{"id":609,"date":"2025-11-21T00:55:16","date_gmt":"2025-11-21T00:55:16","guid":{"rendered":"https:\/\/books.gw-project.org\/an-introduction-to-hydraulic-testing-in-hydrogeology\/?post_type=part&#038;p=609"},"modified":"2026-08-01T14:32:42","modified_gmt":"2026-08-01T14:32:42","slug":"modifications-to-original-release","status":"publish","type":"part","link":"https:\/\/books.gw-project.org\/an-introduction-to-hydraulic-testing-in-hydrogeology\/part\/modifications-to-original-release\/","title":{"raw":"Modifications to Original Release","rendered":"Modifications to Original Release"},"content":{"raw":"<div data-custom-style=\"First Paragraph\">\r\n\r\n<strong><u>Changes from the Original Version to Version 2<\/u><\/strong>\r\n\r\n<\/div>\r\n<div data-custom-style=\"Body Text\">\r\n\r\nOriginal Version: September 18, 2023, Version 2: October 30, 2023\r\n\r\n<\/div>\r\n<div data-custom-style=\"Body Text\">\r\n\r\nPage numbers refer to the original PDF.\r\n\r\n<\/div>\r\n<div data-custom-style=\"Body Text\">\r\n\r\npage ii, added doi\r\n\r\n<\/div>\r\n<div data-custom-style=\"Body Text\">\r\n\r\npage xi, corrected 70 to 90\r\n\r\n<\/div>\r\n<div data-custom-style=\"Body Text\">\r\n\r\npage 153, Figure 87 changed the denominator from 200 to 2000 in the third expression of part a)\r\n\r\n<\/div>\r\n<div data-custom-style=\"Body Text\">\r\n\r\npage 196, changed <em>t<sub>1 <\/sub><\/em>= time at head <em>h<sub>2<\/sub><\/em> to <em>t<sub>1 <\/sub><\/em>= time at head <em>h<sub>1<\/sub><\/em>\r\n\r\n<\/div>\r\n<div data-custom-style=\"Body Text\">\r\n\r\n<strong><u>Changes from the Version 2 to Version 3<\/u><\/strong>\r\n\r\n<\/div>\r\n<div data-custom-style=\"Body Text\">\r\n\r\nVersion 3: March, 6, 2024\r\n\r\n<\/div>\r\n<div data-custom-style=\"Body Text\">\r\n\r\nPage numbers refer to the PDF of Version 2.\r\n\r\n<\/div>\r\n<div data-custom-style=\"Body Text\">\r\n\r\npage iii, corrected APA citation that was missing the third author\u2019s name\r\n\r\n<\/div>\r\n<div data-custom-style=\"Body Text\">\r\n\r\npage 98, a number of changes were made:\r\n\r\n<\/div>\r\n<div data-custom-style=\"Block Text\">\r\n<blockquote>The content of the first 3 paragraphs including table and equations were changed from the following as shown in gray:<\/blockquote>\r\n<\/div>\r\n<div data-custom-style=\"Block Text\">\r\n<blockquote>\r\n<div class=\"bc-mark mark\">Using the relationship f(<em>r<\/em>\/<em>B<\/em>) =\u00a01.7 = exp(<em>r<\/em>\/<em>B<\/em>)K<em><sub>0<\/sub><\/em>(<em>r<\/em>\/<em>B<\/em>), then from <a href=\"https:\/\/books.gw-project.org\/an-introduction-to-hydraulic-testing-in-hydrogeology\/chapter\/hantush%e2%80%91jacob-solution-leaky-confined%e2%80%91no-water-released-from-aquitard-storage\/#X22d552b6d8c60dd43a776e87129f998a8c8caf0\">Figure 48<\/a>, the value between X\u00a0=\u00a01.5 and X\u00a0=\u00a02.0. The interpolation is shown below.