塔河油田3区石炭系超深薄层碎屑岩储层预测研究     

盛海波  刘蕊  付国民  蔡玥  张庭娇 《西安地质学院学报》2011,(4):390-396

针对塔河油田3区石炭系卡拉沙依组地震数据很难识别薄砂体的问题,对比分析了采用地震资料提频处理、分频处理、储层高分辨率敏感参数反演等不同手段得到的储层预测结果,筛选出高分辨率储层敏感参数反演作为卡拉沙依组砂泥岩段储层主要预测手段。通过探讨砂泥岩对声波时差的响应,以及对比分析自然电位、自然伽马以及补偿中子孔隙度与声波时差的关系,确定自然电位与声波时差的相关性最好,由此选取自然电位作为最佳电性敏感参数参与高分辨率敏感参数反演预测。从井点、剖面、平面等方面检验和评价高分辨率储层预测成果,结果表明其反演预测效果较好,符合塔河油田3区石炭系的储层预测要求,实现了对石炭系主力砂体空间展布的解释与描述,建立了塔河油田3区石炭系卡拉沙依组储层模型。  相似文献   

基于雷达回波最大重叠率的一种临近降水预报方法          下载免费PDF全文

李建通  高守亭  郭林 《大气科学》2011,35(3):519-530

基于天气雷达的临近降水预报是雷达短时预报业务系统的重要组成部分,本文在回顾雷达临近降水预报技术发展的基础上,充分考虑新一代天气雷达高时间、空间分辨率的优点,提出两个相邻时刻雷达回波具有最大重叠率的移向、移速是与降水系统整体的移向、移速密切相关的论点,再用此移向、移速对当前雷达回波进行平移,最后采用九点平均的回波生消模型...  相似文献   

江苏省冬小麦播种期对气候要素变化的响应   总被引：7，自引：2，他引：5  

张佩  高苹  刘彦丽 《气象科学》2011,31(6):763-769

利用江苏省35个气象台站1961- 2009年冬小麦播种期内的气象观测资料,采用数理统计方法,分析了近49 a来冬小麦播种期内各气候要素的变化.结果表明:江苏省冬小麦主要播种期内的日平均气温随着时间的推移逐渐升高,且相关显著,其中淮河以南地区升高速度更快;秋季稳定通过15℃的终日总体呈逐年推迟趋势,尽管部分年际间波动较大;按传统播期播种到越冬的≥0℃有效积温与年序也呈极显著正相关关系.分析沭阳、淮安、盱眙、滨海、赣榆和徐州6个农业气象观测站的冬小麦发育期资料,及当地冬小麦播种至越冬前积温资料.结果表明:各地冬小麦播种至越冬≥0℃有效积温总体上逐年增加.此外,冬小麦播种期内降水量的波动较大,尤其自1990s中期以来,各地降水量呈逐年递减趋势.得出结论:江苏省冬小麦应适时晚播,并应趁墒及时播种.  相似文献   

渭河盆地中土层场地对地震动的放大作用   总被引：11，自引：1，他引：10       下载免费PDF全文

王海云 《地球物理学报》2011,54(1):137-150

土层场地对地震动的影响较大,建(构)筑物的选址及其抗震设防必须考虑土层场地的放大作用,以避免或减轻其震害.汶川地震中,布设在渭河盆地中的数字强震动台网共有27个台站(包括2个基岩台站和25个土层台站)获得良好的主震加速度时程.利用这些加速度时程,选择汤峪台做为参考场地,基于考虑几何衰减的传统谱比法分析研究了25个土层场...  相似文献   

松辽盆地深层地震资料叠前时间偏移连片处理技术研究   总被引：2，自引：0，他引：2       下载免费PDF全文

裴江云  张丽艳  王丽娜  林文  张晶  徐伟 《地球物理学报》2011,54(2):294-303

为了建立松辽盆地等时地层格架,深入认识松辽盆地地质特征和结构以及油气聚集规律,本文开展了松辽盆地不同工区、不同时期采集的二维和三维地震资料叠前连片处理技术研究.本文针对叠前连片处理过程中不同区块的非一致性,采用了相应的处理方法和手段,使得连片处理后数据的相位达到一致,区块间拼接带的频率、能量(或振幅)变化自然合理.处理...  相似文献   

基于异常线圈的时间域AEM系统测试和标定方法研究   总被引：3，自引：2，他引：1       下载免费PDF全文

嵇艳鞠  李肃义  于生宝  朱凯光  周逢道  王言章  王世隆  刘焕江  任广群  林君 《地球物理学报》2011,54(10):2690-2697

为了检验和测试时间域航空电磁系统的测量精度和有效性,采用地面铺设闭合的异常线圈模拟地下有限导体的方法,将异常线圈的电磁响应理论值与系统实测数据进行拟合分析,来确定系统误差和飞行几何参数误差.在计算异常线圈电磁响应的基础上,研究了衰减曲线、剖面曲线与线圈的电性、几何参数关系,设计了野外测试实验方案.在长春市大鹅岛附近,采用吊车进行了系统测试,测试结果表明:单点实测数据的平均绝对误差为0.48 mV,系统相对误差小于1%,飞行高度误差为0.4 m、水平偏移误差为0.2 m.基于异常线圈进行时间域航空电磁系统的测试和标定,是一种准确、快速、经济可行的方法,具有野外施工便捷、参数调整灵活等特点,适用于任何时间域电磁测量系统的检测.  相似文献   

