Critical aquifer recharge areas are areas with a critical recharging effect on aquifers used for potable water, including areas where an aquifer that is a source of drinking water is vulnerable to contamination that would affect the potability of the water, or is susceptible to reduced recharge. Critical aquifer recharge area maps shall be periodically revised, modified, and updated to reflect current information.
The following classifications define critical aquifer recharge areas:
(1) Susceptible Aquifer Recharge Areas. Susceptible aquifer recharge areas are those with geologic and hydrologic conditions that promote rapid infiltration of recharge waters to groundwater aquifers. For the purposes of this article, unless otherwise determined by preparation of an aquifer recharge area report authorized under this article, the following geologic units, as identified from available Washington Department of Natural Resources geologic mapping, define susceptible aquifer recharge areas for east Jefferson County:
(c) Beach sand and gravel (Hb);
(e) Floodplain alluvium (Hf);
(f) Vashon recessional outwash in deltas and alluvial fans (Vrd);
(g) Vashon recessional outwash in melt water channels (Vro);
(h) Vashon ice contact stratified drift (Vi);
(i) Vashon ablation till (Vat);
(j) Vashon advance outwash (Vao);
(k) Whidbey formation (Pw); and
(l) Pre-Vashon stratified drift (Py).
(2) Special Aquifer Recharge Protection Areas. Special aquifer recharge protection areas include:
(a) Sole-source aquifers designated by the U.S. Environmental Protection Agency in accordance with the Safe Drinking Water Act of 1974 (42 U.S.C.
300f et seq.), such as Marrowstone Island;
(b) Special protection areas designated by the Washington Department of Ecology under Chapter
173-200 WAC;
(c) Wellhead protection areas determined in accordance with delineation methodologies specified by the Washington Department of Health under authority of Chapter
246-290 WAC;
(d) Groundwater management areas designated by the Washington Department of Ecology in cooperation with local government under Chapter
173-100 WAC.
(3) Seawater Intrusion Protection Zones (SIPZ).
(a) Seawater intrusion protection zones are:
(i) Aquifers and land overlying aquifers with some degree of vulnerability to seawater intrusion. SIPZ are defined either by proximity to marine shoreline or by proximity to groundwater sources that have demonstrated high chloride readings.
(ii) All islands and land area within one-quarter mile of marine shorelines and associated aquifers together compose the coastal SIPZ.
(b) High Risk SIPZ.
(i) Existing individual groundwater sources with a history of chloride analyses above 200 mg/L are categorized as a high risk SIPZ for development proposed under this code.
(ii) Areas within 1,000 feet of a groundwater source with a history of chloride analyses above 200 milligrams per liter (mg/L) are categorized as a high risk SIPZ for development proposed under this code.
(c) At Risk SIPZ. Areas within 1,000 feet of a groundwater source with a history of chloride analyses above 100 milligrams per liter (mg/L) are categorized as at risk SIPZ for development proposed under this code.
(4) Connate Seawater Exception. In some cases, high chloride readings may be indicative of connate seawater (i.e., relic seawater in aquifers as opposed to active seawater intrusion). When best available science or a hydrogeologic evaluation demonstrates that high chloride readings in a particular area are due to connate seawater, the area in question shall not be considered an at risk or high risk SIPZ.
(5) Recommendation from Public Health Department. When the status of an area as either a high risk or an at risk SIPZ is in question, the administrator is responsible for making the determination based upon recommendation from the Jefferson County department of public health.
(Ord. 5-20 § 2 (Appx. A))