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91.
Xavier Bruna Catarino Egydio-Silva Marcos Sadowski Georg Robert de Assis Silva Bruno Takara Victor Junji 《Geotechnical and Geological Engineering》2022,40(3):1345-1361
Geotechnical and Geological Engineering - To optimize the prediction of structural geological conditions in the underground as of data collected at the surface, due to the usual great uncertainties... 相似文献
92.
利用一个微波辐射传输模式,晴天下的大气探测廓线,地面的部分观测资料以及卫星观测的亮温,计算了淮河流域能量和水循环实验(HUBEx)中,寿县地区的热带降雨观测卫星微波成像仪(TRMM/TMI)微波频率的地表比辐射率。通过比较所计算的微波地表比辐射率随地表状况的改变,发现地表微波比辐射率随地表状况的变化存在敏感性,并且其变化是合理的。本中,地表肤温设定等于地表空气温度,并且仅计算了寿县的地表比辐射率,在HUBEx区域上的地表比辐射率的计算需要更多的观测资料。 相似文献
93.
Cornel E. J. de Ronde Gary J. Massoth David A. Butterfield Bruce W. Christenson Junichiro Ishibashi Robert G. Ditchburn Mark D. Hannington Robert L. Brathwaite John E. Lupton Vadim S. Kamenetsky Ian J. Graham Georg F. Zellmer Robert P. Dziak Robert W. Embley Vesselin M. Dekov Frank Munnik Janine Lahr Leigh J. Evans Ken Takai 《Mineralium Deposita》2011,46(5-6):541-584
Brothers volcano, of the Kermadec intraoceanic arc, is host to a hydrothermal system unique among seafloor hydrothermal systems known anywhere in the world. It has two distinct vent fields, known as the NW Caldera and Cone sites, whose geology, permeability, vent fluid compositions, mineralogy, and ore-forming conditions are in stark contrast to each other. The NW Caldera site strikes for ??600?m in a SW?CNE direction with chimneys occurring over a ??145-m depth interval, between ??1,690 and 1,545?m. At least 100 dead and active sulfide chimney spires occur in this field and are typically 2?C3?m in height, with some reaching 6?C7?m. Their ages (at time of sampling) fall broadly into three groups: <4, 23, and 35?years old. The chimneys typically occur near the base of individual fault-controlled benches on the caldera wall, striking in lines orthogonal to the slopes. Rarer are massive sulfide crusts 2?C3?m thick. Two main types of chimney predominate: Cu-rich (up to 28.5?wt.% Cu) and, more commonly, Zn-rich (up to 43.8?wt.% Zn). Geochemical results show that Mo, Bi, Co, Se, Sn, and Au (up to 91?ppm) are correlated with the Cu mineralization, whereas Cd, Hg, Sb, Ag, and As are associated with the dominant Zn-rich mineralization. The Cone site comprises the Upper Cone site atop the summit of the recent (main) dacite cone and the Lower Cone site that straddles the summit of an older, smaller, more degraded dacite cone on the NE flank of the main cone. Huge volumes of diffuse venting are seen at the Lower Cone site, in contrast to venting at both the Upper Cone and NW Caldera sites. Individual vents are marked by low-relief (??0.5?m) mounds comprising predominately native sulfur with bacterial mats. Vent fluids of the NW Caldera field are focused, hot (??300°C), acidic (pH????2.8), metal-rich, and gas-poor. Calculated end-member fluids from NW Caldera vents indicate that phase separation has occurred, with Cl values ranging from 93% to 137% of seawater values. By contrast, vent fluids at the Cone site are diffuse, noticeably cooler (??122°C), more acidic (pH?1.9), metal-poor, and gas-rich. Higher-than-seawater values of SO4 and Mg in the Cone vent fluids show that these ions are being added to the hydrothermal fluid and are not being depleted via normal water/rock interactions. Iron oxide crusts 3?years in age cover the main cone summit and appear to have formed from Fe-rich brines. Evidence for magmatic contributions to the hydrothermal system at Brothers includes: high concentrations of dissolved CO2 (e.g., 206?mM/kg at the Cone site); high CO2/3He; negative ??D and ??18OH2O for vent fluids; negative ??34S for sulfides (to ?4.6??), sulfur (to ?10.2??), and ??15N2 (to ?3.5??); vent fluid pH values to 1.9; and mineral assemblages common to high-sulfidation systems. Changing physicochemical conditions at the Brothers hydrothermal system, and especially the Cone site, occur over periods of months to hundreds of years, as shown by interlayered Cu?