Laboratory analysis backs up field work. Truckee River groundwater project leader Alan McKay in DRI’s EPA-certified Water Analysis Laboratory in Reno. The lab analyzes water samples in support of numerous Truckee River research projects. (Photo by John Doherty)

Top Photo: Keystone for Downtown Renewal. Reno is focusing on the attraction of the Truckee River as the centerpiece of its ongoing effort to revive the downtown core casino and retail district.

From its beginnings at Lake Tahoe to its terminus in Pyramid Lake, the Truckee River is one of the most litigated, adjudicated, and studied little rivers in America. And virtually since the day DRI was founded in 1959, its scientists have been involved in some form of research somewhere along the Truckee River system, unraveling its complex ecology and assessing its response to 150 years of heavy human impacts. (See “DRI’s Long History with a Short River.”)

Today the Institute’s presence in the Truckee River Basin is greater than ever, spurred by a new focus on water quality that has grown out of a partnership of local, state, and federal government agencies dealing with water quality challenges. That focus is also oriented toward the future, seeking new knowledge for maintaining the river’s environmental quality while meeting increasing demands for water resources.

Barely more than 110 miles long, the Truckee drops 2,400 feet from Lake Tahoe to Pyramid Lake, getting used and re-used for rafting, fishing, swimming, kayaking, power generation, drinking, flushing, lawn-watering, light industrial processing, and agriculture along its course. The Truckee Meadows, the collective name for the valleys containing Reno, Sparks, and surrounding urbanization, is in the transition zone where the alpine Sierra Nevada foothills coalesce into the high desert of the Great Basin. And the area, itself, is in its own transition.

DRI scientist Alan McKay, who heads up a large part of DRI’s Truckee River studies, says development and other human influences—along with some natural conditions—affect the river’s water quality along its entire length.

McKay, a DRI associate research hydrologist who has served as the interim director of DRI’s Division of Hydrologic Sciences for two years, says the biggest issue for water quality compliance on the Truckee is the amount of total dissolved solids entering the river from urban and agricultural sources, and ending up in Pyramid Lake.

“A major challenge to future growth in the Truckee Meadows is the ability to treat salinity, the amount of total dissolved solids (TDS) we’re putting into the river,” McKay says.

The Clean Water Act of 1972 sets limits on the amount of salts and other pollutants allowed in the water through a mechanism referred to as the Total Maximum Daily Load, or TMDL. TMDLs present serious challenges to both Nevada and California along the entire length of the river, McKay says.

“The old philosophy for managing river water quality was ‘dilution is the solution for pollution,’” says McKay. “But TMDLs have changed that. The concern is about how many tons actually end up in Pyramid Lake, not the concentration of salts or other pollutants in the river water as the seasonal flow volume changes during the year.”
This change in emphasis reflects the fact that the desert lake is the evaporative terminus for the river. “The water evaporates but the salts stay in the lake. There is a limit to how much salt can be added each year and still maintain the viability of the lake as a fishery resource,” McKay points out.

He says local waste water treatment operators do an excellent job limiting the nutrients that support the growth of algae in the river, though there may be some river management techniques that could reduce that impact further. But the treatment process for removing salinity from wastewater is difficult and very expensive.
McKay says past water quality monitoring has shown that the river’s salinity increases dramatically in the 12-mile reach from Wadsworth, 20 miles east of Reno, to Nixon, just above the river delta at Pyramid Lake. “The graph of the TDS levels goes north just like the map of the river at that point,” he notes.

Data visualization helps to understand the challenge. The artificially colored map shows surface elevations in the region of the delta of the Truckee River at Pyramid Lake, with reds depicting higher elevations and blues lower elevations, and contours representing the thickness of the alluvial sediments above the underlying bedrock. The thickness of the sediment and its geochemistry are important factors in determining the sources of increased salinity in the groundwater entering the river. (Graphic by Michael Widmer, Washoe County Department of Water Resources)

“The conventional wisdom was that the surface water returning from irrigation in the Fernley-Wadsworth area was responsible. But the crop there is mainly alfalfa, and the growers don’t use much, if any, fertilizer. Further research finally showed that surface water return flow from irrigation is responsible for just a small amount of the salinity.”
McKay says this knowledge suggested that a workable solution to, or at least a reduction of, the river’s salinity problem might be accomplished through reducing the groundwater returning to the river by strategically reducing irrigated acreage in the Wadsworth-Fernley river segment.

