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991.
992.
通过对华东地区21 个铀矿区内居民居住环境大气中氡及其子体α潜能浓度的调查,结果表明:居民居室外氡浓度均值范围为6.73—132.9 Bq/m 3,氡子体α潜能浓度均值范围为11.0—78.8nJ/m 3。居室内的平均氡浓度均值范围为14.5—185.8 Bq/m 3,氡子体α潜能浓度均值范围为13.8—104.2 nJ/m 3;对居民饮用水源的取样分析表明,铀浓度均值范围为0.12—1.68 μg/L,钍浓度均值范围为0.02—0.42 μg/L,镭-226 浓度均值范围为0.90—12.1 m Bq/L,与全国和当地的放射性天然本底水平比较接近,均属正常本底水平。 相似文献
993.
全国水文站网管理信息系统研究 总被引:2,自引:0,他引:2
全国水文站网管理信息系统是应用GIS技术开发的信息管理系统,它为优化水文站网,提高站网管理水平,提供了迅速、全面的信息支持系统建成后,可实现水上网图、文、声、像信息的查询、漫游和图形报表的输出。介绍了系统的设计与研究成果。 相似文献
994.
Organic carbon isotopes of the Sinian and Early Cambrian black shales on Yangtze Platform, China 总被引:5,自引:0,他引:5
Organic matter of the Sinian and early Cambrian black shales on the Yangtze Platform belongs to the light carhon group of
isotopes with the δ13C values from - 27% to - 35 %, which are lower than those of the contempomneously deposited carbonates and phosphorites. A carbon isotope-stratified
paleooceanographic model caused by upwelling is proposed, which can be used not only to interpret the characteristies of organic
carbon isotopic compositions of the black shales, but also to interpret the paleogeographic difference in the organic carbon
isotope compositions of various types of sedimentary rocks.
Project supported by the National Natural Science Foundation of China (Grant No. 49472114) and the Open Laboratory of Organic
Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences. 相似文献
995.
Analysis of reservoir water quality using fuzzy synthetic evaluation 总被引:12,自引:0,他引:12
R.-S. Lu S.-L. Lo J.-Y. Hu 《Stochastic Environmental Research and Risk Assessment (SERRA)》1999,13(5):327-336
A general methodology for fuzzy synthetic evaluation is developed and illustrated with a case study of trophic status assessment
for Fei-Tsui Reservoir in Taiwan. The historical data base was collected from the management agency of Fei-Tsui Reservoir
from 1987 to 1996. In fuzzy synthetic evaluation, the classification is determined by a matrix operation of the weighted vector
with the fuzzy evaluation matrix. After all individual membership functions of evaluated factors have been determined, the
fuzzy evaluation matrix can be established. The weighted vector is determined by the analytic hierarchy process method (AHP).
The results of this investigation show that the long-term change of water quality and the overturn phenomena cannot be observed
with the Carlson index from 1987 to 1992 but is expressed by fuzzy synthetic evaluation. Fuzzy synthetic evaluation is better
suited than the Carlson index to rating the trophic status of self-sustaining lakes. Interpretation of the results can provide
valuable information to decision makers and aid reservoir management. 相似文献
996.
1768记录器走纸电机驱动电路的过去和现状768记录器以其先进的技术性能和使用功能,已成为国内几乎所有模拟遥测地震台网一致选用的记录设备。但由于它诞生于70年代,以今天的水准来看,它所采用的一些电路技术已显得陈旧落后,走纸电机驱动电路就是其中之一。7... 相似文献
997.
螺旋CT原理,扫描参数和图像重建 总被引:6,自引:0,他引:6
螺旋CT最显著的特征是X线球管围绕病人旋转时,扫描床上病人连续通过机架,由于滑环技术的发明螺旋CT于1989年投入临床应用,它被广泛接受并成功地应用于人体各个部位的检查。由于产生容积数据,螺旋CT产生较少的呼吸遣漏扫描且可行允许重建,提高了Z轴的分辨率。 相似文献
998.
Tectonothermal history of the basement rocks in the western zone of the North China Craton and its tectonic implications 总被引:47,自引:0,他引:47
The basement of the North China Craton can be divided into the eastern, central and western zones, based on lithological, structural, metamorphic and geochronological data. The western zone comprises two different petrotectonic units: Archaean tonalitic–trondhjemitic–granodioritic (TTG) grey gneisses and metamorphic mafic rocks, and Palaeoproterozoic khondalite series. The former is characterized by isobaric cooling (IBC)-type anticlockwise P–T paths in the north-northwestern part of the zone and near-isothermal decompression (ITD)-type clockwise P–T paths in the eastern part, adjacent to the central zone. On the other hand, the tectonothermal evolution of Palaeoproterozoic khondalite series rocks is characterized exclusively by nearly isothermal decompression following the peak of metamorphism and then cooling, defining clockwise P–T paths. The Archaean TTG gneisses and associated mafic rocks with anticlockwise metamorphic P–T paths reflects an origin related to underplating and intrusion of mantle-derived magmas which may be derived from mantle plumes. They represent a late Archaean continental block in the western part of the North China Craton. The Palaeoproterozoic khondalite series rocks represent passive continental margin deposits. They were metamorphosed and deformed in the late Palaeoproterozoic during the amalgamation of the western continental block with another continental block in the east part of the North China Craton. The ITD-type clockwise P–T–t paths of the Palaeoproterozoic khondalite series rocks record the tectonothermal histories of the collision of the western and eastern continental blocks which resulted in the final assembly of the North China Craton at c. 1800 Ma. 相似文献
999.
钙碱性火山岩构造背景的研究进展 总被引:20,自引:0,他引:20
通过对钙碱性火山岩的岩石学、地球化学、同位素及其构造背景的研究表明,钙碱性火山岩的形成不一定仅限于板块俯冲过程,在不具备板块俯冲的其它构造环境下也能够形成。 相似文献
1000.