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A substantial literature in social sciences, including law and society, examines the intersections of research ethics and institutional review board (IRB) frameworks. Although geographers have engaged this literature, we argue that further involvement in ethical and regulatory discussions will advance opportunities for better understanding and negotiating the complex subjectivities produced in the IRB structure. Drawing on illustrative experiences of researchers, we focus specifically on the institutions convening IRBs, the researchers, and the human “subjects” produced in the IRB process. We conclude with a call for greater open discussion of the power dynamics, subjectivities, and challenges of formal ethical research structures.  相似文献   

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Archaeological sites, the material remnants of our human past, are finite and nonrenewable cultural resources that are under constant threat from environmental forces, development activities, warfare, vandalism, and looting. Site looting is the destructive removal of archaeological objects to supply the art market. Looting is part of an economic system, the antiquities market, that works to supply the demand of collectors for archaeological objects. The destruction of archaeological resources by looters is an international crisis and threatens to obliterate the world’s cultural heritage and our ability to understand past cultures. The scale and intensity of the looting problem can be estimated by studying the extent of site destruction in countries of origin and by investigating the sources of antiquities held by collectors. Finding a solution to the problem of looting will require a focus on the demand side of the market (i.e., collectors) instead of the traditional focus on the supply side (looters, dealers)  相似文献   

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Medicine Lake is a highly saline meromictic lake in eastern South Dakota. A lithostratigraphic and biostratigraphic study of the late-glacial and early post-glacial sediments shows that it was a relatively deep dilute freshwater lake during the period of the Picea pollen zone. When spruce forest changed to a Betula and then to a Quercus/Ulmus woodland in the early post-glacial period, the lake water became more concentrated but remained fresh. However, during the subsequent rapid transition to prairie in the early Holocene, when Gramineae, Ambrosia, and Artemisia dominated dry-land vegetation, the freshwater diatom flora was progressively replaced by a saline assemblage characterized by Cyclotella quillensis, Chaetoceros, and eventually Cyclotella caspia. The lake became permanently saline at about 9000 yr BP. A comparison of the fossil diatom assemblages with surface-sediment samples from a range of lakes in the Dakotas indicates that the change involved an increase in conductivity from about 500 S cm–1 in the late-glacial period to > 10 000 S cm–1 in the early Holocene. This rapid change is also marked by an abrupt increase in sulphate concentration in the sediment, the first appearance of bands of gypsum crystals, and the beginning of a well-laminated core sequence that continues through the remaining sediment record. Conditions of high salinity have prevailed to the present day.Contribution 299, Limnological Research Center.  相似文献   

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The article shows that although a large literature has been produced on the concept of urban governance, its meaning remains ambiguous. The aim of the article is not to ‘prove’ that there is confusion in the concept or to rectify that confusion, but rather to consolidate, categorise, and synthesise the many meanings of urban governance. The article argues that when the concept of ‘urban governance’ is regarded as a cluster of meanings, particularly as decentralisation, entrepreneurialism, and democratisation (DED) and repositioned in a broad political-economic and socio-cultural framework, its full tenor can be grasped for future research.  相似文献   

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Australian placename studies have focused on documenting toponymic histories and issues of concern mainly for placename taxonomy and etymology. Language-external factors such as geographical and environmental conditions have not been of great interest to Australian toponymists. This article assesses the role of geographical and environmental constriction of island places on their toponymy. It considers whether or not island locations breed ‘insular toponymies’ or placename histories inaccessible and not readily accessible to outsider researchers. The case studies are Norfolk Island, South Pacific, and Dudley Peninsula, South Australia, two island environments within political Australia. The results demonstrate that the degree of insularity of the toponymies of the two island environments is driven more by geographical and social factors than linguistic elements. The results put forward several ways in which geographers, linguists, historians, toponymists, and Australian studies scholars could work together and collaborate to better understand Australian island places.  相似文献   

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Mathematical methods from the theory of continuous groups are used to determine whether a non-linear inverse problem, in the form of a functional, can be transformed into a linear inverse problem. If such transformations exist they can be constructed from the solutions of a linear system of differential equations. An illustration of the methodology is given by the linearization of the functional relating basement topography to observed surface gravity. The linearized inversion of gravity data for basement topography is applied to observations from Yucca Mountain, Nevada. A 2.0 km step in the basement to the west of Yucca Mountain, corresponding to the Bare Mountain fault, matches the Bouguer gravity anomaly. The resolution and uncertainty associated with the estimates of basement topography indicate that the structure directly beneath the gravity line is well constrained.  相似文献   

