The Danish Soil Classification From 1939 to 1975 the farmland area dropped from 32.000 sqkm to...
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![Page 1: The Danish Soil Classification From 1939 to 1975 the farmland area dropped from 32.000 sqkm to 28.000 sqkm It raised a need for soil maps for planning.](https://reader035.fdocuments.net/reader035/viewer/2022062619/55152bcd5503465e608b57bf/html5/thumbnails/1.jpg)
The Danish Soil Classification
• From 1939 to 1975 the farmland area dropped from 32.000 sqkm to 28.000 sqkm
• It raised a need for soil maps for planning and administration purposes at national and county level
• The Danish government decided to finance a national soil mapping
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The Danish Soil Classification
• 1975-1980: Soil mapping of the agriculture land mainly based on soil texture of the topsoil
• 1980-1985: Additional soil map on subsoil texture, landform and wetland and the establishment of a Danish pedological soil analytical database
• 1985-1990: Modelling and thematic maps
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Basic requirements
• The areas should be classified on the basis of permanent stable characteristics
• There should be a national standard code of reference that would make it possible to classify as uniform as possible
• The results should clearly illustrate the range of fertile and infertile soils
• The maps should be made in such a way that they might be used in future regional planning
• The mapping should be finished within 3 years (price app. 600.000 Euro)
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The soil map, scale 1:50.000
• Classified area• Texture of the plowlayer and subsoil (12 classes)• Slope (3 classes)• Subsoil geology (app. 50 classes)
• Not classified area• Urban zone• Forest• Coastal dune sands, small arable areas, lakes etc
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Organisation
• In December 1975 ADK was established to undertake the soil sampling, database handling and construction of the maps at scale 1:50.000.
• Crew: 3 AC and 1 technician + some students from the Universities.
• The soil sampling was done by local agronomists and the soil analyses were done at a research laboratory.
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Mapping slopes and surface geology
Slope classes Three slope classes delineated on topographic maps at
scale 1:25000 <6 degrees, 6-12 degrees and >12 degrees
Surface geology Dominant surface geology is shown in a 25ha grid based
on the Danish geological surveys map which cover 75% of the country
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Soil sampling for texture analyses
• ADK distributed topographic maps and questionnaires to local agronomists (advisors) who registered existing texture analyses
• The agronomists were asked to recommend suitable locations for forthcoming soil sampling
• ADK combined the recommendation with infor-mation on topography and surface geology and the final sampling sites were chosen
• The agronomists undertook the soil sampling. 36000 topsoil samples (0-20cm) and 6000 subsoil samples (35-55cm) were taken
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Samplingsites
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Analyses
Texture: 2m, 20m, (63m), 200m, 2000m
Hydrometer method and sieving
Organic C: Determined by a Leco-apparatus
Lime: Determined by treating the samples with HCl
and capture the carbondioxide in
bariumhydroxide
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Texture analyses
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Sample library
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Texture classification
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Map construction
• The borders on the soil maps were drawn by the crew at ADK in cooperation with the local agronomists
• The drawing of the borderlines was based on the texture analyses, landscape analyses, the surface geology maps and the local knowledge from the agronomists involved.
• The maps were digitized and all analytical data were stored in a database. The software was developed as a Ph.D. study at Århus University
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Soil map from Aabenraa
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Soil map of Ribe
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Soil map of Denmark
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Additional soil maps 1980-1985
• Geomorphological map
• Subsoil texture map
• Wetland map
• Potential acid sulfate soil
• Soil map of the forests
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Geomorphological map of Denmark
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Geological Surveys map of Gislum, 1:25000
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Subsoil texture
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Incircled wetlands on a topographic map
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Wetlands
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Soil chemical and physical data
• By combining the different soil maps an area can be characterized as follows:
Topsoil: Fine sand (MCC2) Subsoil: loam (MCC5) Drainange: not wetland Geomorphology: Weichsel moraine
• In order to use the soil maps in planning there is a huge need for soil profile analytical data, chemical as well as physical
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Profile sampling sites
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Soil classification
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Classification system
The classification based exclusively on field observations.
Describe the main pedological development within 120cm.
Describe the presence of gley, lithic and limestone contactwithin 3 sections of the profile: 0-40, 40-80 & 80-120 cm
Describe the thickness and carbon content of the A-horizon
Describe the presence of fragipan, placic horizon,degradated B-horizons, cementation, calcic horizons
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Danish soil classification system, soil orders
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Danish soil classification system, soil groups
Group leveI 1 2 3
Lessive ranker* gley* podzol
rendzin* pseudogley* brunjord
degra stagnogley* brunsol
blandings
typi
*begin at 40-80cm
Example: Degralessive
Podzolpseudogleytypilessive
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Danish soil classification system, soil series
• Gley, lime and lithic contact in the soil section 80-120 cm
• Placic horizon, fragipan, cementation, degradated Bt or Bs horizons, natric horizons, all within 1.2 meter depth
• entic A-horizons (<10cm), kolluvial A horizon (40-80cm) humus poor A-horizon (10-40cm thick and <1% OM), humus rich A-horizon (10-40cm thick and 7-20% OM), histic O-horizon 10-40 cm thick and >20%OM.
