{"id":71,"date":"2012-03-14T21:43:13","date_gmt":"2012-03-14T17:43:13","guid":{"rendered":"https:\/\/www.zond-geo.co\/english\/?page_id=71"},"modified":"2018-10-28T19:56:03","modified_gmt":"2018-10-28T15:56:03","slug":"zondres2d","status":"publish","type":"page","link":"https:\/\/www.zond-geo.co\/english\/zond-software\/ert-and-ves\/zondres2d\/","title":{"rendered":"ZondRes2d"},"content":{"rendered":"<strong>Zondres2d<\/strong> program is \u00a0 designed for two-dimensional interpretation of <strong>electrical tomography<\/strong>\u00a0data by resistivity and <strong>induced polarization<\/strong> method in land, cross-borehole and water cases.\r\n\r\n<strong>Electrical tomography<\/strong> (<strong>Resistivity imaging<\/strong>) is technique including both the method of field observations and technology of processing and field resistivity and IP data interpretation. Its feature is multiple reusing as a source and receiver just the same electrodes position, fixed on a profile line.\r\n<p style=\"text-align: center;\"><a href=\"https:\/\/www.zond-geo.co\/wp-content\/uploads\/ZondRes2d_8.png\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter wp-image-181\" style=\"width: 540px; height: 406px;\" title=\"Polygonal modeling of geolectrical section in ZondRes2d\" src=\"https:\/\/www.zond-geo.co\/wp-content\/uploads\/ZondRes2d_8.png\" alt=\"Polygonal modeling of geolectrical section in ZondRes2d\" width=\"1068\" height=\"774\" \/><\/a><\/p>\r\nSuch approach allows from one hand to work with a modern high-performance instruments, and on the other hand, to apply effective algorithms of modeling and inversion of <strong>resistivity<\/strong> and <strong>IP<\/strong> data. For interpretation(inversion) of <strong>electrical tomography<\/strong> data is used two- and three-dimensional models. It significantly extends the range of electric prospecting solved problems due to sections investigating that are considerably different from \u00abclassic\u00bb <a href=\"https:\/\/www.zond-geo.co\/english\/zond-software\/ert-and-ves\/zondip1d\/\" target=\"_self\">horizontal-layered<\/a>.\r\n<p style=\"text-align: center;\"><a href=\"https:\/\/www.zond-geo.co\/wp-content\/uploads\/ZondRes2d_3.png\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter wp-image-181\" style=\"width: 540px; height: 406px;\" title=\"Results of resistivity inversion for dipole-dipole array\" src=\"https:\/\/www.zond-geo.co\/wp-content\/uploads\/ZondRes2d_3.png\" alt=\"Results of resistivity inversion for dipole-dipole array\" width=\"1092\" height=\"874\" \/><\/a><\/p>\r\nResolution and thus results quality of <strong>electrical tomography<\/strong> is closely connected with the number and density of measurements on the \u00a0site. Their number usually reaches first thousand that is why the question of field measurements efficiency has basic importance and in many aspects defines possibility of practical using of this method. Special instruments with programmed automatic switching of electrodes is applied for reaching of maximum effectiveness of field works.\r\n<p style=\"text-align: center;\"><a href=\"https:\/\/www.zond-geo.co\/wp-content\/uploads\/ZondRes2d_5.png\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter wp-image-181\" style=\"width: 540px; height: 406px;\" title=\"3D presentation of parallel profile sections in ZondRes2d\" src=\"https:\/\/www.zond-geo.co\/wp-content\/uploads\/ZondRes2d_5.png\" alt=\"3D presentation of parallel profile sections in ZondRes2d\" width=\"1228\" height=\"899\" \/><\/a><\/p>\r\n<strong>ZondRes2d<\/strong> represents ready solution for <strong>resistivity and IP imaging<\/strong>, and solves wide range of problems from mathematical modeling and sensitivity analysis to quality control, \u00a0field data processing and 2D inversion. Convenient interface and variety of data visualization features allow to solve wide range of geological problems with maximum effectiveness.\r\n\r\n<strong>ZondRes2d<\/strong> 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.