INSPIRE-WMS Soil / Medium thermal conductivity BB
Description
The interoperable INSPIRE WMS is a display service that displays data in the annex schema ground (derived from the original dataset: Mean thermal conductivity Brandenburg). It gives an overview of the thermal conductivity at permanent wilting point (PWP) - in late summer, the thermal conductivity at field capacity (FK) - in spring, and the difference in thermal conductivity at field capacity (FK) - permanent wilting point (PWP). Thermal conductivity determines the property of the soil to transport thermal energy through conduction. It is the decisive parameter for the use of the soil as a heat source and storage and must be taken into account, among other things, in the application of near-surface geothermal energy (earth heat collectors) or in the construction of underground power cables. To calculate the thermal conductivity, the pedotransfer function (PTF) according to Markert et al. (2017) is used. According to the INSPIRE data specification Soil (D2.8.III.3_v3.0), the contents of the ground map are INSPIRE-compliant. The WMS contains the following layers:
- SO.thermalConductivityFieldCapacity: Thermal conductivity at field capacity (FK) — in spring
- SO.thermalConductivityDifference: Difference in thermal conductivity at field capacity (FK) — permanent wilting point (PWP)
- SO.thermalConductivityWiltingPoint: Thermal conductivity at permanent wilting point (PWP) — late summer
- SO.SoilBody: Delimited and homogeneous part of the floor covering with respect to certain soil characteristics and/or spatial patterns.
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The compliant INSPIRE-WMS Soil / Mittlere Wärmeleitfähigkeit Brandenburg is a view service that delivers data in the annex schema Soil (derived from the original data set: Average thermal conductivity in the soil Brandenburg). It provides an overview of the thermal conductivity at permanent wilting point (PWP) - in late summer, the thermal conductivity at field capacity (FK) - in spring, and the difference in thermal conductivity at field capacity (FK) - permanent wilting point (PWP). The thermal conductivity determines the property of the soil to transport thermal energy by conduction. It is the decisive parameter for the use of the soil as a heat source and storage and, among other things, have to be taken into account when using near-surface geothermal energy (geothermal collectors) or when building underground power cables. To calculate the thermal conductivity, the pedotransfer function (PTF) according to Markert et al. (2017) was used. The content of the soil map is compliant to the INSPIRE data specification for the annex theme Soil (D2.8.III.3_v3.0). The WMS includes the following layers:
- SO.thermalConductivityFieldCapacity: Thermal conductivity at field capacity (FK) - in spring
- SO.thermalConductivityDifference: Difference in thermal conductivity at field capacity (FK) - permanent wilting point (PWP)
- SO.thermalConductivityWiltingPoint: Thermal conductivity at permanent wilting point (PWP) - in late summer
- SO.SoilBody: Part of the soil cover that is delineated and that is homogeneous with regard to certain soil properties and/or spatial patterns.
Resources
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Description |
Link |
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https://inspire.brandenburg.de/services/so_waermeleitf_wms? |
Tags
- interoperabel
- wärmeleitfähigkeit
- wms
- geologie
- bboxbebb
- opendata
- oberboden
- soillayer
- infomapaccessservice
- inspireidentifiziert
- soilbody
- thermalconductivityfieldcapacity
- thermalconductivitywiltingpoint
- process
- depthinterval
- om_observation
- bodenkunde
- mittlere-wärmeleitfähigkeit-brandenburg
- interoperability
- soil
- derivedsoilprofile
- bodenschutz
- brandenburg
- soilderivedobject