Alternate title

Happamien sulfaattimaiden yleiskartta

Date ( Publication )

2014-09-17

Edition

1.0

Identifier

FI / 1000662

Presentation form

digitalGeographicInfo

Purpose

The 1:250 000 scale data on acid sulfate soils is suitable for planning of land use on a general scale, planning and execution of water management and related action plans, monitoring of surface water condition and in the prevention of acidification and metal burden. Moreover, the data can be used in agriculture and forestry, scientific and applied research, and when considering actions that mitigate and prevent problems caused by acid sulfate soils. The scale of the maps (regional planes) is 1:100 000-1:250 000.

The data is unsuitable for determining detailed protection / remediation actions, for example, on a farm-specific level. However, the data can be used for finding targets for more detailed surveys.

Credit

Åbo Akademi, Geologian ja mineralogian laitos

Credit

Helsingin Yliopisto, Elintarvike- ja ympäristötieteiden laitos

Status

Completed

Maintenance and update frequency

As needed

Geosanasto Geosanasto Geosanasto ( Place )

• Finland

Geosanasto Geosanasto Geosanasto ( Temporal )

• Quaternary
• Holocene

Geosanasto Geosanasto Geosanasto ( Theme )

• Environmental effects
• Soils
• Sediments
• Gyttja
• Clay
• Silt
• Fine sand
• Peat
• Sulfides
• pH

GEMET - INSPIRE themes, version 1.0 GEMET - INSPIRE themes, version 1.0 ( Theme )

• Geology

Paikkatietohakemiston asiasanasto Paikkatietohakemiston asiasanasto ( Theme )

• avoindata.fi

Use limitation

The general map data on acid sulfate soils is intended to be used in scales 1:100 000-1:250 000. Users should remember that the planes depicting the occurrence of sulfides are a generalisation or an interpretation of the terrain. In reality, an individual pattern might contain significant variation on the field due to the variation of soil types and groundwater table.

The existence and depth of occurrence of sulfide has been verified with different methods or combinations thereof: sensory evaluation on the field, laboratory analyses of the samples, pH measured on the field and pH incubation. Sensory evaluation is subjective, and if used as the only analysis method, should be considered a potential source of error.

The general survey data on acid sulfate soils cannot be used for detailed farm-specific investigations or for planning farm-specific actions. In the scale specified, the data can be used as an aid in the planning of water management and land use, and targeting more detailed surveys to problematic areas.

Use limitation

http://tupa.gtk.fi/paikkatieto/lisenssi/gtk_open_licence_2.pdf

Access constraints

License

Use constraints

Copyright

Other constraints

Ei muita rajoitteita.

Classification

Unclassified

Denominator

250000

Metadata language

fin

Character set

8859 Part 15

Topic category

• Geoscientific information

Reference system identifier

EPSG / ETRS89 / ETRS-TM35FIN (EPSG:3067) / 7.4

Topology level

Geometry only

Distribution format

• ESRI file gdb ( 10.1 )

OnLine resource

( WWW:LINK-1.0-http--link )

OnLine resource

Happamat sulfaattimaat ( WWW:LINK-1.0-http--link )

Hierarchy level

Dataset

Statement

The background material for the general survey of acid sulfate soils were the GTK soil maps (1:20 000 and 1:200 000), geophysical data from GTK’s airborne surveys, data from GTK’s peat investigations and the terrain database and elevation data of the National Land Survey of Finland. The primary data of the products are the field observations of the field survey and the laboratory analysis results. The surveyed area (the coastal area below the ancient Litorina shore) is surveyed by drainage basin (main division and coastal areas). The final product will consist of a uniform plane covering the entire coastal area below the ancient Litorina shore.

The acid sulfate soil survey consists of the following steps: (1) preliminary research where the survey material is collected and the survey plan is created (2) actual survey on the field (3) laboratory analyses and incubation and (4) processing and finalising the survey data (5) creation of map products (maps indicating the probability of existence, coarse-grained acid sulfate soils, classified observation points and profile point fact sheets) based on the survey data.

The field survey consists of the description of soil boring profiles (profile and survey points) down to 3 metres from the ground surface, collection of soil samples and pH measurements. Most of the field surveys are carried out in the vicinity of the road network. The observation point density is 1-2 / 2 km² on average.

Some samples collected in the field are sent to a laboratory for a more detailed analysis of multiple elements and possibly grain size distribution and humus content analysis. The samples to be analysed are chosen to represent the surveyed area and various lithologies as well as possible and thus support the creation of maps. The pH of all samples is also measured after an oxidation period (incubation) of 9-19 weeks.

Area maps on the probability of the existence of acid sulfate soils and the existence of coarse-grained acid sulfate soils are digitised using ArcMap software. The minimum area of a pattern is approximately 6 hectares. The maps are drawn using the following source materials:

- Field observations and laboratory analysis results (primary material)

- Soil maps, scale 1:20 000 and 1:200 000 (GTK)

- Peat survey data (GTK)

- Low-altitude airborne geophysics (GTK)

o Imaginary component of electrical conductivity (3 kHz)

o Real component of electrical conductivity (3 kHz)

o Apparent characteristic resistivity of electrical conductivity (3 kHz)

- Terrain database of the National Land Survey of Finland.