<\/div><\/blockquote>\r\n<\/div>\r\n<table style=\"width: 51%;\" data-custom-style=\"Table\"><colgroup> <col style=\"width: 9%;\" \/> <col style=\"width: 20%;\" \/> <col style=\"width: 20%;\" \/> <\/colgroup>\r\n<thead>\r\n<tr>\r\n<th style=\"text-align: center;\">\r\n<div class=\"bc-mark mark\">X<\/div><\/th>\r\n<th style=\"text-align: center;\">\r\n<div class=\"bc-mark mark\">K<sub>0<\/sub>(x)<\/div><\/th>\r\n<th style=\"text-align: center;\">\r\n<div class=\"bc-mark mark\">exp (x) K<sub>0<\/sub>(x)<\/div><\/th>\r\n<\/tr>\r\n<\/thead>\r\n<tbody>\r\n<tr>\r\n<td style=\"text-align: center;\">\r\n<div class=\"bc-mark mark\">1.5<\/div><\/td>\r\n<td style=\"text-align: center;\">\r\n<div class=\"bc-mark mark\">0.21<\/div><\/td>\r\n<td style=\"text-align: center;\">\r\n<div class=\"bc-mark mark\">0.96<\/div><\/td>\r\n<\/tr>\r\n<tr>\r\n<td style=\"text-align: center;\">\r\n<div class=\"bc-mark mark\">1.7<\/div><\/td>\r\n<td style=\"text-align: center;\">\r\n<div class=\"bc-mark mark\">0.17 (interpolated)<\/div><\/td>\r\n<td style=\"text-align: center;\">\r\n<div class=\"bc-mark mark\">0.91 (interpolated)<\/div><\/td>\r\n<\/tr>\r\n<tr>\r\n<td style=\"text-align: center;\">\r\n<div class=\"bc-mark mark\">2.0<\/div><\/td>\r\n<td style=\"text-align: center;\">\r\n<div class=\"bc-mark mark\">0.11<\/div><\/td>\r\n<td style=\"text-align: center;\">\r\n<div class=\"bc-mark mark\">0.84<\/div><\/td>\r\n<\/tr>\r\n<\/tbody>\r\n<\/table>\r\n<div data-custom-style=\"Block Text\">\r\n<blockquote>\r\n<div class=\"bc-mark mark\">Given that <em>x<\/em> in <a href=\"https:\/\/books.gw-project.org\/an-introduction-to-hydraulic-testing-in-hydrogeology\/chapter\/hantush%e2%80%91jacob-solution-leaky-confined%e2%80%91no-water-released-from-aquitard-storage\/#X22d552b6d8c60dd43a776e87129f998a8c8caf0\">Figure 48<\/a> equals <em>r<\/em>\/<em>B<\/em>, then <em>r<\/em>\/<em>B<\/em>=1.7, with the observation well located 75 m from the pumping well, then <em>B<\/em> = <em>75\u00a0<\/em>m \/ 1.7 = 44.1\u00a0m. Now using Equation\u00a0<a href=\"https:\/\/books.gw-project.org\/an-introduction-to-hydraulic-testing-in-hydrogeology\/chapter\/hantush%e2%80%91jacob-solution-leaky-confined%e2%80%91no-water-released-from-aquitard-storage\/#Xa93b1e4f422196d37fb83300cc0b32b27a43db7\">(52)<\/a>.<\/div><\/blockquote>\r\n<\/div>\r\n<div data-custom-style=\"Block Text\">\r\n<div class=\"display-math\" data-custom-style=\"Display Equation\">\r\n\r\n[latex]T = \\frac{4250\\ \\frac{m^{3}}{d}\\ 0.17}{2\\ (3.14)\\ 3.7\\ m} = 31.1\\frac{m^{2}}{d}[\/latex]\r\n\r\n<\/div>\r\n<\/div>\r\n<div data-custom-style=\"Block Text\">\r\n<blockquote>\r\n<div class=\"bc-mark mark\">S is then computed from Equation\u00a0<a href=\"https:\/\/books.gw-project.org\/an-introduction-to-hydraulic-testing-in-hydrogeology\/chapter\/hantush%E2%80%91jacob-solution-leaky-confined%E2%80%91no-water-released-from-aquitard-storage\/#Xcbc9563b5d554d8f186baa4c7fb85f0e5456dd9\">(53)<\/a>.