{"id":1357,"date":"2026-05-12T21:47:39","date_gmt":"2026-05-12T21:47:39","guid":{"rendered":"https:\/\/books.gw-project.org\/basic-hydrogeology-an-introduction-to-the-fundamentals-of-groundwater-science\/chapter\/exercise-11\/"},"modified":"2026-05-13T16:48:36","modified_gmt":"2026-05-13T16:48:36","slug":"exercise-11","status":"publish","type":"chapter","link":"https:\/\/books.gw-project.org\/basic-hydrogeology-an-introduction-to-the-fundamentals-of-groundwater-science\/chapter\/exercise-11\/","title":{"raw":"Exercise 11","rendered":"Exercise 11"},"content":{"raw":"
\r\n
\r\n\r\nThis image shows time\u2011drawdown data from a multi\u2011well aquifer test that involved one pumping well and one observation well. The data are from the observation well located 20\u00a0meters from the pumping well. The pumping well was pumped at 100\u00a0m3<\/sup>\/d for 72\u00a0hours.\r\n\r\n<\/div>\r\n
\r\n\r\nAssume the aquifer is a fully confined sandstone with a constant saturated thickness of 20 m.\r\n\r\n<\/div>\r\n
    \r\n \t
  1. Manually fit the data to the Theis type curve provided below it.<\/li>\r\n \t
  2. Then, for [latex]t[\/latex]\u00a0=\u00a01 and[latex]\\ s[\/latex]\u00a0=\u00a01, select match points for 1\/[latex]u[\/latex] and [latex]W(u)[\/latex] and calculate [latex]T,\\ S[\/latex], and [latex]K[\/latex] for the test.<\/li>\r\n \t
  3. Provide the values of t, s, 1\/u, W(u) for the selected match point and show the calculations to determine T, S, and K.<\/li>\r\n<\/ol>\r\n
    \r\n
    \"A<\/blockquote>\r\n<\/div>\r\n
    \r\n\r\n\"A\r\n\r\n<\/div>\r\n
    \r\n\r\nSolution for Exercise\u00a01<\/span><\/a>1<\/u><\/strong>\u2ba7\r\n\r\n<\/div>\r\n
    \r\n\r\nReturn to where text linked to Exercise\u00a011<\/strong><\/span><\/a>\u2ba5\r\n\r\n<\/div>\r\n<\/div>","rendered":"
    \n
    \n

    This image shows time\u2011drawdown data from a multi\u2011well aquifer test that involved one pumping well and one observation well. The data are from the observation well located 20\u00a0meters from the pumping well. The pumping well was pumped at 100\u00a0m3<\/sup>\/d for 72\u00a0hours.<\/p>\n<\/div>\n

    \n

    Assume the aquifer is a fully confined sandstone with a constant saturated thickness of 20 m.<\/p>\n<\/div>\n

      \n
    1. Manually fit the data to the Theis type curve provided below it.<\/li>\n
    2. Then, for [latex]t[\/latex]\u00a0=\u00a01 and[latex]\\ s[\/latex]\u00a0=\u00a01, select match points for 1\/[latex]u[\/latex] and [latex]W(u)[\/latex] and calculate [latex]T,\\ S[\/latex], and [latex]K[\/latex] for the test.<\/li>\n
    3. Provide the values of t, s, 1\/u, W(u) for the selected match point and show the calculations to determine T, S, and K.<\/li>\n<\/ol>\n
      \n

      \"A<\/p><\/blockquote>\n<\/div>\n

      \n

      \"A<\/p>\n<\/div>\n

      \n

      Solution for Exercise\u00a01<\/span><\/a>1<\/u><\/strong>\u2ba7<\/p>\n<\/div>\n

      \n

      Return to where text linked to Exercise\u00a011<\/strong><\/span><\/a>\u2ba5<\/p>\n<\/div>\n<\/div>\n","protected":false},"author":8,"menu_order":94,"template":"","meta":{"pb_show_title":"on","pb_short_title":"","pb_subtitle":"","pb_authors":[],"pb_section_license":""},"chapter-type":[],"contributor":[],"license":[],"class_list":["post-1357","chapter","type-chapter","status-publish","hentry"],"part":1522,"_links":{"self":[{"href":"https:\/\/books.gw-project.org\/basic-hydrogeology-an-introduction-to-the-fundamentals-of-groundwater-science\/wp-json\/pressbooks\/v2\/chapters\/1357","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/books.gw-project.org\/basic-hydrogeology-an-introduction-to-the-fundamentals-of-groundwater-science\/wp-json\/pressbooks\/v2\/chapters"}],"about":[{"href":"https:\/\/books.gw-project.org\/basic-hydrogeology-an-introduction-to-the-fundamentals-of-groundwater-science\/wp-json\/wp\/v2\/types\/chapter"}],"author":[{"embeddable":true,"href":"https:\/\/books.gw-project.org\/basic-hydrogeology-an-introduction-to-the-fundamentals-of-groundwater-science\/wp-json\/wp\/v2\/users\/8"}],"version-history":[{"count":3,"href":"https:\/\/books.gw-project.org\/basic-hydrogeology-an-introduction-to-the-fundamentals-of-groundwater-science\/wp-json\/pressbooks\/v2\/chapters\/1357\/revisions"}],"predecessor-version":[{"id":1868,"href":"https:\/\/books.gw-project.org\/basic-hydrogeology-an-introduction-to-the-fundamentals-of-groundwater-science\/wp-json\/pressbooks\/v2\/chapters\/1357\/revisions\/1868"}],"part":[{"href":"https:\/\/books.gw-project.org\/basic-hydrogeology-an-introduction-to-the-fundamentals-of-groundwater-science\/wp-json\/pressbooks\/v2\/parts\/1522"}],"metadata":[{"href":"https:\/\/books.gw-project.org\/basic-hydrogeology-an-introduction-to-the-fundamentals-of-groundwater-science\/wp-json\/pressbooks\/v2\/chapters\/1357\/metadata\/"}],"wp:attachment":[{"href":"https:\/\/books.gw-project.org\/basic-hydrogeology-an-introduction-to-the-fundamentals-of-groundwater-science\/wp-json\/wp\/v2\/media?parent=1357"}],"wp:term":[{"taxonomy":"chapter-type","embeddable":true,"href":"https:\/\/books.gw-project.org\/basic-hydrogeology-an-introduction-to-the-fundamentals-of-groundwater-science\/wp-json\/pressbooks\/v2\/chapter-type?post=1357"},{"taxonomy":"contributor","embeddable":true,"href":"https:\/\/books.gw-project.org\/basic-hydrogeology-an-introduction-to-the-fundamentals-of-groundwater-science\/wp-json\/wp\/v2\/contributor?post=1357"},{"taxonomy":"license","embeddable":true,"href":"https:\/\/books.gw-project.org\/basic-hydrogeology-an-introduction-to-the-fundamentals-of-groundwater-science\/wp-json\/wp\/v2\/license?post=1357"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}