Research Commons
      • Browse 
        • Communities & Collections
        • Titles
        • Authors
        • By Issue Date
        • Subjects
        • Types
        • Series
      • Help 
        • About
        • Collection Policy
        • OA Mandate Guidelines
        • Guidelines FAQ
        • Contact Us
      • My Account 
        • Sign In
        • Register
      View Item 
      •   Research Commons
      • University of Waikato Research
      • Science and Engineering
      • Science and Engineering Papers
      • View Item
      •   Research Commons
      • University of Waikato Research
      • Science and Engineering
      • Science and Engineering Papers
      • View Item
      JavaScript is disabled for your browser. Some features of this site may not work without it.

      Impacts of conversion from forestry to pasture on soil physical properties of Vitrands (Pumice Soils) in central North Island, New Zealand

      Paripovich, D; Balks, Megan R.; Schipper, Louis A.; Lowe, David J.
      Thumbnail
      Files
      Paripovich et al. 2010 Proceed WSC.pdf
      Published version, 549.6Kb
      Find in your library  
      Citation
      Export citation
      Paripovich, D., Balks, M. R., Schipper, L. A., & Lowe, D. J. (2010). Impacts of conversion from forestry to pasture on soil physical properties of Vitrands (Pumice Soils) in central North Island, New Zealand. In R. J. Gilkes & N. Prakongkep (Eds.), Proceedings of the 19th World Congress of Soil Science: Soil solutions for a changing world (pp. 52–54). Australia.
      Permanent Research Commons link: https://hdl.handle.net/10289/10222
      Abstract
      Tens of thousands of hectares of land have been converted from plantation forest to pasture in the central North Island of New Zealand between 2000 and 2010. The land use change was driven by the perceived better long term returns from dairy farming compared with forestry. Pumice Soils (NZ Soil Classification, equivalent to Vitrands in Soil Taxonomy) in the central North Island are formed on pumice deposited mainly from the AD 232 ± 5 Taupo volcanic eruption. The texture of Pumice Soils (Figure 1) varies from silt to coarse gravel and they have weak structure and erode easily when disturbed. Water holding capacity may be low but increases as the organic matter content of the topsoil is built up.
      Date
      2010-08-01
      Type
      Conference Contribution
      Supervisors
      Lowe, David J.
      Balks, Megan R.
      Schipper, Louis A.
      Publisher
      IUSS
      Rights
      This article has been published in Proceedings of 19th World Congress of Social Science, Soil Solutions for a Changing World, 1-6 August 2010, Brisbane, Australia.
      Collections
      • Science and Engineering Papers [3116]
      Show full item record  

      Usage

      Downloads, last 12 months
      77
       
       

      Usage Statistics

      For this itemFor all of Research Commons

      The University of Waikato - Te Whare Wānanga o WaikatoFeedback and RequestsCopyright and Legal Statement