Terroir 2020 banner
IVES 9 IVES Conference Series 9 Effect of two contrasting soils on grape and wine sensory characteristics in Shiraz

Effect of two contrasting soils on grape and wine sensory characteristics in Shiraz

Abstract

Aims: Berry composition and wine sensory characteristics reflect the origin of grape production and seasonal climatic conditions. The aim of this study was to compare berry and wine sensory characteristics from two contrasting soil types where the vineyard climate, geography, topography, vine and management factors were not different.

Methods and Results: Two adjoining blocks of Shiraz with similar vine age (+/-1 year), identical clone (1654), row orientation (NW, SE) and cordon height were selected for this study. All irrigation, spray and midrow management treatments were identical. Both sites have soils that are texture contrast or duplex brown chromosols. The main distinguishing feature between the two sites being the presence of 10% to 50% ironstone gravel, mainly in the bleached topsoil “E” (or A2) horizon for the “Ironstone” block which is in contrast to the “Sand over clay” block. 

Berry sensory attributes were evaluated using the accepted method of berry sensory assessment (BSA). The method allows for the identification and quantification of berry sensory attributes against standard sensory references by a trained panel. The evaluation of wine sensory attributes was performed using a quantitative descriptive analysis (QDA). Both methods were performed to assess sensory differences in grapes and wine from the two soil types. Berries from the “Ironstone” soil had more intense green/grassy flavour, a higher perception of acidity and greater astringency. This was in contrast to berry samples from the sand over clay soil, which were described as having more intense dried fruit/jammy flavour, a higher perceived sweetness and an elevated toasted flavour. Wines made from fruit from the “Ironstone” soil were found to have more intense red fruit characters, tannin quality and astringency in contrast to the dark fruit, higher colour intensity and confectionary characteristics of the wines made from fruit from “Sand over clay” soils.  Fifty-six soil mineral elements were analysed from each soil horizon, leaf blades, must and wine samples. Results obtained from inductively couple plasma atomic emission spectroscopy (ICP-OES) analysis identified elements some of which were unique to each soil type and some which were in higher concentrations. The differences in the two soils elemental status was translated to leaves, berries and wine from those soils. 

Conclusions: 

Differences were observed in berry and wine sensory characteristics when comparing the fruit harvested from two contrasting soils in close proximity. Soils displayed very similar physical characteristics. Both soils were observed to be texture contrast or duplex brown chromosols. They shared common features of sandy or loamy topsoils (“A” horizons) over brown light clay (LC) to light medium (LMC) “B” horizons with or without highly weathered sandstone in the subsoil or “C” horizon. There was no soil carbonate present at any site and topsoil pH was neutral (pH 6.5-7.5) and decreased slightly to 6.0 in the “B” and “C” horizons.  Root zones, both predicted and observed were not significantly different.

Slight differences were observed between the soils with measures of readily available water (RAW), topsoil depth and a unique layer of gravel in the ironstone soil all of which have been associated in previous research with water movement and plant water availability in soils. Analysis of the chemical composition and concentration of soils, vines, grapes, musts and wines demonstrated distinct differences in the chemical characteristics between the two soil sites. This study was able to investigate soils with different soil chemistries and sensory characteristics for berries and wine in isolation from other known influences including viticultural, environmental, many other soil, and winemaking factors. 

The application of elements to vines in a controlled environment in future work may provide a link between soil chemistry and grape and wine sensory attributes. 

Significance and Impact of the Study: Soil elemental composition is a contentious aspect of terroir especially in relation to the relative importance afforded to climate and soil physical characteristics in previous research. This trial was able to isolate soil for analysis to observe unique elemental compositions in varying concentrations in relation to differences in berry and wine sensory outcomes. The mechanisms by which soil elements might influence sensory outcomes of wines is not widely understood and future research could lead to soils and wines being paired for desired sensory outcomes.

DOI:

Publication date: March 17, 2021

Issue: Terroir 2020

Type: Video

Authors

Anthony Hoare*, Michael McLaughlin, Cassandra Collins

School of Agriculture, Food and Wine, Waite Research Institute, University of Adelaide, Urrbrae, SA, Australia

Contact the author

Keywords

Elemental composition, fruit quality, wine quality, soil chemistry

Tags

IVES Conference Series | Terroir 2020

Citation

Related articles…

Local adaptation tools to ensure the viticultural sustainability in a changing climate

[lwp_divi_breadcrumbs home_text="IVES" use_before_icon="on" before_icon="||divi||400" module_id="publication-ariane" _builder_version="4.19.4" _module_preset="default" module_text_align="center" module_font_size="16px" text_orientation="center"...

austrianvineyards.com: online viewer of all designations of Austrian wine

To digitally record and present all the origins of Austrian wines in the same perfect and clear way was the motivation for the Austrian Wine Marketing Board (Austrian Wine) to start with the project in 2018. In June 2021 the results were presented to the public in an online viewer showing all the designations of Austrian wine, available at https://austrianvineyards.com in a largely barrier-free manner. The online viewer provides tailored individual maps fitted to the respective zoom level. The smallest unit of wine-origins in Austria is called Ried and is displayed in a plot-specific manner highlighting areas under vine. Information on the Ried include administrative district, winegrowing municipality, cadastral municipality, large collective vineyard site, specific winegrowing region, generic winegrowing region, winegrowing area and, in many cases, an illustrative picture. Complementary data on the size, elevation (minimum-maximum), orientation (in 8 sectors plus flat) and gradient (minimum, maximum, average) are based on the area under vine according to the EU’s Integrated Administration and Control System. Additional information covers climate data. The diagrams are taken from the monthly breakdown of data in the annals of the Central Institute for Meteorology and Geodynamics, Austria provide a display of values for air temperature, precipitation, and sunshine hours for the reference year and the long-term average. Seasonal aggregated data on temperature, precipitation, and sunshine hours complete the display. Short descriptions with emphasis on geology and soil, field name in historical maps, etymology of the denomination, and main planted variety complements the available information for the main designations in the online viewer. These descriptions are compiled by winegrowers, geologists, historians, and journalists. All the information and data can be extracted to a pdf-file. Printed vineyard maps are also available. Missing content regarding wine origins in Styria will be completed in winter 2021/22.

