{"id":100,"date":"2022-07-14T00:09:37","date_gmt":"2022-07-14T00:09:37","guid":{"rendered":"https:\/\/books.gw-project.org\/electrical-imaging-for-hydrogeology\/chapter\/solution-exercise-6\/"},"modified":"2023-03-11T17:27:09","modified_gmt":"2023-03-11T17:27:09","slug":"solution-exercise-6","status":"publish","type":"chapter","link":"https:\/\/books.gw-project.org\/electrical-imaging-for-hydrogeology\/chapter\/solution-exercise-6\/","title":{"raw":"Solution Exercise 6","rendered":"Solution Exercise 6"},"content":{"raw":"<div class=\"solution-exercise-6\">\r\n<p class=\"import-Normal\">Current injected [<em class=\"import-GWPCambria\">I<\/em>]:\u00a02\u00a0mA<\/p>\r\n<p class=\"import-Normal\">Apparent resistivity [<em class=\"import-GWPCambria\">\u03c1<\/em>]:\u00a0250\u00a0ohm-m<\/p>\r\n<p class=\"import-Normal\">Noise level:\u00a015\u00a0mV<\/p>\r\n<p style=\"text-align: center;\">[latex]\\displaystyle K_{g}=\\frac{2\\pi }{\\frac{1}{\\overline{AM}}-\\frac{1}{\\overline{AN}}-\\frac{1}{\\overline{BM}}+\\frac{1}{\\overline{BN}}}[\/latex]<\/p>\r\n<p style=\"text-align: center;\">[latex]\\displaystyle K_{g,Wenner}=\\frac{2\\pi }{\\frac{1}{5\\mathrm{m}}-\\frac{1}{10\\mathrm{m}}-\\frac{1}{10\\mathrm{m}}+\\frac{1}{5\\mathrm{m}}}[\/latex]<\/p>\r\n<p class=\"import-Normal\" style=\"text-align: center;\">=<em class=\"import-GWPCambria\">\u00a0<\/em>31.4\u00a0m<\/p>\r\n<p class=\"import-Normal\">For a positive geometric factor with a dipole-dipole array, you need to have the electrodes configured as <em class=\"import-GWPCambria\">A B N M<\/em> (this also gives a positive resistance). If you configure the electrodes as <em class=\"import-GWPCambria\">A B M N<\/em> (as often written) the geometric factor is negative (so is the resistance). Using <em class=\"import-GWPCambria\">A B N M<\/em> the geometric factor is:<\/p>\r\n<p style=\"text-align: center;\">[latex]\\displaystyle K_{g,dipole-dipole}=\\frac{2\\pi }{\\frac{1}{\\overline{AM}}-\\frac{1}{\\overline{AN}}-\\frac{1}{\\overline{BM}}+\\frac{1}{\\overline{BN}}}[\/latex] = [latex]\\displaystyle \\frac{2\\pi }{\\frac{1}{9\\mathrm{m}}-\\frac{1}{6\\mathrm{m}}-\\frac{1}{6\\mathrm{m}}+\\frac{1}{3\\mathrm{m}}}[\/latex] = 56.5 m<\/p>\r\n<p class=\"import-Normal\">If you do the calculation as <em class=\"import-GWPCambria\">A B M N<\/em>, you get a geometric factor of -56.5.<\/p>\r\n<p class=\"import-Normal\">We then need to calculate the apparent resistivity:<\/p>\r\n<p class=\"import-Normal\"><em class=\"import-GWPCambria\">\u03c1<\/em><sub class=\"import-GWPsubscript\"><em><em>a<\/em><\/em><\/sub><em lang=\"de-DE\" xml:lang=\"de-DE\">\u00a0=\u00a0<\/em><em class=\"import-GWPCambria\">K<\/em><sub class=\"import-GWPsubscript\"><em><em>g<\/em><\/em><\/sub>\u0394<em class=\"import-GWPCambria\">V\/I<\/em><\/p>\r\n<p class=\"import-Normal\"><em class=\"import-GWPCambria\">\u03c1<\/em><sub class=\"import-GWPsubscript\"><em><em>a<\/em><\/em><\/sub><sub class=\"import-GWPsubscript\"><em><em>_Wenner<\/em><\/em><\/sub>\u00a0=\u00a0250\u00a0ohm-m\u00a0=\u00a0[latex]\\frac{31.4\\ \\textrm{m}\\ V\\ \\textrm{mV}}{2\\ \\textrm{mA}}[\/latex]<\/p>\r\n<p class=\"import-Normal\">solving for <em>V<\/em> yields <em>V<\/em>\u00a0=\u00a015.9\u00a0mV<\/p>\r\n<p class=\"import-Normal\"><em class=\"import-GWPCambria\">\u03c1<\/em><sub