Valley

Distribution by Scientific Domains
Distribution within Earth and Environmental Science

Kinds of Valley

  • Thame valley
  • alpine valley
  • california central valley
  • central valley
  • dry valley
  • lake valley
  • mcmurdo dry valley
  • po valley
  • rhine valley
  • rift valley
  • river valley
  • silicon valley
  • taylor valley
  • tennessee river valley
  • trent valley

  • Terms modified by Valley

  • valley area
  • valley bottom
  • valley encephalitis
  • valley fill
  • valley floor
  • valley glacier
  • valley region
  • valley side

  • Selected Abstracts


    DIFFERENTIAL ROCK WEATHERING IN THE ,VALLEY OF THE BOULDERS', KÄRKEVAGGE, SWEDISH LAPLAND

    GEOGRAFISKA ANNALER SERIES A: PHYSICAL GEOGRAPHY, Issue 3 2008
    ROBERT G. DARMODY
    ABSTRACT. Kärkevagge is an alpine valley in the low arctic of Swedish Lapland. It is named after, and famous for, its large deposit of immense (c. 10,15 m) boulders that almost fill the lower valley. Above the boulder deposit, on the flanks of the valley, are more recent and generally much smaller (c. 1,3 m) individual boulders that have fallen from the valley-wall cliff face, presumably from post-glacial valley-side unloading. Some of these smaller boulders are seemingly fresh and unweathered while others have been reduced to no more than mounds in the tundra. These boulders must be younger than the larger, lower giant boulder deposit, but are not particularly recent rockfalls as they are partially buried in colluvium. Comparisons of mineralogy and chemistry indicate that the possibility exists that the incompetent, ,rotten' rocks, if not considerably older than their competent neighbors, are inherently self-destructive. They have evidence of increased sulfur content, which is a proxy for pyrite, a known weathering accelerant in Kärkevagge. [source]


    METEOROLOGICAL CONDITIONS DURING SLUSH-FLOW RELEASE AND THEIR GEOMORPHOLOGICAL IMPACT IN NORTHWESTERN ICELAND: A CASE STUDY FROM THE BÍLDUDALUR VALLEY

    GEOGRAFISKA ANNALER SERIES A: PHYSICAL GEOGRAPHY, Issue 3 2006
    ARMELLE DECAULNE
    ABSTRACT. This paper examines triggering factors and geomorphic significance of slush flows in the Bíldudalur valley, northwestern Iceland. The area is prone to release slush flows from two confined gullies, and at least ten flows have been reported since the beginning of the twentieth century. Despite their short path (600 m) and their moderate magnitude (from 6000 to 8000 m3), slush flows in the Bíldudalur valley represent a serious threat for the local community that is situated within the runout and deposition zones. With the help of meteorological data, the release of known slush flows is examined, highlighting the role of heavy rainfall and rapid snow-melt during winter cyclonic activity. The geomorphological impact of slush flows is assessed through the characteristics of the landforms produced during the 1997 and 1998 slush-flow events. It appears that the most obvious characteristics of slush flows in the Bíldudalur valley are the entrainment and deposition of debris, spatially differentiated. Chaotic sedimentation occurs chiefly in the middle part of a clearly concave cone, even if the flows continue beyond the cone. [source]


    HYDROLOGICAL EFFECTS OF AN UNCONTROLLED FLOWING WELL, RED RIVER VALLEY, NORTH DAKOTA, USA,

    JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION, Issue 5 2004
    Philip J. Gerla
    ABSTRACT: In areas of the Red River Valley that overlie permeable Paleozoic sediments, wetlands and salinization have developed where unregulated flowing wells discharge brackish water. Field data were collected to assess the fate of water and salt from a well 25 km northwest of Grand Forks. Drilled during the drought of the 1930s, discharge was used to replenish water in a small oxbow pond used by livestock. The unregulated well discharges about 56 m3/day, measured since 1993. This discharge exceeds ground water flow from the site, thereby forming a ground water mound with a maximum height of 1 m and a diameter of about 300 m. Most soil and underlying sediments near the well have a hydraulic conductivity of 0.3 m3/day. Flow net analysis suggests that less than 25 percent infiltrates, with the remaining water lost to surface flow and evapotranspiration (ET). Evapotranspiration and slow infiltration has led to increased salinization, with shallow soils exhibiting EC to 500 milliSiemens/m. The most pronounced soil salinization occurs along the margins of the oxbow pond and meander scars. Wetland vegetation with low diversity comprises three zones, with species associations similar to those of closed basin prairie potholes to the west. [source]


    WATERSHED SCALING EFFECT ON BASE FLOW NITRATE, VALLEY AND RIDGE PHYSIOGRAPHIC PROVINCE,

    JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION, Issue 5 2001
    Bruce D. Lindsey
    ABSTRACT: A study of stream base flow and NO3 -N concentration was conducted simultaneously in 51 subwatersheds within the 116-square-kilometer watershed of East Mahantango Creek near Klingerstown, Pennsylvania. The study was designed to test whether measurable results of processes and observations within the smaller watersheds were similar to or transferable to a larger scale. Ancillary data on land use were available for the small and large watersheds. Although the source of land-use data was different for the small and large watersheds, comparisons showed that the differences in the two land-use data sources were minimal. A land use-based water-quality model developed for the small-scale 7.3-square-kilometer watershed for a previous study accurately predicted NO3 -N concentrations from sampling in the same watershed. The water-quality model was modified and, using the imagery-based land use, was found to accurately predict NO3 -N concentrations in the subwatersheds of the large-scale 116-square-kilometer watershed as well. Because the model accurately predicts NO3 -N concentrations at small and large scales, it is likely that in second-order streams and higher, discharge of water and NO3 -N is dominated by flow from smaller first-order streams, and the contribution of ground-water discharge to higher order streams is minimal at the large scale. [source]


