St. Croix Research

San Jose, CA, United States

St. Croix Research

San Jose, CA, United States
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Almendinger J.E.,St. Croix Research | Ulrich J.S.,University of Minnesota
Journal of the American Water Resources Association | Year: 2017

Phosphorus export coefficients (kg/ha/yr) from selected land covers, also called phosphorus yields, tend to get smaller as contributing areas get larger because some of the phosphorus mobilized on local fields gets trapped during transport to regional watershed outlets. Phosphorus traps include floodplains, wetlands, and lakes, which can then become impaired by eutrophication. The Sunrise River watershed in east central Minnesota, United States, has numerous lakes impaired by excess phosphorus. The Sunrise is tributary to the St. Croix River, whose much larger watershed is terminated by Lake St. Croix, also impaired by excess phosphorus. To support management of these impairments at both local and regional scales, a Soil and Water Assessment Tool (SWAT) model of the Sunrise watershed was constructed to estimate load reductions due to selected best management practices (BMPs) and to determine how phosphorus export coefficients scaled with contributing area. In this study, agricultural BMPs, including vegetated filter strips, grassed waterways, and reduction of soil-phosphorus concentrations reduced phosphorus loads by 4-20%, with similar percentage reductions at field and watershed spatial scales. Phosphorus export coefficients from cropland in rotation with corn, soybeans, and alfalfa decreased as a negative power function of contributing area, from an average of 2.12 kg/ha/yr at the upland field scale (~0.6 km2) to 0.63 kg/ha/yr at the major river basin scale (20,000 km2). Editor's note: This paper is part of the featured series on SWAT Applications for Emerging Hydrologic and Water Quality Challenges. See the February 2017 issue for the introduction and background to the series. © 2017 American Water Resources Association.

Lamborg C.H.,Woods Hole Oceanographic Institution | Engstrom D.R.,St. Croix Research | Fitzgerald W.F.,University of Connecticut | Balcom P.H.,University of Connecticut
Science of the Total Environment | Year: 2013

Our previous work has documented a correlation between Hg concentrations and 210Pb activity measured in wet deposition that might be used to help apportion sources of Hg in precipitation. Here we present the results of a 27-month precipitation collection effort using co-located samplers for Hg and 210Pb designed to assess this hypothesis. Study sites were located on the east and west coasts of North America, in the continental interior, and on the Florida Peninsula. Relatively high variability in Hg/210Pb ratios was found at all sites regionally and seasonally (e.g., overall: 0.99-9.13ngdpm-1). The ratio of average volume-weighted Hg concentrations and 210Pb activities showed consistent trends (higher in impacted area), with Glacier Bay in southeast Alaska, exhibiting the lowest value. Assuming that Glacier Bay represents a benchmark for a site with no regional contribution, we estimate less than 50% of the Hg input was "global" at the Seattle and Florida sites. Differences in Hg/210Pb in wet deposition could be due to either a regional/local source contribution of Hg, or a regional/local enhancement in the removal of Hg from the atmosphere (i.e., oxidants), however, this approach is not capable of discerning between these two possibilities. Thus, this method of source apportionment represents an estimate of the maximal amount of Hg contributed by regional sources and may be limited in regions of deep convective mixing. © 2012 Elsevier B.V.

Siver P.A.,Connecticut College | Wolfe A.P.,University of Alberta | Edlund M.B.,St. Croix Research
Plant Ecology and Evolution | Year: 2010

Background and aims - The majority of freshwater diatom lineages appear to have evolved before or during the Eocene, with rapid radiation occurring in the Miocene. However, only a few accurately dated fossil localities are available to test this assertion, resulting in an overall poor understanding of the biostratigraphy and early evolution of these organisms. Exquisitely preserved diatoms have been uncovered from Eocene lake sediments deposited post-eruptively in the Giraffe kimberlite pipe (Northwest Territories, Canada). We describe three new pennate diatoms from this deposit and discuss their evolutionary implications. Methods - Both oxidized preparations and whole-rock mudstone samples from the Giraffe Pipe core were examined with light and scanning electron microscopy for diatom remains. Key results - Species belonging to the genera Actinella F.W.Lewis, Oxyneis Round and Nupela Vyverman & Compere are described from the Giraffe Pipe sediments. Oxyneis apporrecta is a unique species with valves that are centrally constricted, infations midway between the center and apices, and protracted and rostrate apices. Actinella giraffensis is a small taxon that lacks a highly complex head pole, and is most closely related to a species known today only from the highlands of New Zealand. Nupela mutabilis has variably shaped valves possessing a raphe and unique areolae characteristic of this genus. These fndings represent the first known fossils for both Oxyneis and Nupela, and the oldest record for Actinella. Conclusions - None of the species are known from extant foras and are therefore considered extinct. However, the morphological features they present, including the structure of the areolae, raphe, rimoportula and girdle bands, share pronounced affinities with modern congeneric taxa. The well-developed raphe found on Nupela mutabilis confrms that the evolution of this structure dates to at least the Middle Eocene, and supports the hypothesis that it may be older than the Paleocene. © 2010 National Botanic Garden of Belgium and Royal Botanical Society of Belgium.

