Regulation 5 Amendment of Schedule
In the Schedule (Groundwater Threshold Values) for Table 1 substitute—
“
Table 1
Threshold values for assessing groundwater chemical status
Parameter Unit To examine if groundwater abstraction is causing saline or other intrusions >To examine if groundwater is providing a significant contribution to the failure of the environmental objectives of associated surface water bodies To examine if the quality of groundwater that is abstracted for potable use is deteriorating, possibly resulting in a need for increased purification To examine the spatial extent of a groundwater body or group of bodies that are exceeding an EU Standard or threshold value (1)The surface water environmental standards are set out in Schedule 1 to The Water Framework Directive (Classification, Priority Substances and Shellfish Waters) Regulations (Northern Ireland) 2015(S.R. 2015 No. 351).
(2)The “dilution factor” is taken to be the fraction of the average annual river flow derived from groundwater inflows. It can be estimated from established hydrological indices such as the baseflow index, or from the ratio of catchment groundwater recharge to effective precipitation.
Ammonium mg/l 0.29 Arsenic μg/l 7.5 Atrazine μg/l 0.075 Cadmium μg/l 3.75 Chloride mg/l 25 Electrical Conductivity μS/cm 800 1875 Lead μg/l 7.5 MCPA μg/l 0.075 Mecoprop μg/l 0.075 Mercury μg/l 0.75 Nitrate (as NO3) mg/l 37.5 37.5 Nitrite μg/l 375 375 Simazine μg/l 0.075 Sulphate mg/l 187.5 Tetrachloroethylene μg/l 7.5 7.5 Trichloroethylene μg/l 7.5 7.5 Any pollutant in relation to which a surface water environmental standard has been setf1 0.5 x (surface water standard divided by dilution factor)f2 ”
Annotations
Footnotes
- f1
(1)
The surface water environmental standards are set out in Schedule 1 to The Water Framework Directive (Classification, Priority Substances and Shellfish Waters) Regulations (Northern Ireland) 2015(S.R. 2015 No. 351).
- f2
(2)
The “dilution factor” is taken to be the fraction of the average annual river flow derived from groundwater inflows. It can be estimated from established hydrological indices such as the baseflow index, or from the ratio of catchment groundwater recharge to effective precipitation.