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Mechanisms
of terroir
As
more new world producers start to take an interest in terroir,
scientists are turning their attention to defining it and explaining
how it affects a wine. Jamie Goode investigates. (This feature
was originally published in Harpers
Weekly, September 12th 2003)
‘Terroir’
is currently an in vogue concept. Once almost exclusively the preserve
of the old world, it’s now a talking point in the new world, too.
The traditional, old world definition of terroir is quite a tricky one
to tie down, but it can probably best be summed-up as the possession
by a wine of a sense of place, or ‘somewhereness’. That is, a wine
from a particular patch of ground expresses characteristics related to
the physical environment in which the grapes are grown. But why the
sea-change in the new world, where for so longer the job of grape
growing was seen merely as a mundane prelude to the work of the all
powerful winemaker?
Even fairly recently, the new
world response to ‘terroir’ was that it was a last ditch marketing
ploy by European winegrowers who were panicking about their increasing
loss of market share. This turn-around is because new world wine
growers have realized that one of the keys to wine quality is starting
with grapes that show homogeneous (even) levels of ripeness, and the
recognition of the role that natural variation within and between
their vineyards plays. With the increasing adoption of technique known
as precision viticulture, vineyards are commonly broken up into
sub-plots sharing similar characteristics (known as natural or basic
terroir units) so that vineyard interventions can be precisely
targeted to where they are needed. But you don’t have to look too
far below the surface to see that there are subtle but important
differences between old world and new world notions of terroir.
Speaking generally, in the old world terroirists aim to make wines
that express the typicity of the specific vineyard site, whereas in
the more pragmatic new world, understanding terroir is seen as a route
to improved quality.
A
taste of the soil?
The notion of terroir is fundamental to the wine industries of
old world countries such as France, Italy and Germany. It’s a
philosophical framework within which wine growers work. Local wine
laws are built around the concepts of appellations, which lend
official sanction to the idea that a combination of certain vineyard
sites and grape varieties creates unique wines that faithfully express
their geographical origins.
Correspondingly, many old world growers
feel they have a duty to make wines faithful to the vineyard sites
they are working with. These growers will commonly make associations
between properties of the wines and the soil types the grapes are
grown on. In some cases these putative associations are quite
specific: people will talk about mineral characters in wines and
associate them with the minerals in the vineyard, taken up by the
roots of the vines.
There’s even a French expression, goût de
terroir, that is used to describe this. Do chalk, flint or slate
soils impart chalky, flinty or slate-like characters to wine? As a
scientist who has a working knowledge of plant physiology, I find this
notion, which I call the ‘literalist’ theory of terroir,
implausible. Yet I can’t get away from the fact that an overwhelming
majority of the world’s most compelling and complex wines are made
by people who hold the notion of terroir as being critical to wine
quality.
Thus the goal of this feature is to explore the mechanisms of
terroir, focusing specifically on soils. Just how do soils affect wine
quality? Is it a direct or indirect relationship? What are the
scientific explanations for terroir effects?
Randall’s
Rocks
In fact, the inspiration for this article came from a
characteristically wacky experiment conducted by Randall Grahm, of
California’s Bonny Doon. Even though he’s from California, Grahm
is actually one of the most eloquent proponents of terroir, and he had
the unusual idea of bypassing the vine and adding rocks directly to
wine, to investigate their influence on flavour.
‘Our experiments were incredibly
simplistic and gross in comparison to the very subtle chemistry that
occurs in mineral extraction in real soils,’ explains Grahm. ‘We
simply took interesting rocks, washed them very well, smashed them up
and immersed them in a barrel of wine for a certain period of time,
until we felt that the wine had extracted some interesting flavours
and we were able to discern significant differences between the
various types.’
