Spatial variability of soil compaction over a vineyard region in relation with soils and cultivation operations

Lagacherie, Philippe; Coulouma, Guillaume; Ariagno, P.; Virat, P.; Boizard, Hubert; Richard, Guy

doi:10.1016/j.geoderma.2005.10.006

Cited by 52 publications

(48 citation statements)

References 16 publications

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“…To begin with, the soil profiles were described by the cropping profile method (Tavares Filho et al, 1999;Roger-Estrade et al, 2004;Lagacherie et al, 2006) to characterize the type and spatial organization of compact soil structures (morphologically homogeneous units, or MHUs, according to Neves et al (2003)). The analysis was performed in three trenches (1.0 x 1.0 x 1.5 m) in each of the three areas (F, NT and PD), at a randomly selected location, with a distance of 100 m between the trenches, which were arranged along the slope (one in the highest part, with least inclination; a second in the middle of the area, with average inclination; and a third in the lowest area, with greatest inclination).…”

Section: Methodsmentioning

confidence: 99%

Characterization of soil structure and porosity under long-term conventional tillage and no-tillage systems

Filho

Tessier

2009

Rev. Bras. Ciênc. Solo

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Different management systems tend to modify soil structure and porosity over the years. The aim of this study was to study modifications in the morphostructure and porosity of dystroferric Red Latosol (Oxisol) under conventional tillage and no-tillage over a 31-year period. The study began with the description of soil profiles based on the cropping profile method, to identify the most compact structures, define sample collection points for physical and chemical analysis, and determine the water retention curve. A forest soil profile was described and used as reference. The results showed that, under conventional tillage, the microaggregate structure of the Oxisol was fragmented between 0 and 0.20 m, and compact (bulk density = 1.52 Mg m -3 ) in the sub-surface layer between 0.20 and 0.50 m. Under no-tillage, the structure became compacted (bulk density = 1.40 Mg m -3 ) between 0 and 0.60 m, but contained fissures and biopores. The volume of the class with a pore diameter of ≥ ≥ ≥ ≥ ≥ 100 μ μ μ μ μm under no-tillage was limited, but practically non-existent in the conventional management system. On the other hand, the classes with a pore diameter of < 100 μ μ μ μ μm were not affected by the type of soil management system. Index terms: Latosol/Oxisol, soil management, cropping profile method, water retention curve.(

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Section: Methodsmentioning

confidence: 99%

Characterization of soil structure and porosity under long-term conventional tillage and no-tillage systems

Filho

Tessier

2009

Rev. Bras. Ciênc. Solo

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“…Soil conditions at the sites Sonberk and Gotberg are almost identical, nevertheless, this beneficial influence is shown only by variants So-A and So-C and maximally up to the depth 240 or 190 mm. But most likely, in all variants at the site Gotberk, there appeared the above-mentioned influence of frequency of travel or heavier vehicles (for chemical protection) similarly to what Lagacherie [1] states. For comparison of the influence of the cover treatment, there can be used the fact that the root zone of plant community affects the soil horizon mostly up to the depth 300-400 mm.…”

Section: Resultsmentioning

confidence: 88%

“…A suitable solution is the use of grassland systems made of diverse species of plant mixtures [1], which are the main tools in maintaining the soil fertility and partially a tool of quality management in viniculture [2][3][4].…”

Section: Introductionmentioning

confidence: 99%

Evaluation of effect of vegetation cover on soil compaction

Burg¹,

Mašán²,

Zemánek³

2017

Engineering for Rural Development

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Abstract. In terms of ensuring the sustainability and permanent soil fertility, the key role in viticulture is played by short-term and permanent greening in the interrow. Additionally, the introduction of these systems can positively affect flora and fauna species diversity in monoculture plantations, like vineyards, which are an integral part of the contemporary cultural landscape. This paper focuses on the evaluation of penetrometric measurements carried out in the years of 2015 and 2016 at 5 sites with different soil conditions and different greening (a mixture of annual greening, a mixture of durable greening, a mixture of durable greening with various plants species, a mixture of durable greening for arid conditions and a mixture of annual greening for pollinators) in the region of South Moravia. Penetrometer measurements were conducted using a manual penetrometer EIJKELKAMP. The water content in the soil at the time of the measurement, expressed in weight percentage was determined by the gravimetric method. Soil samples for moisture determination were collected in triplicate from the depths of 0-0.

