Protection of neighbour buildings due to construction of shield tunnel in mixed ground with sand over weathered granite     

Qing-Long Cui  Huai-Na Wu  Shui-Long Shen  Zhen-Yu Yin  Suksun Horpibulsuk 《Environmental Earth Sciences》2016,75(6):458

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Regulation of secondary soil salinization in semi-arid regions: a simulation research in the Nanshantaizi area along the Silk Road,northwest China   总被引：2，自引：0，他引：2  

Peiyue Li  Jianhua Wu  Hui Qian 《Environmental Earth Sciences》2016,75(8):698

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Numerical simulation of the flow velocity and temperature of the Dongkemadi Glacier     

Wu Zhen  Liu Shiyin  He Xiaobo 《Environmental Earth Sciences》2016,75(5):394

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Coal-measure source rock characteristics and burial evolution history in the Shisanjianfang Area,Tuha Basin     

Zhiyuan Wu  Suping Peng  Wenfeng Du 《Arabian Journal of Geosciences》2016,9(5):417

Shisanjianfang Area in the eastern margin of Taibei Sag, Tuha Basin, is an important region for oil and gas exploration. In this study, a large number of source rock geochemical data were used to analyze the geochemical characteristics of coal-measure source rocks in the Shisanjianfang Area, Tuha Basin, from three aspects, i.e., organic matter abundance, organic matter type, and organic maturity. The results show that the Jurassic Xishanyao Formation (J₂x) in the study area has great thickness, continuous distribution, and high source rock maturity, and is the major source rock horizon in the study area. The seismic data are used in combination with 1D and 2D basin simulation technology to study the distribution characteristics of the source rocks in Shisanjianfang Area. The results of the simulation research on the source rock maturity history in the study area indicate the following: (1) The source rocks in the Xishanyao Formation (J₂x) have a hydrocarbon generation threshold depth of 1800 m, threshold temperature of 95 °C, and hydrocarbon generation threshold time of about 162 Ma. (2) The Xishanyao Formation (J₂x) has a current formation temperature of 50~110 °C and Ro of 0.6~1.1 % in the peak oil generation stage. (3) The source rock maturity in the study area is shown as being higher in the west while lower in the east, and higher in the north while lower in the south, and the favorable exploration area mainly lies in the northwest of the study area. The results of this study could have important implications for the oil and gas exploration in the margins of Xiaocaohu Sag, Tuha Basin.  相似文献   

Areal subsidence under pumping well–curtain interaction in subway foundation pit dewatering: conceptual model and numerical simulations     

Jianxiu Wang  Yuanbin Wu  Xiaotian Liu  Tianliang Yang  Hanmei Wang  Yanfei Zhu 《Environmental Earth Sciences》2016,75(3):198

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Landslide susceptibility zonation using GIS and evidential belief function model     

Yanli Wu  Yutian Ke 《Arabian Journal of Geosciences》2016,9(17):697

The main goal of this paper is to generate a landslide susceptibility map through evidential belief function (EBF) model by using Geographic Information System (GIS) for Qianyang County, Shaanxi Province, China. At first, a detailed landslide inventory map was prepared, and the following ten landslide-conditioning factors were collected: slope angle, slope aspect, curvature, plan curvature, profile curvature, altitude, distance to rivers, geomorphology, lithology, and rainfall. The landslides were detected from the interpretation of aerial photographs and supported by field surveys. A total of 81 landslides were randomly split into the following two parts: the training dataset 70 % (56 landslides) were used for establishing the model and the remaining 30 % (25 landslides) were used for the model validation. The ArcGIS was used to analyze landslide-conditioning factors and evaluate landslide susceptibility; as a result, a landslide susceptibility map was generated by using EBF and ArcGIS 10.0, thus divided into the following five susceptibility classes: very low, low, moderate, high, and very high. Finally, when we validated the accuracy of the landslide susceptibility map, both the success-rate and prediction-rate curve methods were applied. The results reveal that a final susceptibility map has the success rate of 83.31 % and the prediction rate of 79.41 %.  相似文献   

Numerical analysis of 1D coupled infiltration and deformation in layered unsaturated porous medium     

L. Z. Wu  G. G. Liu  L. C. Wang  L. M. Zhang  B. E. Li  B. Li 《Environmental Earth Sciences》2016,75(9):761

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Gas shale hydraulic fracturing: a numerical investigation of the fracturing network evolution in the Silurian Longmaxi formation in the southeast of Sichuan Basin,China, using a coupled FSD approach     

Y. Wang  X. Li  Y. X. Zhang  Y. S. Wu  B. Zheng 《Environmental Earth Sciences》2016,75(14):1093

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A study on the brittleness and progressive failure process of anisotropic shale     

Miaomiao Wang  Pei Li  Xiaowa Wu  Hongran Chen 《Environmental Earth Sciences》2016,75(10):886

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闽西北5月雨量特多年份环流特征及其成因分析     

章达华  张家斌  邝美清  沈永生  卜银军  吴姗 《气象科技》2016,44(1):61-66

利用闽西北三明市的11个县、市1961—2014年5月降雨量资料、常规气象观测资料和NCEP 2.5×2.5°再分析资料等对闽西北历史上5月雨量特多年的降雨量时空分布特征和大气环流特征及其成因进行了分析,结果表明:5月区域性、全区性雨量特多年的环流异常特征是500hPa欧亚中高纬度自西向东环流呈"+-+"的波列分布,鄂霍次克海北侧高度正距平区的稳定少动,起到阻挡冷空气东移的作用,冷空气沿乌拉尔山西侧高度正距平中心前的偏北气流不断南下,使萨彦岭一带高度负距平中心加强,其底部不断分裂小槽东移影响闽西北。925hPa华南北部维持一条稳定切变线;对于2014年5月特例的环流形势分析结果可知,500hPa东亚大槽明显偏东,引导冷空气南下与强大副高西北侧西南暖湿气流交绥在闽西北上空。925hPa闽西北处于气旋式辐合区内。北支槽、南支槽均非常活跃,东移影响闽西北,是导致该地5月区域性降雨量特多的主要原因。  相似文献