反滤回灌井的结构设计理论和方法   总被引：1，自引：0，他引：1  

李旺林 《地下水》2009,31(1):126-129

反滤回灌井是地下水库中一种有效的回灌设施,它由回灌井和回灌池组成,回灌池位于井口、具有反滤功能。介绍了反滤回灌井单井回灌量的计算方法,提出反滤回灌井结构设计的原则和方法。回灌池反滤结构应有两层,上部反滤层应能过滤回灌水中的杂质,选择较细的砂粒;下部反滤层应能防止上层反滤料通过井盖的孔口落入井内,选择较粗的砾类。从过流能力和水流流态的角度。对回灌池的外型进行了优化,探讨了回灌池池口和池底横截面面积的比例,提出应选择抛物线型竖向剖面,同时介绍了回灌池防淤和抗冲设计的方法。  相似文献   

油气层录井的精细解释方法 ——以吉林探区为例     

宋立春 《世界地质》2009,28(1):92-97

采用“四大参数法” (峰值、峰基比、甲烷和重烃) 、全烃曲线形态法和全烃储层灌满系数法, 解决了吉林探区油气层气测低异常和组分发育不全等问题。进一步以地化录井为核心, 结合核磁孔隙度和色谱油性, 建立了地化含油饱和度储层评价体系, 解决了油气层荧光、气测显示异常和电测低电阻的油层评价难题。  相似文献   

水泥粉煤灰碎石桩工程实例     

尚晋敏 《中国勘察设计》2009,(6):74-76

通过某高层住宅地基处理的设计实例,分析了水泥粉煤灰碎石桩（CFG桩）的特性,指出了水泥粉煤灰碎石桩使用时须注意的要点。  相似文献   

我国探月工程可采用的一种月球钻探取样方法的初步分析   总被引：3，自引：0，他引：3  

段新胜  鄢泰宁  顾湘  段苏浩 《地质科技情报》2009,28(6)

美国和前苏联已完成的月球取样方法分别是载人登月取样和地面遥控取样钻机取样。基于美国和前苏联的方法,提出了一种可供我国嫦娥工程选用的月壤钻探取样方案,即用遥控取样钻机,配备硬质合金钻头、空心螺旋钻具,采用振动-回转钻进工艺。在高真空和低重力条件下,可选用空心螺旋钻具来解决排屑和钻压问题。顺利排屑的基本条件为钻具的螺旋升角应小于月壤与钻具之间的摩擦角、钻具的回转速度应大于临界转速。通过分析计算可知在月球上采用外螺旋钻具时,临界转速比在地球上要小得多,因此在获得同样的回转力矩条件下可匹配较小功率的电动机。  相似文献   

“Doing” Critical Geographies with Numbers   总被引：2，自引：1，他引：1  

Tim Schwanen  Mei-Po Kwan 《The Professional geographer》2013,65(4):459-464

Criticisms of quantitative geography have a long history in our discipline. Since the emergence of early Marxist geography, the advent of new theoretical traditions has been accompanied by sustained and sometimes vigorous critiques of spatial analysis. In this introductory article to the second focus section on critical quantitative geographies, we discuss the accuracy of some of the criticisms about the use(s) to which spatial analysis is put and about the philosophical presumptions underpinning quantitative geographies. We argue that spatial analysis and critical geographies should not be considered mutually exclusive of one another—although this does not mean that numbers and critical geographies are entirely comfortable with one another. We suggest that critical geographies cannot dispense with numbers and visualizations based on numerical information. We hope that the articles collected here will inspire geographers to engage with numbers and statistics to challenge inequality and imagine alternative futures.  相似文献   

柴达木盆地石炭系地球物理特征及解释     

尹成明  王财富  马寅生  程烨  程海艳 《地球物理学进展》2013,28(4)