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While links between social and physical disorder, crime, and the fear of crime have long been areas of research interest, few studies have looked at these links from a spatiotemporal viewpoint. This is somewhat surprising, as many of the factors associated with disorder, crime, and fear are known to vary over time and space. This paper uses GISystems to investigate potential spatiotemporal links between these areas in Wollongong, New South Wales, with specific focus on links between graffiti and the fear of crime. The results reveal that the distribution of fear of crime varies considerably over time and is often spatially coincident with concentrations of disorder. Graffiti was found to be one of the most prevalent types of physical disorder. The results are discussed in the context of the “broken windows” thesis and strategic intervention at the community level.  相似文献   

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Northwestern California is prone to regional, high magnitude winter rainstorms, which repeatedly produce catastrophic floods in the basins of the northern Coast Ranges. Major floods on the Eel River in 1955 and 1964 resulted in substantial geomorphic changes to the channel, adjacent terraces, and tributaries. This study evaluated the changes and the effects of a moderate flood in 1997 through field observations and examination of aerial photographs that spanned from 1954 to 1996. The purpose was to document the nature and magnitude of geomorphic responses to these three floods and assess the rates and controls on the recovery of the Eel River and its tributaries. Channel widening from extensive bank erosion was the dominant geomorphic change along the lower Eel River during major floods. As a result of the 1964 flood, the largest amount of widening was 195 m and represented an 80% change in channel width. Channel narrowing characterized the periods after the 1955 and 1964 floods. More than 30 years after the 1964 flood, however, the river had not returned to pre-flood width, which suggests that channel recovery required decades to complete. A long recovery time is unusual given that the Eel River is located in an area with a “superhumid” climate and has an exceptionally high sediment yield. This long recovery time may reflect highly seasonal precipitation and runoff, which are concentrated in 3–5 months each winter. In contrast to the main stem of the Eel River, the dominant effects of floods on the tributaries of the Eel River were rapid aggradation of channel bed and valley floor followed by immediate downcutting. Dendrogeomorphic data, aerial photographs, and field observations indicate that thick wedges of gravel, derived largely from hillslope failures in upper reaches of the tributaries, are deposited at and immediately upstream of the mouths of tributaries as the stage of the Eel River exceeded that of the tributaries during major floods. In the waning stages of the flood, the tributaries cut through the gravel at a rate equal to the lowering of the Eel and generated unpaired terraces and nickpoints. The complete process of deposition and incision can occur within a few days of peak discharge. Although reworking of some sediment on the valley floor may continue for years after large floods, channel morphology in the tributaries appears to be a product of infrequent, high magnitude events. The morphology of the tributary channel also appears to be greatly influenced by the frequency and magnitude of mass wasting in headwater areas of small basins.  相似文献   

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Removed overburden, burial, maturation, and petroleum generation analysis indicates that maturity in the Arkoma Basin and the Ouachita Foldbelt is explained effectively using simple burial models that account for the significant surface erosion that has occurred and assuming geothermal gradients similar to present-day gradients have been approximately constant through geologic time. Regional models, based on analysis at 115 well locations, indicate that from 5,000 to 15,000 ft (1.5–4.5 km) of section, differing with location from north to south and west to east, has been removed from the Arkoma Basin region, and as much as 25,000–40,000 ft (7.5–12 km) have been removed from areas of the Ouachita Foldbelt. Based on burial and thermal history reconstruction, increasing maturation from west to east across the basin is primarily the result of increasing overburden and subsequent surface erosion from west to east. The models predict most publicly available vitrinite reflectance data within a factor of 1.5 at two standard deviations. Comparison of model and measured reflectance-depth trends in six wells indicates that hydrothermal fluid movement should not have modified reflectance by more than approximately 20% in the center of the basin. Analysis indicates that most of the basin is overmature for oil production from intervals below the Spiro Sandstone, except to the north and northwest. Although thermal maturities are high, methane is stable throughout the basin. Except for the basal Arbuckle Group, all formations were thermally immature for oil generation prior to burial by the Mississippian and Morrowan in the Ouachita Foldbelt of Oklahoma and by the Atokan and Desmoinesian over most of the basin and study area. In the deeper part of the present basin, all strata entered and passed through the oil window during or within 10 My after Atokan time. Because no additional major quantities of hydrocarbons were generated after Atokan time, the hydrocarbons must have been emplaced and trapped during this brief time interval.  相似文献   

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《The Journal of geography》2012,111(3):177-179
Abstract

