Aggregation characteristics and maturity of Peak District soils

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dc.contributor.authorBryan, Rorke B.
dc.date.accessioned2015-02-09T03:16:31Z
dc.date.available2015-02-09T03:16:31Z
dc.date.issued1969
dc.description.abstractSoil aggregation and aggregate stability are fundamental factors in determination of soil erodibility. The aggregation characteristics of soils in a region of high erosion potential are measured, and controlling factors examined. A relationship between increasing soil maturity and decreasing aggregate stability is described, and its significance in relation to Penck’s Aufbereitung concept is discussed.en_NZ
dc.format.mimetypeapplication/pdf
dc.identifier.citationBryan, R.B. (1969). Aggregation characteristics and maturity of Peak District soils. Earth Science Journal, 3(1), 1-12.en_NZ
dc.identifier.urihttps://hdl.handle.net/10289/9144
dc.publisherWaikato Geological Society, The University of Waikatoen_NZ
dc.relation.ispartofseriesEarth Science Journalen_NZ
dc.rights© 1969 Waikato Geological Society, The University of Waikato. All items in Research Commons are provided only to permit fair dealing for the purposes of research or private study. They are protected by copyright with all rights reserved unless otherwise indicated.en_NZ
dc.titleAggregation characteristics and maturity of Peak District soilsen_NZ
dc.typeJournal Articleen_NZ
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Volume 3, Number 1, 1969