    WATER SUPPLY EVALUATION OF TAIWAN'S SILICON VALLEY,

    JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION, Issue 5 2001
    Wen-Cheng Huang
    ABSTRACT: The objective of this paper is to examine a deficit in water for the Hsinchu area, the location of Taiwan's "Silicon Valley." The methods suggested in this paper to diagnose water shortage problems are simple and practical. The results show that Hsinchu is in an area without sufficient water to meet demand for domestic and industrial uses. Until the completion of the Baoshan II Reservoir in 2006, the most feasible options for the Taiwan Water Supply Corporation to offset the water deficiency in Hsinchu City over the next five years are: (a) to obtain water gratuitously from the southern Yungheshan Reservoir; (b) to import additional water at an extra charge from other sources such as the northern Shihmen Reservoir and the agricultural sector; and (c) to conduct a comprehensive water conservation program at the Hsinchu Science-based Industrial Park. [source]


    HYDROLOGIC IMPLICATIONS OF GREATER GROUND-WATER RECHARGE TO LAS VEGAS VALLEY, NEVADA,

    JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION, Issue 5 2000
    David J. Donovan
    ABSTRACT: Published estimates of natural recharge in Las Vegas Valley range between 21,000 and 35,000 acre-feet per year. This study examined the underlying assumptions of previous investigations and evaluated the altitude-precipitation relationships. Period-of-record averages from high altitude precipitation gages established in the 1940s through the 1990s, were used to determine strong local altitude-precipitation relationships that indicate new total precipitation and natural recharge amounts and a new spatial distribution of that recharge. This investigation calculated about 51,000 acre-feet per year of natural recharge in the Las Vegas Hydrographic Basin, with an additional 6,000 acre-feet per year from areas tributary to Las Vegas Valley, for a total of 57,000 acre-feet per year. The total amount of natural recharge is greater than estimates from earlier investigations and is consistent with a companion study of natural discharge, which estimated 53,000 acre-feet per year of outflow. The hydrologic implications of greater recharge in Las Vegas Valley infer a more accurate ground-water budget and a better understanding of ground-water recharge that will be represented in a ground-water model. Thus model based ground-water management scenarios will more realistically access impacts to the ground-water system. [source]


    A NEW TEREBRATULID BRACHIOPOD SPECIES FROM THE SIEGENIAN OF THE DRA VALLEY, MOROCCO, AND ITS STRATIGRAPHIC, PALAEOGEOGRAPHIC AND PHYLOGENETIC SIGNIFICANCE

    PALAEONTOLOGY, Issue 4 2008
    MENA SCHEMM-GREGORY
    Abstract:, A new terebratulid brachiopod species, Rhenorensselaeria jansenii, has been identified in the Merzâ-Akhsaï Formation of the Dra Valley, Morocco, and the Grauwacke de Montguyon of the Amorican Massif, France. It is compared with the other known species of Rhenorensselaeria from Europe, Rh. strigiceps and Rh. demerathia, as well as with Rh. macgerriglei from North America, from which it differs in being larger and having coarser costae. Its possible life habit in clusters and its fossil community are compared with those of Rh. strigiceps from the Rheinisches Schiefergebirge (,Rhenish Slate Mountains'), Germany, which it most resembles. A new phylogeny of the subfamily Rhenorensselaerinae is constructed. The close phylogenetic relationship between Rh. jansenii and Rh. strigiceps confirms close palaeobiogeographical relationships between North Africa, France and the Rheinisches Schiefergebirge as well as a wider relationship between Central Europe and Gaspé, eastern Canada, during the Early Devonian. Taxa of Rhenorensselaeria are mainly restricted to the Middle and Upper Siegenian, although rare individuals have been found in the Lower Emsian of Central Europe and North America. Because of their abundance in the Dra Valley and Rheinisches Schiefergebirge and their short life span, rhenorensselaerid taxa can be regarded as important stratigraphical markers of Middle,Late Siegenian and Early Emsian sediments in North Africa and Central Europe. [source]


    Mediator mentors: Improving school climate, nurturing student disposition

    CONFLICT RESOLUTION QUARTERLY, Issue 1 2003
    Pamela S. Lane-Garon
    Mediator Mentors, a collaborative research and service project, was begun by California State University-Fresno faculty and the staff of an elementary school (K,8) in the Central San Joaquin Valley. The purpose of the research was to assess conflict resolution program effects on students (N = 300) and school climate. Cross-age mentoring is an important component of this collaborative project. University students preparing for roles in helping professions served as mentors to elementary students. Impacts on student cognitive and affective perspective taking were assessed and student perceptions of school safety were explored. [source]


    The Journal of the Society for Conservation Biology A global community of conservation professionals

    CONSERVATION BIOLOGY, Issue 2 2006
    Article first published online: 27 MAR 200
    Cover: Old-growth forest of the Hoh River Valley, Olympic National Park, Washington (U.S.A.). For decades the U.S. Pacific Norwest has been a center of controversy over logging and endangered species. This special section explores progress made by the Northwest Forest Plan,a global example of land-use planning,a decade after it was established to end the stalemate over logging and endangered species. Authors include some of the key architects involved in its creation and implementation. Photo by Kevin Schafer. See pages 274,374. [source]


    Spatial Tests of the Pesticide Drift, Habitat Destruction, UV-B, and Climate-Change Hypotheses for California Amphibian Declines