柴达木盆地具有丰富的油气资源,柴北缘、柴西、粜东三湖地区分别以侏罗系、古近系、新近系和第四系为主要勘探目的层.随着北疆石炭系研究的进展和钻探的成功,石炭系已经成为中国西部地区重要的勘探层系,柴达木盆地的石炭系也引起了勘探家的注意,地面地质调查表明石炭系为柴达木盆地一套潜在烃源岩.为了落实石炭系在柴达木盆地内的分布,笔者充分利用近10年来在柴达木盆地及周缘完成的重、磁、电等资料进行了针对石炭系的资料解释、剥层反演和综合研究,明确了石炭系的分布特征,为柴达木盆地石炭系油气勘探指明了方向.  相似文献   

Condensed hyperelements method of non-vertical consistent boundaries for wave propagation analysis in irregular media     

S. Dorafshan  F. Behnamfar  A. Khamesipour  M. Motosaka 《地震工程与工程振动(英文版)》2013,12(4):547-559

The study of wave propagation in finite/infinite media has many applications in geotechnical and structural earthquake engineering and has been a focus of research for the past few decades. This paper presents an analysis of 2D anti- plane problems （Love waves） and 2D in-plane problems （Rayleigh waves） in the frequency domain in media consisting of a near-field irregular and a far-field regular part. The near field part may contain structures and its boundaries with the far-field can be of any shape. In this study, the irregular boundaries of the near-field are treated as consistent boundaries, extending the concept of Lysmer＇s vertical consistent boundaries. The presented technique is called the Condensed Hyperelements Method （CHM）. In this method, the irregular boundary is limited to a vertical boundary at each end that is a consistent boundary at the far-field side. Between the two ends, the medium is discretized with hyperelements. Using static condensation, the stiffness matrix of the far-field is derived for the nodes on the irregular boundary. Examples of the application of the CHM illustrate its excellent accuracy and efficiency.  相似文献   

Perfectly matched layer-absorbing boundary condition for finite-element time-domain modeling of elastic wave equations   总被引：2，自引：0，他引：2  

Zhao Jian-Guo  Shi Rui-Qi 《应用地球物理》2013,10(3):323-336

The perfectly matched layer (PML) is a highly efficient absorbing boundary condition used for the numerical modeling of seismic wave equation. The article focuses on the application of this technique to finite-element time-domain numerical modeling of elastic wave equation. However, the finite-element time-domain scheme is based on the second-order wave equation in displacement formulation. Thus, the first-order PML in velocity-stress formulation cannot be directly applied to this scheme. In this article, we derive the finite-element matrix equations of second-order PML in displacement formulation, and accomplish the implementation of PML in finite-element time-domain modeling of elastic wave equation. The PML has an approximate zero reflection coefficients for bulk and surface waves in the finite-element modeling of P-SV and SH wave propagation in the 2D homogeneous elastic media. The numerical experiments using a two-layer model with irregular topography validate the efficiency of PML in the modeling of seismic wave propagation in geological models with complex structures and heterogeneous media.  相似文献   

On the impossibility of mean-field dynamos with some spherical symmetry of the motions     

Jürgen Reichert 《地球物理与天体物理流体动力学》2013,107(3-4):213-226

Abstract

A spherical mean-field dynamo model is considered in which both the mean motion and the mean electro-motive force due to fluctuating motions show some spherical symmetry. It is shown that under some reasonable assumptions the magnetic field is bound to decay to zero.  相似文献   

Residual vorticity induced by the action of tidal currents in combination with bottom topography in the Southern Bight of the North Sea     

G. J. Komen  H. W. Riepma 《地球物理与天体物理流体动力学》2013,107(1-2):93-110

Abstract

Results are presented of calculations on the generation of residual vorticity by tidal currents over the bottom topography of the Southern Bight of the North Sea. A typical order of magnitude is 10^?6 to 10^?7 s ^?1. This is compared with current measurements on calm days, when similar magnitudes are found. At windspeeds less than about 5 m/s tidal generation of residual vorticity is important; at higher windspeeds wind effects begin to dominate. Our results are relevant in understanding the spatial variability of residual currents, because a non-zero vorticity implies the existence of horizontal gradients in the residual current field.  相似文献