P
Paul W. Williams
Researcher at University of Auckland
Publications - 43
Citations - 5932
Paul W. Williams is an academic researcher from University of Auckland. The author has contributed to research in topics: Karst & Cave. The author has an hindex of 20, co-authored 43 publications receiving 5592 citations. Previous affiliations of Paul W. Williams include University College Dublin.
Papers
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Book
Karst Hydrogeology and Geomorphology
Derek C. Ford,Paul W. Williams +1 more
TL;DR: In this article, the authors discuss the relationship between Karst and general geomorphology and Hydrogeology and discuss the development of Karst underground systems, and present a detailed analysis of these systems.
Book
Karst Geomorphology and Hydrology
Derek C. Ford,Paul W. Williams +1 more
TL;DR: In this paper, the influence of climate, climatic change and other environmental factors on karst development is discussed. And the authors present a detailed analysis of the chemical and kinetic behavior of the kars.
Journal ArticleDOI
The role of the subcutaneous zone in karst hydrology
TL;DR: The subcutaneous zone is the upper weathered layer of rock beneath the soil, but above the permanently saturated (phreatic) zone as discussed by the authors, which is of particular hydrological importance in karst because of its high secondary permeability, arising from the considerable chemical solution in this zone.
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Towards a climate event stratigraphy for New Zealand over the past 30 000 years (NZ‐INTIMATE project)
Brent V. Alloway,David J. Lowe,David J.A. Barrell,Rewi M. Newnham,Peter C. Almond,Paul Augustinus,Nancy A. N. Bertler,Lionel Carter,Nicola Litchfield,Matt S. McGlone,Jamie Shulmeister,Marcus J. Vandergoes,Paul W. Williams,Nz-Intimate members +13 more
TL;DR: The New Zealand Intimate project as mentioned in this paper has developed an event stratigraphy for the New Zealand region over the past 30 000 years, and to reconcile these events against the established climatostratigraphy of the last glacial cycle which has largely been developed from Northern Hemisphere records.
Journal ArticleDOI
The role of the epikarst in karst and cave hydrogeology: a review
TL;DR: The epikarst or subcutaneous zone is located at the top of the aerated or vadose zone in carbonate rocks, and water percolates downwards through a zone dominated by transmission rather than storage that delivers recharge to the saturated or phreatic zone as discussed by the authors.