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通过对大地电磁测深法在西部勘探中优势的分析,结合其地球物理原理,指出建立区域电性模型对MT资料预处理、反演、解释等工作的重要性。结合阿什里地区概况,提出MT首支电阻率统计法、测井电阻率和区域综合资料电性统计等方法来建立区域电性模型。 相似文献
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本文在研究岩芯分析的基础上,描述了文东地区低电阻率油层的岩性、物性、含有性、及电性特征,综合分析了低电阻率油层的成因机理,为找到识别低电阻率油层的有效方法,发现更多的低电阻率油藏,提高油田的储量和产量,具有重要的意义。 相似文献
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岩石电性参数(电阻率、介电常数等)频散是岩石介质的重要特征之一,利用岩石电阻率频散特性发展起来的测井——双频电阻率测井方法,有望改善和提高陆相沉积地层油气评价的质量和能力。应用电性参数的频散特性进行地层评价是目前定义的双频电阻率测井的主要特点。本文从电阻率测井基本原理出发,介绍了双频电阻率测井的理论依据及测井原理,仪器性能指标及适用范围,通过在胜利及中原油田部分井上的测井解释实施,取得了较好效果,证明了双频电阻率电阻率测井方法有效性,特别是在低水淹层的解释上与油藏动态生产特征符合率较高,该项测井技术有着良好的应用前景。 相似文献
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There has been no an effective method to measure resistivity of mineral powder and other powder materials until now. According to the national standards GB/T1410-2006, the method to measure resistivity of mineral powder and other powder materials was studied by using the digital high resistance meter and a small measurement electrode which is adequate for the measurement of flat specimen whose diameter is 18 mm. A formula to calculate resistivity of mineral powder by the testing data of its powder compacts was derived according to the compacts characteristics and the generalized effective medium equation (GEM). Then, taking micro-crystal muscovite for example, the experimental results proves that the measurement method is effective and feasible because the resistivity data of mineral powders are the same as that of their dense blocky samples. Further experimental results show that the volume resistivity and surface resistivity of mineral powder are not influenced by mineral particle size. And the upper and lower faces of powder compacts do not affect the volume resistivity of mineral powder, but affect the surface resistivity obviously. So, it is necessary to characterize the surface resistivity of mineral powder by the testing data of the upper face (punch face) of powder compacts. Moreover, the resistivity of mineral powder is greatly influenced by both the drying time and standing time in air. Therefore, in order to obtain correct result, the samples should be dried to constant weight before testing, isolated from air during cooling and measured immediately when exposed to air, and the testing time should be as short as possible. 相似文献
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黏土矿物(clay minerals)是组成黏土岩和土壤的主要矿物,它是一种含镁、铝为主的水合硅酸盐矿物.研究发现黏土矿物液晶与有机液晶材料相比,具有光、电、磁性能强,热稳定性好,价格低廉等优点.简要介绍了黏土矿物液晶材料的形成机理,概述了片层状黏土液晶材料、纤维型黏土液晶材料、类黏土矿物液晶材料的制备方法和研究现状,同时介绍了不同条件(浓度、离子强度、外电场作用、分散介质、重力作用)对黏土及类黏土分散体系相变的影响,并对黏土矿物液晶材料的应用发展前景进行了概述. 相似文献
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David U. Nannen Antje Herrmann Ralf Loges Klaus Dittert Friedhelm Taube 《Nutrient Cycling in Agroecosystems》2011,89(2):269-280
The stable isotope technique and the difference method are common approaches for estimating fertiliser N uptake efficiency.
Both methods, however, have limitations and their suitability may depend on N management and environmental conditions. A field
experiment was conducted on a humus sandy soil in northern Germany to estimate fertiliser N uptake efficiency of silage maize
in the year of application (Zea mays L.) by the stable isotope and the difference method as influenced by the type of N fertiliser (mineral vs. cattle slurry),
the application mode (separate or combined application), and N rate. Seven N treatments were included (0, 50, 100 and 150 kg
mineral N ha−1; 20, 40 m3 cattle slurry ha−1; 50 kg mineral N ha−1 plus 40 m3 slurry ha−1), where either mineral N or slurry N was labelled, and mineral N was split into two dressings. In addition, 4.1 kg ha−1 labelled mineral N was incorporated into otherwise unlabelled treatments (0, 20, 40 m3 ha−1, and 50 kg mineral N ha−1 plus 40 m3 ha−1) to estimate N uptake from the upper soil layer. Uptake of 15N was followed in leaves, stalk, ear, and the whole crop. Fertiliser N uptake efficiency (FNUE15N) of mineral fertiliser N obtained by the isotope technique ranged between 51 and 61%. Recovered fertiliser N was mainly found
in the ear, while less labelled N remained in leaves and the stalk. The nitrogen rate tended to increase the amount of recovered
N, but the effect was not consistent among plant parts and the whole crop. Plant N uptake from non-fertiliser N was found
to increase N input up to 100 kg N ha−1. Nitrogen recoveries of the two mineral N dressings were similar for the different plant parts as well as for the whole crop.
Fertiliser N uptake efficiency (FNUEdiff) of mineral N estimated by the difference method resulted in substantially higher values compared to FNUE15N, varying between 56 and 98%. More N was taken up from the upper soil layer with increasing N supply, which is regarded as
a major error source of the difference method. Slurry N was taken up less efficient in the year of application than mineral
fertiliser N as indicated by recovery rates of 21–22% (FNUE15N) and 39–62% (FNUEdiff), respectively. When mineral N and slurry were applied together, the difference method estimated significantly lower N uptake
efficiencies for both mineral and slurry N compared to a single application, while values obtained by the isotope method were
not affected. 相似文献
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