<\/div><\/blockquote>\r\n<\/div>\r\n<div data-custom-style=\"Block Text\">\r\n<div class=\"display-math\" data-custom-style=\"Display Equation\">\r\n\r\n[latex]S = \\frac{4\\ \\left( 31.1\\frac{m^{2}}{d} \\right)\\ 0.011d}{2\\ (75\\ m)\\ (44.1)} = 0.0002\\ = \\ 2x10^{- 4}[\/latex]\r\n\r\n<\/div>\r\n<\/div>\r\n<div data-custom-style=\"Block Text\">\r\n<blockquote>to:<\/blockquote>\r\n<\/div>\r\n<div data-custom-style=\"Block Text\">\r\n<blockquote>Using the relationship f(<em>r<\/em>\/<em>B<\/em>) =\u00a01.7 = exp(<em>r<\/em>\/<em>B<\/em>)K<em><sub>0<\/sub><\/em>(<em>r<\/em>\/<em>B<\/em>), then from <a href=\"https:\/\/books.gw-project.org\/an-introduction-to-hydraulic-testing-in-hydrogeology\/chapter\/hantush%e2%80%91jacob-solution-leaky-confined%e2%80%91no-water-released-from-aquitard-storage\/#X22d552b6d8c60dd43a776e87129f998a8c8caf0\">Figure 48<\/a>, the value is between exp(x)K<sub>0<\/sub>(x)\u00a0=\u00a01.66 and exp(x)K<sub>0<\/sub>(x)\u00a0=\u00a01.75. The interpolation is shown below.<\/blockquote>\r\n<\/div>\r\n<table style=\"width: 51%;\" data-custom-style=\"Table\"><colgroup> <col style=\"width: 18%;\" \/> <col style=\"width: 19%;\" \/> <col style=\"width: 13%;\" \/> <\/colgroup>\r\n<thead>\r\n<tr>\r\n<th>x<\/th>\r\n<th>K<sub>0<\/sub>(x)<\/th>\r\n<th>exp (x) K<sub>0<\/sub>(x)<\/th>\r\n<\/tr>\r\n<\/thead>\r\n<tbody>\r\n<tr>\r\n<td>0.40<\/td>\r\n<td>1.11<\/td>\r\n<td>1.66<\/td>\r\n<\/tr>\r\n<tr>\r\n<td>0.37 (interpolated)<\/td>\r\n<td>1.16 (interpolated)<\/td>\r\n<td>1.7<\/td>\r\n<\/tr>\r\n<tr>\r\n<td>0.35<\/td>\r\n<td>1.23<\/td>\r\n<td>1.75<\/td>\r\n<\/tr>\r\n<\/tbody>\r\n<\/table>\r\n<div data-custom-style=\"Block Text\">\r\n<blockquote>Given that <em>x<\/em> = 0.37\u00a0m, with the observation well located 75 m from the pumping well, then <em>B<\/em> = <em>75\u00a0<\/em>m \/ 0.37 = 203\u00a0m. Now using Equation\u00a0<a href=\"https:\/\/books.gw-project.org\/an-introduction-to-hydraulic-testing-in-hydrogeology\/chapter\/hantush%e2%80%91jacob-solution-leaky-confined%e2%80%91no-water-released-from-aquitard-storage\/#Xa93b1e4f422196d37fb83300cc0b32b27a43db7\">(52)<\/a>.<\/blockquote>\r\n<\/div>\r\n<div data-custom-style=\"Block Text\">\r\n<div class=\"display-math\" data-custom-style=\"Display Equation\">\r\n\r\n[latex]T = \\frac{4250\\ \\frac{m^{3}}{d}\\ 1.16}{2\\ (3.14)\\ 3.7\\ m} = 212\\frac{m^{2}}{d}[\/latex]\r\n\r\n<\/div>\r\n<\/div>\r\n<div data-custom-style=\"Block Text\">\r\n<blockquote>S is then computed from Equation\u00a0<a href=\"https:\/\/books.gw-project.org\/an-introduction-to-hydraulic-testing-in-hydrogeology\/chapter\/hantush%E2%80%91jacob-solution-leaky-confined%E2%80%91no-water-released-from-aquitard-storage\/#Xcbc9563b5d554d8f186baa4c7fb85f0e5456dd9\">(53)<\/a>.