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ZondHED1d培训 |
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班级人数--热线:4008699035 手机:15921673576( 微信同号) |
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保障培训效果,坚持小班授课,每个班级的人数限3到5人,超过限定人数,安排到下一期进行学习。 |
授课地点及时间 |
上课地点:【上海】:同济大学(沪西)/新城金郡商务楼(11号线白银路站) 【深圳分部】:电影大厦(地铁一号线大剧院站)/深圳大学成教院 【北京分部】:北京中山学院/福鑫大楼 【南京分部】:金港大厦(和燕路) 【武汉分部】:佳源大厦(高新二路) 【成都分部】:领馆区1号(中和大道) 【广州分部】:广粮大厦 【西安分部】:协同大厦 【沈阳分部】:沈阳理工大学/六宅臻品 【郑州分部】:郑州大学/锦华大厦 【石家庄分部】:河北科技大学/瑞景大厦
开班时间(连续班/晚班/周末班):2020年3月16日 |
课时 |
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质量以及保障 |
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1、如有部分内容理解不透或消化不好,可免费在以后培训班中重听;
☆ 2、在课程结束之后,授课老师会留给学员手机和E-mail,免费提供半年的课程技术支持,以便保证培训后的继续消化;
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☆4、合格学员免费颁发相关工程师等资格证书,提升您的职业资质。 |
☆课程大纲☆ |
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- ZondSP2d 是地球物探分析软件Zond的模块之一,是一款专业的二维自然电位法软件。
- ZondSP2d program is desined for two-dimensional interpretation of self-potential data by (land and borehole variants).
- Self-potential field method is based on studying of the natural electric fields that generate in rocks because of various physical and chemical processes. Small self potentials of diffuse-adsorbtsion and filtering nature exist practically everywhere. Intensive fields of redox nature are observed only over sulphide and graphit deposits. As a rule electronic conductors located in the ionic media are the search objects of self-potential field method. Electric charges as sources of natural electric field are formed on the boundaries of such objects.
- Each cell of model has next ptoperties: resistivity , type conductivity (electronic or ionic). On cells borders with differ types of conductivity sources of the natural field are formed (functional relation of the source intensity vs depth that characterizes spatial distribution of redox factors is used).
- ZondSP2d represents ready solution for self-potential method, and solves wide range of problems from mathematical modeling to field data interpretation. Convenient interface and variety of data visualization features allow to solve wide range of geological problems with maximum effectiveness.
- ZondSP2d uses simple and clear data format which allows easily combining various systems of observation, including different variants of the topography setting up and other additional information.
- Important stage which prevents field measurement is mathematical modeling of petrophysical structure of work site. Modeling gives a chance to make a choice of optimum parameters of the observation system for decision of formulated geological problem.
- As the general task of the program is inversion of resistivity and charges, some variants of inverse problem decision are realized in ZondSP2d, basic of them are: smoothing inversion – to get smooth model and focusing — to get piece-smoothed model of petrophysical parameters with depth.
- While program was designed special consideration given to a priori data accounting. Because of equivalence of inverse geophysical problems, quality of the obtained results strongly depends on the amount of a priori data used. In ZonSP2d there is possibility of weights setting for measurements, fixing and limits making of changing features of different cells, using of a priori model as reference in inversion. There is also possibility to import and display results of measurements by other methods and cross-boreholes data that improved quality of results.
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