class=\"import-GWPsubscript\"><em><em>a<\/em><\/em><\/sub><sub class=\"import-GWPsubscript\"><em><em>_dipole<\/em><\/em><\/sub><sub class=\"import-GWPsubscript\"><em><em>-<\/em><\/em><\/sub><sub class=\"import-GWPsubscript\"><em><em>dipole<\/em><\/em><\/sub>\u00a0=\u00a0250\u00a0ohm-m\u00a0=\u00a0[latex]\\frac{56.5\\ \\textrm{m}\\ V\\ \\textrm{mV}}{2\\ \\textrm{mA}}[\/latex]<\/p>\r\n<p class=\"import-Normal\">solving for <em>V<\/em> yields <em>V<\/em>\u00a0=\u00a08.8\u00a0mV<\/p>\r\n<p class=\"import-Normal\">A negative voltage would be correct for <em class=\"import-GWPCambria\">A B M N<\/em> configuration, as the geometric factor is negative.<\/p>\r\n<p class=\"import-Normal\">In summary:<\/p>\r\n\r\n<table style=\"border-collapse: collapse; width: 100%;\">\r\n<tbody>\r\n<tr style=\"border-bottom: thin solid;\">\r\n<td style=\"width: 20%; text-align: left;\"><strong>Array<\/strong><\/td>\r\n<td style=\"width: 16%; text-align: center;\"><strong>a(m)<\/strong><\/td>\r\n<td style=\"width: 16%; text-align: center;\"><strong>n<\/strong><\/td>\r\n<td style=\"width: 16%; text-align: center;\"><strong><em>K<\/em><sub><em>g<\/em><\/sub><\/strong><\/td>\r\n<td style=\"width: 16%; text-align: center;\"><strong>V(mV)<\/strong><\/td>\r\n<td style=\"width: 16%; text-align: center;\"><strong>SNR<\/strong><\/td>\r\n<\/tr>\r\n<tr style=\"border-bottom: thin solid;\">\r\n<td style=\"width: 20%; text-align: left;\">Wenner<\/td>\r\n<td style=\"width: 16%; text-align: center;\">5<\/td>\r\n<td style=\"width: 16%; text-align: center;\">-<\/td>\r\n<td style=\"width: 16%; text-align: center;\"><span style=\"color: #ff0000;\">31.4<\/span><\/td>\r\n<td style=\"width: 16%; text-align: center;\"><span style=\"color: #ff0000;\">15.9<\/span><\/td>\r\n<td style=\"width: 16%; text-align: center;\"><span style=\"color: #ff0000;\">1.06<\/span><\/td>\r\n<\/tr>\r\n<tr>\r\n<td style=\"width: 20%; text-align: left;\">Dipole-dipole<\/td>\r\n<td style=\"width: 16%; text-align: center;\">3<\/td>\r\n<td style=\"width: 16%; text-align: center;\">3<\/td>\r\n<td style=\"width: 16%; text-align: center;\"><span style=\"color: #ff0000;\">56.5<\/span><\/td>\r\n<td style=\"width: 16%; text-align: center;\"><span style=\"color: #ff0000;\">8.8<\/span><\/td>\r\n<td style=\"width: 16%; text-align: center;\"><span style=\"color: #ff0000;\">0.59<\/span><\/td>\r\n<\/tr>\r\n<\/tbody>\r\n<\/table>\r\n<p class=\"import-Normal\" style=\"text-align: right;\"><a href=\"https:\/\/books.gw-project.org\/electrical-imaging-for-hydrogeology\/chapter\/exercise-6\/\">Return to Exercise 6<\/a><\/p>\r\n\r\n<\/div>","rendered":"<div class=\"solution-exercise-6\">\n<p class=\"import-Normal\">Current injected [<em class=\"import-GWPCambria\">I<\/em>]:\u00a02\u00a0mA<\/p>\n<p class=\"import-Normal\">Apparent resistivity [<em class=\"import-GWPCambria\">\u03c1<\/em>]:\u00a0250\u00a0ohm-m<\/p>\n<p class=\"import-Normal\">Noise level:\u00a015\u00a0mV<\/p>\n<p style=\"text-align: center;\">[latex]\\displaystyle K_{g}=\\frac{2\\pi }{\\frac{1}{\\overline{AM}}-\\frac{1}{\\overline{AN}}-\\frac{1}{\\overline{BM}}+\\frac{1}{\\overline{BN}}}[\/latex]<\/p>\n<p style=\"text-align: center;\">[latex]\\displaystyle K_{g,Wenner}=\\frac{2\\pi }{\\frac{1}{5\\mathrm{m}}-\\frac{1}{10\\mathrm{m}}-\\frac{1}{10\\mathrm{m}}+\\frac{1}{5\\mathrm{m}}}[\/latex]<\/p>\n<p class=\"import-Normal\" style=\"text-align: