117 research outputs found
Dissolved Nutrients from Submarine Groundwater in Flic en Flac Lagoon, Mauritius
The aim of this study was to investigate dissolved nutrients in a submarine groundwater discharge (SGD) in Flic en Flac lagoon on the west coast of the volcanic island of Mauritius. The SGD enters Flic en Flac lagoon through a thin blanket of unconsolidated sediment through a fracture system and is concentrated along the irregular surface of the buried rock. The results show that the major inputs of dissolved nitrate and phosphate in Flic en Flac lagoon arise from agricultural and domestic sources during periods of heavy rain. Dissolved nitrate (150-470 µg/l) and phosphate (10-115 µg/l) concentrations in the SGD, lagoon and offshore in the Flic en Flac region fell within the range of seawater values in the Pacific region. Rainfall caused dissolved nitrate and phosphate transfer through groundwater conduits in the coralline basement of the lagoon, delivering a significant discharge during the cyclone season in summer. The lagoon is subjected to diffuse SGD flows which may contribute to its high dissolved nutrient values. This will lead to a reduction in the lagoon’s assimilative capacity, exacerbating the problem of excessive nutrient input and associated eutrophication in the lagoon. The submarine groundwater discharge thus merits consideration in Mauritian coastal zone management and similar tropical volcanic lagoonal systems
Assessment of groundwater discharges into West Neck Bay, New York, via natural tracers
Author Posting. © Elsevier B.V., 2006. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Continental Shelf Research 29 (2006): 1971-1983, doi:10.1016/j.csr.2006.07.011.A field experiment to compare methods of assessing submarine groundwater discharge (SGD) was held on Shelter Island, NY, in May 2002. We evaluated the use of radon, radium isotopes, and methane to assess SGD rates and dynamics from a glacial aquifer in the coastal zone. Fluxes of radon across the sediment-water interface were calculated from changes in measured surface water inventories following evaluation and correction for tidal effects, atmospheric evasion, and mixing with offshore waters. These fluxes were then converted to SGD rates using the measured radon concentration in the groundwater. We used the short-lived radium isotopes to calculate a horizontal mixing coefficient to assess radon loss by mixing between nearshore and offshore waters. We also made an independent calculation of SGD using the Ra-derived mixing coefficient and the long-lived 226Ra concentration gradient in the bay. Seepage rates were calculated to range between 0 and 34 cm.day-1 using the radon measurements and 15 cm.day-1 as indicated by the radium isotopes. The radiotracer results were consistent and comparable to SGD rates measured directly with vented benthic chambers (seepage meters) deployed during this experiment. These meters indicated rates between 2 and 200 cm.day-1 depending on their location. Both the calculated radon fluxes and rates measured directly by the automated seepage meters revealed a clear reproducible pattern of higher fluxes during low tides. Considering that the two techniques are completely independent, the agreement in the SGD dynamics is significant. Methane concentration in groundwater was very low (~30 nM) and not suitable as SGD tracer at this study site.The SGD intercomparison experiment was partially funded by SCOR, LOICZ, and UNESCO (IOC and IHP). W. C. Burnett acknowledges support from CICEET (Grant# 1368-810-41) and ONR (Grant# 1368-769-27). J. P. Chanton acknowledges support from Seagrant (R\C-E-44). The WHOI researchers acknowledge funding from CICEET (#NA07OR0351, NA17OZ2507)
Isotope tracing of submarine groundwater discharge offshore Ubatuba, Brazil : results of the IAEA–UNESCO SGD project
Author Posting. © Elsevier B.V., 2008. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Journal of Environmental Radioactivity 99 (2008): 1596-1610, doi:10.1016/j.jenvrad.2008.06.010.Results of groundwater and seawater analyses for radioactive (3H, 222Rn, 223Ra, 224Ra, 226Ra, 228Ra) and stable (2H, 18O)
isotopes are presented together with in situ spatial mapping and time-series 222Rn measurements in seawater, direct seepage
measurements using manual and automated seepage meters, pore water investigations using different tracers and piezometric
techniques, and geoelectric surveys probing the coast. This study represents first time that such a new complex arsenal of radioactive
and non-radioactive tracer techniques and geophysical methods have been used for simultaneous submarine groundwater discharge
(SGD) investigations. Large fluctuations of SGD fluxes were observed at sites situated only a few meters apart (from 0 cm d-1 to 360
cm d-1; the unit represents cm3/cm2/day), as well as during a few hours (from 0 cm d-1 to 110 cm d-1), strongly depending on the tidal
fluctuations. The average SGD flux estimated from continuous 222Rn measurements is 17±10 cm d-1. Integrated coastal SGD flux
estimated for the Ubatuba coast using radium isotopes is about 7x103 m3 d-1 per km of the coast. The isotopic composition (δ2H and
δ18O) of submarine waters was characterised by significant variability and heavy isotope enrichment, indicating that the contribution
of groundwater in submarine waters varied from a small percentage to 20%. However, this contribution with increasing offshore
distance became negligible. Automated seepage meters and time-series measurements of 222Rn activity concentration showed a
negative correlation between the SGD rates and tidal stage. This is likely caused by sea level changes as tidal effects induce variations of hydraulic gradients. The geoelectric probing and piezometric measurements contributed to better understanding of the spatial distribution of different water masses present along the coast. The radium isotope data showed scattered distributions with offshore distance, which imply that seawater in a complex coast with many small bays and islands was influenced by local currents and
groundwater/seawater mixing. This has also been confirmed by a relatively short residence time of 1-2 weeks for water within 25 km
offshore, as obtained by short-lived radium isotopes. The irregular distribution of SGD seen at Ubatuba is a characteristic of fractured
rock aquifers, fed by coastal groundwater and recirculated seawater with small admixtures of groundwater, which is of potential
environmental concern and has implications on the management of freshwater resources in the region.This research was
supported by IAEA and UNESCO (IOC and IHP) in the framework of the joint SGD project.
