{"id":99,"date":"2019-11-27T15:32:56","date_gmt":"2019-11-27T15:32:56","guid":{"rendered":"http:\/\/aquifer.geology.buffalo.edu\/?p=99"},"modified":"2022-10-18T21:06:07","modified_gmt":"2022-10-18T21:06:07","slug":"quantifying-hydraulic-conductivity-slug-test","status":"publish","type":"post","link":"https:\/\/aquifer.geology.buffalo.edu\/index.php\/2019\/11\/27\/quantifying-hydraulic-conductivity-slug-test\/","title":{"rendered":"Quantifying Hydraulic Conductivity: Slug Test"},"content":{"rendered":"\n<figure class=\"wp-block-image\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"1024\" src=\"http:\/\/aquifer.geology.buffalo.edu\/wp-content\/uploads\/2019\/11\/SlugTest-1024x1024.jpg\" alt=\"\" class=\"wp-image-177\" srcset=\"https:\/\/aquifer.geology.buffalo.edu\/wp-content\/uploads\/2019\/11\/SlugTest-1024x1024.jpg 1024w, https:\/\/aquifer.geology.buffalo.edu\/wp-content\/uploads\/2019\/11\/SlugTest-150x150.jpg 150w, https:\/\/aquifer.geology.buffalo.edu\/wp-content\/uploads\/2019\/11\/SlugTest-300x300.jpg 300w, https:\/\/aquifer.geology.buffalo.edu\/wp-content\/uploads\/2019\/11\/SlugTest-768x768.jpg 768w\" sizes=\"auto, (max-width: 767px) 89vw, (max-width: 1000px) 54vw, (max-width: 1071px) 543px, 580px\" \/><\/figure>\n\n\n\n<p>Objectives: Quantify hydraulic conductivity in an unconfined\naquifer based on slug test data of changes in water levels over time. <\/p>\n\n\n\n<p>1.&nbsp; The biggest\nunknown in groundwater problems is knowing the hydraulic conductivity of an\naquifer.&nbsp; While there are multiple\nmethods available for quantifying hydraulic conductivity one of the most\npopular methods is the slug test.&nbsp; This\nmethod artificially changes the water level in a well and monitors the response\nback to the static level.&nbsp; Using the data\nprovided below and foldable aquifer model address the following problems.<\/p>\n\n\n\n<p>Table1. Time vs drawdown data.<\/p>\n\n\n\n<figure class=\"wp-block-table\"><table class=\"\"><tbody><tr><td>\n  <strong>Time\n  (sec)<\/strong>\n  <\/td><td>\n  <strong>H-h\/(H-H<\/strong><strong>o<\/strong><strong>)<\/strong>\n  <\/td><\/tr><tr><td>\n  <strong>1<\/strong>\n  <\/td><td>\n  1\n  <\/td><\/tr><tr><td>\n  <strong>10<\/strong>\n  <\/td><td>\n  0.89\n  <\/td><\/tr><tr><td>\n  <strong>20<\/strong>\n  <\/td><td>\n  0.75\n  <\/td><\/tr><tr><td>\n  <strong>30<\/strong>\n  <\/td><td>\n  0.64\n  <\/td><\/tr><tr><td>\n  <strong>50<\/strong>\n  <\/td><td>\n  0.3\n  <\/td><\/tr><tr><td>\n  <strong>100<\/strong>\n  <\/td><td>\n  0.28\n  <\/td><\/tr><tr><td>\n  <strong>120<\/strong>\n  <\/td><td>\n  0.2\n  <\/td><\/tr><tr><td>\n  <strong>180<\/strong>\n  <\/td><td>\n  0.08\n  <\/td><\/tr><tr><td>\n  <strong>200<\/strong>\n  <\/td><td>\n  0.05\n  <\/td><\/tr><tr><td>\n  <strong>300<\/strong>\n  <\/td><td>\n  0.02\n  <\/td><\/tr><\/tbody><\/table><\/figure>\n\n\n\n<p>A. Quantify the hydraulic conductivity using the Hvorslev method. &nbsp;&nbsp;<\/p>\n\n\n\n<p>B. Based on the value of hydraulic conductivity above determine\nif this geologic unit makes a better aquifer or confining unit.