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491.
Evaluation of the reservoir permeability of anthracite coals by geophysical logging data 总被引:1,自引:0,他引:1
Junqian LiDameng Liu Yanbin YaoYidong Cai Yongkai Qiu 《International Journal of Coal Geology》2011,87(2):121-127
Permeability is one of the most significant reservoir parameters. It is commonly obtained by experiment, history simulation, injection/falloff well test and geophysical logging. Among these, geophysical logging remains as the most economic and efficient technique in evaluating coal permeability in the vicinity of an open-hole. In this paper, geophysical logging data are used to evaluate the coal reservoir permeability for the No. 3 coal seam in the southern Qinshui Basin (Fanzhuang and Zhengzhuang coal zones). Ideally coal reservoirs consist of coal matrix and fracture networks that can be represented by a model called a collection of sheets. Based on the model, coal reservoir permeability can be quantitatively calculated using the theoretical formula of kf = 8.50 × 10− 4 w2φf, in which fracture width (w) and fracture porosity (φf) were obtained by dual laterolog and density logging data, respectively. Calculative results show that coal reservoir permeability ranged from 0.017 mD to 0.617 mD for the Fanzhuang coal zone and from 0.047 mD to 1.337 mD for the Zhengzhuang coal zone. The permeability decreases with coal burial depth, reflecting variations in penetration capability of coal reservoirs at varying depths. Comparing results with those from injection/falloff well tests, however, shows that the model-calculated permeability is slightly higher. This is expected because the model did not include the influence from coal anisotropy. 相似文献
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几年以前 ,我国尚未独立开展过海洋电磁探测 ,没有获取海洋岩石层电性资料的技术手段。然而 ,地下岩层的电性参数较之其他物性参数能更好地反映岩石的性质以及岩石所处的物理状态 ,因此迫切需要发展海底大地电磁探测技术。海底大地电磁探测是把仪器布置在海底 ,采集海底大地电磁场数据 ,从而研究海底以下不同深度上介质导电性的分布规律 ,达到了解地下不同深度地质情况的目的。经过两年的努力 ,我们已基本实现了海底大地电磁探测技术的研究目标 相似文献
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Two-dimensional (2-D) resistivity and ground penetrating radar (GPR) surveys facilitate tracing of buried archaeological relics at the archaeological site of the Tell El Rabi'a, southwestern Cairo. These surveys also provide information on variations in depth of the groundwater table, which affect both exhumed and buried archaeological remains. The 2-D electrical resistivity profiles obtained show some high anomalies (up to 6900 Ω m). Based upon on-site calibration at partly exhumed sites, such anomalies are interpreted as pillar crowns and wall-like structures of hard limestone of the Hathour temple. The low background resistivities are interpreted to represent riverine deposits with differing moisture (or saturation) characteristics. The results of the GPR survey show three forms of high-amplitude radar anomalies, denoted as “P, H and R”. The “P” anomalies have semi-hyperbolic shapes, which suggest the presence of thin buried walls. The second, near-horizontal group of anomalies, “H”, may be either due to the presence of thick buried walls or arise from coincidental parallel alignment of survey lines with buried linear structures. The third group of GPR anomalies “R” is composed of chaotic reflections, and interpreted to depict buried stone-filled chambers. Some un-exhumed parts of the study area show weak radar reflections with occasional highly attenuated radar signals. These phenomena are ascribed to differing compaction and moisture characteristics of riverine soil layers. Recommendations with regard to archaeological site-excavation, preservation of archaeological relics, and soil conservation are submitted. 相似文献
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目前地电的方法在我国已应用到地震预报的研究中,为了了解与地下力学场变化相联系的地电变化,需要了解台址下勘探体积内的电阻率分层情况,从而正确地认识各种影响因素对地电阻率的作用。 相似文献
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对采自内蒙东胜、河北张家口、山西离石和湖北通城、秭归等不同自然地理环境区的92个土壤样,分别进行了其各项物理、化学特性的测定,和崩解、溅蚀、贯入试验,发现不同土类的试验结果与其理化性状之间存在规律性,它们是土壤抗蚀性的反映。文中还对不同土壤的抗蚀性大小进行了讨论。 相似文献
500.
用物探方法解决文物保护和考古中的某些难题 总被引:5,自引:0,他引:5
文中介绍了3个实例:(1)测量石雕表面风化深度和防风化液渗入深度;(2)勘查中国现存最古的砖塔--嵩岳寺塔的塔基状况,并查明是否有地宫;(3)在克孜尔千佛洞地区崩坍的堆积层表面查找地下旁侧的山崖中是否有被埋石窟.以上3例在以往用常规方法都难有成效,针对具体情况,灵活地应用电阻率法及地质雷达等方法,解决了考古中的难题. 相似文献