFSG: clay, silt, fine sand, sand and gravel. 0, 0.002, 0.02, 0.2, 2 and 2+

24
Q

Clay soils:

A

Hold more moisture, made of small particles. Negatively charged, will hold more minerals. They stay cool, they swell and crack, they damage roots, they get sticky and their structure deteriorates as they’re worked.

25
Q

Loam:

A

Balance of clay, silt and sand. Clay’s nutrient holding and drainage of sand.

26
Q

Sandy/gravelly soils:

A

Good drainage and encourage vine to grow deeper roots to find consistent water supplies. Also warm up more quickly.

27
Q

Limestone soil:

A

Sedimentary, rich in calcium carbonate, alkaline (usually) and free-draining.

28
Q

Chalk:

A

Like limestone, but less dense. Drains very well.

29
Q

Dolomite:

A

High in magnesium, sedimentary.

30
Q

Sandstone:

A

Made up of quartz (compressed sand particles), sedimentary.

31
Q

Shale:

A

Originally made of clay, soft and sedimentary.

32
Q

Slate:

A

Shale metamorphosised by high pressures and temps. Harder, less porous and found in Mosel.

33
Q

Granite:

A

Hard, dense, free-draining, igneous (solidified magma).

34
Q

Volcanic rocks:

A

Surface lava (Santorini and Madeira).

35
Q

Good soil structure:

A

Stable particle crumbs of 1-5 mm diameter. Organic matter content 3-10%.

36
Q

Poor soil structure can lead to…

A

Capping/crusting, puddling (risks erosion) and sieving (clay deposited and causes clogging).

37
Q

Organic matter consists of:

A

SSCNLM! Sugars, starches, cellulose, nitrogenous compounds, lignin and mineral matter. Breaks down sugars in mineralisation.

38
Q

Humus:

A

Partially decomposed organic matter. Gives structure, retains nutrients (negatively charged), retains water, swells and shrinks and darkens colour for absorption.

39
Q

Aeration:

A

Feeds aerobic organisms, harms bad anaerobic organisms, removes CO2 and feeds roots for growth.

40
Q

Compaction:

A

Can lead to poor rain infiltration and poor soil structure.

41
Q

Nitrogen (N):

A

Drives biochemical reactions and stimulates photosynthesis. Boosts plant growth.

42
Q

Phosphorous (P):

A

Aids energy fixation. Encourages root growth and ripening.

43
Q

Potassium (K):

A

Regulates flow of sugar and water. Encourages ripening.

44
Q

Calcium (Ca):

A

Regulates cell acidity. Forms cell walls.

45
Q

Sulfur (S):

A

Forms part of amino acids and enzymes.

46
Q

Magnesium (Mg):

A

Big part of chlorophyll. Encourages ripening.

47
Q

pH:

A

Measures concentration of hydrogen ions in soil solution. 4-6.9 is acid, 7.1-8.5 is alkaline. Vine can’t tolerate pH below 5 - aluminium exposed and kills plant.

48
Q

Limestone-rich soils:

A

High pH. Iron uptake inhibited, chlorosis risk increased.

49
Q

Over-worked soil:

A

Become more acidic with breakdown of organic material.