    CONSERVATION BIOLOGY, Issue 6 2002
    Carlos Davidson
    In California, the transport and deposition of pesticides from the agriculturally intensive Central Valley to the adjacent Sierra Nevada is well documented, and pesticides have been found in the bodies of Sierra frogs. Pesticides are therefore a plausible cause of declines, but to date no direct links have been found between pesticides and actual amphibian population declines. Using a geographic information system, we constructed maps of the spatial pattern of declines for eight declining California amphibian taxa, and compared the observed patterns of decline to those predicted by hypotheses of wind-borne pesticides, habitat destruction, ultraviolet radiation, and climate change. In four species, we found a strong positive association between declines and the amount of upwind agricultural land use, suggesting that wind-borne pesticides may be an important factor in declines. For two other species, declines were strongly associated with local urban and agricultural land use, consistent with the habitat-destruction hypothesis. The patterns of decline were not consistent with either the ultraviolet radiation or climate-change hypotheses for any of the species we examined. Resumen: Por mucho tiempo se ha sugerido que los pesticidas transportados por el viento son una causa de la declinación de anfibios en áreas sin destrucción de hábitat evidente. En California, el transporte y depósito de pesticidas provenientes del Valle Central, donde se practica la agricultura intensiva, hacia la Sierra Nevada adyacente está bien documentado y se han encontrado pesticidas en el cuerpo de ranas de la Sierra. Por lo tanto, los pesticidas son una causa verosímil de las declinaciones, pero a la fecha no se han encontrado relaciones directas entre los pesticidas y la declinación de anfibios. Construimos mapas de sistemas de información geográfica del patrón espacial de las declinaciones de ocho taxones de anfibios de California, y comparamos los patrones de declinación observados con los esperados por las hipótesis de pesticidas transportados por el viento, la destrucción del hábitat, la radiación ultravioleta y el cambio climático. En cuatro especies, encontramos una fuerte asociación positiva entre las declinaciones y la cantidad de tierras de uso agrícola en dirección contraria a los vientos, lo que sugiere que los pesticidas transportados por el viento pueden ser un factor importante en las declinaciones. Para otras dos especies, las declinaciones se asociaron contundentemente con el uso del suelo urbano y agrícola, lo cual es consistente con la hipótesis de la destrucción del hábitat. Los patrones de declinación no fueron consistentes con la hipótesis de la radiación ultravioleta ni la de cambio climático para ninguna de las especies examinadas. [source]


    An environment for prosperity and quality living accommodating growth in the Thames Valley

    CORPORATE SOCIAL RESPONSIBILITY AND ENVIRONMENTAL MANAGEMENT, Issue 1 2004
    Hugh Howes
    The Thames Valley is seen as the powerhouse of the British economy, and one of the best performing regions in Europe. This economic base offers opportunities for expansion with the potential for it to become the knowledge capital of Europe. Business interests view the area as a highly desirable location, not only because of its markets, skills and proximity to the City and Heathrow but also because of its high quality environment. Companies, however, complain of skills shortages, traffic congestion, lack of suitable premises and housing that is affordable to the workforce. Much of the Thames Valley is either Green Belt or Areas of Outstanding Natural Beauty. Furthermore, the availability of future water supplies, the maintenance of the quality of water in the rivers and managing flood risk are also likely to act as constraints on development in the future. How economic growth is to be achieved with minimal additional development and without detriment to the environment is the central question that is likely to dominate planning in the this region over the next few years. Is it possible to achieve more with existing resources? Copyright © 2004 John Wiley & Sons, Ltd and ERP Environment. [source]


    The geography of climate change: implications for conservation biogeography

    DIVERSITY AND DISTRIBUTIONS, Issue 3 2010
    D. D. Ackerly
    Abstract Aim, Climate change poses significant threats to biodiversity, including impacts on species distributions, abundance and ecological interactions. At a landscape scale, these impacts, and biotic responses such as adaptation and migration, will be mediated by spatial heterogeneity in climate and climate change. We examine several aspects of the geography of climate change and their significance for biodiversity conservation. Location, California and Nevada, USA. Methods, Using current climate surfaces (PRISM) and two scenarios of future climate (A1b, 2070,2099, warmer-drier and warmer-wetter), we mapped disappearing, declining, expanding and novel climates, and the velocity and direction of climate change in California and Nevada. We also examined fine-scale spatial heterogeneity in protected areas of the San Francisco Bay Area in relation to reserve size, topographic complexity and distance from the ocean. Results, Under the two climate change scenarios, current climates across most of California and Nevada will shrink greatly in extent, and the climates of the highest peaks will disappear from this region. Expanding and novel climates are projected for the Central Valley. Current temperature isoclines are projected to move up to 4.9 km year,1 in flatter regions, but substantially slower in mountainous areas because of steep local topoclimate gradients. In the San Francisco Bay Area, climate diversity within currently protected areas increases with reserve size and proximity to the ocean (the latter because of strong coastal climate gradients). However, by 2100 of almost 500 protected areas (>100 ha), only eight of the largest are projected to experience temperatures within their currently observed range. Topoclimate variability will further increase the range of conditions experienced and needs to be incorporated in future analyses. Main Conclusions, Spatial heterogeneity in climate, from mesoclimate to topoclimate scales, represents an important spatial buffer in response to climate change, and merits increased attention in conservation planning. [source]


    Heddleichthys, a new tristichopterid genus from the Dura Den Formation, Midland Valley, Scotland (Famennian, Late Devonian)

