Corrigendum: Pleistocene Rhine–Thames landscapes: geological background for hominin occupation of the southern North Sea region     

Marc P. Hijma  Kim M. Cohen  Wil Roebroeks  Wim E. Westerhoff  Freek S. Busschers 《第四纪科学杂志》2012,27(3):336-336

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Optimization of As(V) adsorption on Fe-RH-MCM-41-immobilized GAC using Box–Behnken Design: Effects of pH,loadings, and initial concentrations     

Kitirote Wantala  Eakkachai Khongkasem  Nuthakarn Khlongkarnpanich  Suthipong Sthiannopkao  Kyoung-Woong Kim 《Applied Geochemistry》2012

This work focused on the removal from water of arsenate in the 100 to 500 μg/L range using Fe-RH-MCM-41 immobilized on GAC by a colloidal impregnation method. A Response Surface Method (RSM) based on the Box–Behnken Design (BBD) was used to evaluate the effects of pH, adsorbent loading, and initial arsenate concentrations. The thermal stability of Fe-RH-MCM-41/GAC was greater than 460 °C because Fe-RH-MCM-41 and epoxy resin covered the GAC, preventing GAC weight loss. The rate and capacity for arsenate adsorption on Fe-RH-MCM-41/GAC were higher than for GAC. The effects of pH, adsorbent loading, and initial arsenate concentration showed significant effects on efficiency, in terms of percent arsenate removal. Significant interaction occurred as positive effects between arsenate and arsenate concentrations, and pH and arsenate concentrations, and as negative effects between pH and pH, adsorbent loading and adsorbent loading, and adsorbent loading and arsenate concentrations.  相似文献   

Influence of trace element fluxes from submarine groundwater discharge (SGD) on their inventories in coastal waters off volcanic island,Jeju, Korea     

Jiwon Jeong  Guebuem Kim  Seunghee Han 《Applied Geochemistry》2012

The concentrations of trace elements in groundwater and seawater were measured in a coastal embayment (Bangdu Bay) of a volcanic island (Jeju) off the southernmost coast of Korea in August and December of 2009. The concentrations of trace elements (Al, Mn, Fe, Co, Ni, and Cu) in the groundwater in summer were approximately 20-fold higher than those in winter, with good correlation to each other. Overall, the concentrations of most of the trace elements in the groundwater were 3- to 70-fold higher than those in the seawater of this Bay. Simple budget calculations showed that large fluxes of submarine groundwater discharge (SGD)-driven trace elements were responsible for the unusually enhanced concentrations of trace elements (particularly for Al, Fe and Co) in the summer seawater. The results imply that the temporal changes in SGD-driven trace element fluxes are large and may contribute considerably to the budget of trace elements in the coastal ocean, particularly off a highly permeable volcanic island.  相似文献   

Flood risk assessment using regional regression analysis   总被引：2，自引：0，他引：2  

Young-Oh Kim  Seung Beom Seo  Ock-Jae Jang 《Natural Hazards》2012,63(2):1203-1217

This study aimed to create a flood risk map for ungauged regions, which have limited flood damage data and other relevant data. The fact that there is a shortage of data that are critical for the establishment of a flood assessment and mitigation plan is not surprising even in developed countries like South Korea. To address this problem, the regional regression concept in statistical hydrology was introduced to the flood risk assessment field in this study, and it was framed with a series of two regression functions: flood damage and regional coefficients. As the second regression function utilizes the local socioeconomic variables, the resulting flood risk map can reflect the spatial characteristics well. The proposed methodology was applied to create flood risk maps for the three metropolitan areas in South Korea. The comparison of the proposed methodology with the existing methods revealed that only the proposed methodology can produce a statistically meaningful flood risk map based on a recent major flood in 2001.  相似文献   

Mortality and Physiological Responses with Regard to the Surf Clam,Mactra quadrangularis,Exposed to Chlorine     

Lee  Seon-Sik  Ahn  Hyung-Jin  Hwang  In-Uk  Kim  Eun  Han  Kyung-Nam 《Ocean Science Journal》2021,56(4):406-412

Ocean Science Journal - Carcinogenic disinfection by-products (DBPs) are formed as the result of the chlorination of power plant water cooling systems for biofouling purposes. Effects of cooling...  相似文献   

Influence of Total Water-Temperature Value on the Size and Weight Characteristics of Pacific Oyster Crassostrea gigas (Thunberg, 1793) in the Aniva Bay (Sakhalin Island) According to Satellite Data     

Kim  A. Ch.  Lozhkin  D. M. 《Izvestiya Atmospheric and Oceanic Physics》2021,57(12):1712-1719

