Skip navigation
  • Home
  • Browse
    • Communities
      & Collections
    • Browse Items by:
    • Publication Date
    • Author
    • Title
    • Subject
    • Department
  • Sign on to:
    • My MacSphere
    • Receive email
      updates
    • Edit Profile


McMaster University Home Page
  1. MacSphere
  2. Open Access Dissertations and Theses Community
  3. Open Access Dissertations and Theses
Please use this identifier to cite or link to this item: http://hdl.handle.net/11375/8960
Full metadata record
DC FieldValueLanguage
dc.contributor.advisorSmith, James E.en_US
dc.contributor.authorBeatty, MB Sarahen_US
dc.date.accessioned2014-06-18T16:44:50Z-
dc.date.available2014-06-18T16:44:50Z-
dc.date.created2011-05-19en_US
dc.date.issued2009en_US
dc.identifier.otheropendissertations/4125en_US
dc.identifier.other5144en_US
dc.identifier.other2020670en_US
dc.identifier.urihttp://hdl.handle.net/11375/8960-
dc.description.abstract<p>Soil water repellency is a spatially and temporally variable near surface phenomenon most often associated with reduced or impeded infiltration into porous media. In recent years, soil water repellency (hydrophobicity) has garnered much attention in the literature due to its detrimental effects on soil water processes and its widespread observance allover the world in both rural and urban settings. While previous work has developed our understanding of these inherently complex systems, insight into their dynamic and variable nature is still lacking. Having utilized existing technologies in a new way, in this study we present a series of systematic field and laboratory based investigations that clarify the roles of fractional wetting and contact angle dynamics on soil water processes using hydrophobic materials found at a wildfire site approximately 1.5 years post-fire. The robust and fundamental approach taken in investigating<br />water repellency in these materials provided the foundation to develop two conceptual models based on our observations and with respect to existing and emerging theory. These models better explain soil water behaviour in hydrophobic systems than is currently afforded by the literature. We found that wetting and infiltration processes are contingent upon the functional relationship between wettable fractions of materials and the rate of contact angle change in non-wettable fractions.</p>en_US
dc.subjectEarth and Environmental Sciencesen_US
dc.subjectOther Environmental Sciencesen_US
dc.subjectOther Environmental Sciencesen_US
dc.titleTHE HYDROLOGICAL EFFECTS OF FRACTIONAL WETTABILITY AND CONTACT ANGLE DYNAMICS IN WATER REPELLENT POROUS MEDIAen_US
dc.typethesisen_US
dc.contributor.departmentEarth and Environmental Sciencesen_US
dc.description.degreeMaster of Science (MS)en_US
Appears in Collections:Open Access Dissertations and Theses

Files in This Item:
File SizeFormat 
fulltext.pdf
Open Access
72.75 MBAdobe PDFView/Open
Show simple item record Statistics


Items in MacSphere are protected by copyright, with all rights reserved, unless otherwise indicated.

Sherman Centre for Digital Scholarship     McMaster University Libraries
©2022 McMaster University, 1280 Main Street West, Hamilton, Ontario L8S 4L8 | 905-525-9140 | Contact Us | Terms of Use & Privacy Policy | Feedback

Report Accessibility Issue