1)induced polarization method激发极化法
1.The application of induced polarization method in Dajia gold deposit;激发极化法在大架金矿床中的应用效果
2.Groundwater detection in metamorphic rock of Taishan group with applying induced polarization method;激发极化法探测泰山群变质岩地下水
3.Application of the induced polarization method to detecting the watershed in the mined out area;用激发极化法探测煤层采空区积水
英文短句/例句
1.This method is known as time-domain IP.这种方法称为时间域激发极化法。
2.Application of Induced Polarization Method in Yingshan Deposits Exploration激发极化法在银山矿区找矿中的应用
3.The Software System about Two-dimension Forward of Dc Resistivity and Induced Polarization;直流电阻率法和激发极化法二维正演软件系统
4.The Math Model Serching for Fire Source by Parallactic Polarizability of Homogeneous Medium;单一介质热源激发极化法探测的数学模型
5.Application of induced polarization method to Liushengdian Mo deposit of Antu,Jilin激发极化法在吉林安图刘生店钼矿的应用
6.SO, according to the principle of the induced polarization method, it is only suitable for prospecting metallic minerals.这样说来，激发极化法的原理决定了它只适于金属矿物的勘查。
7.Application of the IP Method to the Exploration of a Pb-Zn Ore Deposit in Western Yunnan激发极化法在滇西某铅锌多金属矿勘查中的应用
8.THE APPARENT RESISTIVITY PARAMETERS IN DIRECT CURRENT IP METHOD AND THE SECONDARY ELECTRIC FIELD SAMPLING直流激发极化法中的视电阻率参数及二次场采样
9.I am going to introduce to you the induced polarization method because it is the most popular ground geophysical method used in mineral exploration.我给你谈一谈激发极化法，在矿床勘查巾，这种方法是最为常用的一种地表地球物理勘探方法。
10.The Attempt of Detecting Underground Multi-storey Coal Bed Fire Area Position and Limit by Radon Measure Technique and Induced Polarization Method;用测氡技术和激发极化法探测地下多层煤层火区位置和范围的尝试
11.Electrochemiluminescence Determination of Kinetin with Carbon Nanotube/Nafion-Ru(bpy)_3~(2+) Modified Electrode碳纳米管/Nafion-吡啶钌修饰电极电化学发光法测定激动素
12.Experimental Study on Induced Polarization Potential of Rock Frequency Domain岩样频率域激发极化电位的实验研究
13.multi-emitter laser diode多发射极激光二极管
14.The properties of internal excited state of optical polaron are studied by using the linear combination operator and the unitary transformations methods.采用线性组合算符和么正变换相结合的方法,讨论了光学极化子内部激发态的性质.
15.The Research on Some Key Technologies and Theory of Frequency Domain IP Decoupling by Chop-wave;频率域激发极化斩波去耦关键技术与理论研究
16.Experiment Research and Theoretical Analysis on Rock Induced Polarization Phenomenon;岩石激发极化现象的实验研究及理论分析
17.THE NUMERICAL ANALYSIS ON THE RESPONSE OF INDUCED POLARIZATION RELAXATION TIME SPECTRA WELL LOGGING激发极化弛豫时间谱测井仪探测特性理论分析
18.THE APPLICATION OF INDUCED POLARIZATION METHOD TO THE PROGNOSIS OF DABAOSHAN BLIND CU DEPOSIT,WEIXI激电极化法在维西大宝山隐伏铜矿预测中应用
相关短句/例句
Induced polarization激发极化法
1.Effectiveness of natural field induced polarization for detecting poly-metallic deposits;天然场激发极化法在多金属矿区的野外试验效果
2.The application of induced polarization method tothe steadiness research on Liufang dyke in Huainan city;激发极化法在淮南六方堤稳性检测中的应用
3.The induced polarization(IP) method is a good choice in prospecting the metal deposits with low electrical resistivity and high polarization resistance.本文论述了激发极化法在塞钦铜多金属矿勘查找矿中的应用。
3)IP method激发极化法
1.The IP method based on the difference in the polarizability and resistivity of rocks has played an important role in the exploration of concealed and deep ore bodies.结合激发极化法在冀北某铜钼矿勘查中的应用实例,说明在硫化物矿床的勘查中,利用中间梯度装置扫面可以快速地发现并圈定激电异常,利用激电测深可以了解极化体的埋藏深度及空间赋存状态,进而为指导工程验证提供较为充足的依据。
2.A mass of numerical simulations for resistivity and IP method.本文首先回顾了电法勘探地形影响问题的研究现状，总结了现有激发极化法的数值模拟方法，简单介绍了ANSYS有限元软件的主要功能，在进行激发极化法数值模拟过程中的主要步骤及其注意的关键问题。
4)IP charge method充电激发极化法
1.IP charge method is one of the main means of mine geophysical methods with both characteristics of charge and IP method which can be used in the existing projects to maximize the understanding of the underground three dimensional geophysical field and solve geological problem.充电激发极化法是矿山物探的一种主要方法,其兼有充电法与激发极化法的特点,可利用已有的工程,最大限度地了解地下三度空间地球物理场的分布情况,解决地质问题。
5)time domain induced polarization (IP)时域激发极化法
6)phase-IP相位激发极化法
延伸阅读
激发极化法激发极化法induced polarization method J ifa Jihua fa 激发极化法(indueed polariza- tion method)观测、研究被探测 对象在外电场激励下产生的次生极化电 场的变化规律的工程电法勘探方法。断 电瞬间观测到的次生极化电场称为二次 场(△v:，mV)。它的强弱和衰减快慢，除 与充电时间、充电电流和装置类型有关 外，主要与被探测对象的岩性、状态、含 水量和含泥量等因素有关。因此，只要使 充电时间、充电电流和装置类型保持不 变，选择合适的与二次场有关的参数(如 极化率、衰减时、激发比和衰减度等)，研 究这些参数的变化规律即可达到划分岩 性，寻找岩溶、断层破碎带和其他含水构 造的目的。此法的常用观测装置是肘N/AB~1/3的温奈尔装置，可用它做激发极化剖面，也可用它做激发极化测深。图示为激发极化法工作原理示意图。观测方法有断电瞬间观测法和变频法。根据所测得参数的相对变化来推断被探测目标的性质、状态、分布范围等。资料解释以定性解释为主，定量解释方法有待进一步研究。 川厂月 任网l{l 盆l价lee?se十、 死电时[eJ断放电时同 口电造止 b 激发极化法工作原理示意图 a一充放电曲线;b一测量装置 A、B一供电电极;M、N一测量电极;Vl一供电电位差; VZ一极化(二次场)电位差 在工程勘察中，激发极化法观测研究的次生极化场是由离子导体激发极化效应产生的，而由电子导体激发极化效应产生的次生极化场是干扰场。离子导体激发极化效应的机制有电偶层变形、薄膜极化等假说，这些假说尚不能圆满地解决离子导体激发极化效应的机制问题。此方法还不能统一给出反映次生极化场本质的参数，使用的仪器不同，观测、研究的参数也就不同。各国应用激发极化法找水取得了不同程度的效果，特别是在中国北方一些缺水地区收到了良好的地质效果。但该方法的理论、观测技术、解释方法和仪器设备都需要进一步完善和改进。 激发极化法使用的仪器设备是各种型号的激发极化仪。 (范昌隆)