<\/blockquote>\r\n<\/div>\r\n<div data-custom-style=\"Block Text\">\r\n<div class=\"display-math\" data-custom-style=\"Display Equation\">\r\n\r\n[latex]S = \\frac{4\\ \\left( 212\\ \\frac{m^{2}}{d} \\right)\\ 0.011d}{2\\ (75\\ m)\\ (203\\ m)} = 0.0003\\ = \\ 3x10^{- 4}[\/latex]\r\n\r\n<\/div>\r\n<\/div>\r\n<div data-custom-style=\"Block Text\">\r\n<blockquote>In addition the calculation of K\u2019 was changed from the following as shown in gray:<\/blockquote>\r\n<\/div>\r\n<div data-custom-style=\"First Paragraph\">\r\n<div class=\"display-math\" data-custom-style=\"Display Equation\">\r\n\r\n[latex]K' = \\frac{31.1\\frac{m^{2}}{d}\\ 15\\ m}{(44.1m)^{2}} = 0.24\\frac{m}{d}[\/latex]\r\n\r\n<\/div>\r\n<\/div>\r\n<div data-custom-style=\"Block Text\">\r\n<blockquote>to:<\/blockquote>\r\n<\/div>\r\n<div data-custom-style=\"First Paragraph\">\r\n<div class=\"display-math\" data-custom-style=\"Display Equation\">\r\n\r\n[latex]K' = \\frac{212\\frac{m^{2}}{d}\\ 15\\ m}{(203\\ m)^{2}} = 0.08\\frac{m}{d}[\/latex]\r\n\r\n<\/div>\r\n<\/div>\r\n<div data-custom-style=\"Body Text\">\r\n\r\npage 351, corrected format for Author\u2019s name and title\r\n\r\n<\/div>","rendered":"<div data-custom-style=\"First Paragraph\">\n<p><strong><u>Changes from the Original Version to Version 2<\/u><\/strong><\/p>\n<\/div>\n<div data-custom-style=\"Body Text\">\n<p>Original Version: September 18, 2023, Version 2: October 30, 2023<\/p>\n<\/div>\n<div data-custom-style=\"Body Text\">\n<p>Page numbers refer to the original PDF.<\/p>\n<\/div>\n<div data-custom-style=\"Body Text\">\n<p>page ii, added doi<\/p>\n<\/div>\n<div data-custom-style=\"Body Text\">\n<p>page xi, corrected 70 to 90<\/p>\n<\/div>\n<div data-custom-style=\"Body Text\">\n<p>page 153, Figure 87 changed the denominator from 200 to 2000 in the third expression of part a)<\/p>\n<\/div>\n<div data-custom-style=\"Body Text\">\n<p>page 196, changed <em>t<sub>1 <\/sub><\/em>= time at head <em>h<sub>2<\/sub><\/em> to <em>t<sub>1 <\/sub><\/em>= time at head <em>h<sub>1<\/sub><\/em><\/p>\n<\/div>\n<div data-custom-style=\"Body Text\">\n<p><strong><u>Changes from the Version 2 to Version 3<\/u><\/strong><\/p>\n<\/div>\n<div data-custom-style=\"Body Text\">\n<p>Version 3: March, 6, 2024<\/p>\n<\/div>\n<div data-custom-style=\"Body Text\">\n<p>Page numbers refer to the PDF of Version 2.<\/p>\n<\/div>\n<div data-custom-style=\"Body Text\">\n<p>page iii, corrected APA citation that was missing the third author\u2019s name<\/p>\n<\/div>\n<div data-custom-style=\"Body Text\">\n<p>page 98, a number of changes were made:<\/p>\n<\/div>\n<div data-custom-style=\"Block Text\">\n<blockquote><p>The content of the first 3 paragraphs including table and equations were changed from the following as shown in gray:<\/p><\/blockquote>\n<\/div>\n<div data-custom-style=\"Block Text\">\n<blockquote>\n<div class=\"bc-mark mark\">Using the relationship f(<em>r<\/em>\/<em>B<\/em>) =\u00a01.7 = exp(<em>r<\/em>\/<em>B<\/em>)K<em><sub>0<\/sub><\/em>(<em>r<\/em>\/<em>B<\/em>), then from <a href=\"https:\/\/books.gw-project.org\/an-introduction-to-hydraulic-testing-in-hydrogeology\/chapter\/hantush%e2%80%91jacob-solution-leaky-confined%e2%80%91no-water-released-from-aquitard-storage\/#X22d552b6d8c60dd43a776e87129f998a8c8caf0\">Figure 48<\/a>, the value between X\u00a0=\u00a01.5 and X\u00a0=\u00a02.0. The interpolation is shown below.