The following definitions shall apply in this article, including all subparts thereof, unless otherwise specified:
ABANDONED WELLAny well which has been replaced by another well, is no longer in service because of the availability of a public water supply, or no longer serves its intended use due to loss of water quantity or quality. Wells which are connected to uses which are infrequently used and wells which are being held in reserve for development or installed in anticipation of development shall not be considered abandoned if the wells are properly capped and protected from contamination.
ADDED DRAWDOWNThe additional amount of drawdown in a well beyond what is normally expected for that well and that is caused by the pumping of another well nearby.
ALTERTo enlarge, deepen, replace or in any other way change any portion of an existing water supply system. The terms "alteration" and "altered" shall be construed accordingly.
APPLICANTA person required by this article to obtain a well permit.
APPLICATIONThe application form and accompanying documentation required by Nockamixon Township for approval to locate, construct, or alter a water supply.
AQUIFERA formation, group of formations, or part of a formation that contains sufficient saturated permeable material to yield economic quantities of water to wells and springs.
AQUIFER, CONFINEDAn aquifer that is overlain by a confining bed (aquitard). The confining bed has a significantly lower hydraulic conductivity than the aquifer. "Artesian aquifer" is a synonym.
AQUIFER, SEMI-CONFINEDAn aquifer overlain by a low-permeability layer that permits water to slowly migrate through to the aquifer. Also termed "leaky artesian" or "leaky confined" aquifer.
AQUIFER, UNCONFINEDAn aquifer in which there are no confining beds between the zone of saturation and the ground surface. "Water-table aquifer" is a synonym.
AQUITARDA low-permeability unit that can store groundwater and transmit water slowly from one aquifer to another. (Also see "aquifer, confined.")
BASEFLOWThe component of flow in a perennial stream due to groundwater discharging to the stream. Baseflow does not include stormwater runoff that causes flow to increase during precipitation events.
BCHDBucks County Health Department.
BOARDThe Nockamixon Township Board of Supervisors.
CERTIFIED LABORATORYAny laboratory, facility, consulting firm, government or private agency, business entity or other person that the Pennsylvania Department of Environmental Protection has licensed or accredited to perform certain types of analyses of drinking water samples.
CONFINING BEDA body of low hydraulic conductivity material that is stratigraphically adjacent to one or more aquifers.
CONTAMINANTAny physical, chemical, biological, or radiological substance or matter that has an adverse effect on air, water, or soil quality.
CONTRIBUTING AREAThe area of land surface that supplies the withdrawal for a given groundwater well.
DRAWDOWNThe lowering of the water table of an unconfined aquifer or the potentiometric surface of a semi-confined or confined aquifer caused by pumping of groundwater from a well or wells. Drawdown is determined by subtracting the depth to water during pumping from the static water level determined prior to the start of pumping.
DRBCDelaware River Basin Commission.
FLOW RATEThis term shall be interchangeable with "pumping rate" or "pump rate."
GROUNDWATERWater beneath the surface of the ground within a zone of saturation, whether or not flowing through known and definite channels or percolating through underground geologic formations and regardless of whether the result of natural or artificial recharge. The term includes water contained in aquifers, artesian and nonartesian basins, underground watercourses and other bodies of water below the surface of the earth.
HEADThe energy of water per unit weight comprised of elevation, pressure, and velocity components. In a groundwater system, because the velocity component is usually negligible, head is measured as the elevation of the surface of water in a well above a standard datum.
HEAD GRADIENTThe change in head per unit distance in the direction of water movement.
HYDRAULIC CONDUCTIVITYThe measure of a geologic formation's ability to transmit water. It is expressed as the volume of water at the prevailing density and viscosity that will move in a unit time under a unit head gradient through a unit area.
HYDROGEOLOGYThe study of groundwater with particular emphasis given to its chemistry, mode of migration, and relation to the geologic environment.
INFILTRATIONThe flow of water downward from the land surface into and through the upper soil layers. Synonym to "percolation."
LOT OR LOT IN QUESTIONFor the purposes of this article, a designated parcel, tract or area of land established by a plat or otherwise as permitted by law to be used, developed or built upon as a unit and upon which a water supply well is proposed or additional water extraction for an existing land use is proposed. The lot is a parcel of land, used or set aside and available for use as the site of one or more buildings and any buildings accessory thereto or for any other purpose, in one ownership and not divided by a street, nor including any land within the right-of-way of a public or private street upon which said lot abuts, even if the ownership to such right-of-way is in the owner of the lot.
MAXIMUM CONTAMINANT LEVEL (MCL)The maximum permissible concentration of a constituent or contaminant in drinking water. The source of data for MCLs shall be federal and Pennsylvania law, and in the case of a conflict, the stricter (more protective of water quality) provision shall apply.
MULTI-WELL PROJECTAny proposed land use, activity, development, or project that involves the installation of more than one water well as part of the proposed land use, activity, or project. Installation of a second water well on an existing residential property for an accessory use shall not be considered a multi-well project.
