Surface water - salinisation lines

Description

At low discharge of the Rhine or due to a high water level at sea (by storm), salt water from the Nieuwe Waterweg can enter the main water system. As a result, inlet points can become salinised. These lines are an indication of where salinisation may occur

Resources

Name Format Description Link
0 https://geodata.zuid-holland.nl/geoserver/water/wfs?service=WFS&version=2.0.0&request=GetCapabilities
0 https://geodata.zuid-holland.nl/geoserver/water/wms?service=WMS&version=1.3.0&request=GetCapabilities
21 https://geoservices.zuid-holland.nl/arcgis/rest/services/Water/Water_zoetwatervoorziening/MapServer
23 https://www.nationaalgeoregister.nl/geonetwork/srv/dut/catalog.search#/metadata/e08886ca-3f61-4797-81dc-26c17c3760fc
34 https://geodata.zuid-holland.nl/geoserver/water/wms?service=WMS&version=1.3.0&request=GetMap&layers=water%253AOW_VERZILTINGSLIJNEN&bbox=61030.05150000006%252C424662.34959999844%252C107498.59910000116%252C446735.46869999915&width=768&height=364&srs=EPSG%253A28992&maxFeatures=40000&format=image%252Fpng

Tags

  • oppervlaktewater
  • verziltingslijnen
  • verzilting
  • watervoorziening
  • wateraanvoer

Topics

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