    ACTA ZOOLOGICA, Issue 2009
    Daniel Snitting
    Abstract A new tristichopterid genus, Heddleichthys, from the Famennian of Scotland is described based on material previously assigned to a number of different genera, including Glyptopomus, Gyroptychius and Eusthenopteron. The validity of the new genus is established by a discussion of the reasons for the invalidity of the previous assignments. Heddleichthys is characterized by a combination of derived and primitive tristichopterid features. Derived features include the presence of symphyseal dentary fangs and premaxillary pseudofangs, a diamond-shaped symmetric caudal fin, a low posterodorsal expansion of the maxilla, and a posteriorly positioned kite-shaped pineal series. Primitive features include a postorbital and jugal contribution to the orbital margin and a parasphenoid with a ventral keel. External dermal bones are rather poorly preserved in the referred material, with few easily discernible sutures. The holotype specimen, a three-dimensionally preserved skull, was scanned by computed tomography to reveal well-preserved internal dermal bones, including entopterygoids, vomers and parasphenoid. There is no preserved endoskeletal material. As the first representative of derived tristichopterids described from Britain, Heddleichthys lends support to the idea that faunal dispersion between Gondwana and Laurussia in the Late Devonian was widespread. Derived tristichopterids have been described from all continents except South America. In contrast, the basal tristichopterids Eusthenopteron and Tristichopterus are still only described from Laurussia. [source]


    Upper Pleistocene-Holocene geomorphic changes dictating sedimentation rates and historical land use in the valley system of the Chifeng region, Inner Mongolia, northern China

    EARTH SURFACE PROCESSES AND LANDFORMS, Issue 11 2010
    Y. Avni
    Abstract This study focuses on the late Quaternary landscape evolution in the Chifeng region of Inner Mongolia, China, its relations to the history of the Pleistocene-Holocene loess accumulation, erosion and redeposition, and their impact on human occupation. Based on 57 optically stimulated luminescence (OSL) ages of loess sediments, fluvial sand and floodplain deposits accumulated on the hill slopes and floodplains, we conclude that during most of the Pleistocene period the region was blanketed by a thick layer of aeolian loess, as well as by alluvial and fluvial deposits. The loess section is divided into two main units that are separated by unconformity. The OSL ages at the top of the lower reddish loess unit yielded an approximate age of 193,ka, roughly corresponding to the transition from MIS 7 to 6, though they could be older. The upper gray loess unit accumulated during the upper Pleistocene glacial phase (MIS 4,3) at a mean accumulation rate of 0·22,m/ka. Parallel to the loess accumulation on top of the hilly topography, active fans were operating during MIS 4,2 at the outlet of large gullies surrounding the major valley at a mean accumulation rate of 0·24,m/ka. This co-accumulation indicates that gullies have been a long-term geomorphic feature at the margins of the Gobi Desert since at least the middle Pleistocene. During the Holocene, the erosion of the Pleistocene loess on the hills led to the burial of the valley floors by the redeposited sediments at a rate that decreases from 3·2,m/ka near the hills to 1,0·4,m/ka1 in the central part of the Chifeng Valley. This rapid accumulation and the frequent shifts of the courses of the river prevented the construction of permanent settlements in the valley floors, a situation which changed only with improved man-made control of the local rivers from the tenth century AD. Copyright © 2010 John Wiley & Sons, Ltd. [source]


    Quantifying sediment storage in a high alpine valley (Turtmanntal, Switzerland)

    EARTH SURFACE PROCESSES AND LANDFORMS, Issue 13 2009
    Jan-Christoph Otto
    Abstract The determination of sediment storage is a critical parameter in sediment budget analyses. But, in many sediment budget studies the quantification of magnitude and time-scale of sediment storage is still the weakest part and often relies on crude estimations only, especially in large drainage basins (>100,km2). We present a new approach to storage quantification in a meso-scale alpine catchment of the Swiss Alps (Turtmann Valley, 110,km2). The quantification of depositional volumes was performed by combining geophysical surveys and geographic information system (GIS) modelling techniques. Mean thickness values of each landform type calculated from these data was used to estimate the sediment volume in the hanging valleys and the trough slopes. Sediment volume of the remaining subsystems was determined by modelling an assumed parabolic bedrock surface using digital elevation model (DEM) data. A total sediment volume of 781·3×106,1005·7×106,m3 is deposited in the Turtmann Valley. Over 60% of this volume is stored in the 13 hanging valleys. Moraine landforms contain over 60% of the deposits in the hanging valleys followed by sediment stored on slopes (20%) and rock glaciers (15%). For the first time, a detailed quantification of different storage types was achieved in a catchment of this size. Sediment volumes have been used to calculate mean denudation rates for the different processes ranging from 0·1 to 2·6,mm/a based on a time span of 10,ka. As the quantification approach includes a number of assumptions and various sources of error the values given represent the order of magnitude of sediment storage that has to be expected in a catchment of this size. Copyright © 2009 John Wiley & Sons, Ltd. [source]


    Influence of dynamic soil,structure interaction on the nonlinear response and seismic reliability of multistorey systems

    EARTHQUAKE ENGINEERING AND STRUCTURAL DYNAMICS, Issue 3 2007
    Armando Bárcena
    Abstract A set of reinforced concrete structures with gravitational loads and mechanical properties (strength and stiffness) representative of systems designed for earthquake resistance in accordance with current criteria and methods is selected to study the influence of dynamic soil,structure interaction on seismic response, ductility demands and reliability levels. The buildings are considered located at soft soil sites in the Valley of Mexico and subjected to ground motion time histories simulated in accordance with characteristic parameters of the maximum probable earthquake likely to occur during the system's expected life. For the near-resonance condition the effects of soil,structure interaction on the ductility demands depend mainly on radiation damping. According to the geometry of the structures studied this damping is strongly correlated with the aspect ratio, obtained by dividing the building height by its width. In this way, for structures with aspect ratio greater than 1.4 the storey and global ductility demands increase with respect to those obtained with the same structures but on rigid base, while for structures with aspect ratio less than 1.4 the ductility demands decrease with respect to those for the structures on rigid base. For the cases when the fundamental period of the structure has values very different from the dominant ground period, soil,structure interaction leads in all cases to a reduction of the ductility demands, independently of the aspect ratio. The reliability index , is obtained as a function of the base shear ratio and of the seismic intensity acting on the nonlinear systems subjected to the simulated motions. The resulting reliability functions are very similar for systems on rigid or on flexible foundation, provided that in the latter case the base rotation and the lateral displacement are removed from the total response of the system. Copyright © 2006 John Wiley & Sons, Ltd. [source]