+?Au- and Zn-rich zones in chimneys, variable fluid and isotopic compositions, similar shifts in 3He/4He values for both Cone and NW Caldera sites, and overprinting of ??magmatic?? mineral assemblages by water/rock-dominated assemblages. Metals, especially Cu and possibly Au, may be entering the hydrothermal system via the dissolution of metal-rich glasses. They are then transported rapidly up into the system via magmatic volatiles utilizing vertical (??2.5?km long), narrow (??300-m diameter) ??pipes,?? consistent with evidence of vent fluids forming at relatively shallow depths. The NW Caldera and Cone sites are considered to represent stages along a continuum between water/rock- and magmatic/hydrothermal-dominated end-members. 相似文献
94.
95.
Markus Wallner Georg Houben Christoph Lohe Martin Quinger Thomas Himmelsbach 《Hydrogeology Journal》2017,25(8):2303-2321
The identification of potential recharge areas and estimation of recharge rates to the confined semi-fossil Ohangwena II Aquifer (KOH-2) is crucial for its future sustainable use. The KOH-2 is located within the endorheic transboundary Cuvelai-Etosha-Basin (CEB), shared by Angola and Namibia. The main objective was the development of a strategy to tackle the problem of data scarcity, which is a well-known problem in semi-arid regions. In a first step, conceptual geological cross sections were created to illustrate the possible geological setting of the system. Furthermore, groundwater travel times were estimated by simple hydraulic calculations. A two-dimensional numerical groundwater model was set up to analyze flow patterns and potential recharge zones. The model was optimized against local observations of hydraulic heads and groundwater age. The sensitivity of the model against different boundary conditions and internal structures was tested. Parameter uncertainty and recharge rates were estimated. Results indicate that groundwater recharge to the KOH-2 mainly occurs from the Angolan Highlands in the northeastern part of the CEB. The sensitivity of the groundwater model to different internal structures is relatively small in comparison to changing boundary conditions in the form of influent or effluent streams. Uncertainty analysis underlined previous results, indicating groundwater recharge originating from the Angolan Highlands. The estimated recharge rates are less than 1% of mean yearly precipitation, which are reasonable for semi-arid regions. 相似文献
96.
Georg Schettler 《洁净——土壤、空气、水》1992,20(3):142-149
Distribution of Selected Toxic Trace Elements in the Sediment of Lake Breitling near Brandenburg. Considerable enrichments of several heavy metals in relation to the local geological background were found in the surface sediments of Lake Breitling (Havel lake system) (Zn: 50-fold, Cd: 25-fold, Cu: 14-fold, Pb: 13-fold), whereas Be, Co and V are remarkably unchanged if the increased clay mineral content in the more recent sediments is considered. – The heavy metal distribution patterns indicate a high percentage of atmospheric input of these elements, and according to geochemical profiles heavy metal deposition has been constant on a high level for years. – Especially the most enriched Zn which was found to some extent NH4Ac-exchangeable deserves ecotoxic attention. 相似文献
97.
98.
Georg Knetsch 《International Journal of Earth Sciences》1937,28(3-4):208-223
Ohne Zusammenfassung 相似文献
99.
Georg Frebold 《International Journal of Earth Sciences》1924,14(3):261-272
Ohne Zusammenfassung 相似文献