Reavie E.D.,University of Minnesota | Edlund M.B.,St. Croix Research
Journal of Paleolimnology | Year: 2013

Paleolimnological information is often extracted from diatom records using weighted averaging calibration and regression techniques. Larger calibration sample sets yield better inferences because they better characterize the environmental characteristics and species assemblages of the sample region. To optimize inferred information from fossil assemblages, however, it is worth knowing if fewer calibration samples can be used. Furthermore, confidence in environmental reconstructions is greater if we consider the relative importance of (A) similarity between fossil and calibration assemblages and (B) how well fossil taxa respond to the environmental variable of interest. We examine these issues using ~200-year sediment profiles from four Minnesota lakes and a 145-lake surface sediment training set calibrated for total phosphorus (TP). Training set sample sizes ranging from 10 to 145 were created through random sample selection, and models based on these training sets were used to calculate diatom-inferred (DI) TP data from fossil samples. Relationships between DI-TP variability and sample size were used to determine the minimum sample size needed to optimize the model for paleo-reconstruction. Similarly, similarities between fossil and modern assemblages were calculated for each size training set. Finally, fossil and modern assemblages were compared to determine whether older fossil samples had poorer similarity with modern analogs. More than 50-80 samples, depending on lake, were needed to stabilize variability in DI-TP results, and >110 training set samples were needed to minimize modern-fossil assemblage dissimilarities. Dissimilarities appeared to increase with sample age, but only one of the four studied cores displayed a significant trend. We have two recommendations for future studies: (1) be cautious when dealing with smaller training sets, especially if they are used to interpret older fossil assemblages and (2) understand how well fossil taxa are attuned to the variable of interest, as it is critical to evaluating the quality of the diatom-inferred data. © 2013 Springer Science+Business Media Dordrecht.

Anderson N.J.,Loughborough University | Dietz R.D.,University of Minnesota | Engstrom D.R.,St. Croix Research
Proceedings of the Royal Society B: Biological Sciences | Year: 2013

Lakes are a central component of the carbon cycle, both mineralizing terrestrially derived organic matter and storing substantial amounts of organic carbon (OC) in their sediments. However, the rates and controls on OC burial by lakes remain uncertain, as do the possible effects of future global change processes. To address these issues, we derived OC burial rates in 210Pb-dated sediment cores from 116 small Minnesota lakes that cover major climate and land-use gradients. Rates for individual lakes presently range from 7 to 127 g C m-2 yr-1 and have increased by up to a factor of 8 since Euro-American settlement (mean increase: 2.8). Mean pre-disturbance OC burial rates were similar (14-22 g C m-2 yr-1) across all land-cover categories (prairie, mixed deciduous and boreal forest), indicating minimal effect of the regional temperature gradient (approx. 48C) on background carbon burial. The relationship between modern OC burial rates and temperature was also not significant after removal of the effect of total phosphorus. Contemporary burial rates were strongly correlated with lake-water nutrients and the extent of agricultural land cover in the catchment. Increased OC burial, documented even in relatively undisturbed boreal lake ecosystems, indicates a possible role for atmospheric nitrogen deposition. Our results suggest that globally, future land-cover change, intensification of agriculture and associated nutrient loading together with atmospheric N-deposition will enhance OC sequestration by lakes. © 2013 The Author(s) Published by the Royal Society. All rights reserved.

Engstrom D.R.,St. Croix Research | Rose N.L.,University College London
Journal of Paleolimnology | Year: 2013

Lake sediments record the flux of materials (nutrients, pollutants, particulates) through a lake system both qualitatively, as changes in the composition of geochemical and biological tracers, as well as quantitatively, through changes in their rate of burial. Burial rates provide a direct link to contemporary (neo-) limnological studies as well as management efforts aimed at load reductions, but are difficult to reconstruct accurately from single cores owing to the spatial and temporal variability of sediment deposition in most lakes. The accurate determination of whole-lake burial rates from analysis of multiple cores, though requiring more effort per lake, can help resolve such problems and improve our understanding of sediment heterogeneity at multiple scales. Partial solutions to these problems also include focusing corrections based on 210Pb flux, co-evaluation of concentration profiles, trend analysis using multiple lakes, and trend replication based on a small number of cores from the same lake. Recent multi-core studies demonstrate that no single core site faithfully records the whole-lake time-resolved input of materials, but that as few as five well-placed cores can provide a reliable record of whole-lake sediment flux for morphometrically simple basins. Lake-wide sediment fluxes can be coupled with reconstructed outflow losses to calculate historical changes in watershed and atmospheric loading of nutrients, metals, and other constituents. The ability of paleolimnology to accurately assess the sedimentary flux and extend the period of reference into the distant past represents an important contribution to the understanding of biogeochemical processes and their response to human and natural disturbance. © 2013 Springer Science+Business Media Dordrecht.

