Introduction to the special section on establishing state‐led ‘diaspora strategies’ in Asia: Migration‐as‐development reinvented?          下载免费PDF全文

Elaine Lynn‐Ee Ho  Brenda S.A. Yeoh 《Singapore journal of tropical geography》2015,36(2):139-146

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Hydrogeologic Controls on Induced Seismicity in Crystalline Basement Rocks Due to Fluid Injection into Basal Reservoirs     

Yipeng Zhang  Mark Person  John Rupp  Kevin Ellett  Michael A. Celia  Carl W. Gable  Brenda Bowen  James Evans  Karl Bandilla  Peter Mozley  Thomas Dewers  Thomas Elliot 《Ground water》2013,51(4):525-538

A series of M_b 3.8–5.5 induced seismic events in the midcontinent region, United States, resulted from injection of fluid either into a basal sedimentary reservoir with no underlying confining unit or directly into the underlying crystalline basement complex. The earthquakes probably occurred along faults that were likely critically stressed within the crystalline basement. These faults were located at a considerable distance (up to 10 km) from the injection wells and head increases at the hypocenters were likely relatively small (～70–150 m). We present a suite of simulations that use a simple hydrogeologic‐geomechanical model to assess what hydrogeologic conditions promote or deter induced seismic events within the crystalline basement across the midcontinent. The presence of a confining unit beneath the injection reservoir horizon had the single largest effect in preventing induced seismicity within the underlying crystalline basement. For a crystalline basement having a permeability of 2 × 10^?17 m² and specific storage coefficient of 10^?7/m, injection at a rate of 5455 m³/d into the basal aquifer with no underlying basal seal over 10 years resulted in probable brittle failure to depths of about 0.6 km below the injection reservoir. Including a permeable (k_z = 10^?13 m²) Precambrian normal fault, located 20 m from the injection well, increased the depth of the failure region below the reservoir to 3 km. For a large permeability contrast between a Precambrian thrust fault (10^?12 m²) and the surrounding crystalline basement (10^?18 m²), the failure region can extend laterally 10 km away from the injection well.  相似文献   

Foreword to the special issue: Arctic Palaeoclimate and Its Extremes (APEX)     

Martin Jakobsson  Robert F. Spielhagen  Jörn Thiede  Claus Andreasen  Brenda Hall  Ólafur Ingólfsson  Kurt H. Kjær  Thijs van Kolfschoten  Gerhard Krinner  Antony Long  Juha-Pekka Lunkka  Dmitry Subetto  & John Inge Svendsen 《Polar research》2008,27(2):97-104

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Twentieth century eutrophication of the St. Croix River (Minnesota–Wisconsin,USA) reconstructed from the sediments of its natural impoundment     

Mark B. Edlund  Daniel R. Engstrom  Laura D. Triplett  Brenda Moraska Lafrancois  Peter R. Leavitt 《Journal of Paleolimnology》2009,41(4):641-657

Evaluation of land-use effects on coastal and marine ecosystems requires better understanding of the role of rivers in regulating mass transport from terrestrial to oceanic environments. Here we take advantage of the presence of a riverine lake to use paleoecological techniques to quantify impacts of logging, European-style agriculture, urbanization and continued terrestrial disturbance on mass transport and water quality in the northern drainage of the Mississippi River. Two 2-m sediment-cores recovered in 1999 from Lake St. Croix, a natural impoundment of the St. Croix River, were dated using ²¹⁰Pb and ¹³⁷Cs, and analyzed for historical changes (c. 1840–present) in sediment magnetic susceptibility, inorganic and organic matter content, biogenic silica, fossil pigments, and diatom microfossils. Inorganic sediment accumulation increased threefold between the mid-1800s and present, whereas clear signs of eutrophication were only evident after the mid-twentieth century when biogenic silica accumulation increased sixfold, diatom accumulation rates increased 20- to 50- fold, and the diatom community shifted from predominantly benthic species to assemblages composed mainly of planktonic taxa. Similarly, fossil pigment concentrations increased during the 1960s, and diatom-inferred total phosphorus (DI-TP) increased from ~30 μg TP l⁻¹ c. 1910 to ~60 μg l⁻¹ since 1990, similar to historical records since 1980. Together, these patterns demonstrate that initial land clearance did not result in substantive declines in water quality or nutrient mass transport, instead, substantial degradation of downstream environments was restricted to the latter half of the twentieth century. This is one of eight papers dedicated to the “Recent Environmental History of the Upper Mississippi River” published in this special issue of the Journal of Paleolimnology. D. R. Engstrom served as guest editor of the special issue.  相似文献   

