A HYDROLOGICAL SIMULATION OF HAZARDOUS WASTE INJECTION IN THE MT. SIMON, OHIO     

Dennis J. Nealon 《Ground water》1982,20(3):348-349

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Book reviews     

Jesse H. Ausubel  Ronald L. Gilliland  John Opie  Stephen G. Warren  Robin L. Dennis  Paulette Middleton 《Climatic change》1982,4(3):313-322

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Orthodoxy and creativity in theories of mountain building before 1922     

Prof. Dr. John G. Dennis 《International Journal of Earth Sciences》1982,71(2):421-426

In the 1870s, theories of mountain building emerged from little more than speculation to inference based on a growing body of observation and documentation. This coincided with abandonment of models stressing uplift, and their replacement, in the new orthodoxy, by models in which earth contraction led to lateral compression in its outer shell. Nevertheless, perceived weaknesses in this model gave impetus to new theories, some emphasizing primary vertical movement, and others continental displacement or subcrustal flow. The rebel theories added to the understanding of earth processes in important ways, by drawing attention to the weaknesses in the prevailing orthodoxy. But, in 1922, the complete answer remained out of reach.

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Zusammenfassung Die siebziger Jahre des vorigen Jahrhunderts brachten den Anfang von wissenschaftlich fundierten Theorien der Gebirgsbildung. Diese Zeit sah auch den Übergang von Erhebungstheorien zur neuen Lehrmeinung, nach welcher Erdkontraktion zu lateralen Drucken in der Außenhülle der Erde führte. Erkannte Schwächen dieses Modells führten jedoch zu neuen Gegentheorien, von denen einige primäre Vertikalbewegungen in den Vordergrund stellten, während andere Kontinentalverschiebung oder Unterströmungen als den Motor der Gebirgsbildung sahen. Diese Gegentheorien haben den Fortschritt der Erdwissenschaften gefördert, indem sie auf Schwächen der herrschenden Lehrmeinung aufmerksam machten. Aber selbst zu Argands Zeit war ein völlig befriedigendes Modell noch gar nicht erreichbar.

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Résumé C'est dans les années 1870–1880 que commençaient à s'établir les premières théories vraiment scientifiques de l'orogenèse. C'était la décade qui marqua l'abandon des théories à base de soulèvement et le début du règne de la nouvelle orthodoxie d'après laquelle la contraction de la terre mène à la compression latérale d'une pellicule extérieure. Néansmoins, certaines faiblesses du nouveau modèle servaient d'élan à des théories rebelles dont quelques-unes soulignaient l'importance des soulèvements primaires, tandisque d'autres cherchaient le moteur de l'orogenèse dans la dérive des continents ou dans des courants dans une masse quasi-fluide subcrustale. Ces théories rebelles ont avancé la science en soulignant les faiblesses de l'orthodoxie. En fin de compte, une solution complètement satisfaisante ne paraissait pas encore pouvoir être atteinte à l'époque d'Argand.

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Characteristics of air flow above and within soybean canopies     

Dennis D. Baldocchi  Shashi B. Verma  Norman J. Rosenberg 《Boundary-Layer Meteorology》1983,25(1):43-54

Air flow was observed above and within canopies of a number of kinds of soybeans. The Clark cultivar and two isolines of the Harosoy cultivar were studied in 1979 and 1980, respectively. Wind speed above the canopy was measured with cup anemometers. Heated thermistor anemometers were used to measure air flow within the canopy. Above-canopy air flow was characterized in terms of the zero-plane displacement (d), roughness parameter (z _o) and drag coefficient (C _d). d and z _o were dependent on canopy height but were independent of friction velocity in the range 0.55 to 0.75 m s^?1 · C _d for the various canopies ranged from 0.027 to 0.035. Greater C _d values were measured over an erectophile canopy than over a planophile canopy. C _d was not measurably affected by differences in leaf pubescence. Within-canopy wind profiles were measured at two locations: within and between rows. The wind profile was characterized by a region of great wind shear in the upper canopy and by a region of relatively weak wind shear in the middle canopy. Considerable spatial variability in wind speed was evident, however. This result has significant implications for canopy flow modeling efforts aimed at evaluating transport in the canopy. In the lower canopy, wind speed within a row increased with depth whereas wind speed between two rows decreased with depth. The wind speeds at the two locations tended to converge to a common value at a height near 0.10 m. The attenuation of within-canopy air flow was stronger in canopies with greater foliage density. Canopy flow attenuation seemed to decrease with increasing wind speed, suggesting that high winds distorted the shape of the canopy in such a manner that the penetration of wind into the canopy increased.  相似文献   

Detection Time for Plausible Changes in Annual Precipitation, Evapotranspiration, and Streamflow in Three Mississippi River Sub-Basins     

Alan D. Ziegler  Edwin P. Maurer  Justin Sheffield  Bart Nijssen  Eric F. Wood  Dennis P. Lettenmaier 《Climatic change》2005,72(1-2):17-36

