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211.
Results of the DEKORP 1 (BELCORP-DEKORP) deep seismic reflection studies in the western part of the Rhenish Massif 总被引:1,自引:0,他引:1
DEKORP Research GroupH.-J. Anderle R. Bittner R. Bortfeld J. Bouckaert G. Büchel G. Dohr H.-J. Dürbaum H. Durst W. Fielitz E. Flüh T. Gundlach L. Hance A. Henk F. Jordan D. Kläschen M. Klöckner R. Meissner W. Meyer O. Oncken C. Reichert K.-H. Ribbert P. Sadowiak H.-U. Schmincke J. Schmoll R. Walter K. Weber U. Weihrauch Th. Wever 《Geophysical Journal International》1991,106(1):203-227
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Vertical profiles of dissolved Al in the Atlantic Ocean and Mediterranean Sea are presented. Although dissolved Al appears to be involved in the biochemical cycle of elements, Al does not behave solely as a nutrient within the oceans. Physico-chemical processes (i.e. adsorption and/or chemical precipitation) control the concentration and distribution of Alaq within the deep waters.A tentative mass balance model of Alaq in the oceanic system is proposed that takes into account all of the presently known fluxes of Alaq to and through the oceans. To maintain the deep waters of the ocean at steady state, it is necessary to include in the model, processes that remove Alaq from these waters. Thus, model calculations support the conclusions drawn from observations that physico-chemical processes remove Alaq from deep waters. Finally, the proposed model is compatible with the concept that the entire oceanic system is at steady state with respect to dissolved Al. 相似文献
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215.
Marc Stoffyn 《Estuarine, Coastal and Shelf Science》1984,18(4):433-445
Concentrations of the trace elements Fe, Al, Mn, Cu, Cd, Zn and Ni were measured in shallow vertical profiles (maximum depth 500 m) off the Scotian Shelf in the western North Atlantic. The distributions of the trace elements show variations with depth, the most consistent of which are for Fe and Zn. A minimum concentration near the surface followed by an increase with depth is attributed to in situ mechanisms. 相似文献
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217.
Marc Schoeller 《Journal of Hydrology》1976,28(1):45-52
The relationship line between two chemical constituents dissolved in groundwater does not always begin at the graph origin, but at a fixed coordinates point. This allows the separation between rain water, infiltrating water and groundwater. Besides, this relationship line is not always linear. Equations are given for the curvilinear case. 相似文献
218.
Christian Kofler Volkmar Mair Stephan Gruber Maria Cristina Todisco Ian Nettleton Stefan Steger Marc Zebisch Stefan Schneiderbauer Francesco Comiti 《地球表面变化过程与地形》2021,46(7):1311-1327
The fronts of two rock glaciers located in South Tyrol (Italian Alps) failed on 13 August 2014, initiating debris flows in their downslope channels. A multimethod approach including climate, meteorological, and ground temperature data analysis, aerial image correlation, as well as geotechnical testing and modeling, led to the reconstruction of the two events. An integrated investigation of static predisposing factors, slowly changing preparatory factors, and potential triggering events shed light on the most likely reasons for such failures. Our results suggest that the occurrence of front destabilization at the two rock glaciers can only partly be explained by the occurrence of heavy rainfall events. Indeed, antecedent hydrological and thermal ground conditions were characterized by a saturated active layer favored by a snow-rich winter and extensive precipitation in late spring and summer. Also, the rising trend of air temperature during spring and summer months since 1950s might explain the concurrent marked displacement of the two rock glaciers. Indeed, geotechnical investigations have provided strong indications that one of the investigated rock glacier fronts was at a marginally stable state prior to 2014. As rainfall events more intense than the one that occurred in August 2014 were previously recorded in the same area without resulting failures at the studied rock glaciers, we propose that both predisposing and preparatory destabilizing factors have played a key role in the 2014 rock glacier front failures. 相似文献
219.
Grinson George Dattesh V. Desai Chetan A. Gaonkar V. M. Aboobacker P. Vethamony Arga Chandrashekar Anil 《Journal of Oceanography》2013,69(4):451-466
A two-dimensional hydrodynamic and particle tracking model was used to estimate the dispersion and retention of barnacle larvae from their possible spawning sites in a tropical monsoon-influenced estuarine system (central west coast of India). Validation of the hydrodynamic simulations yielded a good match with field measurements. The pattern of larval dispersal in the region varied with the winds and currents. The seasonal changes in abundance could be attributed to physical forcing and weather conditions. The extent of barnacle larval dispersal from spawning sites varied from 10 to 78 km for different sites and seasons. During a 24-h cycle, the larval abundance showed one to two peaks in the estuarine area. The increased larval abundance is favored by the flood currents, pushing the larvae into the estuary. Physical forcing in the region helps in transport of the larvae from their spawning sites hugging to the coast and contributing to the population within the estuary. Field observations and numerical experiments suggest the occurrence of higher larval abundance in the estuary during post-monsoon. The dispersal pattern indicated that the barnacle population present in the estuary is well mixed, and with a seasonally changing pattern. 相似文献
220.