Design and application of a semi-automated filtration system to study the distribution of particulate organic carbon in the water column of a coastal upwelling system     

Rachel R. Holser  Miguel A. Goni  Burke Hales 《Marine Chemistry》2011,123(1-4):67-77

The processes controlling the production, transport and ultimate fate of particulate organic carbon (POC) in marine systems play a major role in the global carbon cycle. Direct measurements of POC concentrations in oceanic waters have been used extensively to investigate these processes, but because of the time-intensive effort associated with manual collection and filtration of water samples, this approach often results in limited temporal or spatial coverage. To increase the frequency of POC measurements, we designed and built a semi-automated filtration system (SAFS) that can be linked to a ship's underway surface water flow system and/or a towed profiling vehicle with pumping capabilities. Our results show that, compared to manual filtration, SAFS provides the ability to easily perform filtrations at high enough frequency to measure POC concentrations at spatial and temporal resolutions that are closer to those possible with in situ sensors. When combined with optical measurements, SAFS allows for the characterization of several distinct pools of particles within different geographical and depth regions of the water column off the Oregon Coast. These initial applications yielded data that provide considerable insight into the sources and character of particles in the water column and prove that this approach can be used to gain valuable information on the biogeochemistry of this and other similar ocean margins.  相似文献   

Chemical evolution of shallow playa groundwater in response to post-pluvial isostatic rebound, Honey Lake Basin, California–Nevada, USA     

Alan L. Mayo  Rachel M. Henderson  David Tingey  William Webber 《Hydrogeology Journal》2010,18(3):725-747

The 1,750-km² endorheic Honey Lake basin (California–Nevada, USA) was part of the 22,000-km² Pleistocene Lake Lahontan pluvial lake system which existed between 5,000 and 40,000 years BP. The basin consists of two subbasins separated by a low elevation divide. Groundwater in the western subbasin has a maximum total dissolved solids (TDS) content of only ～1,300 mg/L; however eastern subbasin groundwater has a maximum TDS of ～46,000 mg/L. This TDS distribution is unexpected because 94% of surface water TDS loading is to the western subbasin. In situ reactions and upwelling thermal groundwater contributing to groundwater chemistry were modeled using NETPATH. The TDS difference between the subbasins is attributed to post-Lake Lahontan isostatic rebound about 13,000 years ago. Prior to rebound the subbasins did not exist and the low point of the basin was in the eastern area where hydraulic isolation from the larger Lake Lahontan and frequent desiccation of the basin surface water resulted in evaporite mineral deposition in accumulating sediments. After rebound, the terminal sink for most surface water shifted to the western subbasin. Although most closed basins have not been impacted by isostatic rebound, results of this investigation demonstrate how tectonic evolution can impact the distribution of soluble minerals accumulating in shallow basins.  相似文献   

The acid catalyzed nitration of methanol: formation of methyl nitrate via aerosol chemistry     

Laura T. Iraci  Brent G. Riffel  Carly B. Robinson  Rebecca R. Michelsen  Rachel M. Stephenson 《Journal of Atmospheric Chemistry》2008,59(3):237-238

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Evaluating and improving semi-analytic modelling of dust in galaxies based on radiative transfer calculations     

Fabio Fontanot  Rachel S. Somerville  Laura Silva  Pierluigi Monaco  Ramin Skibba 《Monthly notices of the Royal Astronomical Society》2009,392(2):553-569

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Empirical constraints on the evolution of the relationship between black hole and galaxy mass: scatter matters     

Rachel S. Somerville 《Monthly notices of the Royal Astronomical Society》2009,399(4):1988-1994

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Working a fraction and making a fraction work: a rough guide for geographers in the academy     

Jacky Birnie  Clare Madge  Rachel Pain†  Parvati Raghuram‡  Gillian Rose‡ 《Area》2005,37(3):251-259

