Inductively mapping expert-derived soil-landscape units within dambo wetland catenae using multispectral and topographic data

Geoderma ◽  
2009 ◽  
Vol 150 (1-2) ◽  
pp. 72-84 ◽  
Author(s):  
Matthew K. Hansen ◽  
David J. Brown ◽  
Philip E. Dennison ◽  
Scott A. Graves ◽  
Ross S. Bricklemyer
Author(s):  
M. Grodzynskyi

Series (succession sequences) of soils that change each other over time and within the landscape units are proper objects for landscape mapping. The soil series give an idea of both retrospective state of a soil before its anthropogenic transformations and of tendencies of soil development in landscape complexes of various types. The names of soils as they are appeared in soil nomenclature of Soil science should not be duplicated in the legends of landscape maps. "Landscape" names for soils have to stress on their features and attributes that are of primary importance for vegetation, water, thermal and other ecological regimes of landscapes. The "landscape" names for different types of Albeluvisols and Phaeozems of Ukraine are suggested. Key words: soil, landscape, landscape map, landscape science.


Soil Research ◽  
2005 ◽  
Vol 43 (2) ◽  
pp. 127 ◽  
Author(s):  
Jochen Schmidt ◽  
Phil Tonkin ◽  
Allan Hewitt

Limited resources and large areas of steeplands with limited field access forced soil and land resource surveyors in New Zealand often to develop generalised models of soil–landscape relationships and to use these to produce soil maps by manual interpretation of aerial photographs and field survey. This method is subjective and non-reproducible. Recent studies showed the utility of digital information and analysis to complement manual soil survey. The study presents quantitative soil–landscape models for the Hurunui and Haldon soil sets (New Zealand), developed from conceptual soil–landscape models. Spatial modelling techniques, including terrain analysis and fuzzy classification, are applied to compute membership maps of landform components for the study areas. The membership maps can be used to derive a ‘hard’ classification of land components and uncertainty maps. A soil taxonomic model is developed based on field data (soil profiles), which attaches dominant soil profiles and soil properties, including their uncertainties, to the defined land components. The method presented in this study is proposed as a potential technique for modelling land components of steepland areas in New Zealand, in which the spatial soil variation is dominantly controlled by landform properties. A soil map was developed that includes the uncertainty in the fundamental definitions of landscape units and the variability of soil properties within landscape units.


OENO One ◽  
1998 ◽  
Vol 32 (4) ◽  
pp. 169 ◽  
Author(s):  
Emmanuelle Vaudour ◽  
Michel-Claude Girard ◽  
L.-M. Bremond ◽  
L. Lurton

<p style="text-align: justify;">In order for the characterization of terroir in vineyard situations to benefit both viticultural and wine making practices, it is necessary to consider the spatial aspect of the vineyard environment. An exploratory approach at characterising terroir in the Nyons-Valreas Basin (figure 1) considers both the spatial analysis and frequency analysis of the harvest. Data gathered from stereoscopic aerial photographic examination, satellite image processing, land surveys, and the Digital Elevation Model are combined and structured within a Geographic Information System along with the existing soil and geological data (figure 2). The result is a comprehensive soils model applicable to a relatively large area (11,340 ha). The Nyons-Valreas Basin is a neogene and quaternary sedimentary basin, and the soils found there are described by 21 soil landscape units which integrate 15 variables (table I). The area examined is considered to be representative of the surrounding regional diversity. The variables used in characterising terroir include soil types, geomorphology, lithology, stratigraphy, vegetation, land form, and land use. The various viticultural terroirs are regarded as parts of agricultural land consistent with both soil landscapes and harvest/wine responses. Multivariate clustering of the soil landscape units indicates that there exists 7 distinct viticultural terroirs, essentially on the basis of geomorphology and soils (figures 3 and 4, table II). Four distinct terroirs were compared (figures 5 and 6) using data gathered from 14 sites over the course of 15 vintages (1982-1996). Grenache is the grape variety planted at each site, and the variables measured at harvest (pH, sugar content, titratable acidity, the weight of 200 berries, and the sugar/acidity ratio) appear to significantly discriminate the sites examined according to the terroir modeling performed (tables III, IV and V).</p>


2018 ◽  
Vol 49 (3) ◽  
pp. 174-182 ◽  
Author(s):  
Paolo Nasta ◽  
Benedetto Sica ◽  
Caterina Mazzitelli ◽  
Paola Di Fiore ◽  
Ugo Lazzaro ◽  
...  

In the last decades, a growing interest in fostering advanced interdisciplinary studies is leading to the establishment of observatories in pilot catchments for long-term monitoring of hydrological variables and fluxes. Nevertheless prior to sensor network installation, this investment necessitates preliminary surveys on key-variables such as near-surface soil moisture in order to prevent risks of erronously distributing sensors by missing sufficient spatial information for understanding hydrological processes within the landatmosphere interactions. The availability of maps describing areas with similar morphological, topographical, soil, and vegetation characteristics enable preliminary surveys to be organized for capturing spatio-temporal variability of soil moisture as best as possible. The soil-landscape classification can be considered as an interesting approach for grouping mapping units with similar hydrological behavior. Therefore, we assume the soil-landscape units as hydrotopes or hydrological similar units. Six transects were established along two hillsides of the Upper Alento River catchment (southern Italy) which is a proper candidate to become a Critical Zone Observatory. In this paper we use a soil-landscape map to infer spatial and temporal dynamics of soil moisture measured along these transects, whereas quantitative analyses were obtained by using multivariate techniques. The effectiveness of available information on soil-landscape mapping units is evaluated with respect to different observed patterns of soil moisture: wetter- and drier-than average observation points belong to agricultural and forested hillslopes, respectively. Soil texture and topographical controlling factors, especially clay content and slope gradient, are found to explain approximately 70% of the observed spatial variations in soil moisture along the forested hillslopes. The spatial structure explained by the environmental controlling factors decreases to 45% in the cases of the agricultural hillslopes mainly due to perturbations induced by grazing and tillage practices.


