March-April 2009

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River Restoration, Done Right (and Wrong)

Saving water to relieve an aquifer, conserve a river, reintroduce its fish, and preserve a community’s quality of life

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Photo: Andy Fisher

By David Engle

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That movie title, “A River Runs Through It,” would make a pretty good one for the story that follows, especially if you take the words literally. In the film, the river courses through rustic mountain vales of the Rockies as it also runs through the lives of fly-fishing young men and their dad. In the admittedly more prosaic account that follows here, the river is not really a metaphor of coming of age, but the tale of a hydrologically complex water usage challenge. It might easily have become a regulatory and economic nightmare as well. This actually did occur, notoriously, in a river basin nearby. Fortunately—in part, because that earlier fiasco was so instructive—the rough events did not recur.

Now, the “it” that the river runs through is not the life of a fictional character, but a striking geologic feature: a deep bed of rocky volcanic basalt, hundreds of feet thick. “Through it,” the river in this story does not run so much as it seeps, at an alarmingly rapid pace, as through a rocky, multi-story sieve. Far below, it eventually pools into a subterranean aquifer: a sort of second underwater river or lake. The unusual vertical “trickle-down” terrain presents the surrounding rural region of about 200,000-plus people, one piece of a daunting puzzle of how to integrate water usage, conservation, and apportionment.

The challenge actually begins with the arcane task of scientifically defining the geologic characteristics. This is necessitated, not so much for attaining knowledge, but to marshal facts in high-profile legal water-rights battles. These have been fought out, so far, across several state supreme courts. Being a vital economic and political challenge, this puzzle morphs into a shared, communitywide enterprise.

In both stories, a river meanders in high mountain canyons. Adventuring boaters catch sight of evergreens and snow-capped mountain peaks. Our river is the Deschutes, in Central Oregon—named for its dramatic chutes or churning rapids, which make it a mecca for whitewater enthusiasts. These and other regional attractions have also been drawing new residents at a spectacular rate: Over the past three-plus decades, local population has grown four-fold. As of the mid 2000s, the US Census Bureau ranked Deschutes County as the fastest growing in Oregon, and twenty-ninth fastest in the nation.

During the decades of explosive growth, accommodating the many claims became increasingly challenging. A very obvious, and somewhat painful, visual reminder of this was the river itself and its tributary flows. Once known for their unfailing gurgling chutes, these have lately shriveled here and there at a worrying pace, into meekly murmuring trickles.

As for the river’s sustaining role, the Deschutes and tributaries support seven irrigation districts, a Central Oregon Cities Organization consisting of nine cities (the largest being Bend, population 60,000) and affiliated drinking water suppliers, the Confederated Tribes of Warm Springs, scattered towns, and farming. All of the cities, towns, farms, and tribes collectively enjoy specific water rights to the Deschutes, its tributaries, or aquifer below.

Photos: Andy Fisher
Agriculturally, a 2002 census reports that 1.77 million acres of this basin are given to farming and livestock; roughly one-tenth is irrigated. Family farms predominate—but most of these draw income from non-farm sources. Deschutes County proper notes one resident involved in its river “is largely home to lifestyle or hobby farming, with just a few areas remaining of large commercial farms,” says Bruce Aylward, Ph.D, director of Ecosystem Economics LLC. For most of the past decade, Aylward has been closely involved in local water, conservation, and biodiversity issues.

Conflicts between cities and environmentalists over how to balance growth with preservation have simmered for years, notes Aylward. Historically, growth has surged with relative little restraint. “Given that we have this system of water rights, it works pretty well for water users, but hasn't worked as well for the environment,” he says.

Concurring is Steve Johnson, district secretary and manager for the Central Oregon Irrigation District (COID), who points out, “This is a common story all over the West—and in the world. There’s increasing demand for water [both for human consumption and in food production], and, at the same time, there’s the question of how to protect, preserve, and sustain the environment—and especially the aquatic systems.”

In early days of Western settlement, the US government built dams to foster farming. States then apportioned water rights to users, and, even all these years later, notes Johnson, “Agriculture still commands about 80% to 90% of water flows,” despite dramatically changing land use and quadrupling newcomers. “So, where does that leave the cities and fish?” he asks.