Little is known about the issues facing geographers working on fractional appointments in higher education institutions in the UK. This paper draws on a survey of UK geography departments and personal experiences to explore some of that territory for the first time. The purpose is both to set the agenda for institutional policy issues and to provide some immediate points of reflection for staff intending to take up fractional work. We consider the place of fractional working in the dominant discourses around paid work, problems of workload division and the impact on professional standing (including the RAE). We suggest that while personal 'life' reasons for fractional working are often positive, fractional workers in the academy risk professional marginalization.  相似文献   

Reflections on participatory research   总被引：2，自引：0，他引：2  

Rachel Pain  Peter Francis 《Area》2003,35(1):46-54

Participatory research approaches are increasingly popular with geographers in developed as well as developing countries, as critical qualitative methodologies which at their best work with participants to effect change. This paper adds to recent debates over the methodologies, practices, philosophical and political issues involved. Drawing on a project on young people, exclusion and crime victimization in Newcastle upon Tyne, England, we discuss the limitations of participatory diagramming and illustrate some of the social and political barriers to meaningful participation in, and action from, this type of research.  相似文献   

Subsolidus physical and chemical mixing of granite and gabbro during mylonitization, South Victoria Land, Antarctica     

C. Rachel Walcott  Dave Craw 《Journal of Structural Geology》1993,15(12)

At Dromedary Massif, Southern Victoria Land, Antarctica, a suite of coarse-grained granite dykes cross-cuts a gabbro pluton which has been partially metamorphosed at amphibolite facies. During regional deformation, strain has been inhomogeneously distributed through the gabbro pluton and has been concentrated in granite dykes. In zones of relatively high strain, the granite dykes have developed a mylonitic fabric. A high strain gradient between granitic mylonite and metagabbroic host rock has induced isochemical mylonitization of the margin of the host. This grain size reduction allowed chemical diffusion between granitic and metagabbroic mylonites, resulting in a marginal zone of biotite-rich mylonite with intermediate composition. Biotite-rich mylonite decoupled from metagabbroic mylonite and flowed with granitic mylonite. Continued folding and transposition of granitic mylonite and biotite-rich mylonite has produced compositionally banded mylonite zones through thorough and irreversible mixing of the two lithologies.  相似文献   

A 24,700-yr paleolimnological history from the Peruvian Andes     

Rachel Hillyer  Bryan G. Valencia  Miles R. Silman 《Quaternary Research》2009,71(1):71-126

A new paleolimnological dataset from Lake Pacucha (13 °S, 3095 m elevation) in the Peruvian Andes provides evidence of changes in lake level over the past 24,700 yr. A late-glacial highstand in lake level gave way to an early-Holocene lowstand. This transition appears to have paralleled precessional changes that would have reduced insolation during the wet-season. The occurrence of benthic/salt-tolerant diatoms and CaCO₃ deposition suggest that the lake had lost much of its volume by c. 10,000 cal yr BP. Pronounced Holocene oscillations in lake level included a second phase of low lake level and heightened volatility lasting from c. 8300 to 5000 cal yr BP. While a polymictic lake formed at c. 5000 cal yr BP. These relatively wet conditions were interrupted by a series of drier events, the most pronounced of which occurred at c. 750 cal yr BP. Paleolimnological changes in the Holocene were more rapid than those of either the last glacial maximum or the deglacial period.  相似文献   

Recapturing quality field experiences and strengthening teaching–research links     

Rachel Spronken-Smith  Mike Hilton 《New Zealand geographer》2009,65(2):139-146

Because of unwieldy numbers, and in an attempt to strengthen teaching–research links, the teaching team of 'Field Research Methods' discarded a class fieldtrip in favour of more flexible fieldwork. The new approach continues to use inquiry-based learning but has research problems more closely linked to staff interests. Students are responsible for most aspects of the research process including some logistical planning of fieldwork. Although often anxious at first, students welcomed this approach and appreciated the host of transferable and research skills they developed. Tutors benefited from the enhanced learning outcomes for students and a strengthening of teaching–research links.  相似文献