Soil and Wine

Author(s):  
Robert E. White

The concept of terroir as a complex interaction among soil, climate, biology, and human intervention is introduced in section 1.1. The belief that the soil in a par­ticular vineyard imparts a distinctive character to the resulting wine is strong in Europe, but less so in the New World. The special character or personality of a wine may be confined to just one small block, less than 0.5 ha, for example, the “core block” within L’Enclos of Château Latour in the Bordeaux region (Borde­lais) of France. Alternatively, a special character may be attributed more widely to wines from an appellation (the commune Pauillac) or to a subregion such as the Haut-Médoc. But soil is very variable in the landscape (chapter 1), so that as the vineyard area increases, the character of a wine is less and less likely to show a dis­tinctive and defining influence of the soil. Soil variation, in combination with a variation in the mesoclimate (section 1.3.2), will mask a clear, intense expression of the underlying terroir. The grape variety, cultural practices, and the wine maker will then dominate the wine character. Thus, the true influence of terroir can only be satisfactorily studied for small areas. As pointed out in section 8.2.1, soil information is typically collected at a low sampling density over large areas to produce general-purpose soil classifica­tions. The resulting soil maps are necessarily of a small scale (e.g., 1:1,000,000), which means the information about small areas (1–10 ha) is unlikely to be very accurate (see box 8.1). Hence, intensive soil surveys, with at least 6 soil pits per ha, are necessary to study the soil factor in terroir when soil variation can be mapped at a large scale (1:5,000). Further, with more widespread use of precision viticulture technology, as discussed in section 5.3.5, the variation in specific soil properties (e.g., depth to an impeding B horizon and soil strength) can be mea­sured at intervals of about 2 m and mapped at a very large scale (>1:1,000). At a small scale (representing a large area), we can make generalizations, such as that soils on limestone or chalk in Burgundy, Champagne, and the Loire Val­ley in France are highly regarded for producing distinctive wines.

2018 ◽  
Vol 12 (3) ◽  
pp. 297-307 ◽  
Author(s):  
Takashi Tanizaki ◽  
Hideki Katagiri ◽  
António Oliveira Nzinga René ◽  
◽  

This paper proposes scheduling algorithms using metaheuristics for production processes in which cranes can interfere with each other. There are many production processes that involve cranes in manufacturing industry, such as in the steel industry, so a general purpose algorithm for this problem can be of practical use. The scheduling problem for this process is very complicated and difficult to solve because the cranes must avoid interfering with each other plus each machine has its own operational constraints. Although several algorithms have been proposed for a specific problem or small-scale problem, general purpose algorithms that can be solved in real time (about 30 minutes or less) in the company’s production planning work have not been developed for large-scale problems. This paper develops some metaheuristic algorithms to obtain suboptimal solutions in a short time, and it confirms their effectiveness through computer experiments.


2016 ◽  
Vol 4 (2) ◽  
pp. 132-148 ◽  
Author(s):  
Francis P. McManamon ◽  
John Doershuk ◽  
William D. Lipe ◽  
Tom McCulloch ◽  
Christopher Polglase ◽  
...  

AbstractPublic agencies at all levels of government and other organizations that manage archaeological resources often face the problem of many undertakings that collectively impact large numbers of individually significant archaeological resources. Such situations arise when an agency is managing a large area, such as a national forest, land management district, park unit, wildlife refuge, or military installation. These situations also may arise in regard to large-scale development projects, such as energy developments, highways, reservoirs, transmission lines, and other major infrastructure projects that cover substantial areas. Over time, the accumulation of impacts from small-scale projects to individual archaeological resources may degrade landscape or regional-scale cultural phenomena. Typically, these impacts are mitigated at the site level without regard to how the impacts to individual resources affect the broader population of resources. Actions to mitigate impacts rarely are designed to do more than avoid resources or ensure some level of data recovery at single sites. Such mitigation activities are incapable of addressing research question at a landscape or regional scale.


1981 ◽  
Vol 61 (4) ◽  
pp. 535-551 ◽  
Author(s):  
K. W. G. VALENTINE

It is becoming common for soil surveys to be made of the same area at different intensities and published at different scales. The principles of cartographic generalization are discussed that control the relationships between the map units and delineations on maps made from such surveys. A study of two sets of maps showed that almost no lines were coincident. Up to 20% of the small scale delinations could be ’inliers’ of different soils and about 15% of the large scale delineations would be outside their small scale equivalents. The same discrepancies are to be expected between large scale soil maps and the smaller scale maps of physiography or vegetation that are often used to stratify soils. Reasons for these discrepancies are discussed under the headings of simplification and classification. Recommendations arc made to guide the preparation of maps and legends for different intensities and scales of survey in the same area. These recommendations have practical implications for the planning of surveys and the designs of computer-based autocartography systems.


