

{"id":83,"date":"2015-05-24T18:17:46","date_gmt":"2015-05-24T22:17:46","guid":{"rendered":"https:\/\/sites.temple.edu\/geotoran\/?page_id=83"},"modified":"2022-08-26T16:24:04","modified_gmt":"2022-08-26T20:24:04","slug":"infiltration-studies-using-hydrogeophysics-czos","status":"publish","type":"page","link":"https:\/\/sites.temple.edu\/geotoran\/research\/infiltration-studies-using-hydrogeophysics-czos\/","title":{"rendered":"Infiltration studies and hydrogeophysics"},"content":{"rendered":"<p>Groundwater recharge is difficult to measure and the role of macropores is not well-understood. We are exploring use of geophysical techniques to map infiltration in natural settings at the NSF-funded Critical Zone Observatories (CZOs) and Critical Zone Network Philadelphia Urban site.<\/p>\n<p>See also the <a href=\"https:\/\/sites.temple.edu\/geotoran\/research\/groundwater-surface-water-interaction\/\">Groundwater-surface water tab<\/a> for other hydrogeophysical studies<\/p>\n<p>RECENT FUNDING: National Science Foundation, Urban Critical Zone processes along the Piedmont-Coastal Plain transition. 2020-2025<\/p>\n<p>PAST FUNDING:\u00a0\u00a0 We received subcontracts and seed grants from Penn State University to work on their National Science Foundation-funded CZO. We also were granted access to the Christiana River CZO to conduct studies on their site.<\/p>\n<table>\n<tbody>\n<tr>\n<td width=\"160\"><a href=\"https:\/\/sites.temple.edu\/geotoran\/files\/2015\/05\/survey_tent.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone wp-image-160\" src=\"https:\/\/sites.temple.edu\/geotoran\/files\/2015\/05\/survey_tent-300x223.jpg\" alt=\"survey_tent\" width=\"247\" height=\"183\" srcset=\"https:\/\/sites.temple.edu\/geotoran\/files\/2015\/05\/survey_tent-300x223.jpg 300w, https:\/\/sites.temple.edu\/geotoran\/files\/2015\/05\/survey_tent.jpg 482w\" sizes=\"auto, (max-width: 247px) 100vw, 247px\" \/><\/a>Resistivity survey in the rain<\/td>\n<td width=\"160\"><a href=\"https:\/\/sites.temple.edu\/geotoran\/files\/2015\/05\/infiltrometer_CRB.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone wp-image-162\" src=\"https:\/\/sites.temple.edu\/geotoran\/files\/2015\/05\/infiltrometer_CRB-225x300.jpg\" alt=\"infiltrometer_CRB\" width=\"177\" height=\"236\" srcset=\"https:\/\/sites.temple.edu\/geotoran\/files\/2015\/05\/infiltrometer_CRB-225x300.jpg 225w, https:\/\/sites.temple.edu\/geotoran\/files\/2015\/05\/infiltrometer_CRB.jpg 350w\" sizes=\"auto, (max-width: 177px) 100vw, 177px\" \/><\/a><\/p>\n<p>Soil infiltrometer<\/td>\n<td width=\"160\"><a href=\"https:\/\/sites.temple.edu\/geotoran\/files\/2015\/05\/bedrock_fracs.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone wp-image-156\" src=\"https:\/\/sites.temple.edu\/geotoran\/files\/2015\/05\/bedrock_fracs-300x225.jpg\" alt=\"bedrock_fracs\" width=\"258\" height=\"194\" srcset=\"https:\/\/sites.temple.edu\/geotoran\/files\/2015\/05\/bedrock_fracs-300x225.jpg 300w, https:\/\/sites.temple.edu\/geotoran\/files\/2015\/05\/bedrock_fracs.jpg 727w\" sizes=\"auto, (max-width: 258px) 100vw, 258px\" \/><\/a>Bedrock fractures<\/td>\n<\/tr>\n<tr>\n<td width=\"160\"><a href=\"https:\/\/sites.temple.edu\/geotoran\/files\/2015\/05\/gpr_survey.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone wp-image-158\" src=\"https:\/\/sites.temple.edu\/geotoran\/files\/2015\/05\/gpr_survey-300x211.jpg\" alt=\"gpr_survey\" width=\"261\" height=\"184\" srcset=\"https:\/\/sites.temple.edu\/geotoran\/files\/2015\/05\/gpr_survey-300x211.jpg 300w, https:\/\/sites.temple.edu\/geotoran\/files\/2015\/05\/gpr_survey.jpg 405w\" sizes=\"auto, (max-width: 261px) 100vw, 261px\" \/><\/a>GPR survey<\/td>\n<td width=\"160\"><a href=\"https:\/\/sites.temple.edu\/geotoran\/files\/2015\/05\/excavation.