水文记录仪器中的数据存储格式

介绍了固态存储式水文数据记录仪器中数据存储的总体安排、水位和雨量数据的存储格式。     

国家防汛指挥系统工程景德镇水情分中心建设

景德镇水情分中心是国家防汛指挥系统工程示范区之一，在全国20个示范区工程建．设中首先通过验收，示范区的建设大大地改善了该地区的水文信息采集手段，实现了水位雨量观测长期自记、固态存储、自动传输，同时实现了水文数据远程下载以及水文资料整编、水情预报自动化。     

JDZ-1型固态存储雨量器观测数据分析

对JDZ-1型固态存储雨量器与虹吸自记雨量计平行观测资料进行了系统分析，分析了两者数据存在误差的影响因素。针对固态存储雨量器使用过程中存在的问题，提出了改进方法，以保证和提高资料质量。     

固态存储数据格式转换和整编应用软件的研制

固态存储数据格式转换和整编应用软件系统主要用于将固态存储器中取出的水文数据转换成整编程序要求的格式,并按整编规范进行整编,实现了水文数据从采集、转换到整编的全部自动化。     

折线逼近法在水文遥测数据处理中的应用

水文资料整编是形成水文监测成果的重要环节,随着水文监测的自动化程度越来越高,数据采集量大幅度增长,大量的数据处理成为水文资料整编的一大难题.本文尝试采用"折线逼近法",对水文遥测数据进行精简处理,尽可能地减少摘录数据量,用最少的摘录数据构成的折线来模拟实际水文要素的变化过程,并使其过程不失真,满足规范要求,便于水文年鉴刊印.该方法在江苏省水文遥测数据直接整编程序软件编制过程中得到应用,获得了较好的效果.     

关于HCJ_1型自记水位计的一点改进

目前,许多水文测站在使用上海气象仪器厂生产的HCJ_1型自记水位计时,都是将记录纸倒装在转筒上,记录笔尖从右向左运行,所绘的水位过程线是反向的。这样,为摘录与整编水位资料带来很大不便,并因此水位数据容易发生错误。为了克服上述缺点,我们作了一点改进。即将原仪器的钢丝轮重新钻孔(如图)。原钢丝轮上的穿孔在b、c位置,现在a、d位置重新钻两个小孔,这     

固态存储雨量器观测资料的误差分析

通过对JDZ－1型固态存储雨量器与虹吸式自记雨量计对比观测资料的计算与分析，找出了产生误差的原因，提出了对JDZ－1型固态存储雨量器进行调试的方法，供使用该仪器的同行参考。     

喀什地区水文测站流量测验垂线精简分析研究

流量测验一般分为常规测验和精简测验方法,而垂线精简方案是降低水文测站人员工作强度,缩短测流时间的有效方式。以新疆喀什地区某水文测站为研究对象,对流量测验垂线进行精简分析,在满足测验精度要求的前提下,对精简后的流量测定精度进行评定,分析精简方案的可行性。结果可知:垂线精简下的水位～流量关系检验的系统误差、标准差以及随机不确定度也均可满足《河流流量测验规范》GB50179-2015的允许误差要求,精简方案切实可行。     

大沽河地下水源地信息管理系统的构建和应用

在大沽河地下水源地自然地理、地质和水文地质条件调查的基础上,系统地收集和整理了钻孔属性信息、地下水水位和水质监测数据,构建了基于Microsoft SQL Server基础数据库和Hydro Geo Analyst信息管理平台的大沽河地下水源地信息管理系统。该系统解决了数据存储不规范、查询提取困难、缺乏系统管理和利用效率低等问题,实现了数据资料的存储、查询和可视化展示,帮助管理者快速、准确、全面地掌握大沽河地下水源地地层和岩性分布、地下水水位和水质的动态变化趋势与空间分布特征。本系统为大沽河地下水源地的合理开发、管理和污染治理提供了数据和技术支持,具有重要的理论意义和实际应用价值。     

固态存储雨量器与自记雨量计对比观测资料回归分析

对DJZ05-1型固态存储雨量器与20cm口径自记雨量计对比观测的资料进行了回归分析，旨在指出各雨量站不同仪器资料比测之间的相关性，从而揭示固态存储雨量器与20cm口径自记雨量计资料两者之间相关性的换算变化规律。     

The terrestrial fauna of the Late Triassic Pant-y-ffynnon Quarry fissures,South Wales,UK and a new species of Clevosaurus (Lepidosauria: Rhynchocephalia)

Pant-y-ffynnon Quarry in South Wales yielded a rich cache of fossils in the early 1950s, including articulated specimens of new species (the small sauropodomorph dinosaur Pantydraco caducus and the crocodylomorph Terrestrisuchus gracilis), but no substantial study of the wider fauna of the Pant-y-ffynnon fissure systems has been published. Here, our overview of existing specimens, a few described but mostly undescribed, as well as freshly processed material, provides a comprehensive picture of the Pant-y-ffynnon palaeo-island of the Late Triassic. This was an island with a relatively impoverished fauna dominated by small clevosaurs (rhynchocephalians), including a new species, Clevosaurus cambrica, described here from a partially articulated specimen and isolated bones. The new species has a dental morphology that is intermediate between the Late Triassic Clevosaurus hudsoni, from Cromhall Quarry to the east, and the younger C. convallis from Pant Quarry to the west, suggesting adaptive radiation of clevosaurs in the palaeo-archipelago. The larger reptiles on the palaeo-island do not exceed 1.5?m in length, including a small carnivorous crocodylomorph, Terrestrisuchus, and a possible example of insular dwarfism in the basal dinosaur Pantydraco.     

