Parent Layer:
Land and Soil
Name: Aquifer Bedrock
Display Field: NAME
Type: Feature Layer
Geometry Type: esriGeometryPolygon
Description: <DIV STYLE="text-align:Left;"><DIV><DIV><P><SPAN STYLE="font-size:10pt">This is a polygon dataset containing nine Bedrock Aquifer classes.</SPAN></P><P STYLE="margin:0 0 14 0;"><SPAN /></P><P STYLE="margin:0 0 14 0;"><SPAN><SPAN>1) Regionally Important Aquifers:</SPAN></SPAN></P><P STYLE="margin:0 0 14 0;"><SPAN><SPAN>Regionally important aquifers are capable of supplying regionally important abstractions (e.g. large public water supplies), or excellent yields (>400 m3/d). Bedrock aquifer units generally have a continuous area of >25 km2 and groundwater predominantly flows through fractures, fissures, joints or conduits. Regionally important sand/gravel aquifers are >10 km2, and groundwater flows between the sand and gravel grains.</SPAN></SPAN></P><P STYLE="margin:0 0 14 0;"><SPAN><SPAN>This group is subdivided into the following types:</SPAN></SPAN></P><P STYLE="margin:0 0 14 0;"><SPAN><SPAN>Rk Regionally Important Karstified Bedrock Aquifer </SPAN></SPAN></P><P STYLE="margin:0 0 14 0;"><SPAN><SPAN>Rf Regionally Important Fissured Bedrock Aquifer </SPAN></SPAN></P><P STYLE="margin:0 0 14 0;"><SPAN><SPAN>Rg Regionally Important Sand/Gravel Aquifer</SPAN></SPAN></P><P STYLE="margin:0 0 14 0;"><SPAN><SPAN>Regionally important karstified aquifers may be further subdivided based on the whether groundwater flows mainly through conduits (Rkc) or more diffusely through solutionally-enlarged fissures (Rkd).</SPAN></SPAN></P><P /><P STYLE="margin:0 0 14 0;"><SPAN><SPAN>2) Locally Important Aquifers:</SPAN></SPAN></P><P STYLE="margin:0 0 14 0;"><SPAN><SPAN>Locally important aquifers are capable of supplying locally important abstractions (e.g. smaller public water supplies, group schemes), or good yields (100-400 m3/d). In the bedrock aquifers, groundwater predominantly flows through fractures, fissures, joints or conduits. Locally important sand/gravel aquifers are typically >1 km2, and groundwater flows between the sand and gravel grains.</SPAN></SPAN></P><P STYLE="margin:0 0 14 0;"><SPAN><SPAN>This group is subdivided into the following types:</SPAN></SPAN></P><P STYLE="margin:0 0 14 0;"><SPAN><SPAN>Lm Locally Important Bedrock Aquifer, Generally Moderately Productive </SPAN></SPAN></P><P STYLE="margin:0 0 14 0;"><SPAN><SPAN>Ll Locally Important Bedrock Aquifer, Moderately Productive only in Local Zones </SPAN></SPAN></P><P STYLE="margin:0 0 14 0;"><SPAN><SPAN>Lk Locally Important Karstified Bedrock Aquifer </SPAN></SPAN></P><P STYLE="margin:0 0 14 0;"><SPAN><SPAN>Lg Locally Important Sand/Gravel Aquifer</SPAN></SPAN></P><P /><P STYLE="margin:0 0 14 0;"><SPAN><SPAN>3) Poor Aquifers:</SPAN></SPAN></P><P /><P STYLE="margin:0 0 14 0;"><SPAN><SPAN>These bedrock aquifers are capable of supplying small abstractions (e.g. domestic supplies, small group schemes), or moderate to low yields (<100 m3/d). Groundwater predominantly flows through a limited and poorly-connected network of fractures, fissures and joints.</SPAN></SPAN></P><P STYLE="margin:0 0 14 0;"><SPAN><SPAN>This group is subdivided into the following types:</SPAN></SPAN></P><P STYLE="margin:0 0 14 0;"><SPAN><SPAN>Pl Poor Bedrock Aquifer, Generally Unproductive except in Local Zones </SPAN></SPAN></P><P STYLE="margin:0 0 14 0;"><SPAN><SPAN>Pu Poor Bedrock Aquifer, Generally Unproductive</SPAN></SPAN></P><P STYLE="margin:0 0 14 0;"><SPAN /></P></DIV></DIV></DIV>
Service Item Id: 0f691b33aefc4f82aae14c378b1c83a5
Copyright Text: Contains Irish Public Sector Data (Geological Survey) licensed under a Creative Commons Attribution 4.0 International (CC BY 4.0) licence
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Value: Rkc
Label: Rkc - Regionally Important Aquifer - Karstified (conduit)
Description: N/A
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Label: LI - Locally Important Aquifer - Bedrock which is Moderately Productive only in Local Zones
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