&nbsp;&nbsp; Please explain your answer. <\/p>\n\n\n\n<figure class=\"wp-block-image\"><img loading=\"lazy\" decoding=\"async\" width=\"759\" height=\"477\" src=\"http:\/\/aquifer.geology.buffalo.edu\/wp-content\/uploads\/2019\/11\/Hevorslev-Slug-Test-Well.png\" alt=\"\" class=\"wp-image-121\" srcset=\"https:\/\/aquifer.geology.buffalo.edu\/wp-content\/uploads\/2019\/11\/Hevorslev-Slug-Test-Well.png 759w, https:\/\/aquifer.geology.buffalo.edu\/wp-content\/uploads\/2019\/11\/Hevorslev-Slug-Test-Well-300x189.png 300w\" sizes=\"auto, (max-width: 706px) 89vw, (max-width: 767px) 82vw, 740px\" \/><\/figure>\n\n\n\n<div class=\"wp-block-file\"><a href=\"http:\/\/aquifer.geology.buffalo.edu\/wp-content\/uploads\/2019\/11\/Hevorslev-Slug-Test-Well.pdf\">Foldable Aquifer Model<\/a><a href=\"http:\/\/aquifer.geology.buffalo.edu\/wp-content\/uploads\/2019\/11\/Hevorslev-Slug-Test-Well.pdf\" class=\"wp-block-file__button\" download>Download<\/a><\/div>\n\n\n\n<div class=\"wp-block-file\"><a href=\"http:\/\/aquifer.geology.buffalo.edu\/wp-content\/uploads\/2022\/10\/Full-Class-Problem.pdf\"><br>Below is a second class problem (PDF)<br>Slug Test Class Problem II<br><\/a><a href=\"http:\/\/aquifer.geology.buffalo.edu\/wp-content\/uploads\/2022\/10\/Full-Class-Problem.pdf\" class=\"wp-block-file__button\" download>Download<\/a><\/div>\n\n\n\n<figure class=\"wp-block-image\"><a href=\"http:\/\/creativecommons.org\/licenses\/by-nc\/4.0\/\"><img decoding=\"async\" src=\"https:\/\/i.creativecommons.org\/l\/by-nc\/4.0\/88x31.png\" alt=\"Creative Commons License\"\/><\/a><\/figure>\n\n\n\n<p><br>This work is licensed under a <a href=\"http:\/\/creativecommons.org\/licenses\/by-nc\/4.0\/\">Creative Commons Attribution-NonCommercial 4.0 International License<\/a>.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Objectives: Quantify hydraulic conductivity in an unconfined aquifer based on slug test data of changes in water levels over time. 1.&nbsp; The biggest unknown in groundwater problems is knowing the hydraulic conductivity of an aquifer.&nbsp; While there are multiple methods available for quantifying hydraulic conductivity one of the most popular methods is the slug test.&nbsp; &hellip; <\/p>\n<p class=\"link-more\"><a href=\"https:\/\/aquifer.geology.buffalo.edu\/index.php\/2019\/11\/27\/quantifying-hydraulic-conductivity-slug-test\/\" class=\"more-link\">Continue reading<span class=\"screen-reader-text\"> &#8220;Quantifying Hydraulic Conductivity: Slug Test&#8221;<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[12,11],"tags":[],"class_list":["post-99","post","type-post","status-publish","format-standard","hentry","category-hydraulic-conductivity","category-hydraulic-head"],"_links":{"self":[{"href":"https:\/\/aquifer.geology.buffalo.edu\/index.php\/wp-json\/wp\/v2\/posts\/99","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/aquifer.geology.buffalo.edu\/index.php\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/aquifer.geology.buffalo.edu\/index.php\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/aquifer.geology.buffalo.edu\/index.php\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/aquifer.geology.buffalo.edu\/index.php\/wp-json\/wp\/v2\/comments?post=99"}],"version-history":[{"count":8,"href":"https:\/\/aquifer.geology.buffalo.edu\/index.php\/wp-json\/wp\/v2\/posts\/99\/revisions"}],"predecessor-version":[{"id":364,"href":"https:\/\/aquifer.geology.buffalo.edu\/index.php\/wp-json\/wp\/v2\/posts\/99\/revisions\/364"}],"wp:attachment":[{"href":"https:\/\/aquifer.geology.buffalo.edu\/index.php\/wp-json\/wp\/v2\/media?parent=99"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/aquifer.geology.buffalo.edu\/index.php\/wp-json\/wp\/v2\/categories?post=99"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/aquifer.geology.buffalo.edu\/index.php\/wp-json\/wp\/v2\/tags?post=99"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}