防爆低频电法透视仪

介绍了一种新型、实用的井下物探仪器－－防爆低频电法透视仪的结构、原理及其配套的资料处理软件系统。该仪器自动化程度高，抗干扰能力强，测量准确，能直实地反映地质情况。     

TBB-REVEALED ANNUAL CYCLE FEATURES OF TROPICAL LFO*

In the context of 1980-1992 JMA(Japan Meteorological Agency) GMS TBB gridded dataset,study is undertaken of annual cycle features of FFT-derived window power spectrum averaged over the record length,with localized space/time characteristics of low-frequency oscillation(LFO) in the tropical atmosphere investigated alongside possible causes.It turns out that the LFO takes on surprisingly noticeable annual cycle features marked by a wider variable range of the LFO periods over northern tropics than the southern counterpart and equatorial vicinity.In addition,on the whole,the signals are more intense in the Northern Hemisphere during summer/autumn and at equatorial/southern latitudes when northern winter/spring occur as well.Also,not all these features are identical for different segments at the same latitudes,displaying signatures on a local basis,and the spatial/temporal locality can be qualitatively interpreted in terms of nonlinear interaction between tropical waves,and modulation of diabatic heating on the LFO periods.     

黄河上游水电工程对局地气候的影响

本文阐述了黄河上游段水电工程概况，并以刘家峡和龙羊峡水库为主对库周各站建加前后各５年或１０年的气象资料进行了对比分析，揭示了水库对周围地区各气候因子影响程度。     

青林省含铁地下水的分布与处理措施

本文根据含铁地下水的形成条件将吉林省含铁地下水划分为四个区,并论述了各区的分布特征。综合国内目前各种地下水除铁技术,着重对各除铁系统的方法、基本原理和适用条件以及经济效益等进行了论述。从环境水文地质学的角度,提出了在含铁地下水区寻找低铁地下水的方法,并通过实例验证是可行的。     

复合片钻头钻进时机械钻速和碎岩功耗的研究

关于复合片钻头钻进大理岩和花岗岩时机械钻速和碎岩功率消耗同规程参数的关系,用实验设计方法进行了试验研究,得出了机械钻速和碎岩功耗与钻压、钻头转速及冲洗液量关系的数学模型;提出了碎岩绝对功耗和相对功耗的概念,而相对碎岩功耗是个更为重要的概念,求出了大理岩相对碎岩功耗最小时的最优钻进规程参数值。     

A NUMERICAL EXPERIMENT OF DYNAMIC EFFECT OF QINGHAI-XIZANG PLATEAU ON SUMMER ATMOSPHERIC LOW FREQUENCY VARIATION

In this paper a numerical experiment is presented of the plateau's dynamic effect in terms of a two-layer spectralmodel, and the focus is put on the large-scale orography-excited ALFV with the summer flow pattern as background.together with its propagation and distribution of some features. The main results are as follows: (1) With the summerflow pattern as background the Plateau can excite ALFV, which is characterized by strong regionality. (2) ALFV of thiskind has a baroclinic (equivalent barotropic) structure on the south (north) side of the topography. (3) Its propagation ismarked by dispersion of quasi-stationary Rossby waves over a spherical surface.     

P-范分布与P-范最小平差

本文提出了 n元p-范分布的概念,从而在极大似然估计的基础上将最小二乘法与一范及无穷范最小平差法统一起来。随后本文还给出了p-范最小平差的计算方法。     

四川盆地志留系生油层主要地质特征

本文利用地质、钻井、测井、试油、实验等项资料.通过沉积相演变,古构造位置对有利生油岩发育的控制,有机质向油气的转化、生成及运移的研究,对四川盆地志留系进行含油气性远景评价和勘探有利区块的预测。     

Virtual rate and mean distance of travel of individual clasts in gravel-bed channels

Travel distances in gravel-bed rivers of tagged particles of various sizes are related to excess stream power estimated for peak discharge. Mean distance of movement, irrespective of grain size, is weakly correlated with stream power, especially near the threshold of movement. There may be several reasons for the weak correlation, including variable effects of bed structure, varying magnitudes of sediment mobilizing events and sampling problems. Grain size itself is of marginal significance. The virtual rate of travel calculated using total time for which the flow is larger than that needed to initiate clast movement also bears a weak relation to the excess stream power over the period. Better results are obtained by relating the virtual rate of travel to the first peak of the flow event only. This implies that the initial seeding of the tagged particles dominates the observations. Nonetheless, an underlying general relation is indicated by the data, which are derived from a wide range of flow regime types.     

The correlation of whistler occurrence rate at a low latitude with thunderstorm activity at its conjugate region and with solar activity

The correlations of occurrence rate of whistlers in January during one solar cycle (1977–1987) at a low latitude station (Yamaoka, geomag. lat. 25°, L=1.26) with thunderstorm activity near its conjugate region and also with solar activity have been investigated, and it is found that the occurrence rate has no correlation with the lightning flashes near the conjugate point, while it is negatively correlated with solar activity. On the basis of these findings it is suggested that the ionospheric absorption is of major importance in the long-term variation of whistler occurrence rate, with the duct formation being of secondary effect, while the lightning activity is only a necessary condition for whistler occurrence.