Atlas of American Agriculture: The American Cornucopia by Richard Pillsbury and John Florin, New York: Prentice-Hall. 1996.278 pp. Maps, charts, tables, bibliography, indices. ISBN 0-02-897333-X. $90.00, hardcover.  相似文献   

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The three broad categories of commodity inputs to the economy are food, fuel, and material, defined as everything else not used for the first two purposes. Material provides physical structure, houses, cars, and packaging; is an important constitutent of modern agriculture in the form of fertilizer and insecticides; and supports the service sector through telecommunications and equipment and paper for our copying machines. The efficient flow of this material is an important factor in the U.S. economy.Correspondence should be directed to Earle B. Amey, U.S. Geological Survey, National Center 983, Reston, Virgina 20192.  相似文献   

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《自然地理学》2013,34(6):474-506
The Cycle of Erosion formulated by the American geographer William Morris Davis in the 1880s remained the dominant paradigm in geomorphology well into the 20th century, before it waned in response to improved understanding of Earth's crustal and surface behavior. The Davisian model sought to explain landforms in terms of structure, process, and stage. Following initial rapid tectonic uplift, landforms were presumed to evolve on a quiescent crust through stages of youth, maturity, and old age, to culminate in a peneplain. A new cycle would be initiated by landform rejuvenation in response to a changing base level of erosion. This model was a reflection of its time, of the cycle mania of the 19th century, which in turn was founded on Hutton's limitless "succession of worlds" and dissatisfaction with earlier notions of landscape origins constrained by limited Earth time. Davis's model was derived from ideas regarding orogenic cycles favored by Dana and Le Conte, and of prolonged subaerial denudation toward base-level observed by Powell and Dutton. The model's supremacy was challenged from time to time, notably by the Pencks (father and son) and by alternative cyclic denudation models that invoked pediplanation and etchplanation rather than peneplanation. The relevance of the Davisian model declined after 1940 in response to a growing awareness of Earth's crustal mobility, changing climates and geomorphic processes, and refined dating of geologic time. The subsequent quantitative revolution in geomorphology, with its emphasis on measurement of form and process aided by rapidly improving technologies, and based in part on lingering antecedents, sounded the death knell for the Davisian model but also triggered something of a theoretical hiatus. In recent years, resurrection of the concept of isostasy, defined by Dutton but ignored by Davis, has led to the formulation of a more realistic but more complex model, briefly introduced here, in which landforms may be viewed as responses to more-or-less continuous interaction between tectonic activity, subaerial denudation, and isostatic adjustment.  相似文献   

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身体、身体观以及人文地理学对身体的研究   总被引:7,自引:3,他引:4  
陶伟  王绍续  朱竑 《地理研究》2015,34(6):1173-1187
1970年代以来,伴随着消费主义和女权运动,身体研究在人文社会学科中兴起,一个被布莱恩·特纳(Bryan Turner)称之为“身体社会崛起”的时代来临了。身体研究成为西方人文与社会科学研究的“新大陆”,众多哲学家、社会理论学家纷纷投身于身体研究,重新解读了身体在认识世界和知识生产中的重要性。身体转向作为文化转向的一部分,同样受到了人文地理学家的关注。许多批判地理学家,如女性主义、马克思主义、反种族主义、后殖民主义、酷儿地理学家认为,身体研究是改善社会、文化、经济关系的可能途径。在“身体转向”的影响下,身体研究逐渐渗入到情感地理学、旅游地理学、乡村地理学等众多研究领域。与此同时,人文地理学家从人文社会科学中引入多种理论,如表演理论、精神分析法、非表征理论等对身体研究进行了探讨和阐释。基于这样的背景,梳理了西方人文地理学中有关身体研究的文献,归纳了人文地理学中身体研究的主要议题和理论,以及由此而展开的一系列具体的研究成果,此工作具有切实的学术意义并对后续相关研究的展开具有指导意义。  相似文献   

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Standards-Directed Education: The Good,the Bad,and the Ugly   总被引:1,自引:1,他引:0  
《The Journal of geography》2012,111(6):271-272
Abstract

GIS Concepts and ArcGIS Methods, David M. Theobald Fort Collins, CO: Conservations Planning Technologies, 2003. 342 pp. ISBN 0-9679208-2-5 $55.00 (paper)

Lies My Teacher Told Me: Everything Your American History Textbook Got Wrong, James W. Loewen New York: A Touchstone Book, Simon &; Schuster. 1995. 383 pp. Figures, references, and index, ISBN: 0684818868. $14.00 (paper).  相似文献   

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