\r\n\r\nThe software works with any (applied in electroprospecting) types of electrodes arrays (two, three and four \u2013 electrodes) or their combinations. \u00a0It&#8217;s also support most popular formats AGI, ABEM, MAE-instruments, ARES, Zonge, Res2dInv, Syscal, Sens2dInv.\r\n<p style=\"text-align: center;\"><a href=\"https:\/\/www.zond-geo.co\/wp-content\/uploads\/ZondRes2d_2.png\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-large wp-image-181\" style=\"width: 540px; height: 406px;\" title=\"ERT mixed survey earth surface and river bottom\" src=\"https:\/\/www.zond-geo.co\/wp-content\/uploads\/ZondRes2d_2-540x406.png\" alt=\"ERT mixed survey earth surface and river bottom\" width=\"540\" height=\"406\" \/><\/a><\/p>\r\nImportant stage which precede field measurement is <a href=\"https:\/\/www.zond-geo.co\/english\/zond-software\/ert-and-ves\/zondres2dp-program\/\" target=\"_self\">mathematical modeling<\/a> of geoelectric structure of work site. Modeling gives a chance to estimate the level of signal and to make a choice of optimum parameters of the observation system for decision of formulated geological problem. <strong>ZondRes2d<\/strong> has great range of tools for <a href=\"https:\/\/www.youtube.com\/watch?v=L5_pag4_W-s\">mathematical modeling and analysis <\/a>of \u00a0DC\u00a0(direct current) \u00a0and induced polarization fields.\r\n<p style=\"text-align: center;\"><a href=\"https:\/\/www.zond-geo.co\/wp-content\/uploads\/ZondRes2d_4.png\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter wp-image-181\" style=\"width: 540px; height: 406px;\" title=\"Visualization of seismic and resistivity sections together in ZondRes2d\" src=\"https:\/\/www.zond-geo.co\/wp-content\/uploads\/ZondRes2d_4.png\" alt=\"Visualization of seismic and resistivity sections together in ZondRes2d\" width=\"1033\" height=\"827\" \/><\/a><\/p>\r\nAs the general task of the program is inversion of geoelectric parameters, some variants of inverse problem decision are realized in <strong>ZondRes2d<\/strong>, basic of them are: smoothing inversion \u2013 to get smooth model and focusing &#8211; to get \u00a0piece-smoothed model of geoelectric parameters with depth.\r\n\r\nWhile 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\u00a0used. In <strong>ZondRes2d<\/strong> 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 \u00a0in inversion. The robust schemas of noise estimation\u00a0are realized in the software. There is also possibility to import and display results of measurements by other methods and logging \u00a0and\u00a0<a href=\"https:\/\/www.youtube.com\/watch?v=RfxKzr00Pms\">boreholes <\/a>data that improved quality of results.\r\n<p style=\"text-align: center;\"><a href=\"https:\/\/www.zond-geo.co\/wp-content\/uploads\/ZondRes2d_6.png\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter wp-image-181\" style=\"width: 540px; height: 406px;\" title=\"Mathematical modeling in ZondRes2d. Isolines of potential inside the Earth.\" src=\"https:\/\/www.zond-geo.co\/wp-content\/uploads\/ZondRes2d_6.png\" alt=\"Mathematical modeling in ZondRes2d. Isolines of potential inside the Earth.\" width=\"1266\" height=\"801\" \/><\/a><\/p>\r\nBasic features:\r\n<ul>\r\n\t<li>\r\n<ul>\r\n\t<li>Both 32 and 64 bit versions are available.<\/li>\r\n<\/ul>\r\n<\/li>\r\n\t<li>Support any electrodes arrays or combinations with arbitrary system of spacings and electrodes positions. The possibility to work with different (number of electrodes) arrays on the same site.<\/li>\r\n\t<li>Measurements at the water surface and the water bottom. Borehole and cross-borehole systems. Any mixed system.<\/li>\r\n\t<li>Four ways for specifying topography. Real-time editing. Setting of <a href=\"https:\/\/www.youtube.com\/watch?v=KEk31HECTIA\">strike parameter<\/a>.<\/li>\r\n\t<li>Two ways for induced polarization inversion. Standard scheme (static IP) and <a href=\"https:\/\/www.youtube.com\/watch?v=TBPSLyGIGw8\">full waveform IP inversion<\/a> for cole-cole parameters (time and frequency domain). Approximate and full solution. <a href=\"https:\/\/www.youtube.com\/watch?v=bU4eviG3Fzc\">Time-lapse inversion.<\/a><\/li>\r\n\t<li><a href=\"https:\/\/www.youtube.com\/watch?v=4kDf3I-GK7A\">Script recording<\/a> for multi-files processing.