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951.
本文从列阵器件测量精度的估计公式出发,推导了用低精度A/D变换器件获得高精度测量结果的一般性证明,还讨论了这种方法的若干可能应用。  相似文献   
952.
固体潮观测数据在进行各种分析之前,需进行平滑处理以便消除各种突跳及错误数据。常用的平滑方法有Lecolazet数字滤波法和Nakai方法。本文讨论了各种方法的特点及存在问题。为了经济、快速而又有效地平滑数据,提出如下建议:对于高精度的观测数据,通常使用数字滤波法处理即可;在少数情况下,数据中出现连续错数,这时可取卅天为时间间隔,在上述滤波法平滑的基础上,分段对数据进行调和分析,如果某几段调和分析的误差较大,那末再进一步对这些数据段用Nakai法进行平滑处理。  相似文献   
953.
IntroductionThe Liaodong Paleoproterozioc fold belt is locat-ed at eastern China -- Korea craton, from Liaodongpeninsula through southern Jilin to north Kore$tothe east, to west Jiaodong peninsu1a to the west. Al-though many discussions, in the literature…  相似文献   
954.
扇贝氨基多糖的红外光谱分析   总被引:1,自引:0,他引:1  
从海湾扇贝中提取出具有抗凝活性的氨基多糖,其中,氨基己糖含量为22.60%,己糖醛酸含量为23.30%,含硫量为6.66%。样品经KBr压片,于10DX-FTIR红外光谱仪中进行光谱扫描,发现,该多糖具有典型的氨基多糖红外光谱,分子中含有-NH,-COO,-OSO3^-等氨基多糖特征基团。与氨基多糖标准品-肝素,6-硫酸软骨素和透明质酸的红外光谱进行比较分析,表明,扇贝氨基多糖与肝素的红外光谱相似  相似文献   
955.
应用因子分析法研究密鲴繁殖力与诸因素的关系。六个变量是体长、体重、成熟系数、绝对怀卵量和相对怀卵量。29个样本、经正交变换得到3个因子:绝对繁殖因子、相对繁殖因子和成熟因子。  相似文献   
956.
The HY-2 satellite was successfully launched on 16 August 2011. The HY-2 significant wave height (SWH) is validated by the data from the South China Sea (SCS) field experiment, National Data Buoy Center (NDBC/ buoys and Jason-1/2 altimeters, and is corrected using a linear regression with in-situ measurements. Com- pared with NDBC SWH, the HY-2 SWH show a RMS of 0.36 m, which is similar to Jason- 1 and Jason-2 SWH with the RMS of 0.35 m and 0.37 m respectively; the RMS of corrected HY-2 SWH is 0.27 m, similar to 0.27 m and 0.23 m of corrected Jason-1 and Jason-2 SWH. Therefore the accuracy of HY-2 SWH products is close to that of Jason-1/2 SWH, and the linear regression function derived can improve the accuracy of HY-2 SWH products.  相似文献   
957.
当前海洋磁力探测中为了消除或减小地磁日变化的影响,必须设立地磁日变观测站(简称日变站)测量磁场变化,提供日变校正资料。依据多年工作经验,对作为基站使用的G882磁力仪和Sentinel磁力仪在工作原理、仪器技术性能、工作使用体会等方面进行综合比较分析。结果表明,Sentinel磁力仪比G882磁力仪对环境适应性更好、灵活性更强,进行日变观测时应优先选用。  相似文献   
958.
The isotopic composition and parameters for deuterium excess of brines, which were sampled in the Si-chuan Basin, show obvious regularities of distribution. The brine isotopic composition shows distinct two systems of marine and terrestrial deposits, with the Middle Triassic strata as the boundary. Brine hydrogen isotopic composition of marine deposits is lower while oxygen isotopic composition is higher than that of the SMOW, respectively, indicating that the brines were derived from seawater with different evaporating degrees at different times. From the Sinian strata, up to the Cambrian, Permian Maokou Formation and the Triassic Jialingjiang Formation, the δD values of brines tend to become relatively positive with the strata becoming younger. Brines of terrestrial deposits are considered to have been derived from precipitation and their isotopic composition is close to the globe meteoric water line (GMWL). Brines of transitional deposits between marine and terrestrial ones (the Upper Triassic Xujiahe Formation) have δD and δ18O values falling between the two end members of marine deposit brines and precipitation, indicating that the brines are a mixture of precipitation and vaporing seawater. Water samples from the brine-bearing strata of different ages show various deuterium excesses (d) with an evident decreasing trend as the age of strata gets older and older. Brine-bearing strata of the Triassic Leikoupo-Jialingjiang Formation, the Permian Maokou Formation, the Cambrian and Sinian strata are all carbonate rocks which have experienced intensive water/rock reaction and the deuterium excess essentially changes with time. All brine-bearing-strata surrounding the basin or faults, as well as those brine wells exploited for resources, have been obviously influenced by the precipitation supply. Therefore, the deuterium excesses of their brines have increased to different extents, depending on the amount of involvement of meteoric water. The variation and distribution of d values of the brines from different Triassic strata are related to the embedded depth of the strata. The deuterium excesses of brines become lower with increasing burial depth of the strata.  相似文献   
959.
The source region of the Yellow River is located in the middle east of the Tibetan Plateau in northwest China. The total area is about 51,700 km2, mainly covered by grassland (79%), unused land (16%) and water (4%). The increasing land utilization in this area has increased the risk of environmental degradation. The land use/cover data (1985 and 2000) provided by the Data Center of Resources and Environment in the Chinese Academy of Sciences were used to analyze the land cover change in the source region of the Yellow River. DEM (1:250,000) data, roads and settlement data were used to analyze the spatial characteristics of grasslands degradation. The ArcGIS 9 software was used to convert data types and do the overlay, reclassification and zonal statistic analysis. Results show that grassland degradation is the most important land cover change in the study area, which occupied 8.24% of the region’s total area. Human activities are the main causes of the grassland degradation in the source region of the Yellow River: 1) the degradation rate is higher on the sunny slope than on the shady slope; 2) the grassland degradation rate decreases with an increase in the elevation, and it has a correlation coefficient of -0.93; 3) the nearer to the settlements the grassland is, the higher the degradation rate. Especially within a distance range of 12 km to the settlements, the grassland degradation rate is highly related with the distance, with a coefficient of -0.99; and 4) in the range of 4 km, the degradation rate decreases with the increase of distance to the roads, with a correlation coefficient of -0.98. Besides some physical factors, human activities have been the most important driving forces of the grassland degradation in the source region of the Yellow River since 1985. To resolve the degradation problems, population control is essential, and therefore, it can reduce the social demand of livestock products from the grassland. To achieve sustainable development, it needs to improve the management of grassland ecosystem.  相似文献   
960.
近几年来虚拟天文台技术的发展极为迅速,各国虚拟天文台研究相继启动,一系列虚拟天文台标准被提出并投入应用,有效地推动了信息技术在天文研究中的应用。科学工作流技术作为高性能计算与虚拟天文台中的关键技术,一直是研究的重点。但长期以来,受到业务工作流技术的影响,科学工作流的具体功能与作用,一直不被广大天文工作者理解和重视,限制了科学工作流的推广与应用。对科学工作流进行了深入分析,介绍了其基本功能和业务模型,详细比较了与业务工作流的差异。最后讨论了科学工作流在天文研究中的应用方法,对科学工作流的发展进行了展望。  相似文献   
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