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41.
The carbonate-rock aquifer in the Great Valley, West Virginia, USA, was evaluated using a database of 687 sinkholes and 350
specific capacity tests to assess structural, lithologic, and topographic influences on the groundwater flow system. The enhanced
permeability of the aquifer is characterized in part by the many sinkholes, springs, and solutionally enlarged fractures throughout
the valley. Yet, vertical components of subsurface flow in this highly heterogeneous aquifer are currently not well understood.
To address this problem, this study examines the apparent relation between geologic features of the aquifer and two spatial
indices of enhanced permeability attributed to aquifer karstification: (1) the distribution of sinkholes and (2) the occurrence
of wells with relatively high specific capacity. Statistical results indicate that sinkholes (funnel and collapse) occur primarily
along cleavage and bedding planes parallel to subparallel to strike where lateral or downward vertical gradients are highest.
Conversely, high specific capacity values are common along prominent joints perpendicular or oblique to strike. The similarity
of the latter distribution to that of springs suggests these fractures are areas of upward-convergent flow. These differences
between sinkhole and high specific capacity distributions suggest vertical flow components are primarily controlled by the
orientation of geologic structure and associated subsurface fracturing. 相似文献
42.
Kurt Heinrichs 《Environmental Geology》2008,56(3-4):643-675
Studies of many years—combining in situ investigation and laboratory analysis—have provided comprehensive information on weathering damage on the rock-cut monuments in the ancient city of Petra in Jordan. These rock-cut monuments represent outstanding world heritage. Many hundred monuments were carved by the Nabataeans from bedrock about 2000 years ago. The awareness of increasing weathering damage on the monuments has resulted in international efforts towards their preservation. The damage diagnosis has addressed the complex mutual relationships between stone types, stone properties, monument exposure regimes, environmental influences, weathering phenomena, development and extent of weathering damage and weathering progression. The rocks were classified lithostratigraphically and petrographically. Results on weathering forms, weathering profiles and weathering products obtained from monument mapping, in situ measurements and laboratory studies revealed a complex diversity of weathering phemomena with respect to type and intensity. Damage categories and damage indices were used to create a reproducible quantitative rating of weathering damage. Detailed results on weathering forms allowed the characterization and quantification of weathering progression including weathering prognoses. Stone properties and states of weathering damage were jointly considered for the rating of the rocks’ susceptibility to weathering. The systematic evaluation of weathering damage and monument exposure regimes can enhance the assessment of weathering factors and processes. 相似文献
43.
Kurt Leuchs 《International Journal of Earth Sciences》1914,5(2):81-87
Ohne Zusammenfassung 相似文献
44.
Kurt Leuchs 《International Journal of Earth Sciences》1913,4(1):15-42
Ohne Zusammenfassung 相似文献
45.
Kurt Leuchs 《International Journal of Earth Sciences》1928,19(1):72-75
Ohne Zusammenfassung 相似文献
46.
Kurt Foucar 《International Journal of Earth Sciences》1937,28(5):448-450
Ohne Zusammenfassung 相似文献
47.
Kurt Leuchs 《International Journal of Earth Sciences》1940,31(1-2):70-76
Ohne Zusammenfassung 相似文献
48.
Prof. Dr. Kurt Wegener 《Pure and Applied Geophysics》1951,19(3-4):170-172
Zusammenfassung Die Solarkonstante 2.4 wird begründet.
Summary The true solar constant 2.4 is proved.相似文献
49.
Prof. Dr. Kurt Wegener 《Pure and Applied Geophysics》1951,20(1):85-85
Ohne Zusammenfassung 相似文献
50.