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151.
张克非 《武汉大学学报(信息科学版)》1990,(3)
本文在顾及局部地形改正、椭球改正及大气改正的情况下,采用实测数据,应用Meissel方法和Wenzel频谱分析方法,对某盆地边缘的高程异常进行了实际计算。并将计算结果同多普勒高程异常进行了比较,证明结果是良好的。此外还对我国精确高程异常的确定提出了一些建议。 相似文献
152.
本文基于笔者采用过的同时考虑房屋层数和场地类别时烈度到水平向地面峰值转换的基本思路,统计研究了烈度与竖向地面峰值的对应关系,明确指出了不同烈度下竖向与水平向峰值的比值应该是有所不同的,并给出了建议的比值,给果可供一般工程抗震设计参考使用。 相似文献
153.
154.
155.
Dirk Goossens 《地球表面变化过程与地形》1985,10(4):353-362
A torn-up road offered the opportunity to sample a dust cloud continuously at different heights during a time interval of 51 hours. In particular the granulometrical characteristics of the dust caught were investigated. It appears that if the air layer in the vicinity of a dust cloud is not too turbulent, the cloud will be clearly granulometrically stratified. The coarse material moves chiefly at the bottom of the cloud, whereas the fine material will occur both at the bottom and at the top. The experiment also shows that the higher the dust in the cloud, the worse it is sorted. Above a critical height, however, the degree of sorting increases again. The variation of the mean dust diameter d50, as a function of the height z, can be expressed in a simple semi-logarithmic equation. The variation of the dust quantity G, as a function of the height z, can also be expressed in a semi-logarithmic form but the correlation is higher when a power equation is used. The ratio of fine silt to coarse silt seems to vary parabolically with height. One can only speak of an optimal transport height in the case of particles > 16 μm. For finer particles, the turbulence of a normal air stream is usually high enough to carry the particles anywhere in the dust cloud, so that one can no longer speak of an optimal transport height. The granulometrical border between aeolian transport in saltation and aeolian transport in suspension lies, according to the results of the experiment, at a diameter of about 63 μm. 相似文献
156.
The heights of the daytime convective boundary layer (CBL), computed by a one-dimensional model for a bare soil surface at a semi-arid station,Anand, during the dry and hot summer month of May 1997, are presented. As input, the model requires surface heat flux, friction velocity and air temperature as functions of time. Temperature data at the one-metre level from a tower and sonic anemometer data at 9.5 m collected during the period 13–17 May 1997 in the Land Surface Processes Experiment (LASPEX-97) are used to compute hourly values of surface heat flux, friction velocity and Obukhov length following the operational method suggested by Holtslag and Van Ulden [J. Climate Appl. Meteorol.
22,517–529 (1983)]. The model has been tested with different values for the potential temperature gradient ( ) above the inversion. The model-estimated CBL heights comparefavourably with observed heights obtained from radiosonde ascents. 相似文献
157.
腰英台油田是东北地区新发现的油田,目前刚开始勘探开发,在勘探开发初期遇到不少问题。其中之一是开采时高含水:就油田的实际油水分布特征进行了分析,分析油水同出的可能原因,认为这是受油藏储层物性及构造幅度和实际油柱高度的影响,由于储层低孔、特低渗。实际构造幅度低,实际油柱高度大多低于油藏产纯油所需的油柱高度,致使油藏大都处于油水过渡带。故开采时多含水,油水同出。根据这一分析,认为进一步的油气勘探重点考虑西部水下冲积扇的有利部位。此处储层物性好,有利于接受更多油源。 相似文献
158.
Barchans of Minqin: Morphometry 总被引:2,自引:0,他引:2
The barchans on the border of Minqin oasis, China, were surveyed. Our data reconfirmed that the height of slipface is proportional to the width of horns and the baseline can be roughly described by parts of an ellipse and a parabola. We attempted to study dune geomorphology using the theory of differential geometry. The geometrical characteristics of the brink can be quantitatively determined by its curvature and torsion. 相似文献
159.
We report on the use of X-ray diffractometry under controlled conditions of temperature and relative humidity (RH-XRD) for
the investigation of NaCl deliquescence in the pore space of glass filter frits, which were used as model substrates. The
study confirms that RH-XRD is an appropriate experimental technique for the in situ observation of phase transformation in
porous materials. It is used for an investigation of both the deliquescence kinetics and the deliquescence humidity within
pores of different median pore diameter. Several major influences affecting deliquescence rates in the pore space close to
the surface of a porous material are discussed. It appears that quite short-term variation of ambient relative humidity, e.g.,
typical daily fluctuations, might induce damaging deliquescence–crystallization cycles within the pore space of building materials.
In agreement with theoretical considerations it was found that confinement of NaCl crystals in pores with median diameters
in the range 1.4–70 μm does not affect the deliquescence humidity of the salt. 相似文献
160.
H. Nahavandchi 《Journal of Geodesy》2002,76(6-7):345-352
It is suggested that a spherical harmonic representation of the geoidal heights using global Earth gravity models (EGM) might
be accurate enough for many applications, although we know that some short-wavelength signals are missing in a potential coefficient
model. A `direct' method of geoidal height determination from a global Earth gravity model coefficient alone and an `indirect'
approach of geoidal height determination through height anomaly computed from a global gravity model are investigated. In
both methods, suitable correction terms are applied. The results of computations in two test areas show that the direct and
indirect approaches of geoid height determination yield good agreement with the classical gravimetric geoidal heights which
are determined from Stokes' formula. Surprisingly, the results of the indirect method of geoidal height determination yield
better agreement with the global positioning system (GPS)-levelling derived geoid heights, which are used to demonstrate such
improvements, than the results of gravimetric geoid heights at to the same GPS stations. It has been demonstrated that the
application of correction terms in both methods improves the agreement of geoidal heights at GPS-levelling stations. It is
also found that the correction terms in the direct method of geoidal height determination are mostly similar to the correction
terms used for the indirect determination of geoidal heights from height anomalies.
Received: 26 July 2001 / Accepted: 21 February 2002 相似文献