The effect of water on accessory phase solubility in subaluminous and peralkaline granitic melts

The solubilities of columbite, tantalite, wolframite, rutile, zircon and hafnon were determined as a function of the water contents in peralkaline and subaluminous granite melts. All experiments were conducted at 1035 °C and 2 kbar and the water contents of the melts ranged from nominally dry to approximately 6 wt.% H₂O. Accessory phase solubilities are not affected by the water content of the peralkaline melt. By contrast, solubilities are affected by the water content of the subaluminous melt, where the solubilities of all the accessory phases examined increase with the water content of the melt, up to 2 wt.% H₂O. At higher water contents, solubilities are nearly constant. It can be concluded that water is not an important control of accessory phase solubility, although the water content will affect diffusivities of components in the melt, thus whether or not accessory phases will be present as restite material. The solubility behaviour in the subaluminous and peralkaline melts supports previous spectroscopic studies, which have observed differences in the coordination of high field strength elements in dry vs. wet subaluminous granitic glasses, but not for peralkaline granitic glasses. Lastly, the fact that wolframite solubility increases with increasing water content in the subaluminous melt suggests that tungsten dissolved as a hexavalent species.     

Quaternary stresses revealed by calcite twinning inversion: insights from observations in the Savonnières underground quarry (eastern France)

Calcite samples were extracted both from the rock matrix and the superficial coating of a karstified fault plane of an underground quarry, located in the eastern border of the Paris basin. The karstification is dated as Quaternary. Analysis of mechanical calcite twinning reveals that only the calcite matrix has also undergone a compression trending WNW that can be attributed to the Mio-Pliocene alpine collision. Both coating and matrix have undergone a strike-slip regime with σ₁ roughly trending north–south, that could correspond to the regional present-day state of stress, a strike-slip compression rather trending NNW, modified by local phenomena. To cite this article: M. Rocher et al., C. R. Geoscience 335 (2003).     

HYDROGEOLOGY

正20141756 Chen Ruige(Mathematical College,China University of Geosciences,Beijing100083,China);Zhou Xun Numerical Simulation of Groundwater Level Fluctuation in a Coastal Confined Aquifer with Sloping Initial Groundwater Level Induced by the Tide(Geological Bulletin of China,ISSN1671-2552,CN11-4648/P,32(7),2013,p.1099-1104,6 illus.,16 refs.) Key words:confined water,groundwater level     

METAMORPHIC PETROLOGY

正20141408 Cai Jia(Institute of Geology,Chinese Academy of Geological Sciences,Beijing100037,China);Liu Fulai Petrogenesis and Metamorphic P-T Conditions of Garnet-Spinel-Biotitebearing Paragneiss in Danangou Area,Daqingshan-Wulashan Metamorphic Complex Belt(Acta Petrologica Sinica,ISSN1000-0569,CN11-1922/P,29(7),     

SERIALS

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GEOPHYSICAL EXPLORATION

正20142386An Guoying(China Aero Geophysical Survey and Remote Sensing Center for Land and Resources,Beijing 100083,China)Application of Satellite Remote Sensing in Regional Hydrogeological Investigation:Taking Cenozoic Strata in Wenquan Sheet(1∶250 000)of Karakoram Range as an Example(Geosci-     

QUATERNARY GEOLOGY & GEOMORPHOLOGY

正20141016An Chengbang(Key Laboratory of Western China’s Environmental Systems,Ministry of Education,Lanzhou University,Lanzhou 730000,China);Zhao Yongtao Lake Records during the Last Glacial Maximum from Xinjiang,NW China and Their Climatic Impli-     

PETROLEUM GEOLOGY

正20141538 Cao Qing(School of Earth Sciences and Engineering,Xi’an Petroleum University,Xi’an 710065,China);Zhao Jingzhou Characteristics and Significance of Fluid Inclusions from Majiagou Formation,Yichuan Huangling Area,Ordos Basin(Advances in Earth Science,ISSN1001-8166,CN62-1091/P,28(7),2013,p.819-828,7 illus.,3 tables,43 refs.)     

GEOCHEMISTRY

正20142002 Wei Hualing(Institute of Geophysical and Geochemical Exploration,Chinese Academy of Geological Sciences,Langfang065000,China);Zhou Guohua Element Content and Mineral Compositions in Different Sizes of Soil in Tongling Area,Anhui Province(Geological Bulletin of China,ISSN1671-2552,CN11-4648/P,32(11),2013,p.1861