Variation in Saturated Hydraulic Conductivity at the Outcrop Scale, the Whanganui Basin, New Zealand-Reference-Cited by-同舟云学术

Variation in Saturated Hydraulic Conductivity at the Outcrop Scale, the Whanganui Basin, New Zealand

Published:2019-11-30 Issue:4 Volume:58 Page:622-637
ISSN:0017-467X
Container-title:Groundwater
language:en
Short-container-title:Groundwater

Author:

Rees Callum¹^ORCID,Palmer Alan²,Palmer Julie²,Singh Ranvir²

Affiliation:

1. Vision Consulting Engineers and Planners Kerikeri Northland New Zealand 0230

2. Environmental Sciences, School of Agriculture and EnvironmentMassey University Palmerston North New Zealand 4442

Publisher

Wiley

Subject

Computers in Earth Sciences,Water Science and Technology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/gwat.12948

Reference40 articles.

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2. Abbott S.T.1994. Sequence stratigraphy sedimentology and paleoecology of Pleistocene cyclothems in the Castlecliff Section Wanganui Basin New Zealand. Unpublished PhD thesis James Cook University of Northern Queensland Australia. 297 p.

3. Begg J.G. A.Palmer M.Gyopari.2005. Geological synopsis of the Manawatu‐Horowhenua area for a review of the region's hydrogeology. Institue of Geological and Nucelar Sciences Client Report 2005/172. 22 p.

4. Effects of sedimentary heterogeneity on groundwater flow in a Quaternary pro-glacial delta environment: joining facies analysis and numerical modelling

5. Cenozoic Mollusca of New Zealand;Beu A.G.;New Zealand Geological Survey Paleontological Bulletin,1990

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