eberg | R Documentation |
Ebergötzen is 10 by 10 km study area in the vicinity of the city of Göttingen in Central Germany. This area has been extensively surveyed over the years, mainly for the purposes of developing operational digital soil mapping techniques (Gehrt and Böhner, 2001), and has been used by the SAGA GIS development team to demonstrate various processing steps.
eberg
table contains 3670 observations (augers) of soil textures at five depths (0–10, 10–30, 30–50, 50–70, and 70–90), and field records of soil types according to the German soil classification system. eberg_grid
contains gridded maps at 100 m resolution that can be used as covariates for spatial prediction of soil variables. eberg_grid25
contains grids at finer resolution (25 m). eberg_zones
is a polygon map showing the distribution of parent material (Silt and sand, Sandy material, Clayey derivats, Clay and loess). eberg_contours
shows contour lines derived from the 25 m DEM of the area using 10 m equidistance.
data(eberg)
The eberg
data frame (irregular points) contains the following columns:
ID
universal identifier
soiltype
a vector containing factors; soil classes according to the German soil classification system: "A"
(Auenboden), "B"
(Braunerde), "D"
(Pelosol), "G"
(Gley), "Ha"
(Moor), "Hw"
(HMoor), "K"
(Kolluvisol), "L"
(Parabraunerde), "N"
(Ranker), "Q"
(Regosol), "R"
(Rendzina), "S"
(Pseudogley), "Z"
(Pararendzina)
TAXGRSC
a vector containing factors; full soil class names according to the German soil classification system (see soiltype
column)
X
a numeric vector; x-coordinate (m) in DHDN / Gauss-Krueger zone 3 (German coordinate system)
Y
a numeric vector; y-coordinate (m) in DHDN / Gauss-Krueger zone 3 (German coordinate system)
UHDICM_*
a numeric vector; upper horizon depth in cm per horizon
LHDICM_*
a numeric vector; lower horizon depth in cm per horizon
SNDMHT_*
a numeric vector; sand content estimated by hand per horizon (0-100 percent); see Ad-hoc-AG Boden (2005) for more details
SLTMHT_*
a numeric vector; silt content estimated by hand per horizon (0-100 percent)
CLYMHT_*
a numeric vector; clay content estimated by hand per horizon (0-100 percent)
The eberg_grid
data frame (regular grid at 100 m resolution) contains the following columns:
PRMGEO6
a vector containing factors, parent material classes from the geological map (mapping units)
DEMSRT6
a numeric vector; elevation values from the SRTM DEM
TWISRT6
a numeric vector; Topographic Wetness Index derived using the SAGA algorithm
TIRAST6
a numeric vector; Thermal Infrared (TIR) reflection values from the ASTER L1 image band 14 (2010-06-05T10:26:50Z) obtained via the NASA's GloVis browser
LNCCOR6
a vector containing factors; Corine Land Cover 2006 classes
x
a numeric vector; x-coordinate (m) in DHDN / Gauss-Krueger zone 3 (German coordinate system)
y
a numeric vector; y-coordinate (m) in DHDN / Gauss-Krueger zone 3 (German coordinate system)
The eberg_grid25
data frame (regular grid at 25 m resolution) contains the following columns:
DEMTOPx
a numeric vector; elevation values from the topographic map
HBTSOLx
a vector containing factors; main soil type according to the German soil classification system (see column "soiltype" above) estimated per crop field
TWITOPx
a numeric vector; Topographic Wetness Index derived using the SAGA algorithm
NVILANx
a numeric vector; NDVI image derived using the Landsat image from the Image 2000 project
x
a numeric vector; x-coordinate (m) in DHDN / Gauss-Krueger zone 3 (German coordinate system)
y
a numeric vector; y-coordinate (m) in DHDN / Gauss-Krueger zone 3 (German coordinate system)
Texture by hand method can be used to determine the content of soil earth fractions only to an accuracy of ±5–10% (Skaggs et al., 2001). A surveyor distinguishes to which of the 32 texture classes a soil samples belongs to, and then estimates the content of fractions; e.g. texture class St2
has 10% clay, 25% silt and 65% sand (Ad-hoc-AG Boden, 2005).
The Ebergötzen dataset is courtesy of Gehrt Ernst (Ernst.Gehrt@niedersachsen.de), the State Authority for Mining, Energy and Geology, Hannover, Germany and Olaf Conrad, University of Hamburg (conrad@geowiss.uni-hamburg.de). The original data set has been prepared for this exercise by Tomislav Hengl (tom.hengl@opengeohub.org).
Ad-hoc-AG Boden, (2005) Bodenkundliche Kartieranleitung. 5th Ed, Bundesanstalt für Geowissenschaften und Rohstoffe und Niedersaechsisches Landesamt für Bodenforshung, Hannover, p. 423.
Böhner, J., McCloy, K. R. and Strobl, J. (Eds), (2006) SAGA — Analysis and Modelling Applications. Göttinger Geographische Abhandlungen, Heft 115. Verlag Erich Goltze GmbH, Göttingen, 117 pp.
Gehrt, E., Böhner, J., (2001) Vom punkt zur flache — probleme des 'upscaling' in der bodenkartierung. In: Diskussionsforum Bodenwissenschaften: Vom Bohrstock zum Bildschirm. FH, Osnabrück, pp. 17-34.
Skaggs, T. H., Arya, L. M., Shouse, P. J., Mohanty, B. P., (2001) Estimating Particle-Size Distribution from Limited Soil Texture Data. Soil Science Society of America Journal 65 (4): 1038-1044. doi: 10.2136/sssaj2001.6541038x
data(eberg) data(eberg_grid) data(eberg_zones) data(eberg_contours) library(sp) coordinates(eberg) <- ~X+Y proj4string(eberg) <- CRS("+init=epsg:31467") gridded(eberg_grid) <- ~x+y proj4string(eberg_grid) <- CRS("+init=epsg:31467") # visualize the maps: data(SAGA_pal) l.sp <- list("sp.lines", eberg_contours, col="black") ## Not run: spplot(eberg_grid["DEMSRT6"], col.regions = SAGA_pal[[1]], sp.layout=l.sp) spplot(eberg_zones, sp.layout=list("sp.points", eberg, col="black", pch="+")) ## End(Not run)
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