Stable isotopes and soil-geomorphology as indicators of Holocene climate change, northern Chihuahuan Desert     

Brenda J. Buck  H. Curtis Monger 《Journal of Arid Environments》1999,43(4):357

Coeval δ¹³C shifts recorded in buried soils at both piedmont slope and basin floor sites in the northern Chihuahuan Desert indicate a major shift from C₄grasses to C₃desert-scrub between 7 and 9 ka. The age assignments are based on stratigraphic correlations to charcoal dates and carbon-14 dates of carbonate. This shift is synchronous with a period of cooling in the North Atlantic that may have triggered a period of drought in the south-western United States. Coinciding with this vegetation change, geomorphic evidence in Rio Grande, piedmont, and basin floor eolian environments indicates a major period of erosion. Subsequent gradual enrichment of pedogenic carbonateδ¹³ C values in younger deposits suggests that C₄grasses rebounded in the late Holocene (approximately 4 ka), which is consistent with other evidence of increased moisture regionally. A period of less severe aridity at approximately 2·2 ka is indicated by erosion and subsequent deposition along the alluvial fans and within the basin, and correlates with depleted pedogenic carbonate δ¹³C values suggesting a decrease in C₄grasses. Isotope and packrat midden records should be used together to infer past environmental conditions at different elevations.  相似文献   

Transnational labour migration and the politics of care in the Southeast Asian family     

Lan Anh Hoang  Brenda S.A. Yeoh  Anna Marie Wattie 《Geoforum》2012,43(4):733-740

Recent increases in female labour migration in and from Asia have triggered a surge of interest in how the absence of the mother and wife for extended periods of time affects the left-behind family, particularly children, in labour-sending countries. While migration studies in the region have shown that the extended family, especially female relatives, is often called on for support in childcare during the mother’s absence it is not yet clear how childcare arrangements are made. Drawing on in-depth interviews with non-parent carers of left-behind children in Indonesia and Vietnam, the paper aims to unveil complexities and nuances around care in the context of transnational labour migration. In so doing it draws attention to the enduring influence of social norms on the organisation of family life when women are increasingly drawn into the global labour market. By contrasting a predominantly patrilineal East Asian family structure in Vietnam with what is often understood as a bilateral South-East Asian family structure in Indonesia, the paper seeks to provide interesting comparative insights into the adaptive strategies that the transnational family pursues in order to cope with the reproductive vacuum left behind by the migrant mother.  相似文献   

Biogeochemical Stratification and Carbonate Dissolution-Precipitation in Hypersaline Microbial Mats (Salt Pond, San Salvador, The Bahamas)     

Mary K. Puckett  Karen S. McNeal  Brenda L. Kirkland  Margaret E. Corley  John E. Ezell 《Aquatic Geochemistry》2011,17(4-5):397-418

Microbial mat communities host complex biogeochemical processes and play a role in the formation of most carbonate rocks by influencing both carbonate precipitation and dissolution. In this study, the biogeochemistry of microbial mats from the hypersaline Salt Pond, San Salvador, Bahamas are described using scanning electron microscopy, X-ray diffraction, microelectrode profiling, fatty acid methyl esters, and carbon and nitrogen analyses. These microbial mats are distinctly layered both chemically and with regard to composition of microbial community, where significant (?? < 0.05) differences are noted between layers and cores. Furthermore, an oxic upper zone and an H₂S-rich lower zone dominate the Salt Pond microbial mats, where H₂S concentrations were measured approaching 8 mM. The high H₂S concentrations along with the lacking evidence of mineral precipitation in SEM images point to the prevalence of carbonate dissolution. Moreover, the high concentrations of organics (3?C9%) reveal that the mats are self-sourcing and can provide ample fuel to sustain the highly active heterotrophic (both aerobic and anaerobic) metabolism. Seasonal differences in sulfide and oxygen concentrations in Salt Pond mats indicate that the carbonate dissolution and precipitation reactions are dynamic in this hypersaline lake.  相似文献   

