{"id":107,"date":"2019-11-27T15:36:10","date_gmt":"2019-11-27T15:36:10","guid":{"rendered":"http:\/\/aquifer.geology.buffalo.edu\/?p=107"},"modified":"2019-11-28T02:57:13","modified_gmt":"2019-11-28T02:57:13","slug":"image-well-and-max-pumping-rate","status":"publish","type":"post","link":"https:\/\/aquifer.geology.buffalo.edu\/index.php\/2019\/11\/27\/image-well-and-max-pumping-rate\/","title":{"rendered":"Image well and max pumping rate"},"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\/ImageWell_contant_Head-1024x1024.jpg\" alt=\"\" class=\"wp-image-174\" srcset=\"https:\/\/aquifer.geology.buffalo.edu\/wp-content\/uploads\/2019\/11\/ImageWell_contant_Head-1024x1024.jpg 1024w, https:\/\/aquifer.geology.buffalo.edu\/wp-content\/uploads\/2019\/11\/ImageWell_contant_Head-150x150.jpg 150w, https:\/\/aquifer.geology.buffalo.edu\/wp-content\/uploads\/2019\/11\/ImageWell_contant_Head-300x300.jpg 300w, https:\/\/aquifer.geology.buffalo.edu\/wp-content\/uploads\/2019\/11\/ImageWell_contant_Head-768x768.jpg 768w\" sizes=\"auto, (max-width: 767px) 89vw, (max-width: 1000px) 54vw, (max-width: 1071px) 543px, 580px\" \/><\/figure>\n\n\n\n<p>\nObjectives: Determine the maximum pumping rate on a well\npossible without drawing water from a lake or wetland. \n\n<br>\n\n1. There are times that you need to determine the maximum\npumping rate in a well that can be used without extracting water from a nearby\nlake or wetland.&nbsp; This is a classic image\nwell problem.&nbsp; The foldable aquifer model\nthat is provided in the problem below asks you to solve this exact style of problem.&nbsp; Before pumping there is a gradient across the\nconfined aquifer that shows water is flowing toward the lake.&nbsp; Use the foldable aquifer model provided to answer\nthe following question \n\n<br><br>\n\nA. Determine the maximum pumping rate at the well that is\npossible without drawing water from the lake.&nbsp;&nbsp;\n\n<\/p>\n\n\n\n<figure class=\"wp-block-image\"><img loading=\"lazy\" decoding=\"async\" width=\"745\" height=\"414\" src=\"http:\/\/aquifer.geology.buffalo.edu\/wp-content\/uploads\/2019\/11\/Image-Well-Constant-Head-BC-and-Gradient.png\" alt=\"\" class=\"wp-image-113\" srcset=\"https:\/\/aquifer.geology.buffalo.edu\/wp-content\/uploads\/2019\/11\/Image-Well-Constant-Head-BC-and-Gradient.png 745w, https:\/\/aquifer.geology.buffalo.edu\/wp-content\/uploads\/2019\/11\/Image-Well-Constant-Head-BC-and-Gradient-300x167.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\/Image-Well-Constant-Head-BC-and-Gradient.pdf\">Foldable Aquifer Model<\/a><a href=\"http:\/\/aquifer.geology.buffalo.edu\/wp-content\/uploads\/2019\/11\/Image-Well-Constant-Head-BC-and-Gradient.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: Determine the maximum pumping rate on a well possible without drawing water from a lake or wetland. 1. There are times that you need to determine the maximum pumping rate in a well that can be used without extracting water from a nearby lake or wetland.&nbsp; This is a classic image well problem.&nbsp; The &hellip; <\/p>\n<p class=\"link-more\"><a href=\"https:\/\/aquifer.geology.buffalo.edu\/index.php\/2019\/11\/27\/image-well-and-max-pumping-rate\/\" class=\"more-link\">Continue reading<span class=\"screen-reader-text\"> &#8220;Image well and max pumping rate&#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":[4,13],"tags":[],"class_list":["post-107","post","type-post","status-publish","format-standard","hentry","category-image-wells","category-well-hydraulics"],"_links":{"self":[{"href":"https:\/\/aquifer.geology.buffalo.edu\/index.php\/wp-json\/wp\/v2\/posts\/107","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=107"}],"version-history":[{"count":5,"href":"https:\/\/aquifer.geology.buffalo.edu\/index.php\/wp-json\/wp\/v2\/posts\/107\/revisions"}],"predecessor-version":[{"id":272,"href":"https:\/\/aquifer.geology.buffalo.edu\/index.php\/wp-json\/wp\/v2\/posts\/107\/revisions\/272"}],"wp:attachment":[{"href":"https:\/\/aquifer.geology.buffalo.edu\/index.php\/wp-json\/wp\/v2\/media?parent=107"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/aquifer.geology.buffalo.edu\/index.php\/wp-json\/wp\/v2\/categories?post=107"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/aquifer.geology.buffalo.edu\/index.php\/wp-json\/wp\/v2\/tags?post=107"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}