<\/div>\n<\/blockquote>\n<\/div>\n<table style=\"width: 51%;\" data-custom-style=\"Table\">\n<colgroup>\n<col style=\"width: 9%;\" \/>\n<col style=\"width: 20%;\" \/>\n<col style=\"width: 20%;\" \/> <\/colgroup>\n<thead>\n<tr>\n<th style=\"text-align: center;\">\n<div class=\"bc-mark mark\">X<\/div>\n<\/th>\n<th style=\"text-align: center;\">\n<div class=\"bc-mark mark\">K<sub>0<\/sub>(x)<\/div>\n<\/th>\n<th style=\"text-align: center;\">\n<div class=\"bc-mark mark\">exp (x) K<sub>0<\/sub>(x)<\/div>\n<\/th>\n<\/tr>\n<\/thead>\n<tbody>\n<tr>\n<td style=\"text-align: center;\">\n<div class=\"bc-mark mark\">1.5<\/div>\n<\/td>\n<td style=\"text-align: center;\">\n<div class=\"bc-mark mark\">0.21<\/div>\n<\/td>\n<td style=\"text-align: center;\">\n<div class=\"bc-mark mark\">0.96<\/div>\n<\/td>\n<\/tr>\n<tr>\n<td style=\"text-align: center;\">\n<div class=\"bc-mark mark\">1.7<\/div>\n<\/td>\n<td style=\"text-align: center;\">\n<div class=\"bc-mark mark\">0.17 (interpolated)<\/div>\n<\/td>\n<td style=\"text-align: center;\">\n<div class=\"bc-mark mark\">0.91 (interpolated)<\/div>\n<\/td>\n<\/tr>\n<tr>\n<td style=\"text-align: center;\">\n<div class=\"bc-mark mark\">2.0<\/div>\n<\/td>\n<td style=\"text-align: center;\">\n<div class=\"bc-mark mark\">0.11<\/div>\n<\/td>\n<td style=\"text-align: center;\">\n<div class=\"bc-mark mark\">0.84<\/div>\n<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<div data-custom-style=\"Block Text\">\n<blockquote>\n<div class=\"bc-mark mark\">Given that <em>x<\/em> in <a href=\"https:\/\/books.gw-project.org\/an-introduction-to-hydraulic-testing-in-hydrogeology\/chapter\/hantush%e2%80%91jacob-solution-leaky-confined%e2%80%91no-water-released-from-aquitard-storage\/#X22d552b6d8c60dd43a776e87129f998a8c8caf0\">Figure 48<\/a> equals <em>r<\/em>\/<em>B<\/em>, then <em>r<\/em>\/<em>B<\/em>=1.7, with the observation well located 75 m from the pumping well, then <em>B<\/em> = <em>75\u00a0<\/em>m \/ 1.7 = 44.1\u00a0m. Now using Equation\u00a0<a href=\"https:\/\/books.gw-project.org\/an-introduction-to-hydraulic-testing-in-hydrogeology\/chapter\/hantush%e2%80%91jacob-solution-leaky-confined%e2%80%91no-water-released-from-aquitard-storage\/#Xa93b1e4f422196d37fb83300cc0b32b27a43db7\">(52)<\/a>.