Science support for some U.S. investigators was provided by grants from the National Science
Foundation (OCE03-50514 to WCB and OCE02-33657 to WSM)
Microscopic theory of atom-molecule oscillations in a Bose-Einstein condensate
In a recent experiment at JILA [E.A. Donley et al., Nature (London) 417, 529
(2002)] an initially pure condensate of Rb-85 atoms was exposed to a specially
designed time dependent magnetic field pulse in the vicinity of a Feshbach
resonance. The production of new components of the gas as well as their
oscillatory behavior have been reported. We apply a microscopic theory of the
gas to identify these components and determine their physical properties. Our
time dependent studies allow us to explain the observed dynamic evolution of
all fractions, and to identify the physical relevance of the pulse shape. Based
on ab initio predictions, our theory strongly supports the view that the
experiments have produced a molecular condensate.Comment: 18 pages, 20 figure
Isotopic, geophysical and biogeochemical investigation of submarine groundwater discharge : IAEA-UNESCO intercomparison exercise at Mauritius Island
Author Posting. © The Author(s), 2011. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Journal of Environmental Radioactivity 104 (2012): 24-45, doi:10.1016/j.jenvrad.2011.09.009.Submarine groundwater discharge (SGD) into a shallow lagoon on the west coast of Mauritius Island (Flic-en-Flac) was
investigated using radioactive (3H, 222Rn, 223Ra, 224Ra, 226Ra, 228Ra) and stable (2H, 18O) isotopes and nutrients. SGD
intercomparison exercises were carried out to validate the various approaches used to measure SGD including radium and radon
measurements, seepage-rate measurements using manual and automated meters, sediment bulk conductivity and salinity surveys.
SGD measurements using benthic chambers placed on the floor of the Flic-en-Flac Lagoon showed discharge rates up to 500
cm/day. Large variability in SGD was observed over distances of a few meters, which were attributed to different
geomorphological features. Deployments of automated seepage meters captured the spatial and temporal variability of SGD with
a mean seepage rate of 10 cm/day. The stable isotopic composition of submarine waters was characterized by significant
variability and heavy isotope enrichment and was used to predict the contribution of fresh terrestrially derived groundwater to
SGD (range from a few % to almost 100 %). The integrated SGD flux, estimated from seepage meters placed parallel to the
shoreline, was 35 m3/m day, which was in a reasonable agreement with results obtained from hydrologic water balance
calculation (26 m3/m day). SGD calculated from the radon inventory method using in situ radon measurements were between 5
and 56 m3/m per day. Low concentrations of radium isotopes observed in the lagoon water reflected the low abundance of U and
Th in the basalt that makes up the island. High SGD rates contribute to high nutrients loading to the lagoon, potentially leading to
eutrophication. Each of the applied methods yielded unique information about the character and magnitude of SGD. The results
of the intercomparison studies have resulted a better understanding of groundwater-seawater interactions in coastal regions. Such
information is an important pre-requisite for the protection management of coastal freshwater resources.The
financial support provided by the IOC and IHP of UNESCO for travel arrangements, and by the IAEA’s Marine
Environment Laboratories for logistics is highly acknowledged. MAC and MEG were supported in part by the US
National Science Foundation (OCE-0425061 and OCE-0751525). PPP acknowledges a support provided by the EU
Research & Development Operational Program funded by the ERDF (project No. 26240220004), and the Slovak
Scientific Agency VEGA (grant No. 1/108/08). The International Atomic Energy Agency is grateful to the
Government of the Principality of Monaco for support provided to its Marine Environment Laboratories
Search for the associated production of a b quark and a neutral supersymmetric Higgs boson which decays to tau pairs
We report results from a search for production of a neutral Higgs boson in
association with a quark. We search for Higgs decays to pairs with
one subsequently decaying to a muon and the other to hadrons. The data
correspond to 2.7fb of \ppbar collisions recorded by the D0 detector
at TeV. The data are found to be consistent with background
predictions. The result allows us to exclude a significant region of parameter
space of the minimal supersymmetric model.Comment: Submitted to Phys. Rev. Letter
Enhancing quantitative approaches for assessing community resilience
Scholars from many different intellectual disciplines have attempted to measure, estimate, or quantify resilience. However, there is growing concern that lack of clarity on the operationalization of the concept will limit its application. In this paper, we discuss the theory, research development and quantitative approaches in ecological and community resilience. Upon noting the lack of methods that quantify the complexities of the linked human and natural aspects of community resilience, we identify several promising approaches within the ecological resilience tradition that may be useful in filling these gaps. Further, we discuss the challenges for consolidating these approaches into a more integrated perspective for managing social-ecological systems
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