This management option was one element of the Truckee River Water Quality Agreement of 1997 that settled long-standing litigation involving the Pyramid Lake Paiute Tribe, the U.S. Environmental Protection Agency (EPA), the state of Nevada, and the cities of Reno and Sparks.

The hard facts and real numbers to support the assumed benefits of this trade-off, however, were lacking, but the research challenge to develop that knowledge played directly to the strength of DRI’s hydrologic sciences capabilities.

Hydrogeologist Michael Widmer of the Washoe County Department of Water Resources recalls the Washoe County Regional Water Planning Commission requested competitive proposals to study groundwater’s role in the river’s salinity in the Wadsworth area and selected DRI for the project based on its strong qualifications. Today, Widmer is the County project manager for the study and a collaborator in the research.

“DRI had the experience and a great deal of knowledge about the river as well as some good ideas for approaching the problem,” he says. “The County is very serious about meeting water quality standards, but we have lacked a thorough understanding of the geochemistry in the watershed and the interaction of the river with the groundwater east of the Truckee Meadows.”

The study’s goals were ambitious: investigate those physical processes that govern the potential sources of fluid and solutes to the river. This included developing a baseline conceptual model for the current conditions in the Fernley area, identifying the origins and sources of high levels of TDS in the groundwater, determining their influence on the TDS loading of the river, and, finally, developing a sophisticated groundwater flow and transport model that could predict the impact of various land-use scenarios on TDS mass loading to the Truckee River.

Bringing all the tools to bear. This map shows where monitoring wells (yellow dots) were placed in irrigated areas (green squares) to sample groundwater heading for the Truckee River. The graphic is an example of how the project involved satellite remote sensing, surface observations, and groundwater monitoring techniques to develop a model of the lower Truckee River recharge system. (Graphic by David McGraw, DRI assistant research hydrologist)

After more than two and a half years of intense field work and complex analysis by DRI, County researchers, and several private consultants, the conclusions suggested a window of opportunity for Washoe County. Groundwater carrying natural mineralization was, indeed, responsible for most of the salinity loading on the lower Truckee River, and, further, a significant portion of that groundwater was being driven by irrigation activities in the river’s watershed.

“This is an outstanding example of ‘science meets policy,’” says McKay. “We’re now working with the County on the next phase to assess the extent of the pollution trading potential identified in those results. If the County acquires enough irrigated acreage and removes it from production, will the associated reduction in high TDS groundwater return provide opportunities for infrastructure expansion in the Truckee Meadows?” This follow-on project is now underway through a collaborative effort that includes DRI and private consultants ECO-Logic and TetraTech.

McKay says the river’s research legacy reveals a piece-meal approach to its various, but related problems. Now, however, he and his fellow researchers would like to “tie it all together, approach it from beginning to end, assessing the hydrology, ecology, and socio-economic aspects of the entire river basin. The goal would be to synthesize all information to provide a better decision-making tool for local and state river management.”

McKay also believes DRI’s Truckee River research has broader implications.

“The Truckee River, all by itself, contains elements of most of the water quality management challenges facing local governments across the western United States. DRI’s experience here can be used to benefit many other communities across this region.”

–John Doherty

Featured in this Issue:

Promoting the General Welfare of the State of Nevada
Tough Land, Tough Choices... Deciding the Fate of Walker Lake
Jacobson Appointed DRI VPAA
Truckee River: Dilution No Longer the Solution to Pollution
DRI's Long History with a Short River
ACES and Clusters Revving Up Environmental Research
DRI's veteran atmospheric modeler anticipates new cluster capabilities
Dr. John J. Warwick Appointed Executive Director of DRI's Hydrologic Sciences Division
GreenPower: Readin', Writin', and Renewable Energy
Grabasnjak Awarded Maxey Fellowship
New Publications from DRI Scientists
DRI Research Foundation Trustee Rudolf Gunnerman Wins Einstein Medal
The 2002 DRI Golf Extravaganza raised over $60,000!
Maki Fellowships Awarded to Rost and Meadows

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