center;\">=<em class=\"import-GWPCambria\">\u00a0<\/em>31.4\u00a0m<\/p>\n<p class=\"import-Normal\">For a positive geometric factor with a dipole-dipole array, you need to have the electrodes configured as <em class=\"import-GWPCambria\">A B N M<\/em> (this also gives a positive resistance). If you configure the electrodes as <em class=\"import-GWPCambria\">A B M N<\/em> (as often written) the geometric factor is negative (so is the resistance). Using <em class=\"import-GWPCambria\">A B N M<\/em> the geometric factor is:<\/p>\n<p style=\"text-align: center;\">[latex]\\displaystyle K_{g,dipole-dipole}=\\frac{2\\pi }{\\frac{1}{\\overline{AM}}-\\frac{1}{\\overline{AN}}-\\frac{1}{\\overline{BM}}+\\frac{1}{\\overline{BN}}}[\/latex] = [latex]\\displaystyle \\frac{2\\pi }{\\frac{1}{9\\mathrm{m}}-\\frac{1}{6\\mathrm{m}}-\\frac{1}{6\\mathrm{m}}+\\frac{1}{3\\mathrm{m}}}[\/latex] = 56.5 m<\/p>\n<p class=\"import-Normal\">If you do the calculation as <em class=\"import-GWPCambria\">A B M N<\/em>, you get a geometric factor of -56.5.<\/p>\n<p class=\"import-Normal\">We then need to calculate the apparent resistivity:<\/p>\n<p class=\"import-Normal\"><em class=\"import-GWPCambria\">\u03c1<\/em><sub class=\"import-GWPsubscript\"><em><em>a<\/em><\/em><\/sub><em lang=\"de-DE\" xml:lang=\"de-DE\">\u00a0=\u00a0<\/em><em class=\"import-GWPCambria\">K<\/em><sub class=\"import-GWPsubscript\"><em><em>g<\/em><\/em><\/sub>\u0394<em class=\"import-GWPCambria\">V\/I<\/em><\/p>\n<p class=\"import-Normal\"><em class=\"import-GWPCambria\">\u03c1<\/em><sub class=\"import-GWPsubscript\"><em><em>a<\/em><\/em><\/sub><sub class=\"import-GWPsubscript\"><em><em>_Wenner<\/em><\/em><\/sub>\u00a0=\u00a0250\u00a0ohm-m\u00a0=\u00a0[latex]\\frac{31.4\\ \\textrm{m}\\ V\\ \\textrm{mV}}{2\\ \\textrm{mA}}[\/latex]<\/p>\n<p class=\"import-Normal\">solving for <em>V<\/em> yields <em>V<\/em>\u00a0=\u00a015.9\u00a0mV<\/p>\n<p class=\"import-Normal\"><em class=\"import-GWPCambria\">\u03c1<\/em><sub class=\"import-GWPsubscript\"><em><em>a<\/em><\/em><\/sub><sub class=\"import-GWPsubscript\"><em><em>_dipole<\/em><\/em><\/sub><sub class=\"import-GWPsubscript\"><em><em>&#8211;<\/em><\/em><\/sub><sub class=\"import-GWPsubscript\"><em><em>dipole<\/em><\/em><\/sub>\u00a0=\u00a0250\u00a0ohm-m\u00a0=\u00a0[latex]\\frac{56.5\\ \\textrm{m}\\ V\\ \\textrm{mV}}{2\\ \\textrm{mA}}[\/latex]<\/p>\n<p class=\"import-Normal\">solving for <em>V<\/em> yields <em>V<\/em>\u00a0=\u00a08.8\u00a0mV<\/p>\n<p class=\"import-Normal\">A negative voltage would be correct for <em class=\"import-GWPCambria\">A B M N<\/em> configuration, as the geometric factor is negative.<\/p>\n<p class=\"import-Normal\">In summary:<\/p>\n<table style=\"border-collapse: collapse; width: 100%;\">\n<tbody>\n<tr style=\"border-bottom: thin solid;\">\n<td style=\"width: 20%; text-align: left;\"><strong>Array<\/strong><\/td>\n<td style=\"width: 16%; text-align: center;\"><strong>a(m)<\/strong><\/td>\n<td style=\"width: 16%; text-align: center;\"><strong>n<\/strong><\/td>\n<td style=\"width: 16%; text-align: center;\"><strong><em>K<\/em><sub><em>g<\/em><\/sub><\/strong><\/td>\n<td style=\"width: 16%; text-align: center;\"><strong>V(mV)<\/strong><\/td>\n<td style=\"width: 16%; text-align: center;\"><strong>SNR<\/strong><\/td>\n<\/tr>\n<tr style=\"border-bottom: thin