    Seismic reliability functions for multistorey frame and wall-frame systems

    EARTHQUAKE ENGINEERING AND STRUCTURAL DYNAMICS, Issue 15 2006
    Jorge L. Alamilla
    Abstract Seismic reliability functions of multistorey frame systems are expressed as values of Cornell's ,index in terms of two alternative measures of the earthquake intensity, normalized with respect to the yield displacement or to the deformation capacity of a simplified model of the global behaviour of the system obtained by pushover analysis. The safety margin is defined as the difference of the natural logarithms of the intensity that leads to collapse and that assumed to act on the system. The problem of defining a deformation capacity for a multistorey system is circumvented in this manner. The method proposed is illustrated through its application to several reinforced concrete rigid frames, including both column-and-beam and wall-frame systems. Ground motion excitations are representative of those recorded at soft soil sites in the Valley of Mexico. A comparison is made of the reliability functions obtained on the basis of the gross section or the cracked section of reinforced concrete members. The results show that the reliability functions do not only depend on the expected values of the normalized intensity, but also on its dispersion, which is sensitive to the ratio of the fundamental period of the system to the dominant period of the ground motion. Some comments are presented about the establishment of reliability-based seismic design criteria for generic systems. Copyright © 2006 John Wiley & Sons, Ltd. [source]


    Semi-empirical model for site effects on acceleration time histories at soft-soil sites.

    EARTHQUAKE ENGINEERING AND STRUCTURAL DYNAMICS, Issue 13 2004
    Part 2: calibration
    Abstract A previously developed simplified model of ground motion amplification is applied to the simulation of acceleration time histories at several soft-soil sites in the Valley of Mexico, on the basis of the corresponding records on firm ground. The main objective is to assess the ability of the model to reproduce characteristics such as effective duration, frequency content and instantaneous intensity. The model is based on the identification of a number of parameters that characterize the complex firm-ground to soft-soil transfer function, and on the adjustment of these parameters in order to account for non-linear soil behavior. Once the adjusted model parameters are introduced, the statistical properties of the simulated and the recorded ground motions agree reasonably well. For the sites and for the seismic events considered in this study, it is concluded that non-linear soil behavior may have a significant effect on the amplification of ground motion. The non-linear soil behavior significantly affects the effective ground motion duration for the components with the higher intensities, but it does not have any noticeable influence on the lengthening of the dominant ground period. Copyright © 2004 John Wiley & Sons, Ltd. [source]


    Identification of soil degradation during earthquake excitations by Bayesian inference

    EARTHQUAKE ENGINEERING AND STRUCTURAL DYNAMICS, Issue 6 2003
    Jianye Ching
    Abstract A Bayesian inference approach is introduced to identify soil degradation behaviours at four downhole array sites. The approach of inference is based on a parametric time-varying infinite impulse response filter model. The approach is shown to be adaptive to the changes of filter parameters and noise amplitudes. Four sites, including the Lotung (Taiwan), Chiba (Japan), Garner Valley (California), and Treasure Island (California) sites with downhole seismic arrays are analysed. Our results show two major types of soil degradation behaviour: the well-known strain-dependent softening, and reduction in stiffness that is not instantaneously recoverable. It is also found that both types of soil degradation are more pronounced in sandy soils than in clayey soils. The mechanism for the second type of soil degradation is not yet clear to the authors and suggested to be further studied. Copyright © 2003 John Wiley & Sons, Ltd. [source]


    Fragmentation, habitat composition and the dispersal/predation balance in interactions between the Mediterranean myrtle and avian frugivores

    ECOGRAPHY, Issue 1 2010
    Juan P. González-Varo
    Human-induced fragmentation and disturbance of natural habitats can shift abundance and composition of frugivore assemblages, which may alter patterns of frugivory and seed dispersal. However, despite their relevance to the functioning of ecosystems, plant-frugivore interactions in fragmented areas have been to date poorly studied. I investigated spatial variation of avian frugivore assemblages and fruit removal by dispersers and predators from Mediterranean myrtle shrubs (Myrtus communis) in relation to the degree of fragmentation and habitat features of nine woodland patches (72 plants). The study was conducted within the chronically fragmented landscape of the Guadalquivir Valley (SW Spain), characterized by ~1% of woodland cover. Results showed that the abundance and composition of the disperser guild was not affected by fragmentation, habitat features or geographical location. However, individual species and groups of resident/migrant birds responded differently: whereas resident dispersers were more abundant in large patches, wintering dispersers were more abundant in fruit-rich patches. Predator abundances were similar between patches, although the guild composition shifted with fragmentation. The proportion of myrtle fruits consumed by dispersers and predators varied greatly between patches, but did not depend on bird abundances. The geographical location of patches determined the presence or absence of interactions between myrtles and seed predators (six predated and three non-predated patches), a fact that greatly influenced fruit dispersal success. Moreover, predation rates were lower (and dispersal rates higher) in large patches with fruit-poor heterospecific environments (i.e. dominated by myrtle). Predator satiation and a higher preference for heterospecific fruits by dispersers may explain these patterns. These results show that 1) the frugivore assemblage in warm Mediterranean lowlands is mostly composed of fragmentation-tolerant species that respond differently to landscape changes; and 2) that the feeding behaviour of both dispersers and predators influenced by local fruit availability may be of great importance for interpreting patterns of frugivory throughout the study area. [source]