• Example: kolluvial pseudogleyey Typilessive• entic Degralessive
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Soil name at order, group and series
Podzol (A-E-Bh-Bs-C)
1)Typipodzol (gley > 120cm depth)
2) gleyey Typipodzol (gley 80-120cm)
3) Gleytypipodzol (gley 40-80cm)
4) Podzolgley (gley 0-40cm)
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Danish pedological soil classification system
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Transformation of soil names to figures
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Finding special soil types
Podzols with placic horizons
Order 06; group 26 = all podzols + series 13 = placic
Soils with Bt and lime beginning below 80-120 cm
Order 05; group 25 = soils with Bt +
Series 16 + 17 = lime beginning below 80 cm
Soils with deep A-horizons
Order 07 = A horizons deeper the 80 cm +
series 01 = A horizons 40-80 cm deep
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Soil toposequence based on soil classification for every 25 meter on the pipeline
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Profile description
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Rendzinleptosol on Senon limestoneCambisol in calcareous loamy till
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Luvisols
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Podzoluvisols
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Regosol and arenosol
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Podzols
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Podzols
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Gleysols
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Inner marsh clay upon a podzol
Fluvisol in outer marsh deposits
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Histosols, one developed on a former podzol
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Histosols
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Soil profile description scheme
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Analyses
• Texture (hydrometer + sieving)• Total carbon (dry combustion)• Total nitrogen (Kjeldahl)• Total organic and inorganic phosphorous• pH(H2O) and pH(CaCl2)• Lime content (Scheibler)• Exchangeable acidity at pH 8.1 (Pipers method)• Exchangeable bases (NH4Ac-extraction at pH7)• DCB, oxalate and pyrophosphate iron and aluminium• KCl-extractable H and Al• Soil water retention (Pressure plate apparatus)
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The use of the databases
Protection of fertile farmland around towns
Irrigation need for agriculture production at county level
Irrigation permission
Hunting zones
Economical compensation for drainage
The potential drainage need at national level
Mapping of potential set aside area
Carbon storage in Danish soils
Nitrate leaching from farmland
Potentially acid sulfate soil
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Example of rules for irrigation permission Ribe County
If a farmer wants to irrigate his fields he has to get a soil
texture analyses of the plowlayer and send it to the county
administration. They use the following equation derived
from the soil profile analytical database
PAW: 2.34*OM% + 0.70*clay + 0.47*silt + 0.18*FS + 3.68
If PAW < 20 the farmer may irrigate with 100mm/ha
If PAW is 20-30 the farmer may irrigate with 75mm/ha
If PAW is >30 the farmer may irrigate with 50mm/ha
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Root Zone CapacityBased on the texture analyses from the Danish Soil Classification and
the geological map, soil profiles at 36.000 sites are constructed with
texture in the depth: 0-30 cm, 30-60 cm and 60-120 cm.
Based on the soil profile analytical database the following equations
between water content at FC and PWP (vol%) can be established:
FC=2.34*%OM + 0.70*%clay + 0.47*%silt + 0.18%*FS + 3.68, r2=0.84
PWP=0.55*%OM + 0.63*%clay + 0.18*silt + 1.12 r2=0.89
Based on root studies an effective root depth for crops in relation to soil
type can be determined and RZC for water in mm can be calculated
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Root zone capacity for barley
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Mean irrigation need for barley production
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Potential drainage need
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Set aside areas in Denmark
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FAO 1974 soil map
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EC-soil map scale 1:1.000.000 - 1985
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FAO 1990
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FAO-soil types on sandy parent materials
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FAO-soil map
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FAO Soil Map Denmark
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FAO-legend
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FAO soil types in relation to landform
![Page 65: The Danish Soil Classification From 1939 to 1975 the farmland area dropped from 32.000 sqkm to 28.000 sqkm It raised a need for soil maps for planning.](https://reader035.fdocuments.net/reader035/viewer/2022062619/55152bcd5503465e608b57bf/html5/thumbnails/65.jpg)
Soil analytical data, proforma 1
![Page 66: The Danish Soil Classification From 1939 to 1975 the farmland area dropped from 32.000 sqkm to 28.000 sqkm It raised a need for soil maps for planning.](https://reader035.fdocuments.net/reader035/viewer/2022062619/55152bcd5503465e608b57bf/html5/thumbnails/66.jpg)
Soil analytical data, proforma 2