<\/li>\r\n\t<li>Special options for <a href=\"https:\/\/www.youtube.com\/watch?v=3XrWxbGzPsg\">large scale<\/a> problem.<\/li>\r\n\t<li>Buffer for 5 models.<\/li>\r\n\t<li>Resistivity and IP data quality control, denoising and editing data module, <a href=\"https:\/\/www.youtube.com\/watch?v=ddH0boEPCPE\">EM removing<\/a>.<\/li>\r\n\t<li>A set of tools for mathematical modeling of geoelectrical section. Standard mesh &#8220;bitmap&#8221; style, arbitrary layered model and polygonal style model. Additional tools for\u00a0gravity, <a href=\"https:\/\/www.youtube.com\/watch?v=x8kdWH6LVJQ\">magnetic <\/a>and <a href=\"https:\/\/www.youtube.com\/watch?v=a2W2akrzsYU\">self potential forward modeling<\/a> and joint inversion.<\/li>\r\n\t<li>Number of the resistivity and IP inversion algorithms : smooth, focusing, robust, block. Setting the reference model for the inversion. Suppressing of the noise component during inversion (robust reweighting).<\/li>\r\n\t<li>Suppression of P \/ C static shifts during inversion. Working with anomalous arrays MAN AMNA (method of true anomalies).<\/li>\r\n\t<li>Setting of limits for models parameters, inserting of a priori geological boundaries and borehole data to inversion. Assignment of weights for datum records. Editor of measurements.<\/li>\r\n\t<li>Estimation of results quality based on sensitivity matrix analysis. Calculation of sensitivity, quality and <a href=\"https:\/\/www.youtube.com\/watch?v=MUo6HPI5fjo\">DOI<\/a> index.<\/li>\r\n\t<li>Cutting of the model edges : by angle or sensitivity level.<\/li>\r\n\t<li>Number of variants for data, model and apriori information visualization. Ability to set a semi <a href=\"https:\/\/www.youtube.com\/watch?v=kdr76GO66WI\">transparent background<\/a> for the resistivity section (geological, seismic sections).<\/li>\r\n\t<li>Three-dimensional visualization of the geoelectric sections along arbitrary system profiles. Maps 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>2D joint inversion with <a href=\"https:\/\/www.youtube.com\/watch?v=1O4Lezy4m1s\">magnetotelluric<\/a>, <a href=\"https:\/\/www.youtube.com\/watch?v=wx8T43jycNM\">refraction seismic<\/a> and <a href=\"https:\/\/www.youtube.com\/watch?v=7q7qjCaZODw\">TDEM<\/a> data.<\/li>\r\n\t<li>Supporting of MMR method<\/li>\r\n\t<li>Exporting to bitmap and vector graphics formats, <a href=\"https:\/\/www.youtube.com\/watch?v=gP_n9yIXwMM\">excel<\/a>, surfer, AUTOCAD. Setting the scale of the exported image. Print images and create reports.<\/li>\r\n<\/ul>\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\/Zondres2d.zip\">download<\/a> \u00a0|\u00a0 Video lesson: <a href=\"https:\/\/www.youtube.com\/watch?v=AchIWUYrPgQ\">download<\/a><\/p>\r\n\r\n<\/div>\r\n<\/div>","protected":false},"excerpt":{"rendered":"<p>Zondres2d program is \u00a0 designed for two-dimensional interpretation of electrical tomography\u00a0data by resistivity and induced polarization method in land, cross-borehole and water cases. Electrical tomography (Resistivity imaging) is technique including both the method of field observations and technology of processing and field resistivity and IP data interpretation. Its feature is multiple reusing as a source [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":18,"menu_order":1,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":"","_links_to":"","_links_to_target":""},"class_list":["post-71","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/pages\/71","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\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/comments?post=71"}],"version-history":[{"count":51,"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/pages\/71\/revisions"}],"predecessor-version":[{"id":2031,"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/pages\/71\/revisions\/2031"}],"up":[{"embeddable":true,"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/pages\/18"}],"wp:attachment":[{"href":"https:\/\/www.zond-geo.co\/english\/wp-json\/wp\/v2\/media?parent=71"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}