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101.
贵州红枫湖纹理沉积物中近代气温记录   总被引:7,自引:0,他引:7  
吴丰昌  万国江 《地理科学》1996,16(4):345-350
本通过红枫湖纹理沉积物柱芯碳酸盐特征剖面与流域气温资料对比、沉积纹理年代校正以及早期成岩化学过程对碳酸盐沉积记录的改造作用等方面的研究,表明湖泊碳酸盐沉积记录基本不受早期成岩作用的影响,碳酸钙含量和CaO/MgO·Al2O3比值可作为湖泊沉物中具高分辨率、短时间尺度的气温变化的代用指标。  相似文献   
102.
建立于秦岭腹地柞水、镇安两县交界的泥盆系沉积岩相地质剖面,有陆相冲积相、过渡相河口湾相、海潮坪相、陆棚相、局限台地相、开阔台地相、台缘生物礁相、台缘斜坡相及次深海盆地浊积岩相,整体反映一微型镶边碳酸盐台地的形成与消亡,保护该地质遗迹对地质科学研究具有重要的实际意义。该剖面已被批准为陕西省第2号自然保护点,并已立碑保护。  相似文献   
103.
松辽白垩纪近海陆相盆地最大湖侵期的泉头组-嫩江组时期,可能发生了三次较大规模的海水入侵事件,时间分别为泉三、四段一青一段(阿尔布期),青二、三段顶部(土仑期)和嫩一、二段(晚桑托-早坎佩尼期)。海水注入使湖盆的水文地球化学和环境地球化学条件均发生改变,并在层序中留下沉积记录。海进期主要表现为:①重同位素组份增加,直至与同期海相层序的同位素组成相同;②介质的盐度指标(Sr/Ba)、碱度指标(Ca+Mg)/(Si+Al)、还原性指标(Zn+Ni)/Ga和硫通量指标(S归一化含量)均系统增加。相反,海退期则上述指标显著降低。根据沉积层序的同位素组成、同期海水的同位素组成和同位素分馏的质量平衡关系,可求出研究层段内同位素的海水来源与淡水来源的比例(混合度)为0-5。并由此恢复出海平面升降曲线。  相似文献   
104.
武安斌  宋春晖 《甘肃地质》1993,2(1):25-34,T003
本文根据岩石类型、沉积构造、生物组合和指相矿物将西成矿田中泥盆统碳酸盐沉积划分为两个相带,7个相和11个亚相,即碳酸盐台地相带和碳酸盐台地边缘相带;台地潮坪相、局限台地相、半开阔台地相、开阔台地相、台缘前斜坡相、生物滩层礁相和礁相。可以看出,区内铅锌矿床的形成和分布明显受着碳酸盐沉积相带的控制。  相似文献   
105.
利用长江三峡工程坝区及外围深部构造的人工地震波记录资料,进行了相对速度幅值、速度反应谱和加速度反应谱衰减特征分析,同时利用历史地震资料经转换方法给出的地震动衰减规律进行对比,反映出由人工地震记录地震动参数衰减特征与由历史资料转换确定的地震动衰减特征是有差异的,在不同地质条件的局部地区,这一差异更为明显。这些结果可为缺乏强震记录的地区的地震动估计提供参考。  相似文献   
106.
ABSTRACT

National and regional water quality monitoring networks have been operated in South Africa since the early 1970s. These originally had text-based inventories that were convenient for specialists who were familiar with the national networks and knew the locations of their sites of interest. However, within two decades the networks had expanded in geographical extent and variables monitored to such an extent that users needed spatial context in order to locate sites that fitted their information requirements. Mapping applications running on the Internet, such as Google Earth and Leaflet, form the foundation of a system for providing online inventories and summaries of the data available on the water quality database. The interfaces were constructed using available software, mainly ArcInfo and R. A recent concern is a decrease in the collection of water quality data, which is reducing the value of data summaries for water resource management.  相似文献   
107.