    Relating streamflow characteristics to specialized insectivores in the Tennessee River Valley: a regional approach,

    ECOHYDROLOGY, Issue 4 2008
    Rodney R. Knight
    Abstract Analysis of hydrologic time series and fish community data across the Tennessee River Valley identified three hydrologic metrics essential to habitat suitability and food availability for insectivorous fish communities in streams of the Tennessee River Valley: constancy (flow stability or temporal invariance), frequency of moderate flooding (frequency of habitat disturbance), and rate of streamflow recession. Initial datasets included 1100 fish community sites and 300 streamgages. Reduction of these datasets to sites with coexisting data yielded 33 sites with streamflow and fish community data for analysis. Identification of critical hydrologic metrics was completed using a multivariate correlation procedure that maximizes the rank correlation between the hydrologic metrics and fish community resemblance matrices. Quantile regression was used to define thresholds of potential ranges of insectivore scores for given values of the hydrologic metrics. Increased values of constancy and insectivore scores were positively correlated. Constancy of streamflow maintains wetted perimeter, which is important for providing habitat for fish spawning and increased surface area for invertebrate colonization and reproduction. Site scores for insectivorous fish increased as the frequency of moderate flooding (3 times the median annual streamflow) decreased, suggesting that insectivorous fish communities respond positively to less frequent disturbance and a more stable habitat. Increased streamflow recession rates were associated with decreased insectivore scores. Increased streamflow recession can strand fish in pools and other areas that are disconnected from flowing water and remove invertebrates as food sources that were suspended during high-streamflow events. Copyright © 2008 John Wiley & Sons, Ltd. [source]


    A dam problem: simulated upstream impacts for a Searsville-like watershed

    ECOHYDROLOGY, Issue 4 2008
    Christopher S. Heppner
    Abstract The integrated hydrology model (InHM), a physics-based hydrologic-response model with sediment-transport capabilities, was used to simulate upstream impacts from dam construction/removal for a generalized approximation of the Searsville watershed in Portola Valley, California. Four 10-year simulation scenarios (pre-dam, early dam, current and post-dam) were considered. Each scenario was simulated using the same sequence of synthetically generated rainfall and evapotranspiration. For each scenario the boundary-value problem was constructed based on the available watershed information (e.g. topography, soils, geology, reservoir bathymetry and land use). The results from the simulations are presented in terms of the temporal and spatial characteristics of hydrologic response and sediment transport. The commonalities/differences between the four Searsville-like watershed scenarios are discussed. The effort demonstrates that heuristic physics-based simulation can be a useful tool for the characterization of dam-related impacts at the watershed scale. Copyright © 2008 John Wiley & Sons, Ltd. [source]


    Water quality, nutrient, phytoplankton and microcrustacean responses to watering of private wetlands in the Murray Valley, New South Wales

    ECOLOGICAL MANAGEMENT & RESTORATION, Issue 2 2009
    Sylvia Zukowski
    First page of article [source]


    Using a Geographic Information System to identify areas with potential for off-target pesticide exposure

    ENVIRONMENTAL TOXICOLOGY & CHEMISTRY, Issue 8 2006
    Thomas G. Pfleeger
    Abstract In many countries, numerous tests are required as part of the risk assessment process before chemical registration to protect human health and the environment from unintended effects of chemical releases. Most of these tests are not based on ecological or environmental relevance but, rather, on consistent performance in the laboratory. A conceptual approach based on Geographic Information System (GIS) technology has been developed to identify areas that are vulnerable to nontarget chemical exposure. This GIS-based approach uses wind speed, frequency of those winds, pesticide application rates, and spatial location of agricultural crops to identify areas with the highest potential for pesticide exposure. A test scenario based on an incident in Idaho (USA) was used to identify the relative magnitude of risk from off-target movement of herbicides to plants in the conterminous United States. This analysis indicated that the western portion of the Corn Belt, the central California valley, southeastern Washington, the Willamette Valley of Oregon, and agricultural areas bordering the Great Lakes are among those areas in the United States that appear to have the greatest potential for off-target movement of herbicides via drift. Agricultural areas, such as the Mississippi River Valley and the southeastern United States, appears to have less potential, possibly due to lower average wind speeds. Ecological risk assessments developed for pesticide registration would be improved by using response data from species common to high-risk areas instead of extrapolating test data from species unrelated to those areas with the highest potential for exposure. [source]


    Emission of legacy chlorinated pesticides from agricultural and orchard soils in British Columbia, Canada

    ENVIRONMENTAL TOXICOLOGY & CHEMISTRY, Issue 6 2006
    Terry F. Bidleman
    Abstract Air samples were collected above agricultural fields in the Fraser Valley and orchards in the Okanagan Valley, British Columbia, Canada, to investigate volatilization of organochlorine pesticides used in the past. Concentrations of pesticides in air were elevated over soils that contained higher residues. Soil/air fugacity ratios at sites with the higher soil residues were calculated relative to air sampled at 40 cm height and background air. The fugacity ratios in the first case indicated net volatilization or soil-air equilibrium for most compounds and occasional net deposition for p,p, -dichlorodiphenyldichloroethene (p,p, -DDE), whereas those in the second case showed a strong potential for net volatilization of all compounds. The enantiomer fraction (EF) of chiral compounds ,-hexachlorocyclohexane (,-HCH), trans -chlordane, cis -chlordane, and o,p, -DDT were determined in overlying air samples and soils. Enantiomer fractions in air corresponded to those in soils at fields in which soil concentrations were high but were decoupled from soil signatures at fields with low soil residues. Mean EFs in air sampled over soils were significantly (p < 0.001) nonracemic for ,-HCH and the chlordanes and agreed with published EFs in regional ambient air. The mean EF of o,p, -DDT for all air samples did not show a significant deviation from racemic EFs (p > 0.2), but EFs of individual samples reflected the ambivalent nature of o,p, -DDT degradation, sometimes preferring the (+) enantiomer and other times the (,) enantiomer. The study indicates that soils are continuing to emit "legacy" pesticides into the regional atmosphere. [source]