1987 ◽  
Vol 16 (2) ◽  
pp. 54-58 ◽  
Author(s):  
M. K. V. Carr

In Africa, Swaziland is atypical in being a small country. Nevertheless, it is agriculturally and climatically diverse and its problems are relevant to other sub Saharan countries. This article reviews large-scale irrigation schemes in the context of such factors as traditional land tenure, soil variation, crop management techniques, and availability of technical support. A later article will discuss problems of small-scale irrigation.


2009 ◽  
Vol 630 ◽  
pp. 299-329 ◽  
Author(s):  
CHLOÉ MICHAUT ◽  
DAVID BERCOVICI

Two-phase viscous gravity current theory has numerous applications in the natural sciences, from small-scale lava, sedimentary and glacial flows, to large-scale flows of partially molten mantle. We develop the general equations for two-phase viscous gravity currents composed of a high viscosity matrix and low viscosity fluid for both constant volume and constant flux conditions. A loss of fluid phase is taken into account at the current's upper boundary and corresponds to the degassing of a lava flow or loss of water in sedimentary flows. As the current spreads, its surface increases and fluid loss is facilitated, which modifies the mixture density and viscosity and thus the current's shape; hence spreading of the flow affects fluid loss and vice-versa. Our results show that two-phase gravity currents retain and transport the fluid out to large distances, but the fluid is almost entirely lost within a region of finite radius. This ‘loss radius’ depends on the flow's volume or flux, fluid and matrix properties as well as on the size of fluid parcels or matrix permeability. Application to lava flows shows that degassing occurs over a large area, which affects gas release and transport in the atmosphere.


2013 ◽  
pp. 3-31 ◽  
Author(s):  
A. V. Belov ◽  
L. P. Sokolova

This paper presents the stages of cartographic study into vegetation of Baikalian Siberia (the southern part of East Siberia). It highlights the ways toward shaping the principles and methods of the Irkutsk (Siberian) school of mapping vegetation as a component of geosystems, the founder of which was Academician V.B.Sochava. The initial stage in studying vegetation of Baikalian Siberia involved cartographic support of the resolution of ecological problems within national programs of integral development and exploitation of natural resources in the country’s eastern regions. The current stage of cartographic study into vegetation of Baikalian Siberia is determined by changes in the nature management paradigm in circumstances where the market economy is being shaped. This stage is characterized by the transition from general purpose-regional small-scale universal mapping to generation of medium- and large-scale assessment-forecast maps of vegetation for ecological accompaniment of a variety of economic measures, such as development of oil and gas fields in the Prebaikalia, an enhancement and promotion of recreation at Baikal, etc. Presented is the algorithm of geobotanical forecasting as a multistage process of conjugate mapping of vegetation. Using the key areas on the Angara-Lena interfluve and in Northern Priolkhonie as an example, different aspects of anthropogenic and natural stability of vegetation are considered from the perspective of geobotanical forecasting. The economic value of vegetation is determined according to its ecologo-protective and resource potentials. Recommendations are made for nature management optimization on a forecasting-geobotanical basis.


1994 ◽  
Vol 3 (4) ◽  
pp. 288-308 ◽  
Author(s):  
David N. Snowdon ◽  
Adrian J. West

VR is already evolving away from single user small-scale demonstrators, and inexorably toward sophisticated environments in which many geographically distributed users can perform a diverse range of activities. There will therefore be a pressure to make such environments increasingly general purpose and dynamic in their support of applications, paralleling perhaps the historical evolution of conventional operating systems. It is from speculations about the nature of such a future large-scale VR system that the AVIARY project has developed. AVIARY provides multiple worlds, each with its own set of laws, that may be tailored to suit particular application domains. The overall structure enables a coherent relationship between worlds to be maintained, which is important both for purposes of code reuse, and to aid users in navigating the system. A prototype implementation exists that addresses underlying implementation issues in the AVIARY model, and, in particular, distribution across heterogeneous processor networks, dynamic management of objects and message types within the system, the separation of graphics processing, and the management of spatial extent. Implementations of the prototype have been tested on a Transputer array, and a heterogeneous network of Sun and Silicon Graphics workstations. The system is currently being ported to a 2.4-Gflop KSR-1 parallel supercomputer. This paper reviews approaches to distributed, multi-application VR systems, presents pertinent elements of the AVIARY design, and describes the prototype implementation with particular attention given to the issues of distribution.


2018 ◽  
Vol 620 ◽  
pp. A6 ◽  
Author(s):  
O. Melnyk ◽  
A. Elyiv ◽  
V. Smolčić ◽  
M. Plionis ◽  
E. Koulouridis ◽  
...  

