Erratum     

Rudolf H. Steiger  Gorica Harnik-?optrajanova  Emil Zimmermann  Niels Henriksen 《Mineralogy and Petrology》1991,43(4):315-315

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Über den Transmissionsfaktor der Globalstrahlung und seine Abhängigkeit vom Aerosol     

Rudolf Schulze 《Pure and Applied Geophysics》1962,51(1):205-213

Zusammenfassung Es wird der Transmissionsfaktor der Globalstrahlung alsm ^te-Wurzel der relativen Bestrahlung (gemessene Globalstrahlung/I _o sinh) definiert. Die Auswertung von Meßreihen gemäß dieser Definition führt zu Transmissionsfaktoren zwischen 0.8 bis 0.9 Eine theoretische Überprüfung führt zu dem gleichen, Ergebnis.

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Summary The transmission factor of the total radiation is defined likem ^th root of relative irradiation (measured total radiation/I _o sinh). The evaluation of measuring series according to the definition yields transmission factors between 0.8–0.9. A theoretical trial yields the same results.

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Kryptovulkanische oder Injektionsbeben     

Rudolf Hoernes 《International Journal of Earth Sciences》1911,2(7):382-410

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Bücher- und Zeitschriftenschau     

Bubnoff  R. Brinkmann  Wilckens  Rudolf Leutelt  Salomon-Calvi 《International Journal of Earth Sciences》1931,22(2):133-138

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Der Bau des Französischen Zentralplateaus     

von Gaertner  Hans Rudolf 《International Journal of Earth Sciences》1937,28(1-2):48-68

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Die Gipfelflur der Alpen     

Rudolf Leutelt 《International Journal of Earth Sciences》1929,20(4-5):330-337

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Mitteilungen     

F. Rudolf Jung 《Ocean Dynamics》1949,2(6):298-300

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Mitteilungen     

F. Rudolf Jung 《Ocean Dynamics》1948,1(2-3):106-108

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Buchbesprechungen     

Rudolf Braun  H. Woker  K. Wubrmann  O. Steinböck 《Aquatic Sciences - Research Across Boundaries》1953,15(1):213-219

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Groundwater fluctuations and footslope ferricrete soils in the humid tropical zone of southern Cameroon     

Emile Temgoua  Henri‐Bosko Djeuda Tchapnga  Emile Tanawa  Claire Guenat  Hans‐Rudolf Pfeifer 《水文研究》2005,19(16):3097-3111

This paper discusses the relationship between the differentiation of ferruginous accumulations and the variable water saturation of footslope soil patterns. An analysis of the slope morphology of a typical hill in the forest zone of southern Cameroon and a seasonal survey of the levels of groundwaters, springs and rivers were considered in relation to the petrology of different soil patterns. The study site is a tabular hillock whose slopes present a progressive development from steep to gentle slopes. The variable residence time of water within the soil, creating an alternation of reducing and oxidizing conditions, affects soil chemistry, structure and lateral extension of the soil patterns. The ferruginous soil patterns, being formed on the footslopes, gradually increase in extent with decreasing slope angle and the relative rise of the groundwater level. The steep footslopes, where groundwater has a shorter residence time, show a soft mottled clay pattern, restricted to the bottom part of the slope. The moderate footslopes exhibit a deep permanent and a temporary perched groundwater table. The latter, with its regular capillary fringe, contributes to more reducing conditions within isolated domains in the soil patterns, and thus to the alternation with oxidizing conditions, generating a continuous hard soil pattern (massive carapace). The more gently dipping footslopes exhibit groundwater levels near the surface and also a significant amplitude of groundwater fluctuation. Iron, previously accumulated in moderate footslope patterns, is reduced, remobilized, and leached. The soil patterns formed develop into a variegated carapace, more extended along the slope, containing less iron, but nevertheless more hardened, due to the important fluctuations of the groundwater table. These patterns are limited to the zone of groundwater fluctuation and deteriorate as the water fluctuation zone recedes. Copyright © 2005 John Wiley & Sons, Ltd.  相似文献