Equipment
The SCWRS provides direct river access and a small fleet of boats, outboard motors, and trailers. Our vessels include an 18-foot jon boat, a 12-foot lightweight rowboat, a Zodiac inflatable two-person boat, and two 17-foot aluminum canoes.
Standard limnological equipment is available, including field meters and samplers for water, plankton, and benthos, plus two GPS units compatible with laptop PCs. Specialized hydrological monitoring equipment includes data loggers, piezometers, and well-leveling potentiometers.
Sediment coring equipment features gravity corers, Livingstone corers, surface piston corers, and over 70 meters of lightweight magnesium-zirconium drive rod. An automated weather station provides continuous meteorological data downloadable via modem.
TAPwaters
The Technical Assistance Program for Watersheds (TAPwaters) uses GIS and hydrological modeling technology to advance watershed research and management. Located in the Spring Creek annex, the TAPwaters office features two high-end workstations, a 4×5-ft. digitizing tablet, and a 54-inch wide-format plotter. A key objective is producing watershed models for St. Croix River tributaries and eventually building a basin-wide model to provide regional context for managing nutrient and sediment loads.
St. Croix Laboratory
SCWRS laboratories analyze various environmental samples, primarily sediment and water. Procedures range from sediment loss on ignition to nutrient analyses, Lead-210 dating, and radioisotopic analyses of soils and sediments.
The main laboratory includes standard equipment: fume hoods, oven, furnace, analytical balances, pH meter, centrifuge, platform shaker, shaking water bath, water purification system, and walk-in cold room. Equipment is available on a per-day or per-sample basis.
Specialized analytical equipment includes a Lachat automated ion analyzer, Dionex DX-100 Ion Chromatograph, Phoenix 8000 UV persulfate carbon analyzer (with solids attachment), UV-Vis spectrophotometer, and bulk freeze dryer. We operate a lead-210 lab with alpha spectrometers for sediment dating and a gamma spectrometry lab for radioisotope tracer analysis. This equipment is available on a limited basis with set-up, per-sample, and waste disposal fees, provided SCWRS analysts perform the analyses.
A fee schedule for analyses, laboratory use, and research services is available.
Facilities
The radiometric dating laboratory at the St. Croix Watershed Research Station is equipped with an EG&G Nuclear alpha spectrometry system (24 detectors), polonium distillation equipment, and 209Po and 210Pb standards. This capacity allows one to two lake sediment or peat cores to be dated each week. In addition, the Station has two EG&G Nuclear ultra-low background gamma spectrometers (well-detectors) for measurement of environmental levels of 137Cs, 7Be, 226Ra, and 210Pb by non-destructive direct gamma assay. The SCWRS dating labs are in near-continuous use for both “in-house” and outside research projects. More than 1,000 cores have been dated for research projects involving 100 institutions and university departments since 1996.
Microscopy Lab
Four carrels with research-grade stereo and compound microscopes with digital imaging are available. Current equipment includes a Leica dissecting scope, Nikon compound scope, and three Olympus compound scopes with phase, darkfield, brightfield, or nomarski capabilities. Cameras and computer interfaces are available. Equipment is subject to availability.
Sediment Dating
Lake sediments and peat cores are essential for studying environmental history, with accurate chronology being critical. Cores are dated to establish the timing of past environmental change and determine material accumulation (sediment, pollutants, micro-fossils) in lakes or wetlands.
Lead-210 Dating
For studies of human impacts (e.g. pollution, eutrophication, erosion), which typically focus on the last 100-200 years, the dating method of choice is 210Pb. Lead-210 is a naturally occurring radioisotope in the 238U-decay series formed by decay of 226Ra, and the subsequent evasion of the intermediary 222Rn (an inert gas) from the earth’s surface. Radon-222 decays through a series of short-lived daughters to 210Pb which is stripped from the atmosphere in precipitation and accumulates in lake sediments and wetlands where it decays away with a half-life of 22 years. Cores are typically dated by analyzing a series of stratigraphic levels from the core surface to a depth where unsupported 210Pb is no longer measurable (roughly 5-8 half-lives). From the resulting 210Pb profile, dates are calculated according to one of several mathematical models that make assumptions regarding the accumulation of 210Pb and sediment at the core site.
Cesium-137 Dating
Additional dating markers should be sought whenever possible to validate the 210Pb chronology. This is especially critical for sites with disturbed watersheds and highly variable sedimentation rates, which are more prone to errors in 210Pb dating. Among the most important of these ancillary dating tools is 137Cs, which provides maker horizons for the 1964 peak from atmospheric nuclear testing and, in Europe, the 1986 peak from the Chernobyl nuclear accident.