Izvestiya, Atmospheric and Oceanic Physics - Long-term average values and anomalies of the duration of the period of positive temperatures and the total water-temperature value have been calculated...  相似文献   

Synmetamorphic granitoids (~ 490 Ma) as accretion indicators in the evolution of the Ol’khon terrane (western Cisbaikalia)     

T.V. Donskaya  D.P. Gladkochub  V.S. Fedorovsky  A.M. Mazukabzov  M. Cho  W. Cheong  J. Kim 《Russian Geology and Geophysics》2013,54(10):1205-1218

We present geological, structural, and geochemical data on synmetamorphic granitoids from the Tutai and South Ol’khon plutons of the Ol’khon terrane (Central Asian Fold Belt) with an estimation of the U–Pb zircon age of the Tutai granites. The structural and petrological data suggest the synfolding and synmetamorphic origin of the granitoids. The U–Pb zircon age of the Tutai granites (488.6 ± 8.0 Ma) almost coincides with the previously estimated age of quartz syenites from the South Ol’khon pluton (495 ± 6 Ma). The plutons occupy the same position in the regional structure. The granitoids underwent final deformations and metamorphism at 464 ± 11 Ma. The Tutai pluton consists of moderately potassic granites, whereas the South Ol’khon pluton is made up of quartz syenites and granites. The geochemical characteristics of the granites from both plutons (low Y and Yb contents, fractionated REE patterns) indicate their formation under conditions of garnet crystallization in deep crustal restite. The higher Y and Yb contents of the South Ol’khon quartz syenites as compared with those of the granites suggest the lack of equilibrium between the quartz syenite magmas and garnet parageneses during their formation or evolution. The Tutai and South Ol’khon granites were derived from quartz-feldspar crustal rocks, whereas the South Ol’khon quartz syenites might have originated from a mixed (crust-mantle) source. It is presumed that the granitoids formed within accretion-thickened crust. Early accretion, which has been first identified in the region, affected not only the Pribrezhnaya zone (the zone of the Tutai and South Ol’khon plutons) but also the entire Anga–Satyurty megazone of the Ol’khon terrane. The accretion ended with the convergence and oblique collision of the Ol’khon terrane and Siberian continent, when strike-slip tectonics became ubiquitous.  相似文献   

Historical-geological modeling of hydrocarbon generation in the Mesozoic–Cenozoic sedimentary basin of the Kara Sea (basin modeling)     

A.E. Kontorovich  L.M. Burshtein  N.A. Malyshev  P.I. Safronov  S.A. Gus’kov  S.V. Ershov  V.A. Kazanenkov  N.S. Kim  V.A. Kontorovich  E.A. Kostyreva  V.N. Melenevskiy  V.R. Livshits  A.A. Polyakov  M.B. Skvortsov 《Russian Geology and Geophysics》2013,54(8):917-957

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Jurassic paleogeography of the West Siberian sedimentary basin     

A.E. Kontorovich  V.A. Kontorovich  S.V. Ryzhkova  B.N. Shurygin  L.G. Vakulenko  E.A. Gaideburova  V.P. Danilova  V.A. Kazanenkov  N.S. Kim  E.A. Kostyreva  V.I. Moskvin  P.A. Yan 《Russian Geology and Geophysics》2013,54(8):747-779

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Multi-Region Boundary Element Analysis for Coupled Thermal-Fracturing Processes in Geomaterials     

Baotang Shen  Hyung-Mok Kim  Eui-Seob Park  Taek-Kon Kim  Manfred W. Wuttke  Mikael Rinne  Tobias Backers  Ove Stephansson 《Rock Mechanics and Rock Engineering》2013,46(1):135-151

This paper describes a boundary element code development on coupled thermal–mechanical processes of rock fracture propagation. The code development was based on the fracture mechanics code FRACOD that has previously been developed by Shen and Stephansson (Int J Eng Fracture Mech 47:177–189, 1993) and FRACOM (A fracture propagation code—FRACOD, User’s manual. FRACOM Ltd. 2002) and simulates complex fracture propagation in rocks governed by both tensile and shear mechanisms. For the coupled thermal-fracturing analysis, an indirect boundary element method, namely the fictitious heat source method, was implemented in FRACOD to simulate the temperature change and thermal stresses in rocks. This indirect method is particularly suitable for the thermal-fracturing coupling in FRACOD where the displacement discontinuity method is used for mechanical simulation. The coupled code was also extended to simulate multiple region problems in which rock mass, concrete linings and insulation layers with different thermal and mechanical properties were present. Both verification and application cases were presented where a point heat source in a 2D infinite medium and a pilot LNG underground cavern were solved and studied using the coupled code. Good agreement was observed between the simulation results, analytical solutions and in situ measurements which validates an applicability of the developed coupled code.  相似文献