    Linear alkylbenzenes in muscle tissues of white croaker near a large ocean outfall in southern California, USA

    ENVIRONMENTAL TOXICOLOGY & CHEMISTRY, Issue 2 2001
    Charles R. Phillips
    Abstract Muscle tissues of a bottom-dwelling marine fish, white croaker (Genyonemus lineatus), collected near a large wastewater outfall in southern California, USA, were analyzed for long-chain linear alkylbenzenes (LABs). Total LABs (summed concentrations of C11 through C14 isomers) were highest (166,748 ng g,1 wet wt) in individuals collected in the immediate vicinity of the Orange County Sanitation District (OCSD; Fountain Valley, CA, USA) outfall diffuser, whereas relatively lower concentrations occurred in fish from mid-shelf and inshore locations at distances of 2.5 and 5 km, respectively, from the outfall. Fish tissue LAB concentrations were roughly proportional to sediment LAB concentrations at the respective collection sites. The extent of LAB degradation, as determined by ratios of internal to external C12 isomers, did not appear to relate to LAB concentrations or sampling location. Tissue DDT and PCB concentrations were not significantly correlated with LABs and, thus, did not appear to relate to recent exposures to sewage residues from the OCSD discharge. Measurements of LAB concentrations in fish tissues may be widely applicable as a monitoring tool for interpreting exposures to sewage discharges. [source]


    Hourly surface wind monitor consistency checking over an extended observation period

    ENVIRONMETRICS, Issue 4 2009
    Scott Beaver
    Abstract A consistency checking methodology is presented to aid in identifying biased values in extended historical records of hourly surface wind measurements obtained from a single station. The method is intended for screening extended observation periods for values which do not fail physical consistency checks (i.e., standard or complex quality assurance methods), yet nonetheless exhibit statistical properties which differ from the bulk of the record. Several specific types of inconsistencies common in surface wind monitoring datasets are considered: annual biases, unexpected values, and discontinuities. The purely empirical method checks for self-consistency in the temporal distribution of the wind measurements by explicitly modeling the diurnal variability. Each year of data is modeled using principal component analysis (PCA) (or empirical orthogonal functions, EOF), then hierarchical clustering with nearest neighbor linkage is used to visualize any annual biases existing in the measurements. The diurnal distributions for wind speed and direction are additionally estimated and visualized to determine any periods of time which are inconsistent with the typical diurnal cycle for a given monitor. The robust consistency checking method is applied to a set of 44 monitors operating in the San Joaquin Valley (SJV) of Central California over a 9-year period. Monitors from the SLAMS, CIMIS, and RAWS networks are considered. Similar inconsistencies are detected in all three networks; however, network-specific types of inconsistencies are found as well. Copyright © 2008 John Wiley & Sons, Ltd. [source]


    Ethnography, Comparison, and Changing Times

    ETHOS, Issue 4 2005
    ROBERT I. LEVY
    This article, based on Levy's Distinguished Lecture at the 2001 meeting of the Society for Psychological Anthropology, summarizes his views on how the psychologies of actors and the community forms and structures in which they are embedded, dancers and their dances, are mutually constituted. In particular, he contrasts two distinct communities where he did field research: Piri, a small village in French Polynesia; and Bhaktapur, a religious city in the Kathmandu Valley of Nepal, suggesting that the particular cultures of these two places give rise to different forms of public life and childrearing, resulting in differing kinds of learning during childhood and ultimately in distinctive experiences of the self. [source]


    Pine mistletoe (Viscum album ssp. austriacum) contributes to Scots pine (Pinus sylvestris) mortality in the Rhone valley of Switzerland