<\/div>\n<\/blockquote>\n<\/div>\n<div data-custom-style=\"Block Text\">\n<div class=\"display-math\" data-custom-style=\"Display Equation\">\n<p>[latex]T = \\frac{4250\\ \\frac{m^{3}}{d}\\ 0.17}{2\\ (3.14)\\ 3.7\\ m} = 31.1\\frac{m^{2}}{d}[\/latex]<\/p>\n<\/div>\n<\/div>\n<div data-custom-style=\"Block Text\">\n<blockquote>\n<div class=\"bc-mark mark\">S is then computed from Equation\u00a0<a href=\"https:\/\/books.gw-project.org\/an-introduction-to-hydraulic-testing-in-hydrogeology\/chapter\/hantush%E2%80%91jacob-solution-leaky-confined%E2%80%91no-water-released-from-aquitard-storage\/#Xcbc9563b5d554d8f186baa4c7fb85f0e5456dd9\">(53)<\/a>.<\/div>\n<\/blockquote>\n<\/div>\n<div data-custom-style=\"Block Text\">\n<div class=\"display-math\" data-custom-style=\"Display Equation\">\n<p>[latex]S = \\frac{4\\ \\left( 31.1\\frac{m^{2}}{d} \\right)\\ 0.011d}{2\\ (75\\ m)\\ (44.1)} = 0.0002\\ = \\ 2x10^{- 4}[\/latex]<\/p>\n<\/div>\n<\/div>\n<div data-custom-style=\"Block Text\">\n<blockquote><p>to:<\/p><\/blockquote>\n<\/div>\n<div data-custom-style=\"Block Text\">\n<blockquote><p>Using the relationship f(<em>r<\/em>\/<em>B<\/em>) =\u00a01.7 = exp(<em>r<\/em>\/<em>B<\/em>)K<em><sub>0<\/sub><\/em>(<em>r<\/em>\/<em>B<\/em>), then from <a href=\"https:\/\/books.gw-project.org\/an-introduction-to-hydraulic-testing-in-hydrogeology\/chapter\/hantush%e2%80%91jacob-solution-leaky-confined%e2%80%91no-water-released-from-aquitard-storage\/#X22d552b6d8c60dd43a776e87129f998a8c8caf0\">Figure 48<\/a>, the value is between exp(x)K<sub>0<\/sub>(x)\u00a0=\u00a01.66 and exp(x)K<sub>0<\/sub>(x)\u00a0=\u00a01.75. The interpolation is shown below.<\/p><\/blockquote>\n<\/div>\n<table style=\"width: 51%;\" data-custom-style=\"Table\">\n<colgroup>\n<col style=\"width: 18%;\" \/>\n<col style=\"width: 19%;\" \/>\n<col style=\"width: 13%;\" \/> <\/colgroup>\n<thead>\n<tr>\n<th>x<\/th>\n<th>K<sub>0<\/sub>(x)<\/th>\n<th>exp (x) K<sub>0<\/sub>(x)<\/th>\n<\/tr>\n<\/thead>\n<tbody>\n<tr>\n<td>0.40<\/td>\n<td>1.11<\/td>\n<td>1.66<\/td>\n<\/tr>\n<tr>\n<td>0.37 (interpolated)<\/td>\n<td>1.16 (interpolated)<\/td>\n<td>1.7<\/td>\n<\/tr>\n<tr>\n<td>0.35<\/td>\n<td>1.23<\/td>\n<td>1.75<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<div data-custom-style=\"Block Text\">\n<blockquote><p>Given that <em>x<\/em> = 0.37\u00a0m, with the observation well located 75 m from the pumping well, then <em>B<\/em> = <em>75\u00a0<\/em>m \/ 0.37 = 203\u00a0m. Now using Equation\u00a0<a href=\"https:\/\/books.gw-project.org\/an-introduction-to-hydraulic-testing-in-hydrogeology\/chapter\/hantush%e2%80%91jacob-solution-leaky-confined%e2%80%91no-water-released-from-aquitard-storage\/#Xa93b1e4f422196d37fb83300cc0b32b27a43db7\">(52)<\/a>.<\/p><\/blockquote>\n<\/div>\n<div data-custom-style=\"Block Text\">\n<div class=\"display-math\" data-custom-style=\"Display Equation\">\n<p>[latex]T = \\frac{4250\\ \\frac{m^{3}}{d}\\ 1.16}{2\\ (3.14)\\ 3.7\\ m} = 212\\frac{m^{2}}{d}[\/latex]<\/p>\n<\/div>\n<\/div>\n<div data-custom-style=\"Block Text\">\n<blockquote><p>S is then computed from Equation\u00a0<a href=\"https:\/\/books.gw-project.org\/an-introduction-to-hydraulic-testing-in-hydrogeology\/chapter\/hantush%E2%80%91jacob-solution-leaky-confined%E2%80%91no-water-released-from-aquitard-storage\/#Xcbc9563b5d554d8f186baa4c7fb85f0e5456dd9\">(53)<\/a>.