- Laser scanning data of the National Land Survey of Finland.

The 1:250 000 scale map contains four probability classes: high, moderate, low, very low. The existence of coarse-grained sulfate soils is described as a plane above the plane describing the probability of sulfate soil existence. A combination of these planes indicates the probability of sulfate soils and whether the area is interpreted to host coarse-grained sulfate soils. The correctness and uniformity of the planes is verified by the geologist in charge.

Profile points and survey points are classified according to boring point attributes and laboratory analysis resultsand the material is used to create a fact sheet for each profile point. The fact sheets present the lithostratigraphy and laboratory analysis results, among other things.

The final product of the map production are polygonal planes tied to a coordinate system and depicting the regional probability of the occurrence of sulfide sediments, and the profile and survey points and fact sheets describing the soil properties. Data collected during the survey is stored in the GTK geoinformation system (GTJ).

The 1:250 000 data of acid sulfate soils are published in the GTK map service. The service presents the polygons depicting the probability of the occurrence of sulfate soils, complemented with polygons depicting the occurrence of coarse-grained sulfate soils, profile and survey points classified by the depth of occurrence of the sulfide layer and the fact sheets of the profile points. The survey and development of survey methods was started at GTK in 2010 along with the CATERMASS Life+ programme (2010-2012).

Description

The acid sulfate soil survey consists of the following steps: (1) preliminary research where the survey material is collected and the survey plan is created (2) actual survey on the field (3) laboratory analyses and incubation and (4) processing and finalising the survey data (5) creation of map products (maps indicating the probability of existence, coarse-grained acid sulfate soils, classified observation points and profile point fact sheets) based on the survey data.

The field survey consists of the description of soil boring profiles (profile and survey points) down to 3 metres from the ground surface, collection of soil samples and pH measurements. Most of the field surveys are carried out in the vicinity of the road network. The observation point density is 1-2 / 2 km² on average.

Some samples collected in the field are sent to a laboratory for a more detailed analysis of multiple elements and possibly grain size distribution and humus content analysis. The samples to be analysed are chosen to represent the surveyed area and various lithologies as well as possible and thus support the creation of maps. The pH of all samples is also measured after an oxidation period (incubation) of 9-19 weeks.

Area maps on the probability of the existence of acid sulfate soils and the existence of coarse-grained acid sulfate soils are digitised using ArcMap software. The minimum area of a pattern is approximately 6 hectares. The maps are drawn using the following source materials:

- Field observations and laboratory analysis results (primary material)

- Soil maps, scale 1:20 000 and 1:200 000 (GTK)

- Peat survey data (GTK)

- Low-altitude airborne geophysics (GTK)

o Imaginary component of electrical conductivity (3 kHz)

o Real component of electrical conductivity (3 kHz)

o Apparent characteristic resistivity of electrical conductivity (3 kHz)

- Terrain database of the National Land Survey of Finland.

- Laser scanning data of the National Land Survey of Finland.

The 1:250 000 scale map contains four probability classes: high, moderate, low, very low. The existence of coarse-grained sulfate soils is described as a plane above the plane describing the probability of sulfate soil existence. A combination of these planes indicates the probability of sulfate soils and whether the area is interpreted to host coarse-grained sulfate soils. The correctness and uniformity of the planes is verified by the geologist in charge.

Profile points and survey points are classified according to boring point attributes and laboratory analysis resultsand the material is used to create a fact sheet for each profile point. The fact sheets present the lithostratigraphy and laboratory analysis results, among other things.

The final product of the map production are polygonal planes tied to a coordinate system and depicting the regional probability of the occurrence of sulfide sediments, and the profile and survey points and fact sheets describing the soil properties. Data collected during the survey is stored in the GTK geoinformation system (GTJ).

The 1:250 000 data of acid sulfate soils are published in the GTK map service. The service presents the polygons depicting the probability of the occurrence of sulfate soils, complemented with polygons depicting the occurrence of coarse-grained sulfate soils, profile and survey points classified by the depth of occurrence of the sulfide layer and the fact sheets of the profile points. The survey and development of survey methods was started at GTK in 2010 along with the CATERMASS Life+ programme (2010-2012).

The general survey and map drawing of acid sulfate soils used ArcGIS GIS software and GTK’s plugins (MAAPELI). The point cards of the survey points were made with the following software: MS Excel, Strater3 / SedLog, CorelDRAW and MS Office Publisher. The field observations are stored using a GPS device.

Description

The background material for the general survey of acid sulfate soils were the GTK soil maps (1:20 000 and 1:200 000), geophysical data from GTK’s airborne surveys, data from GTK’s peat investigations and the terrain database and elevation data of the National Land Survey of Finland. The primary data of the products are the field observations of the field survey and the laboratory analysis results. The surveyed area (the coastal area below the ancient Litorina shore) is surveyed by drainage basin (main division and coastal areas). The final product will consist of a uniform plane covering the entire coastal area below the ancient Litorina shore.

gmd:MD_Metadata

File identifier

a35864db-7cf6-4f30-bf82-b1a52825dc6c XML

Metadata language

fin

Character set

8859 Part 15

Hierarchy level

Dataset

Hierarchy level name

Happamat sulfaattimaat 1:250 000

Date stamp

2018-12-10T15:20:13