NEIGHBOR NOTIFICATION DISTANCEA distance between the boundary of the lot on which a test well is proposed and neighboring wells or groundwater sources that, for all owners of wells or other groundwater sources (e.g., springs) within the distance, the applicant must notify as further set forth in §
234-114. Distances are specified in §
234-114.
OBSERVATION WELLA water well used to observe the elevation of the water table or the potentiometric surface, typically during a pump test or other aquifer test. An observation well is generally constructed similar to a test well.
PaDEPPennsylvania Department of Environmental Protection.
PERENNIAL STREAMA body of water flowing in a channel or bed composed primarily of substrates associated with flowing waters and capable, in the absence of pollution or other man-made stream disturbances, of supporting a benthic macroinvertebrate community which is composed of two or more recognizable taxonomic groups of organisms which are large enough to be seen by the unaided eye and can be retained by a United States Standard No. 30 sieve (28 meshs per inch, 0.595 mm openings) and live at least part of their life cycles within or upon available substrates in a body of water or water transport system.
POROSITYThe voids or openings in rock and soil. Porosity may be expressed quantitatively as the ratio of the volume of openings in a rock or soil to the total volume of the rock or soil.
POTABLE WATERAny water used, or intended to be used, for drinking and/or culinary purposes which is free from impurities in amounts sufficient to cause disease or harmful physiological effects, and complies with the bacteriological and chemical quality standards of the USEPA, PaDEP, and BCHD.
PRODUCTION WELLA water well that supplies water to a given land use, activity, development, or project.
PROVISIONAL CERTIFICATERefers to a written approval issued by Nockamixon Township authorizing well construction and testing in accordance with the applicant's preconstruction and pretesting/analysis submittal package under §
234-120B(1).
PUMP RATEThe rate which water is removed from an aquifer by pumping a well, often expressed in gallons per minute. In this article, this term is interchangeable with "flow rate" and "pumping rate."
PUMP TESTThis shall be interchangeable with "pumping test."
QUALIFIED HYDROGEOLOGISTAn individual licensed by the Commonwealth of Pennsylvania to practice geology, and who specializes in the practice of applying geologic and hydrogeologic principles to interpretation of groundwater conditions and conducting aquifer tests and the analysis of aquifer test data. The individual shall provide a resume or curriculum vitae to document licensure, education and experience requirements.
RECHARGEThe volume of water that infiltrates to an aquifer, often expressed in inches per year per unit area.
RECHARGE AREAAn area at land surface where recharge occurs to a particular aquifer.
REGISTRANTA person required by this article to register a water well.
REPLACEMENT WELLA well installed for the sole purpose of supplanting an existing well that can no longer provide sufficient water to the residence or business on the lot. Within 30 days of approval to operate the replacement well, the existing well must be decommissioned.
SATURATED ZONEThe zone in which the voids in the rock or soil are filled with water at a pressure greater than atmospheric. The water table is the top of the saturated zone in an unconfined aquifer.
STATIC WATER LEVELThe depth from ground surface to water in a well undisturbed by pumping. Also reported as elevation referenced to a standard datum.
STORAGE COEFFICIENT (STORATIVITY)The volume of water an aquifer releases or takes into storage per unit surface area of the aquifer per unit change in head. It equals the product of specific storage and aquifer thickness.
TEST WELLA water well drilled to gather data on water supply availability and quality, and on aquifer characteristics.
TOTAL DAILY DEMANDThe total amount of water used or projected to be used each day by a household or facility, often expressed in gallons per day. In this article, average daily demand and total daily demand shall be considered interchangeable.
TRANSMISSIVITYThe rate at which water of a prevailing density and viscosity is transmitted through a unit width of an aquifer under a unit head gradient. Transmissivity equals hydraulic conductivity multiplied by aquifer thickness.
UNSATURATED ZONEThe zone between ground surface and the water table. Pore spaces in the unsaturated zone contain water at pressures less than atmospheric. Also referred to as "zone of aeration" and "vadose zone."
WATER TABLEThe surface for which water begins to fully occupy porespace. Water table depth (elevation) is measured by the level at which water stands in a well situated in a surficial aquifer.
WELLA hole or excavation larger than four inches in diameter or a hole or excavation deeper than 10 feet in depth that is drilled, bored, cored, driven, jetted, dug, or otherwise constructed for the purpose of removal of, or investigation of, or exploration for, water, regardless of the intended use (e.g., residential, agricultural, industrial, etc.).
WELL PERMITRefers to a written approval issued by Nockamixon Township authorizing the operation of a well or wells in accordance with the permit after the applicant has met the requirements of this article, including, but not limited to, submission of a final report under §
234-120B(3).
WELL RECORDA geologic log and the construction details of a well, which is completed by the well driller subsequent to well installation.