July-August 2000

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Going for Green: Creating a Prairie on New Ground

The closure of an old landfill in a new wildlife management area created an opportunity to study whether a native prairie could be created on imported landfill-cover soils previously seeded with exotic grasses for erosion control.

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By Martha S. Mitchell

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A green canoe cuts quietly through the slack water at the edge of a 2,000-ac. wetland wildlife park where volunteers are surveying the Western painted turtle. As the canoe moves through the dappled shade of Pacific willow at the water's edge, its approach is heralded by the clumsy departure of a great blue heron and the plop of turtles diving for cover. Around a bend, an adult bald eagle and a splotchy juvenile take flight from a cottonwood where they have been keeping an eye on a group of coots. The canoe beaches below a rolling grassland where the shoreline of the fringing riparian woodland is embroidered with the tracks of mink, otter, beaver, Canada goose, muskrat, and raccoon. The soft whistle of a Northern harrier comes from overhead, and cottonwood fuzz drifts on small breaths of warming air.

Flash back half a century. The squalls of gulls and other scavenging birds carry over the open water at the edge of an expanding dump. The site that today is a rolling grassland was a remote swamp at the edge of town where ash from the Portland, OR, area's garbage incinerator was disposed along with every other kind of waste that would not burn. This was not an unusual garbage-disposal practice for the time. But the setting was unusual, for the dump is situated in the floodplain of the lower Columbia River, a stream that drains some 259,000 mi.2 of the Pacific Northwest. This big-league river tumbles out of the Rockies, slices west through the Cascade Range, and sprawls mile-wide into a watery bottomland shared by the Willamette River, creating a riverscape studded with islands, sloughs, and backwater channels. The dump is located in this setting.

Fast forward to the early 1990s. In the years since 1934, St. Johns Landfill has grown to about 250 ac. and is surrounded on all sides by remnant lakes and wetlands of the once-extensive floodplain. These floodplain remnants have been set aside as a regional wildlife park, and the landfill comprises its upland habitat. The regional government, Metro, has acquired the landfill, closed it, started to cap it, and initiated studies to learn whether it will be possible to establish native prairie grasses and shrubs on the manmade slopes.

The Landfill Cap: Functional Requirements

The cap is a layer cake of materials stacked to provide performance not usually required of either natural or human-influenced landscapes. According to Metro's landfill closure plan, the cap must prevent rainwater from seeping into the waste and leaching pollutants into ground and surface water. There can be no ponding of water on the surface, and slopes after settlement must be steep enough to facilitate rapid stormwater drainage. Runoff should not erode the cap. Trees should not be allowed to become established because of the potential for their root systems to damage a subsurface geomembrane that seals the waste beneath. Plants that might support burrowing animals should be avoided for the same reason.

Arial view of former Slandfill area
After a half century as a garbage dump in the floodplain of the Columbia River, the closed 250-ac. St. Johns Landfill became critical habitat in a wildlife management area.

To accomplish these objectives, explains Dennis O'Neil, Metro's landfill manager, the waste was surcharged where necessary to promote settlement and covered with a minimum 6-in. lift of soil that was compacted to achieve low permeability. A 40- to 60-mil welded geomembrane was placed over the compacted soil to serve as a barrier to rainwater from above and gas from below. A 12- to 18-in. layer of sand on top of the geomembrane served as a medium to allow for rooting depth and for the drainage of any rainwater percolating through the topsoil. On steep slopes, a composite of geotextile and drainage mat was placed between the sand and the membrane to facilitate drainage.

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Mark Wilson, a Portland restoration ecologist, led a team to design and oversee the implementation of a landfill-cover vegetation plan. For the top soil layer, Wilson mixed several lifts of soil and compost into the top few inches of the sand layer. The cover-soil depths were designed to vary with landscape position. The nearly flat ridgetops were to be seeded with mesic prairie, the slopes with xeric prairie, and the valley bottoms with a combination of shrubs and mesic prairie. This was the planting medium to be tested in experimental plots on the final landfill cover.

Project economics, soil recycling objectives, and construction deadlines made the acquisition of seed-free topsoil impossible, reports O'Neil. After placement, seedbank tests of the imported soils used for the uppermost soil layer identified huge quantities of non-native grass and pest seeds, he noted in a 1997 report. According to Wilson and Laura Brophy (www.peak.org/~brophyl), another ecologist who worked on the project, an additional problem was a large soil seedbank of perennial rye grass, bent grass, and clover in the recycled soils used for the cover. These aggressive non-natives were legacies of temporary erosion control seeding carried out in the late 1980s during the course of landfill closure. Next Page >

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