    FOREST PATHOLOGY, Issue 5 2006
    M. Dobbertin
    Summary In recent years unusual high mortality of Scots pine (Pinus sylvestris) has been observed in the Swiss Rhone Valley. The exact causes, however, are not known. At a 2-ha monitoring plot, tree mortality and crown condition have been monitored since 1996. Between 1996 and 2004, 59% of the Scots pines died, most of them following the drought periods 1996,1998 and 2003,2004, while only 15% of the deciduous trees died. Crown transparency, needle discolouration, dead branch percentage, mistletoe (Viscum album ssp. austriacum) rating, Tomicus sp. shoot feeding, male flowering effect, tree stem diameter, crown shading and social tree class assessed in 1998 were used in a logistic regression model to predict tree mortality. Crown transparency, mistletoe rating and percentage of dead branches were found significant in the model and the probability of tree mortality increased with increasing rankings of these parameters. Needle discolouration could be used to substitute ,dead branch percentage' as predictor. While crown transparency increased with mistletoe rating, for trees in the same transparency class, trees with medium and heavy mistletoe infection were two to four times more likely to die than trees with no or only low mistletoe infection. For the surviving trees we found that trees with mistletoes showed a significantly higher increase in transparency in the year following a drought than trees without, while in a drought year the opposite was true. At the beginning of the observations no significant differences in transparency had been found between the trees with and without mistletoe. However, by the end of the observation period trees with mistletoe had significantly higher crown transparency. We conclude that mistletoe infection can be considered as both a predisposing factor for tree death, by increasing needle loss following drought and a contributing factor by increasing water stress during drought. Résumé Une forte mortalité des pins sylvestres (Pinus sylvestris) a été observée ces dernières années dans la vallée du Rhône en Suisse. Les causes exactes n'en sont pas connues. La mortalité des arbres et l'état des houppiers ont été suivis depuis 1996 dans une parcelle de 2 ha. Entre 1996 et 2004, 59% des pins sylvestres sont morts, la plupart après les périodes de sécheresse de 1996,98 et 2003,2004, comparéà 15% pour les feuillus. La transparence des houppiers, le jaunissement des aiguilles, le pourcentage de mortalité de branches, une note d'importance du gui (Viscum album ssp. austriacum), les attaques d'alimentation sur pousses par Tomicus sp., la floraison mâle, le diamètre du tronc, l'ombrage du houppier et le statut social des arbres, mesurés en 1998, ont été utilisés dans un modèle de régression logistique pour prédire la mortalité des arbres. La transparence des houppiers, le taux de gui et le pourcentage de branches mortes sont des variables significatives, dont l'augmentation est associée à une augmentation de la probabilité de mortalité des arbres. Le jaunissement des aiguilles pourrait être substituée à la mortalité des branches comme variable prédictrice. Tandis que la transparence des houppiers augmente avec le taux de gui, au sein de la même classe de transparence, les arbres avec une infestation de gui moyenne à forte ont une probabilité de mortalité 2 à 4 fois plus élevée que les arbres à infestation faible ou nulle. Chez les arbres survivants, on observe que les arbres porteurs de gui ont une augmentation plus forte de la transparence du houppier l'année suivant une sécheresse que les arbres sans gui, l'inverse étant vrai pendant une année sèche. La différence de transparence des houppiers entre arbres porteurs de gui et arbres sans gui n'était pas significative au début des observations, alors qu'à la fin de la période, les arbres avec gui ont une transparence plus forte. Nous concluons que l'infestation par le gui peut être considérée à la fois comme un facteur prédisposant à la mortalité, en augmentant la perte d'aiguilles après sécheresse, et un facteur contribuant, en augmentant le stress hydrique pendant la sécheresse. Zusammenfassung Seit einigen Jahren werden im Schweizer Rhonetal hohe Absterberaten der gemeinen Kiefer (Pinus sylvestris L.) beobachtet. Die genauen Ursachen sind bis jetzt unbekannt. Auf der zwei Hektar grossen langfristigen Waldökosystemfläche (LWF) Visp werden seit 1996 jährlich Absterberaten, Kronenverlichtung, Mistelbefall (Viscum album ssp. austriacum) und andere Symptome aufgenommen. Zwischen 1996 und 2004 sind 59% aller Föhren auf der Fläche abgestorben, die meisten nach den Trockenperioden 1996,98 und 2003,2004. Dagegen starben nur 15% der Laubbäume ab. Kronenverlichtung, Nadelverfärbung, Totast- und Totzweiganteil (als Indikatoren der Vitalität des Baumes), Mistelbefallsklasse, Triebabwurf durch Waldgärtner, männliche Blütenbildung, Stammdurchmesser, Kronenkonkurrenz und soziale Stellung, alle im Jahr 1998 erhoben, wurden in einer logistischen Regression zur Bestimmung der Absterbewahrscheinlichkeit auf Signifikanz getestet. Kronenverlichtung, Mistelbefallsklasse und Totastanteil waren in dem Model signifikant. Die Wahrscheinlichkeit des Absterbens stieg dabei mit ansteigender Kronenverlichtung, ansteigendem Mistelbefall und ansteigendem Totastanteil. Der Totastanteil konnte im Model durch die Nadelverfärbung ersetzt werden. Die Kronenverlichtung stieg mit dem Mistelbefall an. Bei gleicher Verlichtung starben jedoch Bäume mit mittlerem und starkem Mistelbefall zwei- bis viermal häufiger ab als Bäume ohne oder mit leichtem Mistelbefall. Von den überlebenden Bäumen zeigten solche mit Mistelbefall einen deutlichen Anstieg der Transparenz im Jahr nach Beginn der Trockenheit im Vergleich zu den Bäumen ohne Misteln, während im Jahr der Trockenheit das Umgekehrte der Fall war. Zu Beginn der Beobachtung ergaben sich keine signifikanten Unterschiede in der Kronentransparenz der überlebenden Bäume mit und ohne Misteln. Am Ende der Beobachtungsperiode wiesen jedoch die Bäume mit Misteln signifikant höhere Kronenverlichtungen auf. Wir schliessen daraus, dass die Misteln auf der einen Seite den Baum langfristig schwächen, indem sie zur Reduzierung der Nadelmasse führen und sie auf der anderen Seite während Trockenheit durch erhöhten Wasserstress zum vorzeitigen Absterben beitragen. [source]


    Ammonoids from the Dalle des Iridet of the Mouydir and Ahnet (Central Sahara) and the Formation d'Hassi Sguilma of the Saoura Valley (Late Tournaisian,Early Viséan; Algeria)

    FOSSIL RECORD-MITTEILUNGEN AUS DEM MUSEUM FUER NATURKUNDE, Issue 1 2010
    Dieter Korn
    Abstract Four ammonoid species are described from the Early Carboniferous (Mississippian) Iridet Formation of the Ahnet and Mouydir (Central Sahara, Algeria); three of which are new: Eurites temertassetensis n. sp., Trimorphoceras teguentourense n. sp., and Trimorphoceras azzelmattiense n. sp. The species can be attributed to the North African Ammonellipsites - Merocanites Assemblage (Fascipericyclus - Ammonellipsites Genus Zone; Late Tournaisian to Early Viséan). Additionally, the two new species Ammonellipsites sguilmensis n. sp. and Muensteroceras beniabbesense n. sp. are described from the time equivalent Hassi Sguilma Formation of the Saoura Valley (north-western Algeria). (© 2010 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim) [source]