Acid saline lake systems give clues about past environments and the search for life on Mars     

Kathleen C. Benison  Brenda Beitler Bowen 《Icarus》2006,183(1):225-229

Acid saline lake systems in Western Australia may be the best known modern terrestrial analog for the Burns formation on Mars and, thus, provide information about past environments and life on Mars.  相似文献   

Second-Hand Spaces: Restructuring Retail Geographies in an Era of E-Commerce   总被引：1，自引：0，他引：1  

Brenda Parker  Rachel Weber 《Urban geography》2013,34(8):1096-1118

Are online markets replacing or remaking second-hand markets in cities? The restructuring of secondary markets in light of virtual outlets like eBay is not well understood. In this article, we describe secondary markets and their important historic, economic, cultural, and social roles in cities. The literature on e-Commerce suggests that virtual retailers compete with bricks-and-mortar stores and potentially displace them. We question whether the internet can substitute for second-hand stores, which have traditionally relied on a loyal and local customer base, personalized shopping experiences, and surprise encounters. Given the historically embedded nature of exchange, we focus on one large Mid-western city, drawing upon survey and interview data from Chicago retailers. Our exploration of supply, demand, and geographic practices reveals subtle and complex alterations in second-hand exchange, rather than a displacement of second-hand markets by eBay. We also find substantive integration, fluidity, and hybridization within and across market sectors. Rather than supplant the production of new goods, secondary markets are intertwined with and deepen primary markets, calling into question some of the presumed benefits of and meanings associated with second-hand exchange as well as the usefulness of categorical distinctions. [Key words: secondary markets, second-hand, resale, thrift, e-commerce, eBay.]  相似文献   

Mississippi prodelta crusts: A clay fabric and geotechnical analysis     

Brenda Myers Bohlke  Richard H. Bennett 《Marine Georesources & Geotechnology》2013,31(1):55-82

Abstract

"Crust”; zones, as defined by shear strength profiles, have been delineated in Mississippi prodelta sediments since the advent of the remote wire‐line probe. Attempts to map the distribution of the “crust”; on the prodelta have been hampered by sparsity of in situ measurements and its apparent lateral discontinuity. Evidence based on clay fabric, geotechnical properties, and the location of selected cores within certain geomorphic zones, suggests the “crusts”; are associated with zones of shearing during an episode of submarine sediment movement on the prodelta.

The clay fabric within the “crust”; zone differs from that found above and below in the high‐porosity sediments. A noticeable degree of clay platelet preferential alignment is characteristic of sediments within the “crust.”; This preferred orientation occurs as localizations rather than as an overall alignment of all the particles. The clay fabric of the higher‐porosity sediments above and below the “crust”; is typified by randomly arranged clay particles and domains, sharing edge‐to‐face contacts which create an open framework. Apparent increases in the coarse silt fraction in the “crust”; zone were observed initially in scanning electron and transmission electron micrographs and later confirmed by grain size analysis. The presence of this silt apparently contributes to the increase in shear strength within the “crust.”; Clay particle arrangement in close proximity to these larger grains is modified in such a manner as to reduce water contents. Transmission electron microscopy and scanning electron microscopy observations of the “crust”; reveal that the void ratio decreases, resulting in a concomitant reduction in the water content as reflected in the geotechnical properties profiles. The type of fabric exhibited by the “crust”; suggests a remolding and dewatering of initially porous silty clay sediments in response to shear stresses operating on the prodelta.

Core samples were recovered from sediments exhibiting a “crust”; in areas identified by other researchers as unstable, based on seismic and acoustic profiles and sidescan sonar records. The prodelta has been modified by a peripheral mudflow at the location where the cores were collected for this study.  相似文献