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“…Depletion of soil fertility in general, along with the concomitant problems of weeds, pests and diseases, is the fundamental root cause of low agricultural production on a global level (Tan et al, 2005). Even if grapevines are not demanding with regard to nutrients, they nevertheless require an adequate supply, which may no longer exist in terroirs where the soils are undergoing degradation processes, especially soil losses (Le Bissonnais et al, 2007;Martínez-Casasnovas et al, 2009Paroissien et al, 2010;Novara et al, 2011;Quiquerez et al, 2014;Chevigny et al, 2014;Lieskovsky and Kenderessy, 2014), nutrient depletion (Ramos and Martínez-Casanovas, 2006), compaction (Lagacherie et al, 2006), salinization and sodization (Clark et al, 2002;Crescimanno and Garofalo, 2006; al., 2007; Costantini and Lorenzetti, 2013), pesticide runoff and deposition (Landry et al, 2005;Louchart and Voltz, 2007;Lacas et al, 2012;Daouk et al, 2013;Lefrancq et al, 2013) and copper contamination (Pieztrak and McPhail, 2004;Chopin et al, 2008;Komárek et al, 2008;Wightwick et al, 2008;Mirlean et al, 2007Mirlean et al, , 2009Rusjan et al, 2007;El Hadri et al, 2012;Fernández-Calviño et al, 2013;El Azzi et al, 2013;Lai et al, 2013). In Burgundy, using vine-stock unearthing-burying measurements (Brenot et al, 2008), Chevigny et al (2014) estimated that the erosion rate had increased significantly over the last decade and also that the spatial distribution of erosion had changed and was now basically controlled by ...…”

Section: Outlook: Terroir Sustainability Assessment and The Design Ofmentioning

confidence: 99%

An overview of the recent approaches to terroir functional modelling, footprinting and zoning

Vaudour

Costantini²,

Jones

et al. 2015

SOIL

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Abstract. Notions of terroir and their conceptualization through agro-environmental sciences have become popular in many parts of world. Originally developed for wine, terroir now encompasses many other crops including fruits, vegetables, cheese, olive oil, coffee, cacao and other crops, linking the uniqueness and quality of both beverages and foods to the environment where they are produced, giving the consumer a sense of place. Climate, geology, geomorphology and soil are the main environmental factors which make up the terroir effect on different scales. Often considered immutable culturally, the natural components of terroir are actually a set of processes, which together create a delicate equilibrium and regulation of its effect on products in both space and time. Due to both a greater need to better understand regional-to-site variations in crop production and the growth in spatial analytic technologies, the study of terroir has shifted from a largely descriptive regional science to a more applied, technical research field. Furthermore, the explosion of spatial data availability and sensing technologies has made the within-field scale of study more valuable to the individual grower. The result has been greater adoption of these technologies but also issues associated with both the spatial and temporal scales required for practical applications, as well as the relevant approaches for data synthesis. Moreover, as soil microbial communities are known to be of vital importance for terrestrial processes by driving the major soil geochemical cycles and supporting healthy plant growth, an intensive investigation of the microbial organization and their function is also required. Our objective is to present an overview of existing data and modelling approaches for terroir functional modelling, footprinting and zoning on local and regional scales. This review will focus on two main areas of recent terroir research: (1) using new tools to unravel the biogeochemical cycles of both macro-and micronutrients, the biological and chemical signatures of terroirs (i.e. the metagenomic approach and regional fingerprinting); (2) terroir zoning on different scales: mapping terroirs and using remoteand proxy-sensing technologies to monitor soil quality and manage the crop system for better food quality.

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Spatial variability of soil compaction over a vineyard region in relation with soils and cultivation operations

Cited by 52 publications

References 16 publications

Characterization of soil structure and porosity under long-term conventional tillage and no-tillage systems

Characterization of soil structure and porosity under long-term conventional tillage and no-tillage systems

Evaluation of effect of vegetation cover on soil compaction

An overview of the recent approaches to terroir functional modelling, footprinting and zoning

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