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51.
Alpine shrub Quercus aquifolioides was selected to study the effects of shrub canopy on throughfall and phreatic water by analyzing the isotopic time series of precipitation, canopy throughfall and phreatic water and examining correlations among these series in Wolong Nature Reserve, Western China. Based on analysis of precipitation data in 2003, the local meteoric water line during the rainy season was δD = 8.28 × δ18O + 8.93, and the primary precipitation moisture in this region originated from the Pacific Ocean in the summer. Stable isotope analysis showed that the main supply of throughfall and phreatic water was from precipitation, and the shrub canopy has an important effect on the processes of rainwater transmuted into throughfall and phreatic water. Moreover, the differences of δD and δ18O values between rainwater and throughfall were relevant to rainfall. Due to interception of the shrub canopy, there had a response hysteresis of phreatic water to the various rainfall events, which was mostly 2 days, except that this hysteresis was ≤1 day when rainfall was >15 mm/day.  相似文献   
52.
塔里木盆地迪那2大型凝析气田的地质特征及其成藏机制   总被引:4,自引:2,他引:2  
塔里木盆地库车坳陷迪那2凝析气田是中国目前发现的储量规模最大的凝析气田,含气层位为古近系苏维依组与库姆格列木群;储集岩以粉砂岩、细砂岩为主,属于低孔低渗储层,近似于致密砂岩气.气藏储量丰度大于15亿方/km2,气油比为8100~12948m3/m3,凝析油含量60~80g/m3;储层温度129 ~ 138℃,地温梯度为2.224℃/1OOm;地层压力为105 ~106MPa,压力梯度为0.39MPa/1OOm,压力系数为2.06~2.29,属于常温超高压凝析气藏.天然气以湿气为主,碳同位素较重,属于典型的煤成气;原油碳同位素较重,生物标志化合物体显出陆相油特征.研究认为,油气主要来自阳霞凹陷侏罗系煤系烃源岩;圈闭形成时间较晚,根据热史、埋藏史、烃源岩热演化史、流体包裹体等资料以及天然气碳同位素动力学拟合的油气充注成藏时间都表明,迪那2凝析气田的成藏时间是在2.5Ma以来,是一个典型的晚期快速充注成藏的大型凝析气田.晚期前陆逆冲挤压作用在形成超压的同时,发生了储层的致密化和烃类的充注,储层致密化过程与烃类充注同步.  相似文献   
53.
以国产高分辨率卫星影像数据为主要信息源,通过对影像进行数据处理,根据影像特征建立了矿山环境遥感解译标志,并对标志图斑进行了野外验证,结合多时相影像的对比,查明矿山基建、开采过程中造成的地貌景观破坏、土地压占、矿产资源开采情况等,分析矿山开发利用状态和地质环境问题。以遥感技术为基础,并利用GIS平台,结合土地利用现状、土地权证、矿山权证等资料,形成矿山环境监测系统,反映矿山环境的变化趋势和规律,为区域地质环境保护、矿山地质环境治理及矿产资源的管理提供决策依据。  相似文献   
54.
对一幢具有转换层的复杂退台式框架剪力墙高层建筑的1/35缩尺模型进行了模拟地震振动台试验,深入研究该结构的动力特性和地震反应特征.试验及理论分析表明:该结构的抗震性能基本满足现行规范要求;由于结构上部逐渐退台,因而结构顶部有较明显的鞭端效应;结构首层和结构转换层及其相邻层的剪力墙、转换层上下层柱是受力较大的区域,应当局...  相似文献   
55.
广州天誉大厦采用型钢混凝土框架一钢筋混凝土筒体的混合结构体系,地面以上结构采用抗震缝兼伸缩缝分隔为南、北塔两个独立结构体系,南塔高186.5 m,北塔高159.5 m.两塔的核心筒总宽度与核心筒总高的比值均超出了规范限值.为研究这种超限高层混合结构的抗震性能,对其进行了缩尺(1/30)模型的振动台试验,并建立了有限元计...  相似文献   
56.
为了做好自动气象站A文件的审核工作,确保气象记录报表的正确,结合自动气象站A文件预审中的主要问题,谈了会审工作中的几点体会。  相似文献   
57.