Context. This work is part of a series of studies focusing on the environment and the properties of the X-ray selected active galactic nuclei (AGN) population from the XXL survey. The present survey, given its large area, continuity, extensive multiwavelength coverage, and large-scale structure information, is ideal for this kind of study. Here, we focus on the XXL-South (XXL-S) field. Aims. Our main aim is to study the environment of the various types of X-ray selected AGN and investigate its possible role in AGN triggering and evolution. Methods. We studied the large-scale (>1 Mpc) environment up to redshift z = 1 using the nearest neighbour distance method to compare various pairs of AGN types. We also investigated the small-scale environment (<0.4 Mpc) by calculating the local overdensities of optical galaxies. In addition, we built a catalogue of AGN concentrations with two or more members using the hierarchical clustering method and we correlated them with the X-ray galaxy clusters detected in the XXL survey. Results. It is found that radio detected X-ray sources are more obscured than non-radio ones, though not all radio sources are obscured AGN. We did not find any significant differences in the large-scale clustering between luminous and faint X-ray AGN, or between obscured and unobscured ones, or between radio and non-radio sources. At local scales (<0.4 Mpc), AGN typically reside in overdense regions, compared to non-AGN; however, no differences were found between the various types of AGN. A majority of AGN concentrations with two or more members are found in the neighbourhood of X-ray galaxy clusters within <25–45 Mpc. Our results suggest that X-ray AGN are typically located in supercluster filaments, but they are also found in over- and underdense regions.


2019 ◽  
Vol 12 (3) ◽  
pp. 893-908 ◽  
Author(s):  
Veiko Lehsten ◽  
Michael Mischurow ◽  
Erik Lindström ◽  
Dörte Lehsten ◽  
Heike Lischke

Abstract. Dynamic global vegetation models are a common tool to assess the effect of climate and land use change on vegetation. Though most applications of dynamic global vegetation models use plant functional types, some also simulate species occurrences. While the current development aims to include more processes, e.g. the nitrogen cycle, the models still typically assume an ample seed supply allowing all species to establish once the climate conditions are suitable. Pollen studies have shown that a number of plant species lag behind in occupying climatological suitable areas (e.g. after a change in the climate) as they need to arrive at and establish in the newly suitable areas. Previous attempts to implement migration in dynamic vegetation models have allowed for the simulation of either only small areas or have been implemented as a post-process, not allowing for feedbacks within the vegetation. Here we present two novel methods simulating migrating and interacting tree species which have the potential to be used for simulations of large areas. Both distribute seeds between grid cells, leading to individual establishment. The first method uses an approach based on fast Fourier transforms, while in the second approach we iteratively shift the seed production matrix and disperse seeds with a given probability. While the former method is computationally faster, it does not allow for modification of the seed dispersal kernel parameters with respect to terrain features, which the latter method allows. We evaluate the increase in computational demand of both methods. Since dispersal acts at a scale no larger than 1 km, all dispersal simulations need to be performed at maximum at that scale. However, with the currently available computational power it is not feasible to simulate the local vegetation dynamics of a large area at that scale. We present an option to decrease the required computational costs through a reduction in the number of grid cells for which the local dynamics are simulated only along migration transects. Evaluation of species patterns and migration speeds shows that simulating along transects reduces migration speed, and both methods applied on the transects produce reasonable results. Furthermore, using the migration transects, both methods are sufficiently computationally efficient to allow for large-scale DGVM simulations with migration.


2020 ◽  
Vol 633 ◽  
pp. A142 ◽  
Author(s):  
Q. M. Zhang ◽  
R. S. Zheng

Aims. In this paper, we report multiwavelength observations of remote coronal dimmings related to an M1.1 circular-ribbon flare in active region (AR) 12434. Methods. The confined flare without a coronal mass ejection was observed by the Atmospheric Imaging Assembly (AIA) and the Helioseismic and Magnetic Imager on board the Solar Dynamics Observatory on 2015 October 16. We obtained global three-dimensional (3D) magnetic fields before the flare using the potential field source surface modeling. Results. A few minutes before the flare hard X-ray peak time (06:13:48 UT), small-scale, weak dimming appeared ∼240″ away from the flare site, which can be observed by AIA only in 131 and 171 Å. Afterward, long and narrow dimmings became evident in all AIA extreme-ultraviolet passbands except 304 Å, while localized core dimming was not clearly observed near the flare site. The large-area dimmings extended southeastward and the areas increased gradually. The total area of dimmings reaches (1.2 ± 0.4) × 104 Mm2 in 193 Å. The maximal relative intensity decreases in 171 and 193 Å reach 90% and 80%, respectively. Subsequently, the dimmings began to replenish and the area decreased slowly, lasting for ≥3 h. The remote dimmings and AR 12434 are connected by large-scale coronal loops. The remote dimmings are associated with the southwest footpoints of coronal loops with weak negative polarities. Possible origins of remote dimmings are discussed.


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