

{"id":578,"date":"2016-07-29T14:39:44","date_gmt":"2016-07-29T18:39:44","guid":{"rendered":"https:\/\/sites.temple.edu\/geophysics\/?p=578"},"modified":"2016-07-29T14:46:22","modified_gmt":"2016-07-29T18:46:22","slug":"more-fun-with-thermal-images","status":"publish","type":"post","link":"https:\/\/sites.temple.edu\/geophysics\/2016\/07\/29\/more-fun-with-thermal-images\/","title":{"rendered":"More fun with thermal images!"},"content":{"rendered":"<p>In collaboration with researchers at Penn State, I been experimenting with using thermal imaging to detect preferential flow in the shallow subsurface. \u00a0The basic idea is to cut a trench upslope and infiltrate ice-water, then monitor the face of a second trench downslope to look for temperature changes. \u00a0Obviously, you do not need a thermal camera to see water emerge (left image) under dry conditions, but we hope to show the thermal approach will work when the ground is already near saturation from previous rains to see if the preferential flow changes with preexisting moisture levels.<\/p>\n<div id=\"attachment_580\" style=\"width: 179px\" class=\"wp-caption alignleft\"><a href=\"https:\/\/sites.temple.edu\/geophysics\/files\/2016\/07\/20160720_105820-e1469817407539.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-580\" class=\"size-medium wp-image-580\" src=\"https:\/\/sites.temple.edu\/geophysics\/files\/2016\/07\/20160720_105820-e1469817407539-169x300.jpg\" alt=\"Experimental setup.\" width=\"169\" height=\"300\" srcset=\"https:\/\/sites.temple.edu\/geophysics\/files\/2016\/07\/20160720_105820-e1469817407539-169x300.jpg 169w, https:\/\/sites.temple.edu\/geophysics\/files\/2016\/07\/20160720_105820-e1469817407539-768x1365.jpg 768w, https:\/\/sites.temple.edu\/geophysics\/files\/2016\/07\/20160720_105820-e1469817407539-576x1024.jpg 576w\" sizes=\"auto, (max-width: 169px) 100vw, 169px\" \/><\/a><p id=\"caption-attachment-580\" class=\"wp-caption-text\">Experimental setup with infiltration trench close to soil pit. (Notice damp areas)<\/p><\/div>\n<div id=\"attachment_579\" style=\"width: 310px\" class=\"wp-caption alignright\"><a href=\"https:\/\/sites.temple.edu\/geophysics\/files\/2016\/07\/FLIR0410.jpg\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-579\" class=\"size-medium wp-image-579\" src=\"https:\/\/sites.temple.edu\/geophysics\/files\/2016\/07\/FLIR0410-300x225.jpg\" alt=\"Preferential flow detected by thermal imagery\" width=\"300\" height=\"225\" srcset=\"https:\/\/sites.temple.edu\/geophysics\/files\/2016\/07\/FLIR0410-300x225.jpg 300w, https:\/\/sites.temple.edu\/geophysics\/files\/2016\/07\/FLIR0410.jpg 320w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><p id=\"caption-attachment-579\" class=\"wp-caption-text\">Thermal image of soil trench face at Garner Run near PSU showing cold water (black) emerging along the trench face having follow preferential flow paths in the shallow unsaturated zone. \u00a0<\/p><\/div>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>In collaboration with researchers at Penn State, I been experimenting with using thermal imaging to detect preferential flow in the shallow subsurface. \u00a0The basic idea is to cut a trench upslope and infiltrate ice-water, then monitor the face of a &hellip; <a href=\"https:\/\/sites.temple.edu\/geophysics\/2016\/07\/29\/more-fun-with-thermal-images\/\">Continue reading <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":606,"featured_media":0,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[],"class_list":["post-578","post","type-post","status-publish","format-standard","hentry","category-uncategorized"],"_links":{"self":[{"href":"https:\/\/sites.temple.edu\/geophysics\/wp-json\/wp\/v2\/posts\/578","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/sites.temple.edu\/geophysics\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/sites.temple.edu\/geophysics\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/sites.temple.edu\/geophysics\/wp-json\/wp\/v2\/users\/606"}],"replies":[{"embeddable":true,"href":"https:\/\/sites.temple.edu\/geophysics\/wp-json\/wp\/v2\/comments?post=578"}],"version-history":[{"count":0,"href":"https:\/\/sites.temple.edu\/geophysics\/wp-json\/wp\/v2\/posts\/578\/revisions"}],"wp:attachment":[{"href":"https:\/\/sites.temple.edu\/geophysics\/wp-json\/wp\/v2\/media?parent=578"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/sites.temple.edu\/geophysics\/wp-json\/wp\/v2\/categories?post=578"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/sites.temple.edu\/geophysics\/wp-json\/wp\/v2\/tags?post=578"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}