Influence of agronomic practices in soil water content in mid-mountain vineyards

In the context of LIFE project MIDMACC (LIFE18 CCA/ES/001099), several pilots have been installed in vineyards in mid mountain areas of Catalonia (NE Spain) to test well stablished agronomic practices to increase the adaptation of Mediterranean mid mountain to climate change. Soil water content (SWC) at three different depths (15, 30 and 45cm) was measured in continuum from August 2020. One pilot (WC) included a well-established green cover (GC), a new GC (NC) and a conventional soil management (CM, tilling+herbicides). NC presented an intermediate state between WC and CM, responding similarly to CM in autumn but quickly reaching similar SWC to WC, then following the same evolution till next spring, with CM presenting lower values along autumn and winter. Then vegetation activation decreased SWC in all plots, (much slower in CM, lacking GC). Sensibility to spring rains is again intermediate for NC, which joins SWC evolution of CM by the end of spring till next autumn. It is expected that NC will resemble WC more and more as its GC develops. In the pilot combining vine training (VSP vs Gobelet) and hillside management (slope vs terrace), no clear pattern could be related with these conditions. However, both terraces seem to be more sensitive to spring rains. A third pilot included new vineyards (7 and 1 year old). In the new vineyard (N), higher canopy development, a spontaneous green cover and row straw resulted in a slower SWC dynamic, not so sensitive to rains but conserving more soil water in spring and most of summer, even with presumably a higher water extraction by vines. In the newest vineyard (VN) the deepest sensor is still sensitive to rain events all over the year and SWC is always highest at this depth, revealing small water capture by vines.

The use of rootstock as a lever in the face of climate change and dieback of vineyard

As viticulture faces challenges such as climate change or vineyard dieback, the choice of the variety and rootstock becomes more and more crucial. To study rootstock levers in the Bordeaux region, a parcel of Cabernet Sauvignon (CS) was planted with four rootstocks in 2014. Twenty repetitions of each of the following four rootstocks were set up: 101-14 MGt, Nemadex AB, 420A MGt and Gravesac. The number of bunches, yields and pruning weights of the vine shoots were measured individually on 240 vines from 2017 to 2021. Since 2020, nitrogen status assessed by assimilable nitrogen level, hydric status assessed by δ13C and berry maturity were measured on 80 samples taken from 20 repetitions of the four rootstocks. A lower yield was measured for CS grafted onto Nemadex AB due to the lower number of bunches and the lower weight of berries. The differences between the other three rootstocks are small, but CS grafted onto 420A MGt was the most productive. The CS grafted onto Nemadex AB had the lowest pruning weight while 101-14 MGt had the highest. In 2020, δ13C showed a more moderate water stress with 101-14 MGt and 420A MGt than with Nemadex AB. Surprisingly, the Gravesac was under more stress than the 101-14 MGt. The nitrogen status in the berries was better for Nemadex AB but this was perhaps due to the significantly lower weight of the berries.Rootstock 101-14 MGt attained the highest accumulation of sugars in the berries while 420A MGt allows to preserve higher acidity. The parcel is still young which may explain some of the results. These measures must therefore be continued over the next several years to fully assess the effects of these rootstocks on the development of the vines and the quality of the production under new climatic conditions.

Grapevine yield estimation in a context of climate change: the GraY model

Grapevine yield is a key indicator to assess the impacts of climate change and the relevance of adaptation strategies in a vineyard landscape. At this scale, a yield model should use a number of parameters and input data in relation to the information available and be able to reproduce vineyard management decisions (e.g. soil and canopy management, irrigation). In this study, we used data from six experimental sites in Southern France (cv. Syrah) to calibrate a model of grapevine yield limited by water constraint (GraY). Each yield component (bud fertility, number of berries per bunch, berry weight) was calculated as a function of the soil water availability simulated by the WaLIS water balance model at critical phenological phases. The model was then evaluated in 10 grapegrowers’ plots, covering a diversity of biophysical and technical contexts (soil type, canopy size, irrigation, cover crop). We identified three critical periods for yield formation: after flowering on the previous year for the number of bunches and berries, around pre-veraison and post-veraison of the same year for mean berry weight. Yields were simulated with a model efficiency (EF) of 0.62 (NRMSE = 0.28). Bud fertility and number of berries per bunch were more accurately simulated (EF = 0.90 and 0.77, NRMSE = 0.06 and 0.10, respectively) than berry weight (EF = -0.31, NRMSE = 0.17). Model efficiency on the on-farm plots reached 0.71 (NRMSE = 0.37) simulating yields from 1 to 8 kg/plant. The GraY model is an original model estimating grapevine yield evolution on the basis of water availability under future climatic conditions.  It allows to evaluate the effects of various adaptation levers such as planting density, cover crop management, fruit/leaf ratio, shading and irrigation, in various production contexts.