ABSTRACT

Large-sample hydrology (LSH) relies on data from large sets (tens to thousands) of catchments to go beyond individual case studies and derive robust conclusions on hydrological processes and models. Numerous LSH datasets have recently been released, covering a wide range of regions and relying on increasingly diverse data sources to characterize catchment behaviour. These datasets offer novel opportunities, yet they are also limited by their lack of comparability, uncertainty estimates and characterization of human impacts. This article (i) underscores the key role of LSH datasets in hydrological studies, (ii) provides a review of currently available LSH datasets, (iii) highlights current limitations of LSH datasets and (iv) proposes guidelines and coordinated actions to overcome these limitations. These guidelines and actions aim to standardize and automatize the creation of LSH datasets worldwide, and to enhance the reproducibility and comparability of hydrological studies.  相似文献   
108.
刘旭 《北京测绘》2020,(5):610-613
针对地下管网隐患数据管理的应用需求,本文基于三维平台设计实现了地下管网健康档案管理平台,在三维场景加载地上精细模型和地下管网数据,以三维可视化的手段对管网各类隐患问题进行信息管理,结合二维GIS操作,实现了净距分析、覆土分析、占压分析等管线隐患分析功能,通过本平台建立的地下管网健康档案数据库,方便用户对各类管网隐患数据进行信息管理和统计,为管道病害修复、管网改造提升提供数据支撑,保证地下管网的安全运行。  相似文献   
109.
This paper compares the palaeolimnological evidence for climate change over the last 200 years with instrumental climate data for the same period at seven European remote mountain lakes. The sites are Øvre Neådalsvatn (Norway), Saanajärvi (Finland), Gossenköllesee (Austria), Hagelseewli (Switzerland), Jezero v Ledvici (Slovenia), Estany Redó (Spain, Pyrenees), and Niné Terianske Pleso (Slovakia). We used multiple regression analysis to transfer homogenised lowland air temperature records to each of the sites, and these reconstructions were validated using data from on-site automatic weather stations. These data showed that mean annual temperature has varied over the last 200 years at each site by between 1 and 2 °C, typical of the high frequency variability found throughout the Holocene, and appropriate, therefore, to test the sensitivity of the various proxy methods used. Sediment cores from each site were radiometrically dated using 210Pb, 137Cs and 241Am and analysed for loss-on-ignition, C, N, S, pigments, diatoms, chrysophytes, Cladocera and chironomids. Comparisons between the proxy data and the instrumental data were based on linear regression analysis with the proxy data treated as response variables and the instrumental data (after smoothing using LOESS regressions) as predictor variables. The results showed few clear or consistent patterns with generally low or very low r2 values. Highest values were found when the data were compared after smoothing using a broad span, indicating that some of the proxy data were capturing climate variability but only at a relatively coarse time resolution. Probable reasons for the weak performance of the methods used include inaccurate dating, especially for earlier time periods, the influence of confounding forcing factors at some sites e.g., air pollution, earthquakes, and the insensitivity of some methods to low amplitude climate forcing. Nevertheless, there were trends in some proxy records at a number of sites that had a relatively unambiguous correspondence with the instrumental climate records. These included organic matter and associated variables (C and N) and planktonic diatom assemblages at the majority of sites and chrysophytes and chironomids at a few sites. Overall for longer term studies of the Holocene, these results indicate the need to be cautious in the interpretation of proxy records, the importance of proxy method validation, the continuing need to use reinforcing multi-proxy approaches, and the need for careful site and method selection.  相似文献   
110.
Peng X  Zhang G  Mai B  Min Y  Wang Z 《Marine pollution bulletin》2002,45(1-12):295-299
Bottom sediments and a 210Pb dated sedimentary core in Macao Estuary were quantitatively analyzed with GC-MS for coprostanol and other sterols. Higher coprostanol concentrations were detected at Port Interior and Lower Qianshan River, indicative of serious sewage pollution from densely populated Macao Island and Zhuhai City. However, very low concentrations of coprostanol were detected around Coloane Island as well as Port Exterior and Maliuzhou River except sites adjacent sewage outlets. Coprostanol pollution in Macao Estuary originates mainly from locally direct discharge of untreated wastewater. The concentrations of coprostanol in ZJ-9 were mainly in range of 150–280 ng/g with an average of 210 ng/g for more than 20 years from early 1970s to early 1990s. However, it increased obviously since 1993, and reached the highest in 1995–1996. However, a sharp decrease of coprostanol concentration from 470 to 31 ng/g after 1996 was observed corresponding to the first wastewater treatment plant in Taipa Island going into action.  相似文献   
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