Yang H.,University College London | Engstrom D.R.,St. Croix Research | Rose N.L.,University College London
Environmental Science and Technology | Year: 2010

We analyzed sediment cores collected from three equatorial zone lakes in the Rwenzori Mountains of Uganda for Hg and dated them using 210Pb. The results show that the lakes have been contaminated by anthropogenic Hg from atmospheric deposition and that the onset of Hg pollution in the region began at least by the late 19th century. Mercury accumulation in all sediment cores increased by about 3-fold since the mid-19th century, a similar increase to that shown in other remote regions worldwide. These results from tropical high-elevation sites are the first for this region and contribute to our understanding of global Hg pollution trends. The atmospheric boundary layer is at a higher altitude in equatorial areas than at midlatitudes, and therefore, Hg deposition in these regions may not be enhanced by diurnal penetration of tropospheric air and associated reactive gaseous mercury as has been reported for mountain lakes at higher latitudes. Furthermore, the relatively low abundance of atmospheric oxidants may limit the amount of gaseous elemental mercury oxidized to the reactive gaseous form in equatorial Africa. These Rwenzori Hg records therefore have important implications for the understanding of Hg dynamics at high elevations in equatorial regions. © 2010 American Chemical Society.

Juggins S.,Northumbria University | Anderson N.J.,Loughborough University | Hobbs J.M.R.,St. Croix Research | Heathcote A.J.,Iowa State University
Journal of Paleolimnology | Year: 2013

Diatoms respond rapidly to eutrophication and diatom-based models for inferring total phosphorus (TP) have found wide application in palaeolimnology, especially in tracking trajectories of past and recent nutrient enrichment and in establishing pre-disturbance targets for restoration. Using new analysis of existing training sets and sediment-cores we examine the statistical and ecological constraints of diatom-inferred TP (DI-TP) models. Although the models show an apparently strong relationship between measured and inferred TP in the training sets, even under cross-validation, the models display three fundamental weaknesses, namely (1) the relationship between TP and diatom relative abundance is heavily confounded with secondary variables such as alkalinity and lake depth, (2) the models contain many taxa that are not significantly related to TP, and (3) comparison between different models shows poor or no spatial replicability. At some sites the sediment-core diatom assemblage change tracks the TP gradient in the training sets and DI-TP reconstructions are consistent with monitored TP data and known catchment histories for the recent past. At others diatom species turnover is apparently related to variables other than TP, and DI-TP fails to even reproduce plausible trends. Pre-disturbance DI-TP values are also questionable at most sites. We argue that these problems pervade many DI-TP models, particularly those where violations of the basic assumptions of the transfer function approach are ignored. © 2013 Springer Science+Business Media Dordrecht.

Agency: National Aeronautics and Space Administration | Branch: | Program: SBIR | Phase: Phase I | Award Amount: 99.52K | Year: 2009

This project will develop a practical method for predicting pattern roughness onset and quantitative effects on heat and mass transfer rates for heatshield materials such as Phenolic Impregnated Carbon Ablator (PICA) and environments such as those anticipated for the Crew Exploration Vehicle (CEV). Surface roughness patterns (e.g., scallops, crosshatching) form on many materials ablating under turbulent flow conditions. Equivalent sand grain roughness models are inaccurate and inappropriate for calculating Stanton numbers. In Phase I, we will develop a near-term method based on pattern roughness data, observations, and models from diverse fields. This method may predict Stanton number increases directly from material and aerothermal environment information instead of sequentially predicting pattern dimensions, equivalent roughness height, and Stanton number effects. We will also plan a more rigorous longer-term model and validation tests to be implemented in Phase II.

Agency: Department of Defense | Branch: Navy | Program: SBIR | Phase: Phase I | Award Amount: 79.99K | Year: 2013

This project will develop and demonstrate a high-temperature ceramic-coated tungsten nosetip for hypervelocity projectiles. The ceramic coating will delay oxidation, which causes increased surface roughness, boundary layer transition, much higher heat transfer rates, and substantial ablation of tungsten and carbon-carbon materials. If laminar flow over the nosetip can be maintained, tungsten"s properties enable it to heat-sink the incident aerodynamic heating and avoid ablation for the Mach 8 launch condition of interest. Development of the ceramic material and coating process will build on our prior ceramic-coated tungsten experience. Phase I will include fabrication and characterization of oxidation-resistant ceramic coated tungsten nosetip specimens.

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