Johnson’s COID residential users draw little or nothing from river, but do tap the aquifer—to which the river is hydrostatically connected.

Herein lies the heart of local problems. 

Conflicts over this connectedness and its consequences came to a head in the mid-1990s, when surging growth necessitated that Bend seek more groundwater. This was answered briskly with a legal writ from WaterWatch of Oregon (WWO). WWO aims, per its mission statement, to “protect and restore flows” to waterways and to “sustain the native fish, wildlife, and the people who depend on healthy rivers.” (www.waterwatch.org)

Photos: Bea Arnstrong
The Swalley Irrigation District Main Canal Piping Project alone will put four times more water back into the Deschutes River than any other project to date.
The core issue here is thus a scientific one: Why should siphoning aquifer hurt the river? Literally “underlying” the hydrology is a physical relationship between the Deschutes’ flow along its bed, and a water table below. Despite the intervening rock–up to 900 feet thick, in some places, Johnson notes—it turns out that, as water is extracted from that deep pool, flows of the river belatedly decrease. The relationship is intuitively perhaps hard to accept. Besides the great physical separation, the voluminous aquifer itself is so huge that, as Aylward says, “the total amount being pumped out [for home use regionwide] is barely measurable”—something like 1.8% of the whole.

This seemed paltry and not worth fighting over. Yet, the physical reality of an alarming impact on surface flows is undeniable. Aylward elaborates on the connectedness as being “linked to the pressure that draws the river down through its rocky substrate. It’s a fairly obvious hydrologic fact, and legal fact, that groundwater is connected to surface water,” he says. “But the impact is definitely less obvious here than in other places”—which he has toured in his professional work.

In the Deschutes, specifically, “if you pull water today, there’s less water in stream three days later—something that has been understood, but [until fairly recently] was not scientifically calculated,” he adds.

With the WaterWatch case in the docket, hydrologists from the US Geological Survey were summoned as experts to investigate the linkage, confirm it scientifically, and, if possible, suggest equitable solutions. The eventual findings fully upheld the WWO claim.

As Aylward recounts, the case eventually landed in the Oregon Supreme Court. After the victory, the state legislature then codified the river-to-aquifer relationship as law. This “was sort of the first necessary step towards developing sustainable surface and groundwater management in Oregon,” he says. “And once the law was passed, there was nothing else to fight.” Similar cases, he adds, have subsequently hit the supreme courts of Idaho and Montana as well.

In this case again, Oregon’s legislative solution, although technically somewhat complex, embodies a simple principle: Pumping water out of the aquifer impacts the river above, even though the actual diminishment may be long delayed. As a fairly straightforward legal solution for aquifer-tapping cities, he says the statute requires that, “You don’t have to worry about when that mitigation water needs to be put in the stream,” you merely have to account for “how much did you pull all year long? And then you go and acquire the water from irrigators [for replenishment]. And then you leave it in stream in the summer.”

As a threshold for determining at what point extraction must be compensated by mitigation, Oregon sets a fairly low impact level of just 1 cubic foot per second (cfs) or 1%, whichever is less, Aylward adds. Bottom line: If a city needs to drink from the aquifer, it must somehow obtain irrigation water from farmers for replenishment—and return it to the river.

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Creating a Water Alliance
Thus, from the necessity for cooperation arose the idea of creating an informal Deschutes Water Alliance (DWA). A precursor of this ad hoc group, the non-profit Deschutes River Conservancy (DRC), had already been in the business of river-flow restoration since the mid-1980s, and so the DRC provided a ready umbrella structure for the DWA, notes DRC’s executive director Tod Heisler.

Whenever the subject of Oregon and water conflict arises, it’s probably impossible not to think of what has been happening, during this same period, in nearby Klamath. The allusion to that river came up in several discussions, in comparing the legal battle in Deschutes. Each time, the tone of voice is lowered, as when one speaks of a somber or regrettable episode—Klamath. In local parlance, it is almost synonymous with a water management fiasco and worst-case outcome.  Next Page >

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