Groundwater Under the Pacific Northwest • November 2-3, 2005 • Stevenson, Washington

ABSTRACT

 Application of Three-Dimensional Groundwater and Nutrient Fate and Transport and Optimization Models for Science Based Policy Development to Protect a Drinking Water Aquifer in the La Pine Region of Central Oregon

Presenter:  Barbara J. Rich, Deschutes County Environmental Health Division
Co-Authors:  Stephen R. Hinkle, David S. Morgan

The La Pine sub-basin of the Upper Deschutes River is underlain by a shallow sole source aquifer that currently supplies drinking water for approximately 18,000 people.  Fifteen thousand lots of one-half to one acre in size were platted in the 1960s and 1970s, prior to Oregon’s land use planning laws, located within a 125-square mile corridor near the scenic Deschutes River and the smaller Little Deschutes River.  Without an understanding of the high water table or the aquifer’s water quality and with no promise of public infrastructure, the lots were marketed nationally at the time to unsuspecting buyers.  At build-out, this area could support as many as 26,000 people. 

The groundwater quality in this region of southern Deschutes County, Oregon is threatened by nitrate contamination from onsite wastewater as a result of rapid rural residential growth over the past 30 years.  Based on data collected over the past 10 years, we now know that the soils in this region are highly porous and permeable with no intervening layer protecting the shallow unconfined aquifer.  These young pumice soils are low in organic matter and rapidly draining, which results in the rapid downward movement of recharge from precipitation.  However, the aquifer receives only about 2.0 inches of total annual precipitation, and so resulting groundwater velocities are low.  The shallow portion of the aquifer, to a depth of about 50 feet below the water table, is highly oxygenated.  Below this, the aquifer becomes suboxic and, coupled with buried carbon sources, becomes a natural denitrifying system.  This natural denitrification protects portions of the La Pine aquifer from nitrate accumulation, but the upper oxic portions remain vulnerable to anthropogenic nitrogen.

Extensive work by the U.S. Geological Survey (USGS), in cooperation with the Oregon Department of Environmental Quality (DEQ) and Deschutes County Environmental Health Division (DCEH), resulted in a detailed investigation of the geochemical processes at work and the development of a three-dimensional groundwater and nutrient fate and transport model for the sub-basin.  The USGS subsequently enhanced the functionality of the 3-D model by linking it with an optimization model developed to define specific management scenarios for the region based on environmental or other constraints.  These constraints may include maximum groundwater nitrate levels, maximum discharges allowed to the river systems and the treatment levels attainable by onsite wastewater treatment systems.

This presentation illustrates several aspects of the policy development process, including the development of science based public policy and regulation in a multi-jurisdictional setting; the use of the NLMM and other results of the scientific investigations to educate local businesses, property owners, and other stakeholders; and the potential for tracking the results of the management activities in terms of environmental outcomes.