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone wp-image-157\" src=\"https:\/\/sites.temple.edu\/geotoran\/files\/2015\/05\/excavation-300x225.jpg\" alt=\"excavation\" width=\"235\" height=\"176\" srcset=\"https:\/\/sites.temple.edu\/geotoran\/files\/2015\/05\/excavation-300x225.jpg 300w, https:\/\/sites.temple.edu\/geotoran\/files\/2015\/05\/excavation.jpg 642w\" sizes=\"auto, (max-width: 235px) 100vw, 235px\" \/><\/a>Trench excavation<\/td>\n<td width=\"160\"><a href=\"https:\/\/sites.temple.edu\/geotoran\/files\/2015\/05\/shale_dye.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-medium wp-image-159\" src=\"https:\/\/sites.temple.edu\/geotoran\/files\/2015\/05\/shale_dye-300x225.jpg\" alt=\"shale_dye\" width=\"300\" height=\"225\" srcset=\"https:\/\/sites.temple.edu\/geotoran\/files\/2015\/05\/shale_dye-300x225.jpg 300w, https:\/\/sites.temple.edu\/geotoran\/files\/2015\/05\/shale_dye.jpg 642w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a>Dye trace in soil<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<p>PUBLICATION<\/p>\n<p>Nyquist, J. E., Toran, L., Pitman, L., Guo, L., &amp; Lin, H. (2018). Testing the fill-and-spill model of subsurface lateral flow using ground-penetrating radar and dye tracing. Vadose Zone Journal, 17(1). <a href=\"https:\/\/sites.temple.edu\/geotoran\/files\/2018\/09\/Nyquistetal_VZJ_2018.pdf\" target=\"_blank\" rel=\"noopener\">pdf<\/a><\/p>\n<p>THESES\/PRESENTATIONS<\/p>\n<p>Milinic, B. 2022. Evaluation of bedrock depth and soil infiltration along Pennypack Creek using electrical resistivity tomography and soil moisture loggers. Unpublished master\u2019s thesis, Temple University., 113 pp.<\/p>\n<p>Pitman, L. 2014. Ground-penetrating radar images of a dye tracer test within the unsaturated zone at the Susquehanna-Shale Hills CZO. Unpublished master\u2019s thesis, Temple University, 182 pp.<\/p>\n<p>Schlosser, K. 2017.\u00a0 Monitoring infiltration from natural storms using time-lapse electrical resistivity tomography.<\/p>\n<p>Pitman, L., Nyquist, J.E., Toran, L., Lin, H., 2014. Ground-penetrating radar images hydrogeological processes within the unsaturated zone at the Susquehanna-Shale Hills CZO. 49th Annual Meeting of the Northeastern Section of the Geological Society of America, March 23-25, Lancaster, PA.<\/p>\n<p>Schlosser, K., Toran, L., Nyquist, J., and Sawyer, A. 2013. A geophysical field investigation of infiltration during rain events in the riparian zone. Geological Society of American Annual Meeting, Denver, CO, October 27-30. Abstracts with Programs. Vol. 45, p 263.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Groundwater recharge is difficult to measure and the role of macropores is not well-understood. We are exploring use of geophysical techniques to map infiltration in natural settings at the NSF-funded Critical Zone Observatories (CZOs) and Critical Zone Network Philadelphia Urban &hellip; <a href=\"https:\/\/sites.temple.edu\/geotoran\/research\/infiltration-studies-using-hydrogeophysics-czos\/\">Continue reading <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":4114,"featured_media":0,"parent":61,"menu_order":4,"comment_status":"open","ping_status":"closed","template":"onecolumn-page.php","meta":{"footnotes":""},"class_list":["post-83","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/sites.temple.edu\/geotoran\/wp-json\/wp\/v2\/pages\/83","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/sites.temple.edu\/geotoran\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/sites.temple.edu\/geotoran\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/sites.temple.edu\/geotoran\/wp-json\/wp\/v2\/users\/4114"}],"replies":[{"embeddable":true,"href":"https:\/\/sites.temple.edu\/geotoran\/wp-json\/wp\/v2\/comments?post=83"}],"version-history":[{"count":0,"href":"https:\/\/sites.temple.edu\/geotoran\/wp-json\/wp\/v2\/pages\/83\/revisions"}],"up":[{"embeddable":true,"href":"https:\/\/sites.temple.edu\/geotoran\/wp-json\/wp\/v2\/pages\/61"}],"wp:attachment":[{"href":"https:\/\/sites.temple.edu\/geotoran\/wp-json\/wp\/v2\/media?parent=83"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}