the danish soil classification

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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. 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. - PowerPoint PPT Presentation

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Page 1: The Danish Soil Classification

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

Page 2: The Danish Soil Classification

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

Page 3: The Danish Soil Classification

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)

Page 4: The Danish Soil Classification

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

Page 5: The Danish Soil Classification

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.

Page 6: The Danish Soil Classification

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

Page 7: The Danish Soil Classification

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

Page 8: The Danish Soil Classification

Samplingsites

Page 9: The Danish Soil Classification

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

Page 10: The Danish Soil Classification

Texture analyses

Page 11: The Danish Soil Classification

Sample library

Page 12: The Danish Soil Classification

Texture classification

Page 13: The Danish Soil Classification

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

Page 14: The Danish Soil Classification

Soil map from Aabenraa

Page 15: The Danish Soil Classification

Soil map of Ribe

Page 16: The Danish Soil Classification

Soil map of Denmark

Page 17: The Danish Soil Classification

Additional soil maps 1980-1985

• Geomorphological map

• Subsoil texture map

• Wetland map

• Potential acid sulfate soil

• Soil map of the forests

Page 18: The Danish Soil Classification

Geomorphological map of Denmark

Page 19: The Danish Soil Classification

Geological Surveys map of Gislum, 1:25000

Page 20: The Danish Soil Classification

Subsoil texture

Page 21: The Danish Soil Classification

Incircled wetlands on a topographic map

Page 22: The Danish Soil Classification

Wetlands

Page 23: The Danish Soil Classification

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

Page 24: The Danish Soil Classification

Profile sampling sites

Page 25: The Danish Soil Classification

Soil classification

Page 26: The Danish Soil Classification

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

Page 27: The Danish Soil Classification

Danish soil classification system, soil orders

Page 28: The Danish Soil Classification

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

Page 29: The Danish Soil Classification

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

Page 30: The Danish Soil Classification

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)

Page 31: The Danish Soil Classification

Danish pedological soil classification system

Page 32: The Danish Soil Classification

Transformation of soil names to figures

Page 33: The Danish Soil Classification

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

Page 34: The Danish Soil Classification

Soil toposequence based on soil classification for every 25 meter on the pipeline

Page 35: The Danish Soil Classification
Page 36: The Danish Soil Classification

Profile description

Page 37: The Danish Soil Classification

Rendzinleptosol on Senon limestoneCambisol in calcareous loamy till

Page 38: The Danish Soil Classification

Luvisols

Page 39: The Danish Soil Classification

Podzoluvisols

Page 40: The Danish Soil Classification

Regosol and arenosol

Page 41: The Danish Soil Classification

Podzols

Page 42: The Danish Soil Classification

Podzols

Page 43: The Danish Soil Classification

Gleysols

Page 44: The Danish Soil Classification

Inner marsh clay upon a podzol

Fluvisol in outer marsh deposits

Page 45: The Danish Soil Classification

Histosols, one developed on a former podzol

Page 46: The Danish Soil Classification

Histosols

Page 47: The Danish Soil Classification

Soil profile description scheme

Page 48: The Danish Soil Classification

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)

Page 49: The Danish Soil Classification

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

Page 50: The Danish Soil Classification

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

Page 51: The Danish Soil Classification

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

Page 52: The Danish Soil Classification

Root zone capacity for barley

Page 53: The Danish Soil Classification

Mean irrigation need for barley production

Page 54: The Danish Soil Classification

Potential drainage need

Page 55: The Danish Soil Classification

Set aside areas in Denmark

Page 56: The Danish Soil Classification

FAO 1974 soil map

Page 57: The Danish Soil Classification

EC-soil map scale 1:1.000.000 - 1985

Page 58: The Danish Soil Classification

FAO 1990

Page 59: The Danish Soil Classification
Page 60: The Danish Soil Classification

FAO-soil types on sandy parent materials

Page 61: The Danish Soil Classification

FAO-soil map

Page 62: The Danish Soil Classification

FAO Soil Map Denmark

Page 63: The Danish Soil Classification

FAO-legend

Page 64: The Danish Soil Classification

FAO soil types in relation to landform

Page 65: The Danish Soil Classification

Soil analytical data, proforma 1

Page 66: The Danish Soil Classification

Soil analytical data, proforma 2