Local retention potential is a calculation of the risk of phosphorus reaching surface water within a DARO and is a weighting of hydrological and geological risk. The hydrological risk is calculated by relating topographical distance to water (the route the water is estimated to run, such as surface or groundwater, to the nearest permanent watercourse, distance), to the extent of the run-off at each individual point (where the water reaches the nearest watercourse, catchment area). The geological risk has been assumed to increase with reduced infiltration capacity (soil species) and thinner soil layers (soil depth) The assumption is that retention decreases if the water/wastewater cannot penetrate/infiltrated into the soil. High risk means low retention, i.e. less phosphorus is naturally fixed in the soil on the way to the receiving water. Low risk and higher retention
results in a higher degree of fixing.
The purpose of the GIS support is to create conditions at a national level for a reasonable, legally certain and more consistent assessment of the level of protection under Chapter 2, Section 3 of the Environmental Code when examining small sewers. The GIS support consists of maps showing the risk of impact on recipient/exposure point due to load from a drain. The maps have been produced through risk assessments based on the legislator’s instructions on criteria for assessing the high/higher level of protection for the entire surface of Sweden.
Build on reliable and scalable technology
FAQ
Frequently Asked Questions
Some basic informations about API Store ®.
Operation and development of APIs are currently fully funded by company Apitalks and its usage is for free.
Yes, you can.
All important information such as time of last update, license and other information are in response of each API call.
In case of major update that would not be compatible with previous version of API, we keep for 30 days both versions so you will have enough time to transfer to new version. We will inform you about the changes in advance by e-mail.