We use diagnostic studies of off-line variable infiltration capacity (VIC) model simulations of terrestrial water budgets and 21st-century climate change simulations using the parallel climate model (PCM) to estimate the time required to detect predicted changes in annual precipitation (P), evapotranspiration (E), and discharge (Q) in three sub-basins of the Mississippi River Basin. Time series lengths on the order of 50–350 years are required to detect plausible P, E, and Q trends in the Missouri, Ohio, and Upper Mississippi River basins. Approximately 80–160, 50, and 140–350 years, respectively, are needed to detect the predicted P, E, and Q trends with a high degree of statistical confidence. These detection time estimates are based on conservative statistical criteria (α = 0.05 and β = 0.10) associated with low probability of both detecting a trend when it is not occurring (Type I error) and not detecting a trend when it is occurring (Type II error). The long detection times suggest that global-warming-induced changes in annual basin-wide hydro-climatic variables that may already be occurring in the three basins probably cannot yet be detected at this level of confidence. Furthermore, changes for some variables that may occur within the 21st century might not be detectable for many decades or until the following century – this may or may not be the case for individual recording station data. The long detection times for streamflow result from comparatively low signal-to-noise ratios in the annual time series. Finally, initial estimates suggest that faster detection of acceleration in the hydrological cycle may be possible using seasonal time series of appropriate hydro-climatic variables, rather than annual time series.  相似文献   

The Determination of Logbook Wind Force and Weather Terms: The English Case     

Dennis Wheeler  Clive Wilkinson 《Climatic change》2005,73(1-2):57-77

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Quantifying geographic variations in associations between alcohol distribution and violence: a comparison of geographically weighted regression and spatially varying coefficient models   总被引：2，自引：1，他引：2  

Lance A. Waller  Li Zhu  Carol A. Gotway  Dennis M. Gorman  Paul J. Gruenewald 《Stochastic Environmental Research and Risk Assessment (SERRA)》2007,21(5):573-588

Past studies consistently indicate measurable local associations between alcohol distribution and the incidence of violence. These results, coupled with measurements of spatial correlation, reveal the importance of spatial analysis in the study of the interaction of alcohol and violence. While studies increasingly incorporate spatial correlation among model residuals to improve precision and reduce bias, to date, most analyses assume associations that are constant and independent of location, an assumption coming under increasing scrutiny in the quantitative geography literature. In this paper, we review and contrast two approaches for the estimation of and inference for spatially heterogeneous effects (i.e., associative factors whose impacts on the outcome of interest vary throughout geographic space). Specifically, we provide an in-depth comparison of “geographically weighted regression” models (allowing covariate effects to vary in space but only allowing relatively ad hoc inference) with “variable coefficient” models (allowing varying effects via spatial random fields and providing model-based estimation and inference, but requiring more advanced computational techniques). We compare the approaches with respect to underlying conceptual structures, computational implementation, and inferential output. We apply both approaches to violent crime, illegal drug arrest, and alcohol distribution data from Houston, Texas and compare results in light of the differing methodological structures of the two approaches.  相似文献   

Local co-operation, ethnic diversity and state territoriality – The case of Haparanda and Tornio on the Sweden – Finland border     

Thomas Lundén  Dennis Zalamans 《GeoJournal》2001,54(1):33-42

The neighbouring towns of Haparanda and Tornio, separated only by a narrow strip of grass and wetland, are divided by the only inhabited land boundary between Finland and Sweden in the southern part of the Torne River. The population represents four different groups in relation to linguistic and cultural backgrounds. In the daily lives of the inhabitants, the state boundary is probably of less significance than linguistic, social and ‘ethnic’ differences. On the local government level there is a strong will to unite forces to make the total area a viable region in spite of its peripheral location, but state legislation makes co-ordination difficult. This may be seen as a necessity, but in the daily lives of the populations, the state boundary defines an area of unequal access, sometimes working in favour of and sometimes barring contacts and co-operation. The media consumption reflects a clear ‘national’ interest with a strong local bias. In their attitudes, Finnish speakers and bilinguals show a greater appreciation of ‘the other’ than unilingual Swedes. This may reflect the actual possibility space (reach) in the local area. This revised version was published online in July 2006 with corrections to the Cover Date.  相似文献   

Evolution of Pangea: paleomagnetic constraints from the Southern Alps, Italy     

Giovanni Muttoni  Dennis V. Kent  James E.T. Channell 《Earth and Planetary Science Letters》1996,140(1-4):97-112

A new early Late Triassic paleopole for Adria has been obtained from the Val Sabbia Sandstone in the Southern Alps. As Early Permian and Jurassic-Cretaceous paleomagnetic data from para-autochthonous regions of Adria such as the Southern Alps are consistent with ‘African’ APWPs[1–2], paleomagnetic data from this region can be used to bolster the West Gondwana APWP in the poorly known Late Permian-Triassic time interval. The Southern Alpine paleopoles are integrated with the West Gondwana and Laurussia APWPs of Van der Voo [1] and used to generate a tectonic model for the evolution of Pangea. The Early Permian overall mean paleopole for West Gondwana and Adria, in conjunction with the coeval Laurussia paleopole, support Pangea B of Morel and Irving [3]. The Late Permian/Early Triassic and the Middle/Late Triassic paleopoles from Adria and Laurussia support Pangea A-2 of Van der Voo and French [4]. The phase of transcurrent motion between Laurasia and Gondwana[5] that caused the Pangea B to A-2 transition occurred essentially in the Permian (at the end of Variscan orogeny) with an average relative velocity of approximately 10 cm/yr. Finally, the Late Triassic/Early Jurassic paleopoles from West Gondwana and Laurussia agree with Pangea A-1 of Bullard et al. [6], the widely accepted Pangea configuration at the time of the Jurassic breakup.  相似文献   

A Controlled Field Test of Surfactant-Enhanced Aquifer Remediation   总被引：4，自引：0，他引：4  

John C. Fountain  Robert C. Starr  Thomas Middleton  Michael Beikirch  Craig Taylor  Dennis Hodge 《Ground water》1996,34(5):910-916

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