Surely, this is taking the literalist notion of
terroir – that flavour compounds are translocated from the soil to
the developing grapes through the vine roots – to its extreme. Grahm
continues, ‘We initially screened a number of different rocks with
bench trials and ultimate decided on a few for larger scale
experimentation - rip rap (granite), Noyo cobble stone, black slate
and Pami pebbles. We certainly took the extraction way too far
as we ended up seeing pH rises of 0.5–0.7 units, i.e. from 3.5 to
4.1 or 4.2, which is clearly beyond the pale for most wines.
Obviously the big pH shift and the lowering of the acidity caused
major changes in the texture and mouthfeel of the wine, but we also
observed dramatic differences in aromatics, length and persistence of
flavour.’
Grahm is convinced of the importance of mineral flavours
in wine. ‘In every case, low doses of minerals (before we really
overdid it), added far more complexity and greater persistence on the
palate.’ His view is that minerality in wines has important
implications for wine quality. ‘It is my personal belief that wines
that are richer in minerals just present way differently. I
believe that in general mineral-rich wines there is a suppression of
obvious fruit. What is most striking to me though about wines
that have higher levels of minerals is that they seem to have a
certain sort of nucleus or density around their centre, they are
gathered, focused, cohered the way a laser coheres light. It is a
different kind of density relative to tannic density, somehow deeper
in the wine than the tannins. In any event, I am utterly
convinced that minerality is the one true key to ageability in wines
and that everything else—tannin, acidity, sulphur dioxide—plays a
far more secondary role.’
It
is unlikely that adding rocks to wines will ever become a common
winemaking manipulation, though. Grahm’s rock-infused wines ran into
some trouble with the regulatory body in California who were finding
elevated levels of nickel and antimony, among other things, so it
looks like this experiment won’t be repeated.
Scientific views of terroir
While in some circles it is
quite common to hear such literalist explanations of terroir, they are
treated with a degree of incredulity by many new world
viticulturalists. I asked viticultural guru Dr Richard Smart what he
thought of popular notions of terroir which propose direct
translocation of flavour molecules from the soil to the grapes, and
hence the wine. ‘This is an absolute nonsense’, he replied. ‘I
have never heard this, yet you say it is popular. Who on earth
postulated this?’
Dawid Saayman, a South African viticultural expert
known for his work on terroir, adds that, ‘I don’t believe that
the minerals taken up by the vine can register as minerality in the
wines. Minerality appears to me to be more the result of absence of
fruitiness.’ But it’s pretty much a given that wines that made
from grapes differing only in the soil in which they were grown taste
different.
So just what is the scientific explanation for these
terroir effects? It is an important question, because providing a
sound scientific footing for terroir is a worthy cause. Not only will
it lend credibility to the concept in the eyes of sceptics, but it
will also help the already converted understand and therefore better
utlilize terroir effects.
If we are going to frame terroir
in scientific language, then we’ll need to start with some plant
physiology. The miracle of the plant kingdom is that these complex
organisms build themselves from virtually nothing: all a plant needs
to grow is some water, sunlight, air and a mix of trace elements and
nutrients. All the complex structure and chemistry of an oak tree, a
daffodil or a grapevine is fashioned from these very basic starting
ingredients. What do vine roots take up from the soil? Primarily
water, along with dissolved mineral ions.
It seems implausible that
such a complex structure as a vine is created from virtually nothing
by photosynthesis – the capture of light by specialized organelles
called chloroplasts, which turn light energy into chemical energy that
the plant can use—but that’s the way it is. As Richard Smart
emphasizes, ‘All flavour compounds are synthesized in the vine, made
from organic molecules derived from photosynthesis ultimately, and
inorganic ions taken up from the soil.’
Professor Jean-Claude
Davidian of the Ecole Nationale Supérieure Agronomique in
Montpellier, echoes these sentiments. ‘Nobody has been objectively
able to show any links between the soil mineral composition and the
flavour or fragrance of the wines’, he says. Davidian adds that
‘those who claim to have shown these links are not scientifically
reliable’.
on
to part two...
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