In this study, a risk-based management model is developed and applied to an industrial zone. The models proposed by the United States Environmental Protection Agency and Han Bing have been improved by adding a residual ratio of volatile organic compounds (VOC) after boiling and deleting the related parameters in half-life. Using this improved model, an integrated process was used to assess human health risk level in the study area. Compared with water quality analysis, the results highlight the importance of applying an integrated approach for decision making on risk levels and water protection. The results of this study demonstrated that: (1) Compared with these permissible level standards in China (GB 3838-2002) and National Primary Drinking Water Regulations of the United States, the residents’ daily life had not been affected by the groundwater in this area (except for relative bad water quality of HB3-4 and HB3-6); (2) The typical detected organic contaminants of all groundwater samples were chloroform, carbon tetrachloride, trichloroethylene and tetrachloroethene, and the pollution sources were mainly industrial sources by preliminary investigations; (3) As for groundwater, the non-carcinogenic risk values of all samples do not exceed the permissible level of 1.0 and the carcinogenic risk values are relatively lower than the permissible level of 1.00E-06 to 1.00E-04; (4) Drinking water pathway of trichloroethylene and tetrachloroethylene mainly contribute to increasing the health risk of residents’ in study areas; (5) In terms of non-carcinogenic risk and carcinogenic risk, the health risk order for drinking water pathway and dermal contact pathway was: drinking water pathway > dermal contact pathway.  相似文献   
58.
http://www.sciencedirect.com/science/article/pii/S1674987111000752   总被引:2,自引:0,他引:2  
A series of environmentalegeological problems have been caused by over-exploitation of deep groundwater (i.e., confined aquifer water) in the North China Plain. In order to better understand the status of deep groundwater over-exploitation and the resultant environmentalegeological problems on a regional scale, the over-exploitation of groundwater has been assessed by way of the groundwater exploitation potential coefficient (i.e., the ratio of exploitable amount of deep groundwater to current exploitation), cumulative land subsidence, and long-term average lowering rate of the groundwater table. There is a good correlation among the results calculated by the different methods. On a regional scale, deep groundwater has been over-exploited and there is no further exploitation potential under the current conditions. The groundwater exploitation degree index takes the exploitation in 2003 as the reference for the calculations, so the results mainly reflect the degree of current groundwater exploitation. The results of over-exploitation of deep groundwater obtained by land subsidence data and long-term average rate of depression of the water table mainly reflect environmentalegeological problems caused by exploitation of deep groundwater.  相似文献   
59.
We inferred late Holocene Adélie penguin occupation history and population dynamics on Zolotov Island, Vestfold Hills, Antarctica, using geochemical data from a dated ornithogenic sediment core (ZOL4). Radiocarbon dates on fossil penguin bones in the core indicate that Adélie penguins occupied the island as early as 1,800 years before present (yr BP), following the retreat of the Sørsdal glacier. This occupation began ~1,200 years later than that observed at Ardley Island and King George Island, in the South Shetland Islands. Phosphorus was identified as the most indicative bio-element for penguin guano in core ZOL4, and was used to infer past penguin population dynamics. Around 1,800 years ago, the Adélie penguin populations at both Zolotov Island and Ardley Island increased rapidly and reached their highest levels ~1,000 yr BP. For the past ~900 years, the penguin populations at Zolotov Island have shown a general rising trend, with fluctuations, while those at Ardley Island have shown a moderate decreasing trend. The Adélie penguin populations at both Ardley Island and Zolotov Island showed a clear decline ~300 years ago, which we interpret as a response to the Little Ice Age, or a neoglacial cooling event.  相似文献   
60.
利用内蒙古东南部通辽、赤峰两站1992—2012年的地面和探空数据,针对两地雨、雨夹雪和雪等不同的降水相态进行对比分析,结果表明:通辽站降雨或雨夹雪时850hPa气温特征较为接近,赤峰站降雨夹雪或雪时850hPa气温特征较为接近;通辽站850~700hPa两层之间的厚度降雨夹雪或雪时特征相近,赤峰站降雨或雨夹雪时特征相近,在箱线图中两层之间的厚度与850hPa温度分别对3种相态出现完全相反的叠加。在850、925hPa气温的判别指标中,赤峰较通辽站:降雨时分别高1.5℃和1.7℃、降雪时分别高2.4℃和3.8℃。气温(T)统计表明:降雨时通辽站气温在4.0℃以上、赤峰站气温在6.0℃以上,降雪时两站均T≤0.0℃,两站气温在0.0℃T≤4.0℃(通辽站,赤峰站为6.0℃)为雨、雨夹雪和雪共同出现的温度区间。虽然两站阈值大小有较大差异,但3种降水相态的出现均与中、低层厚度和低层气温密切相关,与中层的气温关系甚小,说明该地区中、低层厚度和低层气温高低决定地面降水相态。  相似文献   
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