Towards quantitative evaluation of gas injection using time‐lapse seismic data     

Reza Falahat  Asghar Shams  Colin MacBeth 《Geophysical Prospecting》2011,59(2):310-322

Of particular concern in the monitoring of gas injection for the purposes of storage, disposal or improved oil recovery is the exact spatial distribution of the gas volumes in the subsurface. In principle this requirement is addressed by the use of 4D seismic data, although it is recognized that the seismic response still largely provides a qualitative estimate of moved subsurface fluids. Exact quantitative evaluation of fluid distributions and associated saturations remains a challenge to be solved. Here, an attempt has been made to produce mapped quantitative estimates of the gas volume injected into a clastic reservoir. Despite good results using three accurately repeated seismic surveys, time‐delay and amplitude attributes reveal fine‐scale differences though large‐scale agreement in the estimated fluid movement. These differences indicate disparities in the nature of the two attributes themselves, which can be explained by several possible causes. Of most impact are the effects of processing and migration, wave interference effects and noise from non‐repeatability of the seismic surveys. This subject highlights the need for a more careful consideration in 4D acquisition, amplitude processing and use of true amplitude preserving attributes in quantitative interpretation.  相似文献   

Comparing landscape evolution models with quantitative field data at the millennial time scale in the Belgian loess belt     

A. J. A. M. Temme  I. Peeters  E. Buis  A. Veldkamp  G. Govers 《地球表面变化过程与地形》2011,36(10):1300-1312

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Changes of P, Ca, Al and Fe contents in fringe marshes along a pedogenic chronosequence in the Pearl River estuary, South China   总被引：2，自引：0，他引：2  

Rong Xiao  Honggang ZhangHaifeng Gao  Xinhui LiuAndreas Wilkes 《Continental Shelf Research》2011,31(6):739-747

Soil and plant samples were collected in four fringe marsh zones (i.e., A, B, C and D zones) along a pedogenic chronosequence in the Pearl River estuary in the Spring of 2009. Samples were subjected to a total digestion technique and analyzed for P, Ca, Al and Fe in order to study the changes of nutrient contents, storages in soils and their bioavailabilities to wetland plants (e.g. Cyperus malaccensis) in four zones. Results showed that soil Ca increased with depth along soil profiles, while P, Al and Fe generally kept constant in soil profiles in four zones. Al and Fe contents in the top 10 cm soils showed significant decreases from D to A zone, while a significant increase in Ca contents (P<0.05). Significant increases along pedogenic chronosequence for P, Al and Fe at 30-40 cm soil horizons were also observed. Ca was mainly accumulated in plant aboveground parts; Al and Fe were accumulated in the belowground parts; while P was homogenously distributed among the tissues of C. malaccensis. C. malaccensis in D zone had lower Bio-concentration factors (BCFs) of P in the shoots and Al and Fe in the roots, and higher values of Ca in the shoots than those in older zones (P<0.05). Compared to Al and Fe, both Ca and P had relatively higher translocation capacities for C. malaccensis, while only lower TFs for P and higher values for Al and Fe in D zone were observed than those in A and B zones (P<0.05). Except for Al with no significant changes, the total BCFs for P and Fe showed an increasing trend with soil ages, while a decreasing trend for Ca. The total bio-storage factors (TBSFs) of P and Ca declined with the pedogenic time, whereas an increase for Fe. The results of this study can contribute to the wetland conservation and management in the Pearl River estuarine region.  相似文献   

A wetting and drying algorithm with a combined pressure/free-surface formulation for non-hydrostatic models     

S.W. Funke  C.C. Pain  S.C. Kramer  M.D. Piggott 《Advances in water resources》2011,34(11):1483-1495

A wetting and drying method for free-surface problems for the three-dimensional, non-hydrostatic Navier–Stokes equations is proposed. The key idea is to use a horizontally fixed mesh and to apply different boundary conditions on the free-surface in wet and dry zones. In wet areas a combined pressure/free-surface kinematic boundary condition is applied, while in dry areas a positive water level and a no-normal flow boundary condition are enforced. In addition, vertical mesh movement is performed to accurately represent the free-surface motion. Non-physical flow in the remaining thin layer in dry areas is naturally prevented if a Manning–Strickler bottom drag is used. The treatment of the wetting and drying processes applied through the boundary condition yields great flexibility to the discretisation used. Specifically, a fully unstructured mesh with any finite element choice and implicit time discretisation method can be applied. The resulting method is mass conservative, stable and accurate. It is implemented within Fluidity-ICOM [1] and verified against several idealized test cases and a laboratory experiment of the Okushiri tsunami.  相似文献