2014 ◽  
Vol 35 (24) ◽  
pp. 8272-8294
Author(s):  
Jerome S. Lugumira ◽  
David J. Brown ◽  
Philip E. Dennison ◽  
Mathew K. Hansen ◽  
Lee A. Vierling

1964 ◽  
Vol 15 (1) ◽  
pp. 50 ◽  
Author(s):  
FW Hely ◽  
J Brockwell

The distribution of naturalized annual species of Medicago (medics) was studied on the brown acid soils of the Macquarie region of New South Wales, an area approximately 80 miles by 40 miles in extent. Four soil-landscape units were defined and one of these units was subdivided geographically into three parts. Four medics were found: Medicago minima (L.) Bart. and Medicago laciniata (L.) Mill. were by far the dominant annual legumes, occurring in many places at high frequency; Medicago denticulata Willd. and Medicago praecox DC. occurred at few sites and only at low frequency. Marked differences with respect to frequencies of medics were found both between soil-landscape units and the geographical subdivisions. On each unit and subdivision the frequency of M. minima in quadrats was consistently higher than that of M. laciniata. Association between M. minima and M. laciniata in quadrats was variable, but tended to be positive where these two medics occurrcd at low frequency and negative where they occurred at high frequency.


Soil Research ◽  
1994 ◽  
Vol 32 (5) ◽  
pp. 908 ◽  
Author(s):  
GE Rinder ◽  
E Fritsch ◽  
RW Fitzpatrick

Procedures for detailed mapping of a large number of soil features in small landscape units displayed in either vertical cross section (i.e. soil toposequences) or horizontal plane (i.e. soil maps) are presented. Rom hand coloured drawings that display the soil-landscape features, an Apple Macintosh Computer, with Adobe Illustrator and Adobe Patterns and Textures programs, is used to produce high quality coloured maps ready for reproduction in any form (e.g. posters, publications, slides or overhead transparencies). The first step is to produce the detailed computer map with all soil features included. This detailed computer map is made up of the following three layers or bases: (i) a black linework and lettering base, (ii) a polygon base filled with black and white textures, and (iii) a polygon base filled with colours. The detailed computer map, saved as the master file, is very easily modified to generate more simplified and thematic maps by: (i) grouping soil features into larger soil components in order to display soil-landscapes in a more simplified form, (ii) deleting certain soil-landscape components in order to highlight specific soil features, and (iii) adding newly aquired information (e.g. chemical and hydrological data) to previous versions.


1999 ◽  
Vol 79 (3) ◽  
pp. 491-500 ◽  
Author(s):  
Thomas Curt

To investigate the productivity of two coniferous species in granitic uplands of the French Massif Central, relationships between soil–landscape units (= morphopedological units) and forest yield were examined. An alveola landscape model composed of seven main morphopedological units (MPU) characterizes these two granitic areas. In total, 460 forest stands were studied and joined to the MPU. Each type of MPU was correlated to the yield of Norway spruce and Douglas-fir, evaluated by the site index (dominant height of stand at a reference age). Results stress that MPU explain a large part of site index variations: 68.7% in Cevennes uplands and 50% in Limousin for Norway spruce, 42% in Limousin for Douglas-fir. The hierarchy of the productivity among MPU is comparable for both species and study areas. Highest site index values correspond to MPU with deep Brunisols in vales and bottom of alveolas, with a high soil water storage capacity but without waterlogging. Ridges and summits with coarse parent materials topped by shallow and nutrient-depleted soils experience the lowest site index values. The strong relationship between MPU and forest yield can be explained by a combination of ecological factors affecting forest yield: topoclimatic conditions, parent materials and soils. These results stress that inheritances from Tertiary, and from Quaternary periglacial environments still influence the present-day potentials of ecosystems. In conclusion, the advantages and drawbacks of morphopedological surveys for forest applications are discussed. Key words: Soil–landscape units, forest yield, Picea abies (L.) Karst., Pseudotsuga menziesii (Mirb) Franco


2008 ◽  
Vol 3 (1) ◽  
pp. 91-95
Author(s):  
Ruth Amanda Estupiñán

In the red list of threatened species of Pará State, in Brazil, the salamander Bolitoglossa paraensis was listed as vulnerable. Initially the species was considered a synonym with Bolitoglossa altamazonica, but was recently revalidated. This note discusses the validity of the specimens from the west of the Brazilian Amazon identified as B. paraensis. It is also discussed the categorization of the species as vulnerable, and the records of the species was mapped in the Endemism area Belém. In order to establish a Private Natural Reserve (RPPN), a herpetological survey was carried out in different landscape units of the Nova Amafrutas, in Benevides (Pará), and the records of B. paraensis were mapped in these landscape units. By comparing the abundances recorded by Crump (1971) and those results of the present study, suggested that this species is tolerant to antropic “capoeira” forest (old fallows) next to undisturbed forest. More molecular phylogeographic studies are needed in order to establish a stable the taxonomy status for B. paraensis, and also the definition of its real endemic status in the Center of Endemism of Belém.


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