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271.
在分析了现有用于第四纪松散沉积物的取样器及取样方法的优缺点的基础上,作者研制了一种新型的古地磁土样取样器,本文介绍它的结构,特点及使用方法。 相似文献
272.
273.
本文根据广东沙环核电厂厂址地震地质环境特点和有关核法规的技术要求完成了设计地面运动时程的人工合成。从持续时间、合成精度、包络设计谱、功率谱密度函数、多根合成时程的统计不相关等方面讨论了该人工合成设计时程对ASCE4-86StandardandCom-mentaryonStandard和U.S.NRCSatndardReviewPlan两个基本法规技术要求的可接受性。 相似文献
274.
云南红宝石矿床中镁砂川闪石的发现及其意义 总被引:1,自引:1,他引:1
镁砂川闪石是1984年在日本发现的 新矿物,在世界上产地很少。本文对其物理性质、化学成分、X射线粉晶衍射和红外吸收光谱等方面进行了研究。 相似文献
275.
冻土单轴蠕变过程中结构变化的CT动态监测 总被引:9,自引:4,他引:9
CT为岩土材料非破坏的持续检测和内部结构的定量描述提供了可能,利用这一手段观测分析了冻土单轴蠕变过程中结构的变化情况,结果表明蠕变过程中结构缺陷的增生与扩展制约着土的结构的强化与弱化作用,控制着蠕变过程形态特征。易破坏区首先发生于样品的低密段,在软弱段的某一薄弱层面形成一环状低密带,然后向外扩展,最终导致整体结构的破坏。 相似文献
276.
CHARACTERISTICS OF THE SURFACE AND ATMOSPHERIC HEATING FIELDS OVER QINGHAI-XIZANG PLATEAU FOR THE PERIOD FROM AUGUST 1982 TO JULY 1983 总被引:2,自引:1,他引:2
The surface and atmospheric heating fields over the Qinghai-Xizang Plateau are computed by using theobservational data of solar radiation during 1982—1983.The mian results are as follows:The central andnorthern parts of the Plateau act as heat sinks in winter from November to January.Both eastern and south-ern parts of the Plateau are of heat sources.In summer,the main part of the Plateau acts as a strong heatsource,and the center of the heating field is in the southeastern Plateau.However the main part of thePlateau acts as a heat sink for the atmospheric heating fields from October to March.The maximum intensityof the atmospheric heat sink over the central Plateau appears in December and January.From April toSeptember,the main part of the Plateau acts as a heat source for the atmospheric heating fields. 相似文献
277.
278.
Rock magnetic measurements of Nihewan sediments from Xujiayao section demonstrate that magnetite, hematite and maghemite are
dominant remanent magnetization carriers. Monitoring the variations of magnetic susceptibility (MS) and saturating isothermal
remanent magnetization (SIRM) at low temperature are the attractive ways of detecting the presence of magnetite, maghemitization
and superparamagnetic grain sizes. Low-temperature MS investigations suggest that susceptibility enhancement for Xujiayao
samples is mainly due to the remarkable presence of SD/MD magnetite to some degree though some magnetite grains have been
partially oxidized at some depths. It is tentatively concluded that both SD/MD magnetite and hematite are of detrital origin
and carry a characteristic remanent magnetization (ChRM), whereas maghemite can be attributed to be chemical origin, overprinting
a reversed polarity component of Matuyama age. 相似文献
279.
Cunde Xiao Tandong Yao Dahe Qin Seko Katsumoto Jianchen Pu Wenkun Sheng 《中国科学D辑(英文版)》2002,45(4):300-310
Liquid conductivity (EC) measurement was conducted for the samples collected from several snow pits and ice cores over the
Qinghai-Xizang (Tibet) Plateau, with their time range covering seasonal, decadal and centennial scales. Unlike the previous
attention mostly focused on the acidity (H+) responding to the solid conductance (ECM) of glacial ice, we introduce the alkalinity (OH−) of snow and ice to show how it responds to EC. Strong linear relationship was established between EC and OH− for these snow pits and ice cores. Positive correlation is also established between EC and major cations (Ca2+, Mg2+, Na+ and K+). Since the cations are known as the proxies for the intensity of mineral dust influx onto glaciers of the northern Qinghai-Xizang
Plateau, we believe that EC could be used as an indicator for the history of dust input in deep ice core study. In fact, records
in Guliya ice core since the Little Ice Age (LIA) indicate that dust load in glacier may depend on the combination of temperature
and humidity. “Cold-dry” combination favors the dust arising, and results in higher EC and OH− values, while “warm-wet” combination prevents dust form and EC and OH− values are lower. In the past century, with the atmospheric warming and precipitation increasing over the northern plateau,
which means an atmospheric condition of dust decreasing, both EC and OH− displayed rapid decline. 相似文献
280.
The seismotectonic environment and seismic activity in Southwest China region were studied based on new data and new results obtained during the Eighth and Ninth Five-Year Plans,the seismic areas and zones and potential seismic source zones were determined.and the relation between seismic activity parameters and ground motion attenuation was determined.Finally the seismic gound motion zoning maps of the Pangxi region was compiled by using the multi-parameter and multi-scheme method. 相似文献