solid;\">\n<td style=\"width: 20%; text-align: left;\">Wenner<\/td>\n<td style=\"width: 16%; text-align: center;\">5<\/td>\n<td style=\"width: 16%; text-align: center;\">&#8211;<\/td>\n<td style=\"width: 16%; text-align: center;\"><span style=\"color: #ff0000;\">31.4<\/span><\/td>\n<td style=\"width: 16%; text-align: center;\"><span style=\"color: #ff0000;\">15.9<\/span><\/td>\n<td style=\"width: 16%; text-align: center;\"><span style=\"color: #ff0000;\">1.06<\/span><\/td>\n<\/tr>\n<tr>\n<td style=\"width: 20%; text-align: left;\">Dipole-dipole<\/td>\n<td style=\"width: 16%; text-align: center;\">3<\/td>\n<td style=\"width: 16%; text-align: center;\">3<\/td>\n<td style=\"width: 16%; text-align: center;\"><span style=\"color: #ff0000;\">56.5<\/span><\/td>\n<td style=\"width: 16%; text-align: center;\"><span style=\"color: #ff0000;\">8.8<\/span><\/td>\n<td style=\"width: 16%; text-align: center;\"><span style=\"color: #ff0000;\">0.59<\/span><\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<p class=\"import-Normal\" style=\"text-align: right;\"><a href=\"https:\/\/books.gw-project.org\/electrical-imaging-for-hydrogeology\/chapter\/exercise-6\/\">Return to Exercise 6<\/a><\/p>\n<\/div>\n","protected":false},"author":1,"menu_order":43,"template":"","meta":{"pb_show_title":"on","pb_short_title":"","pb_subtitle":"","pb_authors":[],"pb_section_license":""},"chapter-type":[],"contributor":[],"license":[],"class_list":["post-100","chapter","type-chapter","status-publish","hentry"],"part":158,"_links":{"self":[{"href":"https:\/\/books.gw-project.org\/electrical-imaging-for-hydrogeology\/wp-json\/pressbooks\/v2\/chapters\/100","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/books.gw-project.org\/electrical-imaging-for-hydrogeology\/wp-json\/pressbooks\/v2\/chapters"}],"about":[{"href":"https:\/\/books.gw-project.org\/electrical-imaging-for-hydrogeology\/wp-json\/wp\/v2\/types\/chapter"}],"author":[{"embeddable":true,"href":"https:\/\/books.gw-project.org\/electrical-imaging-for-hydrogeology\/wp-json\/wp\/v2\/users\/1"}],"version-history":[{"count":11,"href":"https:\/\/books.gw-project.org\/electrical-imaging-for-hydrogeology\/wp-json\/pressbooks\/v2\/chapters\/100\/revisions"}],"predecessor-version":[{"id":384,"href":"https:\/\/books.gw-project.org\/electrical-imaging-for-hydrogeology\/wp-json\/pressbooks\/v2\/chapters\/100\/revisions\/384"}],"part":[{"href":"https:\/\/books.gw-project.org\/electrical-imaging-for-hydrogeology\/wp-json\/pressbooks\/v2\/parts\/158"}],"metadata":[{"href":"https:\/\/books.gw-project.org\/electrical-imaging-for-hydrogeology\/wp-json\/pressbooks\/v2\/chapters\/100\/metadata\/"}],"wp:attachment":[{"href":"https:\/\/books.gw-project.org\/electrical-imaging-for-hydrogeology\/wp-json\/wp\/v2\/media?parent=100"}],"wp:term":[{"taxonomy":"chapter-type","embeddable":true,"href":"https:\/\/books.gw-project.org\/electrical-imaging-for-hydrogeology\/wp-json\/pressbooks\/v2\/chapter-type?post=100"},{"taxonomy":"contributor","embeddable":true,"href":"https:\/\/books.gw-project.org\/electrical-imaging-for-hydrogeology\/wp-json\/wp\/v2\/contributor?post=100"},{"taxonomy":"license","embeddable":true,"href":"https:\/\/books.gw-project.org\/electrical-imaging-for-hydrogeology\/wp-json\/wp\/v2\/license?post=100"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}