<\/p><\/blockquote>\n<\/div>\n<div data-custom-style=\"Block Text\">\n<div class=\"display-math\" data-custom-style=\"Display Equation\">\n<p>[latex]S = \\frac{4\\ \\left( 212\\ \\frac{m^{2}}{d} \\right)\\ 0.011d}{2\\ (75\\ m)\\ (203\\ m)} = 0.0003\\ = \\ 3x10^{- 4}[\/latex]<\/p>\n<\/div>\n<\/div>\n<div data-custom-style=\"Block Text\">\n<blockquote><p>In addition the calculation of K\u2019 was changed from the following as shown in gray:<\/p><\/blockquote>\n<\/div>\n<div data-custom-style=\"First Paragraph\">\n<div class=\"display-math\" data-custom-style=\"Display Equation\">\n<p>[latex]K' = \\frac{31.1\\frac{m^{2}}{d}\\ 15\\ m}{(44.1m)^{2}} = 0.24\\frac{m}{d}[\/latex]<\/p>\n<\/div>\n<\/div>\n<div data-custom-style=\"Block Text\">\n<blockquote><p>to:<\/p><\/blockquote>\n<\/div>\n<div data-custom-style=\"First Paragraph\">\n<div class=\"display-math\" data-custom-style=\"Display Equation\">\n<p>[latex]K' = \\frac{212\\frac{m^{2}}{d}\\ 15\\ m}{(203\\ m)^{2}} = 0.08\\frac{m}{d}[\/latex]<\/p>\n<\/div>\n<\/div>\n<div data-custom-style=\"Body Text\">\n<p>page 351, corrected format for Author\u2019s name and title<\/p>\n<\/div>\n","protected":false},"parent":0,"menu_order":27,"template":"","meta":{"pb_part_invisible":false,"pb_part_invisible_string":""},"contributor":[],"license":[],"class_list":["post-609","part","type-part","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/books.gw-project.org\/an-introduction-to-hydraulic-testing-in-hydrogeology\/wp-json\/pressbooks\/v2\/parts\/609","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/books.gw-project.org\/an-introduction-to-hydraulic-testing-in-hydrogeology\/wp-json\/pressbooks\/v2\/parts"}],"about":[{"href":"https:\/\/books.gw-project.org\/an-introduction-to-hydraulic-testing-in-hydrogeology\/wp-json\/wp\/v2\/types\/part"}],"version-history":[{"count":9,"href":"https:\/\/books.gw-project.org\/an-introduction-to-hydraulic-testing-in-hydrogeology\/wp-json\/pressbooks\/v2\/parts\/609\/revisions"}],"predecessor-version":[{"id":4159,"href":"https:\/\/books.gw-project.org\/an-introduction-to-hydraulic-testing-in-hydrogeology\/wp-json\/pressbooks\/v2\/parts\/609\/revisions\/4159"}],"wp:attachment":[{"href":"https:\/\/books.gw-project.org\/an-introduction-to-hydraulic-testing-in-hydrogeology\/wp-json\/wp\/v2\/media?parent=609"}],"wp:term":[{"taxonomy":"contributor","embeddable":true,"href":"https:\/\/books.gw-project.org\/an-introduction-to-hydraulic-testing-in-hydrogeology\/wp-json\/wp\/v2\/contributor?post=609"},{"taxonomy":"license","embeddable":true,"href":"https:\/\/books.gw-project.org\/an-introduction-to-hydraulic-testing-in-hydrogeology\/wp-json\/wp\/v2\/license?post=609"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}