随钻判断煤层气方法探讨   总被引：1，自引：0，他引：1  

方锡贤 《中国煤田地质》2004,16(5):16-20,38

结合石油录井技术，阐述了利用岩性组合特征及气测异常预测煤层位置、利用工程参数卡准煤层位置的技术方法。在此基础上探讨了运用常规技术进行地质导向方法和现场计算煤层气量方法。文中还介绍了现场钻遇煤岩的基本特征和现场判断煤层气气层厚度的方法。  相似文献   

降低黄河中下游平原成井含砂量的几种方法   总被引：1，自引：0，他引：1  

苗长军  张方亮 《地下水》2004,26(2):127-128

在砂土含水层取水如何降低成井含砂量。采用的方法有增大滤料厚度，充分滤去水中颗粒；滤料采用颗粒级配适当的优质石英砂；采用新型T形丝滤水管等。  相似文献   

宿州市地下水含铁量高浅析   总被引：1，自引：0，他引：1  

李磊  秦福刚  陈敏虹 《地下水》2004,26(4):260-261

宿州市地下水中铁的含量在1.12～8.50 mg/l之间,超过<生活饮用水标准>(GB5749-85)(＜0.3mg/L)的4～28倍,本文根据含水层的沉积特征、铁的水文地球化学特性,通过采样分析了地下水含铁量高的原因,并提出了相应的解决方法.  相似文献   

Characteristics of frequency content of near-fault ground motions during the Chi-Chi earthquake     

徐龙军  谢礼立 《地震学报(英文版)》2005,18(6):707-716

Introduction The dynamic response of structural systems subjected to earthquake ground shaking is sig-nificantly affected by the frequency content of input ground motions. When the frequency content of a predominant earthquake ground motion closely matches the natural period of a structural sys-tem, the dynamic response is significantly enhanced and thus may cause severe damage (Chopra, 1995). Therefore, it is of great importance to evaluate the frequency content of ground motions. In recent …  相似文献   

Analysis of the distribution coefficients and mobility characteristics of phenols in different soil types     

Zareen Khan  Y. Anjaneyulu 《Environmental Geology》2005,48(1):1-5

Adsorption studies were carried out on soil samples of high organic and low organic content to analyze the distribution coefficient and mobility of phenols. The results show that the amount of phenols adsorbed by the soil varies linearly with the fraction of organic carbon. Soils that are highly organic compared to those with low organic matter content retain the phenols to a greater extent. Adsorption studies on the different soil types indicated that the extent of adsorption of phenols by different kinds of soils is important, as a smaller amount of adsorption by the soil increases the risk of contamination of the groundwater supply.  相似文献   

Numerical Simulation of Moisture Movement in Unsaturated Expansive Soil Slope Suffering Permeation     

Chen Shanxiong* School of Civil Engineering  Mechanics  Huazhong University of Science  Technology  Wuhan  China  Institute of Rock  Soil Mechanics  Chinese Academy of Sciences  Wuhan  China Yu Song Liu Zhiguo Xu Haibin Institute of Rock  Soil Mechanics  Chinese Academy of Sciences  Wuhan  China 《中国地质大学学报(英文版)》2005,16(4)

INTRODUCTION Theinfiltrationandevaporationofwaterinasoil slopeareofparamountimportanceindetermining slopestability.Previousengineeringcasesandstud ieshaveshownthatrainwaterisoftenamajorfactor intheslopefailureofexpansivesoils.Expansivesoils intropicalandsubtropicalzonesareoftenunsaturat ed,andsoilslopesareinastablestateinnormalcli mateconditionsbecauseofthehighsuctionandshear strengthofthesoilmass.However,oncepermeation happensrainwaterwillinfiltrateintothesoilmasswhichleadstoanincreasein…  相似文献   

江汉平原江陵剖面有机碳含量、碳同位素和磁化率的古气候意义   总被引：5，自引：2，他引：5  

王秋良  袁胜元  李长安 《地质科技情报》2006,25(4):59-62

湖泊中的有机碳及其同位素与磁化率指标广泛应用于古气候的重建,但由于各地自然条件的差异,其气候意义具有一定的区域性.对江汉平原江陵剖面沉积物中磁化率参数、总有机碳(TOC)、总氮(TN)及其碳同位素δ(13C)值影响因素与环境气候关系的研究结果表明:沉积物总有机碳(TOC)的变化与总氮(TN)呈正相关关系,而总有机碳(TOC)与同位素δ(13C)、磁化率值则呈负相关关系,其组合可以很好地反映江汉平原地区的环境演变.在暖湿期,沉积物中总有机碳、总氮较高,有机质的δ(13C)值偏负,磁化率偏低;反之,在凉干期,沉积物中总有机碳、总氮较低,有机质的δ(13C)值偏正,磁化率偏高.江汉平原地区6 000 a PB以来的古气候演化经历了3个阶段:即冷干-暖湿-凉干的变化过程.  相似文献   

非饱和黄土渗透性的试验研究   总被引：2，自引：0，他引：2  

梁燕  谢永利  刘保健  于友成 《水文地质工程地质》2006,33(2):27-30

通过对甘肃陇西地区的湿陷性黄土做现场浸水试验和室内渗透试验、粒度分析试验，得到了陇西黄土的渗透系数（K20）随孔隙比（e）和吸力（s）的变化规律，为研究黄土浸水入渗规律，求解湿陷性黄土非稳态渗流方程做了必要的准备。  相似文献   

Calculated and measured values of liquid water content in clean and polluted environments     

J. Fišák  D. Řezáčová  J. Mattanen 《Studia Geophysica et Geodaetica》2006,50(1):121-130

The relationship between liquid water content (LWC) and visibility (VIS) in a fog was examined by a field measurement of LWC values at a clean location of the meteorological observatory Sodankylä (Finland) and in a polluted region at the meteorological observatory Mile?ovka (Czech Republic). Furthermore, the use of a simple regression fog model to determine LWC from VIS is examined by comparing well-known relationships with the measurement results. The results show that the verbal characterization of environment (clean, mild polluted, polluted) is insufficient to calculate the LWC values from visibility. It is necessary to establish an additional criterion based on quantitative fog characteristics or to determine the site-related equation from the previous LWC and VIS measurement.  相似文献   

Effect of loading rate on the volume change behavior of unsaturated residual soil     

Bujang B. K. Huat  Faisal Hj. Ali  F. H. Choong 《Geotechnical and Geological Engineering》2006,24(6):1527-1544

Residual soils occur in most countries of the world but those that occur in greater area and depth are usually found in the tropical humid areas. This research examines the effects of loading rate of applied or net mean stress on the volume change behavior of an unsaturated granitic residual soil. Three loading rates were adopted: fast, slow and extra slow loading rate. It was observed that the loading rate of applied or net mean stress has a pronounced effect on the void ratio and degree of saturation but has an insignificant effect on the water content of residual soils subjected to constant matric suction.  相似文献