{"id":251,"date":"2012-03-28T17:45:01","date_gmt":"2012-03-28T13:45:01","guid":{"rendered":"https:\/\/www.zond-geo.co\/english\/?page_id=251"},"modified":"2020-08-03T13:44:54","modified_gmt":"2020-08-03T09:44:54","slug":"zondsp2d","status":"publish","type":"page","link":"https:\/\/www.zond-geo.co\/english\/zond-software\/gravity-magnetic-self-potential\/zondsp2d\/","title":{"rendered":"ZondSP2D"},"content":{"rendered":"<strong>ZondSP2D<\/strong>\u00a0software is designed \u00a0for two-dimensional interpretation of self-potential data. Software supports different types of sources for can be used for interpretation of different types of self-potential data.\r\n<div><\/div>\r\nSelf-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-adsorption and filtering nature exist practically everywhere. Intensive fields of redox nature are observed only over sulphide and graphite 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.\r\n<div><\/div>\r\n<a href=\"https:\/\/www.zond-geo.co\/english\/sppic1\/\" rel=\"attachment wp-att-4846\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-4846\" src=\"https:\/\/www.zond-geo.co\/english\/files\/2020\/08\/sppic1.png\" alt=\"sppic1\" width=\"540\" height=\"338\" \/><\/a>\r\n\r\n<strong>ZondSP2D<\/strong>\u00a0represents ready solution for self-potential method, and solves wide range of problems from mathematical<a href=\"https:\/\/www.zond-geo.co\/english\/zond-software\/gravity-magnetic-self-potential\/zondsp2dp\/\">\u00a0modeling<\/a>\u00a0\u00a0to field data \u00a0interpretation. Convenient interface and variety of data visualization features allow to solve wide range of geological problems with maximum effectiveness.\r\n<div><\/div>\r\n<strong>ZondSP2D\u00a0<\/strong>uses simple and clear data format which allows easily combining various arrays and topography information. Software fully integrated with <strong>ZondRes2d<\/strong> software, so importing of resistivity background model is very easy.\r\n<div><\/div>\r\nTo each object of model \u00a0resistivity and sources can be assigned. Types of sources different and\u00a0 depends on considering problem. It can be border redox-oxygen nature sources or volumetric sources (poles or oriented dipoles). For redox-oxygen case very convenient functional is used to set source intensity vs depth. Area of volumetric sources presence can be limited by user defined polygons.\r\n<div><\/div>\r\nAs the general task of the program is inversion of source currents, some approaches of inverse problem are used in <strong>ZondSP2D<\/strong>, basic of them are: <em>probability inversion<\/em> \u2013 helps to get more stable source\u00a0 distribution, <em>occam inversion<\/em> \u2013 can be tuned in different way to get alternative results for different settings and <em>parametric inversion<\/em> for small number of parameters problem.\r\n\r\n<a href=\"https:\/\/www.zond-geo.co\/english\/sppic2\/\" rel=\"attachment wp-att-4847\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-4847\" src=\"https:\/\/www.zond-geo.co\/english\/files\/2020\/08\/sppic2.png\" alt=\"sppic2\" width=\"540\" height=\"338\" \/><\/a>\r\n\r\n<em>Basic features:<\/em>\r\n<ul>\r\n\t<li>Linear source has been used in software for calculation of forward problem*.<\/li>\r\n\t<li>Types of current sources: border redox-oxygen; volumetric: poles, horizontal dipoles, vertical dipoles, vectors.<\/li>\r\n\t<li>Supports any electrodes arrays or combinations with arbitrary receiving lines (potential and gradient array).<\/li>\r\n\t<li>Simplest text data format or possibility of importing data from arbitrary column-based text\/excel file.<\/li>\r\n\t<li>Very easy to incorporate topography to model.<\/li>\r\n\t<li>Full integration with <strong>ZondRes2D<\/strong> software helps to import background resistivity model quickly.<\/li>\r\n\t<li>Resistivity model takes from polygons or background model.<\/li>\r\n\t<li>A set of tools for mathematical modeling based on polygonal GUI.<\/li>\r\n\t<li>Buffer for 5 models.<\/li>\r\n\t<li>Inversion algorithms : probability , occam, robust and parametric.<\/li>\r\n\t<li>Number of variants for data, model and a priori information visualization. Ability to set a semitransparent background for the resistivity section (geological, seismic sections).<\/li>\r\n\t<li>Three-dimensional visualization of results sections along arbitrary system profiles. Map of slices of parameters for various depths.<\/li>\r\n\t<li>Geological sections editor and borehole columns editor. Titled boreholes.<\/li>\r\n\t<li>Exporting to bitmap and vector graphics formats, excel, surfer, AUTOCAD. Setting the scale of the exported image. Print images and create reports.<\/li>\r\n<\/ul>\r\n<a href=\"https:\/\/www.zond-geo.co\/english\/sppic3\/\" rel=\"attachment wp-att-4848\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-4848\" src=\"https:\/\/www.zond-geo.co\/english\/files\/2020\/08\/sppic3.png\" alt=\"sppic3\" width=\"540\" height=\"338\" \/><\/a>\r\n\r\n* Explanation: why linear type of source was used in the software. Linear source gives much better fitting, even size of object along strike direction (length of source line in the figure)\u00a0 ~ 0.3-0.5 of distance to source.\r\n<div class=\"finfo\">\r\n<div class=\"finfo-in\">\r\n<p align=\"center\">Version 13 \/ 12 \/ 2023\u00a0|\u00a0 Software: <a href=\"https:\/\/www.zond-geo.co\/zfiles\/Zondsp2d.zip\">download<\/a><\/p>\r\n\r\n<\/div>\r\n<\/div>","protected":false},"excerpt":{"rendered":"<p>ZondSP2D\u00a0software is designed \u00a0for two-dimensional interpretation of self-potential data. Software supports different types of sources for can be used for interpretation of different types of self-potential data. 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-adsorption and [&hellip;]<\/p>\n","protected":false},"author":2,"featured_media":0,"parent":36,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":"","_links_to":"","_links_to_target":""},"class_list":["post-251","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/pages\/251","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/comments?post=251"}],"version-history":[{"count":16,"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/pages\/251\/revisions"}],"predecessor-version":[{"id":4853,"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/pages\/251\/revisions\/4853"}],"up":[{"embeddable":true,"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/pages\/36"}],"wp:attachment":[{"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/media?parent=251"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}