{"id":492,"date":"2022-12-11T23:09:08","date_gmt":"2022-12-11T23:09:08","guid":{"rendered":"https:\/\/books.gw-project.org\/introduction-to-karst-aquifers\/chapter\/exercise-17-solution\/"},"modified":"2023-03-23T17:46:24","modified_gmt":"2023-03-23T17:46:24","slug":"exercise-17-solution","status":"publish","type":"chapter","link":"https:\/\/books.gw-project.org\/introduction-to-karst-aquifers\/chapter\/exercise-17-solution\/","title":{"raw":"Exercise 17 Solution","rendered":"Exercise 17 Solution"},"content":{"raw":"<div class=\"exercise-17-solution\">\r\n<p class=\"import-Normal\">Using an internet search, learn that a hydrograph is a chart of the time series of water level or flow (that is, water level in a well, streamflow, stream gage height, spring flow). A chemograph is a chart of the time series of changing water chemistry (that is, groundwater chemistry, spring or stream water chemistry). Often a time series of discharge is used in conjunction a times series of water chemistry to assess diffuse versus rapid flow of water to a spring, or to estimate the groundwater discharge component of streamflow.<\/p>\r\n<p class=\"import-Normal\" style=\"text-align: right;\"><a href=\"https:\/\/books.gw-project.org\/introduction-to-karst-aquifers\/chapter\/exercise-17\/\"><span class=\"import-Hyperlink\">Return to Exercise 1<\/span><span class=\"import-Hyperlink\">7<\/span><\/a><\/p>\r\n<p class=\"import-Normal\" style=\"text-align: right;\"><a href=\"https:\/\/books.gw-project.org\/introduction-to-karst-aquifers\/part\/methods-of-karst-characterization\/#class-link-to-exercise-17\">Return to where text linked to Exercise 17<\/a><\/p>\r\n\r\n<\/div>","rendered":"<div class=\"exercise-17-solution\">\n<p class=\"import-Normal\">Using an internet search, learn that a hydrograph is a chart of the time series of water level or flow (that is, water level in a well, streamflow, stream gage height, spring flow). A chemograph is a chart of the time series of changing water chemistry (that is, groundwater chemistry, spring or stream water chemistry). Often a time series of discharge is used in conjunction a times series of water chemistry to assess diffuse versus rapid flow of water to a spring, or to estimate the groundwater discharge component of streamflow.<\/p>\n<p class=\"import-Normal\" style=\"text-align: right;\"><a href=\"https:\/\/books.gw-project.org\/introduction-to-karst-aquifers\/chapter\/exercise-17\/\"><span class=\"import-Hyperlink\">Return to Exercise 1<\/span><span class=\"import-Hyperlink\">7<\/span><\/a><\/p>\n<p class=\"import-Normal\" style=\"text-align: right;\"><a href=\"https:\/\/books.gw-project.org\/introduction-to-karst-aquifers\/part\/methods-of-karst-characterization\/#class-link-to-exercise-17\">Return to where text linked to Exercise 17<\/a><\/p>\n<\/div>\n","protected":false},"author":1,"menu_order":64,"template":"","meta":{"pb_show_title":"on","pb_short_title":"","pb_subtitle":"","pb_authors":[],"pb_section_license":""},"chapter-type":[],"contributor":[],"license":[],"class_list":["post-492","chapter","type-chapter","status-publish","hentry"],"part":580,"_links":{"self":[{"href":"https:\/\/books.gw-project.org\/introduction-to-karst-aquifers\/wp-json\/pressbooks\/v2\/chapters\/492","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/books.gw-project.org\/introduction-to-karst-aquifers\/wp-json\/pressbooks\/v2\/chapters"}],"about":[{"href":"https:\/\/books.gw-project.org\/introduction-to-karst-aquifers\/wp-json\/wp\/v2\/types\/chapter"}],"author":[{"embeddable":true,"href":"https:\/\/books.gw-project.org\/introduction-to-karst-aquifers\/wp-json\/wp\/v2\/users\/1"}],"version-history":[{"count":3,"href":"https:\/\/books.gw-project.org\/introduction-to-karst-aquifers\/wp-json\/pressbooks\/v2\/chapters\/492\/revisions"}],"predecessor-version":[{"id":930,"href":"https:\/\/books.gw-project.org\/introduction-to-karst-aquifers\/wp-json\/pressbooks\/v2\/chapters\/492\/revisions\/930"}],"part":[{"href":"https:\/\/books.gw-project.org\/introduction-to-karst-aquifers\/wp-json\/pressbooks\/v2\/parts\/580"}],"metadata":[{"href":"https:\/\/books.gw-project.org\/introduction-to-karst-aquifers\/wp-json\/pressbooks\/v2\/chapters\/492\/metadata\/"}],"wp:attachment":[{"href":"https:\/\/books.gw-project.org\/introduction-to-karst-aquifers\/wp-json\/wp\/v2\/media?parent=492"}],"wp:term":[{"taxonomy":"chapter-type","embeddable":true,"href":"https:\/\/books.gw-project.org\/introduction-to-karst-aquifers\/wp-json\/pressbooks\/v2\/chapter-type?post=492"},{"taxonomy":"contributor","embeddable":true,"href":"https:\/\/books.gw-project.org\/introduction-to-karst-aquifers\/wp-json\/wp\/v2\/contributor?post=492"},{"taxonomy":"license","embeddable":true,"href":"https:\/\/books.gw-project.org\/introduction-to-karst-aquifers\/wp-json\/wp\/v2\/license?post=492"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}